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after the largest events. Surprisingly, there were no fatalities in
California. Residents in Ridgecrest and neighboring unincorporated town Trona had moderate to severe property damage. Two structure fires, loss of power for up to 24 hours in some areas, and Trona was without water. Highway 178, one of the two ways in or out of Trona was blocked from rockslides and impassable shifted sections of asphalt. Ridgecrest had declared a state of emergency as a result. One fatality was reported in Nevada in the following days.
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in 1996 and 1998 when tremors of M5.3, M5.1, M5.2, and M5.0 occurred within a day of each other. These tremors were actually recorded along the eastern side of the Coso
Volcanic Field, 15 miles (24 km). September 30, 2009 to October 6, 2009 there have been 429 earthquakes ranging from 0.1 to 5.2. Some days have activity at about one tremor every minute. On October 2, 2009 there were three earthquakes, (5.2, 4.7, and a 4.9), all within one hour of each other.
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729:, LLC (Reno, Nevada) and sold in 2006. It currently produces 270 MW from four geothermal power plants. More than 100 wells have been drilled throughout the field, with production depths from 2,000 to 12,000 feet (610 to 3,700 m), and temperatures from 200 to 350 °C (392 to 662 °F). Coso began generating electricity in 1987. Improvements have resulted in more efficient use of the resource.
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sparked a surge of activity in the area in and around the Coso
Volcanic Field. The first large quake on July 4 registered M6.4 and the largest on July 5 registered M7.1. Within a week, more than 8000 (M1.0-4.5) smaller earthquakes had joined the swarm, though only 27 quakes larger than M4.5 occurred
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The Coso
Volcanic Field is one of the most seismically active regions in the United States, producing dozens of tremors in the M1 and M2 range each week. Tremors in the M3 range occur at a rate of 2–6 per month and M4 quakes occur two-three times each year. Recent activity in the M5 range happened
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to make knives, projectile points, and the like (Hughes 1998). The chief period of exploitation was between approximately 3000 and 1000 years ago, when people mined obsidian by constructing benches in hillsides and digging deep pits to access raw materials (Elston and Zeier 1984; Gilreath and
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flows over a surface of little relief. Then, during the ensuing period of approximately 1.5 million years, eruptive activity included chemically more evolved rocks erupted upon a faulted terrain of substantial relief. Following a 1.5-million-year hiatus with few eruptions, a
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assessment carried out in the 1970s defined a potential resource of 650 megawatts electric with a nominal life span of 30 years. Judged by the youthfulness of the rhyolite lavas and by a zone of low seismic velocity crust roughly beneath the rhyolite, a
407:, and West Cactus Peak. These different subsources were used to varying degrees in different time periods, but the Sugarloaf and West Sugarloaf were the most commonly exploited geochemical types (Eerkens and Rosenthal 2004; Ericson and Glascock 2004).
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content is essentially constant at 77 percent. Other major-element constituents are nearly invariant. However, trace-element contents vary and help define 7 age groups, each of unique chemical composition.
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Elston, Robert G. and
Charles D. Zeier. 1984. The Sugarloaf Obsidian Quarry. Report prepared for the Naval Weapons Center, China Lake, California, by Intermountain Research. NWC Administrative Publication
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Eerkens, Jelmer W. and
Jeffrey S. Rosenthal. 2004. Are Obsidian Subsources Meaningful Units of Analysis?: Temporal and Spatial Patterning of Subsources in the Coso Volcanic Field, Southeastern California.
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Gilreath, Amy J. and
William R. Hildebrandt. 1997. Prehistoric Use of the Coso Volcanic Field. Contributions of the University of California Archaeological Research Facility No. 56, Berkeley, California.
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and flows developed on Basin and Range terrain of essentially the same form as today's landscape. Many of the young basalt flows are inter-canyon, occupying parts of the present-day drainage system.
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A basaltic lava flow that is typical of the process that created the stepped terraces of Coso as it flowed across the landscape, producing a more or less flat surface eroding to a sheer front.
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at Coso preceded the onset of Basin and Range crustal extension there, as expressed by normal faulting. The earlier of the two principal periods of volcanism began with the emplacement of
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Garfinkel, Alan P. 2007. Archaeology and Rock Art of the
Eastern Sierra and Great Basin Frontier. Maturango Museum Publication Number 22. Maturango Press, Ridgecrest, California.
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Ericson, Jonathon E. and
Michael D. Glascock. 2004. Subsource Characterization: Obsidian Utilization of Subsources of the Coso Volcanic Field, Coso Junction, California, USA.
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1045:. Rock Art Research 26(2):179–197. The Journal of the Australian Rock Art Research Association (AURA) and of the International Federation of Rock Art Organizations (IFRAO).
