Sanma Province Wikidata ID: Q740640
Note that to see the 'Geology' layer (layer options in top right corner) you may have to zoom out.
| 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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| 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 |
| 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_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 |
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.