HYDROGEOLOGY OF THE THERMAL LANDSLIDE
Conference
·
OSTI ID:892168
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.
- Research Organization:
- Stanford University, Stanford, California
- Sponsoring Organization:
- USDOE
- DOE Contract Number:
- AS03-80SF11459
- OSTI ID:
- 892168
- Report Number(s):
- SGP-TR-84; CONF-850107-24; TRN: US200622%%753
- Resource Relation:
- Conference: 10. annual workshop on geothermal reservoir engineering, Stanford, CA (US), 01/22/1985
- Country of Publication:
- United States
- Language:
- English
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·
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·
OSTI ID:892168