{"pageNumber":"385","pageRowStart":"9600","pageSize":"25","recordCount":10959,"records":[{"id":70230341,"text":"70230341 - 1976 - Water-quality data for canals in eastern Broward County, Florida 1969-1974","interactions":[],"lastModifiedDate":"2025-04-25T15:16:23.144223","indexId":"70230341","displayToPublicDate":"1976-01-01T00:00:00","publicationYear":"1976","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"FL 75-009","displayTitle":"Water-Quality Data for Canals in Eastern Broward County, Florida 1969-1974","title":"Water-quality data for canals in eastern Broward County, Florida 1969-1974","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70230341","collaboration":"Prepared in cooperation with Broward County Environmental Quality Control Board and Central and Southern Florida Flood Control District","usgsCitation":"Waller, B., Miller, W.L., and Beaven, T., 1976, Water-quality data for canals in eastern Broward County, Florida 1969-1974: Open-File Report FL 75-009, 156 p., https://doi.org/10.3133/70230341.","productDescription":"156 p.","numberOfPages":"156","costCenters":[{"id":27821,"text":"Caribbean-Florida Water Science Center","active":true,"usgs":true}],"links":[{"id":398315,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70230341/coverthb.jpg"},{"id":398316,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70230341/ofr-fl-75009.pdf","text":"Report","size":"5.22 MB","linkFileType":{"id":1,"text":"pdf"},"description":"OFR FL 75-009"}],"country":"United States","state":"Florida","county":"Broward County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -80.54569321020263,\n              26.280939961326084\n            ],\n            [\n              -80.54569321020263,\n              26.023977390206696\n            ],\n            [\n              -80.07917922157858,\n              26.023977390206696\n            ],\n            [\n              -80.07917922157858,\n              26.280939961326084\n            ],\n            [\n              -80.54569321020263,\n              26.280939961326084\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","contact":"<p><a href=\"https://www.usgs.gov/centers/car-fl-water\" data-mce-href=\"https://www.usgs.gov/centers/car-fl-water\">Caribbean-Florida Water Science Center</a><br>U.S. Geological Survey<br>3321 College Avenue<br>Davie, FL 33314</p><p><a href=\"../contact\" data-mce-href=\"../contact\">Contact Pubs Warehouse</a></p>","publishedDate":"1975-10-01","noUsgsAuthors":false,"publicationDate":"1975-10-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Waller, B.G.","contributorId":75970,"corporation":false,"usgs":true,"family":"Waller","given":"B.G.","email":"","affiliations":[],"preferred":false,"id":840031,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, W. L.","contributorId":79128,"corporation":false,"usgs":true,"family":"Miller","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":840032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beaven, T.R.","contributorId":84757,"corporation":false,"usgs":true,"family":"Beaven","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":840033,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70157471,"text":"70157471 - 1975 - Ground-water resources and geology of Waukesha County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:36:47","indexId":"70157471","displayToPublicDate":"2015-05-11T09:00:00","publicationYear":"1975","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":"29","title":"Ground-water resources and geology of Waukesha County, Wisconsin","docAbstract":"<p>Good-quality water is available from the sand-and-gravel, Niagara, and sandstone aquifers in Waukesha County, Wis. As much as 15 gallons per minute (0.95 litres per second) can be obtained from wells almost everywhere in the county. Several hundred gallons per minute are available from aquifers in the glacial drift that fill bedrock valleys to thicknesses of 300 feet (91 metres) or more. Estimated well yields from much of the surficial outwash in western Waukesha County exceed 500 gallons per minute (31 litres per second). Estimated well yields from most of the Niagara aquifer, a dolomite as much as 325 feet (99 metres) thick in the eastern two-thirds of the county, exceed 50 gallons per minute (3.2 litres per second). The sandstone aquifer underlies the entire county and ranges in thickness from about 400 feet (120 metres) in the northwest corner to about 2,400 feet (730 metres) in the southeast corner. This aquifer yields more than 1,000 gallons per minute (63 litres per second) to wells over most of the county and is the principal source for municipal and subdivision water. Ground water in Waukesha County is of good quality and is suitable for most uses. Most of the water is a calcium magnesium bicarbonate type, is very hard [more than 180 mg/l (milligrams per litre) hardness], and requires softening for some uses. The ground water locally contains iron and manganese concentrations that exceed the limits (0.3 and 0.05 mg/l, respectively) recommended by the U.S. Public Health Service (1962, p. 7). Water high in sulfate and dissolved solids (saline water) is present locally in the Niagara and sandstone aquifers. Water from one well contained excessive nitrate (more than 45 mg/l). With one exception, wells sampled at irregular intervals indicated no significant changes in their chemical characteristics with time. About 24.3 million gallons per day (1.06 cubic metres per second) of ground water was pumped in the county in 1970. Sixty-two percent was withdrawn from the sandstone aquifer. More than one-half of the latter amount was for domestic use, and more than one-third was for industrial and commercial uses.&nbsp;</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Gonthier, J.B., 1975, Ground-water resources and geology of Waukesha County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 29, vii, 47 p.","productDescription":"vii, 47 p.","numberOfPages":"55","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308483,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350393,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic29/"}],"country":"United States","state":"Wisconsin","county":"Waukesha County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5401,43.1978],[-88.4183,43.1964],[-88.3027,43.1954],[-88.1827,43.1948],[-88.0639,43.194],[-88.0664,43.1076],[-88.0682,43.0202],[-88.0692,42.9725],[-88.0675,42.9334],[-88.0699,42.8447],[-88.1868,42.8451],[-88.3044,42.8444],[-88.5413,42.8445],[-88.5413,42.9341],[-88.5407,43.0232],[-88.5407,43.111],[-88.5401,43.1978]]]},\"properties\":{\"name\":\"Waukesha\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ecae4b058f706e512db","contributors":{"authors":[{"text":"Gonthier, Joseph B.","contributorId":74350,"corporation":false,"usgs":true,"family":"Gonthier","given":"Joseph","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573258,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157468,"text":"70157468 - 1975 - Ground-water resources and geology of Jefferson County, Wisconsin","interactions":[],"lastModifiedDate":"2018-01-08T19:37:35","indexId":"70157468","displayToPublicDate":"2015-04-13T08:00:00","publicationYear":"1975","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":"33","title":"Ground-water resources and geology of Jefferson County, Wisconsin","docAbstract":"<p>A steadily increasing population in Jefferson County, Wisconsin, is expanding the need for good-quality ground water. This need can be met by good-quality water available from the sand-and-gravel, Galena-Platteville, and sandstone aquifers. As much as 15 gallons per minute (0.95 liters per second) can be obtained from wells almost everywhere in the county. Yields of more than 1,000 gallons per minute (63 liters per second) are available from glacial drift where it contains a sufficient thickness of saturated sand and gravel. The Galena-Platteville aquifer is a dolomite that occurs mainly in the eastern one-half of the county and is locally more than 300 feet (90 meters) thick. Estimated well yields from this aquifer exceed 500 gallons per minute (32 liters per second). The sandstone aquifer underlies nearly the entire county except for small areas in the northwest corner. It is more than 1,100 feet (330 meters) thick in the southwest along the Dane-Jefferson County line. This aquifer is capable of yielding more than 1,000 gallons per minute (63 liters per second) to wells in much of the county and is the principal source of municipal water. The chemical quality of water from the three aquifers is similar. The water is very hard, having a median hardness between 315 and 325 milligrams per liter. Median values for dissolved solids range between 325 and 349 milligrams per liter. Iron and manganese commonly are present in bothersome amounts (combined total exceeding 0.3 milligrams per liter. About 13.0 million gallons per day (0.570 cubic meters per second) of ground water was pumped in the county in 1972, 87 percent from the sandstone aquifer. About 62 percent of the total water pumped was for industrial and commercial purposes, 26 percent for residential use, and 12 percent for municipal, irrigation, and institutional use.