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Tuesday, October 13, 2020 | History

2 edition of Geologic and geophysical investigation of the Beowawe geothermal area, North-Central Nevada. found in the catalog.

Geologic and geophysical investigation of the Beowawe geothermal area, North-Central Nevada.

Mary Lou C. Zoback

Geologic and geophysical investigation of the Beowawe geothermal area, North-Central Nevada.

by Mary Lou C. Zoback

  • 135 Want to read
  • 9 Currently reading

Published by Stanford University, School of Earth Sciences in Stanford, Calif .
Written in English


Edition Notes

2 col. fold. maps in end pocket.

SeriesPublications : geological sciences -- 16.
ID Numbers
Open LibraryOL19740155M

A sequence of lava flows in the Sheep Creek Range (Nevada) provide a record of transitional field behavior, likely during a polarity reversal at Ma Two transitional directions recurred during this event as well as during two other Miocene reversals recorded at localities in Oregon and California. Full text of "A Geologic Reconnaissance in Southwestern Nevada and Eastern California" See other formats.

EPA/ May PROCEEDINGS OF THE FIRST WORKSHOP ON SAMPLING GEOTHERMAL EFFLUENTS October , Las Vegas, Nevada conducted by Monitoring Systems Design and Analysis Staff Monitoring Systems Research 6 Development Division Environmental Monitoring and Support Laboratory Las Vegas, Nevada U.S. Environmental Protection Agency Region . Full text of "Geologic Investigations in the Basin and Range of Nevada Using Skylab/EREP Data" See other formats.

Commission file number NEVADA GEOTHERMAL POWER INC. (Exact name of Registrant as specified in its charter) Not Applicable (Translation of Registrant's name into English. The HC/CUEP area principally lies along the east side of the Cortez Mountains in Eureka and Lander counties, Nevada. A small portion of the HC/CUEP area extends to the western flank of the Cortez Mountains. Current exploration activities within the HC/CUEP Plan of Operations (Plan) boundary have been centralized in the Horse Canyon area.


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Geologic and geophysical investigation of the Beowawe geothermal area, North-Central Nevada by Mary Lou C. Zoback Download PDF EPUB FB2

Geolologic [i.e. Geologic] and geophysical investigation of the Beowawe geothermal area, north-central Nevada. Stanford, Calif.: Stanford University, School of Earth Sciences, (OCoLC) The purpose of this paper is to describe the geology and geophysics of a part of the eastern northern Nevada rift (synonymous with the northern Nevada rift of Zoback, ; Zoback et al., ) that encompasses the Beowawe geothermal system in north-central Nevada and the assumptions, extrapolations, and geophysical modeling conducted to generate a 3D geologic by: 8.

A three-dimensional (3D) geologic model of part of the northern Nevada rift encompassing the Beowawe geothermal system was developed from a series of two-dimensional (2D) geologic and geophysical. The Beowawe geothermal system, also kno\'In as The Geysers, Hes 30km ( mf) southeast of Battle Mountafn.

astride the Lander-Eureka county Hne fnthe:Whirlwind Valley of north-central Nevada (Figure 1). Beowawe ranks among the hottest of the numerous known geothermal systems in the Great Basin.(Gars i de ana i ng, File Size: 5MB.

The Beowawe Geysers in north-central Nevada are the discharge from a hydrothermal-convection system in a region of high heat flow. The site of thermal-fluid upflow (at about 18 kg/s before drilling and well testing) appears to be related to the intersection at depth of two major fault zones.

Assuming steady-state conditions, recharge within the drainage basin could account for both thermal and. The Beowawe Geysers, Nevada, Before Geothermal Developmerlt By Donald E.

White ABSTRACT The history of natural activity of the Beowawe Geysers in north-central Nevada is documented before geothermal drill­ ing and production, which started in Previously, the Beowawe Geysers area was second only to Yellowstone Na­File Size: 5MB.

Geophysical studies in northern Nevada have resulted in several models for the origin and significance of a series of prominent geophysical features known as the northern Nevada rifts (NNRe, NNRc, NNRw, Fig.

1) (Glen and Ponce, ; Ponce and Glen, ).The originally named northern Nevada rift (Zoback and Thompson, ; Zoback et al., ), expressed by a prominent aeromagnetic anomaly Cited by: 8.

Progress report}, author = {Trexler, D.T.}, abstractNote = {To evaluate lineament analysis as a technique for geothermal exploration an area of known geothermal activity and high regional heat flow was selected as a test area. An area of north-central Nevada coincident with the Winnemucca AMS sheet and encompassing four Known Geothermal.

conducted at the Hot Pot geothermal prospect area in north-central Nevada under the USDOE (United States Department of Energy) Geothermal Technologies Program. The project objective was to utilize innovative seismic data processing, integrated with existing geological, geophysical andAuthor: Michael Lane, Richard Schweickert.

