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ReportsHydrogen Isotopes in Eocene River Gravels and Paleoelevation of the Sierra Nevada
We determine paleoelevation of the Sierra Nevada, California, by tracking the effect of topography on precipitation, as recorded in hydrogen isotopes of kaolinite exposed in gold-bearing river deposits from the Eocene Yuba River. The data, compared with the modern isotopic composition of precipitation, show that about 40 to 50 million years ago the Sierra Nevada stood tall ( Geological and Environmental Sciences, Stanford University, 450 Serra Mall, Building 320, Stanford, CA 94305, USA. * To whom correspondence should be addressed. E-mail: mulch{at}pangea.stanford.edu
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Science. ISSN 0036-8075 (print), 1095-9203 (online)