</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Borman, R.G., and Trotta, L.C., 1975, Ground-water resources and geology of Jefferson County, Wisconsin: Wisconsin Geological & Natural History Survey Information Circular 33, vi, 31 p.","productDescription":"vi, 31 p.","numberOfPages":"39","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308479,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350394,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic33/"}],"country":"United States","state":"Wisconsin","county":"Jefferson County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.5401,43.1978],[-88.5407,43.111],[-88.5407,43.0232],[-88.5413,42.9341],[-88.5413,42.8445],[-88.66,42.8453],[-88.7757,42.8455],[-88.8951,42.8457],[-89.0119,42.8471],[-89.013,42.8762],[-89.0132,42.9353],[-89.0107,43.0271],[-89.0109,43.0849],[-89.01,43.1131],[-89.0094,43.2],[-88.8919,43.1995],[-88.7732,43.1998],[-88.6563,43.1986],[-88.5401,43.1978]]]},\"properties\":{\"name\":\"Jefferson\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ec9e4b058f706e512d5","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":573252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trotta, L. C.","contributorId":63410,"corporation":false,"usgs":true,"family":"Trotta","given":"L.","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573253,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70046307,"text":"70046307 - 1975 - Geology of Griggs and Steele Counties","interactions":[],"lastModifiedDate":"2018-05-23T12:18:49","indexId":"70046307","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"64-1","title":"Geology of Griggs and Steele Counties","docAbstract":"Griggs and Steele Counties, located at the eastern edge of the Williston basin, are underlain by 400 to 2,600 feet of Paleozoic and Mesozoic rocks that dip gently to the west. The Cretaceous Greenhorn, Carlile, Niobrara, and Pierre Formations lie directly beneath the glacial drift, and shale of the Pierre Formation is exposed in several places along the Sheyenne River. The Pleistocene Coleharbor Formation, which covers most of the area, consists mainly of glacial, fluvial, and lake sediment. The Coleharbor Formation averages 200 to 300 feet thick, but it is as much as 550 feet thick in some of the buried valleys. The Holocene Walsh Formation occurs in parts of the area, chiefly sloughs and river bottomland. It consists mainly of alluvial and eolian sediment. Griggs County and the western two-thirds of Steele County are part of the Drift Prairie, which is characterized by flat to gently rolling topography that is rugged in areas of end moraines and intense ice thrusting, subdued on the ground moraine and outwash plains. Associated with these major landforms are numerous washboard moraines, drumlins, eskers, kames, meltwater trenches, and water-washed areas. The eastern third of Steele County is a nearly flat area covered by lake deposits of the glacial Lake Agassiz. As the Late Wisconsinan glacier in eastern North Dakota thinned and receded eastward, it was increasingly affected by the topography over which it was flowing. This resulted in lobation of the glacier. Locally intense areas of thrusting developed within the lobate glacier, and large blocks of subglacial material were moved short distances. Large areas of Griggs County were washed by water flowing from the glacier, and in some areas gravel and sand were deposited. Continued withdrawal of the glacier resulted in ponding of melt water in parts of the two counties. These and other ponds tended to coalesce at lower and lower elevations, eventually forming Lake Agassiz, which flooded part of eastern Steele County.","language":"English","publisher":"North Dakota Geological Survey","publisherLocation":"Grand Forks, ND","collaboration":"Prepared by the North Dakota Geological Survey in cooperation with the North Dakota State Water Commission, the water management districts of Griggs and Steele Counties, and the United States Geological Survey; this report was also published as North Dakota County Ground-Water Studies 21-1","usgsCitation":"Bluemle, J.P., 1975, Geology of Griggs and Steele Counties: Bulletin 64-1, vii, 49 p.; Maps: 2 Sheets: 36 x 18 inches.","productDescription":"vii, 49 p.; Maps: 2 Sheets: 36 x 18 inches","numberOfPages":"50","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":273368,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70046307.png"},{"id":273366,"type":{"id":11,"text":"Document"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-251/GriggsSteele_Part_1.pdf"},{"id":273367,"type":{"id":17,"text":"Plate"},"url":"https://www.swc.nd.gov/4dlink9/4dcgi/GetSubContentPDF/PB-252/GriggsSteele_Part_1_Plates.pdf"}],"country":"United States","state":"North Dakota","county":"Griggs County, Steele County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98.5019,47.2394 ], [ -98.5019,47.6742 ], [ -97.4504,47.6742 ], [ -97.4504,47.2394 ], [ -98.5019,47.2394 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51b1bbd2e4b022a6a540f9cb","contributors":{"authors":[{"text":"Bluemle, John P.","contributorId":104375,"corporation":false,"usgs":true,"family":"Bluemle","given":"John","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":479433,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70039598,"text":"70039598 - 1975 - Norfolk and environs: A land use perspective","interactions":[],"lastModifiedDate":"2012-08-15T01:02:00","indexId":"70039598","displayToPublicDate":"2012-01-01T11:18:48","publicationYear":"1975","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}},"seriesNumber":"Volume 2, Part A","title":"Norfolk and environs: A land use perspective","docAbstract":"The Norfolk-Portsmouth Standard Metropolitan Statistical Area (SMSA) in southeastern Virginia was the site of intensive testing of a number of land resources assessment methods, built around the availability of remotely sensed data from the Earth Resources Technology Satellite (ERTS-I), later renamed LANDSAT I. The Norfolk tests were part of a larger experiment known as the Central Atlantic Regional Ecological Test Site (CARETS), designed to test the extent to which LANDSAT and associated high-altitude aircraft data could be used as cost-effective inputs to a regional land use information system. The Norfolk SMSA contains a variety of land uses typical of the urbanized eastern seaboard, along with typical associated problems: rapid urbanization; heavy recreational, commercial, and residential demands on fragile beaches and coastal marsh environments; industrial, transportation, and governmental land and water uses impacting on residential and agricultural areas; drainage and land stability difficulties affecting construction and other uses; and increasing difficulties in maintaining satisfactory air and water quality.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039598","collaboration":"Sponsored jointly by the National Aeronautics and Space Administration and the U.S. Geological Survey","usgsCitation":"Alexander, R.H., Buzzanell, P.J., Fitzpatrick, K.A., Lins, H.F., and McGinty, H.K., 1975, Norfolk and environs: A land use perspective: Final Report Volume 2, Part A, viiii, 348 p., https://doi.org/10.3133/70039598.","productDescription":"viiii, 348 p.","numberOfPages":"363","costCenters":[{"id":296,"text":"Geography Program","active":false,"usgs":true}],"links":[{"id":259601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Delaware;Maryl;New Jersey;North Carolina;Pennsylvania;Virginia","city":"Norfolk;Portsmouth;Washington D.C.","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78,36 ], [ -78,38 ], [ -75,38 ], [ -75,36 ], [ -78,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a67bae4b0c8380cd7347b","contributors":{"authors":[{"text":"Alexander, Robert H.","contributorId":53807,"corporation":false,"usgs":true,"family":"Alexander","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buzzanell, Peter J.","contributorId":30083,"corporation":false,"usgs":true,"family":"Buzzanell","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":466533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzpatrick, Katherine A.","contributorId":54846,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Katherine","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466536,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":466532,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McGinty, Herbert K. III","contributorId":43214,"corporation":false,"usgs":true,"family":"McGinty","given":"Herbert","suffix":"III","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":466534,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70039597,"text":"70039597 - 1975 - Norfolk and environs: A land use perspective","interactions":[],"lastModifiedDate":"2012-08-15T01:02:00","indexId":"70039597","displayToPublicDate":"2012-01-01T10:44:03","publicationYear":"1975","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}},"seriesNumber":"Volume 2, Part A","title":"Norfolk and environs: A land use perspective","docAbstract":"The Norfolk-Portsmouth Standard Metropolitan Statistical Area (SMSA) in southeastern Virginia was the site of intensive testing of a number of land resources assessment methods, built around the availability of remotely sensed data from the Earth Resources Technology Satellite (ERTS-I), later renamed LANDSAT I. The Norfolk tests were part of a larger experiment known as the Central Atlantic Regional Ecological Test Site (CARETS), designed to test the extent to which LANDSAT and associated high-altitude aircraft data could be used as cost-effective inputs to a regional land use information system. The Norfolk SMSA contains a variety of land uses typical of the urbanized eastern seaboard, along with typical associated problems: rapid urbanization; heavy recreational, commercial, and residential demands on fragile beaches and coastal marsh environments; industrial, transportation, and governmental land and water uses impacting on residential and agricultural areas; drainage and land stability difficulties affecting construction and other uses; and increasing difficulties in maintaining satisfactory air and water quality.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/70039597","collaboration":"Sponsored jointly by the National Aeronautics and Space Administration and the U.S. Geological Survey","usgsCitation":"Alexander, R.H., Buzzanell, P.J., Fitzpatrick, K.A., Lins, H.F., and McGinty, H.K., 1975, Norfolk and environs: A land use perspective: Final Report Volume 2, Part A, viii, 348 p.; 11 Plates: 85 x 104 cm. or smaller, https://doi.org/10.3133/70039597.","productDescription":"viii, 348 p.; 11 Plates: 85 x 104 cm. or smaller","numberOfPages":"363","costCenters":[{"id":296,"text":"Geography Program","active":false,"usgs":true}],"links":[{"id":259603,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Delaware;Maryl;New Jersey;North Carolina;Pennsylvania;Virginia","city":"Norfolk;Portsmouth;Washinton;D.C.","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -78,36 ], [ -78,38 ], [ -75,38 ], [ -75,36 ], [ -78,36 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a67b9e4b0c8380cd73475","contributors":{"authors":[{"text":"Alexander, Robert H.","contributorId":53807,"corporation":false,"usgs":true,"family":"Alexander","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":466530,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Buzzanell, Peter J.","contributorId":30083,"corporation":false,"usgs":true,"family":"Buzzanell","given":"Peter","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":466528,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fitzpatrick, Katherine A.","contributorId":54846,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"Katherine","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":466531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lins, Harry