Abstract
ABSTRACTA revised hydration rate for obsidian from the central Arizona Government Mountain-Sitgreaves Peak source area is presented. Data obtained since 1975 suggest that the hydration characteristics of obsidian from 1 to 6,000 years B.P. can best be predicted using a simple squared diffusion model. This new rate improves the accuracy of previously reported rates and, consequently, will increase the usefulness of obsidian hydration dating throughout central and northern Arizona.
Talk to us
Join us for a 30 min session where you can share your feedback and ask us any queries you have
Schedule a callDisclaimer: All third-party content on this website/platform is and will remain the property of their respective owners and is provided on "as is" basis without any warranties, express or implied. Use of third-party content does not indicate any affiliation, sponsorship with or endorsement by them. Any references to third-party content is to identify the corresponding services and shall be considered fair use under The CopyrightLaw.
