{"pageNumber":"5359","pageRowStart":"133950","pageSize":"25","recordCount":165623,"records":[{"id":70157469,"text":"70157469 - 1976 - Ground-water resources and geology of St. Croix County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:36:02","indexId":"70157469","displayToPublicDate":"2015-02-09T08:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"32","title":"Ground-water resources and geology of St. Croix County, Wisconsin","docAbstract":"<p>The increasing need for good-quality ground water in St. Croix County, caused by a steadily increasing population, can be met from the sand-and-gravel and sandstone aquifers. As much as 15 gallons per minute (0.95 litres per second) can be obtained from wells almost everywhere in the county. Yields of more than 1,000 gallons per minute (63 litres per second) are available from glacial deposits and alluvium where there is sufficient thickness of saturated sand and gravel. The sandstone aquifer underlies the entire county and is more than 1,000 feet (300 metres) thick in the southwest near River Falls. In St. Croix County the sandstone aquifer is all bedrock younger than Precambrian age and includes, in ascending order, from oldest to youngest, sandstones of Cambrian age (in ascending order, the Mount Simon, Eau Claire, Galesville, and Franconia Sandstones, and the Trempealeau Formation); and the Prairie du Chien Group, St. Peter Sandstone, and Galena-Platteville unit (Platteville and Decorah Formations and Galena Dolomite, undifferentiated), all of Ordovician age. This aquifer is capable of yielding more than 1,000 gallons per minute (63 litres per second) to wells in much of the county and is the principal source of municipal water.</p>\n<p>The chemical quality of water from the two aquifers is similar. The water from both aquifers is hard to very hard, having a median hardness between 180 and 190 milligrams per litre. Iron and manganese are locally present in botherSome amounts (combined total exceeding 0.3 milligrams per litre). Nitrate is a minor problem in both aquifers, with median concentrations more than 10 milligrams per litre, possibly indicating some contamination of ground water by organic matter.</p>\n<p>About 3.83 million gallons per day (0.168 cubic metres per second) of ground water was pumped in the county in 1974, of which 94 percent was from the sandstone aquifer. About 44 percent of the total water pumped was for industrial and commercial use, 42 percent for residential</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Borman, R.G., 1976, Ground-water resources and geology of St. Croix County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 32, vii, 30.","productDescription":"vii, 30","numberOfPages":"38","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308480,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350392,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic32/"}],"country":"United States","state":"Wisconsin","county":"St. Croix County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-92.1564,45.2097],[-92.1568,45.1215],[-92.136,45.121],[-92.1364,45.0315],[-92.1356,44.9447],[-92.1367,44.8579],[-92.2584,44.8582],[-92.3752,44.8622],[-92.4969,44.8622],[-92.6193,44.8626],[-92.7411,44.862],[-92.7644,44.8622],[-92.7637,44.8647],[-92.763,44.8671],[-92.7628,44.8716],[-92.7632,44.8753],[-92.7632,44.8759],[-92.7654,44.8795],[-92.7685,44.8842],[-92.7689,44.8848],[-92.7698,44.8865],[-92.7721,44.8905],[-92.7738,44.8933],[-92.7743,44.895],[-92.775,44.8982],[-92.7729,44.901],[-92.7707,44.9023],[-92.7677,44.9036],[-92.767,44.9039],[-92.7645,44.9046],[-92.7606,44.9068],[-92.7569,44.9105],[-92.7547,44.9159],[-92.7534,44.9237],[-92.753,44.9362],[-92.753,44.9369],[-92.7523,44.9481],[-92.7526,44.9522],[-92.7527,44.9527],[-92.7547,44.9571],[-92.7593,44.9639],[-92.7643,44.9707],[-92.7646,44.9711],[-92.7652,44.9723],[-92.7672,44.9765],[-92.7686,44.9796],[-92.7688,44.9817],[-92.7694,44.9909],[-92.7683,44.9997],[-92.7682,45.0005],[-92.7677,45.0023],[-92.7657,45.0108],[-92.7639,45.0196],[-92.7639,45.0237],[-92.7645,45.0265],[-92.7664,45.0292],[-92.7683,45.0325],[-92.7707,45.0344],[-92.7741,45.037],[-92.7745,45.0373],[-92.7793,45.0397],[-92.7837,45.0421],[-92.7881,45.0453],[-92.7926,45.0481],[-92.7952,45.0499],[-92.7984,45.0531],[-92.8005,45.0567],[-92.8016,45.0597],[-92.8018,45.0634],[-92.8019,45.0647],[-92.8015,45.0668],[-92.8008,45.07],[-92.8001,45.0723],[-92.7982,45.0746],[-92.7955,45.0768],[-92.795,45.0772],[-92.7917,45.0791],[-92.7885,45.0806],[-92.7871,45.0815],[-92.7847,45.083],[-92.7803,45.0849],[-92.7743,45.0889],[-92.7689,45.0927],[-92.7624,45.0972],[-92.7596,45.0995],[-92.7591,45.0999],[-92.7548,45.1026],[-92.7513,45.1045],[-92.7472,45.1073],[-92.7467,45.1076],[-92.7446,45.11],[-92.7433,45.112],[-92.7422,45.1135],[-92.7415,45.1172],[-92.7426,45.121],[-92.7441,45.1264],[-92.7459,45.1309],[-92.7484,45.1373],[-92.749,45.1419],[-92.7489,45.1446],[-92.7484,45.1483],[-92.7473,45.1515],[-92.7475,45.1551],[-92.7483,45.1597],[-92.7472,45.1634],[-92.7475,45.1668],[-92.748,45.1698],[-92.7493,45.173],[-92.7522,45.1759],[-92.7557,45.178],[-92.7589,45.1812],[-92.7622,45.1847],[-92.7629,45.1853],[-92.764,45.1895],[-92.7637,45.1972],[-92.7632,45.2009],[-92.7619,45.2041],[-92.7603,45.2065],[-92.76,45.2069],[-92.7579,45.2097],[-92.6517,45.21],[-92.53,45.21],[-92.4063,45.2091],[-92.2839,45.2094],[-92.1564,45.2097]]]},\"properties\":{\"name\":\"Saint Croix\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d7","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","interactions":[{"subject":{"id":42244,"text":"ofr76463 - 1976 - Bedrock topography map of Walworth County, Wisconsin","indexId":"ofr76463","publicationYear":"1976","noYear":false,"title":"Bedrock topography map of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":1},{"subject":{"id":42264,"text":"ofr76462 - 1976 - Bedrock geology map of Walworth County, Wisconsin","indexId":"ofr76462","publicationYear":"1976","noYear":false,"title":"Bedrock geology map of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":2},{"subject":{"id":44023,"text":"ofr76464 - 1976 - Water-table map of Walworth County, Wisconsin, 1973","indexId":"ofr76464","publicationYear":"1976","noYear":false,"title":"Water-table map of Walworth County, Wisconsin, 1973"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":3},{"subject":{"id":46009,"text":"ofr76465 - 1976 - Map showing thickness of unconsolidated materials of Walworth County, Wisconsin","indexId":"ofr76465","publicationYear":"1976","noYear":false,"title":"Map showing thickness of unconsolidated materials of Walworth County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":70047687,"text":"70047687 - 1976 - Ground-water resources and geology of Walworth County, Wisconsin","indexId":"70047687","publicationYear":"1976","noYear":false,"title":"Ground-water resources and geology of Walworth County, Wisconsin"},"id":4}],"lastModifiedDate":"2018-01-08T19:59:35","indexId":"70047687","displayToPublicDate":"2013-01-01T13:21:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"34","title":"Ground-water resources and geology of Walworth County, Wisconsin","docAbstract":"Population growth in Walworth County, Wisconsin, requires an increasing amount of ground water. Good quality water is available from the sand-and gravel, Niagara, Galena-Platteville, and sandstone aquifers in the county. As much as 15 gallons per minute (0.95 liters per second) can be obtained from individual wells almost everywhere in the county. Well yields of 1,000 gallons per minute (63 liters per second) are available from glacial drift where it contains sufficient thickness of saturated sand and gravel. The sand-and-gravel aquifer is an important source of municipal water. Estimated well yields from most of the Niagara aquifer, a Silurian age dolomite as thick as 125 feet (38.1 meters), exceed 100 gallons per minute (6.3 liters per second). The Niagara aquifer occurs in the eastern third of the county. The Galena-Platteville aquifer, chiefly dolomite, is present in the western half of the county where it is as thick as 325 feet (99.1 meters). Estimated yields from this aquifer exceed 500 gallons per minute (32 liters per second). The sandstone aquifer underlies the entire county and ranges from less than 800 feet (240 meters) thick in the northwest corner to more than 2,200 feet (670 meters) in the east. This aquifer is capable of yielding 1,000 gallons per minute (63 liters per second) to individual wells and is a principal source of municipal water.","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","collaboration":"Prepared by United States Department of the Interior Geological Survey in cooperation with Wisconsin Geological and Natural History Survey","usgsCitation":"Borman, R.G., 1976, Ground-water resources and geology of Walworth County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 34, vii, 45 p.","productDescription":"vii, 45 p.","numberOfPages":"54","costCenters":[],"links":[{"id":276760,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047687.JPG"},{"id":276759,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/ic34/"}],"country":"United States","state":"Wisconsin","county":"Walworth County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.776008,42.492041 ], [ -88.776008,42.84625 ], [ -88.301522,42.84625 ], [ -88.301522,42.492041 ], [ -88.776008,42.492041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52136e34e4b0b08f446198e6","contributors":{"authors":[{"text":"Borman, Ronald G.","contributorId":69944,"corporation":false,"usgs":true,"family":"Borman","given":"Ronald","email":"","middleInitial":"G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":482722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","interactions":[{"subject":{"id":52599,"text":"ofr67127 - 1967 - Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania","indexId":"ofr67127","publicationYear":"1967","noYear":false,"title":"Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","indexId":"70047436","publicationYear":"1976","noYear":false,"title":"Geology and ground-water resources of northern Mercer County, Pennsylvania"},"id":1},{"subject":{"id":55850,"text":"ofr68158 - 1968 - Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania","indexId":"ofr68158","publicationYear":"1968","noYear":false,"title":"Progress report on the ground-water conditions of the Shenango and Stoneboro 15-minute quadrangles, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047436,"text":"70047436 - 1976 - Geology and ground-water resources of northern Mercer County, Pennsylvania","indexId":"70047436","publicationYear":"1976","noYear":false,"title":"Geology and ground-water resources of northern Mercer County, Pennsylvania"},"id":2}],"lastModifiedDate":"2013-08-06T15:25:36","indexId":"70047436","displayToPublicDate":"2013-01-01T09:18:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Geology and ground-water resources of northern Mercer County, Pennsylvania","docAbstract":"The Shenango and Stoneboro 15-minute quadrangles are in northwestern Pennsylvania and are about 60 miles north of Pitts burgh. These two quadrangles comprise the following 7%-minute quadrangles: Greenville West, Greenville East, Sharpsville, Fredonia, Hadley, New Lebanon, Jackson Center, and Sandy Lake. The area covered by the two quadrangles includes the northern two thirds of Mercer County and a small amount of adjoining southern Crawford County.","language":"English","publisher":"Pennsylvania Bureau of Topographic and Geologic Survey","collaboration":"Prepared by the U. S. Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Schiner, G., and Kimmel, G., 1976, Geology and ground-water resources of northern Mercer County, Pennsylvania: Water Resource Report 33, 136 p.; Maps: 2 Sheets.","productDescription":"136 p.; Maps: 2 Sheets","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276094,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047436.PNG"},{"id":276093,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016321.zip"}],"country":"United States","state":"Pennsylvania","county":"Mercer County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.518715,41.069935 ], [ -80.518715,41.490429 ], [ -79.998161,41.490429 ], [ -79.998161,41.069935 ], [ -80.518715,41.069935 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae3e4b0e21cafa49c47","contributors":{"authors":[{"text":"Schiner, G. R.","contributorId":85175,"corporation":false,"usgs":true,"family":"Schiner","given":"G. R.","affiliations":[],"preferred":false,"id":482040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kimmel, G.E.","contributorId":23976,"corporation":false,"usgs":true,"family":"Kimmel","given":"G.E.","email":"","affiliations":[],"preferred":false,"id":482039,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046298,"text":"70046298 - 1976 - Bouguer gravity map of California, San Jose","interactions":[{"subject":{"id":41091,"text":"ofr74184 - 1974 - Preliminary Bouguer gravity map of the San Jose 1 degree by 2 degrees Quadrangle, California","indexId":"ofr74184","publicationYear":"1974","noYear":false,"title":"Preliminary Bouguer gravity map of the San Jose 1 degree by 2 degrees Quadrangle, California"},"predicate":"SUPERSEDED_BY","object":{"id":70046298,"text":"70046298 - 1976 - Bouguer gravity map of California, San Jose","indexId":"70046298","publicationYear":"1976","noYear":false,"title":"Bouguer gravity map of California, San Jose"},"id":1}],"lastModifiedDate":"2013-06-05T14:22:21","indexId":"70046298","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"title":"Bouguer gravity map of California, San Jose","language":"English","publisher":"California Division of Mines and Geology","publisherLocation":"Sacramento, CA","usgsCitation":"Robbins, S.L., Oliver, H., and Holden, K.D., 1976, Bouguer gravity map of California, San Jose, Map: 1 Sheet.","productDescription":"Map: 1 Sheet","costCenters":[],"links":[{"id":273327,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"San Jose","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.045672,37.124493 ], [ -122.045672,37.469538 ], [ -121.589154,37.469538 ], [ -121.589154,37.124493 ], [ -122.045672,37.124493 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b05de2e4b030b5198011ce","contributors":{"authors":[{"text":"Robbins, Stephen L.","contributorId":68291,"corporation":false,"usgs":true,"family":"Robbins","given":"Stephen","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":479414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oliver, Howard W.","contributorId":78704,"corporation":false,"usgs":true,"family":"Oliver","given":"Howard W.","affiliations":[],"preferred":false,"id":479415,"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":479413,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042949,"text":"70042949 - 1976 - A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","interactions":[{"subject":{"id":13783,"text":"ofr72129 - 1972 - Genesis of oil in metalliferous veins, San Juan Mountains, Colorado","indexId":"ofr72129","publicationYear":"1972","noYear":false,"title":"Genesis of oil in metalliferous veins, San Juan Mountains, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042949,"text":"70042949 - 1976 - A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","indexId":"70042949","publicationYear":"1976","noYear":false,"title":"A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado"},"id":1}],"lastModifiedDate":"2015-08-25T14:23:55","indexId":"70042949","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado","docAbstract":"<p>A tarry, benzene-soluble material is present in metal-rich veins in the Idarado mine, Ouray County, Colo., in an area not known to have petroleum resources. The material was compared chemically, spectometrically, and chromatographically with oils from four fields in the nearby Paradox basin. Each of these oil fields contains reservoir rocks equivalent to rock units known to extend beneath volcanic rocks near the mine. Carbon and sulfur isotope data and gas chromatographic data indicate a similarity between the oil from the nearby Sierra field and the oil from the mine. Thus, it seems both geologically and chemically possible that oil in the mine originated in Cretaceous sediments. Variations in the composition of oil from the mine and differences between the mine oil and Sierra oil, notably in the distributions of hydrocarbons, are attributed to bacterial degradation.</p>","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Journal of Research of the U.S. Geological Survey","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Gerrild, P.M., 1976, A geochemical study of oil in metalliferous veins, Idarado Mine, San Juan Mountains, Colorado: Journal of Research of the U.S. Geological Survey, v. 4, no. 5, p. 593-599.","productDescription":"7 p.","startPage":"593","endPage":"599","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266702,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266701,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue5/report.pdf"}],"country":"United States","state":"Colorado","county":"Ouray County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.1,\n              36.8\n            ],\n            [\n              -109.1,\n              39\n            ],\n            [\n              -106,\n              39\n            ],\n            [\n              -106,\n              36.8\n            ],\n            [\n              -109.1,\n              36.8\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"4","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd70e4b0d965cd9f22e0","contributors":{"authors":[{"text":"Gerrild, Peter M.","contributorId":37340,"corporation":false,"usgs":true,"family":"Gerrild","given":"Peter","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472654,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043279,"text":"70043279 - 1976 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","interactions":[{"subject":{"id":13217,"text":"ofr75215 - 1975 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal Systems, Duchesne County, Utah","indexId":"ofr75215","publicationYear":"1975","noYear":false,"title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal Systems, Duchesne County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043279,"text":"70043279 - 1976 - Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","indexId":"70043279","publicationYear":"1976","noYear":false,"title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah"},"id":1}],"lastModifiedDate":"2016-12-12T13:36:59","indexId":"70043279","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"50","title":"Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah","docAbstract":"This report describes the study of the Rocky Point Canal system in the vicinity of Duchesne and the Grey Mountain-Pleasant Valley Canal system between Duchesne and Myton, in the Uinta Basin, Duchesne County, Utah. The Rocky Point Canal diverts from the left bank of the Duchesne River about 4 mi north of Duchesne. This canal splits into the upper Rocky Point Canal and the lower Rocky Point Canal about 5.2 mi below its head. The Grey Mountain Canal diverts from the right bank of the Duchesne River about 6 mi east of Duchesne. At a point about 7.6 mi below the head, the Pleasant Valley Canal diverts from the right bank of the Grey Mountain Canal.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United State Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cruff, R., and Hood, J.W., 1976, Seepage study of the Rocky Point Canal and the Grey Mountain-Pleasant Valley Canal systems, Duchesne County, Utah: Technical Publication 50, vi, 53 p.","productDescription":"vi, 53 p.","numberOfPages":"64","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":267164,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331874,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-280"},{"id":331875,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009c.pdf"}],"country":"United States","state":"Utah","county":"Duchesne County","otherGeospatial":"Grey Mountain-Pleasant Valley Canal System, Rocky Point Canal","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-109.9746,40.8065],[-109.9747,40.8038],[-109.9725,40.6903],[-109.9742,40.6087],[-109.9741,40.547],[-109.9737,40.4757],[-109.9737,40.4109],[-109.9742,40.3964],[-109.974,40.3819],[-109.9738,40.346],[-109.9744,40.2589],[-109.9748,40.2444],[-109.9747,40.2295],[-109.9748,40.1832],[-109.9746,40.1673],[-109.9752,40.1469],[-109.9753,40.1419],[-109.9755,40.1134],[-109.9757,40.1093],[-109.9751,40.0644],[-109.9749,40.0499],[-109.9746,39.9782],[-109.9743,39.9646],[-109.974,39.8912],[-109.9739,39.8744],[-109.9729,39.8036],[-109.9867,39.8038],[-110.0249,39.8049],[-110.0435,39.8047],[-110.0627,39.805],[-110.0818,39.8053],[-110.1004,39.8052],[-110.1076,39.8053],[-110.1381,39.8053],[-110.1567,39.8055],[-110.1734,39.8053],[-110.1908,39.8056],[-110.2112,39.8054],[-110.2471,39.8055],[-110.2656,39.8057],[-110.2854,39.806],[-110.3028,39.8058],[-110.3219,39.8056],[-110.359,39.8056],[-110.3782,39.8059],[-110.404,39.8053],[-110.4219,39.8051],[-110.4411,39.8058],[-110.4603,39.8055],[-110.4698,39.8057],[-110.4974,39.8055],[-110.5165,39.8058],[-110.5164,39.8112],[-110.535,39.8119],[-110.5529,39.8121],[-110.5721,39.8119],[-110.5912,39.8125],[-110.6595,39.8137],[-110.7451,39.8137],[-110.8559,39.8157],[-110.8574,39.8719],[-110.8569,39.9009],[-110.8887,39.9017],[-110.8881,39.937],[-110.89,40.0091],[-110.8904,40.0232],[-110.8907,40.0781],[-110.8931,40.0822],[-110.8944,40.1103],[-110.8937,40.4304],[-110.9016,40.431],[-110.9011,40.4586],[-110.9009,40.4736],[-110.9013,40.489],[-110.9019,40.5634],[-110.9001,40.6786],[-110.8929,40.6799],[-110.891,40.6821],[-110.8916,40.684],[-110.8934,40.6858],[-110.8939,40.6894],[-110.8945,40.6908],[-110.8975,40.6958],[-110.8986,40.7017],[-110.8997,40.7085],[-110.8942,40.7126],[-110.8911,40.7148],[-110.8856,40.7188],[-110.8898,40.7216],[-110.8915,40.728],[-110.8842,40.7288],[-110.8794,40.7292],[-110.8769,40.7296],[-110.8655,40.7255],[-110.8618,40.7245],[-110.8546,40.7222],[-110.8479,40.7253],[-110.8425,40.723],[-110.8353,40.7188],[-110.8298,40.7161],[-110.8208,40.7105],[-110.8184,40.7119],[-110.8043,40.7204],[-110.7878,40.7297],[-110.7829,40.7319],[-110.7804,40.7333],[-110.7755,40.7355],[-110.7615,40.7413],[-110.7548,40.743],[-110.7529,40.7448],[-110.7499,40.7457],[-110.7469,40.7448],[