Origins of water and solutes in and north of the Norris-Mammoth Corridor, Yellowstone National Park

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This study was initiated to investigate the impacts of geothermal development in the Corwin Springs Known Geothermal Resources Area (KGRA) on the hydrothermal features of Yellowstone National Park. To determine possible hydrogeochemical connections, we used the diagnostic stable and radioactive isotopes of several elements, and the chemical and gas compositions of thermal and cold waters from the Norris-Mammoth Corridor and areas north of the Park. The investigations were particularly comprehensive in the Mammoth Hot Springs area, Corwin Springs KGRA, and Chico Hot Springs. The geochemical tools used are still subject to uncertainties of 1 - 5%. Preliminary interpretation of the data, especially the ??D and ??18O values of water, 87Sr/86Sr ratios, ??11B values, composition and isotopes of noble gases and several conservative chemical species would indicate that the waters from Mammoth Hot Springs and La Duke Spring area have evolved chemically and isotopically by reactions with different rock types, and are probably not directly connected. These data indicate that a component (<20%) of water in Bear Creek Springs may be derived from the Mammoth system.

Additional publication details

Publication type Conference Paper
Publication Subtype Conference Paper
Title Origins of water and solutes in and north of the Norris-Mammoth Corridor, Yellowstone National Park
ISBN 0934412677
Volume 14
Issue pt 1
Year Published 1990
Language English
Publisher Publ by Geothermal Resources Council
Publisher location Davis, CA, United States
Larger Work Title Transactions - Geothermal Resources Council
First page 705
Last page 714
Conference Title 1990 International Symposium on Geothermal Energy
Conference Location Kailua-Kona, HI, USA
Conference Date 20 August 1990 through 24 August 1990
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