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Thursday, July 30, 2020 | History

1 edition of Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985 found in the catalog.

Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985

Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985

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Published by Dept. of the Interior, U.S. Geological Survey, Books and Open-File Reports Section [distributor] in Sacramento, Calif, Denver, CO .
Written in English

    Subjects:
  • Geochemistry -- California -- Mono County -- Long Valley,
  • Hydrology -- California -- Mono County -- Long Valley

  • Edition Notes

    Statementby C.D. Farrar ... [et al.]
    SeriesWater-resources investigations report -- 87-4090
    ContributionsFarrar, C. D., Geological Survey (U.S.)
    The Physical Object
    Paginationvi, 71 p. :
    Number of Pages71
    ID Numbers
    Open LibraryOL14282224M

    The Owens Valley, a long, narrow valley along the east side of the Sierra Nevada in east-central California, is the main source of water for the city of Los Angeles. The city diverts most of the surface water in the valley into the Owens River-Los Angeles Aqueduct system, which transports the water more than miles south to areas of.   Long Valley caldera, in east-central California, has been the site of research on both geothermal resources and volcanic hazard mitigation over the past 30 years (Fig. 1, Fig. 2).Recent reports describe the history and present state of volcanic unrest in this region (e.g. Miller, , Hill et al., ), and numerous papers describe the present-day hydrothermal system and its utilization for Cited by:

      The Inyo Craters (North Inyo Crater and South Inyo Crater), and a third crater, Summit Crater, are the largest of more than a dozen to yr-B.p. phreatic craters that lie in a 1-km-square area at the south end of the Inyo Volcanic Chain, on the west side of the Long Valley Caldera in eastern California. The three craters are aligned within a 1-km-long northsouth system of fissures and Cited by: Geothermal systems of the Mono Basin-Long Valley region, eastern California and western Nevada: California Division of Mines and Geology, Open-File Report SAC, p. Hill, M.C., a, Preconditioned conjugate-gradient 2 (PCG2), a computer program for solving ground-water flow equations: U.S. Geological Survey Water-Resources.

    Volcanism, structure, and geochronology of Long Valley Caldera, Mono County, California: Authors: Bailey, Roy A.; Dalrymple, G. Brent; Lanphere, Marvin A. Abstract Long Valley caldera, a by km elliptical depression on the east front of the Sierra Nevada, formed . Geologic units in Mono county, California. Additional scientific data in this geographic area. Mesozoic granitic rocks, unit 3 (Sierra Nevada, (Long Valley Caldera) (Quaternary ( Ma)) at surface, covers 10 % of this area. Quaternary pyroclastic and volcanic mudflow deposits.


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The Cambridge English Course 2 Split Edition Students book A

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Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985 Download PDF EPUB FB2

This report presents hydrologic and caldera, Mono County, California, collect during The data presented herein Geological Survey's program of monitoring to detect changes caused by magmatic processes.

The study began inand described in Farrar and others () and geochemical data for Cited by: Get this from a library. Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, [C D Farrar; Geological Survey (U.S.);]. HYDROLOGIC AND GEOCHEMICAL MONITORING IN LONG VALLEY CALDERA, MONO COUNTY, CALIFORNIA, By C.D.

Farrar, M.L. Sorey, S.A. Rojstaczer, A.C. Steinemann, and M.D. Clark ABSTRACT The U.S. Geological Survey continued to monitor hydrologic and geochemical conditions in the Long Valley caldera during The monitoring is directedCited by: The Long Hydrologic and geochemical monitoring in Long Valley Caldera caldera is a potentially active volcanic area on the eastern side of the Sierra Nevada in east-central California.

Hydrologic and geochemical monitoring of surface and subsurface features began in July to determine if changes were occurring in response to processes causing earthquakes and crustal deformation. Differences since in fluid chemistry of springs has been.

The U.S. Geological Survey continued to monitor hydrologic and geochemical conditions in the Long Valley caldera during The monitoring is directed toward detecting changes in the hydrologic system caused by tectonic or magmatic processes.

Data collected during include chemical and isotopic composition of water from selected streams sites, springs, and wells; pumpage from four. Long Valley Caldera is a depression in eastern California that is adjacent to Mammoth valley is one of the Earth's largest calderas, measuring about 20 miles (32 km) long (east-west), 11 miles (18 km) wide (north-south), and up to 3, feet ( m) deep.