-110.7426,40.7443],[-110.7377,40.746],[-110.7341,40.7469],[-110.7298,40.7473],[-110.7213,40.7472],[-110.7171,40.749],[-110.7128,40.7512],[-110.7085,40.7521],[-110.7025,40.7507],[-110.6989,40.7493],[-110.694,40.7478],[-110.6886,40.7442],[-110.682,40.7414],[-110.6808,40.7414],[-110.6729,40.7404],[-110.6668,40.743],[-110.6626,40.7439],[-110.6571,40.7425],[-110.6535,40.7424],[-110.6473,40.7469],[-110.638,40.7577],[-110.6275,40.7671],[-110.6245,40.7689],[-110.6226,40.7689],[-110.6184,40.7684],[-110.6112,40.7651],[-110.607,40.7628],[-110.5998,40.7591],[-110.5845,40.7617],[-110.5779,40.7611],[-110.5694,40.7601],[-110.5603,40.7587],[-110.553,40.7631],[-110.5468,40.7671],[-110.5437,40.7716],[-110.5363,40.7747],[-110.5315,40.7733],[-110.5285,40.7714],[-110.5244,40.7669],[-110.5244,40.7659],[-110.5172,40.7622],[-110.5068,40.7658],[-110.4989,40.767],[-110.4915,40.7715],[-110.4816,40.7786],[-110.478,40.7777],[-110.4738,40.7758],[-110.469,40.7744],[-110.4647,40.7743],[-110.461,40.7765],[-110.4561,40.7792],[-110.4505,40.7841],[-110.4469,40.7832],[-110.4379,40.7808],[-110.4318,40.7825],[-110.4299,40.7839],[-110.4244,40.7874],[-110.4219,40.7897],[-110.4195,40.7906],[-110.4159,40.7887],[-110.4116,40.7873],[-110.4068,40.7868],[-110.4032,40.7854],[-110.3983,40.7853],[-110.394,40.7871],[-110.3867,40.7874],[-110.3764,40.7887],[-110.3666,40.7903],[-110.3618,40.7916],[-110.3586,40.7952],[-110.3592,40.798],[-110.3543,40.8006],[-110.3517,40.806],[-110.3516,40.8115],[-110.349,40.8178],[-110.341,40.8245],[-110.3326,40.8203],[-110.3235,40.8197],[-110.3094,40.8223],[-110.2923,40.8257],[-110.277,40.8304],[-110.2697,40.8322],[-110.2593,40.8343],[-110.2551,40.8347],[-110.2502,40.8337],[-110.243,40.8313],[-110.2375,40.8308],[-110.2315,40.8285],[-110.2243,40.8274],[-110.2218,40.827],[-110.2158,40.8273],[-110.2109,40.8282],[-110.197,40.8234],[-110.1897,40.8238],[-110.1777,40.8209],[-110.1645,40.8134],[-110.1609,40.8134],[-110.1414,40.8145],[-110.128,40.8138],[-110.1232,40.8133],[-110.119,40.8128],[-110.1123,40.8122],[-110.1099,40.8117],[-110.1087,40.8117],[-110.1027,40.8085],[-110.0991,40.8066],[-110.0899,40.8096],[-110.0832,40.8118],[-110.068,40.8116],[-110.0644,40.8106],[-110.0577,40.81],[-110.054,40.8109],[-110.0473,40.8144],[-110.0417,40.8184],[-110.0398,40.8193],[-110.0338,40.8169],[-110.0169,40.8139],[-110.0018,40.8096],[-109.9904,40.8063],[-109.9789,40.8065],[-109.9746,40.8065]]]},\"properties\":{\"name\":\"Duchesne\",\"state\":\"UT\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51177e05e4b0893acf3fffd0","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":473275,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":473276,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042931,"text":"70042931 - 1976 - Tectonic framework of petroliferous rocks in Alaska: hydrocarbons","interactions":[{"subject":{"id":13884,"text":"ofr75149 - 1975 - Tectonic framework of petroliferous rocks in Alaska","indexId":"ofr75149","publicationYear":"1975","noYear":false,"title":"Tectonic framework of petroliferous rocks in Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70042931,"text":"70042931 - 1976 - Tectonic framework of petroliferous rocks in Alaska: hydrocarbons","indexId":"70042931","publicationYear":"1976","noYear":false,"title":"Tectonic framework of petroliferous rocks in Alaska: hydrocarbons"},"id":1}],"lastModifiedDate":"2013-01-29T09:52:19","indexId":"70042931","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"25","title":"Tectonic framework of petroliferous rocks in Alaska: hydrocarbons","docAbstract":"Alaska, which contains about 28% of the land and continental shelf of the United States, is estimated by the U.S. Geological Survey to contain about one third of the nation's undiscovered oil and about one sixth of its undiscovered natural gas. The Survey estimates that fields discovered in Alaska through 1972 ultimately may produce about 26 billion bbl of oil and 68 Tcf of natural gas. In northern Alaska, Paleozoic and Mesozoic shelf and slope carbonate and clastic rocks of the Brooks Range orogen were thrust relatively northward over the depressed south margin of the Paleozoic and Mesozoic Arctic platform. A foredeep, the Colville geosyncline, developed across the depressed margin of the platform in earliest Cretaceous time. Detritus from the Brooks Range filled the foredeep and prograded northward to fill the Cretaceous and Tertiary North Chukchi and Umiat-Camden basins and form the progradational Beaufort shelf. The largest petroleum reserves (Prudhoe Bay and associated fields) and the best prospects for additional large discoveries in Alaska lie in the areally extensive upper Paleozoic to Tertiary carbonate and clastic rocks of northern Alaska. In southern Alaska, a series of arc-trench systems developed on oceanic rocks during Jurassic and Cretaceous time. Between these arcs and the metamorphic (continental) terranes of east-central and northern Alaska, large back-arc and arc-trench gap basins received thick volcanic and detrital deposits. These deposits were extensively, and commonly intensely, deformed and disrupted by mid-Jurassic to Tertiary plutonism, Laramide oroclinal bending, wrench faulting, and arc-related compression. This deformation, coupled with low porosity (in part produced by diagenetic mobilization of labile constituents), has left these rocks with only modest, local prospects for petroleum. Laramide events compressed and consolidated (\"continentalized\") the late Mesozoic back-arc basin deposits and welded them to the older continental terranes on the north and east. Subsequent sedimentation was localized and nonmarine except in onshore and offshore coastal basins, where thick sections of mixed marine and nonmarine Tertiary sediments accumulated. The Aleutian arc and the associated Queen Charlotte transform-fault system have dominated structural and depositional patterns in southern Alaska, including many of the Tertiary coastal basins, since the early Cenozoic. The Tertiary coastal basins are areally extensive, and in some areas contain many large folds. They are known to be petroliferous in Bristol Bay and the Gulf of Alaska, and to contain major accumulations of oil and gas at Cook Inlet, but they are relatively little explored.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Circum-Pacific energy and mineral resources (AAPG Memoir 25)","largerWorkSubtype":{"id":3,"text":"Organization Series"},"language":"English","publisher":"AAPG","publisherLocation":"Tulsa, OK","usgsCitation":"Grantz, A., and Kirschner, C., 1976, Tectonic framework of petroliferous rocks in Alaska: hydrocarbons, chap. <i>of</i> Circum-Pacific energy and mineral resources (AAPG Memoir 25), p. 291-307.","productDescription":"17 p.","startPage":"291","endPage":"307","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266659,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266658,"type":{"id":15,"text":"Index Page"},"url":"https://archives.datapages.com/data/specpubs/mineral1/data/a175/a175/0001/0250/0291.htm"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,51.2 ], [ 172.5,71.4 ], [ -130.0,71.4 ], [ -130.0,51.2 ], [ 172.5,51.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd95e4b0d965cd9f2393","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":472602,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kirschner, C.E.","contributorId":81107,"corporation":false,"usgs":true,"family":"Kirschner","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":472603,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042814,"text":"70042814 - 1976 - Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","interactions":[{"subject":{"id":15841,"text":"ofr7518 - 1975 - Exploration for porphyry copper deposits in Pakistan using digital processing of ERTS-1 data","indexId":"ofr7518","publicationYear":"1975","noYear":false,"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of ERTS-1 data"},"predicate":"SUPERSEDED_BY","object":{"id":70042814,"text":"70042814 - 1976 - Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","indexId":"70042814","publicationYear":"1976","noYear":false,"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data"},"id":1}],"lastModifiedDate":"2023-08-17T20:03:26.50537","indexId":"70042814","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data","docAbstract":"<p>Rock-type classification by digital-computer processing of Landsat-1 (formerly ERTS-1) multispectral scanner data has been used to select 23 prospecting targets in the Chagai District, Pakistan, 5 of which have proved to be large areas of hydrothermally altered porphyry containing pyrite. The known porphyry copper deposit at Saindak was used as a control area. Empirical maximum and minimum apparent reflectance limits were selected for each multispectral scanner band in each rock type classified, and a relatively unrefined classification table was prepared. Where the values for all four bands fitted within the limits designated for a particular class, a symbol for the presumed rock type was printed by the computer at the appropriate location; these symbols formed a classification map. Drainage channels, areas of mineralized quartz diorite, areas of pyrite-rich rock, and the approximate limit of propylitic alteration were very well delineated on the computer-generated map of the test area. The classification method was then used to evaluate 2,100 km<sup>2</sup> in the Mashki Chah region, east of the test area, and a partial check of the results was made in the field. The results of the experiment show that outcrops of hydrothermally altered and mineralized rock can be identified from Landsat-1 data under favorable conditions. The empirical method of digital computer classification of the multispectral scanner data was relatively unrefined and rapid. The five mineralized prospecting sites identified are in locations that I would not have selected as favorable on the basis of geologic knowledge or photogeologic interpretation at the time of the investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Schmidt, R.G., 1976, Exploration for porphyry copper deposits in Pakistan using digital processing of Landsat-1 data: Journal of Research of the U.S. Geological Survey, v. 4, no. 1, p. 27-34.","productDescription":"8 p.","startPage":"27","endPage":"34","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266418,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue1/report.pdf","text":"report","size":"16.