Geologic Studies In The Basin And Range Colorado Plateau Transition In Southeastern Nevada Southwestern Utah And Northwestern Arizona 1992
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U.S. Geological Survey Bulletin
Author | : Helaine W. Markewich |
Publisher | : |
Total Pages | : 414 |
Release | : 1994 |
Genre | : Geology |
ISBN | : |
Isotopic Ages and Stratigraphy of Cenozoic Rocks of the Marysvale Volcanic Field and Adjacent Areas, West-central Utah
Author | : Peter D. Rowley |
Publisher | : |
Total Pages | : 44 |
Release | : 1994 |
Genre | : Geology, Stratigraphic |
ISBN | : |
Paleoseismic Investigation and Long-term Slip History of the Hurricane Fault in Southwestern Utah
Author | : William R. Lund |
Publisher | : Utah Geological Survey |
Total Pages | : 87 |
Release | : 2007 |
Genre | : Science |
ISBN | : 1557917604 |
This 81 page report presents the results of a study of the Hurricane fault in Utah.
U.S. Geological Survey Bulletin
Author | : Ed DeWitt |
Publisher | : |
Total Pages | : 402 |
Release | : 1983 |
Genre | : Argon-argon dating |
ISBN | : |
New Publications of the Geological Survey
Author | : Geological Survey (U.S.) |
Publisher | : |
Total Pages | : 438 |
Release | : 1990 |
Genre | : Geology |
ISBN | : |
Geology of the Sulphurdale geothermal-resource area, Beaver and Millard Counties, Utah
Author | : P.D. Rowley |
Publisher | : Utah Geological Survey |
Total Pages | : 33 |
Release | : 2013-04-15 |
Genre | : |
ISBN | : |
This 27-page report analyzes new detailed (1:12,000 scale) geologic mapping of a 14 square mile area centered by the high-temperature (350°F) Sulphurdale heat source, which at the surface makes up a circular area about a mile in diameter that is likely caused by a magma body at depth. A former small steam-driven geothermal electric power plant in the circular area is being replaced by a larger plant (Enel Green Power North America) that will use binary technology. Five cross sections tied to and at the same scale as the map help interpret the likely extent of the geothermal resource. Sulfur derived from evaporites at depth was initially mined at a solfatara above the heat source; associated sulfuric acid seeped downward to remove the Kaibab Limestone and Toroweap Formation from the subsurface.