Subsurface Geology Of The Raft River Geothermal Area, Idaho

The Raft River Valley Occupies An Upper Cenozoic Structural Basin Filled With Nearly 1,600 M Of Fluvial Silt, Sand, And Gravel.

Data and Resources

Metadata Source

Additional Info

Field Value
Citation Date 1980-01-01T00:00:00

Harvest Information

Original ID 9D9E899034C44D14BF586F1A47C5C32F
Index Date 2014-06-17T13:15:21
Original Format ISO-USGIN
Original Version 1.2

Author

Name H. R. Covington
Organization AMAX Exploration, Inc.
Email sbivens@egi.utah.edu

Geographic Extent

North Bound 49.0011461
South Bound 41.9880051
East Bound -111.043495
West Bound -117.2413657