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Correlation of Volcanic Ash Deposits by Activation Analysis of Glass Separates1

Published online by Cambridge University Press:  20 January 2017

G. A. Borchardt ,
M. E. Harward  and
R. A. Schmitt
R. A. Schmitt
Affiliation:
Former Graduate Research Assistant, presently NRC Postdoctoral Research Associate, U.S. Geological Suryey, Denver Federal Center, Denver, Colorado, Professors in the Departments of Soils and of Chemistry, Oregon State University, respectively
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Abstract

Volcanic ash deposits whose source is the Cascade Mountains area were correlated on the basis of 19 elemental abundances obtained by instrumental neutron activation analysis (INAA). After activation of glassy separates in a TRIGA reactor, gammaray spectra were obtained and analyzed with computer programs. The elements Na, Sm, Sc, Fe, Ce, Hf, and Th were determined with relative standard deviations less than 5%; the precision for La, Co, Eu, Yb, Cs, Ba, and Lu was less than 17%; larger errors were obtained for Rb, Ta, Nd, Tb, and Cr. A statistical method was developed for correlation on the basis of relative elemental compositions unique to the ash deposits. Elemental abundances of Mazama glassy separates were independent of distance from the source. The site to site chemical variability of crystal rich Glacier Peak and St. Helens ash layers was greater than for Mazama and Newberry ashes. The Rb, Yb, Lu, Th, and Ta contents in Newberry glass were more than twice those in Mazama glass. The concentrations of trace elements in Glacier Peak and St. Helens ashes generally were less than one-half those in Mazama glass. The presence of Mazama ash has been confirmed at sites in Oregon, Washington, Alberta, and in sediments of the Pacific Ocean.

Type
Original Articles
Information
Quaternary Research , Volume 1 , Issue 2 , April 1971 , pp. 247 - 260
Copyright
University of Washington

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Footnotes

1

Technical Paper No. 2901, Oregon Agricultural Experiment Station, Corvallis, Oregon. Supported in part by AEC contract AT (45-1) 2062.

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