Site: Mono Island

Island: Shortland Islands

Fabrics:

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
tpr110	0	1	6	2	3	1	0	0	0	0	0	3	0	0	microlitic
Shortland feldspathic	0	0	6	1	1	1	0	0	0	0	0	1	0	0	Solomons

Slides:

Slide	Fabric	Possible Origin	Cal.	Quartz	Feldspar	Pyroxene	Amphibole	Opaques	Olivine	Biotite	Muscovite	Epidote	Garnet/ Spinel	Ig./Met. Rocks	Sed. Rocks	Grog	Lithics
WD_103_11	tpr110 (Shortland feldspathic)	Bougainville/SI	0	0	6	1	3	1	0	0	0	0	0	2	0	0	microlitic
WD_103_2	tpr110 (Shortland feldspathic)	Bougainville/SI	0	0	6	1	3	1	0	0	0	0	0	2	0	0	microlitic

WD_103_11

shortlandM2 — Sherd M2 from Mono Island (Shortland Islands). Slide WD_103_11 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.

Late Period Ware,. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.

WD_103_2

shortlandM1 — Sherd M1 from Mono Island (Shortland Islands). Slide WD_103_2 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.

Middle Period Ware. Feldspathic sands in which plagioclase mineral grains of volcanic derivation form the predominant grain type. Distinguised from others by the green hornblende lacking brown pleochromic tints.