{"pageNumber":"5352","pageRowStart":"133775","pageSize":"25","recordCount":165227,"records":[{"id":38696,"text":"pp813H - 1976 - Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","interactions":[{"subject":{"id":7852,"text":"ofr75559 - 1975 - Summary appraisals of the nation's groundwater resources: Arkansas-White-Red region","indexId":"ofr75559","publicationYear":"1975","noYear":false,"title":"Summary appraisals of the nation's groundwater resources: Arkansas-White-Red region"},"predicate":"SUPERSEDED_BY","object":{"id":38696,"text":"pp813H - 1976 - Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","indexId":"pp813H","publicationYear":"1976","noYear":false,"chapter":"H","title":"Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region"},"id":1}],"lastModifiedDate":"2021-12-14T21:16:32.492485","indexId":"pp813H","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":"H","title":"Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region","docAbstract":"<p>The Arkansas-White-Red Region, an area of265,000 square miles (6.86x10<sup>11&nbsp;</sup>square metres), is characterized by diversity in geography, climate, and geology and, in turn, by diversity in water resources and water problems. The western semiarid part of the region is water deficient, that is, potential evapotranspiration exceeds precipitation. The eastern, humid part has a surplus. Water use in the region in 1970 averaged 10 billion gallons per day (438 cubic metres per second), of which more than 65 percent was ground water. The largest use of ground water was for irrigation of crops, mostly in the water-deficient areas of Texas, Oklahoma, Kansas, and Colorado. Because of its ready availability and widespread occurrence, ground water is used throughout the region to supply municipal and rural water needs. The most productive aquifers, capable of yielding more than 50 gallons per minute (0.0032 cubic metres per second) to individual wells, are alluvium, carbonate. rocks, gypsum, and sandstone. Fresh water in storage in aquifers in the region is estimated to be 2 billion acre-feet (2.5x10<sup>12</sup> cubic metres). In addition, a large, unmeasured volume of saline water (containing more than 1,000 milligrams per litre of dissolved solids) underlies the fresh water at depths generally less than 500 feet (150 metres).</p>\n<p>The flow of water in each aquifer depends upon the physical and hydrologic characteristics of the aquifer, the climate, and the relation to, and the character of, adjacent rocks and streams. These factors also determine the effect of water-supply development or other man-induced stresses on the flow and the quality of water in the aquifers. Analog and digital models of aquifers can be used to evaluate stresses on aquifers and thereby provide water managers and planners with efficient tools for planning the development and continued use of aquifers.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp813H","usgsCitation":"Bedinger, M.S., and Sniegocki, R., 1976, Summary appraisals of the nation's ground-water resources – Arkansas-White-Red region: U.S. Geological Survey Professional Paper 813, vi, 31 p., https://doi.org/10.3133/pp813H.","productDescription":"vi, 31 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":122583,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0813h/report-thumb.jpg"},{"id":65550,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0813h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392887,"rank":3,"type":{"id":36,"text":"NGMDB 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,{"id":28108,"text":"wri7563 - 1976 - Preliminary digital model of ground-water flow in the Madison Group, Powder River Basin and adjacent areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska","interactions":[],"lastModifiedDate":"2018-03-08T13:47:25","indexId":"wri7563","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":"75-63","title":"Preliminary digital model of ground-water flow in the Madison Group, Powder River Basin and adjacent areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska","docAbstract":"A digital simulation model was used to analyze regional ground-water flow in the Madison Group aquifer in the Powder River Basin in Montana and Wyoming and adjacent areas. Most recharge to the aquifer originates in or near the outcrop areas of the Madison in the Bighorn Mountains and Black Hills, and most discharge occurs through springs and wells. Flow through the aquifer in the modeled areas was approximately 200 cubic feet per second. The aquifer can probably sustain increased ground-water withdrawals of up to several tens of cubic feet per second, but these withdrawals probably would significantly lower the potentiometric surface in the Madison aquifer in a large part of the basin. (Woodard-USGS)","language":"English","publisher":"U. S. Geological Survey","doi":"10.3133/wri7563","usgsCitation":"Konikow, L.F., 1976, Preliminary digital model of ground-water flow in the Madison Group, Powder River Basin and adjacent areas, Wyoming, Montana, South Dakota, North Dakota, and Nebraska: U.S. Geological Survey Water-Resources Investigations Report 75-63, Report: v, 44 p.; 6 Plates, https://doi.org/10.3133/wri7563.","productDescription":"Report: v, 44 p.; 6 