Coiled - Morobe/EH (None - 0 BP)
Laminated ware - Carolines ( - BP)
Polynesian Plainware (2650 - 1700 BP)
Non-coiled - Morobe (500 - 0 BP)
Early Lapita Solomons (3000 - 2500 BP)
Middle Lapita North Solomons (2500 - 2200 BP)
Recent North Solomons (300 - 0 BP)
Early East PNG (4000 - 3000 BP)
Transitional Far Western (2350 - 1900 BP)
Ancestral East PNG (1700 - 500 BP)
North PNG Lapita (4000 - 2000 BP)
Non-coiled West Sepik (500 - 0 BP)
Non-coiled East Sepik (500 - 0 BP)
Coiled West Sepik (500 - 0 BP)
Coiled East Sepik (500 - 0 BP)
Non-coiled Solomons (500 - 0 BP)
Non-coiled Central (500 - 0 BP)
Early Pre-Latte (3500 - 2500 BP)
Intermediate Pre-Latte (2500 - 1600 BP)
Transitional Marianas (1600 - 1000 BP)
Latte plainware (1000 - 429 BP)
West Carolines Calcareous/Volcanic Sand (3000 - 600 BP)
Palau blackware (2300 - 2300 BP)
Palau grog ware (2500 - 200 BP)
Yap laminated ware (1100 - 0 BP)
Nan Madol Plainware (1000 - 800 BP)
East Carolines Calcareous (2500 - 1000 BP)
Late Post Lapita Manus (1600 - 900 BP)
Fiji Lapita (Sigatoka) (3200 - 2100 BP)
Loyalty Island Post-Lapita (2800 - 2500 BP)
Lapita Vanuatu (3000 - 2700 BP)
Late Port Moresby (300 - 0 BP)
Middle Port Moresby (1200 - 300 BP)
Red Slip Gulf (1600 - 1200 BP)
Early Port Moresby (2000 - 2100 BP)
Early Mailu Is. (2000 - 1500 BP)
South PNG Lapita (2900 - 2200 BP)
Middle Lapita (3140 - 2950 BP)
Plainware Santa Cruz (2700 - 2000 BP)
Sinapupu imported (2100 - 800 BP)
Western Solomons Incised-Impressed (1000 - 0 BP)
Settlement Marquesa (1250 - 850 BP)
Expansion Period Marquesas (650 - 350 BP)
Admiralty Post-Lapita (1800 - 800 BP)
Admiralty Historical (800 - 0 BP)
Post Lapita Buka (2200 - 0 BP)
Early Shortland (1500 - 1000 BP)
Middle Shortland (1000 - 300 BP)
Post-Lapita Solomons (2500 - 0 BP)
Northern New Caledonia Post-Lapita (2900 - 0 BP)
Southern New Caledonia Post-Lapita (2900 - 0 BP)
Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP)
Post-Lapita Erromango and Aneityum (2800 - 2000 BP)
Post-Lapita Banks (2700 - 2000 BP)
Post-Lapita Malakula (2700 - 0 BP)
Late Malakula ware (600 - 0 BP)
Maluku European era (1000 - 0 BP)
Early Metal Age (North Maluku) (2500 - 1000 BP)
Neolithic red-slipped (3350 - 2500 BP)
Coiled Maluku Tengah (1000 - 0 BP)
Non-coiled Maluku Tengah (1000 - 0 BP)
Early Metal Age Maluku Tengah (2300 - 1000 BP)
Early Maluku Tengah (3150 - 2300 BP)
Futuna Island Wikidata ID: Q664321
Wallis Islands Wikidata ID: Q4338915
Samoan Islands Wikidata ID: Q162126
Manus Province Wikidata ID: Q874935
Mariana Islands Wikidata ID: Q153732
Guam Island Wikidata ID: Q16635
Admiralty Islands Wikidata ID: Q119230
Morobe Province Wikidata ID: Q853664
Eastern Highlands Province Wikidata ID: Q849812
| None (0) | Minor (1) | Few (2) | Common (3) | Frequent (4) | Major (5) | Very Dominant (6) |
| 0% | 0-5% | 5-15% | 15-30 % | 30-50% | 50-70% | 70-100% |
| Name | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics/ Region |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr327 | 0 | 1 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microphaneritic |
| Alofi andesitic | 0 | 1 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | NE Melanesia |
| tpr324 | 0 | 1 | 5 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| Futuna feldspathic | 0 | 1 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | NE Melanesia |
| tpr325 | 0 | 1 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, lathwork |
| Futuna lithic | 0 | 1 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | NE Melanesia |
| tpr326 | 0 | 1 | 3 | 4 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| Futana ferromagnesian | 0 | 1 | 2 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | NE Melanesia |
| tpr127 | 0 | 1 | 4 | 2 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
| Buka microgranular | 0 | 0 | 3 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Solomons |
| tpr131 | 0 | 1 | 6 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | microlitic, felsitic, microphaneritic, chert |
| New Ireland cherty feldspathic | 0 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr132 | 6 | 0 | 3 | 2 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, microphaneritic |
| New Ireland hybrid | 3 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr133 | 0 | 1 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | microphaneritic |
| Exotic New Ireland lithic | 0 | 1 | 2 | 3 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | Bismarck |
| tpr134 | 1 | 0 | 2 | 5 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| TLTF olivine placer | 0 | 0 | 0 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr193 | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| Boduna feldspathic | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr134a | 2 | 0 | 3 | 5 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| TLTF placer | 0 | 0 | 2 | 4 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr178a | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| TLTF feldspathic | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr103 | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| New Ireland volcanic sand | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr104 | 1 | 0 | 1 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| New Ireland pyroxenic placer | 0 | 0 | 1 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr105 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| New Ireland calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr106 | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Exotic New Ireland quartz-calcite | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr194 | 2 | 1 | 1 | 4 | 0 | 6 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| Arawe placer | 0 | 0 | 1 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr195 | 6 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| Watom hybrid | 3 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr196 | 0 | 0 | 3 | 4 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Watom placer | 0 | 0 | 2 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr198 | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Watom feldspathic | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr315 | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic mica | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr316 | 0 | 0 | 6 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| Tanga feldspathic pyroxenic | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr318 | 2 | 0 | 2 | 5 | 1 | 6 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| Tanga pyroxene opaque placer | 0 | 0 | 1 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr319 | 0 | 0 | 1 | 2 | 0 | 6 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| Tanga opaque placer | 0 | 0 | 0 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr320 | 3 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, felsitic, vitric |
| Tanga lithic hybrid | 2 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Bismarck |
| tpr321 | 0 | 0 | 3 | 2 | 2 | 6 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| Exotic Tanga hornblendic hybrid | 0 | 0 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Bismarck |
| tpr322 | 0 | 0 | 6 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| Tanga hornblendic pyroxenic | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr463 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| New Britain calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr464 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| New Britain opaque | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr465 | 4 | 2 | 6 | 4 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | na |
| Kreslo feldspathic | 1 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr466 | 0 | 1 | 3 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | na |
| Kreslo lithic | 0 | 1 | 3 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Bismarck |
| tpr467 | 0 | 0 | 2 | 6 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Kreslo pyroxenic placer | 0 | 0 | 2 | 4 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr468 | 3 | 2 | 3 | 5 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Kreslo opaque placer | 0 | 0 | 1 | 1 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr107 | 0 | 0 | 6 | 4 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| New Ireland feldspathic-pyroxenic | 0 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr108 | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| New Ireland placer beach | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr192 | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| Garua feldspathic | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr135 | 0 | 0 | 4 | 4 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Kolombangara pyroxenic | 0 | 0 | 3 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr137 | 5 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Kolombangara feldspathic hybrid | 5 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr172 | 0 | 1 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric, felsitic, microphaneritic |
| Taumako andesitic | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Solomons |
| tpr173 | 0 | 0 | 4 | 6 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Taumako pyroxenic placer | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr128 | 0 | 1 | 6 | 4 | 1 | 2 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic, microlitic |
| Buka plagioclase pyroxene | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr101 | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland feldspathic non-placer | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr102 | 0 | 0 | 3 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland pyroxene rich-placer | 0 | 0 | 3 | 3 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr102a | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| New Ireland placer | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr178 | 0 | 1 | 4 | 3 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| Bismarck pyroxenic | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
| tpr179 | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, lathwork |
| Bismarck feldspathic | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Bismarck |
| tpr180 | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Bismarck lithic | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Bismarck |
| tpr313 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Tanga calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr317 | 0 | 0 | 2 | 6 | 0 | 3 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| Tanga pyroxene placer | 0 | 0 | 1 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr323 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Futuna/Uvea calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | NE Melanesia |
| tpr328 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Uvea basaltic lithic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | NE Melanesia |
| tpr289 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Savaii basaltic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr294 | 0 | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| Samoan colluvium | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr290a | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric |
| Samoan crushed microlitic lithic | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Samoa |
| tpr292 | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| Samoan ferromagnesian stream | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Samoa |
| tpr295 | 0 | 0 | 1 | 5 | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Samoan ferromagnesian beach | 0 | 0 | 0 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Samoa |
| tpr291 | 3 | 0 | 2 | 3 | 1 | 3 | 3 | 1 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Samoan lithic | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Samoa |
| tpr290b | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Samoan crushed lathwork lithic | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Samoa |
| tpr293a | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic |
| Samoan felsitic trachytic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr293b | 1 | 0 | 2 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork, vitric |
| Samoan microlitic trachytic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Samoa |
| tpr294a | 0 | 0 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic A | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr294b | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic |
| Samoan basaltic lithic B | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr294c | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic C | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr294d | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| Samoan basaltic lithic D | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr291b | 6 | 0 | 1 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | lathwork, vitric |
| Samoan calcareous | 5 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Samoa |
| tpr291a | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, lathwork |
| Samoan hybrid vitric | 1 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Samoa |
| tpr295b | 2 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| Samoan ferromagnesian lithic | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Samoa |
| tpr295a | 3 | 1 | 1 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| Samoan ferromagnesian crystal | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Samoa |
| tpr1 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| Saipan hybrid sand | 6 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Marianas |
| tpr3 | 6 | 3 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| Saipan hybrid | 6 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Marianas |
| tpr4 | 3 | 5 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | limeclast, felsitic, microlitic |
| Saipan quartz-rich | 2 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Marianas |
| tpr7 | 6 | 3 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| Saipan hybrid quartz | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Marianas |
| tpr22 | 1 | 3 | 4 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic |
| Saipan quartzose | 0 | 3 | 3 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | Marianas |
| tpr8 | 5 | 4 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic |
| Saipan hybrid quartzose | 4 | 3 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Marianas |
| tpr10 | 0 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| Saipan dacitic | 0 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Marianas |
| tpr11 | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| Saipan dacitic-vitric | 0 | 1 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Marianas |
| tpr12 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| Saipan vitric | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Marianas |
| tpr13 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric, felsitic |
| Saipan feldspar andesitic | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Marianas |
| tpr15 | 0 | 0 | 4 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic, felsitic |
| Saipan andesitic | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Marianas |
| tpr19 | 0 | 0 | 5 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| Guam vitric andesitic | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Marianas |
| tpr2 | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| Saipan volcanic | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Marianas |
| tpr20 | 0 | 0 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Guam lithic andesitic | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Marianas |
| tpr21 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Guam lithic hi andesitic | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Marianas |
| tpr25 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| Guam vitric | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Marianas |
| tpr28 | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| Saipan andesitic | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Marianas |
| tpr5 | 0 | 4 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| Saipan dacitic | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Marianas |
| tpr6 | 0 | 1 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, felsitic, vitric |
| Marianas andesitic | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Marianas |
| tpr35 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| Yap hybrid lithic metavolcanic | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Carolines |
| tpr36 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| Yap hybrid | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Carolines |
| tpr38 | 6 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | metavolcanic |
| Yap hybrid calcareous | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Carolines |
| tpr43 | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic |
| Yap hybrid metavolcanic | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Carolines |
| tpr51 | 5 | 0 | 3 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Palau hybrid type III | 3 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Carolines |
| tpr52 | 4 | 0 | 2 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| Palau hybrid type IV | 1 | 0 | 0 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Carolines |
| tpr53 | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic, felsitic |
| Palau lithic type V | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Carolines |
| tpr39 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| Yap grog | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | Carolines |
| tpr41 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 3 | chert |
| Palau-Yap quartzose grog | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | Carolines |
| tpr49 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| Palau grog type A/I | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | Carolines |
| tpr50 | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, vitric, microlitic |
| Palau grog type B/C/D | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 1 | Carolines |
| tpr54 | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | vitric, microlitic |
| Palau grog type II | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | Carolines |
| tpr272 | 0 | 0 | 4 | 0 | 1 | 2 | 0 | 0 | 4 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| Yap metavolcanic | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | Carolines |
| tpr34 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| Yap natural metavolcanic type A | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Carolines |
| tpr42 | 0 | 6 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | microphaneritic |
| Yap quartzose | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Carolines |
| tpr493 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 6 | lathwork, vitric |
| Pohnpei grog | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 4 | Carolines |
| tpr494 | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| Pohnpei placer | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Carolines |
| tpr210 | 6 | 0 | 3 | 2 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, lathwork |
| Pohnpei hybrid | 5 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Carolines |
| tpr45 | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| Chuuk calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Carolines |
| tpr492 | 4 | 0 | 3 | 3 | 0 | 1 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| Kosrae calcareous | 3 | 0 | 1 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | Carolines |
| tpr374 | 1 | 1 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| Niuatoputapu lithic | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Tonga |
| tpr375 | 0 | 1 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| Niuatoputapu lithic-placer | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Tonga |
| tpr376 | 0 | 1 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| Niuatoputapu placer | 0 | 0 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Tonga |
| tpr377 | 2 | 1 | 2 | 6 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Niuatoputapu hybrid | 1 | 0 | 1 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr378 | 6 | 0 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Niuatoputapu calcareous | 5 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr379 | 0 | 0 | 3 | 6 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| Vava'u pyroxenic | 0 | 0 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr380 | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, felsitic, vitric |
| Vava'u parially placered | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Tonga |
| tpr381 | 1 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, felsitic, vitric |
| Vava'u lithic | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Tonga |
| tpr429 | 0 | 0 | 3 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Lifuka pyroxenic | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Tonga |
| tpr430 | 4 | 1 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Lifuka partially pyroxenic | 0 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Tonga |
| tpr431 | 2 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | na |
| Lifuka lithic | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Tonga |
| tpr436 | 0 | 0 | 4 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| Ata vitric | 0 | 0 | 4 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Tonga |
| tpr437 | 0 | 3 | 6 | 4 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, plutonite, vitric |
| Eua gabbroic | 0 | 1 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr440 | 0 | 1 | 3 | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Tongatapu partial placer | 0 | 0 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr379a | 0 | 0 | 2 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| Vava'u opaque | 0 | 0 | 2 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr426 | 3 | 1 | 2 | 6 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Haapi placer | 0 | 0 | 1 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr427 | 1 | 0 | 1 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Haapi opaque | 1 | 0 | 1 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr428 | 0 | 1 | 3 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Pukatoalo pyroxenic | 0 | 1 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr438 | 0 | 1 | 3 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Tongatapu placer | 0 | 0 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr439 | 3 | 1 | 3 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | na |
| Tongatapu hybrid | 3 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Tonga |
| tpr208 | 0 | 4 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| Tonga unplacered | 0 | 4 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr209 | 2 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microlitic |
| Tonga quartz-free placer | 2 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Tonga |
| tpr296 | 0 | 5 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 1 | 1 | 1 | 3 | 0 | quartzite, amphibolite, tectonite, chert |
| New Caledonian quartzose | 0 | 4 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | New Caledonia |
| tpr297 | 6 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 2 | 3 | 0 | quartzite, chert, amphibolite |
| New Caledonian hybrid quartzose | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | New Caledonia |
| tpr298 | 4 | 3 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | quartzite, amphibolite, tectonite |
| New Caledonian quartzose placer | 0 | 2 | 2 | 2 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | New Caledonia |
| tpr299 | 0 | 4 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 2 | 1 | 2 | 6 | 0 | chert, quartzite, tectonite, argillitic, amphibolite |
| New Caledonian lithic quartzose | 0 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | New Caledonia |
| tpr301 | 6 | 3 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 5 | 0 | chert, tectonite, quartzite, vitric |
| New Caledonian hybrid lithic quartzose | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | New Caledonia |
| tpr302 | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 1 | 1 | 0 | 2 | 4 | 0 | quartzite, amphibolite, plutonite, tectonite |
| New Caledonian quartzose-ophiolitic | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 4 | 0 | New Caledonia |
| tpr303 | 5 | 3 | 3 | 3 | 2 | 2 | 0 | 0 | 0 | 1 | 1 | 3 | 3 | 0 | quartzite, tectonite, microphaneritic, amphibolite, plutonite, chert |
| New Caledonian hybrid quartzose-ophiolitic | 1 | 1 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | New Caledonia |
| tpr304 | 3 | 2 | 1 | 1 | 1 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | na |
| New Caledonian quartzose-ophiolitic placer | 3 | 2 | 1 | 1 | 1 | 5 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | New Caledonia |
| tpr305 | 0 | 2 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | microlitic, quartzite, tectonite |
| New Caledonian basaltic | 0 | 1 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 1 | 0 | New Caledonia |
| tpr306 | 0 | 0 | 2 | 4 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic, vitric, plutonite |
| New Caledonian basaltic placer | 0 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | New Caledonia |
| tpr307 | 2 | 1 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | microlitic, chert, argillitic, quartzite |
| New Caledonian hybrid basaltic placer | 2 | 1 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | New Caledonia |
| tpr308 | 0 | 2 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | microlitic, serpentinite, chert |
| New Caledonian plagiogranite | 0 | 2 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | New Caledonia |
| tpr309 | 5 | 2 | 3 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | amphibolite, quartzite |
| New Caledonian hybrid amphibolite | 5 | 1 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | New Caledonia |
| tpr310 | 6 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | serpentinite |
| New Caledonian hybrid ultramafic | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | New Caledonia |
| tpr311 | 6 | 0 | 1 | 1 | 0 | 6 | 0 | 0 | 0 | 0 | 4 | 1 | 1 | 0 | serpentinite, chert |
| New Caledonian hybrid ultramafic placer | 1 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | New Caledonia |
| tpr312 | 6 | 0 | 1 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| New Caledonian calcareous | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | New Caledonia |
