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Lost Hills Oil Field

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flooding. The early peak in production took place in 1917, during which 4 million barrels (640,000 m) of oil were pumped; then production steadily declined, with a few spikes, until the enhanced recovery techniques which began to be employed in the 1960s began to pay off. In 1981 the field produced almost 6 million barrels (950,000 m), and has remained a high producer, reaching close to 12 million barrels (1,900,000 m) in 2006. During that year it had the fourth-largest production increase in the state, and preliminary estimates for 2007 show that production has increased yet again, to 12.2 million barrels (1,940,000 m)
261:, began drilling for more nearby; they soon found the Cahn and Reef Ridge pools, in 1913, and then the Tulare pool in 1915. There were relatively few wells on the field for the first several decades; indeed, by 1979, there were only 39 wells producing from the Monterey Formation, and each of these wells only produced an average of eight barrels per day. It took the development of advanced recovery technology to turn the Lost Hills into a high-producing oil field. 219:
recoverable from the unit (only three to four percent so far). According to Chevron's estimate, there are approximately 2.2 billion barrels (350,000,000 m) of oil in place in the Lost Hills Field, only five percent of which has been extracted. The oil in place is about twenty times greater than the California Department of Oil and Gas reserves estimate (109 million barrels (17,300,000 m)), which is volume that can be economically produced.
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per year. The dropping land surface causes operational problems, including fractures of well casings, and sometimes complete well failures. Waterflooding – the practice of filling the reservoir with water to push petroleum to recovery wells, and thereby also reoccupying the space vacated by oil and gas – has partially mitigated the problem. Some wells have actually disappeared into craters: in 1976, a
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immediately exploding into flame, knocking over the massive drilling rig, destroying the trailer, and melting the nearby drilling equipment. This enormous pillar of fire, which rose to 340 feet (100 m) into the sky, could be seen more than 40 miles (64 km) away, and the quantity of oil release was estimated at 2,000
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Drillers Martin and Dudley accidentally discovered the Lost Hills Oil Field in July 1910. They were drilling a water well for livestock grazing; instead of finding groundwater, however, they struck oil, specifically the Etchegoin Pool at a depth of 530 feet (160 m). Other drillers, encouraged by
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The climate in the Lost Hills area is arid to semi-arid, with an average rainfall of 5 to 6 inches (130 to 150 mm) a year, almost all in the winter months. Vegetation in the vicinity of the field is mostly grassland and sparse scrub, with some adjacent orchards, although in the oil field itself
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being drilled into a promising anticlinal fold underneath the Monterey Formation, northeast of the main Lost Hills field, reached the depth of 17,000 feet (5,200 m) and hit a previously untapped reservoir of gas under intense pressure. Natural gas and petroleum condensate burst from the well,
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of the ground surface as it collapses into the area vacated by the petroleum after being pumped out. Portions of the hills overlying the oil field have subsided up to 8 feet (2.4 m) in the central region of operations, and subsidence occurs field-wide at a rate of about 9 inches (230 mm)
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Unusual for a California oil field, the years of maximum recovery were not early in the 20th century, but recently: peak oil production from the Etchegoin Pool did not occur until the early 21st century, assisted by several enhanced recovery technologies, including water flooding and cyclic steam
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The Belridge Diatomite portion of the Monterey Formation defines the productive limits of the field. Characteristic of this rock unit is that it is full of oil – almost 50% of the unit is saturated, and the unit has high porosity, in the 45% to 70% range – but very little of the oil has been
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In 1998, the Lost Hills Field was the site of one of the largest and most spectacular well blowouts in modern U.S. history. The Bellevue blowout – also called the "Bellevue gusher" – involved six months of uncontrolled natural gas expulsion, and a gigantic gas fire that lasted two weeks.
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While only the 18th-largest oil field in California in size, in total remaining reserves it ranks sixth, with the equivalent of over 110 million barrels (17,000,000 m) producible reserves still in the ground, according to the California Division of Oil, Gas and Geothermal Resources