Plates","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":56935,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56936,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56937,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":95695,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0063/report.pdf","size":"3057","linkFileType":{"id":1,"text":"pdf"}},{"id":158718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0063/report-thumb.jpg"},{"id":56932,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56933,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":56934,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1975/0063/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4b1","contributors":{"authors":[{"text":"Konikow, Leonard F. 0000-0002-0940-3856 lkonikow@usgs.gov","orcid":"https://orcid.org/0000-0002-0940-3856","contributorId":158,"corporation":false,"usgs":true,"family":"Konikow","given":"Leonard","email":"lkonikow@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":199232,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47087,"text":"ofr76297 - 1976 - Field compilation map of the geology of the Keystone area, Black Hills, South Dakota","interactions":[],"lastModifiedDate":"2012-09-05T01:01:46","indexId":"ofr76297","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":"76-297","title":"Field compilation map of the geology of the Keystone area, Black Hills, South Dakota","language":"English","doi":"10.3133/ofr76297","usgsCitation":"Norton, J.J., 1976, Field compilation map of the geology of the Keystone area, Black Hills, South Dakota: U.S. Geological Survey Open-File Report 76-297, 1 Map: 92 x 100 cm., https://doi.org/10.3133/ofr76297.","productDescription":"1 Map: 92 x 100 cm.","costCenters":[],"links":[{"id":135582,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84115,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0297/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","datum":"Mean Sea Level","country":"United States","state":"South Dakota","otherGeospatial":"Black Hills;Keystone;Mount Rushmore","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.5,43.833333333333336 ], [ -103.5,44 ], [ -103.33333333333333,44 ], [ -103.33333333333333,43.833333333333336 ], [ -103.5,43.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f5aa6","contributors":{"authors":[{"text":"Norton, James Jennings","contributorId":59412,"corporation":false,"usgs":true,"family":"Norton","given":"James","email":"","middleInitial":"Jennings","affiliations":[],"preferred":false,"id":234609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42147,"text":"ofr76364 - 1976 - Aeromagnetic map for parts of Caliente and Lund 1° by 2° quadrangles, Nevada","interactions":[],"lastModifiedDate":"2021-10-01T18:57:00.733119","indexId":"ofr76364","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":"76-364","title":"Aeromagnetic map for parts of Caliente and Lund 1° by 2° quadrangles, Nevada","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76364","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Aeromagnetic map for parts of Caliente and Lund 1° by 2° quadrangles, Nevada: U.S. Geological Survey Open-File Report 76-364, 1 Plate: 32.00 × 52.00 inches, https://doi.org/10.3133/ofr76364.","productDescription":"1 Plate: 32.00 × 52.00 inches","costCenters":[],"links":[{"id":175315,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":390141,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15315.htm"},{"id":98804,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1976/0364/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","country":"United States","state":"Nevada","otherGeospatial":"Caliente and Lund 1° by 2° quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115,\n              37.0\n            ],\n            [\n              -116,\n              37.0\n            ],\n            [\n              -116,\n              38.25\n            ],\n            [\n              -115,\n              38.25\n            ],\n            [\n              -115,\n              37.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69839f","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":530864,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34421,"text":"b1405D - 1976 - Stratigraphy of the layered gabbroic Dufek Intrusion, Antarctica","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1405D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1405","chapter":"D","title":"Stratigraphy of the layered gabbroic Dufek Intrusion, Antarctica","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1405D","usgsCitation":"Ford, A., 1976, Stratigraphy of the layered gabbroic Dufek Intrusion, Antarctica: U.S. Geological Survey Bulletin 1405, iv, p. D1-D36, ill. ;24 cm., https://doi.org/10.3133/b1405D.","productDescription":"iv, p. D1-D36, ill. ;24 cm.","costCenters":[],"links":[{"id":163056,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1405d/report-thumb.jpg"},{"id":62360,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1405d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699e7e","contributors":{"authors":[{"text":"Ford, Arthur B.","contributorId":52578,"corporation":false,"usgs":true,"family":"Ford","given":"Arthur B.","affiliations":[],"preferred":false,"id":212947,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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 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,{"id":10378,"text":"ofr76808 - 1976 - Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:06:20","indexId":"ofr76808","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":"76-808","title":"Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington","docAbstract":"On the Yakima Indian Reservation, Washington, only about 5 percent of the Satus Creek basin--in the relatively flat eastern lowland adjacent to and including part of the Yakima River lowland--is agriculturally developed, mostly through irrigation. Because the basin 's streams do not contain adequate water for irrigation, most irrigation is by canal diversion from the adjoining Toppenish Creek basin. Irrigation application of as much as 9.25 acre-feet per acre per year, combined with the presence of poorly drained silt and clay layers in this area, and the natural upward discharge of ground water from deeper aquifers (water-bearing layers), has contributed to a waterlogging problem, which has affected about 10,500 acres, or about 25 percent of the irrigated area. In the upland of the basin, a large average annual base flow of about 30 cubic feet per second in Logy Creek indicates the presence of a potentially highly productive aquifer in young (shallow) basalt lavas underlying the higher western parts of the upland. This aquifer may provide a reservoir from which streamflow may be augmented by ground-water pumping or, alternatively, it may be used as a source of ground water for irrigation of upland areas directly. (Woodard-USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76808","usgsCitation":"Molenaar, D., 1976, Outline of the water resources of the Status Creek basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Open-File Report 76-808, ix, 31 leaves :ill., maps(2 fold.) ;27 cm., https://doi.org/10.3133/ofr76808.","productDescription":"ix, 31 leaves :ill., maps(2 fold.) ;27 cm.","costCenters":[],"links":[{"id":142299,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a33d","contributors":{"authors":[{"text":"Molenaar, Dee","contributorId":34485,"corporation":false,"usgs":true,"family":"Molenaar","given":"Dee","email":"","affiliations":[],"preferred":false,"id":161284,"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":10710,"text":"ofr76601 - 1976 - Principal facts for gravity observations in the Charles Sheldon Antelope Range, Nevada-Oregon","interactions":[],"lastModifiedDate":"2012-02-02T00:06:25","indexId":"ofr76601","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":"76-601","title":"Principal facts for gravity observations in the Charles Sheldon Antelope Range, Nevada-Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr76601","usgsCitation":"Plouff, D., Robbins, S.L., and Holden, K.D., 1976, Principal facts for gravity observations in the Charles Sheldon Antelope Range, Nevada-Oregon: U.S. Geological Survey Open-File Report 76-601, 22 leaves :ill., map ;28 cm., https://doi.org/10.3133/ofr76601.","productDescription":"22 leaves :ill., map ;28 cm.","costCenters":[],"links":[{"id":143284,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a10f","contributors":{"authors":[{"text":"Plouff, Donald","contributorId":94657,"corporation":false,"usgs":true,"family":"Plouff","given":"Donald","email":"","affiliations":[],"preferred":false,"id":161837,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robbins, S. L.","contributorId":49766,"corporation":false,"usgs":true,"family":"Robbins","given":"S.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":161836,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holden, K. D.","contributorId":30597,"corporation":false,"usgs":true,"family":"Holden","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":161835,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":69547,"text":"hu43 - 1976 - Hydrologic Unit Map-1974, State of Texas","interactions":[],"lastModifiedDate":"2023-12-19T22:02:51.432454","indexId":"hu43","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":"43","subseriesTitle":"Texas 1974","title":"Hydrologic Unit Map-1974, State of Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu43","isbn":"607768002","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map-1974, State of Texas: U.S. Geological Survey Hydrologic Unit 43, 4 Plates: 52.51 x 41.44 inches or smaller, https://doi.org/10.3133/hu43.","productDescription":"4 Plates: 52.51 x 41.44 inches or 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,{"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":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":48296,"text":"ofr76300H - 1976 - Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1976","interactions":[],"lastModifiedDate":"2024-04-08T21:57:45.565626","indexId":"ofr76300H","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":"76-300","chapter":"H","title":"Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1976","docAbstract":"<p><span>The preliminary geomagnetic data included here is made available to scientific personnel and organizations, as part of a cooperative effort and on a data exchange basis because of the early need by some users. To avoid delay, all of the data is copied from original forms processed at the observatory; therefore it should be regarded as preliminary.