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Modified StoneSAJH136033, 136037, 13605

Mudstone, incised, three fragments now glued together. Carved with eye and possibly mouth location, segmented concentric circle border around "face." Darkened areas, object appears burnt. Decoration on both sides. Still needs SAJH number affixed.

Material
mudstone
Holding Institution
The Burke: University of Washington
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Modified StoneSAJH130573

Incised mudstone with incised lines; "face" on one side, "SAJH 130573" written in white on one broken end, "47/1" written in black, upside down from the first. White dot next to "47/1" and above SAJH number.

Material
mudstone
Holding Institution
The Burke: University of Washington
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Concretion, Clay2004-63/50

Clay concretion is made from mudstone and is unifacially flaked. (S. Iles 5/5/2004)

Material
mudstone stone
Holding Institution
The Burke: University of Washington
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Concretion, Clay2004-63/9

Clay concretion is made from mudstone and is incised with straight lines across the center of one side. (S. Iles 5/5/2004)

Material
mudstone stone
Holding Institution
The Burke: University of Washington
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BeadT-396.02

Mudstone bead (Figure 11.1d; Larson & Lewarch 1995: 11-2 to 11-10).

Material
stone and mudstone
Holding Institution
The Burke: University of Washington
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BeadT-369.01

Mudstone bead (Figure 11.2c; Larson & Lewarch 1995: 11-2 to 11-10).

Material
stone and mudstone
Holding Institution
The Burke: University of Washington
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BeadT-368.01

Mudstone bead (Larson & Lewarch 1995: 11-2 to 11-10).

Material
stone and mudstone
Holding Institution
The Burke: University of Washington
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Core45GR79/2004-63/6

Core is made out of siltstone, is flaked, and is elliptical in shape. Original bag stated: "blow-out," "surface," "found on beach in sandy soil," and "7/6/61." (S. Iles, 4/27/2004)

Material
siltstone stone
Holding Institution
The Burke: University of Washington
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Chipped Stone Tool45GR73/2004-63/24

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)

Material
siltstone stone
Holding Institution
The Burke: University of Washington
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Abrader2019.O.006:363

tan, depression on one side indicating use as abrader, flattened deression on other side, fine grained, opaque

Material
siltstone
Holding Institution
Sto:lo Research & Resource Management Centre
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