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,{"id":48302,"text":"ofr76665 - 1976 - Basic data from five core holes in the Raft River geothermal area, Cassia County, Idaho","interactions":[],"lastModifiedDate":"2013-11-26T11:05:52","indexId":"ofr76665","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-665","title":"Basic data from five core holes in the Raft River geothermal area, Cassia County, Idaho","docAbstract":"<p>Studies of the geothermal aspect-of the Bridge area of \nthe Raft River basin in south-central Idaho (fig. 1) by the \nU.S. Geological Survey began in 1972 when Young and Mitchell \n(1973) made a geochemical and geologic reconnaissance of \nselected thermal waters in Idaho. The Bridge area had been \ndesignated the Frazier known geothermal resource area \n(Frazier KGRA) by the U.S. Geological Survey (Godwin and \nothers-, 1971) . Since 1972, several units of the Geological \nSurvey have studied the area to provide data for the U.S. \nEnergy Research and Development Administration, which proposes to ascertain whether the geothermal resource can be \ndeveloped for power generation and other uses. The studies \ninclude geologic mapping, geophysical surveys, water sampling, test drilling, and studies of all available drill- \nhole data. A list of reports already prepared on the area \nis included with this report.</p>\n<br/>\n<p>Core drilling of five holes began in August 1974 and \nwas completed in March 1975. These holes are referred to as \nintermediate-depth core holes, principally because in the \nspring of 1974, 35 auger holes 25 to 98 feet (7.6 to 30\nmeters) were completed in the area (Crosthwaite, 1974), and \nthe Aerojet Nuclear Company, under the auspices of the U.S. \nEnergy Research and Development Administration, was planning \nsome deep drilling 4,000 to 6,000 feet (1,200 to 1,800 \nmeters) (fig. 1). The purpose of the core drilling was to \nprovide information to test geophysical interpretations of \nthe subsurface structure and lithology and to provide hydrologic and geologic data on the shallow part of the geothermal \nsystem. Samples of the core were made available to several \ndivisions and branches of the Geological Survey and to \npeople and agencies outside the Survey. This report presents the basic data from the core holes that had been \ncollected to September 1, 1975, and includes lithologic and \ngeophysical well logs, chemical analyses of water (table 1), \nand laboratory analyses of cores (table 2) that were completed as of the above date. The data were collected by the \nIdaho District office, Hydrologic Laboratory, Borehole \nGeophysics Research Project, and Drilling, Sampling, and \nTesting Section, all of the Water Resources Division, and \nthe Branch of Central Environmental Geology of the Geologic \nDivison.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Boise, ID","doi":"10.3133/ofr76665","collaboration":"Prepared in cooperation with the Idaho Department of Water Resources","usgsCitation":"Crosthwaite, E.G., 1976, Basic data from five core holes in the Raft River geothermal area, Cassia County, Idaho: U.S. Geological Survey Open-File Report 76-665, 11 p., https://doi.org/10.3133/ofr76665.","productDescription":"11 p.","numberOfPages":"11","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":171160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0665/report-thumb.jpg"},{"id":84953,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0665/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84954,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0665/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84955,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0665/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84956,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0665/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84957,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0665/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84958,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0665/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Idaho","county":"Cassia County","otherGeospatial":"Raft River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.675537,41.990119 ], [ -113.675537,42.454874 ], [ -113.125062,42.454874 ], [ -113.125062,41.990119 ], [ -113.675537,41.990119 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640c4f","contributors":{"authors":[{"text":"Crosthwaite, E. G. (compiler)","contributorId":25451,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E.","suffix":"(compiler)","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":237147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28394,"text":"wri768 - 1976 - Digital model to predict effects of pumping from the Arikaree aquifer in the Dwyer area, southeastern Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:49","indexId":"wri768","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-8","title":"Digital model to predict effects of pumping from the Arikaree aquifer in the Dwyer area, southeastern Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri768","usgsCitation":"Lines, G.C., 1976, Digital model to predict effects of pumping from the Arikaree aquifer in the Dwyer area, southeastern Wyoming: U.S. Geological Survey Water-Resources Investigations Report 76-8, iv, 24 p. :ill., maps (some fold. in pocket) ;26 cm. --, https://doi.org/10.3133/wri768.","productDescription":"iv, 24 p. :ill., maps (some fold. in pocket) ;26 cm. --","costCenters":[],"links":[{"id":118921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0008/report-thumb.jpg"},{"id":57193,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57194,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57195,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57196,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57197,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57198,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57199,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0008/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0008/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a9b2","contributors":{"authors":[{"text":"Lines, G. C.","contributorId":30577,"corporation":false,"usgs":true,"family":"Lines","given":"G.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":199723,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48304,"text":"ofr76728 - 1976 - Flood of June 27, 1975, in City of Ames, Iowa","interactions":[],"lastModifiedDate":"2016-02-22T15:03:48","indexId":"ofr76728","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-728","title":"Flood of June 27, 1975, in City of Ames, Iowa","docAbstract":"<p>On June 27, 1975, the city of Ames and vicinity sustained severe flooding from Squaw creek and the south Skunk River. The storm which preceded the flood was net particularly outstanding in its intensity or duration. However, antecedent conditions plus the timing and direction of the storm were \"ideally tuned\" to cause the flood.