<?xml version='1.0' encoding='utf-8'?>
<oai_dc:dc xmlns:dc="http://purl.org/dc/elements/1.1/" xmlns:oai_dc="http://www.openarchives.org/OAI/2.0/oai_dc/" xmlns:xsi="http://www.w3.org/2001/XMLSchema-instance" xsi:schemaLocation="http://www.openarchives.org/OAI/2.0/oai_dc/ http://www.openarchives.org/OAI/2.0/oai_dc.xsd">
  <dc:creator>E. G. Crosthwaite (compiler)</dc:creator>
  <dc:date>1976</dc:date>
  <dc:description>&lt;p&gt;Studies of the geothermal aspect-of the Bridge area of 
the Raft River basin in south-central Idaho (fig. 1) by the 
U.S. Geological Survey began in 1972 when Young and Mitchell 
(1973) made a geochemical and geologic reconnaissance of 
selected thermal waters in Idaho. The Bridge area had been 
designated the Frazier known geothermal resource area 
(Frazier KGRA) by the U.S. Geological Survey (Godwin and 
others-, 1971) . Since 1972, several units of the Geological 
Survey have studied the area to provide data for the U.S. 
Energy Research and Development Administration, which proposes to ascertain whether the geothermal resource can be 
developed for power generation and other uses. The studies 
include geologic mapping, geophysical surveys, water sampling, test drilling, and studies of all available drill- 
hole data. A list of reports already prepared on the area 
is included with this report.&lt;/p&gt;
&lt;br/&gt;
&lt;p&gt;Core drilling of five holes began in August 1974 and 
was completed in March 1975. These holes are referred to as 
intermediate-depth core holes, principally because in the 
spring of 1974, 35 auger holes 25 to 98 feet (7.6 to 30
meters) were completed in the area (Crosthwaite, 1974), and 
the Aerojet Nuclear Company, under the auspices of the U.S. 
Energy Research and Development Administration, was planning 
some deep drilling 4,000 to 6,000 feet (1,200 to 1,800 
meters) (fig. 1). The purpose of the core drilling was to 
provide information to test geophysical interpretations of 
the subsurface structure and lithology and to provide hydrologic and geologic data on the shallow part of the geothermal 
system. Samples of the core were made available to several 
divisions and branches of the Geological Survey and to 
people and agencies outside the Survey. This report presents the basic data from the core holes that had been 
collected to September 1, 1975, and includes lithologic and 
geophysical well logs, chemical analyses of water (table 1), 
and laboratory analyses of cores (table 2) that were completed as of the above date. The data were collected by the 
Idaho District office, Hydrologic Laboratory, Borehole 
Geophysics Research Project, and Drilling, Sampling, and 
Testing Section, all of the Water Resources Division, and 
the Branch of Central Environmental Geology of the Geologic 
Divison.&lt;/p&gt;</dc:description>
  <dc:format>application/pdf</dc:format>
  <dc:identifier>10.3133/ofr76665</dc:identifier>
  <dc:language>en</dc:language>
  <dc:publisher>U.S. Geological Survey</dc:publisher>
  <dc:title>Basic data from five core holes in the Raft River geothermal area, Cassia County, Idaho</dc:title>
  <dc:type>reports</dc:type>
</oai_dc:dc>