772:. The Coso Volcanic Field shows examples of volcanic activity, probably last active 30,000 to 40,000 years ago, but ash emission and small cone building episodes may be
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area, often producing hundreds of tremors over periods as short as a few days. This brisk and robust seismic activity is common in volcanic areas, such as
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rhyolite. Thirty-eight rhyolite domes and flows form an elongate array atop a north-trending 8 by 20 kilometres (5.0 mi × 12.4 mi) horst of
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is exposed locally on most extrusions, and analyses of fresh glass indicate that all of the rhyolite is of the so-called high-silica variety;
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craters, and a few filled and overrode their craters to feed flows a kilometer or two long. The two oldest domes contain several percent
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Hughes, Richard E. 1988. The Coso
Volcanic Field Reexamined: Implications for Obsidian Sourcing and Hydration Dating Research.
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Bighorn Hunting, Resource Depression, and Rock Art in the Coso Range of Eastern California: A Computer Simulation Model
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Hildebrand 1997). Obsidian from the volcanic fields was traded all the way to the California coast in
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bedrock. Nearby uneroded constructional forms are exhibited by most domes. Many are nested within
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959:"Must Reads: Ridgecrest earthquake mystery: Why so little destruction from huge temblors?"
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898:"Electricity Data Browser - List of plants for geothermal, California, all sectors, Coso"
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recognize at least four different geochemical subsources: Sugarloaf, West Sugarloaf,
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Paradigm Shifts, Rock Art Studies, and the "Coso Sheep Cult" of Eastern California
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Myth, Ritual and Rock Art: Coso Decorated Animal-Humans and the Animal Master
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Garfinkel, Alan P., Donald R. Austin, David Earle, and Harold Williams. 2009.
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984:"How could a Ridgecrest earthquake kill someone 95 miles away in Nevada?"
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and locally within the rhyolite field. A multi-disciplinary program of
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from the Coso Volcanic Fields was heavily exploited by Native American
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The Navy 1 geothermal power plant of the Coso Geothermal Power Project
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Commercial power development began in the 1980s. Located within the
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body may be the source of thermal energy for the geothermal system.
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Garfinkel, Alan P., David A. Young, and Robert M. Yohe, II. 2010.
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931:. Geothermal Resources Council. September 2002. Archived from
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The Coso Volcanic Field is well known as a geothermal area.
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Geothermal field in Inyo County, California,United States
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725:, power plants at the Coso Geothermal were operated by
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are part of the Coso Field, created by the prehistoric
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are present along faults bounding the rhyolite-capped
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335:The Coso Volcanic Field is best known for its
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1052:. Journal of Archaeological Science 37:42–51.
1035:. North American Archaeologist 27(3):203–244
8:
743:July 4th and 5th, 2019 two large earthquakes
1707:Volcanic fields of the Great Basin section
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80:Learn how and when to remove this message
43:This article includes a list of general
1727:Geothermal power stations in California
817:
679:Related media on Commons
508:Coso Geothermal Power Project - Navy 1
1073:Recent Earthquakes for the Coso Range
892:
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7:
1702:Landforms of Inyo County, California
1697:Protected areas of the Mojave Desert
1078:USGS Coso Volcanic Field, California
862:
860:
858:
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823:
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719:Naval Air Weapons Station China Lake
291:Naval Air Weapons Station China Lake
553:Geothermal power station
1570:Imperial Solar Energy Center South
1343:Big Creek No. 1, 2, 2A, 3, 4 and 8
1267:Los Esteros Critical Energy Center
49:it lacks sufficient corresponding
25:
1575:Imperial Solar Energy Center West
1015:Journal of Archaeological Science
423:
100:
34:
1636:Solar Energy Generating Systems
1560:Desert Stateline Solar Facility
1262:Huntington Beach Energy Project
1247:Donald Von Raesfeld Power Plant
957:Lin, Rong-Gong (10 July 2019).
1555:Centinela Solar Energy Project
1535:California Flats Solar Project
1:
1722:Volcanic fields of California
1540:California Valley Solar Ranch
579:13,000 ft (4,000 m)
442:Coso Geothermal Power Project
418:Coso Geothermal Power Project
411:Coso Geothermal Power Project
270:, at the western edge of the
1626:Ivanpah Solar Power Facility
1621:Genesis Solar Energy Project
1172:Puente Hills Energy Recovery
590:7,874 ft (2,400 m)
124:7,874 ft (2,400 m)
1717:Monogenetic volcanic fields
1666:San Gorgonio Pass Wind Farm
1520:Antelope Valley Solar Ranch
1031:Garfinkel, Alan P. 2006.
776:(>10,000 years) in age.
645:Annual net output
399:and regions further east.
351:; the rest are essentially
277:and northern region of the
1743:
1580:McCoy Solar Energy Project
1565:Desert Sunlight Solar Farm
1530:Blythe Solar Power Project
1287:Russell City Energy Center
1252:Gateway Generating Station
241:Monogenetic volcanic field
1590:Panoche Valley Solar Farm
1545:Campo Verde Solar Project
684:
606:
602:
576:Max. well depth
434:
422:
393:Santa Barbara, California
325:of basalt lava flows and
99:
1676:Tehachapi Pass Wind Farm
1282:Moss Landing Power Plant
1193:Argus Cogeneration Plant
838:Global Volcanism Program
1671:Shiloh Wind Power Plant
1661:Altamont Pass Wind Farm
1656:Alta Wind Energy Center
1383:Mammoth Pool Powerhouse
922:"Geothermal California"
843:Smithsonian Institution
622:Nameplate capacity
268:Inyo County, California
64:more precise citations.