</p>\n<p>In terms of magnitude of discharge as well as of damages this was the most severe flood on record, with losses estimated by city and Iowa State University officials at over a million dollars. The most unfortunate loss involved the drowning of a young person.</p>\n<p>The peak discharge at the Squaw Creek station, 206 mi<sup>2</sup> (534 km<sup>2</sup>), was measured at 11,300 ft<sup>3</sup>/s (320 m<sup>3</sup>/s), which is 1.6 times the 100-year flood. The south Skunk River above the confluence with Squaw creek, 315 mi<sup>2</sup> (816 km<sup>2</sup>), peaked at 5,330 ft<sup>3</sup>/s (151 m<sup>3</sup>). The recurrence interval of this discharge is 6.0 years. The peak discharge on the South Skunk River below the confluence with Squaw creek, 556 mi<sup>2</sup> (1440 km<sup>2</sup>), was 14,700 ft<sup>3</sup>/s (416 m<sup>3</sup>/s), which is 1.1 times the 100-year flood.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/ofr76728","collaboration":"Prepared in cooperation with the Highway Research Board, Highway Division, Iowa Department of Transportation","usgsCitation":"Lara, O.G., and Heinitz, A.J., 1976, Flood of June 27, 1975, in City of Ames, Iowa: U.S. Geological Survey Open-File Report 76-728, v, 56 p., https://doi.org/10.3133/ofr76728.","productDescription":"v, 56 p.","numberOfPages":"66","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":286006,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0728/report.pdf"},{"id":286007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0728/report-thumb.jpg"}],"country":"United States","state":"Iowa","city":"Ames","otherGeospatial":"South Skunk River, Squaw Creek","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.56849670410156,\n              42.01052981889534\n            ],\n            [\n              -93.58497619628906,\n              42.05235185455305\n            ],\n            [\n              -93.62068176269531,\n              42.08905095219165\n            ],\n            [\n              -93.57948303222656,\n              42.12267315117259\n            ],\n            [\n              -93.58154296875,\n              42.14355068927749\n            ],\n            [\n              -93.6309814453125,\n              42.19240775778094\n            ],\n            [\n              -93.66325378417969,\n              42.222924262739824\n            ],\n            [\n              -93.70376586914062,\n              42.2752765520868\n            ],\n            [\n              -93.71681213378906,\n              42.301182475461204\n            ],\n            [\n              -93.75869750976562,\n              42.34129022434778\n            ],\n            [\n              -93.93241882324219,\n              42.28594498725423\n            ],\n            [\n              -93.95027160644531,\n              42.27578461376819\n            ],\n            [\n              -93.95027160644531,\n              42.23461834757937\n            ],\n            [\n              -93.94134521484374,\n              42.196477476842915\n            ],\n            [\n              -93.93791198730469,\n              42.17968819665961\n            ],\n            [\n              -93.90495300292969,\n              42.109939567658415\n            ],\n            [\n              -93.8788604736328,\n              42.06560675405716\n            ],\n            [\n              -93.74496459960938,\n              41.9727643622653\n            ],\n            [\n              -93.66325378417969,\n              41.97378534488489\n            ],\n            [\n              -93.56849670410156,\n              42.01052981889534\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eed3d","contributors":{"authors":[{"text":"Lara, Oscar G.","contributorId":19555,"corporation":false,"usgs":true,"family":"Lara","given":"Oscar","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":237149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Heinitz, Albert J.","contributorId":43355,"corporation":false,"usgs":true,"family":"Heinitz","given":"Albert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":237150,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26303,"text":"wri7537 - 1976 - Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri7537","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75-37","title":"Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California","language":"ENGLISH","publisher":"Water Resources Division, U.S. Geological Survey,","doi":"10.3133/wri7537","usgsCitation":"Bradford, W.L., 1976, Distribution and movement of zinc and other heavy metals in South San Francisco Bay, California: U.S. Geological Survey Water-Resources Investigations Report 75-37, iv, 58 p. :ill. ;27 cm., https://doi.org/10.3133/wri7537.","productDescription":"iv, 58 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":118990,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0037/report-thumb.jpg"},{"id":55106,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64966b","contributors":{"authors":[{"text":"Bradford, Wesley L.","contributorId":95451,"corporation":false,"usgs":true,"family":"Bradford","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":196143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39586,"text":"pp813E - 1976 - Summary appraisals of the nation's ground-water resources – California region","interactions":[],"lastModifiedDate":"2021-12-14T21:19:21.369651","indexId":"pp813E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"813","chapter":"E","title":"Summary appraisals of the nation's ground-water resources – California region","docAbstract":"<p>Most people in the California Region live in a semiarid or arid climate, with precipitation less than the potential evapotranspiration- environments of perennial water deficiency. The deficiency becomes most onerous during the characteristically rainless summers and during recurrent droughts that may continue for 10--20 years. However, water from winter rain and snow can be stored for use during the dry summer months, and water stored during a wet climatic period can be used in a succeeding dry period; moreover, perennial deficiency can be overcome by bringing water from areas of perennial surplus. Ground-water reservoirs have especial significance in arid and semiarid regions as repositories where water is stored or can be stored with minimum loss by evaporation.