Long Valley was formedyears ago when a very large eruption released very hot ash that later cooled to form the Bishop Location: Mono County, California, United States. The Long Valley Hydrologic Advisory Committee (LVHAC), formed inreviews hydrological data and makes non-binding suggestions for monitoring and project conditions meant to protect the thermal and non-thermal hydrologic resources of the Long Valley Caldera.

Long Valley Caldera hosts a large hydrothermal system, with hot groundwater, boiling springs, and hydrothermal system is recharged with water primarily from snow-melt in the Sierra Nevada highlands along the western rim of the water infiltrates to depths of a few kilometers where it is heated to at least °C ( °F) by hot rock near geologically young.

Long Valley caldera and the Mono–Inyo volcanic chain of eastern California (Fig. 1, Fig. 2, Fig. 3) form one of several geologically youthful volcanic systems in gh these areas pose potential hazards to population centers from future volcanic eruptions (Miller, ), they also provide an abundance of recreational opportunities, spectacular scenery, natural thermal phenomena Cited by: Gas monitoring can either be conducted close to the source in ground-based campaigns or from a distance using remote sensing.

Between and a large amount of CO 2 was detected near the edge of Long Valley Caldera at Mammoth Mountain; the event also coincided with an earthquake swarm. Hydrologic and topographic changes in Long Valley caldera, California, induced by geothermal development Proceedings from the 15th New Zealand Geothermal Workshop, p.

2 Howle, J.F. and Farrar, C.D. Hydrologic data for Long Valley caldera, Mono County, California, U.S. Geological Survey Open-File Report 96 File Size: 4MB. Geochemical modeling of the near-surface hydrothermal system beneath the southern moat of Long Valley Caldera, California Article in Fuel and Energy Abstracts 40(2) June with 24 Reads.

Stuart Rojstaczer. BoxStanford, CA [email protected] Education: Stanford University, Ph.D. Applied Earth Sciences, University of Illinois, M. The Mono Lake Visitor Center includes interpretive information about the area in addition to views.

References Bailey, R.A.,Geologic map of Long Valley caldera, Mono-Inyo Craters volcanic chain, and vicinity, Mono County, California. U.S. Geological Survey Miscellaneous Investigations Map I. Abers, G., The subsurface structure of Long Valley Caldera, Mono County, California; a preliminary synthesis of gravity, seismic, and drilling geochronology of Long Valley Caldera, Mono County, California.

Journal of Geophysical Research, 81(5): D.D. and Anonymous, A transient model of the geothermal system of the. Discover Hot Creek Geological Site in Mono County, California: This naturally heated mountainous creek has created a group of neon blue pools of potentially deadly boiling water.

Steady decrease in extension rate within the Long Valley caldera, eastern California, – American Geophysical Union, EOS abstracts, v. 66, no. 46, p. Lee, C.H.,Report on the physical and economic limits of the underground water resources of Owens Valley: Los Angeles Department of Water and Power, unpublished report, 23 p.

Long Valley caldera, a 17‐ by 32‐km elliptical depression on the east front of the Sierra Nevada, formed m.y.

ago during eruption of the Bishop tuff. Subsequent intracaldera volcanism included er Cited by: Ash darkened the skies above Clark Air Base (U.S. Air Force) in the Philippines for weeks after the eruption of Mount Pinatubo in June Although the eruption was the world's second largest in the 20th century, the base was blanketed with a layer of pumice and ash only about 10 to 15 cm (about 4 to 6 in) thick at a distance of 20 km ( mi) from Pinatubo.

eastern margin of the Sierra Nevada 30 km south of Mono Lake. The caldera formed from the collapse of the Long Valley magma chambers following the explosive eruption that produced the Bishop tuff m.y.

ago (Bailey et al., ). The basement rocks in the immediate area of Long Valley are Jurassic and. The Tri-Valley Groundwater Management District meets regularly to discuss groundwater issues in the communities of Benton, Hammil Valley and Chalfant. Members: Richard Moss.The U.S.

Geological Survey occupied the Long Valley gravity network six times from to We reoccupied this network twice, in the summer of (33 stations), and the summer of (Hydrologic Monitoring Summary Long Valley Caldera, California. (!): ORMAT internal report. Related Geothermal Exploration Activities Activities (1) Development Wells At Long Valley Caldera Geothermal Area (Associates, ) Areas (1) Long Valley Caldera Geothermal Area.