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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 |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| tpr16 | 6 | 0 | 1 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 1 | 0 | 0 | na |
| Guam calcareous | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | Marianas |
| tpr17 ** | 0 | 0 | 2 | 6 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| Guam pyroxenic | 0 | 0 | 1 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 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 |
| tpr20 ** | 0 | 0 | 3 | 3 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| Guam lithic andesiitic | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 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 |
| 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 |
| tpr18 | 4 | 0 | 2 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| Guam hybrid | 2 | 0 | 1 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 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 |
| 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 |
| Slide | Fabric | Possible Origin | Cal. | Quartz | Feldspar | Pyroxene | Amphibole | Opaques | Olivine | Biotite | Muscovite | Epidote | Garnet/ Spinel | Ig./Met. Rocks | Sed. Rocks | Grog | Lithics |
|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|---|
| WD_5_25 | tpr16 (Guam calcareous) | Guam | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_5_6 | tpr17 (Guam pyroxenic) | Guam | 0 | 0 | 2 | 5 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, vitric |
| WD_7_24 | tpr21 (Guam lithic hi andesitic) | Guam | 0 | 0 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_7_21 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 3 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_2_25 | tpr22 (Saipan quartzose) | Saipan | 0 | 3 | 4 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 3 | 0 | 0 | vitric, felsitic |
| WD_8_5 | tpr19 (Guam vitric andesitic) | Guam | 0 | 0 | 5 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | felsitic, microlitic, vitric |
| WD_5_17 | tpr16 (Guam calcareous) | Guam | 6 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | na |
| WD_5_14 | tpr18 (Guam hybrid) | Guam | 4 | 0 | 2 | 4 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_5_7 | tpr18 (Guam hybrid) | Guam | 4 | 0 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | felsitic, vitric |
| WD_5_15 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 3 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| WD_7_16 | tpr19 (Guam vitric andesitic) | Guam | 0 | 0 | 3 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_7_4 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 3 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, microlitic |
| WD_7_8 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 1 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| WD_7_3 | tpr21 (Guam lithic hi andesitic) | Guam | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| WD_15_23 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 1 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric |
| WD_5_20 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 3 | 2 | 0 | 3 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| WD_5_13 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic |
| WD_5_9 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 2 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, vitric |
| WD_8_12 | tpr18 (Guam hybrid) | Guam | 2 | 0 | 1 | 5 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | vitric, microlitic |
| WD_8_14 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | microlitic, vitric |
| WD_8_16 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric |
| WD_8_9 | tpr21 (Guam lithic hi andesitic) | Guam | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | microlitic, vitric |
| WD_7_23 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 1 | 0 | 2 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric |
| WD_6_17 | tpr8 (Saipan hybrid quartzose) | Saipan | 4 | 4 | 2 | 1 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 2 | 0 | 0 | microlitic, felsitic |
| WD_7_19 | tpr19 (Guam vitric andesitic) | Guam | 0 | 0 | 4 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 4 | 0 | 0 | vitric, microlitic |
| WD_7_1 | tpr21 (Guam lithic hi andesitic) | Guam | 0 | 0 | 1 | 2 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 6 | 0 | 0 | vitric, microlitic |
| WD_2_23 | tpr5 (Saipan dacitic) | Saipan | 0 | 3 | 3 | 0 | 0 | 1 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | vitric, felsitic |
| WD_5_18 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, vitric |
| WD_5_8 | tpr20 (Guam lithic andesiitic) | Guam | 0 | 0 | 2 | 3 | 0 | 0 | 0 | 0 | 0 | 0 | 0 | 5 | 0 | 0 | felsitic, vitric |
Calcareous temper.
Pyroxenic volcanic sand temper. Clinopyroxene dominant, but minor orthopyroxene.
Andesitic temper sand rich in glassy volcanic rock fragments and lacking any calcareous grains indicative of coastal origin.
Sand temper likely derived from wares made on Guam.
Sand temper likely derived from wares made on Saipan.
Historic sherd. Feldspathic andesitic volcanic sand temper, moderately sorted and composed of subrounded to subangular grains of very fine to medium size.
Nomna-11 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Calcareous.
Nomna-8 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Hybrid lithic.
Volcanic calcareous temper.
Nomna-9 has a full slide scan available (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.
Lithic volcanic sand.
Lowly lithic sand temper.
Mediumly lithic sand temper.
Mediumly lithic sand temper.
Highly lithic sand temper.
Volcanic sand temper rich in brownish to reddish glassy lithic fragments. Early historic sherd.
Volcanic sand temper.
Groundmass rock fragment suite distinct from that at Nomna Bay (more microlitic than vitric).
Lithic-rich volcanic sand temper.
Hybrid beach sand temper in which calcareous reef detritus is admixed with terrigenous grains derived from volcanic rocks.
Poorly sorted volcanic sand temper rich in glassy volcanic rock fragments characteristic of indigenous Guam tempers.
Poorly sorted volcanic sand temper rich in glassy volcanic rock fragments characteristic of indigenous Guam tempers.
Poorly sorted volcanic sand temper rich in glassy volcanic rock fragments characteristic of indigenous Guam tempers.
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.
Hybrid quartose dactic. Called 443 in report. Imported. pre-latte.
Lowly lithic sand temper.
Highly lithic sand temper.
Contains quartz-bearing temper sand diagnostic of derivation from Saipan.
Indigenous source.
Volcanic sand temper.