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:

Abstract:

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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