Pyroxenic Opaque: Dominated by pyroxenic inclusions with opaques.
Late Lapita Solomons (2700 - 1800 BP)
Post-Lapita Solomons (2500 - 0 BP)
Early Post-Lapita Solomons (2700 - 2000 BP)
| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| Max | 0 | 0 | 4 | 4 | 1 | 4 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Min | 0 | 0 | 3 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | Solomons |
| Slide | Site | Possible Origin | Ware | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_35_25 | Kolombangara (Kolombangara) | 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 | Kolombangara (Kolombangara) | Kolombangara | Early Post-Lapita Solomons (2700 - 2000 BP) | 0 | 0 | 4 | 4 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | microlitic, vitric |
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.