Abstract. The Pearl Host Spring Geothermal Project funded by the DoE Geothermal Program was a joint academic (KU/UT & OU) and industry collaboration (Sierra and Ram Power) to investigate structural controls and the importance of low-angle normal faults on geothermal fluid flow through a multifaceted geological, geophysical, and geochemical investigation in west-central : Daniel F.

Stockli. GEOLOGY, AND GEOTHERMAL RESEARCH Of THE JEMEZ MOUNTAINS AND VICINITY, NORTH-CENTRAL NEW MEXICO By Cynthia G. Abeyta and Bruce M. Delaney U.S. GEOLOGICAL SURVEY Open-File Report Prepared in cooperation with the U.S. BUREAU OF INDIAN AFFAIRS and the NEW MEXICO STATE ENGINEER OFFICE Albuquerque, New Mexico Author: Cynthia G.

Abeyta, Bruce M. Delaney. The Beowawe geothermal field is located on the boundary of Eureka and Lander counties in north-central Nevada.

The reservoir is located within the Malpais Fault Zone (MFZ) on the southeast margin of Whirlwind Valley (Figure 1). A dual-flash geothermal power plant with a capacity of MW (gross) has operated at Beowawe since December File Size: KB.

Edquist, R.K.,Geophysical Investigation of the Baltazor Hot Springs Known Geothermal Resource Area and the Painted Hills Thermal Area, Humboldt County, Nevada: Utah University, Salt Lake City, Earth Science Lab, ESL, p.

GPS baseline across the Crescent fault in north central Nevada, a typical Basin and Range normal fault, indicating horizontal shortening oriented normal to the trace of the fault of 2 mm/yr [Wernicke et al., ]. Given the typical long-term displacement rates across Basin and Range nor-mal faults of – mm/yr [e.g., Thompson and Burke.

Nevada Geology and Mining History Catalog I - Federal Publications. Home Page: Sale: D. / THE BEOWAWE GEYSERS, NEVADA, BEFORE GEOTHERMAL DEVELOPMENT, pb, 25 pages, 23 figs., 3 tables, $ 8 I / GEOLOGIC MAP OF THE MOUNT ICHABOD AREA, NEVADA, $ 10 I / GEOLOGIC MAP OF THE ROWLAND-BEARPAW MOUNTAIN AREA, NEVADA, $ Structural inferences from geologic and geophysical data at the Beowawe KGRA, North-central Nevada.

Geothermal Resources Council Transactions, 3, - Smith, C. Nevada Map Geologic map and sections of the southern Cherry Creek and northern Egan Ranges, White Pine county, Nevada. By William H. Fritz. The map sheet has a color map and sections and lots of explanatory text.

$5. Nevada Map Geologic map of north-central Nevada. By John H. Stewart and John E. Carlson. New Zealand Geothermal Workshop Proceedings 19 - 21 November Auckland, New Zealand STRUCTURAL AND TECTONIC CONTROLS OF GEOTHERMAL ACTIVITY IN THE BASIN AND RANGE PROVINCE, WESTERN USA James E. Faulds1, Nicholas Hinz1, and Corné Kreemer1 1 Nevada Bureau of Mines and Geology, University of Nevada, Reno, Nevada USA.

GEOTHERMAL BIBLIOGRAPHY OF UTAH — Baker, C.H., Jr.,Water resources of the Heber‐Kamas‐Park City area, north central Utah: Utah Murphy, P.J., and Gwynn, J.W.,Geothermal investigation of the Warm Springs fault geothermal system, Salt Lake County, Utah: Utah Geological and Mineral Survey Report of Investigation File Size: KB.

Geothermal sites at Lake Bogoria. Geothermal activity at Lake Bogoria has been linked to N–S trending dyke injections at 3–6 km depth near Arus (Mulwa and Mariita, ).

Renaut () mapped ∼ hot-spring vents at Lake Bogoria in About 60 hot and boiling (98 °C) springs discharge from pools at Loburu delta-plain on the Cited by:. References. Adams, M. C., Moore, J. N., and Forster, C., Fluid flow in volcanic terrains—hydrogeochemisty of the Meager Mountain thermal system.Holes were drilled to a depth of 40 ft and logged using both geologic examination and down-hole geophysical surveying.

The data identify a large complex of very coarse-grained sediment (clasts up to 8 mm) with interbedded finer-grained sands, silts and clays, underlying a fairly uniform layer of silty clay 6 .EPA/ June PROCEED I NGS OF THE SECOND WORKSHOP ON SAMPLING GEOTHERMAL EFFLUENTS FebruaryLas Vegas, Nevada Sponsored by Environmental Monitoring and Support Laboratory Las Vegas, Nevada Industrial Environmental Research Laboratory Cincinnati, Ohio Office of Energy, Minerals and Industry Washington, D.C.

of the U.S. Environmental .