F. 0000-0001-5385-9247 hlins@usgs.gov","orcid":"https://orcid.org/0000-0001-5385-9247","contributorId":1505,"corporation":false,"usgs":true,"family":"Lins","given":"Harry","email":"hlins@usgs.gov","middleInitial":"F.","affiliations":[{"id":502,"text":"Office of Surface Water","active":true,"usgs":true}],"preferred":true,"id":466527,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"McGinty, Herbert K. III","contributorId":43214,"corporation":false,"usgs":true,"family":"McGinty","given":"Herbert","suffix":"III","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":466529,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":5224810,"text":"5224810 - 1975 - Emperor penguins nesting on Inaccessible Island","interactions":[],"lastModifiedDate":"2012-02-02T00:15:10","indexId":"5224810","displayToPublicDate":"2010-06-16T12:19:11","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":812,"text":"Antarctic Journal of the United States","active":true,"publicationSubtype":{"id":10}},"title":"Emperor penguins nesting on Inaccessible Island","docAbstract":"Emperor penguins were observed nesting on Inaccessible I. during the 1973 winter. This is the southernmost nesting of emperor penguins thus far recorded; it also could be the first record of emperors attempting to start a new rookery. This site, however, may have been used by emperors in the past. The closest reported nesting of these penguins to Inaccessible I. is on the Ross Ice Shelf east of Cape Crozier. With the exception of the Inaccessible I. record, there is little evidence that emperor penguins breed in McMurdo Sound proper.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Antarctic Journal of the United States","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"6806_Jonkel.pdf","usgsCitation":"Jonkel, G., and Llano, G., 1975, Emperor penguins nesting on Inaccessible Island: Antarctic Journal of the United States, v. 9, no. 3, p. 93-95.","productDescription":"93-95","startPage":"93","endPage":"95","numberOfPages":"3","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":196376,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"9","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db6056db","contributors":{"authors":[{"text":"Jonkel, G.M.","contributorId":55104,"corporation":false,"usgs":true,"family":"Jonkel","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":342748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Llano, G.A.","contributorId":56335,"corporation":false,"usgs":true,"family":"Llano","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":342749,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70164431,"text":"70164431 - 1975 - Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana","interactions":[],"lastModifiedDate":"2016-02-03T17:15:44","indexId":"70164431","displayToPublicDate":"2008-12-28T00:00:00","publicationYear":"1975","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":"Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana","docAbstract":"<p>A gravity survey of the Henrys Lake quadrangle shows that a gravity low with about 10 milligals of closure coincides with the Henrys Lake basin. The low is interpreted to reflect a basin fill of 1,100 m or more of Cenozoic sediments and volcanic rock. The data indicate that on the east and probably on the west the basin is bounded by northwest- and north-trending faults, and near its waist by the east-trending Centennial fault. A model constructed across the Henrys Lake basin suggests a northwest-trending fault, located near the southeast corner of Henrys Lake and concealed beneath the basin fill. The sparse gravity data east of the Centennial Mountains are not sufficient to provide any evidence on the extension of the Centennial fault across the Henrys Lake basin.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","usgsCitation":"Peterson, D.L., and Witkind, I.J., 1975, Preliminary results of a gravity survey of the Henrys Lake quadrangle, Idaho and Montana: Journal of Research of the U.S. Geological Survey, v. 3, no. 2.","productDescription":"6 p.","startPage":"228","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":316566,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":316565,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/journal/1975/vol3issue2/report.pdf","text":"Report","size":"28.00 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Idaho, Montana, Wyoming","otherGeospatial":"Henrys Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111,\n              44.25\n            ],\n            [\n              -111,\n              45\n            ],\n            [\n              -111.75,\n              45\n            ],\n            [\n              -111.75,\n              44.25\n            ],\n            [\n              -111,\n              44.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"3","issue":"2","edition":"223","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56b33320e4b0cc79997f3420","contributors":{"authors":[{"text":"Peterson, Donald L.","contributorId":28597,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":597214,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkind, Irving J.","contributorId":14469,"corporation":false,"usgs":true,"family":"Witkind","given":"Irving","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":597215,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010132,"text":"70010132 - 1975 - Elevation changes in the central Transverse Ranges near Ventura, California","interactions":[],"lastModifiedDate":"2025-08-29T16:31:40.639785","indexId":"70010132","displayToPublicDate":"2003-04-10T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Elevation changes in the central Transverse Ranges near Ventura, California","docAbstract":"<p>Profiles of elevation changes developed from repeated levelings in the east-trending Transverse Ranges near Ventura, California, reveal three general types of vertical movements: </p><p>1. (1) broadly defined regional tilting; </p><p>2. (2) sharply defined differential movements across recently active faults; and </p><p>3. (3) differential subsidence centering on producing oil fields. </p><p>Down-to-the-southeast tilting is evident in profiles along the coast this sense of movement, however, is the inverse of that that may have prevailed during late Pleistocene time. Profiles along lines extending north and northwest from Ventura show prominent inflections formed by up-to-the-north differential movements that coincide roughly with the Red Mountain fault; this fault is a north-dipping reverse fault that displaces a Holocene(?) soil zone and along which scarps and sag ponds are preserved. A similar inflection coincides with the Padre Juan fault; post-Pleistocene activity on the Padre Juan, however, is uniquely indicated by the geodetic data. Contemporary integrity of the structural block extending northward from the Red Mountain fault is suggested by the apparent absence of differential movements across the Munson Creek, Tule Creek, Santa Ynez, and Arroyo Parida faults since at least 1934. Subsidence is recognized over both the Ventura and Rincon oil fields; although maximum subsidence has not been recorded in either case, 277 mm of differential subsidence was measured within the Ventura field between 1934 and 1968.&nbsp;</p>","language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-444-41420-5.50018-6","issn":"00401951","usgsCitation":"Buchanan-Banks, J.M., Castle, R.O., and Ziony, J., 1975, Elevation changes in the central Transverse Ranges near Ventura, California: Tectonophysics, v. 29, no. 1-4, p. 113-125, https://doi.org/10.1016/B978-0-444-41420-5.50018-6.","productDescription":"13 p.","startPage":"113","endPage":"125","costCenters":[],"links":[{"id":219052,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","city":"Ventura","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.42138671875,\n              34.20498790244057\n            ],\n            [\n              -119.00527954101562,\n              34.20498790244057\n            ],\n            [\n              -119.00527954101562,\n              34.34230217446123\n            ],\n            [\n              -119.42138671875,\n              34.34230217446123\n            ],\n            [\n              -119.42138671875,\n              34.20498790244057\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a08cbe4b0c8380cd51c95","contributors":{"authors":[{"text":"Buchanan-Banks, Jane M.","contributorId":29421,"corporation":false,"usgs":true,"family":"Buchanan-Banks","given":"Jane","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":358061,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Castle, Robert O.","contributorId":22741,"corporation":false,"usgs":true,"family":"Castle","given":"Robert","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":358062,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ziony, Joseph I.","contributorId":16829,"corporation":false,"usgs":true,"family":"Ziony","given":"Joseph I.","affiliations":[],"preferred":false,"id":358060,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010147,"text":"70010147 - 1975 - Garnet peridotite xenoliths in a Montana, U.S.A., kimberlite","interactions":[],"lastModifiedDate":"2025-07-09T16:00:37.465035","indexId":"70010147","displayToPublicDate":"2003-03-26T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3067,"text":"Physics and Chemistry of the Earth","active":true,"publicationSubtype":{"id":10}},"title":"Garnet peridotite xenoliths in a Montana, U.S.A., kimberlite","docAbstract":"<div id=\"abstracts\" class=\"Abstracts u-font-serif\"><div id=\"abs1\" class=\"abstract author\"><div id=\"abssec1\"><p id=\"spara1\">Within a swarm of late middle Eocene subsilicic-alkalic diatremes, one diatreme 270 by 370 m and an associated dike contain common xenoliths of granulite and rare xenoliths of spinel peridotite and garnet peridotite. Six garnet lherzolite xenoliths have been found and these show a range of textures. Four are granular, and two are intensely sheared. Phlogopite is absent from the intensely sheared xenoliths and is thought to be primary in part in the granular xenoliths. Estimated temperatures and depths of equilibration of xenolith pyroxenes range from 920<sup>°</sup>C, 106 km (32 kbar) to 1315<sup>°</sup>C, 148 km (47 kbar). The xenoliths show increasing amounts of deformation with greater inferred depths of origin. The temperature-depth points suggest a segment of an Eocene geotherm for Montana which is similar in slope to the steep portion of the pyroxene-determined Lesotho geotherm (BOYD and NIXON, this volume) and is considerably steeper than typical calculated shield and continental geotherms at present. The steep trend could be a result of plate-tectonic shearing and magma ascension within an Eocene low-velocity zone. Preservation of intensely sheared textures requires rapid transport of material from about 150 km depth during active deformation of relatively dry rock. The occurrence of monticellite peridotite in this kimberlite diatreme suggests that magmas which crystallized to monticellite peridotite at relatively shallow depth could be one of the primitive types of kimberlite magma.