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The dynamic floor of Yellowstone Lake, Wyoming, USA : The last 14 k.y. of hydrothermal explosions, venting, doming, and faulting

Morgan, L. A. (author)
United States Geological Survey, Reston
Shanks, W. C.P. (author)
United States Geological Survey, Reston
Pierce, K. L. (author)
United States Geological Survey, Reston
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Iverson, N. (author)
New Mexico Bureau of Geology and Mineral Resources
Schiller, C. M. (author)
Montana State University
Brown, S. R. (author)
University of Nebraska - Lincoln
Zahajska, P. (author)
Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science
Cartier, R. (author)
Lund University,Lunds universitet,Kvartärgeologi,Geologiska institutionen,Naturvetenskapliga fakulteten,Quaternary Sciences,Department of Geology,Faculty of Science
Cash, R. W. (author)
University of Illinois at Urbana-Champaign
Best, J. L. (author)
University of Illinois at Urbana-Champaign
Whitlock, C. (author)
Montana State University
Fritz, S. (author)
University of Nebraska - Lincoln
Benzel, W. (author)
US Geological Survey, Denver
Lowers, H. (author)
US Geological Survey, Denver
Lovalvo, D. A. (author)
Licciardi, J. M. (author)
University of New Hampshire, Durham
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 (creator_code:org_t)
2023
2023
English 28 s.
In: Bulletin of the Geological Society of America. - 0016-7606. ; 135:3-4, s. 547-574
  • Journal article (peer-reviewed)
Abstract Subject headings
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  • Hydrothermal explosions are significant potential hazards in Yellowstone National Park, Wyoming, USA. The northern Yellowstone Lake area hosts the three largest hydrothermal explosion craters known on Earth empowered by the highest heat flow values in Yellowstone and active seismicity and deformation. Geological and geochemical studies of eighteen sublacustrine cores provide the first detailed synthesis of the age, sedimentary facies, and origin of multiple hydrothermal explosion deposits. New tephrochronology and radiocarbon results provide a four-dimensional view of recent geologic activity since recession at ca. 15–14.5 ka of the >1-km-thick Pinedale ice sheet. The sedimentary record in Yellowstone Lake contains multiple hydrothermal explosion deposits ranging in age from ca. 13 ka to ~1860 CE. Hydrothermal explosions require a sudden drop in pressure resulting in rapid expansion of high-temperature fluids causing fragmentation, ejection, and crater formation; explosions may be initiated by seismicity, faulting, deformation, or rapid lake-level changes. Fallout and transport of ejecta produces distinct facies of subaqueous hydrothermal explosion deposits. Yellowstone hydrothermal systems are characterized by alkaline-Cl and/or vapor-dominated fluids that, respectively, produce alteration dominated by silica-smectite-chlorite or by kaolinite. Alkaline-Cl liquids flash to steam during hydrothermal explosions, producing much more energetic events than simple vapor expansion in vapor-dominated systems. Two enormous explosion events in Yellowstone Lake were triggered quite differently: Elliott’s Crater explosion resulted from a major seismic event (8 ka) that ruptured an impervious hydrothermal dome, whereas the Mary Bay explosion (13 ka) was triggered by a sudden drop in lake level stimulated by a seismic event, tsunami, and outlet channel erosion.

Subject headings

NATURVETENSKAP  -- Geovetenskap och miljövetenskap -- Geokemi (hsv//swe)
NATURAL SCIENCES  -- Earth and Related Environmental Sciences -- Geochemistry (hsv//eng)

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