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":266419,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Pakistan","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 60.87,23.54 ], [ 60.87,37.06 ], [ 77.82,37.06 ], [ 77.82,23.54 ], [ 60.87,23.54 ] ] ] } } ] }","volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026611e4b0d4f5ea817bd9","contributors":{"authors":[{"text":"Schmidt, Robert G.","contributorId":19243,"corporation":false,"usgs":true,"family":"Schmidt","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":472320,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","interactions":[{"subject":{"id":14188,"text":"ofr76323 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"ofr76323","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":70042934,"text":"70042934 - 1976 - Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","indexId":"70042934","publicationYear":"1976","noYear":false,"title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado"},"id":1}],"lastModifiedDate":"2016-12-12T13:40:24","indexId":"70042934","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"53","title":"Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado","docAbstract":"<p>This report presents a part of the results of an investigation of the hydrology of the northern Uinta Basin area by the U.S. Geological Survey in cooperation with the Division of Water Rights, Utah Department of Natural Resources. The purpose of the report is to summarize the hydraulic and geohydrologic characteristics of the aquifers in the area.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights ","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights ","usgsCitation":"Hood, J.W., 1976, Characteristics of aquifers in the northern Uinta Basin area, Utah and Colorado: Technical Publication 53, vi, 71 p.","productDescription":"vi, 71 p.","numberOfPages":"80","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331878,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-330"},{"id":331879,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009f.pdf"}],"country":"United States","state":"Colorado, Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.0,37.0 ], [ -114.0,42.0 ], [ -102.0,42.0 ], [ -102.0,37.0 ], [ -114.0,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd7fe4b0d965cd9f2319","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":472616,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","interactions":[{"subject":{"id":10744,"text":"ofr7787 - 1977 - Electronic thermal sensor and Landsat data collection platform technology","indexId":"ofr7787","publicationYear":"1977","noYear":false,"title":"Electronic thermal sensor and Landsat data collection platform technology"},"predicate":"SUPERSEDED_BY","object":{"id":70043109,"text":"70043109 - 1976 - Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","indexId":"70043109","publicationYear":"1976","noYear":false,"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>"},"id":1}],"lastModifiedDate":"2013-02-05T12:00:58","indexId":"70043109","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":360,"text":"Final Report","active":false,"publicationSubtype":{"id":6}},"title":"Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>","docAbstract":"Five Data Collection Platforms (DCP) were integrated electronically with thermall sensing systems, emplaced and operated in an analog mode at selected thermally significant volcanic and geothermal sites. The DCP's transmitted 3260 messages comprising 26,080 ambient, surface, and near-surface temperature records at an accuracy of ±1.15 &deg;C for 1121 instrument days between November 14, 1972 and April 17, 1974. In harsh, windy, high-altitude volcanic environments the DCP functioned best with a small dipole antenna. Sixteen kg of alkaline batteries provided a viable power supply for the DCP systems, operated at a low-duty cycle, for 5 to 8 months. A proposed solar power supply system would lengthen the period of unattended operation of the system considerably. Special methods of data handling such as data storage via a proposed memory system would increase the significance of the twice-daily data reception enabling the DCP's to record full diurnal-temperature cycles at volcanic or geothermal sites. Refinements in the temperature-monitoring system designed and operated in experiment SR 251 included a backup system consisting of a multipoint temperature scanner, a servo mechanism and an analog-to-digital recorder. Improvements were made in temperature-probe design and in construction of corrosion-resistant seals by use of a hydrofluoric-acid-etching technique.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System","largerWorkSubtype":{"id":6,"text":"USGS Unnumbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70043109","usgsCitation":"Preble, D.M., Friedman, J.D., and Frank, D., 1976, Electronic thermal sensor and Data Collection Platform technology: Part 5 in <i>Thermal surveillance of active volcanoes using the Landsat-1 Data Collection System</i>: Final Report, 64 p., https://doi.org/10.3133/70043109.","productDescription":"64 p.","costCenters":[{"id":615,"text":"Volcano Hazards Program","active":true,"usgs":true}],"links":[{"id":266996,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5112382ce4b0ebe69d7eb6ce","contributors":{"authors":[{"text":"Preble, Duane M.","contributorId":36560,"corporation":false,"usgs":true,"family":"Preble","given":"Duane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":472977,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedman, Jules D.","contributorId":79464,"corporation":false,"usgs":true,"family":"Friedman","given":"Jules","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":472978,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frank, David","contributorId":13969,"corporation":false,"usgs":true,"family":"Frank","given":"David","affiliations":[],"preferred":false,"id":472976,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70042912,"text":"70042912 - 1976 - Rise of a variable-viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls","interactions":[{"subject":{"id":14563,"text":"ofr74251 - 1974 - Rise of a variable viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls","indexId":"ofr74251","publicationYear":"1974","noYear":false,"title":"Rise of a variable viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls"},"predicate":"SUPERSEDED_BY","object":{"id":70042912,"text":"70042912 - 1976 - Rise of a variable-viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls","indexId":"70042912","publicationYear":"1976","noYear":false,"title":"Rise of a variable-viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls"},"id":1}],"lastModifiedDate":"2022-06-15T14:42:26.277635","indexId":"70042912","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Rise of a variable-viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls","docAbstract":"Relatively rigid plates making up the outer 50 to 100 km of the Earth are steadily separating from one another along narrow globe-circling zones of submarine volcanism, the oceanic spreading centers. Continuity requires that the viscous underlying material rise beneath spreading centers and accrete onto the steadily diverging plates. It is likely that during the rise the viscosity changes systematically and that the viscous tractions exerted on the plates contribute to the unique pattern of submarine mountains and earthquake faults observed at spreading centers. The process is modeled by viscous creep in a wedge-shaped conduit (with apex at the sea floor) in which the viscosity varies as <i>r<sup>m</sup></i> where <i>r</i> is distance from the apex and <i>m</i> is a parameter. For these conditions, the governing differential equations take a simple form. The solution for the velocity is independent of <i>r</i> and of the sign of <i>m</i>. As viscous stresses vary as <i>r<sup>m-1</sup></i>, the pattern of stress on the conduit wall is sensitive to viscosity variation. For negative <i>m</i>, the viscous pressure along the base of the conduit is quite uniform; for positive <i>m</i>, it falls toward zero in the axial region as the conduit base widens. For small opening angles, viscous forces push the plates apart, and for large ones, they oppose plate separation. Though highly idealized, the solution provides a tool for investigating tectonic processes at spreading centers.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Lachenbruch, A.H., and Nathenson, M., 1976, Rise of a variable-viscosity fluid in a steadily spreading wedge-shaped conduit with accreting walls: Journal of Research of the U.S. Geological Survey, v. 4, no. 2, p. 181-188.","productDescription":"8 p.","startPage":"181","endPage":"188","costCenters":[{"id":237,"text":"Earthquake Science Center","active":true,"usgs":true},{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":266647,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266646,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue2/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"4","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5108fd91e4b0d965cd9f237e","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":472580,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nathenson, Manuel 0000-0002-5216-984X mnathnsn@usgs.gov","orcid":"https://orcid.org/0000-0002-5216-984X","contributorId":1358,"corporation":false,"usgs":true,"family":"Nathenson","given":"Manuel","email":"mnathnsn@usgs.gov","affiliations":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"preferred":true,"id":472579,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","interactions":[{"subject":{"id":15062,"text":"ofr75615 - 1975 - Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho","indexId":"ofr75615","publicationYear":"1975","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges, Gooding and Jerome Counties, Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":70042717,"text":"70042717 - 1976 - Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","indexId":"70042717","publicationYear":"1976","noYear":false,"title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho"},"id":1}],"lastModifiedDate":"2013-01-18T14:10:29","indexId":"70042717","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":301,"text":"Water Information Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"42","title":"Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho","docAbstract":"Springs discharging from the Snake Plain aquifer contribute approximately 6,000 cubic feet per second (170 cubic metres per second) to flow in the Snake River between Milner and King Hill. Before irrigation began on the Snake River Plain north and east of the springs, total spring discharge was about 4,200 cubic feet per second (120 cubic meters per second). Increasing amounts of irrigated acreage from the early 1900's to the mid-1940's contributed more irrigation-return water to the aquifer resulting in increased discharge at the springs. Maximum discharge of about 6,800 cubic feet per second (190 cubic metres per second) occurred during the late 1940's and early 1950's. Increased use of pumped ground water for irrigation and changing irrigation practices have since resulted in a decline in spring discharge.","language":"English","publisher":"Idaho Department of Water Resources","publisherLocation":"Boise, ID","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Idaho Department of Water Resources, Statehouse, Boise, Idaho","usgsCitation":"Moreland, J.A., 1976, Digital-model analysis of the effects of water-use alternatives on spring discharges Gooding and Jerome Counties, Idaho: Water Information Bulletin 42, vi, 46 p.; ill.; maps.","productDescription":"vi, 46 p.; ill.; maps","startPage":"i","endPage":"46","numberOfPages":"53","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":265963,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":265962,"type":{"id":11,"text":"Document"},"url":"https://www.idwr.idaho.gov/WaterInformation/Publications/wib/wib42-water-use_alternatives.pdf"}],"country":"United