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Worked obsidian flake-knife base(?). Analysis code #4.
Obsidian crescent. Analysis code #4.
Worked obsidian ornament. Analysis code #1.
Worked obsidian pebble (scraper fragment?). No analysis code given.
Obsidian perforator fragment(?). Analysis code #3.
Utilized obsidian chunk(?). Both ends have been removed by retouch. Analysis code #4.
Chipped stone tool is made out of chalcedony and is unifacially flaked. Original bag stated: "blow-out," and "on surface of blowout in sandy soil with much dertris." (S. Iles, 4/27/2004)
Chipped stone tool is made out of chert and is unifacially flaked. Original bag stated: "Columbia River," "cave site," and "6/21/61." (S. Iles, 4/27/2004)
Chipped stone tool is made out of siltstone and is bifacially flaked. Original bag stated: "found on surface, on sandy moist soil along bank of river (Columbia)," "Crescent Bar at Cordes Junction," "Eastern Wash.," and "7/4/61." (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. Fitzgerald identified this material as orginating from the Cordiss Junction general vacinity, however, based on the site number, this material does not appear to be from the Cordiss Junction area. The material appears to be from an area several miles south of Cordiss Junction. (S. Iles 5/18/04)
Chipped stone tool is made out of chert and is bifacially flaked. Original bag stated: "found on surface, on sandy moist soil along bank of river (Columbia)," "Crescent Bar at Cordes Junction," "Eastern Wash.," and "7/4/61." (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. Fitzgerald identified this material as orginating from the Cordiss Junction general vacinity, however, based on the site number, this material does not appear to be from the Cordiss Junction area. The material appears to be from an area several miles south of Cordiss Junction. (S. Iles 5/18/04)