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Obsidian from the Country Club Site, 14CO3 - Page

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These two fragments of obsidian were excavated from a Great Bend aspect village site in Cowley County during Phase IV archeological investigations in 1995. In 2005, they, along with other obsidian from the site, were sent for xray-florescence (XRF) testing, a chemical and elemental analysis that determines where material, such as these two obsidian flakes, came from originally. It was determined the obsidian from the site was Valles Rhyolite from the Cerro del Medio member and Cerro Toledo Rhyolite from the Obsidian Ridge member, both places found in the Jemez Mountains in New Mexico. Thus XRF studies help archeologists to learn about ancient trade patterns. The Country Club site had been much impacted by a water line, golf greens, roads, and highways. Excavations had been occurring at the site since 1916.

Date: 1400-1725 CE

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Obsidian from the Country Club Site, 14CO3 - 1Obsidian from the Country Club Site, 14CO3 - 2

Obsidian from the Country Club Site, 14CO3 - 1

Item Number: 455318
Call Number: 14CO3-145-1 & 14CO3-0-62
KSHS Identifier: DaRT ID: 455318

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