Title: |
Hydrogeology of the Thermal Landslide |
Authors: |
James V. Vantine |
Geo Location: |
The Geysers, California |
Conference: |
Stanford Geothermal Workshop |
Year: |
1985 |
Session: |
The Geysers Thermal Area |
Language: |
English |
File Size: |
265KB |
View File: |
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The large Thermal Landslide overlies the initial area of geothermal development at The Geysers. The landslide is waterbearing while the underlying Franciscan formation bedrock units are essentially non-waterbearing except where affected by hydrothermal alteration. Perched ground water moving through the landslide is heated prior to discharge as spring flow.
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