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Major- and trace-element characterization, expanded distribution, and a new chronology for the latest Pleistocene Glacier Peak tephras in western North America

Published online by Cambridge University Press:  20 January 2017

Stephen C. Kuehn ,
Duane G. Froese ,
Paul E. Carrara ,
Franklin F. Foit Jr. ,
Nicholas J.G. Pearce  and
Peter Rotheisler
Stephen C. Kuehn*
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, 1-26 Earth Sciences Building, Edmonton, AB, Canada T6G 2E3
Duane G. Froese
Affiliation:
Department of Earth and Atmospheric Sciences, University of Alberta, 1-26 Earth Sciences Building, Edmonton, AB, Canada T6G 2E3
Paul E. Carrara
Affiliation:
United States Geological Survey, Box 25046, Denver Federal Center Mail Stop 980, Denver, CO 80225-0046, USA
Franklin F. Foit Jr.
Affiliation:
School of Earth and Environmental Sciences, Washington State University, PO Box 642812, Pullman, WA 99164-2812, USA
Nicholas J.G. Pearce
Affiliation:
Institute of Geography and Earth Sciences, Aberystwyth University, Aberystwyth, SY23 3DB, Wales, UK
Peter Rotheisler
Affiliation:
Department of Geography and Earth and Environmental Science, Okanagan College, 1000 KLO Road, Kelowna, BC, Canada V1Y 4X8
*
⁎Corresponding author. Fax: +1 780 492 2030. Email Address:[email protected], [email protected]
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Abstract

The Glacier Peak tephra beds are among the most widespread and arguably some of the most important late Pleistocene chronostratigraphic markers in western North America. These beds represent a series of closely-spaced Plinian and sub-Plinian eruptions from Glacier Peak, Washington. The two most widespread beds, Glacier Peak ‘G’ and ‘B’, are reliably distinguished by their glass major and trace element abundances. These beds are also more broadly distributed than previously considered, covering at least 550,000 and 260,000 km2, respectively. A third bed, the Irvine bed, known only from southern Alberta, is similar in its major-element composition to the Glacier Peak G bed, but it shows considerable differences in trace element concentrations. The Irvine bed is likely considerably older than the G and B tephras and probably records an additional Plinian eruption, perhaps also from Glacier Peak but from a different magma than G through B. A review of the published radiocarbon ages, new ages in this study, and consideration in a Bayesian framework suggest that the widespread G and B beds are several hundred years older than widely assumed. Our revised age is about 11,600 14C yr BP or a calibrated age (at 2 sigma) of 13,710–13,410 cal yr BP.

Keywords

Glacier PeakTephraTephrochronologyMajor-element analysisTrace-element analysisElectron probe microanalysis (EPMA)Radiocarbon datingBayesian calibrationLate Pleistocene
Type
Articles
Information
Quaternary Research , Volume 71 , Issue 2 , March 2009 , pp. 201 - 216
Copyright
University of Washington

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