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr76300H","usgsCitation":"Townshend, J., Papp, J., Moorman, M., Deadmon, C., and Tilton, S., 1976, Preliminary geomagnetic data, College Observatory, Fairbanks, Alaska: August 1976: U.S. Geological Survey Open-File Report 76-300, 23 p., https://doi.org/10.3133/ofr76300H.","productDescription":"23 p.","costCenters":[],"links":[{"id":427563,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1976/0300-h/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":171155,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1976/0300-h/report-thumb.jpg"}],"country":"United States","state":"Alaska","city":"Fairbanks","otherGeospatial":"College Observatory","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -148.0653003052681,\n              64.95550985834566\n            ],\n            [\n              -148.0653003052681,\n              64.8015944335609\n            ],\n            [\n              -147.35118897714307,\n              64.8015944335609\n            ],\n            [\n              -147.35118897714307,\n              64.95550985834566\n            ],\n            [\n              -148.0653003052681,\n              64.95550985834566\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abce4b07f02db673785","contributors":{"authors":[{"text":"Townshend, J.B.","contributorId":30623,"corporation":false,"usgs":true,"family":"Townshend","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":237130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Papp, J.E.","contributorId":95057,"corporation":false,"usgs":true,"family":"Papp","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":237131,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moorman, M.J.","contributorId":12084,"corporation":false,"usgs":true,"family":"Moorman","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":237127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Deadmon, C.E.","contributorId":17672,"corporation":false,"usgs":true,"family":"Deadmon","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":237129,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Tilton, S.P.","contributorId":15670,"corporation":false,"usgs":true,"family":"Tilton","given":"S.P.","email":"","affiliations":[],"preferred":false,"id":237128,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":28718,"text":"wri7557 - 1976 - Hydrologic effects of storms of June 24-28, 1974, in Lee and Collier Counties, Florida","interactions":[],"lastModifiedDate":"2019-07-16T09:12:37","indexId":"wri7557","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":"75-57","title":"Hydrologic effects of storms of June 24-28, 1974, in Lee and Collier Counties, Florida","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7557","usgsCitation":"Miller, R.A., and Benson, M.A., 1976, Hydrologic effects of storms of June 24-28, 1974, in Lee and Collier Counties, Florida: U.S. Geological Survey Water-Resources Investigations Report 75-57, v, 30 p. , https://doi.org/10.3133/wri7557.","productDescription":"v, 30 p. ","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":159405,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0057/report-thumb.jpg"},{"id":365569,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Collier County, Lee County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.452392578125,\n              25.61676284310854\n            ],\n            [\n              -80.82092285156249,\n              25.61676284310854\n            ],\n            [\n              -80.82092285156249,\n              27.147144835991796\n            ],\n            [\n              -82.452392578125,\n              27.147144835991796\n            ],\n            [\n              -82.452392578125,\n              25.61676284310854\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606f2c","contributors":{"authors":[{"text":"Miller, Robert A.","contributorId":52938,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200283,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Benson, Manuel A.","contributorId":41405,"corporation":false,"usgs":true,"family":"Benson","given":"Manuel","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200282,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66817,"text":"i829C - 1976 - Map showing ground water conditions in the Fairbanks D-2 SW Quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:20","indexId":"i829C","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":"829","subseriesTitle":"NONE","chapter":"C","title":"Map showing ground water conditions in the Fairbanks D-2 SW Quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/i829C","usgsCitation":"Pewe, T.L., and Bell, J.W., 1976, Map showing ground water conditions in the Fairbanks D-2 SW Quadrangle, Alaska: U.S. Geological Survey IMAP 829, 1 map :col. ;58 x 49 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/i829C.","productDescription":"1 map :col. ;58 x 49 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":106997,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9657.htm","linkFileType":{"id":5,"text":"html"},"description":"9657"},{"id":188321,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -148,64.75 ], [ -148,64.86749999999999 ], [ -147.75,64.86749999999999 ], [ -147.75,64.75 ], [ -148,64.