1712:Pleistocene lava domes
1550:Catalina Solar Project
1428:San Francisquito No. 1
1242:Alamitos Energy Center
1177:Sunshine Gas Producers
873:Coso Operating Company
796:Coso Rock Art District
723:Ridgecrest, California
669:Coso Operating Company
611:Units operational
548:Coso Operating Company
497:36.03333°N 117.81667°W
389:San Luis Obispo County
289:. They are within the
1443:White Rock Powerhouse
1272:Metcalf Energy Center
869:"Project Information"
833:"Coso Volcanic Field"
598:Power generation
395:, and throughout the
1631:Mojave Solar Project
1600:Springbok Solar Farm
1525:Beacon Solar Project
1393:New Bullards Bar Dam
1378:Loon Lake Powerhouse
635:Capacity factor
530:Commission date
502:36.03333; -117.81667
18:BLM Geothermal Plant
1491:William R. Gianelli
1388:Moccasin Powerhouse
1353:Caribou No. 1 and 2
1257:Glenarm Power Plant
766:Yellowstone Caldera
758:Long Valley Caldera
660:External links
584:Site elevation
492: /
264:Coso Volcanic Field
148: /
95:Coso Volcanic Field
1585:Mount Signal Solar
1368:Jaybird Powerhouse
806:Lists of volcanoes
752:are common in the
371:Prehistoric Period
114:Highest point
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1403:New Exchequer Dam
1398:New Don Pedro Dam
1348:Camino Powerhouse
1338:Belden Powerhouse
750:Earthquake swarms
695:
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534:Navy I: May 1987
293:and northeast of
275:geologic province
260:
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16:(Redirected from
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1605:Topaz Solar Farm
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1448:William E. Warne
1333:Balch Powerhouse
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727:Caithness Energy
688:edit on Wikidata
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1413:Oroville Dam
1358:Devil Canyon
1326:Conventional
1208:
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992:. Retrieved
987:
978:
966:. Retrieved
962:
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940:. Retrieved
933:the original
929:GRC Bulletin
928:
916:
905:. Retrieved
901:
876:. Retrieved
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846:. Retrieved
836:
801:Fossil Falls
748:
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696:
405:Joshua Ridge
374:
334:
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283:Fossil Falls
263:
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189:Parent range
76:
67:
48:
1438:Trinity Dam
1373:Keswick Dam
1214:The Geysers
1028:19:779–805.
902:www.eia.gov
770:Yellowstone
614:3 x 30.7 MW
562:Flash steam
545:Operator(s)
524:Operational
500: /
487:117°49′00″W
475:Coordinates
465:Inyo County
380:Coso People
349:phenocrysts
337:Pleistocene
295:Little Lake
287:Owens River
220:Age of rock
177:Inyo County
155: /
130:Coordinates
62:introducing
1691:Categories
1595:Solar Star
1486:Thermalito
1433:Shasta Dam
1418:Parker Dam
1363:Folsom Dam
1202:Geothermal
1118:California
1062:3:253–265.
907:2020-02-04
878:2020-02-04
848:2009-01-06
812:References
791:Coso Range
733:Seismicity
707:geothermal
616:6 x 30 MW
506: (
484:36°02′00″N
469:California
330:lava domes
256:39,000 yrs
245:Lava domes
229:Quaternary
195:Coso Range
45:references
1017:31:21–29.
867:cosogeo.
699:Fumaroles
385:San Diego
345:tuff ring
311:volcanism
168:Geography
120:Elevation
1457:Pumped-
1319:electric
1233:Natural
1154:Biomass
1127:storage
1125:Battery
988:LA Times
963:LA Times
780:See also
774:Holocene
457:Location
376:Obsidian
357:Obsidian
341:Mesozoic
327:rhyolite
225:Pliocene
202:Topo map
173:Location
143:117°49′W
1614:Thermal
1481:O'Neill
1466:Castaic
1459:storage
1317:Hydro-
1301:Nuclear
1224:Mammoth
994:10 July
968:10 July
675:Commons
665:Website
447:Country
353:aphyric
320:bimodal
305:Geology
214:Geology
140:36°02′N
58:improve
1292:Valley
942:18 May
764:, and
654:(2018)
649:1,175
639:53.7%
626:272.2
521:Status
315:basalt
281:. The
47:, but
1504:Solar
1471:Helms
936:(PDF)
925:(PDF)
760:near
712:magma
703:horst
686:[
568:Wells
1649:Wind
1209:Coso
1186:Coal
1156:(≥10
1129:(≥10
1021:313.
996:2019
970:2019
944:2014
754:Coso
558:Type
297:and
262:The
243:and
207:USGS
1235:gas
1116:in
768:at
741:On
651:GWh
571:139
361:SiO
227:to
1693::
1512:PV
1158:MW
1131:MW
986:.
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927:.
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887:^
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857:^
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820:^
628:MW
467:,
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1106:e
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690:]
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363:2
83:)
77:(
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68:(
54:.
20:)
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