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December 22, 2005Geology

Dissected hydrologic system at the Grand Canyon: Interaction between deeply derived fluids and plateau aquifer waters in modern springs and travertine

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Authors

LCLaura J. CrosseyUniversity of New MexicoTFTobias P. FischerUniversity of California, Santa BarbaraPPP. Jonathan PatchettUniversity of Arizona

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Crossey et al. (2005) studied this question.

synapsesocial.com/papers/69d8197d3eff0c9dfaae360chttps://doi.org/10.1130/g22057.1
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Also Consider

Synapse has enriched 3 closely related papers on similar clinical questions. Consider them for comparative context:

  1. 1Variability of karstic permeability between unconfined and confined aquifers, Grand Canyon region, Arizona2000 · 32 citations
  2. 2Carbon dioxide and helium emissions from a reservoir of magmatic gas beneath Mammoth Mountain, California1998 · 223 citations
  3. 3Ages of Travertine Deposits in Eastern Grand Canyon National Park, Arizona1990 · 27 citations