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d2a","contributors":{"authors":[{"text":"Pewe, T. L.","contributorId":35786,"corporation":false,"usgs":true,"family":"Pewe","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":275130,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bell, J. W.","contributorId":54288,"corporation":false,"usgs":true,"family":"Bell","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":275131,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":69515,"text":"hu47 - 1976 - Hydrologic Unit Map-1974, State of Washington","interactions":[],"lastModifiedDate":"2023-12-19T22:16:34.887928","indexId":"hu47","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":"47","subseriesTitle":"Washington 1974","title":"Hydrologic Unit Map-1974, State of Washington","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu47","isbn":"607768037","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map-1974, State of Washington: U.S. Geological Survey Hydrologic Unit 47, 1 Plate: 50.65 x 37.59 inches, https://doi.org/10.3133/hu47.","productDescription":"1 Plate: 50.65 x 37.59 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,{"id":68581,"text":"ha578 - 1976 - Teton Dam flood of June 1976, Rose quadrangle, Idaho","interactions":[],"lastModifiedDate":"2013-11-12T14:30:48","indexId":"ha578","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"578","title":"Teton Dam flood of June 1976, Rose quadrangle, Idaho","docAbstract":"The failure of the Teton Dam caused extreme flooding along the Teton River, Henrys Fork, and Snake River in southeastern Idaho on June 5-8, 1976. No flooding occurred downstream from American Falls Reservoir. The inundated areas and maximum water-surface elevations are shown in a series of 17 hydrologic atlases. The area covered by the atlases extends from Teton Dam downstream to American Falls Reservoir, a distance of 100 miles. The extent of flooding shown on the maps was obtained by field inspections and aerial photographs made during and immediately after the flood. There may be small isolated areas within the boundaries shown that were not flooded, but the identification of these sites was beyond the scope of the study. The elevation data shown are mean-sea-level elevations of high-water marks identified in the field. This particular map (in the 17-map series) shows conditions in the Rose quadrangle. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha578","usgsCitation":"Bartells, J.H., and Hubbard, L.L., 1976, Teton Dam flood of June 1976, Rose quadrangle, Idaho: U.S. Geological Survey Hydrologic Atlas 578, 1 Plate: 21.00 x 27.00 inches, https://doi.org/10.3133/ha578.","productDescription":"1 Plate: 21.00 x 27.00 inches","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":190098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90219,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/578/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","projection":"Polyconic projection","datum":"1927 North American Datum","country":"United States","state":"Idaho","otherGeospatial":"Rose Quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.375,43.25 ], [ -112.375,43.375 ], [ -112.25,43.375 ], [ -112.25,43.25 ], [ -112.375,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683e11","contributors":{"authors":[{"text":"Bartells, John H.","contributorId":54240,"corporation":false,"usgs":true,"family":"Bartells","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278510,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hubbard, Larry L.","contributorId":91492,"corporation":false,"usgs":true,"family":"Hubbard","given":"Larry","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":278511,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26658,"text":"wri7683 - 1976 - Measured and simulated ground-water levels in the Franklin area, southeastern Virginia","interactions":[],"lastModifiedDate":"2019-07-17T09:48:49","indexId":"wri7683","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":"76-83","title":"Measured and simulated ground-water levels in the Franklin area, southeastern Virginia","docAbstract":"The Lower Cretaceous aquifer is the principal source of water in Southeastern Virginia. Synoptic water-level measurements made since 1970 have been used to verify a digital model of the aquifer. Measurements made in December 1973, August and December 1974 were used to further verify the model, using updated pumpage for those periods. The close agreement of the potentiometric maps based on measured and simulated water levels indicates that the model is simulating hydrologic conditions satisfactorily. (Woodard-USGS)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri7683","usgsCitation":"Cosner, O.J., 1976, Measured and simulated ground-water levels in the Franklin area, southeastern Virginia: U.S. Geological Survey Water-Resources Investigations Report 76-83, 5 Plates: 34.04 x 22.01 inches, https://doi.org/10.3133/wri7683.","productDescription":"5 Plates: 34.04 x 22.01 inches","costCenters":[],"links":[{"id":365655,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365654,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365656,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365657,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":365658,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1976/0083/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158210,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1976/0083/report-thumb.jpg"}],"country":"United States","state":"Virginia","city":"Franklin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.0306396484375,\n              36.608913667193676\n            ],\n            [\n              -76.7889404296875,\n              36.608913667193676\n            ],\n            [\n              -76.7889404296875,\n              36.71466899719828\n            ],\n            [\n              -77.0306396484375,\n              36.71466899719828\n            ],\n            [\n              -77.0306396484375,\n              36.608913667193676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db61081f","contributors":{"authors":[{"text":"Cosner, O. J.","contributorId":19587,"corporation":false,"usgs":true,"family":"Cosner","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":196789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34486,"text":"b1419 - 1976 - Annotated bibliography of the geology of selenium, 1958-74","interactions":[],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"b1419","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1419","title":"Annotated bibliography of the geology of selenium, 1958-74","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1419","usgsCitation":"Gent, C.A., 1976, Annotated bibliography of the geology of selenium, 1958-74: U.S. Geological Survey Bulletin 1419, 49 p. ;23 cm., https://doi.org/10.3133/b1419.","productDescription":"49 p. ;23 cm.","costCenters":[],"links":[{"id":96440,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1419/report.pdf","size":"3525","linkFileType":{"id":1,"text":"pdf"}},{"id":164166,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1419/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67be91","contributors":{"authors":[{"text":"Gent, Carol A.","contributorId":40646,"corporation":false,"usgs":true,"family":"Gent","given":"Carol","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":213038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14053,"text":"ofr7657 - 1976 - Principal facts for gravity stations in the western part of the Goldfield 2 degrees sheet, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:51","indexId":"ofr7657","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":"76-57","title":"Principal facts for gravity stations in the western part of the Goldfield 2 degrees sheet, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr7657","usgsCitation":"Healey, D., 1976, Principal facts for gravity stations in the western part of the Goldfield 2 degrees sheet, Nevada: U.S. Geological Survey Open-File Report 76-57, 15 p. :map ;27 cm., https://doi.org/10.3133/ofr7657.","productDescription":"15 p. :map ;27 cm.","costCenters":[],"links":[{"id":147247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6677fa","contributors":{"authors":[{"text":"Healey, D.L.","contributorId":52964,"corporation":false,"usgs":true,"family":"Healey","given":"D.L.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":168854,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":69514,"text":"hu42 - 1976 - Hydrologic Unit Map-1974, State of Tennessee","interactions":[],"lastModifiedDate":"2023-12-19T21:50:22.175556","indexId":"hu42","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":"42","subseriesTitle":"Tennessee 1974","title":"Hydrologic Unit Map-1974, State of Tennessee","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/hu42","isbn":"607767995","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1976, Hydrologic Unit Map-1974, State of Tennessee: U.S. Geological Survey Hydrologic Unit 42, 1 Plate: 64.32 x 20.20 inches, https://doi.org/10.3133/hu42.","productDescription":"1 Plate: 64.32 x 20.20 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,{"id":26944,"text":"wri769 - 1976 - A technique for estimating the time of travel of water in Indiana streams","interactions":[],"lastModifiedDate":"2016-05-16T10:23:38","indexId":"wri769","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":"76-9","title":"A technique for estimating the time of travel of water in Indiana streams","docAbstract":"<p>Estimates of the traveltime of waterborne particles in streams is important for pollution studies and in the event of spills of contaminants. This report provides data for the 16 Indiana streams on which time-of-travel information has been obtained and a means for estimating the velocity of any naturally flowing stream in Indiana with a drainage area of 80 square miles (210 square kilometres) or more.</p>\n<p>Measured velocity rates compiled from the time-of-travel data collected in Indiana are releated to 25, 50, 100, and 200 percent of the average discharge of streams shown in this report. Velocities at these discharges are significantly related to their respective watershed characteristics (average discharge and slope). Generalized relations of the velocities as functions of the streams' watershed characteristics are developed as multivariate regression equations using the data from each of the measured streams.</p>\n<p>Examples of uses and applications of the measured data and the predictive equations are given.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri769","collaboration":"Prepared in cooperation with Indiana Department of Natural Resources and Indiana State Board of Health","usgsCitation":"Eikenberry, S.E., and Davis, L.G., 1976, A technique for estimating the time of travel of water in Indiana streams: U.S. Geological Survey Water-Resources Investigations Report 76-9, vi, 39 p., https://doi.org/10.3133/wri769.","productDescription":"vi, 39 p.","startPage":"1","endPage":"39","numberOfPages":"48","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science 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