</p>\n<p>Nearly all the ground-water reservoirs of the California Region are in alluvial sediments of valleys and plains that flank the mountain ranges. The largest, underlying the vast Central Valley, occupies 10 percent of the area of the region, has an estimated usable capacity exceeding 100 million acre-feet (125 cubic kilometres), and has an annual pumpage from wells of about 13 million acre-feet (16 cubic kilometres). Another 10 percent of the region is occupied by 55 developed ground-water reservoirs that are widely distributed; aggregate annual pumpage from them is about 3 1/2 million acre-feet (4 cubic kilometres). In the southeastern desert about 60 ground-water reservoirs occupy still another 10 percent of the region; these have been explored only enough to show that most have some usable water, but current use is negligible. In northeastern California and adjacent Oregon and Nevada, ground-water reservoirs are identified only in valleys and lowlands where wells are feasible, but basaltic rocks of the Cascade Range and Modoc Plateau are excellent aquifers distributed over an area constituting about 15 percent of the region. In sum, slightly less than half the California Region is underlain by ground-water reservoirs, either in valley fill or in volcanic rocks, which can yield significant quantities of water to wells.</p>\n<p>The rest of the California Region includes the mountains, canyons, slopes, and foothills of the Sierra Nevada, Coast Ranges, and Basin Ranges, whose consolidated rocks and products of their weathering may be permeable locally but are not generally so. Here, the prevailing method of ground-water development is still mostly trial and error, and while in many places a well can yield enough water for a family, some families might have to do without amenities such as flush toilets and automatic washers.</p>\n<p>For more than half a century the California Region has led all others in North America in pumping of ground water as well as in the area, variety, yield, and export of crops irrigated by water from wells. It has led in the development and use of deep-well turbine pumps for large yield and in the drilling of water wells to great depths. At the same time, such developments have resulted in the elimination of artesian pressures that produced thousands of flowing wells in the 19th century and led to the wide distribution of \"falling water tables.\" Also, California was first to induce encroachment of seawater into wells (in 1906); first to recognize subsidence of land caused by pumping from wells (in 1933), generating news about land sinking in San Jose, Long Beach, and along the Delta-Mendota and Friant-Kern Canals; and first to experience pollution of ground-water reservoirs by brines, chemicals, industrial wastes, and petroleum byproducts including gasoline. The region has led in research in several fields leading to solution of many of these problems.</p>\n<p>Ground-water problems developed rapidly after World War II with booming population, agriculture, industry, and water demand during several years of regionwide drought. Water levels in wells trended downward almost everywhere as a natural effect of the drought and at accelerated rates in areas of pumping for new enterprises or to supplement subnormal surface-water supplies. The declines in many pumping areas exceeded 100 feet (30 metres), and in some confined aquifers the potentiometric surface was drawn down more than 330 feet (100 metres). The depletion of ground-water storage has had \"permanent\" side effects, including subsidence of the land exceeding 10 feet (3 metres) in extensive areas, and seawater intrusion that ended the useful lives of many wells along the coast and as much as 6 miles (10 kilometres) inland. Some problems have been solved, but these solutions have at times created other problems. Many ground-water reservoirs have gone through one or more stages - exploration for productive aquifers, exploitation and development for use of the water, restriction to the perennial supply or \"safe\" yield, importation of surface water, artificial recharge of ground water, conjunctive use of surface and ground water, protection of water quality, and integrated management of use and disposal of water. This evolutionary sequence is unique for each reservoir, and so generalizations become difficult in a regional appraisal; also, the changes with time are significant and varied, and knowledge of prior events is a prerequisite in an appraisal of the resource in a specific year.</p>\n<p>As of 1970, water levels in many wells had risen significantly from the minimum levels of record reached during the 1960's or earlier; only in areas of new development and in desert areas of long-continued \"mining\" of nonreplenished water was ground-water storage still being depleted. Land subsidence has continued at diminishing rates and practically has come to a halt in some areas; invading seawater has been stopped or nudged back in most places where problems were significant. The current, favorable situation has been helped by climatic variations, from drought in 1945-52 and exceedingly dry years in 1959 and 1961 to above-normal precipitation in 1969 and 1970; but most of the serious problems have been solved by human efforts, including especially the implementation of the California Water Plan, transporting water from areas of perennial surplus to areas where it is used in lieu of ground water or for ground-water replenishment. All major urban areas now import water to supplement or replace the water pumped from wells. Extensive agricultural areas that formerly were irrigated solely by ground water now obtain some of their water from surface reservoirs and canals, especially in the Central Valley. With surface water available as an alternative supply, well owners can view their ground&nbsp;water with complacency. But complacency can lead to neglect and carelessness and consequent deterioration of the ground-water resource by pollution.</p>\n<p>Claiming heritage from the English Common Law, the existing California law grants to the landowner (riparian) and private enterprise (appropriator) rights to the water stored in ground-water reservoirs or discharged from them, including the base flow of streams. Ground-water development has been by private and local enterprise, and the California legislature has protected and encouraged local responsibility, control, and management of ground water. As to surface water, a constitutional amendment in 1928 limited riparian rights to the quantities of water that were \"reasonably required for the beneficial use to be served.\" The surpluses have become public waters which are collected, stored, transported, and delivered under various contracts by Federal, State, and other agencies. The agencies have not stored water underground because of uncertainty as to their rights, but some local agencies have been encouraged with favorable pricing schedules to undertake the artificial recharge and management of ground-water reservoirs. Thus, conjunctive use of surface and ground water has become a matter of interagency negotiation.