</p></div></div></div><ul id=\"issue-navigation\" class=\"issue-navigation u-margin-s-bottom u-bg-grey1\"></ul>","language":"English","publisher":"Elsevier","doi":"10.1016/B978-0-08-018017-5.50023-7","issn":"00791946","usgsCitation":"Carter, H.B., and Boyd, F., 1975, Garnet peridotite xenoliths in a Montana, U.S.A., kimberlite: Physics and Chemistry of the Earth, v. 9, p. 247-255, https://doi.org/10.1016/B978-0-08-018017-5.50023-7.","productDescription":"9 p.","startPage":"247","endPage":"255","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":219353,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70184367,"text":"70184367 - 1975 - Descriptions and chemical analyses for selected wells in the Tehama-Colusa Canal Service Area, Sacramento Valley, California","interactions":[],"lastModifiedDate":"2017-03-09T13:46:41","indexId":"70184367","displayToPublicDate":"1999-12-26T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Descriptions and chemical analyses for selected wells in the Tehama-Colusa Canal Service Area, Sacramento Valley, California","docAbstract":"<p>The Tehama-Colusa Canal Service Area is in the northwestern part of the Sacramento Valley, in parts of Yolo, Colusa, Glenn, and Tehama Counties. The area includes 450 square miles (1,160 square kilometres). The boundaries are: West, the eastern slopes of the Coast Ranges; north, Elder Creek; northeast, the Sacramento River and the Glenn-Colusa Canal; east and southeast, the Colusa Basin Drainage Canal; and south, Oat Creek. </p><p>Between April and July 1974, 393 wells were selectively canvassed and between August and October 1974, water samples were collected for chemical analysis from 222 wells of the 393 wells canvassed. Field determinations of alkalinity, conductance, pH, and temperature were made on the site at the time of sampling. The samples were then field prepared for shipment and analysis for individual constituents at the Geological Survey Central Laboratory, Salt Lake City, Utah. Descriptive data for water wells are listed in table 1, chemical data in tables 2 and 3, and the location of these wells is shown on maps 1-28. </p><p></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70184367","collaboration":"Prepared in cooperation with the California Department of Water Resources","usgsCitation":"Fogelman, R.P., 1975, Descriptions and chemical analyses for selected wells in the Tehama-Colusa Canal Service Area, Sacramento Valley, California: Open-File Report, iv, 52 p., https://doi.org/10.3133/70184367.","productDescription":"iv, 52 p.","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true}],"links":[{"id":337024,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":337223,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70184367/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":2580,"text":"wsp2030 - 1975 - Summary of floods in the United States during 1969","interactions":[{"subject":{"id":55898,"text":"ofr6980 - 1969 - Flood of July 27-28, 1969, in southeastern New York","indexId":"ofr6980","publicationYear":"1969","noYear":false,"title":"Flood of July 27-28, 1969, in southeastern New York"},"predicate":"SUPERSEDED_BY","object":{"id":2580,"text":"wsp2030 - 1975 - Summary of floods in the United States during 1969","indexId":"wsp2030","publicationYear":"1975","noYear":false,"title":"Summary of floods in the United States during 1969"},"id":1}],"lastModifiedDate":"2015-09-29T16:32:08","indexId":"wsp2030","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2030","title":"Summary of floods in the United States during 1969","docAbstract":"<p>The most outstanding floods in the United States during 1969 are described in chronological order. The areas most seriously affected by flooding were: Central and southern California (January and February); the upper Midwestern States of North Dakota, South Dakota, Minnesota, Iowa, Wisconsin, and Illinois (April); north-central Ohio (July); Mississippi, Alabama, and Virginia (Hurricane Camille in August); and Florida and Georgia (September). Severe floods in central and southern California were caused by three storms during January and February. At least 60 lives were lost. Homes and property were destroyed or damaged, by rainstorms, floods, and mudflows. Many floods approached or exceeded the maximum known. The severe flood damage was due partly to recent home construction in floodprone areas. The April floods in the upper Midwestern States of North Dakota, South Dakota, Minnesota, Iowa, Wisconsin, and Illinois were expected because of a large accumulation of snow containing as much as 8 inches of water. Flood-protection procedures, together with cool temperatures, had a mitigating effect on the flood. The floods were the largest since the late 1800's, and their recurrence intervals exceeded 50 years at many of the gaged sites. Estimates of flood damage were about $147 million. More than a million acres of rich agricultural land were inundated, thousands of culverts and bridges were washed out, 23,000 people were forced from their homes and 11 lives were lost in the six-State flood area. Intense rainstorms and wind with gusts as much as 100 miles per hour, July 4-5, caused record floods in north-central Ohio, July 4-8. The storm and floods left trees uprooted, more than $66 million in damage, and 41 deaths. In many places the floods were the largest of record. Together with the wind and rainstorm, the hydrologic conditions were among the most significant experienced in the area. Hurricane Camille was the most intense hurricane on record to enter the United States mainland. It struck the Mississippi-Alabama coast on August 18, with tidal waves as high as 25 feet above mean sea level and wind velocities more than 190 miles per hour. Tidal wave and flood damage was about $1.3 billion. In Mississippi the known dead totaled 139 and 76 other persons were missing. The hurricane intensity decreased as it moved inland until it merged with severe rainstorms over the Appalachian mountains. The intensified hurricane then caused record-breaking floods of streams in a 50-mile-wide area as it moved eastward from Sulphur Springs, W. Va., to Fredericksburg, Va. Total flood damage in Virginia exceeded $116 million. There were 113 known deaths, 102 injuries, and 39 people missing. A tropical storm that was nearly stationary over northwest Florida for about 48 hours, September 20-23 produced record rains and floods. Near Quincy, Fla., the total rainfall for the period exceeded 20 inches. On Little River near Quincy, the peak discharge was nearly twice the previous maximum of record and was three times that of a 50-year flood. Flood damage to agricultural lands, bridges, culverts, and roads was about $1.7 million.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2030","collaboration":"Prepared in cooperation with Federal, State, and local agencies","usgsCitation":"Reid, J., 1975, Summary of floods in the United States during 1969: U.S. Geological Survey Water Supply Paper 2030, Report: 173 p.; Preceding Publications, https://doi.org/10.3133/wsp2030.","productDescription":"Report: 173 p.; Preceding Publications","numberOfPages":"180","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":138152,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2030/report-thumb.jpg"},{"id":28856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2030/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Most of these deposits are in the State of Para, but some are in Amazonas and Maranhao.</p><p>Discovery of large-scale resources of bauxite in the Amazon Region is so recent that mining has not begun, but government geologists estimate the total resources in aluminum deposits in the lower Amazon to be in the multibillion ton range.</p><p>The annual production rate of bauxite ore in Brazil, much of it from Pops de Caldas in Minas Gerais, is about 760,000 metric tons of ore from which about 100,000 tons of aluminum metal is produced, most of which is consumed by Brazilian industry.</p><p>The Amazon bauxite deposits are on terraces formed on sedimentary rocks of Tertiary age; in Minas Gerais the deposits are formed on Precambrian metasedimentary rock, and at Poos de Caldas on a circular alkalic pluton of Cretaceous age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7530","usgsCitation":"White, M.G., 1975, Aluminum resources of Brazil: U.S. Geological 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Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":172986,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26123,"text":"wri7450 - 1975 - Stream reconnaissance for nutrients and other water-quality parameters, Greater Pittsburgh Region, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-07T08:58:07","indexId":"wri7450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"50-74","title":"Stream reconnaissance for nutrients and other water-quality parameters, Greater Pittsburgh Region, Pennsylvania","docAbstract":"<p>Eighty-five stream sites in and near the six-county Greater Pittsburgh Region were sampled in mid-June 1971 in mid-October 1972. Data are reported for 89 sites because 4 substitute sites were sampled in the second period. Drainage areas of the basins sampled ranged from 4.1 to 19,5000 square miles (10.6 to 50,500 square kilometres). The chemical analyses included constituents of three general classes: (1) nutrients, (2) activity indicators, and (3) dominant anions. Modification of the natural chemical and physical characteristics of the surface waters by man's activities is evident in some of the data. However, the activities are so diverse in type and in areal extent that their influence in terms of cause and effect is often obscure.