| tpr296b | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| New Caledonian feldspathic | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | New Caledonia |
| tpr296a | 0 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | quartzite, vitric, plutonite |
| New Caledonian amphibolic | 0 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | New Caledonia |
| tpr310a | 0 | 2 | 6 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 5 | 1 | 0 | vitric, plutonite, metavolcanic, amphibolite, quartzite, chert, phyllite |
| New Caledonian ultramafic | 0 | 1 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | New Caledonia |
| tpr249 | 4 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | limeclast, microlitic, felsitic, vitric, microphaneritic |
| Malakula limeclast hybrid | 3 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr233 | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| Efate standard | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr235 | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| Efate lithic-poor | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr207 | 2 | 3 | 3 | 6 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| Exotic Tonga pyroxenic placer | 0 | 1 | 1 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Tonga |
| tpr462 | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| Exotic Tuam lithic | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | PNG |
| tpr480 | 4 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| Exotic Tuam pyroxenic hybrid | 3 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | PNG |
| tpr481 | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| Exotic Tuam pyroxenic | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | PNG |
| tpr161 | 0 | 0 | 4 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic |
| Santa Cruz hornblende-feldspar | 0 | 0 | 4 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr161a | 0 | 1 | 2 | 5 | 3 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Santa Cruz hornblende-pyroxene | 0 | 0 | 1 | 5 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr163 | 0 | 0 | 3 | 3 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| Santa Cruz lithic | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr164 | 0 | 0 | 3 | 4 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| Santa Cruz transitional | 0 | 0 | 2 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr165 | 0 | 0 | 3 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| Santa Cruz placer | 0 | 0 | 1 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr166 | 4 | 0 | 2 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| Santa Cruz hybrid lithic | 1 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr167 | 4 | 0 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| Santa Cruz hybrid transitional | 1 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr168 | 4 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Santa Cruz hybrid placer | 2 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Vanuatu |
| tpr245 | 6 | 0 | 2 | 1 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| Tikopia calcareous | 6 | 0 | 1 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Vanuatu |
| tpr241 | 0 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| Vanikolo-Tikopia feldspathic | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr242 | 0 | 0 | 4 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| Vanikolo-Tikopia opaque-rich | 0 | 0 | 4 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr243 | 0 | 0 | 4 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| Vanikolo-Tikopia lithic | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| tpr501 | 0 | 4 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | metavolcanic |
| Choiseul quartzose feldspathic | 0 | 4 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr502 | 1 | 1 | 3 | 2 | 5 | 3 | 0 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | metavolcanic |
| Choiseul amphibolic | 0 | 0 | 1 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr503 | 1 | 2 | 4 | 2 | 4 | 3 | 0 | 0 | 0 | 2 | 0 | 3 | 0 | 0 | metavolcanic |
| Choiseul amphibole feldspathic | 0 | 1 | 4 | 0 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | Solomons |
| tpr504 | 2 | 1 | 2 | 1 | 6 | 3 | 0 | 0 | 0 | 1 | 0 | 2 | 0 | 0 | metavolcanic |
| Choiseul amphibolic hybrid | 0 | 0 | 1 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr153 | 6 | 1 | 1 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Choiseul calcareous | 6 | 1 | 1 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Solomons |
| tpr138 | 0 | 2 | 3 | 2 | 5 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| Exotic Kolombangara hornblendic-hypabassal | 0 | 1 | 2 | 1 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | Solomons |
| tpr23 | 6 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Mariana calcareous | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Marianas |
| tpr250 | 0 | 0 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic, microlitic, vitric |
| Malakula pyribole-poor | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Vanuatu |
| tpr260 | 0 | 0 | 4 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic, microlitic, vitric |
| Malakula med lithic | 0 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| tpr251 | 0 | 0 | 3 | 3 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, microlitic, vitric, microphaneritic |
| Malakula pyroxenic lithic | 0 | 0 | 3 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| tpr216 | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | quartzite, plutonite, metavolcanic |
| Exotic Malo chrome spinel | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | Vanuatu |
| tpr217 | 0 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric, felsitic |
| Malo feldspathic | 0 | 0 | 4 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr218 | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric, felsitic |
| Malo pyroxenic | 0 | 0 | 2 | 4 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr219 | 0 | 0 | 3 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric, felsitic |
| Santo-Malo lithic | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| tpr222a | 0 | 0 | 1 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Erromango olivine beach | 0 | 0 | 1 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Vanuatu |
| tpr225 | 0 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| Efate unplacered | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr226 | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| Efate partially placered | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr227 | 6 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| Efate hybrid | 1 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr228 | 0 | 0 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| Efate pyroxenic placer | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr229 | 0 | 0 | 3 | 3 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| Efate opaque-rich placer | 0 | 0 | 1 | 2 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr230 | 3 | 4 | 2 | 2 | 3 | 1 | 0 | 1 | 1 | 1 | 1 | 2 | 3 | 0 | metavolcanic, tectonite |
| Exotic Efate metasedimentary quartzose | 0 | 4 | 2 | 1 | 2 | 1 | 0 | 1 | 1 | 1 | 1 | 1 | 2 | 0 | Vanuatu |
| tpr231 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | chert, felsitic |
| Exotic Efate quartzose hybrid | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | Vanuatu |
| tpr232 | 0 | 1 | 5 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| Exotic Efate feldspathic hornblendic | 0 | 1 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr264 | 4 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, microlitic, vitric, microphaneritic |
| Malakula hybrid lithic | 4 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr266 | 0 | 0 | 1 | 4 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microlitic, microphaneritic |
| Malakula opaque-rich | 0 | 0 | 0 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr268 | 6 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| Aneityum hybrid type A | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Vanuatu |
| tpr269 | 4 | 0 | 2 | 6 | 0 | 6 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, lathwork |
| Aneityum hybrid olivine placer type B | 0 | 0 | 0 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Vanuatu |
| tpr444 | 6 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| Malakula calcareous | 6 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Vanuatu |
| tpr445 | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| Exotic Vao vitric | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr37 | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| Yap natural metavolcanic type D | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Carolines |
| tpr441 | 0 | 0 | 1 | 5 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Marquesan beach placer | 0 | 0 | 1 | 4 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Marquesa |
| tpr442 | 0 | 0 | 4 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Marquesan beach feldspathic pyroxenic | 0 | 0 | 4 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Marquesa |
| tpr171 | 0 | 5 | 4 | 2 | 2 | 1 | 0 | 1 | 0 | 1 | 0 | 3 | 2 | 0 | microphaneritic, felsitic, microlitic, siltstone, tectonite, chert |
| Rewa Delta orogen | 0 | 3 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | Fiji |
| tpr100 | 0 | 0 | 4 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| Mussau type K | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr92 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Mussau type A | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr93 | 6 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | felsitic, vitric, chert |
| Mussau type B | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr94 | 6 | 1 | 1 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| Mussau type CD | 0 | 0 | 1 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Bismarck |
| tpr95 | 0 | 0 | 6 | 0 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| Mussau type E | 0 | 0 | 5 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr96 | 0 | 1 | 5 | 2 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| Mussau type F | 0 | 1 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Bismarck |
| tpr97 | 4 | 1 | 4 | 5 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| Mussau type G | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr98 | 5 | 0 | 2 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| Mussau type H | 5 | 0 | 2 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr99 | 1 | 2 | 5 | 3 | 1 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | felsitic, vitric |
| Mussau type J | 0 | 2 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Bismarck |
| tpr191a | 1 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| Manus andesitic placer | 0 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr191 | 0 | 0 | 4 | 4 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Manus andesitic | 0 | 0 | 3 | 3 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Bismarck |
| tpr125 | 6 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| Buka calcareous hybrid | 6 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr117 | 0 | 0 | 5 | 2 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Meinakapa feldspathic | 0 | 0 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr120 | 0 | 0 | 4 | 1 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| Kieta partial placer | 0 | 0 | 4 | 1 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Solomons |
| tpr121 | 0 | 0 | 4 | 2 | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| Kieta placer | 0 | 0 | 2 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr116 | 0 | 0 | 5 | 2 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Pidia manual | 0 | 0 | 4 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr119 | 0 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| Asio sparse-pyroxenic-vitric | 0 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Solomons |
| tpr115 | 0 | 0 | 5 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Pidia feldspathic-hornblendic natural | 0 | 0 | 5 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr118 | 0 | 0 | 4 | 4 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| Pidia modern | 0 | 0 | 4 | 4 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr112 | 0 | 0 | 6 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Paubake feldspathic non-placer manual | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr113 | 0 | 0 | 4 | 3 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Paubake partial placer manual | 0 | 0 | 4 | 3 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr114 | 0 | 0 | 3 | 4 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Paubake placer manual | 0 | 0 | 3 | 4 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr111 | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| Paubake feldspathic natural temper | 0 | 0 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr110 | 0 | 1 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| Shortland feldspathic | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr141 | 0 | 2 | 3 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| Roviana plainware A-opaque rich | 0 | 2 | 3 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Solomons |
| tpr142 | 3 | 1 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| Roviana plainware B-feldspathic | 0 | 1 | 4 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Solomons |
| tpr143 | 0 | 0 | 3 | 2 | 5 | 3 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | felsitic, vitric, microphaneritic |
| Roviana plainware C-hornblendic | 0 | 0 | 2 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Solomons |
| tpr144 | 0 | 1 | 2 | 2 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, vitric, microphaneritic |
| Roviana plainware D-lithic | 0 | 0 | 2 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Solomons |
| tpr136 | 0 | 0 | 2 | 2 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| Exotic Kolombangara hornblendic | 0 | 0 | 2 | 2 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| tpr150 | 6 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | na |
| Exotic Roviana quartz-calcite | 2 | 3 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Solomons |
| tpr146 | 0 | 0 | 3 | 3 | 4 | 5 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Vella Lavella type A-hornblende-pyroxene | 0 | 0 | 2 | 2 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr147 | 0 | 0 | 5 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Vella Lavella type B-brown hornblendic | 0 | 0 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr148 | 0 | 0 | 5 | 1 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Vella Lavella type C-green hornblendic | 0 | 0 | 3 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr149 | 0 | 0 | 2 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| Vella Lavella type D-hornblende poor | 0 | 0 | 1 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr151 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Roviana vitric | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Solomons |
| tpr152 | 0 | 3 | 3 | 3 | 0 | 4 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| Roviana quartzose | 0 | 3 | 3 | 2 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | Solomons |
| tpr271 | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 3 | 4 | 0 | 0 | 1 | 0 | 0 | plutonite |
| Markham Valley sericitic feldspathic | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | PNG |
| tpr255 | 0 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| Epi mafic lithic | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr236 | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| Efate lithic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr220 | 2 | 0 | 2 | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, lathwork, microlitic |
| Erromango pyroxenic | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr221 | 3 | 0 | 3 | 4 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric, microlitic |
| Erromango feldspathic non-placer | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr222 | 3 | 0 | 2 | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric, microlitic |
| Erromango olivine placer | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr280 | 0 | 1 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, felsitic, microlitic |
| Exotic Aneityum vitric quartz | 0 | 1 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Vanuatu |
| tpr214 | 1 | 0 | 5 | 4 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric, felsitic |
| Santo stream | 0 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr256 | 0 | 0 | 5 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| Banks volcanic | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | Vanuatu |
| tpr258 | 0 | 0 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Banks vitric | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Vanuatu |
| tpr252 | 0 | 0 | 3 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic, microlitic, vitric |
| Malakula hornblendic | 0 | 0 | 3 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Vanuatu |
| tpr270 | 0 | 5 | 5 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| PNG highlands quartz feldspar | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | PNG |
| tpr459 | 2 | 2 | 3 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic, vitric |
| Madang pyroxenic lithic | 0 | 0 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | PNG |
| tpr460 | 0 | 2 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic |
| Madang feldspathic lithic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | PNG |
| tpr274 | 1 | 1 | 3 | 6 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, lathwork |
| Huon pyroxenic | 0 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | PNG |
| tpr458 | 6 | 2 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| Huon calcareous | 5 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | PNG |
| tpr483 | 0 | 1 | 5 | 4 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, lathwork, microphaneritic, plutonite |
| Huon feldspathic lithic | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | PNG |
| tpr486 | 0 | 2 | 3 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, microphaneritic |
| Huon feldspathic pyroxenic | 0 | 2 | 3 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | PNG |
| tpr179a | 1 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | microlitic |
| Huon grog | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | PNG |
| tpr300 | 0 | 0 | 1 | 1 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 1 | microlitic |
| Huon ferruginous | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | PNG |
| tpr482 | 0 | 2 | 4 | 1 | 5 | 3 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | 0 | microphaneritic |
| Exotic Tuam amphibolic | 0 | 0 | 4 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | PNG |
| tpr83 | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic, lathwork |
| Halmahera volcanic | 0 | 0 | 4 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | Maluku |
| tpr63a | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Aru quartz-calcite | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Maluku |
| tpr63b | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Aru quartz-calcite | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Maluku |
| tpr63c | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Aru quartz-calcite | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Maluku |
| Slide | Fabric | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| IL_1_39 | tpr461 (Madang feldspathic hybrid) | Madang | Non-coiled - Madang ( - 0 BP) | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, microphaneritic |
| IL_1_55 | tpr484 (Huon quartzose) | Madang | Non-coiled - Madang ( - 0 BP) | 0 | 4 | 4 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| IL_1_37 | tpr485 (Madang placer) | Madang | Non-coiled - Madang ( - 0 BP) | 0 | 1 | 2 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| IL_1_21 | tpr458 (Huon calcareous) | Madang | Non-coiled - Madang ( - 0 BP) | 5 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_32_25 | tpr127 (Buka microgranular) | Buka | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
| WD_38_3 | tpr131 (New Ireland cherty feldspathic) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_1 | tpr131 (New Ireland cherty feldspathic) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_2 | tpr131 (New Ireland cherty feldspathic) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 1 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_7 | tpr131 (New Ireland cherty feldspathic) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 5 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_12 | tpr132 (New Ireland hybrid) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 3 | 0 | 3 | 2 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_9 | tpr132 (New Ireland hybrid) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 6 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_10 | tpr132 (New Ireland hybrid) | New Ireland | Early Far Western Lapita (3500 - 2770 BP) | 5 | 0 | 3 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, microphaneritic |
| WD_38_13 | tpr133 (Exotic New Ireland lithic) | North Bougainville? | Early Far Western Lapita (3500 - 2770 BP) | 0 | 1 | 2 | 3 | 2 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | microphaneritic |
| WD_38_14 | tpr134 (TLTF olivine placer) | TLTF or New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 1 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_38_15 | tpr134 (TLTF olivine placer) | TLTF or New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 0 | 4 | 1 | 4 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| JS_1_3 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| JS_1_6 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork, felsitic, vitric |
| JS_1_4 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| JS_1_5 | tpr193 (Boduna feldspathic) | New Britain | Early Far Western Lapita (3500 - 2770 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, lathwork |
| WD_31_16 | tpr103 (New Ireland volcanic sand) | New Ireland | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_31_17 | tpr104 (New Ireland pyroxenic placer) | New Ireland | Middle Far Western Lapita (3050 - 2300 BP) | 1 | 0 | 1 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| WD_31_19 | tpr104 (New Ireland pyroxenic placer) | New Ireland | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 1 | 5 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_31_13 | tpr105 (New Ireland calcareous) | New Ireland | Middle Far Western Lapita (3050 - 2300 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_31_14 | tpr106 (Exotic New Ireland quartz-calcite) | Admiralty | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 3 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_41_11 | tpr194 (Arawe placer) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 1 | 0 | 1 | 4 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_41_13 | tpr194 (Arawe placer) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 2 | 0 | 0 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_104_13 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 5 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_14 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 6 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_3 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 6 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_7 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 6 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_8 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 5 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_41_24 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 5 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_41_25 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 5 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_104_12 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_15 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_19 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_2 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_4 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_5 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 4 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_10 | tpr195 (Watom hybrid) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 3 | 0 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic, microlitic |
| WD_104_16 | tpr196 (Watom placer) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 2 | 4 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_104_18 | tpr196 (Watom placer) | New Britain | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 3 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_104_1 | tpr198 (Watom feldspathic) | New Britain-Solomons | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric, microlitic |
| WD_104_17 | tpr198 (Watom feldspathic) | New Britain-Solomons | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric, microlitic |
| WD_30_17 | tpr320 (Tanga lithic hybrid) | Unknown | Middle Far Western Lapita (3050 - 2300 BP) | 2 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, felsitic, vitric |
| WD_30_20 | tpr321 (Exotic Tanga hornblendic hybrid) | Feni | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_30_21 | tpr322 (Tanga hornblendic pyroxenic) | Feni | Middle Far Western Lapita (3050 - 2300 BP) | 0 | 0 | 4 | 4 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_41_9 | tpr192 (Garua feldspathic) | New Britain | Late Far Western Lapita (2980 - 1800 BP) | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| WD_41_10 | tpr192 (Garua feldspathic) | New Britain | Late Far Western Lapita (2980 - 1800 BP) | 0 | 1 | 5 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, vitric |
| WD_35_22 | tpr137 (Kolombangara feldspathic hybrid) | Solomons | Late Lapita Solomons (2700 - 1800 BP) | 5 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_105_3 | tpr172 (Taumako andesitic) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 1 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric, felsitic, microphaneritic |
| WD_105_4 | tpr172 (Taumako andesitic) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 1 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric, felsitic, microphaneritic |
| WD_105_6 | tpr172 (Taumako andesitic) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 1 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric, felsitic, microphaneritic |
