A late Pleistocene tephra layer in the southern Great Basin and Colorado Plateau derived from Mono Craters, California

Quaternary Research
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Abstract

A newly identified tephra in stratified deposits in southwestern Utah, dated ???14,000 14C yr B.P., may aid in correlating late Pleistocene deposits across parts of the southern Great Basin and west-central Colorado Plateau. Geochemical analyses of the ash suggest the tephra originated from Mono Craters, California, and most probably correlates with Wilson Creek ash #3. Because the ash is 2 mm thick ???550 km from its source, the event may have been larger than others correlated to Mono Craters eruptions. ?? 2002 University of Washington.
Publication type Article
Publication Subtype Journal Article
Title A late Pleistocene tephra layer in the southern Great Basin and Colorado Plateau derived from Mono Craters, California
Series title Quaternary Research
DOI 10.1006/qres.2002.2326
Volume 57
Issue 3
Year Published 2002
Language English
Larger Work Type Article
Larger Work Subtype Journal Article
Larger Work Title Quaternary Research
First page 382
Last page 390
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