States","state":"Idaho","county":"Gooding County;Jerome County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.0875,42.4981 ], [ -115.0875,43.2001 ], [ -113.9308,43.2001 ], [ -113.9308,42.4981 ], [ -115.0875,42.4981 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50fa7d53e4b061045bf9ac32","contributors":{"authors":[{"text":"Moreland, Joe A.","contributorId":48171,"corporation":false,"usgs":true,"family":"Moreland","given":"Joe","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":472107,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","interactions":[{"subject":{"id":13216,"text":"ofr74214 - 1974 - Estimating mean streamflow in the Duchesne River basin, Utah","indexId":"ofr74214","publicationYear":"1974","noYear":false,"title":"Estimating mean streamflow in the Duchesne River basin, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":1},{"subject":{"id":16124,"text":"ofr75392 - 1975 - Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah","indexId":"ofr75392","publicationYear":"1975","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin; Millard, Beaver, and Iron counties, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70042823,"text":"70042823 - 1976 - Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","indexId":"70042823","publicationYear":"1976","noYear":false,"title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah"},"id":2}],"lastModifiedDate":"2016-12-12T13:38:13","indexId":"70042823","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"51","title":"Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah","docAbstract":"The Pine Valley drainage basin is an area of about 730 square miles (1,890 square kilometres) in Millard, Beaver, and Iron Counties in southwestern Utah. Total annual precipitation in the basin averages about 410,000 acre-ft (acre-feet) or 506 hm<sup>3</sup> (cubic hectometres). Less than 500 acre-ft (0.6 hm<sup>3</sup>) of runoff reaches the playa on the lowest part of the valley floor. There is no surface outflow from the basin. All streams are ephemeral except in short headwater reaches of a few streams where perennial or intermittent ground-water discharge sustains flow. Surface-water development and use in the basin are insignificant.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the U.S. Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights.","usgsCitation":"Stephens, J.C., 1976, Hydrologic reconnaissance of the Pine Valley drainage basin, Millard, Beaver, and Iron counties, Utah: Technical Publication 51, iv, 38 p.","productDescription":"iv, 38 p.","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":266429,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":267163,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009d.pdf"},{"id":331876,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-300"}],"country":"United States","state":"Utah","county":"Beaver County, Iron County, Millard County","otherGeospatial":"Pine Valley Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              38.884619201291905\n            ],\n            [\n              -113.27728271484374,\n              37.96801944035648\n            ],\n            [\n              -114.0106201171875,\n              37.96801944035648\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026618e4b0d4f5ea817c00","contributors":{"authors":[{"text":"Stephens, Jerry C.","contributorId":81493,"corporation":false,"usgs":true,"family":"Stephens","given":"Jerry","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":472331,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","interactions":[{"subject":{"id":16567,"text":"ofr75322 - 1975 - Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A.","indexId":"ofr75322","publicationYear":"1975","noYear":false,"title":"Geology and geophysics of the southern Raft River valley geothermal area, Idaho, U.S.A."},"predicate":"SUPERSEDED_BY","object":{"id":70042576,"text":"70042576 - 1976 - Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","indexId":"70042576","publicationYear":"1976","noYear":false,"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA"},"id":1}],"lastModifiedDate":"2017-11-03T11:01:24","indexId":"70042576","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA","docAbstract":"The Raft River valley, near the boundary of the Snake River plain with the Basin and Range province, is a north-trending late Cenozoic downwarp bounded by faults on the west, south, and east. Pleistocene alluvium and Miocene-Pliocene tuffaceous sediments, conglomerate, and felsic volcanic rocks aggregate 2 km in thickness. Large gravity, magnetic, and total field resistivity highs probably indicate a buried igneous mass that is too old to serve as a heat source. Differing seismic velocities relate to known or inferred structures and to a suspected shallow zone of warm water. Resistivity anomalies reflect differences of both composition and degree of alteration of Cenozoic rocks. Resistivity soundings show a 2 to 5 ohm·m unit with a thickness of 1 km beneath a large part of the valley, and the unit may indicate partly hot water and partly clayey sediments. Observed self-potential anomalies are believed to indicate zones where warm water rises toward the surface. Boiling wells at Bridge, Idaho are near the intersection of north-northeast normal faults which have moved as recently as the late (?) Pleistocene, and an east-northeast structure, probably a right-lateral fault. Deep circulation of ground water in this region of relatively high heat flow and upwelling along faults is the probable cause of the thermal anomaly.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Williams, P., Mabey, D.R., Zohdy, A.A., Ackermann, H.D., Hoover, D.B., Pierce, K.L., and Oriel, S.S., 1976, Geology and geophysics of the southern Raft River Valley geothermal area, Idaho, USA, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1273-1282.","productDescription":"10 p.","startPage":"1273","endPage":"1282","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":265587,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Raft River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.24,42.0 ], [ -117.24,49.0 ], [ -111.04,49.0 ], [ -111.04,42.0 ], [ -117.24,42.0 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50f293f4e4b0c9e41dd3ab73","contributors":{"authors":[{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":471858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mabey, Don R.","contributorId":43741,"corporation":false,"usgs":true,"family":"Mabey","given":"Don","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":471855,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zohdy, Adel A. R.","contributorId":61799,"corporation":false,"usgs":true,"family":"Zohdy","given":"Adel","email":"","middleInitial":"A. R.","affiliations":[],"preferred":false,"id":471856,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ackermann, Hans D.","contributorId":44539,"corporation":false,"usgs":false,"family":"Ackermann","given":"Hans","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":471854,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Hoover, Donald B.","contributorId":89877,"corporation":false,"usgs":true,"family":"Hoover","given":"Donald","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":471857,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Pierce, Kenneth L. kpierce@usgs.gov","contributorId":1609,"corporation":false,"usgs":true,"family":"Pierce","given":"Kenneth","email":"kpierce@usgs.gov","middleInitial":"L.","affiliations":[{"id":547,"text":"Rocky Mountain Geographic Science Center","active":true,"usgs":true},{"id":481,"text":"Northern Rocky Mountain Science Center","active":true,"usgs":true},{"id":318,"text":"Geosciences and Environmental Change Science Center","active":true,"usgs":true}],"preferred":true,"id":471853,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Oriel, Steven S.","contributorId":108079,"corporation":false,"usgs":true,"family":"Oriel","given":"Steven","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":471859,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70042515,"text":"70042515 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","interactions":[{"subject":{"id":17647,"text":"ofr76257 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","indexId":"ofr76257","publicationYear":"1976","noYear":false,"title":"Saline water in the Little Arkansas River Basin area, south-central Kansas"},"predicate":"SUPERSEDED_BY","object":{"id":70042515,"text":"70042515 - 1976 - Saline water in the Little Arkansas River Basin area, south-central Kansas","indexId":"70042515","publicationYear":"1976","noYear":false,"title":"Saline water in the Little Arkansas River Basin area, south-central Kansas"},"id":1}],"lastModifiedDate":"2013-01-10T14:49:37","indexId":"70042515","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":243,"text":"Chemical Quality Series","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"3","title":"Saline water in the Little Arkansas River Basin area, south-central Kansas","docAbstract":"Ground water in unconsolidated deposits of Pleistocene age in part of the Little Arkansas River basin has been polluted by the influx of saline water. The source of the saline water generally is oil-field brine that leaked from disposal ponds on the land surface. Locally, pollution by saline water also has been caused by upwelling of oil-field brine injected under pressure into the \"lost-circulation zone\" of the Lower Permian Wellington Formation and, possibly, by leakage of brine from corroded or improperly cased disposal wells. Anomalously high concentrations of chloride ion in some reaches of the Little Arkansas River probably can be attributed to pollution by municipal wastes rather than from inflow of saline ground water. Hydraulic connection exists between the \"lost-circulation zone\" and unconsolidated deposits, as evidenced by the continuing development of sinkholes, by the continuing discharge of saline water through springs and seeps along the Arkansas River south of the Little Arkansas River basin and by changes in the chloride concentration in water pumped from wells in the \"lost-circulation zone.\" The hydraulic head in the \"lost-circulation zone\" is below the base of the unconsolidated deposits, and much below the potentiometric surface of the aquifer in those deposits. Any movement of water, therefore, would be downward from the \"fresh-water\" aquifer to the saline \"lost-circulation zone.\"","language":"English","publisher":"University of Kansas Publications","publisherLocation":"Lawrence, KS","collaboration":"Prepared cooperatively by the Kansas Geological Survey and the U.S. Geological Survey","usgsCitation":"Leonard, R., and Kleinschmidt, M.K., 1976, Saline water in the Little Arkansas River Basin area, south-central Kansas: Chemical Quality Series 3, iii, 24 p.; ill.; maps.","productDescription":"iii, 24 p.; ill.; maps","startPage":"i","endPage":"24","numberOfPages":"28","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":265515,"type":{"id":11,"text":"Document"},"url":"https://www.kgs.ku.edu/Publications/Bulletins/CQS3/cqs3.pdf"},{"id":265516,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Little Arkansas River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -102.05,37.0 ], [ -102.05,40.0 ], [ -94.59,40.0 ], [ -94.59,37.0 ], [ -102.05,37.