334:. Vol. I (1998), Vol. II (1992), Vol. III (1982). California Department of Conservation, Division of Oil, Gas, and Geothermal Resources (DOGGR). 1,472 pp. Lost Hills Field information pp. 256–259. PDF file available on CD from www.consrv.ca.gov. 115:. The hills rise scarcely more than 200 feet (61 m) above the San Joaquin Valley to the east, and only 100 feet (30 m) or less above the Antelope Plain to the west; in places they are almost flat. The hills and associated oil field are between 268:
As of 1997, four pools – the Tulare, Etchegoin, Cahn, and Reef Ridge – continued to have active recovery operations using waterflooding, steam flooding, and fire flooding. As of 2008, the principal operators on the Lost Hills Field were
80:, the principal operator, estimates considerably more oil in the ground). Production at Lost Hills has been increasing steadily: as of the end of 2006, it was California's second fastest-growing oil field, exceeded only by the nearby 239:
well blew out, and quickly collapsed into a crater over 15 feet (4.6 m) deep and 30 feet (9.1 m), taking with it the concrete pad, casing, and pumping unit. Yet another Getty well suffered the same fate in 1978.
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Well spacing on Lost Hills varies based on the geologic characteristics in the unit being drilled, with one well per 5 acres (20,000 m) in siliceous shale to one well per 1.25 acres (5,100 m) in
91:. In 1998, one of the field's gas wells was the site of a spectacular blowout, producing a pillar of fire which burned for 14 days and was visible more than 40 miles (64 km) away. 175:
movement. The Lost Hills Field occupies a portion of a SE-plunging anticline. There are six oil pools in the five producing units, which are, from the top, the
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to the west, both of which parallel the field; Interstate 5 runs about 4 miles (6.4 km) away and Route 33 about 7 miles (11 km). The
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The Lost Hills Field underlies a long, low range of southeast-to-northwest trending hills of the same name adjacent to the
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Natural gas well in the southeast extension of the Lost Hills Field, owned by Solimar and Livingstone Energy.
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on the south, along the western edge of the San Joaquin Valley. These anticlines run closely parallel to the
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California Department of Conservation, Oil and Gas Statistics, Annual Report, December 31, 2006.
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California Department of Conservation, Oil and Gas Statistics, Annual Report, December 31, 2006
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California Department of Conservation, Oil and Gas Statistics, Annual Report, December 31, 2006
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California Department of Conservation, Oil and Gas Statistics, Preliminary 2007 Annual Report
346:. California Division of Oil and Gas. Sacramento, 1984 and 1990. Available on the web at 465: 477:
California State Regional Water Quality Control Board: Discharge Conditions for Lost Hills
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Advanced Reservoir Characterization in the Antelope Shale to Establish the Viability of CO
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Advanced Reservoir Characterization in the Antelope Shale to Establish the Viability of CO
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Lost Hills Field Trial: Incorporating New Technology for Reservoir Management, p. 4
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Chevron USA Production Company, prepared for US Department of Energy, April 2000.
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Chevron USA Production Company, prepared for US Department of Energy, April 2000.
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age; the Reef Ridge Shale, McClure Shale, and Devilwater Shale, members of the
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Oil well with storage tanks in the background: Lost Hills Field, April 2008
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of California, which had recently been subject to antitrust litigation and
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Enhanced Oil Recovery in California's Monterey Formation Siliceous Shales
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Enhanced Oil Recovery in California's Monterey Formation Siliceous Shales
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below the Temblor, but none of these lowest units have had oil pools.
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most vegetation has been removed from the areas of active operations.
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runs adjacent to the field boundary on the northeast, and the town of
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in the Williamson Lease identified further rock units as old as the
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and Miocene age. A well drilled to 11,553 feet (3,521 m) by
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age, which can be found in much of coastal California; and the
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A peculiarity of the Lost Hills operations is the pronounced