</p>\n<p>Of all the constraints on effective use of ground-water reservoirs, the most formidable may be the attitudes of people. Assurance of water supply is vital in areas of water deficiency, and Government has assumed increasing responsibility for the welfare of people in these areas. Unfortunately, when Government provides this assurance, most beneficiaries demand continued subsidy to the exclusion of perhaps cheaper private development. Indeed, as the water resources are presently segregated-with private rights predominant in ground water and public interest dominant in surface water-ground-water development has suffered for lack of public concern. The region has the scientific and technologic capability for effective use of groundwater reservoirs, as shown by the achievements and programs of several districts, but many districts are not organized or staffed for such comprehensive management and will need assistance and scientific expertise available from State and Federal agencies. Those agencies, in turn, may not have the scientific data that are essential to prevent haphazard activities and to enable programs to be organized for the most effective and attractive utilization of the water resources. In these days of increasing concern over pollution, existing data are generally inadequate to assess the natural deterioration of ground waters as a basis for defining pollution.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813E","usgsCitation":"Thomas, H.E., and Phoenix, D.A., 1976, Summary appraisals of the nation's ground-water resources – California region: U.S. Geological Survey Professional Paper 813, Report: iv, 51 p.; Plate: 20.00 x 25.84 inches, https://doi.org/10.3133/pp813E.","productDescription":"Report: iv, 51 p.; Plate: 20.00 x 25.84 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":67170,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0813e/plate-1.pdf","text":"Plate 1","size":"7.39 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 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,{"id":20985,"text":"ofr76443 - 1976 - Flood-plain delineation for Cameron Run Basin, Fairfax County-Alexandria City, Virginia","interactions":[],"lastModifiedDate":"2014-04-09T13:17:28","indexId":"ofr76443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-443","title":"Flood-plain delineation for Cameron Run Basin, Fairfax County-Alexandria City, Virginia","docAbstract":"Flood-Plain Delineation for Cameron Run Basin Water-surface profiles of the 25-, 50-, and 100-year recurrence interval discharges have been computed for all streams and reaches of channels in Fairfax County, Virginia, having a drainage area greater than 1 square mile except for Dogue Creek, Little Hunting Creek, and that part of Cameron Run above Lake Barcroft. Maps having a 2-foot contour interval and a horizontal scale of 1 inch equals 100 feet have been used for a base on which flood boundaries were delineated for 25-, 50-, and 100-year floods to be expected in each basin under ultimate development conditions. Included are techniques employed in computing discharges and profiles as well as the flood profiles and maps on which flood boundaries have been delineated for that part of Cameron Run basin below Lake Barcroft in both Fairfax County and the city of Alexandria.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76443","collaboration":"Prepared in cooperation with the County of Fairfax","usgsCitation":"Soule, P., 1976, Flood-plain delineation for Cameron Run Basin, Fairfax County-Alexandria City, Virginia: U.S. Geological Survey Open-File Report 76-443, 94 p., https://doi.org/10.3133/ofr76443.","productDescription":"94 p.","numberOfPages":"96","costCenters":[],"links":[{"id":154371,"rank":0,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0443/report.pdf"},{"id":286005,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0443/report-thumb.jpg"}],"country":"United States","state":"Virginia","county":"Fairfax County","city":"Alexandria City","otherGeospatial":"Cameron Run Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -77.5,38.5 ], [ -77.5,39.0 ], [ -77.0,39.0 ], [ -77.0,38.5 ], [ -77.5,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e5620","contributors":{"authors":[{"text":"Soule, Pat L.","contributorId":71576,"corporation":false,"usgs":true,"family":"Soule","given":"Pat L.","affiliations":[],"preferred":false,"id":183621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55108,"text":"wdrWY751 - 1976 - Water resources data for Wyoming, water year 1975","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"wdrWY751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"WY-75-1","title":"Water resources data for Wyoming, water year 1975","language":"ENGLISH","doi":"10.3133/wdrWY751","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Wyoming, water year 1975: U.S. Geological Survey Water Data Report WY-75-1, 646 p., https://doi.org/10.3133/wdrWY751.","productDescription":"646 p.","costCenters":[],"links":[{"id":181829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f146f","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":532255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27300,"text":"wri7648 - 1976 - Thermal loading of Hyco Lake, North Carolina : the effect of heated water on temperature and evaporation, 1966-74","interactions":[],"lastModifiedDate":"2019-07-16T11:50:46","indexId":"wri7648","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-48","title":"Thermal loading of Hyco Lake, North Carolina : the effect of heated water on temperature and evaporation, 1966-74","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7648","usgsCitation":"Giese, G.L., 1976, Thermal loading of Hyco Lake, North Carolina : the effect of heated water on temperature and evaporation, 1966-74: U.S. Geological Survey Water-Resources Investigations Report 76-48, viii, 46 p., https://doi.org/10.3133/wri7648.","productDescription":"viii, 46 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":365595,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0048/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158682,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0048/report-thumb.jpg"}],"country":"United States","state":"North Carolina","otherGeospatial":"Hyco Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.24163818359375,\n              36.361586786517776\n            ],\n            [\n              -79.24163818359375,\n              36.54163950596125\n            ],\n            [\n              -78.92715454101562,\n              36.54163950596125\n            ],\n            [\n              -78.92715454101562,\n              36.361586786517776\n            ],\n            [\n              -79.24163818359375,\n              36.361586786517776\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a57e4b07f02db62e1b1","contributors":{"authors":[{"text":"Giese, G. L.","contributorId":44898,"corporation":false,"usgs":true,"family":"Giese","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197876,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56333,"text":"wdrNC751 - 1976 - Water resources data for North Carolina, water year 