</p>\n<br>\n<p>Nutrient concentrations were high enough to indicate potential problems at about a quarter of the sampling sites. Temperature, dissolved oxygen, and pH values indicated a generally favorable capacity for regeneration or recovery from degradation, although a number a streams east of the Allegheny and Monongahela Rivers are marginal or lacking in the capacity. Regionally, sulfate is the dominant ion and was observed in concentrations of 40 milligrams per litre or more at 90 percent of the sites. Bicarbonate exceeded 100 milligrams per litre at 22 sites. A moderate to high degree of mineralization, as indicated by conductance readings of more than 500 micromhos per cetrimetre at half of the sampling sites, is a characteristic of the region's surface waters.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7450","usgsCitation":"Beall, R.M., 1975, Stream reconnaissance for nutrients and other water-quality parameters, Greater Pittsburgh Region, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 50-74, Report: iv, 47 p.; 2 Plates: 16.60 x 21.93 inches and 13.75 and 16.71 inches, https://doi.org/10.3133/wri7450.","productDescription":"Report: iv, 47 p.; 2 Plates: 16.60 x 21.93 inches and 13.75 and 16.71 inches","numberOfPages":"54","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":286676,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":286673,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0050/plate-1.pdf"},{"id":286674,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0050/plate-2.pdf"},{"id":286675,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0050/report.pdf"}],"scale":"500000","country":"United States","state":"Pennsylvania","otherGeospatial":"Greater Pittsburgh Region","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.5,39.75 ], [ -80.5,41.25 ], [ -78.75,41.25 ], [ -78.75,39.75 ], [ -80.5,39.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a5141","contributors":{"authors":[{"text":"Beall, Robert M.","contributorId":90695,"corporation":false,"usgs":true,"family":"Beall","given":"Robert","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":195857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":11158,"text":"ofr75291 - 1975 - Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","interactions":[{"subject":{"id":11158,"text":"ofr75291 - 1975 - Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","indexId":"ofr75291","publicationYear":"1975","noYear":false,"title":"Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":2350,"text":"wsp1798D - 1968 - Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado","indexId":"wsp1798D","publicationYear":"1968","noYear":false,"chapter":"D","title":"Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado"},"id":1}],"supersededBy":{"id":2350,"text":"wsp1798D - 1968 - Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado","indexId":"wsp1798D","publicationYear":"1968","noYear":false,"title":"Fluvial sediment in the drainage area of K-79 reservoir, Kiowa Creek basin, Colorado"},"lastModifiedDate":"2024-05-08T18:50:29.639498","indexId":"ofr75291","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-291","title":"Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina","docAbstract":"<p>The sediment-transport characteristics of streams were determined in a 6,000-square-mile (15,500-square-kilometre) area of the Coastal Plain and Piedmont regions of eastern North Carolina during 1969-73. The study covered all or parts of 21 counties and included data for 28 sediment-sampling stations located in parts of 4 major river basins, the Roanoke, Pamlico, Neuse, and Cape Fear. Annual suspended-sediment yields ranged from 333 to 12 tons per square mile (117 to 4.2 tonnes per square kilometre). Streams in the Piedmont region have the highest yields. Suspended-sediment yield decreases in an eastward direction from the Piedmont to the Coastal Plain region.</p><p>Sediment characteristics are directly affected by topography, storm runoff, geology, land use, and man-made detention structures. At one sampling station in the 1973 water year 44 percent of the suspended sediment tonnage was transported during 34 days of high flow. In the Piedmont region, sediment yields vary indirectly with the percentage of forest cover in the basin, but there appears to be no definite relationship between forest cover and yield in the Coastal Plain region. Large lakes act as sediment-detention reservoirs. Average annual sediment yields ranged from 98 to 333 tons per square mile (34 to 117 tonnes per square kilometre) for 3 headwater streams which flow into Hyco Lake in Person County; however, the yield for the station less than 2 miles (3.2 kilometres) downstream from Hyco Dam was about 12 tons per square mile (4.2 tonnes per square kilometre).</p><p>Most suspended sediment during floods in Piedmont streams ranges in size from sand to silt, whereas the suspended material in flooding streams in the Coastal Plain is generally clay size.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75291","collaboration":"Prepared in cooperation with the North Carolina Department of Natural & Economic Resources","usgsCitation":"Simmons, C.E., 1975, Sediment characteristics of streams in the eastern Piedmont and western Coastal Plain regions of North Carolina: U.S. Geological Survey Open-File Report 75-291, v, 33 p., 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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc0b4","contributors":{"authors":[{"text":"Simmons, Clyde E.","contributorId":71528,"corporation":false,"usgs":true,"family":"Simmons","given":"Clyde","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":162642,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25980,"text":"wri7446 - 1975 - Evaluation of reservoir sites in North Carolina: Regional relations for estimating the reservoir capacity needed for a dependable water supply","interactions":[],"lastModifiedDate":"2020-08-06T02:01:45.865387","indexId":"wri7446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-46","title":"Evaluation of reservoir sites in North Carolina: Regional relations for estimating the reservoir capacity needed for a dependable water supply","docAbstract":"<p><span>Draft-storage-frequency relations, which show the storage required for a </span><span>reservoir to furnish a specified withdrawal or draft are regionalized for </span><span>four zones in the State, using the mean annual flow of the streams as an </span><span>index. The differences between the zones primarily reflect differences in </span><span>the variability of stream flow.</span></p><p><span>To assure the available draft will fall below 75 percent of the mean annual flow of a stream only once in 50 years on the average, a reservoir in the mountains would need a usable storage capacity of 45 percent of the mean annual runoff of the impounded stream. In comparison, reservoirs in parts of the Piedmont furnishing a draft of 75 percent of the mean annual flow must have usable storage equal to 60 percent of the mean annual runoff of the stream. In the inner Coastal Plain the storage required increases to 84 per-cent, and in the outer Coastal Plain to about 110 percent. These increases in storage necessary to furnish a certain draft are indicative of the general increase in streamflow variability, both seasonally and between years, that occurs from west to east in the State. </span></p><p><span>Net evaporative draft, the evaporative loss from reservoirs when annual evaporation exceeds annual precipitation, also varies from west to east. For instance, a reservoir impounding a Piedmont stream, and designed with a 5 percent chance of deficiency, will have a net evaporative draft about twice as large as a similar sized reservoir in the Coastal Plain. In the mountains, annual precipitation always exceeds evaporation because of the cooler temperatures and higher rates of precipitation. </span></p><p><span>Annual net evaporation is also proportionately smaller for large reser</span><span>voirs than for small ones. On a Coastal Plain reservoir, with storage equivalent to the mean annual runoff of the stream and being drafted at 90 percent of the mean annual flow, the net evaporation for a stream with a mean annual runoff of only 500 acre-feet (0.62 cubic hectometres) is three times as great as for a stream with mean annual runoff of 100,000 acre-feet (123 cubic hectometres). Thus, one large reservoir has less evaporation loss than several small ones capable of furnishing, collectively, the same reliable draft.</span></p><p><span>Under some circumstances, sedimentation can quickly reduce the available storage in a reservoir, thus decreasing the reliable draft. Estimated sedi-mentation rates in the Piedmont can range from 240 acre-feet per year (0.3 cubic hectometres per year) in a severely exposed drainage basin of 10 square miles (26 square kilometres) to 0.4 acre-feet per year (493 cubic metres per year) in a wooded basin of the same size. </span></p><p><span>Seepage beneath and around a reservoir dam is normally not significant in the State. The usual engineering practices should be followed, however, to avoid locating the dam on an open or active fault, cavernous limestone, or continuous beds of sand or gravel. </span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7446","collaboration":"Prepared in cooperation with the North Carolina Department of Natural and Economic Resources","usgsCitation":"Arteaga, F., and Hubbard, E., 1975, Evaluation of reservoir sites in North Carolina: Regional relations for estimating the reservoir capacity needed for a dependable water supply: U.S. Geological Survey Water-Resources Investigations Report 74-46, Report: v, 60 p.; 1 Plate: 34.95 x 16.66 inches, https://doi.org/10.3133/wri7446.","productDescription":"Report: v, 60 p.; 1 Plate: 34.95 x 16.66 inches","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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F.","contributorId":66666,"corporation":false,"usgs":true,"family":"Hubbard","given":"E. F.","affiliations":[],"preferred":false,"id":195581,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25860,"text":"wri7442 - 1975 - Water resources of the Toppenish Creek Basin, Yakima Indian Reservation, Washington","interactions":[],"lastModifiedDate":"2013-07-15T15:37:00","indexId":"wri7442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-42","title":"Water resources of the Toppenish Creek Basin, Yakima Indian Reservation, Washington","docAbstract":"The Yakima River, which flows along the eastern margin of the Yakima Indian