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd714ae4b0b29085107974","contributors":{"authors":[{"text":"Leonard, Robert B.","contributorId":14407,"corporation":false,"usgs":true,"family":"Leonard","given":"Robert B.","affiliations":[],"preferred":false,"id":471676,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kleinschmidt, Melvin K.","contributorId":32793,"corporation":false,"usgs":true,"family":"Kleinschmidt","given":"Melvin","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":471677,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042824,"text":"70042824 - 1976 - Regional geologic framework off northeastern United States","interactions":[{"subject":{"id":15831,"text":"ofr7560 - 1975 - Structure of continental margin off Mid-Atlantic states (Baltimore Canyon Trough)","indexId":"ofr7560","publicationYear":"1975","noYear":false,"title":"Structure of continental margin off Mid-Atlantic states (Baltimore Canyon Trough)"},"predicate":"SUPERSEDED_BY","object":{"id":70042824,"text":"70042824 - 1976 - Regional geologic framework off northeastern United States","indexId":"70042824","publicationYear":"1976","noYear":false,"title":"Regional geologic framework off northeastern United States"},"id":1}],"lastModifiedDate":"2023-01-25T16:42:25.487197","indexId":"70042824","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Regional geologic framework off northeastern United States","docAbstract":"<p>Six multichannel seismic-reflection profiles taken across the Atlantic continental margin off the northeastern United States show an excess of 14 km of presumed Mesozoic and younger sedimentary rocks in the Baltimore Canyon trough and 8 km in the Georges Bank basin.</p><p>Beneath the continental rise, the sedimentary prism thickness exceeds 7 km south of New Jersey and Maryland, and it is 4.5 km thick south of Georges Bank. Stratigraphically, the continental slope–outer edge of the continental shelf is a transition zone of high-velocity sedimentary rock, probably carbonate, that covers deeply subsided basement.</p><p>Acoustically, the sedimentary sequence beneath the shelf is divided into three units which are correlated speculatively with the Cenozoic, the Cretaceous, and the Jurassic-Triassic sections. These units thicken offshore, and some have increased seismic velocities farther offshore. The uppermost unit thickens from a fraction of a kilometer to slightly more than a kilometer in a seaward direction, and velocity values range from 1.7 to 2.2 km/sec. The middle unit thickens from a fraction of a kilometer to as much as 5 km (northern Baltimore Canyon trough), and seismic velocity ranges from 2.2 to 5.4 km/sec. The lowest unit thickens to a maximum of 9 km (northern Baltimore Canyon), and velocities span the 3.9 to 5.9-km/sec interval.</p><p>The spatial separation of magnetic and gravity anomalies on line 2 (New Jersey) suggests that in the Baltimore Canyon region the magnetic-slope anomaly is due to edge effects and that the previously reported free-air and isostatic gravity anomalies over the outer shelf may be due in part to a lateral increase in sediment density (velocity) near the shelf edge. The East Coast magnetic anomaly and the free-air gravity high both coincide over the outer shelf edge on line 1 (Georges Bank) but are offset by 20 km from the ridge on the reflection profile. Because the magnetic-slope-anomaly wavelength is nearly 50 km across, a deep source is likely. In part, the positive free-air gravity anomaly likewise may represent the significant lateral density increase within the sedimentary section toward the outer edge of the shelf.</p>","language":"English","publisher":"American Association of Petroleum Geologists","publisherLocation":"Tulsa, OK","doi":"10.1306/C1EA35E1-16C9-11D7-8645000102C1865D","usgsCitation":"Schlee, J., Behrendt, J.C., Grow, J., Robb, J.M., Mattick, R.E., Taylor, P.T., and Lawson, B.J., 1976, Regional geologic framework off northeastern United States: American Association of Petroleum Geologists Bulletin, v. 60, no. 6, p. 926-951, https://doi.org/10.1306/C1EA35E1-16C9-11D7-8645000102C1865D.","productDescription":"26 p.","startPage":"926","endPage":"951","numberOfPages":"26","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266431,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Atlantic Ocean","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -74.57445495565841,\n              34.54201079036788\n            ],\n            [\n              -67.00870217573663,\n              32.68969202501184\n            ],\n            [\n              -64.4151885851629,\n              33.653394442107356\n            ],\n            [\n              -58.9581858826422,\n              40.6927360683957\n            ],\n            [\n              -68.50221203592804,\n              42.200234266771474\n            ],\n            [\n              -70.993156429557,\n              40.57584686002005\n            ],\n            [\n              -73.8834116106613,\n              39.16159111213017\n            ],\n            [\n              -75.18467319036125,\n              36.48592421852297\n            ],\n            [\n              -74.48849487074959,\n              34.39791504686983\n            ],\n            [\n              -74.57445495565841,\n              34.54201079036788\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"60","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51026629e4b0d4f5ea817c51","contributors":{"authors":[{"text":"Schlee, John","contributorId":16078,"corporation":false,"usgs":true,"family":"Schlee","given":"John","affiliations":[],"preferred":false,"id":472336,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Behrendt, John C. jbehrendt@usgs.gov","contributorId":25945,"corporation":false,"usgs":true,"family":"Behrendt","given":"John","email":"jbehrendt@usgs.gov","middleInitial":"C.","affiliations":[{"id":218,"text":"Denver Federal Center","active":false,"usgs":true},{"id":213,"text":"Crustal Imaging and Characterization Team","active":false,"usgs":true}],"preferred":false,"id":472334,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grow, John A.","contributorId":51739,"corporation":false,"usgs":true,"family":"Grow","given":"John A.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":472335,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Robb, James M.","contributorId":73272,"corporation":false,"usgs":true,"family":"Robb","given":"James","email":"","middleInitial":"M.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":472338,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mattick, Robert E.","contributorId":44130,"corporation":false,"usgs":true,"family":"Mattick","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":472333,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Taylor, P. T.","contributorId":69858,"corporation":false,"usgs":true,"family":"Taylor","given":"P.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":472337,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Lawson, B. J.","contributorId":11905,"corporation":false,"usgs":true,"family":"Lawson","given":"B.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":472332,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":70042740,"text":"70042740 - 1976 - Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","interactions":[{"subject":{"id":15965,"text":"ofr75566 - 1975 - Textural distribution of sea-floor sediments, South Texas Outer Continental Shelf","indexId":"ofr75566","publicationYear":"1975","noYear":false,"title":"Textural distribution of sea-floor sediments, South Texas Outer Continental Shelf"},"predicate":"SUPERSEDED_BY","object":{"id":70042740,"text":"70042740 - 1976 - Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","indexId":"70042740","publicationYear":"1976","noYear":false,"title":"Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf"},"id":1}],"lastModifiedDate":"2016-06-08T16:39:16","indexId":"70042740","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf","docAbstract":"The general texture of sea-floor sediments along the south Texas Outer Continental Shelf was evaluated in terms of gravel, sand, silt, and clay components. The gravel component is quantitatively minor and is concentrated mainly in the southern sector; it consists, for the most part, of relict biogenic detritus dominated by molluscan shells. The sand component consists of terrigenous and biogenic detritus. Modern sand is localized along the shoreface sector, whereas palimpsest and relict sands characterize the northern and southern sectors, which are the respective locations of the ancestral Brazos-Colorado 'and Rio Grande deltas. The central sector contains an extensive modern mud blanket that appears to be migrating southward over relict deposits of the ancestral Rio Grande delta. The silt fraction is the highly dominant component of the mud blanket; silt appears to be hydraulically trapped within the shelf environment and constitutes the most abundant detrital component within the Outer Continental Shelf region. The subordinate clay component of the mud blanket is concentrated toward the shelf break and may be largely escaping into deeper water environments.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Shideler, G.L., 1976, Textural distribution of sea-floor sediments, south Texas Outer Continental Shelf: Journal of Research of the U.S. Geological Survey, v. 4, no. 6, p. 703-713.","productDescription":"11 p.","startPage":"703","endPage":"713","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":266234,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266227,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue6/report.pdf","text":"Report","size":"20.3 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","otherGeospatial":"Texas Outer Continental Shelf","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.72,25.84 ], [ -97.72,30.0 ], [ -93.52,30.0 ], [ -93.52,25.84 ], [ -97.72,25.84 ] ] ] } } ] }","volume":"4","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50ffc323e4b0ca65fed0d2b1","contributors":{"authors":[{"text":"Shideler, Gerald L.","contributorId":89137,"corporation":false,"usgs":true,"family":"Shideler","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":472134,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70043958,"text":"70043958 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","interactions":[{"subject":{"id":8473,"text":"ofr76182 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","indexId":"ofr76182","publicationYear":"1976","noYear":false,"title":"Seepage study of canals in Beaver Valley, Beaver County, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":70043958,"text":"70043958 - 1976 - Seepage study of canals in Beaver Valley, Beaver County, Utah","indexId":"70043958","publicationYear":"1976","noYear":false,"title":"Seepage study of canals in Beaver Valley, Beaver