Hostname: page-component-586b7cd67f-rdxmf Total loading time: 0 Render date: 2024-11-30T21:50:02.811Z Has data issue: false hasContentIssue false
  • English
  • Français

Geology of the Ruby Site Area, Wyoming 48 CA 302

Published online by Cambridge University Press:  20 January 2017

John Albanese
John Albanese*
Affiliation:
Casper, Wyoming
Get access Rights & Permissions [Opens in a new window]

Abstract

Quaternary sediments in the Ruby site area are of post-altithermal age. Two past alternating cycles of deposition and erosion are evident. The oldest depositional unit contains an archaeological site which yielded a radiocarbon date of A.D. 280 ± 135 years. This older formation was deposited in post-Kaycee-pre-Lightning time. A stratigraphic unit of this age has not been previously reported in the Powder River Basin and is herein named the South Butte formation. The youngest depositional unit in the area is the Lightning formation. Erosion and downcutting began about 1900 and has continued to the present.

Type
Reports
Information
American Antiquity , Volume 36 , Issue 1 , January 1971 , pp. 91 - 95
Copyright
Copyright © The Society for American Archaeology 1971

Access options

Get access to the full version of this content by using one of the access options below. (Log in options will check for institutional or personal access. Content may require purchase if you do not have access.)

References

Haynes, C. V. Jr. 1966 Geochronology of late Quaternary alluvium. Interim Research Report No. 10. Geochronology Laboratories, University of Arizona.Google Scholar
Haynes, C. V. Jr., and Grey, D. C. 1965 The Sister’s Hill site and its bearing on the Wyoming post-glacial alluvial chronology. Plains Anthropologist 10:196–207.CrossRefGoogle Scholar
Leopold, L. B., and Miller, J. P. 1954 A postglacial chronology for some alluvial valleys in Wyoming. U. S. Geological Survey Water Supply Paper 1261.Google Scholar