1975","interactions":[],"lastModifiedDate":"2020-08-12T20:42:51.475357","indexId":"wdrNC751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NC-75-1","title":"Water resources data for North Carolina, water year 1975","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNC751","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for North Carolina, water year 1975: U.S. Geological Survey Water Data Report NC-75-1, xiv, 426 p., https://doi.org/10.3133/wdrNC751.","productDescription":"xiv, 426 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,{"id":26507,"text":"wri7675 - 1976 - Summary of geology and ground-water resources of Passaic County, New Jersey","interactions":[],"lastModifiedDate":"2016-10-25T12:24:00","indexId":"wri7675","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-75","title":"Summary of geology and ground-water resources of Passaic County, New Jersey","docAbstract":"<p>Ground water in Passaic County occurs in intergranular openings of&nbsp;unconsolidated stratified deposits of Quaternary age and in joints and&nbsp;fractures in consolidated rocks of Precambrian, Paleozoic, and Triassic&nbsp;age.</p><p>The Brunswick Formation of Triassic age is the most important aquifer in the southeastern one-third of Passaic County. Reported yields of public supply and industrial wells range from 50 to 510 gallons per minute (3 to 32 litres per second) and the median yield is 130 gallons per minute (8 litres per second). Most of these wells are 200 to 400 feet (61 to 122 metres) deep. The median yield of all public supply and industrial wells over 300 feet (91 metres) deep and 8 inches (203 millimetres) or larger in diameter is 230 gallons per minute (15 litres per second). Crystalline rocks of Precambrian age are the major source of ground water for domestic use in the northwestern two-thirds of Passaic County. Reported well yields range from 1 to 200 gallons per minute (.06 to 13 litres per second). The median reported yield of domestic wells is 5 gallons per minute (.31 litres per second) and that of public supply wells is 30 gallons per minute (2 litres per second).</p><p>Other consolidated rocks--rocks of Paleozoic age and the Watchung Basalt of Traissic age--are utilized primarily for domestic water supplies in Passaic County. Reported yields of wells tapping the Paleozoic rocks range from less than 1 to 35 gallons per minute (.06 to 2 litres per second) and the median yield is 10 gallons per minute (.63 litres per second). Reported yields of domestic wells tapping the Watchung Basalt range from less than 1 to 40 gallons per minute (.06 to 3 litres per second) and the median yield is 12 gallons per minute (.76 litres per second). However, reported yields of nine industrial and commercial wells range from 50 to 180 gallons per minute (3 to 11 litres per second).</p><p>Unconsolidated stratified deposits of Quaternary age are locally an important source of ground water for public supply and industrial use in parts of Passaic County. These deposits have not been extensively explored but are potentially an important source of ground water for future development. Reported yields of wells tapping the stratified deposits range from 4 to 920 gallons per minute (.25 to 58 litres per second). The median reported yield of domestic wells is 16 gallons per minute (1 litre per second) and that of public supply and industrial wells is 130 gallons per minute (8 litres per second. Depths of wells depend upon the thickness of the deposits. Reported depths range from 22 to 170 feet (7 to 52 metres).</p><p>The quality of ground water in Passaic County varies from one aquifer to another. Water from the Precambrian rocks is soft to moderately hard (34 to 104 milligrams per litre) and is low in dissolved solids (66 to 159 milligrams per litre). Water from the Brunswick Formation is moderately hard to very hard (89 to 540 milligrams per litre). The dissolved solids content ranges from 129 to 563 milligrams per litre). The occurrence of more highly mineralized water at depth in the Brunswick Formation is indicated by an analysis, made in 1885, of 16,000 milligrams per litre of dissolved solids at a depth of 2,050 feet (625 metres) in a well in Paterson. Water from two wells tapping the Quaternary deposits is moderately hard (65 and 83 milligrams per litre) and has dissolved solids contents of 122 and 133 milligrams per litre).</p><p>Water use from both surface and ground-water supplies in Passaic County averaged about 106 million gallons per day (4.6 cubic metres per second) in 1965. Ground water probably accounts for 5 to 10 percent of this total. Ground-water pumpage by the major public supply companies in the county has increased from 2.1 million gallons per day (.09 cubic metres per second) in 1951 to 4.39 million gallons per day (.19 cubic metres per second) in 1968. About 80 percent of the 4.39 million gallons per day (.19 cubic metres per second) was from wells tapping the Brunswick Formation in the southern part of the county.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Trenton, NJ","doi":"10.3133/wri7675","usgsCitation":"Carswell, L., and Rooney, J., 1976, Summary of geology and ground-water resources of Passaic County, New Jersey: U.S. Geological Survey Water-Resources Investigations Report 76-75, Report: vi, 47 p.; 3 Figures, https://doi.org/10.3133/wri7675.","productDescription":"Report: vi, 47 p.; 3 Figures","costCenters":[],"links":[{"id":157842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7675.jpg"},{"id":330375,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330376,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0075/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330377,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0075/figure-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":330378,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0075/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"New Jersey","county":"Passaic 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L.D.","contributorId":6435,"corporation":false,"usgs":true,"family":"Carswell","given":"L.D.","email":"","affiliations":[],"preferred":false,"id":196511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rooney, J.G.","contributorId":72414,"corporation":false,"usgs":true,"family":"Rooney","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":196512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55950,"text":"wdrNV751 - 1976 - Water resources data for Nevada, water year 1975","interactions":[],"lastModifiedDate":"2024-07-22T21:03:55.873227","indexId":"wdrNV751","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NV-75-1","title":"Water resources data for Nevada, water year 1975","docAbstract":"<p>Water resources data for the 1975 water year for Nevada consist of records of discharge and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels in wells. This report contains discharge records for 120 gaging stations; stage and contents for 21 lakes and reservoirs; water-quality data for continuing-record stations at 23 stream sites and for partial-record stations at 5 stream sites and 2 lake sites; and water levels for 62 observation wells. Also included are 121 crest-stage partial-record stations and 13 low-flow partial-record stations. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Nevada.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrNV751","collaboration":"Prepared in cooperation with the State of Nevada and with other agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Water resources data for Nevada, water year 1975: U.S. Geological Survey Water Data Report NV-75-1, xv, 292 p., https://doi.org/10.3133/wdrNV751.","productDescription":"xv, 292 p.","costCenters":[],"links":[{"id":431320,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1975/nv-75-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184292,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1975/nv-75-1/report-thumb.jpg"}],"country":"United 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,{"id":11386,"text":"ofr76583 - 1976 - Ground-water exploration in northeastern Kenya","interactions":[],"lastModifiedDate":"2012-02-02T00:06:26","indexId":"ofr76583","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-583","title":"Ground-water exploration in northeastern Kenya","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76583","usgsCitation":"Swarzenski, W., and Wanyeki, S., 1976, Ground-water exploration in northeastern Kenya: U.S. Geological Survey Open-File Report 76-583, ii, 14 leaves :fold. map (in pocket) ;29 cm.; (8 p. - PGS), https://doi.org/10.3133/ofr76583.","productDescription":"ii, 14 leaves :fold. map (in pocket) ;29 cm.; (8 p. - PGS)","costCenters":[],"links":[{"id":143065,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce6a","contributors":{"authors":[{"text":"Swarzenski, W.V.","contributorId":80243,"corporation":false,"usgs":true,"family":"Swarzenski","given":"W.V.","email":"","affiliations":[],"preferred":false,"id":163051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wanyeki, Simon","contributorId":8855,"corporation":false,"usgs":true,"family":"Wanyeki","given":"Simon","email":"","affiliations":[],"preferred":false,"id":163050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3376,"text":"cir730 - 1976 - Geologic appraisal of the petroleum potential of offshore southern California; the borderland compared to onshore coastal basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir730","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"730","title":"Geologic appraisal of the petroleum potential of offshore southern California; the borderland compared to onshore coastal basins","docAbstract":"Offshore southern California is part of a much larger Pacific continental margin, and the two areas have a similar geologic history at least as far back as middle Tertiary time. Assessment of the petroleum potential of the offshore Southern California borderland is accomplished by examining the adjacent highly explored productive coastal basins in the tectonically unstable area west of the San Andreas fault. Known oil and gas accumulations in this region can be characterized as follows: 88 percent comes from the Los Angeles and Ventura basins; 87 percent has been found in late Miocene and younger strata and only 0.2 percent has been found in Eocene strata; 80 percent has been found in thick deposits of deep-water turbidite reservoirs; and 5 percent has been found in fractured Miocene siliceous shale reservoirs. The percentage of siliceous shale reservoirs will increase as a result of recent discoveries in this rock type in the Santa Barbara Channel. Of the 212 known fields only 5 are giants (greater than 500 million barrels), and these fields account for 52 percent of all past production from the region. Most fields are faulted anticlines, and the largest fields have the highest oil recoveries per acre. \r\n\r\nGeologic knowledge of the offshore is limited by the availability of data. Data have been obtained from geophysical surveys, analyses of bedrock samples from the sea floor, and extrapolations of data from the mainland and offshore islands. Several factors have a negative effect on the assessment of the petroleum potential of the southern California borderland. They are: \r\n\r\n1. The Neogene section is relatively thin, and the Paleogene section is thin and has a limited distribution. \r\n\r\n2. Over large areas, Miocene sediments apparently rest directly on basement. \r\n\r\n3. Along much of the Santa Rosa-Cortes Ridge, sediments are uplifted and truncated, exposing Paleogene rocks. \r\n\r\n4. Organic content in Paleogene sediments is believed too low to generate large amounts of petroleum. \r\n\r\n5. Source rocks are immature, even in sediments as old as Eocene. \r\n\r\n6. Burial and thermal history are insufficient for the generaton of hydrocarbons over much of the borderland area. \r\n\r\n7. Documented oil and gas seeps are unknown seaward of the Channel Islands.\r\n\r\n8. Limited exploratory drilling nearshore, the best prospective area, has not been favorable. \r\n\r\n9. Adequate or thick reservoirs of deep-water turbidire origin are not evident. \r\n\r\nThese negative factors are partly offset by the following positive factors: \r\n\r\n1. Miocene sediments are excellent potential source rocks. \r\n\r\n2. Asphaltic oil in rocks of Monterey-type lithology may be generated at lower than normal temperatures. \r\n\r\n3. Shallow-water sands of reservoir quality possibly are present in the uppermost Paleogene and lowermost Neogene section. \r\n\r\n4. Potential structural traps may be analogous to major structural producing trends onshore. \r\n\r\n5. Fractured shale reservoirs may be present along flanks of major banks and ridges. \r\n\r\n6. Buried and unsampled Paleogene and Late Cretaceous sediments may be better source rocks than those sampled and measured. \r\n\r\nThe southern California borderland, although a part of a locally rich petroliferous region, has no known basins with geologic histories or characteristics similar to the Los Angeles and Ventura basins. Some offshore basins are similar to less endowed basins in terms of petroleum potential such as the Santa Maria and Salinas basins. Areas with the best petroleum potential may be in deep water (greater than 500 m). Some of the past high estimates of the petroleum potential may have been overstated; the existing geologic data tend to substantiate low estimates of 0.6 to 5.8 billion barrels of oil and 0.6 to 5.8 trillion ft3 of gas for the southern California borderland at the 5 and 95 percent probability level.