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Welded rhyolitic tuffs in southeastern Idaho

G. R. Mansfield·C.S. Ross
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Abstract

Rocks of rhyolitic type in eastern Idaho and adjacent parts of Wyoming were observed by the Teton Division of the Hayden Surveys under Orestes St. John (Report of the geological field work of the Teton Division, U.S. Geol. and Geog. Surv. Terr., 11th Ann. Rep., pp. 498–504, 1879), who described them as trachytes. He noted their relations to different types of underlying sedimentary rocks and their tendency to conform with the preexisting topography, but considered them all as flows. ©1935. American Geophysical Union. All Rights Reserved.

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Eos, Transactions, American Geophysical UnionArticle
90° N90° S · 180° W ← longitude → 180° E
Source-reported bounding extent: 41.988057° to 49.000912° latitude; -117.243027° to -111.044156° longitude. This indicates report coverage, not an exact sampling location. View area on OpenStreetMap.

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G. R. Mansfield, C.S. Ross. 2014-08-18. Welded rhyolitic tuffs in southeastern Idaho. https://doi.org/10.1029/tr016i001p00308

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