| WD_105_7 | tpr172 (Taumako andesitic) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric, felsitic, microphaneritic |
| WD_105_1 | tpr173 (Taumako pyroxenic placer) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_105_2 | tpr173 (Taumako pyroxenic placer) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_105_5 | tpr173 (Taumako pyroxenic placer) | Taumako | Late Lapita Solomons (2700 - 1800 BP) | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_32_2 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_3 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Malasang (700 - 500 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_32_5 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_9 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Mararing (500 - 100 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_1 | tpr128 (Buka plagioclase pyroxene) | North Bougainville | Recent Buka (300 - 0 BP) | 0 | 0 | 5 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| WD_31_1 | tpr101 (New Ireland feldspathic non-placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_31_3 | tpr102 (New Ireland pyroxene rich-placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 4 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_31_10 | tpr102a (New Ireland placer) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_41_16 | tpr105 (New Ireland calcareous) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_31_23 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_41_19 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 4 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_41_21 | tpr107 (New Ireland feldspathic-pyroxenic) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_31_24 | tpr108 (New Ireland placer beach) | New Ireland | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_102_1 | tpr134 (TLTF olivine placer) | TLTF or New Britain | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 2 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_102_2 | tpr178 (Bismarck pyroxenic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 1 | 3 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_102_4 | tpr178 (Bismarck pyroxenic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 4 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_102_3 | tpr179 (Bismarck feldspathic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, lathwork |
| WD_102_5 | tpr180 (Bismarck lithic) | Anir | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 2 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| WD_33_1 | tpr313 (Tanga calcareous) | Tanga | Transitional Far Western (2350 - 1900 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_33_13 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 2 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_11 | tpr315 (Tanga feldspathic pyroxenic mica) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_33_5 | tpr316 (Tanga feldspathic pyroxenic) | Tanga | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_30_8 | tpr318 (Tanga pyroxene opaque placer) | Tanga | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 1 | 3 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| WD_30_2 | tpr317 (Tanga pyroxene placer) | Tanga not Boeng | Transitional Far Western (2350 - 1900 BP) | 0 | 0 | 1 | 6 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | lathwork, microlitic |
| FL_1_23 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| FL_1_24 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| FL_1_25 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitiric |
| FL_1_48 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, vitric |
| FL_1_49 | tpr295 (Samoan ferromagnesian beach) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 4 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric |
| FL_1_51 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| FL_1_50 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, vitric |
| FL_1_29 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| FL_1_26 | tpr290b (Samoan crushed lathwork lithic) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| FL_1_27 | tpr295 (Samoan ferromagnesian beach) | Upolu | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 3 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, vitric |
| WD_79_1 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_10 | tpr294b (Samoan basaltic lithic B) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic |
| WD_79_11 | tpr294b (Samoan basaltic lithic B) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic |
| WD_79_15 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_16 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_17 | tpr294c (Samoan basaltic lithic C) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_19 | tpr294d (Samoan basaltic lithic D) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_20 | tpr294d (Samoan basaltic lithic D) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_79_6 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_79_9 | tpr294b (Samoan basaltic lithic B) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_24 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_10 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_87_3 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_12 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_16 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_17 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_18 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_87_4 | tpr294a (Samoan basaltic lithic A) | Olomoana Mountain Tutuila | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_22_11 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, victric, lathwork |
| WD_22_22 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| WD_22_5 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork, vitric |
| WD_25_20 | tpr289 (Savaii basaltic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_25_17 | tpr294 (Samoan colluvium) | Aunu'u | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_25_14 | tpr294 (Samoan colluvium) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, lathwork |
| WD_25_11 | tpr293a (Samoan felsitic trachytic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic |
| WD_22_23 | tpr294 (Samoan colluvium) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_22_12 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, lathwork, vitric |
| WD_22_13 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_22_14 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_22_15 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_22_18 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_25_13 | tpr294 (Samoan colluvium) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_22_21 | tpr290a (Samoan crushed microlitic lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 5 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_24_1 | tpr291 (Samoan lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 1 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_24_13 | tpr291 (Samoan lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 3 | 0 | 1 | 3 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_24_18 | tpr291b (Samoan calcareous) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 6 | 0 | 1 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | lathwork, microlitic |
| WD_24_19 | tpr292 (Samoan ferromagnesian stream) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| WD_24_20 | tpr292 (Samoan ferromagnesian stream) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| WD_24_23 | tpr292 (Samoan ferromagnesian stream) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| WD_24_24 | tpr292 (Samoan ferromagnesian stream) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 5 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| WD_24_4 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 4 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork |
| WD_25_1 | tpr293b (Samoan microlitic trachytic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_23_18 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 3 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_23_13 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 3 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_22_8 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 5 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_22_7 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, microlitic |
| WD_22_6 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, microlitic |
| WD_25_8 | tpr293b (Samoan microlitic trachytic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_25_5 | tpr293b (Samoan microlitic trachytic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_23_24 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 3 | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork |
| WD_23_21 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 1 | 4 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork |
| WD_23_22 | tpr295 (Samoan ferromagnesian beach) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 0 | 3 | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| WD_22_10 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| WD_22_4 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_22_3 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 3 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, microlitic |
| WD_22_1 | tpr290b (Samoan crushed lathwork lithic) | Samoa | Samoa Polynesian Plainware (2500 - 1700 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, microlitic |
| FP_1_3 | tpr291a (Samoan hybrid vitric) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 1 | 0 | 0 | 2 | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, lathwork |
| FP_1_19 | tpr291a (Samoan hybrid vitric) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 2 | 0 | 0 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, lathwork |
| FP_1_2 | tpr291b (Samoan calcareous) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 5 | 0 | 0 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric |
| FP_1_14 | tpr291b (Samoan calcareous) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 6 | 0 | 1 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric |
| FP_1_11 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| FP_1_12 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, lathwork |
| FP_1_1 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 3 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork |
| FP_1_4 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 3 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork, vitric |
| FP_1_5 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| FP_1_9 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 1 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | lathwork |
| FP_1_10 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | Lathwork |
| FP_1_18 | tpr291 (Samoan lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 2 | 0 | 0 | 2 | 1 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| FP_1_7 | tpr295b (Samoan ferromagnesian lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 2 | 0 | 0 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | Lathwork, vitric |
| FP_1_13 | tpr295b (Samoan ferromagnesian lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | lathwork, vitric |
| FP_1_20 | tpr295b (Samoan ferromagnesian lithic) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitiric, lathwork |
| FP_1_8 | tpr295a (Samoan ferromagnesian crystal) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 1 | 0 | 0 | 2 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| FP_1_15 | tpr295a (Samoan ferromagnesian crystal) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 1 | 0 | 0 | 3 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| FP_1_16 | tpr295a (Samoan ferromagnesian crystal) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork |
| FL_1_4 | tpr295a (Samoan ferromagnesian crystal) | Upolu | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 0 | 3 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, vitric |
| WD_23_3 | tpr295a (Samoan ferromagnesian crystal) | Samoa | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 1 | 3 | 0 | 1 | 4 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_23_6 | tpr295a (Samoan ferromagnesian crystal) | Samoa | Samoa Eastern Lapita (2800 - 2700 BP) | 3 | 0 | 1 | 2 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_23_8 | tpr295a (Samoan ferromagnesian crystal) | Samoa | Samoa Eastern Lapita (2800 - 2700 BP) | 0 | 0 | 1 | 2 | 0 | 1 | 3 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_23_9 | tpr295a (Samoan ferromagnesian crystal) | Samoa | Samoa Eastern Lapita (2800 - 2700 BP) | 2 | 0 | 1 | 3 | 0 | 1 | 4 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_1_12 | tpr1 (Saipan hybrid sand) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_1_13 | tpr1 (Saipan hybrid sand) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 1 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_20 | tpr23 (Mariana calcareous) | Mariana | Early Pre-Latte (3500 - 2500 BP) | 6 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_1_23 | tpr3 (Saipan hybrid) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 3 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_15 | tpr4 (Saipan quartz-rich) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 3 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | limeclast |
| WD_8_23 | tpr7 (Saipan hybrid quartz) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 3 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_8_25 | tpr7 (Saipan hybrid quartz) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 3 | 1 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_14 | tpr7 (Saipan hybrid quartz) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 2 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_2 | tpr7 (Saipan hybrid quartz) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_7 | tpr7 (Saipan hybrid quartz) | Saipan | Early Pre-Latte (3500 - 2500 BP) | 6 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_1_1 | tpr1 (Saipan hybrid sand) | Saipan | Intermediate Pre-Latte (2500 - 1600 BP) | 6 | 1 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_19 | tpr22 (Saipan quartzose) | Saipan | Intermediate Pre-Latte (2500 - 1600 BP) | 1 | 3 | 3 | 2 | 0 | 2 | 0 | 1 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic |
| WD_6_9 | tpr8 (Saipan hybrid quartzose) | Saipan | Intermediate Pre-Latte (2500 - 1600 BP) | 5 | 3 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic |
| WD_6_17 | tpr8 (Saipan hybrid quartzose) | Saipan | Intermediate Pre-Latte (2500 - 1600 BP) | 4 | 4 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic |
| WD_2_4 | tpr4 (Saipan quartz-rich) | Saipan | Transitional Marianas (1600 - 1000 BP) | 2 | 5 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | limeclast, felsitic, microlitic |
| WD_2_14 | tpr10 (Saipan dacitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_2_13 | tpr11 (Saipan dacitic-vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| WD_2_12 | tpr11 (Saipan dacitic-vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| WD_2_6 | tpr11 (Saipan dacitic-vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_2_7 | tpr11 (Saipan dacitic-vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | felsitic |
| WD_2_11 | tpr11 (Saipan dacitic-vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_4_16 | tpr12 (Saipan vitric) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, felsitic |
| WD_4_24 | tpr15 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_4_18 | tpr15 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_4_21 | tpr15 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 3 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_4_5 | tpr15 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_4_8 | tpr15 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_7_16 | tpr19 (Guam vitric andesitic) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_7_19 | tpr19 (Guam vitric andesitic) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| WD_1_18 | tpr2 (Saipan volcanic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 3 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_1_16 | tpr2 (Saipan volcanic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 3 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_1_20 | tpr2 (Saipan volcanic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_7_23 | tpr20 (Guam lithic andesitic) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| WD_7_24 | tpr21 (Guam lithic hi andesitic) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_8_1 | tpr21 (Guam lithic hi andesitic) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_8_3 | tpr25 (Guam vitric) | Guam | Latte plainware (1000 - 429 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_4_11 | tpr28 (Saipan andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| WD_1_25 | tpr3 (Saipan hybrid) | Saipan | Latte plainware (1000 - 429 BP) | 6 | 3 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_2_16 | tpr5 (Saipan dacitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 4 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_2_1 | tpr5 (Saipan dacitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_2_3 | tpr5 (Saipan dacitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, felsitic |
| WD_2_22 | tpr5 (Saipan dacitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_4_1 | tpr6 (Marianas andesitic) | Saipan | Latte plainware (1000 - 429 BP) | 0 | 1 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, felsitic, vitric |
| WD_5_1 | tpr6 (Marianas andesitic) | Marianas | Latte plainware (1000 - 429 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, vitric |
| WD_5_3 | tpr6 (Marianas andesitic) | Marianas | Latte plainware (1000 - 429 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_5_4 | tpr6 (Marianas andesitic) | Marianas | Latte plainware (1000 - 429 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, vitric |
| WD_6_16 | tpr7 (Saipan hybrid quartz) | Saipan | Latte plainware (1000 - 429 BP) | 6 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_6_12 | tpr8 (Saipan hybrid quartzose) | Saipan | Latte plainware (1000 - 429 BP) | 4 | 4 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_10_14 | tpr35 (Yap hybrid lithic metavolcanic) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| WD_9_10 | tpr36 (Yap hybrid) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_9_12 | tpr36 (Yap hybrid) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_10_11 | tpr38 (Yap hybrid calcareous) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 6 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | metavolcanic |
| WD_10_2 | tpr43 (Yap hybrid metavolcanic) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic |
| WD_10_5 | tpr43 (Yap hybrid metavolcanic) | Yap | West Carolines Calcareous/Volcanic Sand (3000 - 600 BP) | 6 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic |
| WD_10_10 | tpr39 (Yap grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_10_6 | tpr39 (Yap grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_9_14 | tpr41 (Palau-Yap quartzose grog) | Yap | Palau grog ware (2500 - 200 BP) | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | chert |
| WD_10_9 | tpr41 (Palau-Yap quartzose grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 3 | chert |
| WD_9_1 | tpr41 (Palau-Yap quartzose grog) | Yap | Palau grog ware (2500 - 200 BP) | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | chert |
| WD_9_13 | tpr41 (Palau-Yap quartzose grog) | Yap | Palau grog ware (2500 - 200 BP) | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 2 | chert |
| WD_10_1 | tpr41 (Palau-Yap quartzose grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | na |
| WD_10_3 | tpr41 (Palau-Yap quartzose grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | na |
| WD_10_4 | tpr41 (Palau-Yap quartzose grog) | Palau | Palau grog ware (2500 - 200 BP) | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | na |
| WD_12_5 | tpr49 (Palau grog type A/I) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_12_7 | tpr49 (Palau grog type A/I) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_13_11 | tpr49 (Palau grog type A/I) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_13_14 | tpr49 (Palau grog type A/I) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_13_7 | tpr49 (Palau grog type A/I) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_13_10 | tpr50 (Palau grog type B/C/D) | Babeldoab | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_13_13 | tpr50 (Palau grog type B/C/D) | Babeldoab | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_13_15 | tpr50 (Palau grog type B/C/D) | Babeldoab | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_13_16 | tpr50 (Palau grog type B/C/D) | Babeldoab | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_13_17 | tpr50 (Palau grog type B/C/D) | Babeldoab | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_13_9 | tpr50 (Palau grog type B/C/D) | Babeldoab (or nearby) | Palau grog ware (2500 - 200 BP) | 0 | 2 | 3 | 1 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 3 | felsitic, microlitic |
| WD_9_4 | tpr272 (Yap metavolcanic) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| WD_9_5 | tpr272 (Yap metavolcanic) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 4 | 0 | 0 | metavolcanic |
| WD_9_7 | tpr272 (Yap metavolcanic) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| WD_9_8 | tpr272 (Yap metavolcanic) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| WD_10_12 | tpr34 (Yap natural metavolcanic type A) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | metavolcanic |
| WD_9_17 | tpr42 (Yap quartzose) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 6 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microphaneritic |
| WD_9_20 | tpr42 (Yap quartzose) | Yap | Yap laminated ware (1100 - 0 BP) | 0 | 6 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microphaneritic |
| FL_1_89 | tpr493 (Pohnpei grog) | Pohnpei | Nan Madol Plainware (1000 - 800 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 5 | Vitric, lathwork |
| FL_1_64 | tpr493 (Pohnpei grog) | Pohnpei | Nan Madol Plainware (1000 - 800 BP) | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 4 | vitric, lathwork |
| FL_1_65 | tpr493 (Pohnpei grog) | Pohnpei | Nan Madol Plainware (1000 - 800 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 5 | vitric, lathwork |
| FL_1_74 | tpr493 (Pohnpei grog) | Pohnpei | Nan Madol Plainware (1000 - 800 BP) | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 5 | vitric, lathwork |
| FL_1_75 | tpr494 (Pohnpei placer) | Pohnpei | Nan Madol Plainware (1000 - 800 BP) | 0 | 0 | 1 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, lathwork |
| WD_90_1 | tpr210 (Pohnpei hybrid) | Pohnpei | East Carolines Calcareous (2500 - 1000 BP) | 5 | 0 | 2 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_99_1 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_99_16 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_99_20 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_99_4 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_99_5 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_99_6 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_99_7 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_99_9 | tpr45 (Chuuk calcareous) | Chuuk | East Carolines Calcareous (2500 - 1000 BP) | 6 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| FL_1_78 | tpr210 (Pohnpei hybrid) | Pohnpei | East Carolines Calcareous (2500 - 1000 BP) | 5 | 0 | 2 | 1 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, lathwork |
| WD_71_14 | tpr379a (Vava'u opaque) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 2 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_71_15 | tpr381 (Vava'u lithic) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_71_22 | tpr381 (Vava'u lithic) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_71_16 | tpr379 (Vava'u pyroxenic) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_71_23 | tpr379 (Vava'u pyroxenic) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 1 | 0 | 2 | 6 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric, felsitic |
| WD_71_19 | tpr380 (Vava'u parially placered) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric, felsitic |
| WD_71_24 | tpr380 (Vava'u parially placered) | Vava'u | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric, felsitic |
| WD_71_26 | tpr440 (Tongatapu partial placer) | Tongatapu | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 1 | 4 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_73_17 | tpr430 (Lifuka partially pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 4 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_18 | tpr429 (Lifuka pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_19 | tpr430 (Lifuka partially pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_20 | tpr430 (Lifuka partially pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_22 | tpr429 (Lifuka pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_23 | tpr429 (Lifuka pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_25 | tpr430 (Lifuka partially pyroxenic) | Lifuka | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_72_21 | tpr436 (Ata vitric) | Ata | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 4 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_72_20 | tpr436 (Ata vitric) | Ata | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 0 | 4 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| WD_72_17 | tpr437 (Eua gabbroic) | Eua | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 1 | 4 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, plutonite, vitric |
| WD_72_18 | tpr437 (Eua gabbroic) | Eua | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 1 | 3 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, plutonite, vitric |
| WD_72_19 | tpr437 (Eua gabbroic) | Eua | Tonga Polynesian Plainware (2600 - 1700 BP) | 0 | 3 | 6 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, plutonite, vitric |
| WD_71_21 | tpr381 (Vava'u lithic) | Kapa | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_71_1 | tpr439 (Tongatapu hybrid) | Tongatapu | Tonga Eastern Lapita (2800 - 2600 BP) | 3 | 1 | 2 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_71_2 | tpr439 (Tongatapu hybrid) | Tongatapu | Tonga Eastern Lapita (2800 - 2600 BP) | 3 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric, felsitic |
| WD_71_4 | tpr440 (Tongatapu partial placer) | Tongatapu | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 0 | 3 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, felsitic, vitric |
