Slide: WD_57_6

Plagioclase-rich non-placer temper. Stream origin. Non-Lapita.

Mineral and Rock Abundances

Fabric: tpr221 - Erromango feldspathic non-placer

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%
Cal. QuartzFeldspar Pyroxene Amphibole Opaques OlivineBiotite Muscovite Epidote Garnet/ Spinel Ig./Met. Rocks Sed. Rocks Grog Lithics
0 0 3 4 0 3 0 0 0 0 0 3 0 0 lathwork, vitric, microlitic

Images

62-2 has a full slide scan available. Imaged by K. Hardy and M. Leclerc, ANU.


Sherd: 62-2

None

Period: None wikidata:

Site: Ifo (Erromango)

Suspected origin site: Erromango

References:

147 Erromango, Vanuatu, 1998 (see 177) (Dickinson, W.)

170 Erromango, Vanuatu, Nendo, Santa Cruz group, 1998 (see 177) (Dickinson, W.)

177 Erromango, Vanuatu, correction to 147 and 170, 1998 (Dickinson, W.)