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Title: Geology and geothermal resources of the Rexburg Area, eastern Idaho

Abstract

A brief description of major Cenozoic geologic features of the Rexburg area and a discussion of their geothermal significance are presented. The study area, identified as having geothermal potential, is approximately circular, about 55 km across, and centered on the town of Rexburg. It is roughly coextensive with a complex of about eight calderas of Pliocene age, here named the Rexburg caldera complex. These calderas were the source of several major rhyolitic volcanic deposits present along the southeast margin of the eastern Snake River Plain. The geology of this area was previously mapped in reconnaissance (Prostka and Hackman, 1974) and much of it as remapped in detail in 1977 because of its recognized geothermal potential.

Authors:
;
Publication Date:
Research Org.:
Geological Survey, Denver, CO (USA)
OSTI Identifier:
6369347
Report Number(s):
USGS-OFR-78-1009
ON: DE83902374
Resource Type:
Technical Report
Country of Publication:
United States
Language:
English
Subject:
15 GEOTHERMAL ENERGY; IDAHO; GEOLOGY; GEOTHERMAL RESOURCES; CALDERAS; MAPPING; VOLCANIC REGIONS; FEDERAL REGION X; NORTH AMERICA; RESOURCES; USA; Geothermal Legacy; 150201* - Geology & Hydrology of Geothermal Systems- USA- (-1989); 150101 - Geothermal Energy- Resources & Availability- USA- (-1989)

Citation Formats

Prostka, H.J., and Embree, G.F. Geology and geothermal resources of the Rexburg Area, eastern Idaho. United States: N. p., 1978. Web. doi:10.2172/6369347.
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Prostka, H.J., & Embree, G.F. Geology and geothermal resources of the Rexburg Area, eastern Idaho. United States. doi:10.2172/6369347.
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Prostka, H.J., and Embree, G.F. Sun . "Geology and geothermal resources of the Rexburg Area, eastern Idaho". United States. doi:10.2172/6369347. https://www.osti.gov/servlets/purl/6369347.
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@article{osti_6369347,
title = {Geology and geothermal resources of the Rexburg Area, eastern Idaho},
author = {Prostka, H.J. and Embree, G.F.},
abstractNote = {A brief description of major Cenozoic geologic features of the Rexburg area and a discussion of their geothermal significance are presented. The study area, identified as having geothermal potential, is approximately circular, about 55 km across, and centered on the town of Rexburg. It is roughly coextensive with a complex of about eight calderas of Pliocene age, here named the Rexburg caldera complex. These calderas were the source of several major rhyolitic volcanic deposits present along the southeast margin of the eastern Snake River Plain. The geology of this area was previously mapped in reconnaissance (Prostka and Hackman, 1974) and much of it as remapped in detail in 1977 because of its recognized geothermal potential.},
doi = {10.2172/6369347},
journal = {},
number = ,
volume = ,
place = {United States},
year = {Sun Jan 01 00:00:00 EST 1978},
month = {Sun Jan 01 00:00:00 EST 1978}
}
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Technical Report:
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DOI:  10.2172/6369347
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