Applied relief and carved paddle decorated.
| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 |
| 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_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 |
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.