| WD_71_7 | tpr438 (Tongatapu placer) | Tongatapu | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_71_8 | tpr438 (Tongatapu placer) | Tongatapu | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_73_1 | tpr426 (Haapi placer) | Ha'api | Tonga Eastern Lapita (2800 - 2600 BP) | 2 | 0 | 1 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_73_2 | tpr426 (Haapi placer) | Ha'apai | Tonga Eastern Lapita (2800 - 2600 BP) | 1 | 1 | 2 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_73_3 | tpr426 (Haapi placer) | Ha'api | Tonga Eastern Lapita (2800 - 2600 BP) | 2 | 0 | 1 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_73_4 | tpr426 (Haapi placer) | Ha'apai | Tonga Eastern Lapita (2800 - 2600 BP) | 3 | 0 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_73_6 | tpr426 (Haapi placer) | Ha'apai | Tonga Eastern Lapita (2800 - 2600 BP) | 2 | 0 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_73_9 | tpr428 (Pukatoalo pyroxenic) | Ha'ano | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 1 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_73_10 | tpr428 (Pukatoalo pyroxenic) | Ha'ano | Tonga Eastern Lapita (2800 - 2600 BP) | 0 | 1 | 3 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_89_22 | tpr208 (Tonga unplacered) | Tongatapu | Tonga Early Eastern Lapita (2900 - 2800 BP) | 0 | 4 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_5 | tpr209 (Tonga quartz-free placer) | Tongatapu | Tonga Early Eastern Lapita (2900 - 2800 BP) | 2 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microlitic |
| WD_71_5 | tpr440 (Tongatapu partial placer) | Tongatapu | Tonga Early Eastern Lapita (2900 - 2800 BP) | 0 | 1 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_71_6 | tpr438 (Tongatapu placer) | Tongatapu | Tonga Early Eastern Lapita (2900 - 2800 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felstic, vitric |
| WD_71_9 | tpr438 (Tongatapu placer) | Tongatapu | Tonga Early Eastern Lapita (2900 - 2800 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_73_7 | tpr426 (Haapi placer) | Ha'apai | Tonga Early Eastern Lapita (2900 - 2800 BP) | 0 | 1 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_73_8 | tpr426 (Haapi placer) | Ha'apai | Tonga Early Eastern Lapita (2900 - 2800 BP) | 2 | 0 | 1 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_27_11 | tpr298 (New Caledonian quartzose placer) | New Caledonia | Southern Lapita (3050 - 2750 BP) | 4 | 2 | 2 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | plutonite, victric, quartzite |
| WD_27_10 | tpr296b (New Caledonian feldspathic) | New Caledonia | Southern Lapita (3050 - 2750 BP) | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_26_1 | tpr297 (New Caledonian hybrid quartzose) | New Caledonia | Southern Lapita (3050 - 2750 BP) | 1 | 5 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | metavolcanic, amphibolite, tectonite, quartzite |
| WD_27_5 | tpr303 (New Caledonian hybrid quartzose-ophiolitic) | Grand Terre | Southern Lapita (3050 - 2750 BP) | 5 | 2 | 2 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | vitric, quartzite, metravolcanic |
| WD_27_8 | tpr310a (New Caledonian ultramafic) | New Caledonia | Podtanean (2900 - 2200 BP) | 0 | 2 | 6 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 1 | 0 | metavolcanic, amphibolite, tectonite, quartzite |
| WD_27_9 | tpr296 (New Caledonian quartzose) | New Caledonia | Podtanean (2900 - 2200 BP) | 0 | 4 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 3 | 0 | metavolcanic, amphibolite, tectonite, quartzite |
| WD_27_6 | tpr296a (New Caledonian amphibolic) | New Caledonia | Podtanean (2900 - 2200 BP) | 0 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | quartzite, vitric, plutonite |
| WD_27_7 | tpr296a (New Caledonian amphibolic) | New Caledonia | Podtanean (2900 - 2200 BP) | 0 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 2 | 0 | quartzite, vitric, plutonite |
| WD_26_15 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Podtanean (2900 - 2200 BP) | 0 | 3 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 5 | 0 | metavolcanic, amphibolite, tectonite, quartzite |
| WD_26_22 | tpr302 (New Caledonian quartzose-ophiolitic) | Grand Terre | Podtanean (2900 - 2200 BP) | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 4 | 0 | quartzite, amphibolite, plutonite, tectonite |
| WD_58_24 | tpr249 (Malakula limeclast hybrid) | Malakula | Malua Ware (2700 - 2500 BP) | 3 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | limeclast, microlitic, felsitic, vitric, microphaneritic |
| WD_91_16 | tpr207 (Exotic Tonga pyroxenic placer) | exotic | Lapita (3500 - 2300 BP) | 0 | 3 | 3 | 4 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic |
| WD_89_8 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 2 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_12 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 1 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_16 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 3 | 2 | 5 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_15 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 2 | 1 | 1 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_1 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 2 | 1 | 5 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_14 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 2 | 2 | 5 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_21 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 2 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_18 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_19 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 1 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_89_27 | tpr207 (Exotic Tonga pyroxenic placer) | unknown | Lapita (3500 - 2300 BP) | 0 | 1 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| IL_2_5 | tpr462 (Exotic Tuam lithic) | ? | Lapita (3500 - 2300 BP) | 4 | 0 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| IL_2_8 | tpr480 (Exotic Tuam pyroxenic hybrid) | ? | Lapita (3500 - 2300 BP) | 3 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | lathwork, microlitic |
| IL_2_7 | tpr480 (Exotic Tuam pyroxenic hybrid) | ? | Lapita (3500 - 2300 BP) | 4 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microlitic |
| IL_2_6 | tpr481 (Exotic Tuam pyroxenic) | ? | Lapita (3500 - 2300 BP) | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | lathwork, microlitic |
| WD_94_16 | tpr207 (Exotic Tonga pyroxenic placer) | exotic | Lapita (3500 - 2300 BP) | 0 | 3 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, lathwork |
| WD_72_1 | tpr207 (Exotic Tonga pyroxenic placer) | ? | Lapita (3500 - 2300 BP) | 0 | 1 | 2 | 6 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_72_2 | tpr207 (Exotic Tonga pyroxenic placer) | ? | Lapita (3500 - 2300 BP) | 0 | 1 | 3 | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, felsitic, vitric |
| WD_72_5 | tpr207 (Exotic Tonga pyroxenic placer) | ? | Lapita (3500 - 2300 BP) | 0 | 1 | 3 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic, vitric |
| WD_91_17 | tpr161 (Santa Cruz hornblende-feldspar) | exotic | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 4 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic |
| WD_91_20 | tpr161a (Santa Cruz hornblende-pyroxene) | exotic | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 1 | 5 | 3 | 2 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | na |
| WD_84_3 | tpr163 (Santa Cruz lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_106_5c | tpr163 (Santa Cruz lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| WD_84_5 | tpr163 (Santa Cruz lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_88_17 | tpr163 (Santa Cruz lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| WD_88_24 | tpr163 (Santa Cruz lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| WD_106_5b | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_7c | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_9a | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_82_18 | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_84_2 | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_88_11 | tpr164 (Santa Cruz transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 3 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_82_6 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_3 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_4 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_5a | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_6 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_7a | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_7b | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_8a | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_8b | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_8c | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_9c | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_82_10 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_88_20 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 6 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_88_7 | tpr165 (Santa Cruz placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 0 | 0 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_84_1 | tpr166 (Santa Cruz hybrid lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 1 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic |
| WD_84_7 | tpr166 (Santa Cruz hybrid lithic) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 1 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_88_14 | tpr167 (Santa Cruz hybrid transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 4 | 0 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_82_20 | tpr167 (Santa Cruz hybrid transitional) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 1 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_106_9b | tpr168 (Santa Cruz hybrid placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 4 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_88_9 | tpr168 (Santa Cruz hybrid placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 4 | 0 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_82_14 | tpr168 (Santa Cruz hybrid placer) | Nendo | Lapita Santa Cruz and Reef Is (3100 - 2700 BP) | 2 | 0 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_52_18 | tpr241 (Vanikolo-Tikopia feldspathic) | Vanikolo, Banks or Santo | Sinapupu imported (2100 - 800 BP) | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_52_13 | tpr242 (Vanikolo-Tikopia opaque-rich) | Vanikolo, Banks or Santo | Sinapupu imported (2100 - 800 BP) | 0 | 0 | 4 | 0 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_52_7 | tpr243 (Vanikolo-Tikopia lithic) | Vanikolo, Banks or Santo | Sinapupu imported (2100 - 800 BP) | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_88_1 | tpr243 (Vanikolo-Tikopia lithic) | Vanikolo, Banks or Santo | Sinapupu imported (2100 - 800 BP) | 0 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_34_22 | tpr138 (Exotic Kolombangara hornblendic-hypabassal) | Choiseul? | Northwest Choiseul Plainware (300 - 0 BP) | 0 | 2 | 3 | 2 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_34_23 | tpr138 (Exotic Kolombangara hornblendic-hypabassal) | Choiseul? | Northwest Choiseul Plainware (300 - 0 BP) | 0 | 2 | 3 | 2 | 4 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_34_24 | tpr138 (Exotic Kolombangara hornblendic-hypabassal) | Choiseul? | Northwest Choiseul Plainware (300 - 0 BP) | 0 | 1 | 2 | 1 | 5 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_57_21 | tpr216 (Exotic Malo chrome spinel) | New Caledonia | Western Lapita (3000 - 2500 BP) | 1 | 2 | 2 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 3 | 3 | 1 | 0 | quartzite, plutonite, metavolcanic |
| WD_51_16 | tpr217 (Malo feldspathic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_17 | tpr217 (Malo feldspathic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_18 | tpr217 (Malo feldspathic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_14 | tpr218 (Malo pyroxenic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 3 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_51_15 | tpr218 (Malo pyroxenic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 5 | 1 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_51_4 | tpr219 (Santo-Malo lithic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_51_6 | tpr219 (Santo-Malo lithic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_51_8 | tpr219 (Santo-Malo lithic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_57_5 | tpr221 (Erromango feldspathic non-placer) | Erromango | Western Lapita (3000 - 2500 BP) | 3 | 0 | 3 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork, microlitic, limeclast |
| WD_57_4 | tpr222a (Erromango olivine beach) | Erromango | Western Lapita (3000 - 2500 BP) | 0 | 0 | 1 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_43_1 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_3 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_14 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_18 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_21 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_22 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_4 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_5 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_6 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_7 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_42_9 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_43_11 | tpr225 (Efate unplacered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_5 | tpr226 (Efate partially placered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_7 | tpr226 (Efate partially placered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_9 | tpr226 (Efate partially placered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_47_24 | tpr226 (Efate partially placered) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_44_14 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 5 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_18 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 6 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_13 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 3 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_15 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 2 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_44_16 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 2 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_45_20 | tpr227 (Efate hybrid) | Efate | Western Lapita (3000 - 2500 BP) | 1 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic, felsitic |
| WD_45_1 | tpr228 (Efate pyroxenic placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_45_10 | tpr228 (Efate pyroxenic placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_45_6 | tpr228 (Efate pyroxenic placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_45_12 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_45_11 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_45_13 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_45_14 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 3 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_45_15 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_45_23 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 1 | 2 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_46_10 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 1 | 3 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_46_13 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_22 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_23 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 3 | 2 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_24 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 3 | 3 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_25 | tpr229 (Efate opaque-rich placer) | Efate | Western Lapita (3000 - 2500 BP) | 0 | 0 | 4 | 3 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_4 | tpr230 (Exotic Efate metasedimentary quartzose) | New Caledonia | Western Lapita (3000 - 2500 BP) | 3 | 4 | 2 | 2 | 3 | 1 | 0 | 1 | 1 | 1 | 1 | 1 | 2 | 0 | metavolcanic, tectonite |
| WD_46_5 | tpr230 (Exotic Efate metasedimentary quartzose) | New Caledonia | Western Lapita (3000 - 2500 BP) | 0 | 4 | 2 | 2 | 2 | 1 | 0 | 1 | 1 | 1 | 1 | 2 | 3 | 0 | metavolcanic, tectonite |
| WD_46_21 | tpr230 (Exotic Efate metasedimentary quartzose) | New Caledonia | Western Lapita (3000 - 2500 BP) | 3 | 4 | 2 | 1 | 3 | 1 | 0 | 1 | 1 | 1 | 1 | 2 | 2 | 0 | metavolcanic, tectonite |
| WD_46_3 | tpr230 (Exotic Efate metasedimentary quartzose) | New Caledonia | Western Lapita (3000 - 2500 BP) | 1 | 4 | 2 | 2 | 2 | 1 | 0 | 1 | 1 | 1 | 1 | 2 | 3 | 0 | metavolcanic, tectonite |
| WD_46_15 | tpr231 (Exotic Efate quartzose hybrid) | New Caledonia | Western Lapita (3000 - 2500 BP) | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 2 | 0 | chert, felsitic |
| WD_46_16 | tpr231 (Exotic Efate quartzose hybrid) | New Caledonia | Western Lapita (3000 - 2500 BP) | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | chert, felsitic |
| WD_46_19 | tpr231 (Exotic Efate quartzose hybrid) | New Caledonia | Western Lapita (3000 - 2500 BP) | 0 | 3 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 3 | 3 | 0 | chert, felsitic |
| WD_46_12 | tpr232a (Exotic Efate hornblendic) | Central Vanuatu or Solomons | Western Lapita (3000 - 2500 BP) | 4 | 1 | 2 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_14 | tpr232a (Exotic Efate hornblendic) | Central Vanuatu or Solomons | Western Lapita (3000 - 2500 BP) | 4 | 1 | 2 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_11 | tpr232 (Exotic Efate feldspathic hornblendic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 1 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_46_9 | tpr232 (Exotic Efate feldspathic hornblendic) | Santo | Western Lapita (3000 - 2500 BP) | 0 | 1 | 5 | 3 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| WD_53_6 | tpr268 (Aneityum hybrid type A) | Aneityum | Western Lapita (3000 - 2500 BP) | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_53_13 | tpr269 (Aneityum hybrid olivine placer type B) | Aneityum | Western Lapita (3000 - 2500 BP) | 1 | 0 | 1 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, lathwork, microlitic |
| ML_1_4 | tpr444 (Malakula calcareous) | Vao | Western Lapita (3000 - 2500 BP) | 6 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| ML_1_3 | tpr266 (Malakula opaque-rich) | Malakula | Western Lapita (3000 - 2500 BP) | 0 | 0 | 1 | 3 | 1 | 6 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, microphaneritic, microlitic |
| ML_1_2 | tpr266 (Malakula opaque-rich) | Malakula | Western Lapita (3000 - 2500 BP) | 0 | 0 | 0 | 4 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic |
| ML_1_6 | tpr260 (Malakula med lithic) | Malakula | Western Lapita (3000 - 2500 BP) | 0 | 0 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, microlitic, vitric |
| ML_1_5 | tpr264 (Malakula hybrid lithic) | Malakula | Western Lapita (3000 - 2500 BP) | 4 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, limeclast, microphaneritic, microlitic |
| ML_1_1 | tpr445 (Exotic Vao vitric) | Central Vanuatu | Western Lapita (3000 - 2500 BP) | 0 | 0 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| WD_12_19 | tpr53 (Palau lithic type V) | Babeldoab (or nearby) | Ulong Basal (3000 - 2400 BP) | 0 | 0 | 2 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic, felsitic |
| WD_12_11 | tpr50 (Palau grog type B/C/D) | Babeldoab (or nearby) | Ulong Middle (2400 - None BP) | 0 | 0 | 4 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 2 | vitric, microlitic |
| WD_12_13 | tpr51 (Palau hybrid type III) | Babeldoab (or nearby) | Ulong Middle (2400 - None BP) | 4 | 0 | 3 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, vitric |
| WD_12_14 | tpr52 (Palau hybrid type IV) | Babeldoab (or nearby) | Ulong Middle (2400 - None BP) | 1 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| WD_12_8 | tpr54 (Palau grog type II) | Babeldoab (or nearby) | Ulong Upper (None - 300 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| WD_9_2 | tpr272 (Yap metavolcanic) | Yap | Yap plainware (1900 - 0 BP) | 0 | 0 | 4 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | metavolcanic |
| WD_10_13 | tpr37 (Yap natural metavolcanic type D) | Yap | Yap plainware (1900 - 0 BP) | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_10_8 | tpr37 (Yap natural metavolcanic type D) | Yap | Yap plainware (1900 - 0 BP) | 0 | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | metavolcanic |
| WD_39_25 | tpr100 (Mussau type K) | TLTF | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_36_4 | tpr92 (Mussau type A) | Mussau or Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_36_7 | tpr92 (Mussau type A) | Mussau or Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_36_8 | tpr92 (Mussau type A) | Mussau or Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_36_17 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 1 | 0 | felsitic, vitric, chert |
| WD_36_20 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_36_24 | tpr93 (Mussau type B) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 6 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | felsitic, vitric, chert |
| WD_37_2 | tpr94 (Mussau type CD) | Admiralty | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 2 | 1 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_37_24 | tpr95 (Mussau type E) | Manus | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 6 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_37_22 | tpr95 (Mussau type E) | Manus | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 6 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_37_25 | tpr95 (Mussau type E) | Manus | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 5 | 0 | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_39_2 | tpr96 (Mussau type F) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_39_3 | tpr96 (Mussau type F) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_39_5 | tpr96 (Mussau type F) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 4 | 2 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_39_6 | tpr96 (Mussau type F) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 3 | 2 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_39_8 | tpr97 (Mussau type G) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 4 | 3 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_39_12 | tpr97 (Mussau type G) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 1 | 3 | 2 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_39_13 | tpr97 (Mussau type G) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 0 | 0 | 2 | 5 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_39_18 | tpr98 (Mussau type H) | Manus or Lavongai | Early Mussau Lapita (3250 - 2950 BP) | 5 | 0 | 2 | 2 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_36_2 | tpr92 (Mussau type A) | Mussau or Admiralty | Late Mussau Lapita (2950 - 2700 BP) | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_37_6 | tpr94 (Mussau type CD) | Admiralty | Late Mussau Lapita (2950 - 2700 BP) | 3 | 1 | 1 | 1 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_39_17 | tpr98 (Mussau type H) | Manus or Lavongai | Late Mussau Lapita (2950 - 2700 BP) | 5 | 0 | 2 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic, vitric |
| WD_39_20 | tpr99 (Mussau type J) | Manus, Lavongai or New Britain | Late Mussau Lapita (2950 - 2700 BP) | 1 | 2 | 5 | 0 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_39_21 | tpr99 (Mussau type J) | Manus, Lavongai or New Britain | Late Mussau Lapita (2950 - 2700 BP) | 0 | 2 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_41_4 | tpr191 (Manus andesitic) | Manus | Admiralty Transitional (2300 - 1900 BP) | 0 | 0 | 4 | 3 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_41_5 | tpr191 (Manus andesitic) | Manus | Admiralty Post-Lapita (1800 - 800 BP) | 0 | 0 | 3 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_41_7 | tpr191 (Manus andesitic) | Manus | Admiralty Historical (800 - 0 BP) | 0 | 0 | 4 | 3 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_41_8 | tpr191 (Manus andesitic) | Manus | Admiralty Historical (800 - 0 BP) | 0 | 0 | 3 | 3 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_41_6 | tpr191a (Manus andesitic placer) | Manus | Admiralty Historical (800 - 0 BP) | 0 | 0 | 2 | 4 | 2 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_101_1 | tpr125 (Buka calcareous hybrid) | Buka | Buka ware (2500 - 2200 BP) | 6 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| WD_101_2 | tpr125 (Buka calcareous hybrid) | Buka | Buka ware (2500 - 2200 BP) | 6 | 0 | 2 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_101_3 | tpr127 (Buka microgranular) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
| WD_32_13 | tpr127 (Buka microgranular) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 3 | 2 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
| WD_32_20 | tpr127 (Buka microgranular) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 2 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 5 | 0 | 0 | microphaneritic, microlitic |
| WD_32_23 | tpr128 (Buka plagioclase pyroxene) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 5 | 2 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_101_4 | tpr128 (Buka plagioclase pyroxene) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_15 | tpr128 (Buka plagioclase pyroxene) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 4 | 4 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_22 | tpr128 (Buka plagioclase pyroxene) | Buka | Post Lapita Buka (2200 - 0 BP) | 0 | 0 | 5 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| WD_32_24 | tpr131 (New Ireland cherty feldspathic) | New Ireland or Central Solomons | Post Lapita Buka (2200 - 0 BP) | 0 | 1 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | microlitic, felsitic, microphaneritic, chert |
| WD_35_15 | tpr117 (Meinakapa feldspathic) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 5 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_35_16 | tpr117 (Meinakapa feldspathic) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 5 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_35_17 | tpr117 (Meinakapa feldspathic) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic |
| WD_35_2 | tpr120 (Kieta partial placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 4 | 1 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_35_6 | tpr120 (Kieta partial placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 4 | 1 | 4 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_35_3 | tpr121 (Kieta placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 2 | 2 | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_35_1 | tpr121 (Kieta placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 3 | 1 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_35_4 | tpr121 (Kieta placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 4 | 2 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_35_5 | tpr121 (Kieta placer) | Central Bougainville | Kieta ware (1500 - 0 BP) | 0 | 0 | 3 | 1 | 3 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_35_12 | tpr116 (Pidia manual) | Central Bougainville | Asio ware (1000 - 300 BP) | 0 | 0 | 4 | 1 | 4 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_35_9 | tpr115 (Pidia feldspathic-hornblendic natural) | Central Bougainville | Pidia (300 - 0 BP) | 0 | 0 | 5 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric, microlitic |
| WD_35_11 | tpr115 (Pidia feldspathic-hornblendic natural) | Central Bougainville | Pidia (300 - 0 BP) | 0 | 0 | 5 | 1 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_35_14 | tpr118 (Pidia modern) | Central Bougainville | Pidia (300 - 0 BP) | 0 | 0 | 4 | 4 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_34_4 | tpr112 (Paubake feldspathic non-placer manual) | South Bougainville | Early Buin (1000 - 300 BP) | 0 | 0 | 6 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_34_2 | tpr112 (Paubake feldspathic non-placer manual) | South Bougainville | Early Buin (1000 - 300 BP) | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_34_5 | tpr112 (Paubake feldspathic non-placer manual) | South Bougainville | Early Buin (1000 - 300 BP) | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_34_8 | tpr112 (Paubake feldspathic non-placer manual) | South Bougainville | Early Buin (1000 - 300 BP) | 0 | 0 | 5 | 2 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_34_11 | tpr111 (Paubake feldspathic natural temper) | South Bougainville | Late Buin (300 - 0 BP) | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_34_13 | tpr111 (Paubake feldspathic natural temper) | South Bougainville | Late Buin (300 - 0 BP) | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_34_17 | tpr111 (Paubake feldspathic natural temper) | South Bougainville | Late Buin (300 - 0 BP) | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_34_19 | tpr111 (Paubake feldspathic natural temper) | South Bougainville | Late Buin (300 - 0 BP) | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_34_20 | tpr111 (Paubake feldspathic natural temper) | South Bougainville | Late Buin (300 - 0 BP) | 0 | 0 | 6 | 2 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_13 | tpr110 (Shortland feldspathic) | Bougainville/SI | Early Shortland (1500 - 1000 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_14 | tpr110 (Shortland feldspathic) | Bougainville/SI | Early Shortland (1500 - 1000 BP) | 0 | 0 | 6 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_103_4 | tpr110 (Shortland feldspathic) | Bougainville/SI | Early Shortland (1500 - 1000 BP) | 0 | 0 | 6 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic |
| WD_103_9 | tpr110 (Shortland feldspathic) | Bougainville/SI | Middle Shortland (1000 - 300 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_15 | tpr110 (Shortland feldspathic) | Bougainville/SI | Middle Shortland (1000 - 300 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_2 | tpr110 (Shortland feldspathic) | Bougainville/SI | Middle Shortland (1000 - 300 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_103_7 | tpr110 (Shortland feldspathic) | Bougainville/SI | Middle Shortland (1000 - 300 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_1 | tpr110 (Shortland feldspathic) | Bougainville/SI | Late Shortland (300 - 0 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_103_11 | tpr110 (Shortland feldspathic) | Bougainville/SI | Late Shortland (300 - 0 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| WD_103_3 | tpr110 (Shortland feldspathic) | Bougainville/SI | Late Shortland (300 - 0 BP) | 0 | 0 | 6 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| WD_88_2 | tpr245 (Tikopia calcareous) | Tikopia | Kiki wares (2900 - 2100 BP) | 6 | 0 | 2 | 1 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_40_1 | tpr141 (Roviana plainware A-opaque rich) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 2 | 3 | 0 | 1 | 5 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_3 | tpr142 (Roviana plainware B-feldspathic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 1 | 5 | 1 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_5 | tpr143 (Roviana plainware C-hornblendic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 0 | 3 | 2 | 5 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_4 | tpr143 (Roviana plainware C-hornblendic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 0 | 2 | 1 | 4 | 2 | 0 | 0 | 0 | 1 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_6 | tpr143 (Roviana plainware C-hornblendic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 0 | 3 | 2 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_7 | tpr143 (Roviana plainware C-hornblendic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 0 | 3 | 1 | 4 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_8 | tpr143 (Roviana plainware C-hornblendic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 0 | 3 | 1 | 4 | 2 | 0 | 0 | 0 | 1 | 0 | 4 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_40_9 | tpr144 (Roviana plainware D-lithic) | Choiseul? | Roviana Plainware (800 - 100 BP) | 0 | 1 | 2 | 2 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, vitric, microphaneritic |
| WD_35_25 | tpr135 (Kolombangara pyroxenic) | Kolombangara | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 4 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_35_23 | tpr135 (Kolombangara pyroxenic) | Kolombangara | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 4 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
| WD_35_21 | tpr136 (Exotic Kolombangara hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 2 | 5 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | felsitic |
| WD_38_16 | tpr150 (Exotic Roviana quartz-calcite) | Unknown | Early Post-Lapita Solomons (2700 - 2000 BP) | 4 | 4 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | na |
| WD_40_20 | tpr150 (Exotic Roviana quartz-calcite) | exotic | Early Post-Lapita Solomons (2700 - 2000 BP) | 6 | 3 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | na |
| WD_40_21 | tpr150 (Exotic Roviana quartz-calcite) | unknown | Early Post-Lapita Solomons (2700 - 2000 BP) | 6 | 3 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | na |
| WD_38_17 | tpr150 (Exotic Roviana quartz-calcite) | Unknown | Early Post-Lapita Solomons (2700 - 2000 BP) | 5 | 3 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | na |
| WD_38_20 | tpr150 (Exotic Roviana quartz-calcite) | Unknown | Early Post-Lapita Solomons (2700 - 2000 BP) | 2 | 5 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_78_2 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 2 | 3 | 5 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic |
| WD_78_3 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 3 | 4 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, felsitic |
| WD_78_4 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 3 | 2 | 3 | 4 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_78_8 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 2 | 3 | 4 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_7 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 3 | 3 | 3 | 3 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_9 | tpr146 (Vella Lavella type A-hornblende-pyroxene) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 3 | 2 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_78_1 | tpr147 (Vella Lavella type B-brown hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 4 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_78_10 | tpr147 (Vella Lavella type B-brown hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 5 | 1 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_12 | tpr147 (Vella Lavella type B-brown hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_17 | tpr148 (Vella Lavella type C-green hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_18 | tpr148 (Vella Lavella type C-green hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 5 | 0 | 3 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_78_15 | tpr148 (Vella Lavella type C-green hornblendic) | Vella Lavella | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 4 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_78_20 | tpr149 (Vella Lavella type D-hornblende poor) | New Georgia | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 4 | 1 | 3 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_78_21 | tpr149 (Vella Lavella type D-hornblende poor) | New Georgia | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 2 | 5 | 2 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, vitric |
| WD_78_22 | tpr149 (Vella Lavella type D-hornblende poor) | New Georgia | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 1 | 5 | 0 | 3 | 1 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| KH_1_37 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_36 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 1 | 1 | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_34 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 5 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| KH_1_40 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | na |
| KH_1_39 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 5 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | plutonite |
| KH_1_41 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_43 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_44 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_22 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_25 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 0 | 0 | 2 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_27 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 0 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_32 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_31 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | plutonite |
| JS_1_25 | tpr271 (Markham Valley sericitic feldspathic) | Markham Valley | gur (Adzera) (300 - 0 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 4 | 0 | 0 | 0 | 0 | 0 | na |
| WD_26_7 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 4 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 5 | 0 | metavolcanic, amphibolite, tectonite, quartzite |
| WD_26_13 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 3 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 1 | 6 | 0 | metalcanic, amphibolite, tectonite, quartzite |
| WD_27_4 | tpr312 (New Caledonian calcareous) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 6 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_27_1 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 3 | 1 | 1 | 1 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 6 | 0 | quartzite, metavolcanic, chert, tectonite |
| WD_27_12 | tpr302 (New Caledonian quartzose-ophiolitic) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 1 | 1 | 0 | 2 | 4 | 0 | metavolcanic, plutonite, vitric, quartzite |
| WD_27_13 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | metavolcanic, amphibolite, quartzite, plutonite |
| WD_27_14 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | metavolcanic, amphibolite, quartzite, plutonite |
| WD_27_15 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | metavolcanic, amphibolite, quartzite, plutonite |
| WD_27_17 | tpr299 (New Caledonian lithic quartzose) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 2 | 2 | 0 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 5 | 0 | metavolcanic, amphibolite, quartzite, plutonite |
| WD_27_16 | tpr306 (New Caledonian basaltic placer) | Grand Terre | Northern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 1 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic, vitric, lathwork |
| WD_27_18 | tpr302 (New Caledonian quartzose-ophiolitic) | Grand Terre | Southern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 4 | 0 | quartzite, metavolcanic, plutonite, vitric |
| WD_27_19 | tpr302 (New Caledonian quartzose-ophiolitic) | Grand Terre | Southern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 3 | 3 | 2 | 2 | 1 | 0 | 0 | 0 | 1 | 0 | 2 | 4 | 0 | metavolcanic, quartzite, vitric, plutonite |
| WD_27_20 | tpr306 (New Caledonian basaltic placer) | Grand Terre | Southern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 0 | 2 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic, lathwork, vitric, plutonite |
| WD_27_21 | tpr306 (New Caledonian basaltic placer) | Grand Terre | Southern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 0 | 2 | 4 | 0 | 2 | 2 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | metavolcanic, lathwork, vitric, plutonite |
| WD_27_22 | tpr306 (New Caledonian basaltic placer) | Grand Terre | Southern New Caledonia Post-Lapita (2900 - 0 BP) | 0 | 0 | 2 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 1 | 0 | metavolcanic, vitric, lathwork, plutonite |
| WD_48_17 | tpr255 (Epi mafic lithic) | Epi | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic |
| WD_48_16 | tpr255 (Epi mafic lithic) | Epi | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, vitric |
| WD_47_10 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_13 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_16 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_17 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_18 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_2 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_21 | tpr239 (Shepherd feldspathic) | Shepherd Islands or Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_22 | tpr239 (Shepherd feldspathic) | Shepherd islands or Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_47_4 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_6 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_47_8 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_48_19 | tpr239 (Shepherd feldspathic) | Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| WD_58_12 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_13 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_15 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_6 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_8 | tpr233 (Efate standard) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_1 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_16 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_17 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_18 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_58_2 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_58_7 | tpr235 (Efate lithic-poor) | Efate | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 6 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| WD_47_20 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| ML_1_7 | tpr227 (Efate hybrid) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 1 | 0 | 5 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, vitric |
| ML_1_8 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric |
| ML_1_9 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic |
| ML_1_10 | tpr239 (Shepherd feldspathic) | Efate-Shepherd Islands | Post-Lapita Efate and Shepherd Islands (2900 - 1200 BP) | 0 | 0 | 5 | 2 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric |
| WD_57_1 | tpr220 (Erromango pyroxenic) | Erromango | Post-Lapita Erromango and Aneityum (2800 - 2000 BP) | 0 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, lathwork, microlitic |
| WD_57_6 | tpr221 (Erromango feldspathic non-placer) | Erromango | Post-Lapita Erromango and Aneityum (2800 - 2000 BP) | 0 | 0 | 3 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric, microlitic |
| WD_57_8 | tpr222 (Erromango olivine placer) | Erromango | Post-Lapita Erromango and Aneityum (2800 - 2000 BP) | 0 | 0 | 1 | 6 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric, microlitic |
| WD_53_4 | tpr269 (Aneityum hybrid olivine placer type B) | Aneityum | Post-Lapita Erromango and Aneityum (2800 - 2000 BP) | 0 | 0 | 2 | 5 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork, microlitic |
| WD_53_3 | tpr280 (Exotic Aneityum vitric quartz) | Exotic | Post-Lapita Erromango and Aneityum (2800 - 2000 BP) | 0 | 1 | 3 | 1 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, felsitic, microlitic |
| ML_1_13 | tpr214 (Santo stream) | Santo | uro tano (Wusi) (500 - 0 BP) | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | felsitic, microlitic |
| WD_52_3 | tpr256 (Banks volcanic) | Banks | Post-Lapita Banks (2700 - 2000 BP) | 0 | 0 | 3 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_52_1 | tpr258 (Banks vitric) | Banks | Post-Lapita Banks (2700 - 2000 BP) | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| KH_1_21 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_1 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_2 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_3 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_4 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_5 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_6 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_7 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_8 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_9 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_10 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_17 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_16 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_15 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_11 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 1 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_12 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_13 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_18 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_19 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_20 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_33 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_14 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_23 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_24 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_26 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_28 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 1 | 1 | 0 | 2 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_29 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_30 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_35 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_42 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_38 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 4 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | plutonite |
| KH_1_46 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_47 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_48 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 2 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| KH_1_45 | tpr270 (PNG highlands quartz feldspar) | Eastern Highlands | kabe (Agarabi) (300 - 0 BP) | 0 | 5 | 4 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | plutonite |
| IL_2_16 | tpr459 (Madang pyroxenic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 2 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
| IL_1_1 | tpr459 (Madang pyroxenic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 2 | 0 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| IL_1_38 | tpr459 (Madang pyroxenic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 1 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| IL_2_35 | tpr459 (Madang pyroxenic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic, vitric |
| IL_2_15 | tpr459 (Madang pyroxenic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 0 | 3 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic |
| IL_2_56 | tpr460 (Madang feldspathic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 1 | 5 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, microphaneritic |
| IL_2_55 | tpr460 (Madang feldspathic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 0 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic, microlitic |
| IL_2_36 | tpr460 (Madang feldspathic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 2 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic |
| IL_1_20 | tpr460 (Madang feldspathic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 2 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic, lathwork |
| IL_1_6 | tpr460 (Madang feldspathic lithic) | Madang | bodi (Bilibil) (500 - 0 BP) | 0 | 1 | 4 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | microphaneritic, microlitic, lathwork |
| IL_1_60 | tpr300 (Huon ferruginous) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic |
| JS_1_36 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_14 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_37 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_38 | tpr300 (Huon ferruginous) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| JS_1_39 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_40 | tpr300 (Huon ferruginous) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| JS_1_42 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_43 | tpr274 (Huon pyroxenic) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 3 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| JS_1_44 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_45 | tpr179a (Huon grog) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 6 | na |
| JS_1_47 | tpr300 (Huon ferruginous) | Huon | Type X (1000 - 500 BP) | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| IL_2_4 | tpr482 (Exotic Tuam amphibolic) | ? | Type Y (1700 - 500 BP) | 0 | 0 | 4 | 0 | 5 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| IL_2_3 | tpr482 (Exotic Tuam amphibolic) | ? | Type Y (1700 - 500 BP) | 0 | 2 | 4 | 1 | 2 | 3 | 0 | 0 | 0 | 0 | 1 | 2 | 0 | 0 | microphaneritic |
| IL_1_61 | tpr274 (Huon pyroxenic) | Huon | Ancestral Sio (1700 - 500 BP) | 0 | 1 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_2_1 | tpr274 (Huon pyroxenic) | Huon | Ancestral Sio (1700 - 500 BP) | 0 | 0 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_2_2 | tpr483 (Huon feldspathic lithic) | Huon | Ancestral Sio (1700 - 500 BP) | 0 | 0 | 5 | 1 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 4 | 0 | 0 | microlitic, plutonite, microphaneritic |
| IL_1_66 | tpr274 (Huon pyroxenic) | Sio | Ancestral Sio (1700 - 500 BP) | 0 | 1 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, microphaneritic |
| IL_1_63 | tpr274 (Huon pyroxenic) | Sio | Ancestral Sio (1700 - 500 BP) | 0 | 1 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, microphaneritic |
| IL_1_68 | tpr486 (Huon feldspathic pyroxenic) | Sio | Ancestral Sio (1700 - 500 BP) | 0 | 2 | 3 | 3 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, microphaneritic |
| IL_1_57 | tpr459 (Madang pyroxenic lithic) | Madang | Ancestral Madang (1300 - 500 BP) | 2 | 2 | 2 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microphaneritic |
| IL_1_58 | tpr458 (Huon calcareous) | Huon | Ancestral Madang (1300 - 500 BP) | 6 | 2 | 2 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| IL_2_59 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 1 | 0 | 3 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_2_45 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 1 | 0 | 2 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| IL_2_33 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| IL_2_67 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_2_57 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric |
| IL_2_65 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| IL_2_60 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 1 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | vitric |
| IL_2_29 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_1_17 | tpr274 (Huon pyroxenic) | Huon | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| IL_2_19 | tpr458 (Huon calcareous) | Huon | Sio ware (600 - 0 BP) | 6 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| IL_2_25 | tpr458 (Huon calcareous) | Huon | Sio ware (600 - 0 BP) | 6 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| IL_2_20 | tpr483 (Huon feldspathic lithic) | Sio | Sio ware (600 - 0 BP) | 0 | 0 | 4 | 4 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, microphaneritic, microlitic |
| IL_2_61 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 5 | 1 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | lathwork, vitric, microphaneritic |
| IL_1_18 | tpr483 (Huon feldspathic lithic) | Sio | Sio ware (600 - 0 BP) | 0 | 1 | 4 | 2 | 0 | 1 | 0 | 2 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic |
| IL_1_31 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 5 | 1 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| IL_1_15 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 0 | 2 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| IL_2_26 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 1 | 1 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, microphaneritic |
| IL_1_12 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 1 | 1 | 6 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microphaneritic, microlitic |
| IL_2_39 | tpr459 (Madang pyroxenic lithic) | Sio | Sio ware (600 - 0 BP) | 0 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | microlitic, lathwork, microphaneritic |
| IL_1_28 | tpr274 (Huon pyroxenic) | Sio | Sio ware (600 - 0 BP) | 0 | 1 | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic |
| IL_1_56 | tpr483 (Huon feldspathic lithic) | Sio | Sio ware (600 - 0 BP) | 0 | 1 | 4 | 3 | 0 | 1 | 0 | 1 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, lathwork |
| WD_16_6 | tpr63a (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_16_18 | tpr63a (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 6 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_16_12 | tpr63b (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_16_11 | tpr63b (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_16_19 | tpr63b (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 5 | 4 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| WD_16_24 | tpr63c (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_16_10 | tpr63c (Aru quartz-calcite) | Aru | Aru ware (800 - 0 BP) | 3 | 5 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
Madang style sherd. CAUTION: Section less than 30microns. Plagioclase (5%), volcanic rock fragments (<5%), ferruginized pellets and accessory shell fragments are all less than 0.6 m in diameter. The clay is red brown and contains abundant fine grained quartz, feldspar and iron oxides.