Reservation, provides about 93 percent of the irrigation water for the eastern part of the Toppenish Creek basin--the major agricultural area in the basin . During 1972, the total surface water diverted from all streams and from ground-water irrigation was nearly 700,000 acre-feet (863 million cubic metres).","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wri7442","collaboration":"Prepared in cooperation with the Yakima Tribal Council","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1975, Water resources of the Toppenish Creek Basin, Yakima Indian Reservation, Washington: U.S. Geological Survey Water-Resources Investigations Report 74-42, viii, 144 p., https://doi.org/10.3133/wri7442.","productDescription":"viii, 144 p.","costCenters":[],"links":[{"id":158292,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":271058,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0042/report.pdf"}],"country":"United States","state":"Washington","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.7857,45.5435 ], [ -124.7857,49.0024 ], [ -116.9156,49.0024 ], [ -116.9156,45.5435 ], [ -124.7857,45.5435 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f02fd","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":529222,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":19428,"text":"ofr75336 - 1975 - Low-flow Characteristics of Eau Claire River Basin near Antigo, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-13T09:31:06","indexId":"ofr75336","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-336","title":"Low-flow Characteristics of Eau Claire River Basin near Antigo, Wisconsin","docAbstract":"<p>This report presents low-flow characteristics at six sites on streams in the Eau Claire River basin near Antigo, Wis., where applications for irrigation permits were made. The low-flow characteristics presented are the annual minimum 7-day mean flows at the 2-year recurrence interval and 10-year recurrence interval. A seepage run made October 10, 1974, showed a substantial gain in discharge from site 2 (3.75 ft3/s [cubic feet per second] or 0.11 m3/s (cubic metres per second) to site 6 (30.6 ft3/s or 0.87 m3/s) on the East Branch Eau Claire River and from site 12 (3.98 ft3/s or 0.11 m3/s) to site 16 (18.1 ft3/s or 0.51 m3/s) on the West Branch Eau Claire River; a fairly constant discharge between sites 6 (30.6 ft3/s or 0.87 m3/s) and 11 (32.3 ft3/s or 0.91 m3/s) on the East Branch and sites 16 (18.1 ft3/s or 0.51 m3/s) and 20 (18.8 ft3/s or 0.53 m3/s) on the West Branch; and a substantial gain in discharge from site 23 (57.3 ft3/s or 1.62 m3/s) to site 24 (63.4 ft3/s or 1.80 m3/s) on the Eau Claire River. A gaging station was established at the downstream potential irrigation site to collect continuous stage and discharge data on streamflow to assist the Wisconsin Department of Natural Resources in the regulation of irrigation withdrawals.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75336","collaboration":"Prepared in cooperation with the Wisconsin Department of Natural Resources","usgsCitation":"Holmstrom, B.K., 1975, Low-flow Characteristics of Eau Claire River Basin near Antigo, Wisconsin: U.S. Geological Survey Open-File Report 75-336, Report: 19 p.; 1 Plate: 24.00 x 32.00 inches, https://doi.org/10.3133/ofr75336.","productDescription":"Report: 19 p.; 1 Plate: 24.00 x 32.00 inches","numberOfPages":"19","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":152640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0336/report-thumb.jpg"},{"id":48902,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48903,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0336/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"48000","country":"United States","state":"Wisconsin","city":"Antigo","otherGeospatial":"Eau Claire","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -89.3243408203125,\n              44.9715991458543\n            ],\n            [\n              -89.3243408203125,\n              45.390735154248894\n            ],\n            [\n              -88.9727783203125,\n              45.390735154248894\n            ],\n            [\n              -88.9727783203125,\n              44.9715991458543\n            ],\n            [\n              -89.3243408203125,\n              44.9715991458543\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6449b5","contributors":{"authors":[{"text":"Holmstrom, B. K.","contributorId":90728,"corporation":false,"usgs":true,"family":"Holmstrom","given":"B.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":180886,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28271,"text":"wri7540 - 1975 - Digital models of a glacial outwash aquifer in the Pearl-Sallie Lakes area, west-central Minnesota","interactions":[],"lastModifiedDate":"2024-04-22T19:07:29.804101","indexId":"wri7540","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"75-40","title":"Digital models of a glacial outwash aquifer in the Pearl-Sallie Lakes area, west-central Minnesota","docAbstract":"<p>-p^e need for study of lake-ground-water interchange has been accentuated by eutrophication of lakes in the Pearl-Sallie Lakes area of west-central Minnesota. The local ground-water flow system is dominated by an outwash aquifer that is sandwiched between two till layers in the western part of the area and exposed at the land surface in the eastern part. Ground water discharges from the aquifer into lakes in the outwash area but is recharged from lakes in the till-covered area. Irregular aquifer geometry resulted in a complex ground-water flow system. Simulation of the system by areal and vertical-section models showed that the lakes significantly control groundwater flow near their boundaries. Inadequate field data and complex geology caused difficulty in obtaining solutions with the vertical-section model. The models may be used to guide collection and interpretation of field data, and quantification of the ground-water flow system. With modification, they could be used to predict aquifer response to transient stresses. They also could be incorporated into more complex models to determine the movement of solutes in the ground-water system.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri7540","collaboration":"Prepared in cooperation with the U. S. Environmental Protection Agency","usgsCitation":"Larson, S.P., McBride, M.S., and Wolf, R.J., 1975, Digital models of a glacial outwash aquifer in the Pearl-Sallie Lakes area, west-central Minnesota: U.S. Geological Survey Water-Resources Investigations Report 75-40, iv, 39 p., https://doi.org/10.3133/wri7540.","productDescription":"iv, 39 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":428010,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_34478.htm","linkFileType":{"id":5,"text":"html"}},{"id":95706,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1975/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159603,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1975/0040/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Pearl-Sallie Lakes area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -95.95991134643555,\n              46.749388725669824\n            ],\n            [\n              -95.95991134643555,\n              46.803819640791566\n            ],\n            [\n              -95.86687088012695,\n              46.803819640791566\n            ],\n            [\n              -95.86687088012695,\n              46.749388725669824\n            ],\n            [\n              -95.95991134643555,\n              46.749388725669824\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65aa2a","contributors":{"authors":[{"text":"Larson, S. P.","contributorId":34903,"corporation":false,"usgs":true,"family":"Larson","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":199505,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McBride, Mark S.","contributorId":96694,"corporation":false,"usgs":true,"family":"McBride","given":"Mark","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":199506,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wolf, R. J.","contributorId":21518,"corporation":false,"usgs":true,"family":"Wolf","given":"R.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":199504,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":12459,"text":"ofr7527 - 1975 - Hydrology of three sinkhole basins in southwestern Seminole County, Florida","interactions":[],"lastModifiedDate":"2024-07-31T20:08:21.251923","indexId":"ofr7527","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-27","title":"Hydrology of three sinkhole basins in southwestern Seminole County, Florida","docAbstract":"<p>The southwestern part of Seminole County--in east-central Florida-is characterized by sinkholes formed by the subsidence of surficial deposits into solution cavities in the underlying limestone deposits. The area includes three sinkhole basins created by such subsidence: Cranes Roost, Palm Springs, and Grace Lake.</p><p>Cranes Roost basin (drainage area, 5.02 square miles) contains a closed drainage system of lakes and swamps--including Lakes Adelaide, Florida, and Mobile--that terminates at Cranes Roost sink. It also contains Lake Orienta and two unnamed sinks which do not overflow into Cranes Roost sink.</p><p>Palm Springs basin (drainage area, 1.77 square miles) includes Lake Marion, Eleventh Hole Pond, and several small unconnected sinks.</p><p>Grace Lake basin (drainage area, 1.64 square miles) includes Island Lake which overflows into Grace Lake.</p><p>The recent spread of urban development has tended to encroach on the flood plains of lakes in these sinkhole basins and cause concern over the flood hazard that results. An investigation was made of the area to document the highest known lake levels, to examine possible effects of urbanization with regard to increasing the flood hazard, and to appraise the possibilities of controlling lake levels to reduce or limit the flood hazard.</p><p>The highest lake stages of record in the three sinkhole basins occurred in September 1960. Analyses of the hydrologic relations between lake stages, ground-water levels, stream discharges, and rainfall in the area indicated that the lake stages of September 1960 probably were the highest attained since at least 1895.</p><p>Cultural development that increases the percentage of a sink basin covered by impervious materials will cause more rapid runoff of a larger part of the rainfall in the basin. Thus, as development progresses, lake stages seldom reached under natural conditions may be reached more frequently unless the lake levels are controlled.