Evolution and present state of the hydrothermal system in Long Valley Caldera
Journal Article
·
· J. Geophys. Res.; (United States)
OSTI ID:6480192
Evidnece for previous periods of hydrothermal activity in Long Valley Caldera exists in the form of extensive deposits of hydrothermal alteration products at several locations within the caldera and saline deposits in Searles Lake which contain mineral assemblages contributed by hot spring discharge from Long Valley. Hydrothermal activity was more intense in the past and probably involved fluid circulation to depths of several kilometers or more with heat supplied by the Long Valley magma chamber. During the past 40,000 years the heat source may have shifted to the Inyo-Mono magmatic system beneath the west moat, where deep fluid circulation supplied hot water to shallower zones of lateral flow within the Bishop Tuff beneath the resurgent dome. The present-day hydrothermal system in Long Valley appears to consist of two principal zones in which hot water flows laterally from west to east at depths of less than 1 km within and around the resurgent dome. Maximum measured temperatures within these zones are near 170/sup 0/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/sup 0/ may exist at greater depths within the Bishop Tuff beneath the west moat. Regions possibly containing silicic melt detected by shear wave attenuation of depths of 4--5 km beneath the resurgent dome have probably not been in place long enough to influence sensibly the overlying thermal regime within the upper 2 km of caldera fill.
- Research Organization:
- U.S. Geological Survey, Menlo Park, California
- OSTI ID:
- 6480192
- Journal Information:
- J. Geophys. Res.; (United States), Journal Name: J. Geophys. Res.; (United States) Vol. 90:B13; ISSN JGREA
- Country of Publication:
- United States
- Language:
- English
Similar Records
Preliminary Hot Dry Rock geothermal evaluation of Long Valley Caldera, California
Implications of a magnetic model of the Long Valley Caldera, California
Structure and stratigraphy beneath a young phreatic vent: South Inyo Crater, Long Valley caldera, California
Technical Report
·
Sat Feb 28 23:00:00 EST 1981
·
OSTI ID:6564207
Implications of a magnetic model of the Long Valley Caldera, California
Journal Article
·
Sun Jul 10 00:00:00 EDT 1977
· J. Geophys. Res.; (United States)
·
OSTI ID:7101363
Structure and stratigraphy beneath a young phreatic vent: South Inyo Crater, Long Valley caldera, California
Journal Article
·
Wed Nov 09 23:00:00 EST 1988
· J. Geophys. Res.; (United States)
·
OSTI ID:6392555
Related Subjects
15 GEOTHERMAL ENERGY
150201* -- Geology & Hydrology of Geothermal Systems-- USA-- (-1989)
CALDERAS
CALIFORNIA
CHEMISTRY
ENERGY SYSTEMS
FEDERAL REGION IX
GEOCHEMISTRY
GEOPHYSICAL SURVEYS
GEOTHERMAL SYSTEMS
HYDROTHERMAL ALTERATION
HYDROTHERMAL SYSTEMS
LONG VALLEY
MAGMA SYSTEMS
MINERALS
NORTH AMERICA
SEISMIC SURVEYS
SURVEYS
TEMPERATURE MEASUREMENT
USA
150201* -- Geology & Hydrology of Geothermal Systems-- USA-- (-1989)
CALDERAS
CALIFORNIA
CHEMISTRY
ENERGY SYSTEMS
FEDERAL REGION IX
GEOCHEMISTRY
GEOPHYSICAL SURVEYS
GEOTHERMAL SYSTEMS
HYDROTHERMAL ALTERATION
HYDROTHERMAL SYSTEMS
LONG VALLEY
MAGMA SYSTEMS
MINERALS
NORTH AMERICA
SEISMIC SURVEYS
SURVEYS
TEMPERATURE MEASUREMENT
USA