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Point, Chipped Stone1989-57/35-L-38
Black obsidian corner-notched point with corner of base broken. K. Peterson 11/30/98
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Biface1989-57/35-N-6
Black obsidian cylindrical biface fragment. D. Bradley 01/14/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-F-156
Black obsidian side-notched point. D. Bradley 01/11/99
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Biface1989-57/35-R-333
Black obsidian biface fragment that is broken at one end and comes to a point at the opposite end. There is an adhering matrix on one side. M. Christopher 11/02/1998.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-L-14
Black obsidian shouldered, stemmed point with concave base. Tip, one shoulder, and base corners are broken. K. Peterson 11/23/98
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Scraper, Stone1989-57/35-D-32
Black obsidian bifacial scraper. M. Christopher 5/28/98
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-F-41
Black obsidian, stemmed point with a concave base and broken tip. One side is corner-notched, the other is side notched. 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 Stone1989-57/2-183
Brown, chert, shouldered, stemmed point. E. Perez-Lizano, 1/20/98
- Material
- chert stone
- Holding Institution
- The Burke: University of Washington
Point, Chipped Stone1989-57/35-R-92
Black obsidian, side-notched point with a concave base. D. Bradley 10-26-98.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington
Point, Biface1989-57/35-R-246
Black obsidian, leaf-shaped biface that is broken at one end. There is an adhering matrix on one side. 11/02/98 D. Bradley.
- Material
- obsidian stone
- Holding Institution
- The Burke: University of Washington