</p><p>In Crane Roost basin, the levels of Lakes Mobile, Adelaide, and Florida could be controlled by enlarging their surface outlets and adding control structures; however, such measures might be ineffective unless the level of Cranes Roost also was controlled. The level of Cranes Roost could be controlled by removal of water by pumping or by providing a surface outlet; pumping might be ineffective during extreme wet periods because of the potential for inflow from upstream lakes and the potential for ground-water inflow from the Floridan aquifer. The level of Lake Orienta could be Controlled by removal of water by pumping or by providing a surface outlet.</p><p>In the Palm Springs sink basin, the levels of Lake Marion and the several small sinks could be controlled by removal of water by pumping or by providing surface outlets. For the several sinks, however, providing a surface outlet would require an extensive excavation and pumping might prove impractical because of seepage induced from the Floridan aquifer.</p><p>The level of Island Lake--in Grace Lake sink basin-could be controlled by enlarging its surface outlet and providing a control structure. The peak stage of Grace Lake could be reduced by lowering its outlet to the north, but release of water during wet periods might cause downstream flooding.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7527","collaboration":"Prepared in cooperation with the Board of County Commissioners of Seminole County","usgsCitation":"Anderson, W., and Hughes, G., 1975, Hydrology of three sinkhole basins in southwestern Seminole County, Florida: U.S. Geological Survey Open-File Report 75-27, Report: 59 p.; 6 Figures: 17.73 x 23.92 inches or smaller, https://doi.org/10.3133/ofr7527.","productDescription":"Report: 59 p.; 6 Figures: 17.73 x 23.92 inches or smaller","costCenters":[],"links":[{"id":431759,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431758,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431757,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431756,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431755,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431754,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1975/0027/figure-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":431753,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0027/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146526,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0027/report-thumb.jpg"}],"country":"United States","state":"Florida","county":"Seminole County","otherGeospatial":"southwestern Seminole County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.53839079697836,\n              28.867357027113812\n            ],\n            [\n              -81.53839079697836,\n              28.66338961826405\n            ],\n            [\n              -81.14420156315663,\n              28.66338961826405\n            ],\n            [\n              -81.14420156315663,\n              28.867357027113812\n            ],\n            [\n              -81.53839079697836,\n              28.867357027113812\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc746","contributors":{"authors":[{"text":"Anderson, Warren","contributorId":7712,"corporation":false,"usgs":true,"family":"Anderson","given":"Warren","affiliations":[],"preferred":false,"id":166171,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hughes, G.H.","contributorId":73975,"corporation":false,"usgs":true,"family":"Hughes","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":166172,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8993,"text":"ofr75150 - 1975 - Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","interactions":[{"subject":{"id":8993,"text":"ofr75150 - 1975 - Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","indexId":"ofr75150","publicationYear":"1975","noYear":false,"title":"Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":58767,"text":"mf642 - 1975 - Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska","indexId":"mf642","publicationYear":"1975","noYear":false,"title":"Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska"},"id":1}],"supersededBy":{"id":58767,"text":"mf642 - 1975 - Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska","indexId":"mf642","publicationYear":"1975","noYear":false,"title":"Reconnaissance geologic map of St. Matthew Island, Bering Sea, Alaska"},"lastModifiedDate":"2023-12-08T18:44:52.063774","indexId":"ofr75150","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-150","title":"Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska","docAbstract":"<p>Reconnaissance investigations of the heretofore little known volcanic assemblage on St. Matthew Island provide significant information on the tectonic history of the Bering Sea shelf. St. Matthew Island is made up of approximately 500 m of subaerial calc-alkaline volcanic rocks ranging in composition from high-alumina basalt to rhyolite. Four K-Ar analyses of samples from this volcanic sequence give Late Cretaceous ages of 65-77 m.y., and intercalated carbonaceous tuff layers yield Cretaceous pollen assemblages. Along the northeast coast of St. Matthew Island the volcanic rocks are intruded by granodiorite that gives an early Tertiary K-Ar age of 61 m.y.</p><p>Correlations with on-land geology in northeast Siberia and marine geophysical data from the western Bering Sea strongly suggest that St. Matthew Island represents a southeastward extension of the Okhotsk-Chukotsk belt, a Late Cretaceous and early Tertiary volcanic arc that borders the Pacific margin of Siberia for 3,000 km. The apparent continuation of this volcanic arc along the margin of the Bering shelf at least as far east as St. Matthew Island supports suggestions by Burk and by Scholl and others that in late Mesozoic time the Pacific plate margin coincided with the present-day Bering shelf margin and did not shift to the Aleutian trench until the end of Cretaceous or the beginning of Tertiary time.</p><p>During the summer of 1971 the U.S. Geological Survey conducted a reconnaissance expedition to St. Matthew Island in the central Bering Sea aboard the Survey research vessel Don J. Miller II. The purpose of the expedition was to obtain basic geologic information on the age and lithologic character of the volcanic rocks on St. Matthew as part of a broad program of onshore and offshore investigations of the energy and mineral resources of the Bering Sea shelf. St. Matthew Island had not been mapped previously and available geologic information was confined to brief notes from early exploratory surveys of the Bering Sea region published more than 50 years ago (Dawson, 1894; Emerson, 1910).</p><p>St. Matthew Island together with two small neighboring islands, Hall and Pinnacle, is situated 400 km west of mainland Alaska on the broad continental shelf that connects Alaska and Siberia (fig. 1). Although these islands have a combined area of only 350<sup>2</sup> km, they are important because they provide a rare subaerial exposure of the geology of the shelf and furnish new information on the tectonic history of the Bering Sea region.</p><p>This report briefly describes the geology of the island and suggests how the island fits into the tectonic framework of the Bering Sea region.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75150","usgsCitation":"Patton, W.W., Lanphere, M.A., Miller, T.P., and Scott, R., 1975, Age and tectonic significance of volcanic rocks on St. Matthew Island, Bering Sea, Alaska: U.S. Geological Survey Open-File Report 75-150, 18 p., https://doi.org/10.3133/ofr75150.","productDescription":"18 p.","costCenters":[],"links":[{"id":423344,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0150/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144105,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0150/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Bering Sea, St. Matthew Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -173.19656898891907,\n              60.72952223911312\n            ],\n            [\n              -173.19656898891907,\n              60.248433293048976\n            ],\n            [\n              -172.1421533581664,\n              60.248433293048976\n            ],\n            [\n              -172.1421533581664,\n              60.72952223911312\n            ],\n            [\n              -173.19656898891907,\n              60.72952223911312\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6896f3","contributors":{"authors":[{"text":"Patton, William Wallace Jr.","contributorId":72346,"corporation":false,"usgs":true,"family":"Patton","given":"William","suffix":"Jr.","email":"","middleInitial":"Wallace","affiliations":[],"preferred":false,"id":158681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanphere, Marvin A. alder@usgs.gov","contributorId":2696,"corporation":false,"usgs":true,"family":"Lanphere","given":"Marvin","email":"alder@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158678,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"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":158679,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Scott, Richard A.","contributorId":14414,"corporation":false,"usgs":true,"family":"Scott","given":"Richard A.","affiliations":[],"preferred":false,"id":158680,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":35616,"text":"b1395B - 1975 - Revision of the type Mankomen Formation (Pennsylvanian and Permian), Eagle Creek area, eastern Alaska Range, Alaska","interactions":[],"lastModifiedDate":"2022-08-26T19:17:24.496464","indexId":"b1395B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1395","chapter":"B","title":"Revision of the type Mankomen Formation (Pennsylvanian and Permian), Eagle Creek area, eastern Alaska Range, Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1395B","usgsCitation":"Richter, D.H., and Dutro, J.T., 1975, Revision of the type Mankomen Formation (Pennsylvanian and Permian), Eagle Creek area, eastern Alaska Range, Alaska: U.S. Geological Survey Bulletin 1395, iii, 25 p., https://doi.org/10.3133/b1395B.","productDescription":"iii, 25 p.","costCenters":[],"links":[{"id":96979,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1395b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167516,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1395b/report-thumb.jpg"},{"id":405707,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21510.