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir730","usgsCitation":"Taylor, J.C., 1976, Geologic appraisal of the petroleum potential of offshore southern California; the borderland compared to onshore coastal basins: U.S. Geological Survey Circular 730, iv, 43 p. :ill., maps ;26 cm. , https://doi.org/10.3133/cir730.","productDescription":"iv, 43 p. :ill., maps ;26 cm. ","costCenters":[],"links":[{"id":124495,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1976/0730/report-thumb.jpg"},{"id":30386,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1976/0730/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9c1","contributors":{"authors":[{"text":"Taylor, James Carlton","contributorId":18745,"corporation":false,"usgs":true,"family":"Taylor","given":"James","email":"","middleInitial":"Carlton","affiliations":[],"preferred":false,"id":146746,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65906,"text":"i1001 - 1976 - Topographic map of the Aeolis Quadrangle of Mars","interactions":[],"lastModifiedDate":"2019-11-12T09:31:19","indexId":"i1001","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1001","title":"Topographic map of the Aeolis Quadrangle of Mars","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/i1001","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Topographic map of the Aeolis Quadrangle of Mars: U.S. Geological Survey IMAP 1001, 1 Plate: 28.00 x 24.00 inches, https://doi.org/10.3133/i1001.","productDescription":"1 Plate: 28.00 x 24.00 inches","costCenters":[],"links":[{"id":189437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":101222,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1001/plate-1.pdf","size":"4602","linkFileType":{"id":1,"text":"pdf"}}],"scale":"5000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629de5","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":534259,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":43632,"text":"ofr76111 - 1976 - Land use and land cover and associated maps for Pratt, Kans.","interactions":[],"lastModifiedDate":"2012-02-02T00:10:30","indexId":"ofr76111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-111","title":"Land use and land cover and associated maps for Pratt, Kans.","language":"ENGLISH","doi":"10.3133/ofr76111","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Land use and land cover and associated maps for Pratt, Kans.: U.S. Geological Survey Open-File Report 76-111, 6 maps., https://doi.org/10.3133/ofr76111.","productDescription":"6 maps.","costCenters":[],"links":[{"id":172556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b26e4b07f02db6b05e8","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531275,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48307,"text":"ofr76890 - 1976 - Ground-water records for northeastern Oklahoma : Part 1, records of wells, test-holes, and springs","interactions":[],"lastModifiedDate":"2014-07-10T12:51:38","indexId":"ofr76890","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-890","title":"Ground-water records for northeastern Oklahoma : Part 1, records of wells, test-holes, and springs","docAbstract":"<p>The U. S. Geological Survey has collected data on Oklahoma's ground-water resources since 1934. Most of these data were collected as part of specific ground-water studies conducted in cooperation with various Federal, State, and local agencies.</p>\n<br/>\n<p>Although a large amount of ground-water data have been published, they are scattered through a variety of reports and are not readily available on a regional basis. Furthermore, a considerable amount of data have never been published and can be obtained only from the files of the Geological Survey. The purpose of this report is to make available both published and unpublished records for approximately 3,360 wells, test-holes, and springs in 23 counties in northeastern Oklahoma. In addition, selected references to pertinent ground-water reports covering parts of the 23-county area are included for those requiring more specific information.</p>\n<br/>\n<p>The stratigraphic nomenclature and age determinations used in the report are those accepted by the Oklahoma Geological Survey and do not necessarily agree with those of the U.S. Geological Survey.</p>\n<br/>\n<p>Acknowledgment is extended to the many hundreds of individuals who have provided the data compiled in this report.</p>","language":"English","publisher":"U.s. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr76890","usgsCitation":"Havens, J., and Bergman, D.L., 1976, Ground-water records for northeastern Oklahoma : Part 1, records of wells, test-holes, and springs: U.S. Geological Survey Open-File Report 76-890, v. ; 27 cm., https://doi.org/10.3133/ofr76890.","productDescription":"v. ; 27 cm.","costCenters":[],"links":[{"id":171267,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667063","contributors":{"authors":[{"text":"Havens, John S.","contributorId":13949,"corporation":false,"usgs":true,"family":"Havens","given":"John S.","affiliations":[],"preferred":false,"id":237154,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, DeRoy L.","contributorId":87606,"corporation":false,"usgs":true,"family":"Bergman","given":"DeRoy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":237155,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26962,"text":"wri7638 - 1976 - History of dredging and filling of lagoons in the San Juan area, Puerto Rico","interactions":[],"lastModifiedDate":"2022-01-10T20:26:23.557335","indexId":"wri7638","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-38","title":"History of dredging and filling of lagoons in the San Juan area, Puerto Rico","docAbstract":"<p>Laguna La Torrecilla, Laguna de Pinones, Laguna San Jose, and Laguna del Condado, in the San Juan, Puerto Rico area, are located within a metropolitan area of more than 1 million people. Bathymetric maps made during the study, in 1973, showed that Lagunas La Torrecilla, San Jose, and del Condado have been modified by dredging and filling; whereas, Laguna de Pinones has remained in a near natural state. Laguna La Torrecilla has been dredged to a depth, in places, of about 18 meters, and Lagunas San Jose and del Condado, in places to about 11 meters. Dredging in the San Juan lagoons has been harmful, beneficial, and in a few instances has had little or no noticeable effect on the water quality. Usually, dredging in the connecting canals has been beneficial if the water entering the lagoons through the canals was of better quality than the water in the lagoon. Dredging in the mouths of lagoons has been beneficial; whereas, filling or blocking the mouths has been harmful.