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The Lost Hills Field is one of a series of oil fields along
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The Lost Hills field also contains considerable reserves of
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The Bellevue Gusher, at the San Joaquin Geological Society
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San Joaquin Geological Society: Oil history in Kern County
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to the west, and formed as a result of compression from
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Pictures and description of the 1998 Bellevue Blowout
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California Oil and Gas Fields, Volumes I, II and III
135:, which passes through the field from east to west. 543:"San Joaquin Geological Society: Bellevue Blowout" 597: 495: 493: 499:DOGGR, California Oil and Gas Fields, p. 257 490: 131:is on the other side of the aqueduct along 243: 284: 146: 98: 18: 606:Natural gas fields in the United States 598: 611:Oil fields in Kern County, California 107:on Lost Hills Oilfield near route 46. 35:. Other oil fields are shown in gray. 280: 13: 14: 632: 354: 297:On the evening of November 23, a 16:Kern County, California oilfield 535: 523: 511: 502: 249:the find, including the mighty 481: 470: 459: 450: 430: 421: 410: 390: 378: 1: 325: 70: 203:, underneath the others, of 51:Range, north of the town of 7: 10: 637: 582:35.6158861°N 119.7247056°W 397:Pasqual R. Perri, et al. 142: 94: 437:Pasqual R. Perri, et al. 133:California State Route 46 616:Oil fields in California 587:35.6158861; -119.7247056 371: 290: 244:History and operations 152: 108: 103:There are hundreds of 36: 288: 163:on the north and the 150: 102: 22: 344:Lost Hills Oil Field 41:Lost Hills Oil Field 25:Lost Hills Oil Field 578: /  320:standard conditions 185:Etchegoin Formation 165:Midway-Sunset Field 125:California Aqueduct 621:San Joaquin Valley 314:(2.3 million 291: 193:Monterey Formation 161:Coalinga Oil Field 153: 113:San Joaquin Valley 109: 37: 29:San Joaquin Valley 201:Temblor formation 169:San Andreas Fault 628: 593: 592: 590: 589: 588: 583: 579: 576: 575: 574: 571: 558: 557: 555: 554: 545:. Archived from 539: 533: 527: 521: 515: 509: 506: 500: 497: 488: 485: 479: 474: 468: 463: 457: 454: 448: 434: 428: 425: 419: 414: 408: 394: 388: 382: 281:Bellevue blowout 213:Upper Cretaceous 177:Tulare Formation 119:to the east and 636: 635: 631: 630: 629: 627: 626: 625: 596: 595: 586: 584: 580: 577: 572: 569: 567: 565: 564: 562: 561: 552: 550: 541: 540: 536: 528: 524: 516: 512: 507: 503: 498: 491: 486: 482: 475: 471: 464: 460: 455: 451: 442: 435: 431: 426: 422: 415: 411: 402: 395: 391: 383: 379: 374: 357: 328: 283: 275:Aera Energy LLC 246: 209:Mobil Oil Corp. 145: 97: 73: 17: 12: 11: 5: 634: 624: 623: 618: 613: 608: 573:119°43′28.94″W 560: 559: 534: 522: 510: 508:Land, p. 13-14 501: 489: 480: 469: 458: 449: 440: 429: 420: 409: 400: 389: 376: 375: 373: 370: 369: 368: 363: 356: 355:External links 353: 352: 351: 348:their FTP site 342:Paul E. Land, 340: 335: 327: 324: 282: 279: 245: 242: 144: 141: 121:State Route 33 96: 93: 72: 69: 15: 9: 6: 4: 3: 2: 633: 622: 619: 617: 614: 612: 609: 607: 604: 603: 601: 594: 591: 570:35°36′57.19″N 549:on 2016-02-02 548: 544: 538: 531: 526: 519: 514: 505: 496: 494: 484: 478: 473: 467: 462: 456:Chevron, 2000 453: 446: 444: 433: 424: 418: 413: 406: 404: 393: 386: 381: 377: 367: 364: 362: 359: 358: 349: 345: 341: 339: 336: 333: 330: 329: 323: 321: 318:) per day at 317: 313: 309: 305: 300: 295: 287: 278: 276: 272: 271:Chevron Corp. 266: 262: 260: 259:Supreme Court 256: 252: 241: 238: 233: 228: 226: 220: 216: 214: 210: 206: 202: 198: 194: 190: 186: 182: 178: 174: 170: 166: 162: 158: 149: 140: 136: 134: 130: 126: 122: 118: 114: 106: 101: 92: 90: 85: 83: 79: 78:Chevron Corp. 68: 66: 65:United States 62: 58: 54: 50: 46: 42: 34: 30: 26: 21: 563: 551:. Retrieved 547:the original 537: 525: 513: 504: 483: 472: 461: 452: 438: 432: 427:Land, p. 3-9 423: 412: 398: 392: 380: 343: 337: 331: 316:cubic metres 299:wildcat well 296: 292: 267: 263: 251:Standard Oil 247: 229: 221: 217: 159:between the 154: 137: 117:Interstate 5 110: 86: 82:Cymric Field 74: 40: 38: 24: 585: / 487:Land, p. 12 181:Pleistocene 89:natural gas 57:Kern County 55:in western 43:is a large 31:of central 600:Categories 553:2008-04-12 326:References 312:cubic feet 306:(320  232:subsidence 157:anticlines 129:Lost Hills 71:Production 61:California 53:Lost Hills 49:Lost Hills 33:California 255:broken up 237:Getty Oil 225:diatomite 205:Oligocene 183:age; the 105:pumpjacks 63:, in the 45:oil field 189:Pliocene 173:tectonic 520:, p. 67 304:barrels 257:by the 197:Miocene 143:Geology 95:Setting 47:in the 27:in the 532:, p. 1 387:, p. 2 372:Notes 195:, of 187:, of 179:, of 273:and 39:The 23:The 602:: 492:^ 277:. 227:. 84:. 67:. 59:, 556:. 445:. 441:2 405:. 401:2 350:. 308:m 76:(

Index


San Joaquin Valley
California
oil field
Lost Hills
Lost Hills
Kern County
California
United States
Chevron Corp.
Cymric Field
natural gas

pumpjacks
San Joaquin Valley
Interstate 5
State Route 33
California Aqueduct
Lost Hills
California State Route 46

anticlines
Coalinga Oil Field
Midway-Sunset Field
San Andreas Fault
tectonic
Tulare Formation
Pleistocene
Etchegoin Formation
Pliocene

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