Nguna-Emau: Basalt / Picro-Basalt, Composite type, Stratovolcano(es).
East Epi: Basalt / Picro-Basalt, Cluster type, Stratovolcano(es).
Kuwae: Basalt / Picro-Basalt, Caldera type, Caldera.
Pomare: , Composite type, Stratovolcano.
Tavani Ruro: , Composite type, Stratovolcano.
Tongoa: , Composite type, .
Northeast Shepherd Islands: Basalt / Picro-Basalt, Composite type, Stratovolcano(es).
Unnamed: , Composite type, Stratovolcano.
Northern Efate: , Cluster type, Stratovolcano(es).
Northwest Shepherd Islands: , Composite type, Complex.
Southern Shepherd Islands: , Composite type, Stratovolcano.
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Many fabrics have a range of abundances. The range maximum (top) and minimum (bottom) are shown.
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| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 |
| tpr239 ** | 0 | 0 | 5 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, felsitic, microlitic |
| Shepherd feldspathic | 0 | 0 | 4 | 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 |
| 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 |
| tpr232a | 4 | 1 | 2 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, microlitic, felsitic |
| Exotic Efate hornblendic | 4 | 1 | 2 | 1 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 3 | 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 |
| Slide | Fabric | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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_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_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_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_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_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_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_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_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_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_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_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_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_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_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 |
| 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_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_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 |
| WD_47_25 | tpr219 (Santo-Malo lithic) | Malo | 0 | 0 | 3 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic | |
| 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_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_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_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_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_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 |
Rock fragments are mafic, with less felsic.
Rock fragments are mafic, with less felsic.
Pale (felsic) vitric, may be from Efate.
Vitric.
Feldspathic standard Efate.
Feldspathic standard Efate.
Feldspathic standard Efate.
Tan vitric.
Vitric.
Vitric.
Feldspathic standard Efate.
Vitric.
Probably from Mele Plain.
Probably from Mele Plain.
Probably from Mele Plain.
TC66 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
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.
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.
TC39 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
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.
Vitric.
Plagioclase-rich.
Tan pumiceous vitrics.
Tan pumiceous vitrics
Tan pumiceous vitrics.
Vitric.
Found Tongoa (Shepherd Islands). Tan vitric.
Microlitic.
Vitric.
Vitric.
Vitric.
Vitric.
Vitric.
Lapita sherd.
Tan vitric.
Tan vitric. Retoka.
Feldspathic standard Efate.