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7638","usgsCitation":"Ellis, S.R., 1976, History of dredging and filling of lagoons in the San Juan area, Puerto Rico: U.S. Geological Survey Water-Resources Investigations Report 76-38, iv, 25 p., https://doi.org/10.3133/wri7638.","productDescription":"iv, 25 p.","costCenters":[],"links":[{"id":55848,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124192,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0038/report-thumb.jpg"},{"id":394128,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35054.htm"}],"country":"United States","state":"Puerto Rico","city":"San Juan","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -66.083,\n              18.417\n            ],\n            [\n              -65.95,\n              18.417\n            ],\n            [\n              -65.95,\n              18.467\n            ],\n            [\n              -66.083,\n              18.467\n            ],\n            [\n              -66.083,\n              18.417\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db68849b","contributors":{"authors":[{"text":"Ellis, S. R.","contributorId":103278,"corporation":false,"usgs":true,"family":"Ellis","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":197323,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28776,"text":"wri7610 - 1976 - Geohydrology of the Anza-Terwilliger area, Riverside County, California","interactions":[],"lastModifiedDate":"2016-09-29T15:24:02","indexId":"wri7610","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"76-10","title":"Geohydrology of the Anza-Terwilliger area, Riverside County, California","docAbstract":"<p>The Anza-Terwilliger area consists of about 96 square miles (24-9 square kilometres) in the upper parts of the Santa Margarita River and Coyote Creek drainage basins in Riverside County, Calif., about 90 miles (145 kilometres) southeast of Los Angeles. This report deals with geology, steady state and transient state of ground water, net depletion of ground water, surface-water flow, precipitation, chemistry of water, land and water use, and gravity data for the Anza-Terwilliger area. The data indicate that the rate of ground-water depletion ha's accelerated since 1950. Pumping depressions adjacent to the Cahuilla Indian Reservation have increased the hydraulic gradient and are.causing water beneath the reservation to flow toward these depressions. Total depletion of ground water since 1950 is about 14,000 acre-feet (17.3 cubic hectometres). Chemical analyses indicate that the ground water in local areas contains concentrations of nitrate above that recommended by the Environmental Protection Agency for human consumption.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/wri7610","usgsCitation":"Moyle, W.R., 1976, Geohydrology of the Anza-Terwilliger area, Riverside County, California: U.S. Geological Survey Water-Resources Investigations Report 76-10, iv, 25 p., https://doi.org/10.3133/wri7610.","productDescription":"iv, 25 p.","numberOfPages":"32","costCenters":[],"links":[{"id":159583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri7610.PNG"},{"id":329144,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1976/0010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","county":"Riverside County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.83685302734375,\n              33.456651301881855\n            ],\n            [\n              -116.83685302734375,\n              33.601466321878846\n            ],\n            [\n              -116.51550292968749,\n              33.601466321878846\n            ],\n            [\n              -116.51550292968749,\n              33.456651301881855\n            ],\n            [\n              -116.83685302734375,\n              33.456651301881855\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a89fb","contributors":{"authors":[{"text":"Moyle, W. R. Jr.","contributorId":85938,"corporation":false,"usgs":true,"family":"Moyle","given":"W.","suffix":"Jr.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48287,"text":"ofr76164 - 1976 - Flood-plain delineation for regional flood in Dane County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-09T14:23:51","indexId":"ofr76164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"76-164","title":"Flood-plain delineation for regional flood in Dane County, Wisconsin","language":"English","publisher":"U.S. Geological Society","doi":"10.3133/ofr76164","usgsCitation":"Krug, W.R., 1976, Flood-plain delineation for regional flood in Dane County, Wisconsin: U.S. Geological Survey Open-File Report 76-164, 160 leaves : ill., maps ; 61 x 92 cm., https://doi.org/10.3133/ofr76164.","productDescription":"160 leaves : ill., maps ; 61 x 92 cm.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":171041,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Dane County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-89.0094,43.286],[-89.0084,43.2555],[-89.0094,43.2],[-89.01,43.1131],[-89.0109,43.0849],[-89.0107,43.0271],[-89.0132,42.9353],[-89.013,42.8762],[-89.0119,42.8471],[-89.132,42.8479],[-89.2488,42.8478],[-89.3689,42.8484],[-89.3688,42.8575],[-89.4832,42.858],[-89.6026,42.8575],[-89.7196,42.8587],[-89.8377,42.8598],[-89.8375,42.9471],[-89.8386,43.0317],[-89.8384,43.1181],[-89.8394,43.205],[-89.8325,43.2123],[-89.825,43.2187],[-89.8175,43.226],[-89.8125,43.2342],[-89.8088,43.2369],[-89.8012,43.2365],[-89.7874,43.2356],[-89.771,43.237],[-89.7579,43.2379],[-89.7529,43.2443],[-89.7485,43.2507],[-89.7391,43.2548],[-89.7259,43.2644],[-89.7171,43.2739],[-89.714,43.2821],[-89.7165,43.2867],[-89.7235,43.2935],[-89.7209,43.2935],[-89.6008,43.2932],[-89.4819,43.2942],[-89.3617,43.2954],[-89.3624,43.2832],[-89.246,43.2834],[-89.1271,43.2827],[-89.0094,43.286]]]},\"properties\":{\"name\":\"Dane\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e6ff8","contributors":{"authors":[{"text":"Krug, William R.","contributorId":53381,"corporation":false,"usgs":true,"family":"Krug","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":237090,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69512,"text":"hu37 - 1976 - Hydrologic Unit Map-1974, State of Oregon","interactions":[],"lastModifiedDate":"2023-12-19T21:45:45.78372","indexId":"hu37","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"37","subseriesTitle":"Oregon 1974","title":"Hydrologic Unit Map-1974, State of Oregon","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu37","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map-1974, State of Oregon: U.S. Geological Survey Hydrologic Unit 37, 1 Plate: 54.96 x 42.94 inches, https://doi.org/10.3133/hu37.","productDescription":"1 Plate: 54.96 x 42.94 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,{"id":69511,"text":"hu36 - 1976 - Hydrologic Unit Map-1974, State of Oklahoma","interactions":[],"lastModifiedDate":"2023-12-19T21:40:46.479662","indexId":"hu36","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":319,"text":"Hydrologic Unit","code":"HU","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"36","subseriesTitle":"Oklahoma 1974","title":"Hydrologic Unit Map-1974, State of Oklahoma","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu36","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map-1974, State of Oklahoma: U.S. Geological Survey Hydrologic Unit 36, 1 Plate: 54.10 x 34.28 inches, https://doi.org/10.3133/hu36.","productDescription":"1 Plate: 54.10 x 34.28 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