Slide: WD_102_3

Non-Lapita. Well sorted, subrounded to subangular aggreates that are probably beach sands. Volcanic rocks are felsitic (microcrystalline quartz-feldspar groundmass mosaic commonly with plagioclase microphenocrysts).

Mineral and Rock Abundances

Fabric: tpr179 - Bismarck feldspathic

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.	Quartz	Feldspar	Pyroxene	Amphibole	Opaques	Olivine	Biotite	Muscovite	Epidote	Garnet/ Spinel	Ig./Met. Rocks	Sed. Rocks	Grog	Lithics
0	0	5	1	1	0	0	0	0	0	0	4	0	0	felsitic, lathwork

Images

AnirL6 — Sherd AnirL6 from Ambitle (Ambitle). Slide WD_102_3 from Dickinson Collection, Bishop Museum. x4 Magnification PPL (left) XPL (right). Scale bar: 0.5mm. High resolution image in VIMIPO (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.

AnirL6 — Sherd AnirL6 from Ambitle (Ambitle). Slide WD_102_3 from Dickinson Collection, Bishop Museum. x4 Magnification PPL (left) XPL (right). Scale bar: 0.5mm. High resolution image in VIMIPO (user: Guest pwd: Guest). Imaged by K. Hardy and M. Leclerc, ANU.

Sherd: AnirL6

Non-Lapita

Period: None wikidata:

Site: Ambitle (Ambitle)

Suspected origin site: Anir

References:

043 Anir, Solomon 1972 (Dickinson, W.)

200 Kamgot, Ambitle, Fani, PNG, 2000 (Dickinson, W.)