Madang style. Paddle impressed. CAUTION: Section less than 30microns. Pyroxene grains (10%) range in size from 0.1 up to 0.7 mm in length. Quartz and feldspar grains (<10%) range from less than 0.1 up to 0.2 mm in length. There are some hypocrystalline volcanic rock fragments which contain large pyroxene crystals set in a ground mass of smaller pyroxene crystals, plagioclase, opaques and altered glass. The sherd also contains trace amounts of iron oxide and carbonate shell fragments.
Madang style. CAUTION: Section less than 30microns. This sherd is characterized by angular to subrounded magnetite grains (5%) less than 0.2 mm in length. Pyroxene grains (1%) are less than 0.2 mm in length. Plagioclase grains (<1%) are generally less than 0.2 mm in length. But there are rare grains of quartz and feldspar up to 1 mm across. There are also trace amounts of red ferruginized grains and rare shell in the red clay.
Madang style. CAUTION: Section less than 30microns. Subrounded shelly fragments up to 0.3 mm in diameter make up less than 10%. Quartz, chert and feldspar grains (<10%) are all less than 0.2 mm in length. There are some dark red-black ferruginized clasts up to 0.5 mm and the clay is brown.
Poorly sorted temper sand characteristic of Buka temper types.
Feldspathic sand temper.
Feldspathic.
Feldspathic sand temper.
Feldspathic.
Hybrid (mixed terrigenous-calcareous) sand temper.
Hybrid (mixed terrigenous-calcareous) sand temper.
Hybrid (mixed terrigenous-calcareous) sand temper.
Moderately sorted and mineralogically complex lithic sand temper, with microgranular hypabyssal.
Well sorted and subrounded to subangular pyroxenic beach placer temper, basaltic lithics are hyalopilitic.
Well sorted and subrounded to subangular pyroxenic beach placer temper, basaltic lithics. Microlitics are hyalopilitic.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Lapita sherd. Pyroxenes are 1/3 orthopyroxene.
Poorly sorted, fine-grained volcanic sands of likely stream (non-local) origin.
Well sorted, fine- to medium-grained placer beach sand, wholly lacking in hornblende, but rich in clinopyroxene and opaque iron oxides.
Well sorted, fine- to medium-grained placer beach sand, wholly lacking in hornblende, but rich in clinopyroxene and opaque iron oxides.
Almost exclusively calcareous temper sand with sparse subspherical hydrous iron oxide grains.
Hybrid (mixed terrigenous-calcareous) beach sand temper of anomalous composition unlikely to derive from anywhere on New Ireland or within the Bismarck Archipelago.
Moderately to well sorted, fine- to medium-grained, subrounded placer beach sands rich in opaque iron oxide grains of high specific gravity and containing minor admixtures of calcareous reef detritus. Has orthopyroxene in addition to clinopyroxene.
Moderately to well sorted, fine- to medium-grained, subrounded placer beach sands rich in opaque iron oxide grains of high specific gravity and containing minor admixtures of calcareous reef detritus. Has orthopyroxene in addition to clinopyroxene.
Hybrid Calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass) and andesitic arc.
Hybrid Calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass) and andesitic arc.
Hybrid Calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass) and andesitic arc.
Hybrid Calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass) and andesitic arc.
Hybrid Calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass) and andesitic arc.
Hybrid calcareous- volcanic sand.
Hybrid calcareous- volcanic sand.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Hybrid calcareous with plagioclase and augite, opaques and rock fragments (pale brown vitric glass). Andesitic arc.
Placered plagioclase and augite, opaques and rock fragments.
Placered plagioclase and augite, opaques and rock fragments.
Plagioclase high.
Plagioclase high.
Angkikita. Well sorted, strongly abraded, hybrid lithic, non-placer aggregate temper sand. Microlitic rocks dominant, also felsitic and vitric.
Angkikita. Hornblendic hybrid temper sand with vitric volcanic rock fragments as dominant grain type.
Angkikita. Hornblendic-pyroxenic aggregate temper sand, subangular to subrounded, moderately sorted, and variably placered.
Generally andesitic, fine- to medium-grained, subangular to subrounded temper sand of probable beach origin. Clinopyroxene dominant, but minor orthopyroxene.
Generally andesitic, fine- to medium-grained, subangular to subrounded temper sand of probable beach origin. Has orthopyroxene in addition to clinopyroxene.
Well sorted and subrounded feldspathic hybrid sand composed of unplacered volcanic sand admixed with more abundant calcareous reef grains.
Volcanic (Andesitic). Andesitic volcanic sand , moderately well sorted, subrounded volcanic sand, predominantly volcanic rock fragments, mainly microlitic but partly felsitic or glassy, and also including some microcrystalline fragments of hypabyssal igneous rocks plagioclase feldspar, and minor clinopyroxene.
Andesitic Temper. andesitic volcanic sand , moderately well sorted, subrounded volcanic sand, predominantly volcanic rock fragments, mainly microlitic but partly felsitic or glassy, and also including some microcrystalline fragments of hypabyssal igneous rocks plagioclase feldspar, and minor clinopyroxene
Volcanic Temper. andesitic volcanic sand , moderately well sorted, subrounded volcanic sand, predominantly volcanic rock fragments, mainly microlitic but partly felsitic or glassy, and also including some microcrystalline fragments of hypabyssal igneous rocks plagioclase feldspar, and minor clinopyroxene
Dentate-stamped Lapita sherd. Andesitic (lithic) Taumako temper sand. andesitic volcanic sand , moderately well sorted, subrounded volcanic sand, predominantly volcanic rock fragments, mainly microlitic but partly felsitic or glassy, and also including some microcrystalline fragments of hypabyssal igneous rocks plagioclase feldspar, and minor clinopyroxene
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.
Pyroxene-rich placer sand, placer black sand formed by intensive reworking of volcanic debris.clinopyroxene grains, Plagioclase feldspars and volcanic rock fragments.
Microphaneritic.
Microphaneritic.
Microphaneritic.
Microphaneritic.
Microphaneritic.
Feldspathic non-placer sand temper.
Pyroxene-rich beach placer sand temper.
Hornblende-rich, feldspathic sand temper of probable beach origin.
Calcareous sand temper, rare plagioclase and clinopyroxene.
Moderately sorted and subrounded sand temper of probable stream origin that is plagioclase-rich.
Volcanic sand temper.
Feldspathic sand temper.
Well sorted placer sand temper of probable beach origin that contains subordinate but prominent hornblende grains. Leached calcareous.
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands Olivine and hornblende present. Has orthopyroxene in addition to the more abundant clinopyroxene. Microlitics are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic volcanic rock fragments are hyalopilitic.
Non-Lapita. Moderately sorted, subangular to subrounded aggregates, probably stream sands. Microlitic lithics are hyalopilitic.
Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands. Volcanic rocks are felsitic (microcrystalline quartz-feldspar groundmass mosaic commonly with plagioclase microphenocrysts).
Non-Lapita. Vitric glass. Well sorted, subrounded to subangular aggreates that are probably beach sands. Microlitic lithics are hyalopilitic.
Exclusively calcareous temper sand. From reef. From Lifafaesing.
Lifafaesing site. Feldspathic temper sand that contains abundant clinopyroxene and sparse mica.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and biotite.
Angkikita site. Feldspathic temper sand that contains abundant clinopyroxene and no biotite.
Angkikita. Mixed pyroxene/opaque iron oxide ferromagnesian placer sand temper.
Lifafaesing. Pyroxene-rich ferromagnesian placer sand temper.
Oceanic basaltic.
Oceanic basalt.
Olivine basalt.
Brown vitrics.
Probably wrong thickness.
Thick coares sherd. Basaltic.
Basaltic.
Thin fine sherd. Basaltic.
Thin fine sherd. Basaltic.
Crystal.
Intersertal with tachylitic glass and subordinate hyalopilitic. A3.
Intersertal to intergranular (fluidal fabric).
Intersertal to intergranular (fluidal fabric).
Intergranular with minor hyalopilitic
Intergranular with minor hyalopilitic.
Intergranular with minor hyalopilitic
Subophitic with minor hyalopilitic.
Subophitic with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular (fluidal fabric).
Intersertal with tachylitic glass and subordinate hyalopilitic. A3.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Intersertal to intergranular with minor hyalopilitic.
Basaltic rock fragments have glassy groundmass with plagioclase laths and altered pyroxene and olivines.
Rocks have holocrystalline plagioclase-clinopyroxene groundmasses.
Lithics with plagioclase, pyroxene and olivine laths.
Basaltic rock.
Very weathered inclusions.
Weathered.
Trachytic.
Vacuoles suggest the past presence of calcareous inclusions.
Basaltic temper.
Crushed rock temper.
Basaltic lithic temper.
Basaltic lithic temper.
Basaltic.
Sparse temper.
Feldspathic basaltic temper.
Sparse basaltic temper.
Mixed temper.
Calcareous temper.
Profuse basaltic temper.
Profuse basaltic temper.
Profuse basaltic temper.
Profuse basaltic temper.
Sparse basaltic temper.
Trachytic microlitic.
Ferromagnetic.
Ferromagnetic.
Lithic.
Crushed rock.
Crushed rock.
Trachytic.
Trachytic microlitic.
Ferromagnetic.
Ferromagnetic.
Ferromagnetic.
Crushed rock.
Crushed rock.
Crushed rock.
Crushed rock.
Decorated sherd, reduced. Brown glass, with holocrystalline basaltic.
Brown glass. Mainly holocrystalline basaltic lithics. Reduced sherd.
Decorated reduced sherd. Contains deliberately added shell.
Decorated body oxidised sherd. Vitrophytic basaltic lithics with some altered red glass. Shell not deliberately added.
Coarse fabric, oxidised. May also contain trachyitic lithics (feldspathic basalts).
Coarse temper. May also contain trachyitic lithics (feldspathic basalts). Trachytic feldspathic basalt probably derive from Fagaloa Volcanics.
Picritic basalt. High olivine to pyroxene ratio. Reduced sherd.
Decorated sherd. Oxidised. Olivine is altered to iddingsite. Less olivine than pyroxene. Picritic basalt fragments with reddish glass. Tuff.
Oxidised sherd. Picritiic and vitric basalt fragments. Reddish glass. Olivines altered to iddingsite.
Reduced. High olivine to pyroxene ratio. Picritic basalts with reddish glass.
Reduced. Low olivine to pyroxene ratio.
Reduced core. Altered olivine. Reddish vitrics. Tuff. Picritic basalts.
Picritic, holocrystalline and vitric basalt lithics, with some vitrophytic. Altered olivine. Similar olivine and pyroxene levels.
Oxidised sherd. Altered olivine. More olivine than pyroxene. Fresh vitrics. Lithics vitric and holocrystalline, with some picritic and vitrophytic.
Reduced core. Mainly vitric and vitrophytic lithics.
Oxidised sherd. Has trace quartz and feldspars from Fagaloa formation.
Oxidised sherd. Picritic lithics. Altered olivines. More olivines than pyroxenes.
Oxidised sherd. Equal olivines and pyroxenes. Mainly picritic basaltic lithics.
Ferromagnesian.
Crystal lithic beach sand.
Crystal lithic.
Crystal lithic beach sand.
Crystal lithic beach sand.
Classified differently in 2 reports. Type A or B, andesitic aggregate sand temper likely from Saipan, fineware.
Type A CQT. Dacitic aggregate sand temper likely from Saipan, fineware.
Calcareous sands. Pre-latte sherd.
TYPE C MVQT. Mixed quartzose (dacitic)-calcareous hybrid temper sand. Thin red ware.
Pre-Latte sherd. Quartz-rich quartzose sand temper.
Hybrid quartz grains and calcareous detritus.
Hybrid quartz grains and calcareous detritus.
Hybrid temper sand (85-90% of total grain population is calcareous reef detritus). Pre-latte.
Quartz-calcite temper.
Quartz-calcite temper, dacitic and reef deitrius source. Pre latte red-ware lime-filled. Manually added.
Type A CQT. Mixed dacitic (quartz-bearing)-calcareous (>90%) hybrid temper sand, thick red ware.
Deeply weathered; Volcanic sand temper. Pre-latte sherd.
Hybrid sand temper containing unstrained quartz as the most abundant terrigenous grain. Pre-latte.
Hybrid quartose dactic. Called 443 in report. Imported. pre-latte.
Quartz-rich temper sands composed of the same grain types observed in quartz-rich soils and derivative sands of north-central Saipan. Pre-Latte sherd.
Quartz-rich dacitic volcanic sand temper.
Glass-rich dacitic volcanic sand temper.
Glass- rich dacitic volcanic sand, type B. Marianas trailed sherd.
Poorly sorted dacitic volcanic sand temper of simple mineralogy and probable fluvial origin, composed dominantly of volcanic glass rock fragments.
Quartzose dacitic volcanic sand temper. Fine temper.
East Pagan, Apansantate beside Latte site '1819'. Quartzose sand temper.
Glass-rich volcanic sand , Type C, tan to brown vesicular glass. Marianas cordmarked sherd. Clinopyroxene and orthopyroxene.
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Quartz-poor (andesitic) volcanic sands in sherds with red pastes. Clinopyroxene dominant, but minor orthopyroxene.
Hybrid with much leeching of calcareous grains, so numbers may be unrepresentative.
Quartz-poor (andesitic) volcanic sands in sherds with red pastes.
Quartz-free aggregate volcanic sand temper in which microlitic volcanic rock fragments of intermediate character are dominant.
Moderately sorted and mineralogically complex andesitic volcanic sand temper of fine to coarse size and probable fluvial origin.
Lowly lithic sand temper.
Lowly lithic sand temper.
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Wholly non-calcareous, poorly sorted andesitic sand temper made up dominantly of vitric, microlitic and some felsitic volcanic lithic fragments, feldspar is plagioclase. Coarseware. Clinopyroxene and orthopyroxene.
Type B VST. Terrigenous andesitic (non-quartzose) volcanic sand temper. Clinopyroxene dominant, but minor orthopyroxene.
Wholly non-calcareous, poorly sorted andesitic sand temper made up dominantly of vitric volcanic lithic fragments, feldspar is plagioclase. Coarseware.
Moderately sorted andesitic volcanic sand temper of probable fluvial origin composed of subangular to subrounded grains of fine to coarse sand rich in glassy volcanic rock fragments.
Andesitic temper sand rich in glassy volcanic rock fragments and lacking any calcareous grains indicative of coastal origin.
Deeply weathered. Volcanic sand temper.
Poorly sorted, subangular to subrounded, andesitic volcanic sand temper rich in glassy volcanic rock fragments of tan to brown hues in thin section.
Coarse temper. Quartz-free andesitic temper sands. Probably from Saipan as orthopyroxene present.
TYPE C MVQT. Quartz-rich dacitic sand temper of Saipan origin intermingled with more abundant calcareous sand. Coarseware.
Quartzose (dacitic) volcanic sands in sherds with black pastes.
Quartzose volcanic temper sand rich in grains of volcanic glass. Sabanan Fiang benchland east of the island crest in north-central Saipan. Latte sherd. Dacitic.
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Quartzose volcanic temper sand rich in grains of volcanic glass. Sabanan Fiang benchland east of the island crest in north-central Saipan. Latte sherd. Dacitic.
Quartzose glass-rich volcanic sand temper.
Quartz-poor volcanic sand temper of feldspathic composition and andesitic character. Latte. Clinopyroxene and orthopyroxene.
Poorly sorted, subangular to subrounded, andesitic volcanic sand temper rich in glassy volcanic rock fragments of tan to brown hues in thin section. Clinopyroxene dominant, but minor orthopyroxene.
Marianas Plainware. Volcanic sand temper. Clinopyroxene dominant, but minor orthopyroxene.
Volcanic sand tempers of andesitic character. Latte sherd. Clinopyroxene dominant, but minor orthopyroxene.
Hybrid calcareous-quartz beach sand temper.
Temper with reddish surfaces but uniformly dark and hackly interiors, contains quartz-rich temper sand admixed with calcareous grains.
Yap metavolcanic temper admixed with calcareous grains (reef detritus).
