PRESENT STATE OF THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA.
By: Michael L. Sorey
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Abstract
Results of test drilling to depths of 2 km and data on the chemical and isotopic content of waters from hot springs and fumaroles permit a conceptual model of the present-day hydrothermal system in Long Valley caldera to be delineated. The model consists of two principal zones in which hot water flows laterally from west to east at depths less than 1 km within and around the resurgent dome. Maximum measured temperatures within these zones are near 170 degree C, but estimates from chemical geothermometers and extrapolation of a high temperature gradient measured in a recent drill hole indicate that a source reservoir at temperatures near 240 degree C may exist at greater depths in the Bishop Tuff beneath the west moat.
| Publication type | Conference Paper |
|---|---|
| Publication Subtype | Conference Paper |
| Title | PRESENT STATE OF THE HYDROTHERMAL SYSTEM IN LONG VALLEY CALDERA, CALIFORNIA. |
| ISBN | 0934412596 |
| Volume | 9 |
| Issue | pt 1 |
| Year Published | 1985 |
| Language | English |
| Publisher | Geothermal Resources Council |
| Publisher location | Davis, CA, USA |
| Larger Work Title | Transactions - Geothermal Resources Council |
| First page | 485 |
| Last page | 490 |
| Conference Title | 1985 International Symposium on Geothermal Energy. Geothermal Resources Council 1985 Annual Meeting. |
| Conference Location | Kailua-Kona, HI, USA |
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