Hot Springs of the Valley of Ten Thousand Smokes

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Previous articleNext article FreeThe Temperatures of Hot Springs and the Sources of Their Heat and Water Supply. IIHot Springs of the Valley of Ten Thousand SmokesE. G. ZiesE. G. Zies Search for more articles by this author PDFPDF PLUS Add to favoritesDownload CitationTrack CitationsPermissionsReprints Share onFacebookTwitterLinkedInRedditEmail SectionsMoreDetailsFiguresReferencesCited by The Journal of Geology Volume 32, Number 4May - Jun., 1924 Article DOIhttps://doi.org/10.1086/623097 Views: 28Total views on this site Citations: 13Citations are reported from Crossref PDF download Crossref reports the following articles citing this article:Fernando Tornos, Francisco Velasco, John M. Hanchar The Magmatic to Magmatic-Hydrothermal Evolution of the El Laco Deposit (Chile) and Its Implications for the Genesis of Magnetite-Apatite Deposits, Economic Geology 112, no.77 (Nov 2017): 1595–1628.https://doi.org/10.5382/econgeo.2017.4523Julie A. Bowles, Jeffrey S. Gee, Mike J. Jackson, Margaret S. Avery Geomagnetic paleointensity in historical pyroclastic density currents: Testing the effects of emplacement temperature and postemplacement alteration, Geochemistry, Geophysics, Geosystems 16, no.1010 (Oct 2015): 3607–3625.https://doi.org/10.1002/2015GC005910Mike Jackson, Julie A. Bowles Curie temperatures of titanomagnetite in ignimbrites: Effects of emplacement temperatures, cooling rates, exsolution, and cation ordering, Geochemistry, Geophysics, Geosystems 15, no.1111 (Nov 2014): 4343–4368.https://doi.org/10.1002/2014GC005527Noor Hogeweg, T.E.C. Keith, E.M. Colvard, S.E. Ingebritsen Ongoing hydrothermal heat loss from the 1912 ash-flow sheet, Valley of Ten Thousand Smokes, Alaska, Journal of Volcanology and Geothermal Research 143, no.44 (May 2005): 279–291.https://doi.org/10.1016/j.jvolgeores.2004.12.003Gordon N. Keating The role of water in cooling ignimbrites, Journal of Volcanology and Geothermal Research 142, no.1-21-2 (Apr 2005): 145–171.https://doi.org/10.1016/j.jvolgeores.2004.10.019Elizabeth Warner Holt 18O/16O evidence for an early, short-lived (∼10 yr), fumarolic event in the Topopah Spring Tuff near the proposed high-level nuclear waste repository within Yucca Mountain, Nevada, USA, Earth and Planetary Science Letters 201, no.3-43-4 (Aug 2002): 559–573.https://doi.org/10.1016/S0012-821X(02)00735-5Elizabeth Warner Holt, Hugh P. Taylor 18O/16O mapping and hydrogeology of a short-lived (≈10 years) fumarolic (>500°C) meteoric–hydrothermal event in the upper part of the 0.76 Ma Bishop Tuff outflow sheet, California, Journal of Volcanology and Geothermal Research 83, no.1-21-2 (Jul 1998): 115–139.https://doi.org/10.1016/S0377-0273(98)00014-6Carey Gazis, Hugh P. Taylor, Ken Hon, Andrei Tsvetkov Oxygen isotopic and geochemical evidence for a short-lived, high-temperature hydrothermal event in the Chegem caldera, Caucasus Mountains, Russia, Journal of Volcanology and Geothermal Research 73, no.3-43-4 (Oct 1996): 213–244.https://doi.org/10.1016/0377-0273(96)00023-6Lisa Shevenell, Fraser Goff Evolution of hydrothermal waters at Mount St. Helens, Washington, USA, Journal of Volcanology and Geothermal Research 69, no.1-21-2 (Dec 1995): 73–94.https://doi.org/10.1016/0377-0273(95)00021-6T.E.C. Keith, J.M. Thompson, R.A. Hutchinson, L.D. White Geochemistry of waters in the Valley of Ten Thousand Smokes region, Alaska, Journal of Volcanology and Geothermal Research 49, no.3-43-4 (Feb 1992): 209–231.https://doi.org/10.1016/0377-0273(92)90015-6Terry E.C. Keith Fossil and active fumaroles in the 1912 eruptive deposits, Valley of ten thousand smokes, Alaska, Journal of Volcanology and Geothermal Research 45, no.3-43-4 (Apr 1991): 227–254.https://doi.org/10.1016/0377-0273(91)90061-4J.B. Koenig Geothermal exploration in the Western United States, Geothermics 2 (Jan 1970): 1–13.https://doi.org/10.1016/0375-6505(70)90001-5P. L. Ward, T. Matumoto A summary of volcanic and seismic activity in Katmai National Monument, Alaska, Bulletin Volcanologique 31, no.11 (Dec 1967): 107–129.https://doi.org/10.1007/BF02597009