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Drill, Chipped Stone45DO3/2004-63/1

Drill is made out of chaldecony and is rod-shaped and flaked. Original bag stated: "Cordis Junction," "Eastern Washington," "Columbia River," "surface," and "8/2/61." (S. Iles, 4/20/2004) Robert Greengo identified that "Cordiss Junction is (was) probably a point on the Burlington Northern railroad that runs from Wenatchee to the east, very near Crescent Bar and Trinidad," WA. (S. Iles 5/18/04)

Material
chalcedony stone
Holding Institution
The Burke: University of Washington
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Utilized Flake2003-146/18

Utilized flake is made out of basalt and is flaked unifacially. (S.Iles 3/30/2004)

Material
basalt stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/7

Point is made out of basalt and is flaked bifacially. It has a contracting stem. There is tape or label residue on the mid-section of both sides. (S.Iles 3/30/2004)

Material
basalt stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/6

Point is made out of basalt and is flaked bifacially. It is unstemmed and has a contracting base. There is tape and label residue on the mid-section of both sides. (S.Iles 3/30/2004)

Material
basalt stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/5

Point is made out of basalt and is flaked bifacially. It is broken and is missing the stem. (S.Iles 3/30/2004)

Material
basalt stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/4

Point is made out of dacite and is flaked bifacially. It is unstemmed with a contracting base. There is a white residue on one side of the tip. (S.Iles 3/30/2004)

Material
dacite stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/3

Point is made out of obsidian and is flaked bifacially. It is corner notched. (S.Iles 3/30/2004)

Material
obsidian stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone2003-146/1

Stone point with contracting stem. (S.Iles 3/30/2004)

Material
stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone1999-97/241

This is a crystalline volcanic rock (basalt) point with a tapering, triangular base with semi-conspicuous shoulders. Tip of the base is missing. The middle third of the point is serrated. J. Fisher 07/15/03

Material
crystalline volcan stone
Holding Institution
The Burke: University of Washington
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Point, Chipped Stone1999-97/240

This is a crystalline volcanic rock (basalt) point with a tapering, triangular base with inconspicuous shoulders. Tip of the point is missing. J. Fisher 07/15/03

Material
crystalline volcan stone
Holding Institution
The Burke: University of Washington
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