Temper in which calcareous grains are dominant, but are admixed with minor amounts of Yap metavolcanics.
Temper in which calcareous grains are dominant, but are admixed with minor amounts of Yap metavolcanics.
Hybrid temper.
Moderately sorted, subrounded shoreline temper sand. Yap origin.
Probably 44_1.
Broken-sherd temper indistinguishable from temper in sherds from Palau.
Broken-sherd temper indistinguishable from temper in sherds from Palau.
Broken-sherd temper, with quartzose and cherty grains.
Broken-sherd temper in which quartzose and cherty grains are abundant.
Broken-sherd temper in which quartzose and cherty grains are abundant.
Broken-sherd temper in which quartzose and cherty grains are abundant.
Palau origin.
Broken-sherd aggregate temper sand. Palau origin.
Palau origin.
Contains a temper composed of broken pottery. 1978-38-7 (1) from Babelduab.
Contains a temper composed of broken pottery. 1978-38-7 (2) from Babelduab.
Type A' Palauan temper type; grog temper essentially lacking any terrigenous sand grains.
'Type A' Palauan temper type; grog temper essentially lacking any terrigenous sand grains.
'Type A' Palauan temper type; grog only.
Mixtures of grog particles and terrigenous grains (terrigenous grains more abundant than grog particles). Grains either felsic or mafic.
'Type B' Palauan temper type; hybrid feldspathic-lithic sand temper composed of mixed volcanic and calcareous sand.
Mixtures of grog particles and terrigenous grains (terrigenous grains more abundant than grog particles). Grains either felsic or mafic.
'Type B' Palauan temper type; hybrid feldspathic-lithic sand temper composed of mixed volcanic and calcareous sand.
'Type B' Palauan temper type; hybrid feldspathic-lithic sand temper composed of mixed volcanic and calcareous sand.
Mixtures of grog particles and terrigenous grains (terrigenous grains more abundant than grog particles). Grains either felsic or mafic.
Metavolcanic greenschist, schist micaceous.
Micaceous metavolcanic greenschist.
Yap natural metavolcanic.
Yap natural metavolcanic.
Foliated, polycrystalline metavolcanic rock temper sand, from Yap.
Quartzose.
Quartzose.
Grog and lithic. Lithics could be naturally part of clay. Higher exposure has brigher XPL.
Grog and lithics.
Grog and lithics. Higher exposure has brigher XPL.
Grog and lithics
Volcanic lithics mixed with sand.
Hybrid temper sand of mixed calcareous and terrigenous grains. Optically amorphous chitinous grains of tan coloration derived from crab or echinoid shells. Glassy rock fragments, microcrystalline volcanic rock fragments, clinopyroxenes, opaques, plagioclase.
Subrounded calcareous sand.
Calcareous and minor glassy (tan to brown) volcanic rock fragment. Opaque mineral.
Calcareous and minor plagioclase feldspar, clinopyroxene, intersertal volcanic rock fragment, glassy (brown) volcanic rock fragment, and opaque mineral.
Subrounded calcareous sand.
Calcareous and minor glassy (red-orange) volcanic rock fragment and opaque mineral.
Calcareous and minor intersertal volcanic rock fragment, glassy (tan) volcanic rock fragment.
Calcareous and minor glassy (tan and red-orange) volcanic rock fragment, and opaque mineral.
Calcareous and minor plagioclase feldspar, glassy (brown) volcanic rock fragment.
Calcareous reef debris hybrid.
Plain. Opaque.
Plain. Lithic.
Undecorated Lapitoid sherd. Lithic.
Plain. Pyroxenic.
Undecorated Lapitoid sherd. Pyroxenic.
Plain. Partial pyroxenic.
Undecorated Lapitoid sherd. Partial pyroxenic.
Partial placer.
Polynesian plainware. Has orthopyroxene. P index 0.88.
Polynesian plainware. Has orthopyroxene. P index 0.9.
Polynesian plainware. Has orthopyroxene. P index 0.9.
Polynesian plainware. Has orthopyroxene. P index 0.88.
Polynesian plainware. Has orthopyroxene. P index 0.89.
Polynesian plainware. Has orthopyroxene. P index 0.87.
Polynesian plainware. Has orthopyroxene. P index 0.86.
Vitric fabric. Some orthopyroxene.
Vitric fabric.
Gabbro fabric.
Gabbro fragments.
Gabbro fragments.
Lapita sherd. Lithic. Glassy predominate.
Hybrid partial placer.
Hybrid placer.
Partial placer.
Placer, Py index 0.85.
Placer. Orthopyroxenes and clinopyroxene.
Lapita sherd. Has orthopyroxene- Pindex 0.85.
Lapita sherd. Py index 0.81.
Lapita sherd. P index 0.86.
Lapita sherd. With orthopyroxenes.
Lapita sherd. Has orthopyroxene.
Lapita sherd. Orthopyroxenes present. P index 0.85.
Lapita sherd. Has orthopyroxenes. P index 0.86.
Unplacered sand temper possessing a 50-50 quartz to plagioclase ratio.
Moderately placered sand temper containing almost no quartz.
Partial placer.
Placer. Pyx index 0.88.
Placer. Py index 0.88
Lapita sherd. Has orthopyroxene. Py index 0.82
Lapita sherd. Has olivine. Has Py index 0.88.
Lapita sherd.
Lapita sherd. Plagioclase dominates, very weathered.
Lapita sherd. Quartzose temper.
Lapita sherd.
Ophiolitic. Non-Lapita sherd. Has granitic, gabbro and ultramafic rock fragments.
Non-Lapita sherd.
Amphibole rich. Ophiolitic. Granite and ultramafic rocks.
Amphibole rich. Ophiolitic. Granitoid and ultramafic rock source.
Has serpentite.
From Wattom-Wano.
Hybrid with limeclast calcareous and feldspar, microlitic and felsitic rock volcanic sands. Older sherd.
Placer quartose pyroxenic with opaque iron oxides.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sands. Moderately to well sorted aggregates of dominantly subangular to partly subrounded grains, and are inferred to be beach placers (calcareous) clinopyroxene, plagioclase, and quartz.mineral (pyroxene dacite) and exclusively volcanic rock fragments. some sherds have hornblende
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Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Pyroxenic placer sand temper interpreted as exotic to Nukuleka.
Lapita style. The pale brown clay contains remnant shelly fragments, up to 0.3 mm in length. Volcanic rock fragments contain mainly plagioclase crystals and tiny feldspar grains up to 0.5 mm in length. Subrounded ferruginized clasts and angular feldspar grains are about 0.2 mm in length. Contains wavy layers of red brown clay.
Lapita style. CAUTION: Section less than 30microns. This sample contains colourless to pale green pyroxene crystals (10%) up to 0.4 mm in length. Angular feldspar grains are up to 0.3 mm in length and there is less than 5%. There are rare grains of volcanic rock fragments up to 0.4 mm across, elongate to rounded ferruginized clasts of clay up to 2 mm in length, and carbonate shell fragments, about 0.5 mm across.
Lapita sherd. CAUTION: Section less than 30microns. This sample is similar to 8/1 but contains more and larger shelly fragments and fewer and smaller pyroxene grains. Volcanic rock fragments are up to 0.8 mm in length and consist of small feldspar crystals and opaque particles set in a glassy groundmass.
Lapita sherd. CAUTION: Section less than 30microns. This sample has reddish brown clay containing pyroxene crystals up to 0.5 mm in length. Feldspar grains up to 0.5mm in length, show growth rings. Volcanic rock fragments are composed mainly of glass with minor feldspar crystals. Opaque grains are up to 0.2 mm across.
Exotic pyroxenic temper.
Exotic placer. No orthopyroxene.
Western Lapita style sherd. No orthopyroxene in the temper.
Exotic sherd. No orthopyroxene.
Placer green-brown hornblende, with opaque iron oxides with either feldspars or augite pyroxenes. Microlitics are hyalopilitic.
Pyroxene, hornblende exotic.
Volcanic rock fragments dominant. Augitic clinopyroxene,minor opaque iron oxide grains and olivine grains, and rare hornblende grains are also present.
Lithic.
Lithic sand temper.
Lithic.
Lithic.
Transitional.
Transitional.
Transitional.
Transitional placer (35%-60% ferromagnesian grains) sand temper.
Transitional placer (35%-60% ferromagnesian grains) sand temper.
Transitional.
Transitional. Augitic clinopyroxene, minor opaque iron oxide grains and olivine grains, and rare hornblende grains are also present.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Placer sand.
Hybrid lithic sand temper with calcareous grains.
Hybrid lithic sand temper with ghost vacuoles.
Hybrid transitional.
Hybrid transitional placer (35%-60% ferromagnesian grains) sand temper with calcareous grains.
Hybrid placer.
Hybrid placer sand temper with calcareous grains.
Hybrid placer sand temper with calcareous grains.
Feldspathic-plagioclase, volcanic rock fragments (hyalopilitic-pilotaxitic and glassy vitric), some pyroxenes and hornblende.
Iron oxide opaques, plagioclase and volcanic rock fragments (hyalopilitic-pilotaxitic and glassy vitric).
Volcanic rock fragments (hyalopilitic-pilotaxitic and glassy vitric) and iron oxide opaques, plagioclase and pyroxenes.
Lithic.
Green hornblende.
Green hornblende.
Green hornblende.
Chrome spinel, orthopyroxene, and serpentinite grains are characteristic of ultramafic detritus.
Dominantly plagioclase, some pyroxene, partly crystalline volcanic rock fragments, some volcanic glass.
Feldspar rich.
Dominantly plagioclase, some pyroxene, partly crystalline volcanic rock fragments, some volcanic glass, some calcareous.
Pyroxene rich with opaque iron oxides.
Pyroxene rich with opaque iron oxides.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark vitric.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark vitric.
Volcanic rock fragments- poorly sorted alluvial sand, microlitic with dark vitric.
Lapita sherd. Plagioclase-rich non-placer. Calcareous grains appear to be reworked limeclasts, rather than modern reef detritus. Stream origin.
Lapita sherd, beach origin.
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Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar, clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
UPLT- Unusually high microlitic/ highest local felsitic lithics.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Unplacered local sand temper with plagioclase and microlitic/vitric volcanic rock fragments. Plagioclase feldspar , clinopyroxene , and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, vitric or glassy fragments of tan to brown (or red) volcanic glass.
Partially placered local sand temper, with dominant proportion of plagioclase, but significant proportions of clinopyroxene and opaque iron oxides. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Partially placered local sand temper, with dominant proportion of plagioclase, but significant proportions of clinopyroxene and opaque iron oxides. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Partially placered local sand temper, with dominant proportion of plagioclase, but significant proportions of clinopyroxene and opaque iron oxides. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Lapita sherd.
Hybrid-sand Efate temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Hybrid partially placered sand temper.
Hybrid-sand Efate temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Hybrid-sand Efate temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Hybrid-sand Efate temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Hybrid-sand Efate temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
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Pyroxenic Efate placer sand temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Pyroxenic Efate placer sand temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Pyroxenic Efate placer sand temper. Plagioclase feldspar, clinopyroxene, and opaque iron oxide grains. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
Strongly placered stream sand temper with dominant proportion of opaque iron oxides and subequal proportions of plagioclase and vitric volcanic rock fragments. Microlitic fragments in which birefringent plagioclase microlites are embedded in tan to brown volcanic glass, felsitic fragments composed of microgranular quartz-feldspar mosaics formed by devitrification of felsic volcanic glass, and vitric or glassy fragments of tan to brown (or red) volcanic glass.
NCMHT. K feldspar, mica and highest numbers of glaucophane.
Highest number of metamorphic rock fragments.
NCMT.
Quartzose-rich sand temper suggeting New Caledonian origin.
NCQT.
NCQT.
NCQT.
Hornblende.
HSET.
Hornblende.
NEHT.
Opaque iron oxide grains, and vitric volcanic rock fragments composed of mafic sideromelane (basaltic glass). The calcareous grains are skeletal and micritic (pelletal) debris of modern reefal origin, and the calcareous aggregates are well sorted sands with textures appropriate for a beach origin.
Olivine placer sand. Clinopyroxene dominant, but minor orthopyroxene.
Dominated by calcareous reef debritus. Beach origin. Possibly local. Very few volcanic rock fragments of altered volcanic glass.
Volcanic opaque-rich placer sand. Lapita sherd.
Volcanic placer. Medium opaque inclusions. Lapita sherd.
Felsitic lithic. Andesitic origin from bedrock in the interior of Malakula.
Limeclast volcanic lithic hybrid.
Tan glass vitrics with micro vesicular/pumiceous texture. Opaque rich, pink clay. Plagioclase.
Volcanic sand tempers, predominantly, polyminerallic volcanic rock fragments, with reddish vitric (glassy) groundmasses, but also some with microlitic and felsitic groundmass textures (all suitable for derivation from andesitic source rocks).
Mixtures of grog particles and terrigenous grains (terrigenous grains more abundant than grog particles). Grains either felsic or mafic. Vitric and microlitic lithics.
Non-placered hybrid of terrigenous and calcareous sand grains.
Placered hybrid of terrigenous and calcareous sand grains.
Grog (composed of broken pottery).
Detritus derived mostly from metavolcanic greenschist.
Temper sand mainly composed of plagioclase and clinopyroxene grains, but with subordinate proportions of Yap metavolcanics.
Temper sand mainly composed of plagioclase and clinopyroxene grains, but with subordinate proportions of Yap metavolcanics.
Type K. Feldspathic-pyroxenic.
Calcareous (Type A).
Calcareous (Type A).
Calcareous (Type A).
Calcareous marginally hybrid (Type B).
Calcareous marginally hybrid (Type B).
Calcareous marginally hybrid (Type B).
Opaque rich placer sands (Type CD).
Hornblendic-feldspathic, pyroxenic-free (Type E).
Hornblendic-feldspathic, pyroxenic-free (Type E).
Hornblendic-feldspathic, pyroxenic-free (Type E).
Pyroxene bearing hornblendic-feldspathic (Type F).
Pyroxene bearing hornblendic-feldspathic (Type F).
Pyroxene bearing hornblendic-feldspathic (Type F).
Pyroxene bearing hornblendic-feldspathic (Type F).
Pyroxenic (Type G).
Pyroxenic (Type G).
Pyroxenic (Type G).
Hybrid non-placer (Type H).
Calcareous (Type A).
Opaque rich placer sands (Type CD).
Hybrid non-placer (Type H).
Quartose feldspathic (Type J).
Quartose feldspathic (Type J).
Quartz-free andesitic temper sand. Stream sand present. Pyroxene < Hornblende.
Quartz-free andesitic temper sand. Stream sand present. Pyroxene > Hornblende.
Quartz-free andesitic temper sand. Stream sand present. Pyroxene < Hornblende.
Quartz-free andesitic temper sand. Stream sand present. Pyroxene < Hornblende.
Quartz-free andesitic temper sand. Coastal placer sand present. Pyroxene > Hornblende.
Lapita. Well sorted and rounded calcareous sand. Plagioclase.
Lapita. well sorted and rounded calcareous sand. Plagioclase.
Non-Lapita. Poorly sorted and weathered volcanic sand. Plagioclase and microphaneritic igneous rock fragments (microgranular grains composed dominantly of plagioclase-clinopyroxene with subophitic internal texture of clinopyroxene crystals partly enclosing plagioclase laths), microlitic volcanic rock fragments, opaque iron oxides, clinopyroxene, green hornblende, and deeply weathered brown biotite
Buka wares Fine-grained microgranular rock fragments dominant.
Buka wares Fine-grained microgranular rock fragments dominant.
Nissan-11 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Plagioclase and lesser clinopyroxene dominant.
Non-Lapita. Poorly sorted and weathered volcanic sand. Plagioclase and pyroxene.
Buka wares. Plagioclase and lesser clinopyroxene dominant.
Buka wares. Plagioclase and lesser clinopyroxene dominant.
Chert/metachert, quartzose/quartzite, felsite, and siltstone present. Some plagioclase altered albite.
Prehistoric potsherd. Poorly sorted, angular to subangular feldspathic aggregate sand temper.
Prehistoric potsherd. Poorly sorted, angular to subangular feldspathic aggregate sand temper.
Prehistoric potsherd. Poorly sorted, angular to subangular feldspathic aggregate sand temper.
Hornblendic plagioclase feldspathic stream temper. Kieta tradition sherd.
Hornblendic plagioclase feldspathic stream temper. Kieta tradition sherd.
Well sorted fine to medium grain, placer sands, rich in opaque iron oxides and hornblende, lesser plagioclase feldspars.
Well sorted fine to medium grain, placer sands, rich in opaque iron oxides and hornblende, lesser plagioclase feldspars.
Well sorted fine to medium grain, placer sands, rich in opaque iron oxides and hornblende, lesser plagioclase feldspars.
Well sorted fine to medium grain, placer sands, rich in opaque iron oxides and hornblende, lesser plagioclase feldspars.
Prehistoric potsherd. Moderately sorted, fine- to medium-grained, subangular to subrounded temper sand.
Prehistoric potsherd. Poorly sorted, angular to subangular feldspathic aggregate sand temper, tan to brown vitrics. Andesitic.
Prehistoric potsherd. Poorly sorted, angular to subangular feldspathic aggregate sand temper, tan to brown vitrics. Andesitic.
Modern potsherd. Clinopyroxene dominant, but minor orthopyroxene.
Maybe tempered. Plagioclase, with hornblende and clinopyroxene.
Tempered. Plagioclase, with hornblende and clinopyroxene.
Tempered. Plagioclase, with hornblende and clinopyroxene.
Tempered. Plagioclase, with hornblende and clinopyroxene.
Untempered. Plagioclase, with hornblende and clinopyroxene.
Untempered. Plagioclase, with hornblende and clinopyroxene.
Untempered. Plagioclase, with hornblende and clinopyroxene.
Untempered. Plagioclase, with hornblende and clinopyroxene.
Untempered. Plagioclase, with hornblende and clinopyroxene.
Early/Middle Transition Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Early Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Early Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Middle Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Early/Middle Transition Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Middle Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Middle Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Late Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Late Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Late Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.
Tikopia calcareous.
Rovianna Plainware A. Opaque-rich but quartz-bearing placer temper.
Rovianna Plainware B. Moderately sorted, fine, and subangular feldspathic but quartz-bearing sand temper.
Rovianna Plainware C. Moderately sorted, fine, and subangular hornblendic but quartz-free sand temper.
Rovianna Plainware C. Moderately sorted, fine, and subangular hornblendic but quartz-free sand temper.
Roviana Plainware C. Moderately sorted, fine, and subangular hornblendic but quartz-free sand temper.
Roviana Plainware C. Moderately sorted, fine, and subangular hornblendic but quartz-free sand temper.
Roviana Plainware C. Moderately sorted, fine, and subangular hornblendic but quartz-free sand temper.
Roviana Plainware D. Moderately sorted, fine, and subangular lithic but quartz-bearing sand temper.
Well sorted and subrounded to subangular aggregates of pyroxenic placer sand. Likely indigenous to Kolombangara.
Well sorted and subrounded to subangular aggregates of pyroxenic placer sand. Likely indigenous to Kolombangara.
Well sorted and subrounded to subangular aggregate of hornblendic placer sand. Likely exotic to Kolombangara.
Exotic quartz-calcite sand temper.
Hybrid quartz-calcite sand temper.
Hybrid quartz-calcite sand temper.
Exotic quartz-calcite sand temper.
Exotic quartz-calcite sand temper.
Matusuroto site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Irigila site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Matusuroto site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Matusuroto site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Matusuroto site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Irigila site. Mainly brown hornblende, but also green and oxyhornblende. Mildly to strongly placered hornblende-pyroxene sand temper.
Matusuroto site. Less placered (feldspathic) brown-hornblendic sand temper.
Matusuroto site. Less placered (feldspathic) brown-hornblendic sand temper.
Matusuroto site. Less placered (feldspathic) brown-hornblendic sand temper
Totutotu site. Variably placered green-hornblendic sand temper.
Totutotu site. Variably placered green-hornblendic sand temper.
Matusuroto site. Variably placered green-hornblendic sand temper.
Matusuroto site. Strongly placered hornblende-poor pyroxenic sand temper
Irigila site. Strongly placered hornblende-poor pyroxenic sand temper.
Matusuroto site. Strongly placered hornblende-free pyroxenic sand temper.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Rocks degraded with sericite. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim. Cut on neck.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim.
Imported Adzera- example of non-tempered, non-placer, mica, sericite rich. Cut perpendicular to rim. Rim cut.
Adzera-type comb and incised decoration
Non-Lapita sherd. Has quartzose-lithic temper.
Non-Lapita sherd. Has quartzose-lithic temper.
Non-Lapita sherd.
Non-Lapita sherd.
Quartz mica-schist lithics.
Lithic.
Lithic.
Lithic.
Lithic.
Ophiolitic temper.
Quartz-ophiolitic.
Quartz-ophiolitic.
Ophiolitic.
Ophiolitic.
Ophiolitic.
Rock fragments are mafic, with less felsic.
Rock fragments are mafic, with less felsic.
Vitric.
Tan vitric.
Tan vitric.
Tan vitric. Retoka.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Pale (felsic) vitric, may be from Efate.
Vitric.
Vitric.
Vitric.
Probably from Mele Plain.
Probably from Mele Plain.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Probably from Mele Plain.
Found Tongoa (Shepherd Islands). Tan vitric.
Plagioclase-rich.
Tan pumiceous vitrics.
Tan pumiceous vitrics
Tan pumiceous vitrics.
Plagioclase-poor and pyroxene rich temper. Non-Lapita sherd. Stream origin.
62-2 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Plagioclase-rich non-placer temper. Stream origin. Non-Lapita.
A pyroxene-rich (plagioclase-poor and lithic-poor) placer. Stream origin.
Olivine placer sand.
Quartz. Vitric.
Clinopyroxene-rich. Modern sherd.
Poorly sorted, subangular to subrounded volcanic sand temper probably representing natural temper embedded in sandy clay bodies collected from slightly reworked colluvium or ravine fillings on inland flanks of island volcanoes, contains clinopyroxene and plagioclase feldspar typical of sands derived from bedrock volcanic assemblages of basalt and mafic andesite. Abundant polycrystalline lithic fragments of: (a)microlitic grains with plagioclase laths or microlites, and (b) vitrics.
Colourless felsic glass.
Agarabi-ware. Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Sparse clinopyroxene. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim. Plain sherd.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Clinopyroxene. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim- at rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim probably.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich.
Non-tempered, tectonic highlands, non-placer, quartz- feldspar rich. Cut perpendicular to rim.
Madang style sherd. "CAUTION: Section less than 30microns. Pyroxene grains (<5%) are sub angular to sub rounded and up to 0.3 mm in length. Plagioclase grains, (<5%) are less than 0.2 mm in length. Sub rounded shelly fragments make up less than 2%. There is accessory volcanic rock fragments, red clay clasts and iron oxides.
Madang style sherd. "CAUTION: Section less than 30microns. This sherd contains a mixture of shelly fragments, pyroxene, plagioclase , iron oxide and volcanic rock fragments. All these components are present in roughly the same amounts. The grain size rarely exceeds 0.3 mm in length. There are some large clasts made up of ferruginized clay and feldspar. These could be weathered volcanic rock fragments or previous pot fragments. The clay is dark brown.
Madang style sherd. CAUTION: Section less than 30microns. Pyroxene and plagioclase grains are up to 0.3 mm in length. Magnetite grains are subrounded and elongate and less than 0.2 mm. Volcanic rock fragments are less than 0.2 mm in length. There are some minor quartzitic grains and red ferruginized grains. The clay is red brown and contains a small percentage of quartz and feldspar.
Madang style sherd. CAUTION: Section less than 30microns. Pyroxene crystals are about 0.3 mm in length. Plagioclase crystals are about 0.1 mm in length. Volcanic rock fragments are hypohyaline in texture and consist of plagioclase laths and altered glass. The are some yellow brown rounded clay clasts, red clay clasts, subrounded iron oxides are about 0.2 mm in length. The clay is brown and contains fine quartz and ferruginized opaques.
Madang style sherd. CAUTION: Section less than 30microns. Does not contain carbonate shell fragments and there are some large porphyritic dacite rock fragments. Volcanic rock fragments are also more abundant.
Madang style sherd. CAUTION: Section less than 30microns. Angular and subrounded feldspar grains, are generally 0.2 mm in diameter. Rock fragments are both volcanic and quartzitic. Volcanic rock fragments, up to 0.3 mm in length, generally contain plagioclase, opaques and minor pyroxene. A few grains consist of abundant iron oxide, altered glass and minor plagioclase. The quartz rock fragments are subrounded, about 0.2 mm across and are composed of small quartz mosaics.
Madang style sherd. CAUTION: Section less than 30microns. Angular to subrounded plagioclase crystals are the main mineral component. Pyroxene grains up to 0.3 m in length. Altered rock fragments generally contain plagioclase microlites and glass. Ferruginized clay clasts up to 1 mm in length are rare. Red iron oxide pellets and black magnetite present.
Madang style. CAUTION: Section less than 30microns. Angular quartz and feldspar grains (about 10%), Minor pyroxene grains are all <0.2 mm in length. There are some minor volcanic rock fragments which contain plagioclase, iron oxides and altered glass. Opaque minerals range in size from 0.1 to 0.5 mm in length, and there is less than 5% of those. The clay is red brown.
Madang style. CAUTION: Section less than 30microns. Angular feldspar and chert grains make up less than 10% of the sherd and are up to 0.4 mm in length. Volcanic rock fragments are found in two forms, one form consists of long thin plagioclase laths and skeletal iron oxides set in altered glass. The other form contains eutectic intergrowths of quartz and feldspar. The sherd also contains red ferruginized c lasts, iron oxides and minor pyroxene. The clay is red brown.
Madang style. CAUTION: Section less than 30microns. Quartz and plagioclase (about 10%) are less than 0.3 mm in length. There are some large volcanic rock fragments which contain plagioclase and pyroxene laths with minor iron oxide and also volcanic rock fragments which contain potash feldspar, plagioclase and quartz. Pyroxene grains are minor components and are up to 0.4 mm in length. There are also ferruginized clasts and iron oxides. The clay is red brown.
X style sherd. CAUTION: Section less than 30microns. This red brown sherd is characterized by sub rounded to rounded black clasts up to 2 rnn across and small amounts of quartz grains widely scattered through the sherd.
Type X sherd. Grog B. Contains subordinate ferruginous grains. KAM F/TIM.33 Open site. Body.
Type X sherd. Grog C.
Type X, GrogC
Type X sherd.
Type X, GrogA
Type X sherd.
Type X sherd. GrogA.
Type X sherd.
Type X, GrogA
Type X, GrogB
Type X sherd.
Type Y style. Contains high levels of amphibole. The amphibole is green to brown and the blades and prisms range from 0.1 to 0.5 mm in length. The angular amphibole grains make up about 10% of the sherd. Plagioclase (<10%) occurs as large rectangular crystals which show growth rings. Some of the grains are partly sericitized. Other plagioclase crystals are small and angular. Magnetite (<1%) .
Type Y style. This sherd contains quartz, feldspar, amphibole, pyroxene, magnetite, spinel, rock fragments, ferruginized clay clasts and relict shells. The quartz and feldspar grains (10%) are generally angular and 0.2 mm in length. Amphibole blades (<5%) are green to brown, and less than 0.2 mm across. Magnetite (5%) occurs as rounded grains. Pale green pyroxene crystals are rare. Spinel is an accessory mineral occurring as angular grains up to 0.2 mm.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene grains range in size from 0.1 up to 0.7 mm in length. There are some ferruginized clay pellets, up to 2 mm in length. Minor plagioclase and iron oxide minerals are also present. The sherd also contains abundant fine grained quartz grains, less than 0.1 mm
Sio style sherd. "CAUTION: Section less than 30microns. Pyroxene crystals are angular and about 0.4 mm in diameter. They are unaltered and show prominent cleavage traces. Volcanic rock fragments essentially contain ferruginized glass, feldspar crystals and small plagioclase laths. Opaques, rounded red brown clay clasts, ferruginized fossil fragments and feldspar grains are minor components. The clay is dark brown.
Sio style. CAUTION: Section less than 30microns. in diameter. Volcanic rock fragments (<10%) are up to 0.5 rnn across and contain feldspar microlites, opaques and altered glass. Angular pyroxene crystals are accessory. Elongate and rounded pellets are devoid of inclusions. The sherd also contains some large (up to 2 nm in length) ferruginized fragments which also contain opaques and plagioclase. These may be broken pot fragments. Opaque minerals.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (<5%) are up to 0.3 mm in length. Red ferruginized clasts (<1%). Opaques and strongly altered volcanic rock fragments are accessory components. The sherd also contains less than 5% of fine grained angular quartz.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (10%) are generally less than 0.3 mm in length. There are several large (up to 0.8 mm) dark ferruginized clasts and minor weathered volcanic rock fragments and angular quartz grains.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (<5%) are up to 0.3 mm in length. Angular quartz and feldspar grains make up about 10% of the sherd. These grains are generally small, <0.1 mm but range up to 0.2 mm. Opaque grains, (<5%) are subrounded and up to 0.4 mm in length. There are some minor rock fragments. The clay is red brown.
Madang style sherd. CAUTION: Section less than 30microns. Pyroxene occurs in grains up to 0.3 mm in length. Shelly fragments, are subrounded and less than 0.3 mm in length. Opaque minerals and black ferruginized grains are minor. There are some rock fragments containing pyroxene and plagioclase crystals, opaques and a trace of altered glass. Between these large grains there are abundant fine angular quartz grains.
Madang style sherd. CAUTION: Section less than 30 microns. Shelly fragments are generally subrounded and about 0.2 mm across. Plagioclase grains are about 0.1 mm in diameter and there are abundant small quartz grains widely scattered through the sherd. Opaque minerals are minor and there are some red to black ferruginized clasts. Pyroxene is rare.
Sio style sherd. CAUTION: Section less than 30microns. The pyroxene, Less than 5% forms elongate angular grains up to 0.3 mm in length. Angular feldspar grains (<5%) are widely scattered through the clay. There are a small number of dark brown to black ferruginized clasts. Angular rock fragments are composed of plagioclase laths and altered glass. There are some large fragments, up to 2 mm in length, which are composed of fine particles of clay, feldspar and brown iron oxide.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene crystals are elongate, up to 0.4 mm in length and are the dominant temper. Small amounts of plagioclase ranging in size from 0.1 to 0.3 mm in length are also present. The clay is dark brown.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene crystals are generally 0.3 mm in length. There is also minor amounts of altered volcanic rock fragments up to 1 mm across. Ferruginized clay clasts up to 0.5 mm across and small angular feldspar grains. The clay is dark red brown.
Sio style sherd. "CAUTION: Section less than 30microns. Pyroxene occurs as elongate blades and short stubby crystals ranging from 0,1 to 0.4 mm in length. Rectangular and angular plagioclase crystals, show weak seritization. Angular rock fragments generally contain plagioclase crystals, altered pyroxene crystals and opaques, all of which are less than 0.1 mm in length. Rounded red clay pellets are up to 0.3 nm in diameter. The clay is dark red brown.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene grains occur as elongate blades, up to 0.5 mm in length, angular stubby grains 0.2 mm in length, and as well developed crystals up to 0.3 mm across. Small angular plagioclase grains. Rock fragments composed of plagioclase crystals up to 0.3 nm in length are rare. Volcanic rock fragments are generally less than 0.2 mm in length and composed of opaques, clay and relict feldspar.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene crystals are abundant and make up most of the sample. They are closely packed, angular and about 0.3 mm in length. Plagioclase crystals are a minority. Opaque minerals are rare The clay is red brown.
Sio style sherd. CAUTION: Section less than 30microns. Contains abundant pyroxene and smaller amounts of volcanic rock fragments, plagioclase crystals and clay.
Sio style sherd. CAUTION: Section less than 30microns. Pyroxene crystals range from 0.1 to 0.5 mm in length. Plagioclase crystals are angular and less than 0.2 mm in length. Volcanic rock fragments are less than 0.5 mm in length and contain relict plagioclase, altered glass and mafic minerals and fine opaques. The clay is dark brown.
Sio style sherd. CAUTION: Section less than 30microns. Closely packed pyroxene grains are about 0.3 mm in length. There are some altered volcanic rock fragments and iron oxides. Small angular plagioclase grains are accessory.
Sio style sherd. CAUTION: Section less than 30microns. Shelly fragments are generally subrounded and less than 1 mm in diameter. Pyroxene grains are up to 0.3 mm in length. Plagioclase occurs as angular grains less than 0.2 mm in length. There is also accessory iron oxides and red clay pellets. The clay is red brown
Sio style sherd. CAUTION: Section less than 30microns. Shelly fragments, are up to 1 mm in length. Pyroxene crystals, plagioclase crystals range in size from <0.1 up to 0.2 mm in length. There is also accessory iron oxide grains and the clay is red brown.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (5%) are generally less than 0.4 m in length. Plagioclase laths (5%) are less than 0.2 mm in length. There are some large volcanic rock fragments made up of abundant plagioclase laths, minor pyroxene and fine grained opaques in a hypocrystallne texture. Accessory iron oxide and red ferruginized clay pellets are also present. The clay is dark brown.
Sio style. CAUTION: Section less than 30microns. Pyroxene crystals (<5%) are pale green to brown widely scattered and about 0.3 mm across. Volcanic rock fragments (<5%) are angular and up to 0.5 mm across. They contain plagioclase laths, opaques and altered glass. Red brown clay clasts up to 1 mm across contain small crystals of plagioclase and iron oxide. Rounded iron oxide grains make tp less than 2% of the sherd. The clay is red brown.
Sio style. CAUTION: Section less than 30microns. This dark red to black sherd contains abundant quartz and plagioclase up to 0.1 mm in length. There are some large pyroxene and volcanic rock fragments up to 0.4 mm in length but these grains are only accessory.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (<10%) are generally about 0.3 mm in length. Plagioclase grains (<5%) are less than 0.2 nm in length. There are some volcanic rock fragments, up to 0.7 mm across which are mainly composed of plagioclase laths, fine opaques and altered glass. This sherd also contains accessory iron oxides and red ferruginized grains.
Sio style. CAUTION: Section less than 30microns. Pyroxene crystals are less than 0.5 mm in length and make up about 5% of the sherd. Plagioclase grains are less than 0.2 mm in diameter and make up less than 5%. There are also some volcanic rock fragments, ferruginized clasts and opaque minerals. The clay is dark brown.
Sio style. CAUTION: Section less than 30microns. Pyroxene crystals are generally 0.5 mm in length and make up about 10% of the sherd. Altered volcanic rock fragments 5% are up to 0.5 mm in length and contain plagioclase laths, altered glass and mafic minerals. There are some red ferruginized clasts, the brown clay also contains small amounts of fine quartz and feldspar.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (<5%) are up to 0.5 mm in length. There are some large clasts more than 1 mm in length which resemble previous pot fragments. There are some red to black ferruginized grains and volcanic rock fragments. There is a small amount of fine grained quartz and feldspar in the brown clay.
Sio style. CAUTION: Section less than 30microns. Pyroxene crystals (<5%) are generally 0.2 mm in length and there are some large ones up to 0.5 mm in length. There is some altered volcanic rock fragments up to 0.5 mm in length, contain thin plagioclase crystals and yellow brown altered glass. Opaque minerals (5%) are less than 0.2 mm in length. There are some red ferruginized clasts up to 0.4 m in length and brown ferruginized clay clasts up to 0.1 mm in diameter. The clay is a pale brown.
Sio style. CAUTION: Section less than 30microns. Pyroxene grains (<5%) are up to 0.5 mm in length. There are minor chert fragments, red ferruginized clasts and iron oxide grains. The clay is pale brown and contains abundant fine grained quartz and feldspar. Volcanic rock fragments are rare.
Pyroxene grains (10%).Quartz and feldspar grains (<10%). There are some hypocrystalline volcanic rock fragments which contain large pyroxene crystals set in a ground mass of smaller pyroxene crystals, plagioclase, opaques and altered glass. The sherd also contains trace amounts of iron oxide and carbonate shell fragments.
WM-16-13 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Temper sand in which calcareous grains are predominant, with terrigenous grains rare but present.
Calcareous.
NLSU6 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Temper sand in which calcareous grains are dominant, with terrigenous grains present in significant amounts.
Quartz-calcite.
Quartz-calcite.
NLA4 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Stained. Temper sand in which calcareous and terrigenous grains are present in subequal proportions.
Quartz-calcite.