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Heterogeneity, Correlatives, and Proposed Stratigraphic Nomenclature of Hayes Tephra Set H, Alaska

Published online by Cambridge University Press:  20 January 2017

Abstract

Several Holocene tephra deposits of Hayes volcano constitute a marker horizon in southern and east-central Alaska. Their identification is aided by high amphibole/pyroxene ratio and biotite in trace amounts, unique among Holocene tephra deposits of the region. However, correlations are obscured by chemical heterogeneity of the glass which occurs at a scale less than the size of a lapilli. Single-shard analyses confirm that the heterogeneity is due neither to fractionation nor to plagioclase microlites. The heterogeneity may be due to mixing of magmas prior to eruption. It is proposed that the deposits be informally called Hayes tephra set H.

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Articles
Copyright
University of Washington

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References

Beget, J. E. Reger, R. D. Pinney, DeAnne, Gillispie, Tom, , and Campbell, Kathy, (1991). Correlation of the Holocene Jarvis Creek, Tangle Lakes, Cantwell, and Hayes tephras in south-central and central Alaska. Quaternary Research 35, 174189.CrossRefGoogle Scholar
Bowers, P. (1979). The Cantwell ash bed, a Holocene tephra in the central Alaska range. Alaska Division of Geological and Geophysical Surveys Geologic Report 61, 1924.Google Scholar
Davis, J. O. (1985), Correlation of late Quaternary tephra layers in a long pluvial sequence near Summer Lake, Oregon. Quaternary Research 23, 2853.CrossRefGoogle Scholar
Mullineaux, D. R. Hyde, J. H., and Rubin, Meyer, (1975). Widespread late glacial and postglacial tephra deposits from Mount St. Helens volcano, Washington. U.S. Geological Survey Journal of Research 3, 329335.Google Scholar
Nielson, C. H., and Sigudsson, H. (1981). Quantitative methods for electron microprobe analysis of sodium in natural and synthetic glasses. American Mineralogist 66, 547552.Google Scholar
North American Commission on Stratigraphic Nomenclature (NASCN) (1983). North American Stratigraphic code. American Association of Petroleum Geologists Bulletin 67, 841875.Google Scholar
Péwé, T. L. (1975). “Quaternary Stratigraphic Nomenclature in Unglaciated Central Alaska.” U.S. Geological Survey Professional Paper 862.Google Scholar
Reger, R. D. Pew£, T. L. Hadleigh-West, Frederick, , and Skarland, Ivar, (1964). Geology and archeology of the Yardang Flint Station. University of Alaska Anthropological Papers 12, 92100.Google Scholar
Riehle, J. R. (1985). A reconnaissance of the major tephra deposits in the upper Cook Inlet region, Alaska. Journal of Volcanology and Geothermal Research 26, 3774.CrossRefGoogle Scholar
Riehle, J. R. Bowers, P. M., and Ager, T. A. (1990). The Hayes tephra deposits, an upper Holocene marker horizon in south-central Alaska. Quaternary Research 33, 276290.CrossRefGoogle Scholar
Riehle, J. R. Champion, D. E. Brew, D. A., and Lanphere, M. A.. Pyroclastic deposits of the Mount Edgecumbe volcanic field, southeast Alaska: eruptions of a stratified magma chamber. Journal of Volcanology and Geothermal Research 53, 117143.CrossRefGoogle Scholar
Riehle, J. R. Mann, D. H. Peteet, D. M. Engstrom, D. R. Brew, D. A., and Meyer, C. E. (1992). The Mount Edgecumbe tephra deposits, a marker horizon in southeastern Alaska near the PleistoceneHolocene boundary. Quaternary Research 37, 183202 CrossRefGoogle Scholar