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Point, Chipped Stone1989-57/35-R-365
Black obsidian, side-notched, lanceolate point. One side of base is broken. 11/02/98 D. Bradley.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-R-90
Black obsidian, side-notched point with broken tip. D. Bradley 10-26-98.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-R-89
Black obsidian, side-notched point. D. Bradley 10-26-98.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-F-56
Black obsidian, side-notched point with concave base and broken tip. There is an adhering matrix on one side. M. Christopher 01/08/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-F-117
Black obsidian point, one side is side-notched the opposite side is basal-notched. Tip is broken. D. Bradley 01/11/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-R-74
Black obsidian, side-notched point with contracting stem and concave base. D. Bradley 10-26-98.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-I-7
Black obsidian, side-notched point with broken tip and base. There is an adhering matrix on one side. D. Bradley 01/14/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-Q-87
Black obsidian point; one side is corner-notched and the other side is side-notched. D. Bradley 02/05/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped StoneW3/7/1888
Brown. Basal edge remains, convex.
- Material
- chert stone and pebble
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-A-114
Black obsidian, side-notched point with concave base and tip broken horizontally to base. There is an adhering matrix on one side. K. Peterson 2/5/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington