Abstract
AbstractA hydration rate for obsidian of 1.3 μm2 per 1,000 radiocarbon years has been calculated for the lower Columbia River Valley of Oregon and Washington. The rate provides a means for dating prehistoric archaeological sites containing obsidian in terms of their radiocarbon age.
Publisher
Cambridge University Press (CUP)
Subject
Museology,Archaeology,Arts and Humanities (miscellaneous),History
Cited by
3 articles.
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