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Publisher

National Cave and Karst Research Institute

Publication Date

November 2013

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Lee J. Florea Department of Geological Sciences, Ball State University 2000 W. University Ave. Muncie, IN 47306, USA lflorea@bsu.edu Camille McKinney Timpanogos Cave National Monument R.R. 3 Box 200 American Fork, Utah 84003, USA Cami_McKinney@nps.gov Chelsie R. Dugan Department of Geological Sciences, Ball State University 2000 W. University Ave. Muncie, IN 47306, USA crduganlawre@bsu.edu AbstractThis manuscript considers the hydrology and geochemistry of water resources within Timpanogos Cave National Monument in American Fork, Utah. In particular, data are presented for five cave pools within the Monument and the American Fork River that flows through the Monument. Two independent dye trace attempts in this study have not established a connection between the surface near the canyon rim at the south border of the Monument and the cave pools or the river. Ion chemistry of the pools reveals elevated sulfate concentrations. Analysis of sulfate and other reaction products suggests the possibility of combined carbonic and sulfuric acids as speleogenetic agents. Enrichment of 13C in dissolved inorganic carbon above expected values provides initial support of this hypothesis. The enrichment of sulfate in the cave pools when coupled with higher concentrations of fluorine, suggest increased interaction with bedrock influenced in the past by hydrothermal activity. This is especially relevant in pools with muted water-level fluctuations during the course of the study. Other pools have greater water-level variation and unexpectedly have a very consistent chemical composition. One hypothesis is that the source waters for the pools with stable geochemical character are from the talus near the canyon rim. Evidence from the stable isotopes of oxygen and hydrogen within water samples support this hypothesis- cave pools with constant water levels are more enriched in heavier isotopes and thus derived from lower elevations compared to cave pools with variable water level and depletion in the heavier isotopes. Open Access - Permission by Publisher See Extended description for more information.

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Article

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serial

Identifier

K26-03266

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