County, Utah"},"id":1}],"lastModifiedDate":"2016-12-11T10:22:58","indexId":"70043958","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"52","title":"Seepage study of canals in Beaver Valley, Beaver County, Utah","docAbstract":"A study of the gains or losses of nine canals near Beaver, Utah, was made to aid in the water allocation of the canal systems. The canals included in this study are Manderfield Ditch, Last Chance Canal, Christiansen Ditch, Mammoth Canal, City Ditch, Owens Ditch, South Field Ditch, Patterson Ditch and Aberdare Canal. Four sets of seepage measurements were made during 1974, but flow was observed in all nine canals only during the set of measurements made in June. Adjustments for fluctuations in flow in the canals were made from information obtained from water-stage recorders operated at selected locations along the canals during the time of each seepage run.","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared by the United States Geological Survey in cooperation with the Utah Department of Natural Resources Division of Water Rights","usgsCitation":"Cruff, R., and Mower, R.W., 1976, Seepage study of canals in Beaver Valley, Beaver County, Utah: Technical Publication 52, iv, 45 p.","productDescription":"iv, 45 p.","numberOfPages":"50","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":268160,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":268159,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w920009e.pdf"},{"id":331877,"rank":3,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-5-320"}],"country":"United States","state":"Utah","county":"Beaver County","otherGeospatial":"Aberdare Canal, Christiansen Ditch, City Ditch, Last Chance Canal, Mammoth Canal, Manderfield Ditch, Owens Ditch, Patterson Ditch, South Field Ditch","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.8,\n              38.1\n            ],\n            [\n              -112.8,\n              38.5\n            ],\n            [\n              -112.4,\n              38.5\n            ],\n            [\n              -112.4,\n              38.1\n            ],\n            [\n              -112.8,\n              38.1\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"512b44bae4b0523e997a81ad","contributors":{"authors":[{"text":"Cruff, R.W.","contributorId":77510,"corporation":false,"usgs":true,"family":"Cruff","given":"R.W.","email":"","affiliations":[],"preferred":false,"id":474552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mower, R. W.","contributorId":34898,"corporation":false,"usgs":true,"family":"Mower","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":474551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042909,"text":"70042909 - 1976 - A portable helium sniffer","interactions":[{"subject":{"id":13673,"text":"ofr75532 - 1975 - A portable helium sniffer","indexId":"ofr75532","publicationYear":"1975","noYear":false,"title":"A portable helium sniffer"},"predicate":"SUPERSEDED_BY","object":{"id":70042909,"text":"70042909 - 1976 - A portable helium sniffer","indexId":"70042909","publicationYear":"1976","noYear":false,"title":"A portable helium sniffer"},"id":1}],"lastModifiedDate":"2016-01-25T18:17:35","indexId":"70042909","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2446,"text":"Journal of Research of the U.S. Geological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A portable helium sniffer","docAbstract":"<p>A portable helium sniffer has been developed for field use. The instrument is mounted in a four-wheel-drive pickup truck and can detect 50 parts per billion of helium in soil gas. The usefulness of helium sniffing in soil is being investigated as a prospecting tool in gas, oil, uranium, and geothermal prospecting as well as in earthquake prediction.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Friedman, I., and Denton, E., 1976, A portable helium sniffer: Journal of Research of the U.S. Geological Survey, v. 4, no. 1, p. 35-36.","productDescription":"2 p.","startPage":"35","endPage":"36","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":266641,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266640,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue1/report.pdf","text":"Report","size":"16.18 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"volume":"4","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5107ac09e4b0df796f216e46","contributors":{"authors":[{"text":"Friedman, Irving","contributorId":90664,"corporation":false,"usgs":true,"family":"Friedman","given":"Irving","email":"","affiliations":[],"preferred":false,"id":472574,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Denton, E.H.","contributorId":75144,"corporation":false,"usgs":true,"family":"Denton","given":"E.H.","email":"","affiliations":[],"preferred":false,"id":472573,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043033,"text":"70043033 - 1976 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","interactions":[{"subject":{"id":14197,"text":"ofr75362 - 1975 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","indexId":"ofr75362","publicationYear":"1975","noYear":false,"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration"},"predicate":"SUPERSEDED_BY","object":{"id":70043033,"text":"70043033 - 1976 - Audio-magnetotelluric methods in reconnaissance geothermal exploration","indexId":"70043033","publicationYear":"1976","noYear":false,"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration"},"id":1}],"lastModifiedDate":"2013-01-31T11:28:37","indexId":"70043033","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Audio-magnetotelluric methods in reconnaissance geothermal exploration","docAbstract":"An audio-magnetotelluric (AMT) system has been developed by the U.S. Geological Survey for low-cost reconnaissance exploration of geothermal regions. This is an electromagnetic sounding technique in which the scalar or Cagniard resistivity is computed at 12 frequencies logarithmically spaced from 7.5 to 18 600 Hz. Our system uses natural source fields except at the two upper frequencies of 10 200\nand 18 600 Hz where artificial VLF sources are available. As a reconnaissance technique we use AMT surveys in conjunction with regional gravity, magnetic, and telluric surveys. The exploration depth is a function of the resistivities of the lithologic section, but typically ranges from the surface to 0.2 km in low-resistivity areas and to greater than 2 km in high-resistivity regions. Results of the initial reconnaissance AMT surveys provide a rational basis for deciding on the extent of costlier follow-up surveys. As part of the U.S. Geological Survey geothermal program, surveys were conducted in Long Valley and Surprise Valley, California; the Vale, Ore-Weiser, Idaho region; and Bruneau-Grand View, Raft River, and Island Park regions of Idaho. AMT surveys in five additional known geothermal resource areas (KGRA's) have been scheduled for completion by May 1975. In the Raft River and Bruneau-Grand View regions and Long Valley, follow-up electrical surveys substantiated the effectiveness of the AMT technique for reconnaissance surveying.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Hoover, D., and Long, C.L., 1976, Audio-magnetotelluric methods in reconnaissance geothermal exploration, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1059-1064.","productDescription":"6 p.","startPage":"1059","endPage":"1064","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510ba07ae4b0947afa3c856c","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":472809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Long, C. L.","contributorId":98699,"corporation":false,"usgs":true,"family":"Long","given":"C.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":472810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043031,"text":"70043031 - 1976 - Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","interactions":[{"subject":{"id":14265,"text":"ofr75368 - 1975 - Gravity and magnetic studies of The Geysers-Clear Lake geothermal region, California","indexId":"ofr75368","publicationYear":"1975","noYear":false,"title":"Gravity and magnetic studies of The Geysers-Clear Lake geothermal region, California"},"predicate":"SUPERSEDED_BY","object":{"id":70043031,"text":"70043031 - 1976 - Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","indexId":"70043031","publicationYear":"1976","noYear":false,"title":"Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA"},"id":1}],"lastModifiedDate":"2013-01-31T11:10:00","indexId":"70043031","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA","docAbstract":"Gravity and magnetic fields in The Geysers-Clear Lake region are interpreted in relation to the known geology and other available geophysical data. New gravity data provide additional detail with the area of geothermal steam production. Computer techniques were used for removal of the regional gravity field, anomaly enhancement, and modeling subsurface structures. The gravity field was separated into three components: (1) a regional field presumed to be due to deep crustal structure related to the continental margin; (2) a residual gravity low of approximately 30 mgal centered over Mount Hannah and having an approximate diameter of 20 km, which is caused, according to our model, by a magma chamber whose top lies within 10 km of the surface; and (3) a closed residual low over the original steam production field. This low is probably related to effects within 1.5 km of the surface and was modeled as a steam-saturated reservoir structure. Local magnetic highs correlate with surface outcrops of serpentinite and relief on the volcanic rocks. Upward continuation of the aeromagnetic data suggests that the serpentinite body along the Collayomi fault may extend to a depth of more than 3 km near Boggs Mountain, but that other serpentinite bodies are probably more shallow. A long-wavelength magnetic high (centered at ~39&deg;03'N 122&deg;33'W) and a magnetic low (centered at ~38&deg:43'N 122&deg;47'W) give half-width depth estimates of about 10 km. The center of the Mount Hannah gravity low lies in an area between these features and appears devoid of deep magnetic expression.