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Alaska","otherGeospatial":"Eagle Creek area, eastern Alaska Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -144.5,\n              63\n            ],\n            [\n              -144.333,\n              63\n            ],\n            [\n              -144.333,\n              63.083\n            ],\n            [\n              -144.5,\n              63.083\n            ],\n            [\n              -144.5,\n              63\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602945","contributors":{"authors":[{"text":"Richter, Donald H.","contributorId":61021,"corporation":false,"usgs":true,"family":"Richter","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dutro, J. Thomas Jr.","contributorId":102878,"corporation":false,"usgs":true,"family":"Dutro","given":"J.","suffix":"Jr.","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":214951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28451,"text":"wri7444 - 1975 - Floods in east Baton Rouge Parish and adjacent areas, Louisiana, for the period 1953-74","interactions":[],"lastModifiedDate":"2020-08-20T19:36:15.985027","indexId":"wri7444","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"74-44","title":"Floods in east Baton Rouge Parish and adjacent areas, Louisiana, for the period 1953-74","docAbstract":"<p><span>Flood damage resulting from development in flood plains in East Baton </span><span>Rouge Parish, La., and adjacent areas has caused economic losses, making </span><span>governmental officials and planners aware of the need for flood maps. Based </span><span>on information in private and official files, flood maps have been prepared </span><span>for 7 1/2-minute topographic quadrangles to show the interpretative </span><span>delineation of the highest flood elevation that occurred between the years </span><span>1953 and 1974. The flood boundaries were mapped on the following quadrangles: </span><span>Port Hudson, Zachary, Fred, Pride, Pine Grove, Walls, Scotlandville, Comite, </span><span>Watson, Baton Rouge West, Baton Rouge East, Denham Springs, Plaquemine, </span><span>St. Gabriel, and Prairieville.</span></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7444","collaboration":"Prepared in cooperation with East Baton Rouge Parish Department of Public Works, under the auspices of Louisiana Department of Public Works","usgsCitation":"Lowe, A.S., 1975, Floods in east Baton Rouge Parish and adjacent areas, Louisiana, for the period 1953-74: U.S. Geological Survey Water-Resources Investigations Report 74-44, Report: iv, 12 p.; 16 Plates: 22.95 x 28.99 inches and smaller, https://doi.org/10.3133/wri7444.","productDescription":"Report: iv, 12 p.; 16 Plates: 22.95 x 28.99 inches and smaller","costCenters":[],"links":[{"id":377235,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377234,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377233,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377232,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377231,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377230,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377229,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377228,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377227,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377226,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377225,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377224,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377223,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377222,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1974/0044/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159569,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1974/0044/report-thumb.jpg","linkFileType":{"id":1,"text":"pdf"}},{"id":377238,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377237,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":377236,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1974/0044/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Lousiana","county":"Baton Rouge Parish","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.3,\n              30.25\n            ],\n            [\n              -90.75,\n              30.25\n            ],\n            [\n              -90.75,\n              30.75\n            ],\n            [\n              -91.3,\n              30.75\n            ],\n            [\n              -91.3,\n              30.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dce4b07f02db5e1c22","contributors":{"authors":[{"text":"Lowe, Alfred S.","contributorId":74820,"corporation":false,"usgs":true,"family":"Lowe","given":"Alfred","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":199823,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15452,"text":"ofr75592 - 1975 - Interim report on petroleum resource potential and geologic hazards in the outer continental shelf of the Gulf of Alaska Tertiary province","interactions":[],"lastModifiedDate":"2023-10-04T21:26:10.548207","indexId":"ofr75592","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-592","title":"Interim report on petroleum resource potential and geologic hazards in the outer continental shelf of the Gulf of Alaska Tertiary province","docAbstract":"<p>The potential for discovering large accumulations of petroleum on the Outer Continental Shelf of the Gulf of Alaska Tertiary Province cannot be evaluated with much confidence at present because of the inadequacies of the available offshore geological and geophysical data. The 22 deep test wells that have been drilled since 1954 have been unsuccessful because structure is complex and because suitable reservoir rocks have not been found in favorable structural positions. Although it is possible that the factors controlling accumulation of petroleum may improve offshore, regional stratigraphic and structural considerations together with the limited geophysical data suggest that this is not necessarily the case. Extrapolation of onshore geology together with the limited amount of marine geophysical data, indicate that the eastern Gulf of Alaska Outer Continental Shelf is geologically complex and consists of several areas with markedly differing structural styles and petroleum potential.</p><p><br></p><p><br data-mce-bogus=\"1\"></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75592","usgsCitation":"Plafker, G., Bruns, T.R., and Page, R.A., 1975, Interim report on petroleum resource potential and geologic hazards in the outer continental shelf of the Gulf of Alaska Tertiary province: U.S. Geological Survey Open-File Report 75-592, iv, 74 p., https://doi.org/10.3133/ofr75592.","productDescription":"iv, 74 p.","costCenters":[],"links":[{"id":421629,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0592/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":393923,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15212.htm"},{"id":149013,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0592/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Gulf of Alaska","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -152,\n              56\n            ],\n            [\n              -136,\n              56\n            ],\n            [\n              -136,\n              60.5\n            ],\n            [\n              -152,\n              60.5\n            ],\n            [\n              -152,\n              56\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0d7d","contributors":{"authors":[{"text":"Plafker, George","contributorId":3920,"corporation":false,"usgs":false,"family":"Plafker","given":"George","email":"","affiliations":[],"preferred":false,"id":171156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bruns, Terry R.","contributorId":29420,"corporation":false,"usgs":true,"family":"Bruns","given":"Terry","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":171158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Page, Robert A.","contributorId":17207,"corporation":false,"usgs":true,"family":"Page","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":171157,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":42658,"text":"ofr75531 - 1975 - Preliminary surficial geologic map of the East Brookfield quadrangle, Worcester County, Massachusetts","interactions":[],"lastModifiedDate":"2022-04-05T18:37:01.992651","indexId":"ofr75531","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1975","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"75-531","title":"Preliminary surficial geologic map of the East Brookfield quadrangle, Worcester County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr75531","usgsCitation":"Pomeroy, J.S., 1975, Preliminary surficial geologic map of the East Brookfield quadrangle, Worcester County, Massachusetts: U.S. Geological Survey Open-File Report 75-531, Report: 7 p.; 2 Plates: 19.38 × 27.15 inches and 33.39 × 10.43 inches, https://doi.org/10.3133/ofr75531.","productDescription":"Report: 7 p.; 2 Plates: 19.38 × 27.15 inches and 33.39 × 10.43 inches","costCenters":[],"links":[{"id":398130,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93251.htm"},{"id":80434,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1975/0531/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80433,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0531/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":80432,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1975/0531/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":176099,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1975/0531/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Worcester County","otherGeospatial":"East Brookfield quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -72.125,\n              42.125\n            ],\n            [\n              -72,\n              42.125\n            ],\n            [\n              -72,\n              42.25\n            ],\n            [\n              -72.125,\n              42.25\n            ],\n            [\n              -72.125,\n              42.125\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8539","contributors":{"authors":[{"text":"Pomeroy, John S.","contributorId":18329,"corporation":false,"usgs":true,"family":"Pomeroy","given":"John","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":226895,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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