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"U.S. Energy Research and Development Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Isherwood, W., 1976, Gravity and magnetic studies of the Geysers-Clear Lake geothermal region, California, USA, <i>in</i> Proceedings: second United Nations Symposium on the development and use of geothermal resources, San Francisco, California, USA, 20-29 May 1975, v. 2, p. 1065-1073.","productDescription":"9 p.","startPage":"1065","endPage":"1073","costCenters":[{"id":255,"text":"Energy Resources Program","active":true,"usgs":true}],"links":[{"id":266800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.41,32.53 ], [ -124.41,42.0 ], [ -114.13,42.0 ], [ -114.13,32.53 ], [ -124.41,32.53 ] ] ] } } ] }","volume":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"510ba08ae4b0947afa3c85ac","contributors":{"authors":[{"text":"Isherwood, William F.","contributorId":71547,"corporation":false,"usgs":true,"family":"Isherwood","given":"William F.","affiliations":[],"preferred":false,"id":472806,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25234,"text":"25234 - 1976 - Water Resources of the Upper New River Basin, West Virginia","interactions":[{"subject":{"id":48283,"text":"ofr7669 - 1975 - Water resources of the Upper New River basin, West Virginia","indexId":"ofr7669","publicationYear":"1975","noYear":false,"title":"Water resources of the Upper New River basin, West Virginia"},"predicate":"SUPERSEDED_BY","object":{"id":25234,"text":"25234 - 1976 - Water Resources of the Upper New River Basin, West Virginia","indexId":"25234","publicationYear":"1976","noYear":false,"title":"Water Resources of the Upper New River Basin, West Virginia"},"id":1}],"lastModifiedDate":"2013-07-01T15:06:18","indexId":"25234","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":286,"text":"River Basin Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"4","title":"Water Resources of the Upper New River Basin, West Virginia","language":"ENGLISH","publisher":"West Virginia Geological and Economic Survey","publisherLocation":"Morgantown, WV","collaboration":"Prepared by the United States Geological Survey in cooperation with the West Virginia Geological and Economic Survey and the West Virginia Department of Natural Resources, Division of Water Resources","usgsCitation":"Clark, W.E., Chisholm, J.L., and Frye, P.M., 1976, Water Resources of the Upper New River Basin, West Virginia: River Basin Bulletin 4, vii, 87 p.; Maps: 3 Sheets.","productDescription":"vii, 87 p.; Maps: 3 Sheets","costCenters":[],"links":[{"id":274390,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":274389,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_40242.htm"}],"scale":"250000","country":"United States","state":"West Virginia","otherGeospatial":"New River Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.629,37.228 ], [ -79.629,38.739 ], [ -81.399,38.739 ], [ -81.399,37.228 ], [ -79.629,37.228 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51d2a4efe4b0ca1848338aa2","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193341,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chisholm, James L.","contributorId":77911,"corporation":false,"usgs":true,"family":"Chisholm","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":193339,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Frye, Prentis M.","contributorId":98792,"corporation":false,"usgs":true,"family":"Frye","given":"Prentis","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":193340,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70043504,"text":"70043504 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","interactions":[{"subject":{"id":15451,"text":"ofr7684 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","indexId":"ofr7684","publicationYear":"1976","noYear":false,"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":70043504,"text":"70043504 - 1976 - Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","indexId":"70043504","publicationYear":"1976","noYear":false,"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska"},"id":1}],"lastModifiedDate":"2013-02-13T14:55:50","indexId":"70043504","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska","docAbstract":"Perhaps the world's longest and most complete onshore sedimentary record of late Cenozoic glaciation is preserved in the Gulf of Alaska Tertiary province that extends 800 km along the coast of southern Alaska. The Yakataga Formation, with an aggregate outcrop thickness of about 5,000 m, is characterized by variable amounts of distinctive neritic marine tillite-like diamictite and laminated siltstone containing dropstones interpreted as ice-rafted glacial debris. The lithology, sedimentary structures and molluscan fauna of the formation suggest that active tidal glaciers or an ice shelf were present along the landward margin of the basin possibly beginning in early or early middle Miocene time. Dropstone distribution in outcrop sections indicates that glaciers reached tidewater intermittently during the Miocene and were almost continually present throughout the Pliocene and much of the Pleistocene. Paleomagnetic and nannoplankton dating of the upper 1,181 m of the Yakataga Formation at Middleton Island indicate that this part of the sequence probably was entirely deposited during the Matuyama reversed polarity epoch of the Pleistocene during which the sedimentation rate was of the order of 1 m/1,000 years. Lithologically similar deposits of poorly consolidated sandy mud and pebbly mud continue to accumulate locally near tidal glaciers in the same area, and older late Quaternary deposits are undoubtedly present offshore. The anomalous late Cenozoic glaciation recorded in the sediments along the Gulf of Alaska margin reflects a fortuitous combination of a subsiding shelf basin adjacent to an area of extremely high elevations and exceptionally heavy precipitation, an environment that persists to the present.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Recent and ancient sedimentary environments in Alaska: Proceedings of the Alaska Geological Society Symposium held April 2-4, 1975, at Anchorage, Alaska","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"Alaska Geological Society","publisherLocation":"Anchorage, AK","usgsCitation":"Plafker, G., and Addicott, W., 1976, Glaciomarine deposits of Miocene through Holocene age in the Yakataga Formation along the Gulf of Alaska margin, Alaska, <i>in</i> Recent and ancient sedimentary environments in Alaska: Proceedings of the Alaska Geological Society Symposium held April 2-4, 1975, at Anchorage, Alaska, p. Q1-Q23.","productDescription":"23 p.","startPage":"Q1","endPage":"Q23","costCenters":[],"links":[{"id":267358,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 172.5,51.2 ], [ 172.5,71.4 ], [ -130.0,71.4 ], [ -130.0,51.2 ], [ 172.5,51.2 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511cc402e4b0f79c4d2cebf3","contributors":{"editors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":509211,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":473732,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Addicott, W.O.","contributorId":17609,"corporation":false,"usgs":true,"family":"Addicott","given":"W.O.","affiliations":[],"preferred":false,"id":473733,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70043506,"text":"70043506 - 1976 - Beacon Hill end moraine, Boston: new explanation of an important urban feature","interactions":[{"subject":{"id":14425,"text":"ofr7557 - 1975 - Beacon Hill End Moraine, Boston; a new explanation of an important urban feature","indexId":"ofr7557","publicationYear":"1975","noYear":false,"title":"Beacon Hill End Moraine, Boston; a new explanation of an important urban feature"},"predicate":"SUPERSEDED_BY","object":{"id":70043506,"text":"70043506 - 1976 - Beacon Hill end moraine, Boston: new explanation of an important urban feature","indexId":"70043506","publicationYear":"1976","noYear":false,"title":"Beacon Hill end moraine, Boston: new explanation of an important urban feature"},"id":1}],"lastModifiedDate":"2013-02-20T13:04:04","indexId":"70043506","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Beacon Hill end moraine, Boston: new explanation of an important urban feature","docAbstract":"The usefulness of geology to engineers is in direct proportion to how well it helps us predict the subsurface; these predictions, in turn, depend on our knowledge of the geomorphic processes that molded the terrain. The uncertainties of interpretation are particularly great in glaciated terrain because our understanding of both glacial processes and history is so incomplete, a fact well illustrated in Beacon Hill. Recent construction activities in the eastern part of the hill, until now classified as a drumlin, have shown that it is better interpreted as an end moraine formed by a Wisconsonian glacial readvance. Instead of the firm till that was anticipated as foundation material, excavations exposed a complex of sand, gravel, and clay, with only minor zones of till. The structure of these deposits strongly suggests that originally they were plates of the glacial bed that froze to the glacier and were transported englacially. Thrust faulting and other deformations are glacial structures formed within the ice in the glacier's terminal zone. In spite of the complex englacial history, these deposits lost little of their original appearance and intergranular relationships. Upon deglaciation, the frozen moraine thawed, and slumping formed complex secondary structures on the ridge's lower flanks.","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Urban Gomorphology (Geological Society of America, Special Paper 174)","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Geological Society of America","publisherLocation":"Boulder, CO","usgsCitation":"Kaye, C., 1976, Beacon Hill end moraine, Boston: new explanation of an important urban feature, chap. <i>of</i> Urban Gomorphology (Geological Society of America, Special Paper 174), v. 174, p. 7-20.","productDescription":"14 p.","startPage":"7","endPage":"20","costCenters":[],"links":[{"id":267360,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts","city":"Boston","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.1911,42.2279 ], [ -71.1911,42.3989 ], [ -70.9232,42.3989 ], [ -70.9232,42.2279 ], [ -71.1911,42.2279 ] ] ] } } ] }","volume":"174","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"511cc3f7e4b0f79c4d2cebc8","contributors":{"editors":[{"text":"Coates, Donald R.","contributorId":111569,"corporation":false,"usgs":true,"family":"Coates","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":509212,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Kaye, Clifford A.","contributorId":17624,"corporation":false,"usgs":true,"family":"Kaye","given":"Clifford A.","affiliations":[],"preferred":false,"id":473735,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70007417,"text":"70007417 - 1976 - Journal of Research of the U. S. Geological Survey, 1976, volume 4, issue 6","interactions":[],"lastModifiedDate":"2022-04-20T20:36:31.408617","indexId":"70007417","displayToPublicDate":"2012-02-07T08:32:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Journal of Research of the U. S. Geological Survey, 1976, volume 4, issue 6","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70007417","usgsCitation":"U.S. Geological Survey, 1976, Journal of Research of the U. S. Geological Survey, 1976, volume 4, issue 6, 132 p., https://doi.org/10.3133/70007417.","productDescription":"132 p.","costCenters":[],"links":[{"id":115866,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue6/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":399277,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31662.htm"},{"id":399276,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31660.htm"},{"id":399275,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31659.htm"},{"id":204642,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/journal/1976/vol4issue6/report-thumb.jpg"},{"id":399274,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_31658.htm"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a401de4b0c8380cd64ac3"}
]}