{"pageNumber":"5577","pageRowStart":"139400","pageSize":"25","recordCount":165626,"records":[{"id":62072,"text":"a2 - 1973 - Reconnaissance geologic map of the Mount Elizabeth and Mount Kathleen quadrangles, Transantarctic Mountains, Antarctica","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"a2","displayToPublicDate":"1994-01-01T01:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":305,"text":"Antarctic Map","code":"A","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2","title":"Reconnaissance geologic map of the Mount Elizabeth and Mount Kathleen quadrangles, Transantarctic Mountains, Antarctica","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/a2","usgsCitation":"Lindsay, J., Gunner, J., and Barrett, P.J., 1973, Reconnaissance geologic map of the Mount Elizabeth and Mount Kathleen quadrangles, Transantarctic Mountains, Antarctica: U.S. Geological Survey Antarctic Map 2, 1 Sheet, 29 1/2 x 35 inches, https://doi.org/10.3133/a2.","productDescription":"1 Sheet, 29 1/2 x 35 inches","costCenters":[],"links":[{"id":112497,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://repository.agic.umn.edu/maps/usgs/geologic/a2_mount_elizabeth_mount_kathleen/","linkFileType":{"id":5,"text":"html"}},{"id":248262,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/a/02/report.pdf","size":"43","linkFileType":{"id":1,"text":"pdf"}},{"id":248263,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/a/02/plate-1.pdf","size":"6067","linkFileType":{"id":1,"text":"pdf"}},{"id":253081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/a/02/report-thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 165,-84 ], [ 165,-83 ], [ 177,-83 ], [ 177,-84 ], [ 165,-84 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db64176d","contributors":{"authors":[{"text":"Lindsay, J.F.","contributorId":54666,"corporation":false,"usgs":true,"family":"Lindsay","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":266862,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gunner, John","contributorId":58345,"corporation":false,"usgs":true,"family":"Gunner","given":"John","email":"","affiliations":[],"preferred":false,"id":266863,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barrett, P. J.","contributorId":96347,"corporation":false,"usgs":false,"family":"Barrett","given":"P.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":266864,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15242,"text":"ofr73205 - 1973 - Reconnaissance geology of the Balakot and Mahandri quadrangles, Hazara District, Pakistan","interactions":[{"subject":{"id":15242,"text":"ofr73205 - 1973 - Reconnaissance geology of the Balakot and Mahandri quadrangles, Hazara District, Pakistan","indexId":"ofr73205","publicationYear":"1973","noYear":false,"title":"Reconnaissance geology of the Balakot and Mahandri quadrangles, Hazara District, Pakistan"},"predicate":"SUPERSEDED_BY","object":{"id":5811,"text":"pp716C - 1975 - Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas","indexId":"pp716C","publicationYear":"1975","noYear":false,"chapter":"C","title":"Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas"},"id":1}],"supersededBy":{"id":5811,"text":"pp716C - 1975 - Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas","indexId":"pp716C","publicationYear":"1975","noYear":false,"title":"Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr73205","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-205","title":"Reconnaissance geology of the Balakot and Mahandri quadrangles, Hazara District, Pakistan","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr73205","usgsCitation":"Offield, T.W., and Abdullah, S., 1973, Reconnaissance geology of the Balakot and Mahandri quadrangles, Hazara District, Pakistan: U.S. Geological Survey Open-File Report 73-205, ii, 41 p. :maps (some folded) ;27 cm., https://doi.org/10.3133/ofr73205.","productDescription":"ii, 41 p. :maps (some folded) ;27 cm.","costCenters":[],"links":[{"id":147125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640a82","contributors":{"authors":[{"text":"Offield, Terry W.","contributorId":15196,"corporation":false,"usgs":true,"family":"Offield","given":"Terry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170803,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abdullah, S.K.M.","contributorId":67896,"corporation":false,"usgs":true,"family":"Abdullah","given":"S.K.M.","email":"","affiliations":[],"preferred":false,"id":170804,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12941,"text":"ofr7343 - 1973 - Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County Idaho","interactions":[{"subject":{"id":12941,"text":"ofr7343 - 1973 - Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County Idaho","indexId":"ofr7343","publicationYear":"1973","noYear":false,"title":"Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":33972,"text":"b1391C - 1975 - Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County, Idaho","indexId":"b1391C","publicationYear":"1975","noYear":false,"chapter":"C","title":"Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County, Idaho"},"id":1}],"supersededBy":{"id":33972,"text":"b1391C - 1975 - Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County, Idaho","indexId":"b1391C","publicationYear":"1975","noYear":false,"title":"Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County, Idaho"},"lastModifiedDate":"2012-02-02T00:06:57","indexId":"ofr7343","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-43","title":"Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County Idaho","language":"ENGLISH","publisher":"U.S.Geological Survey],","doi":"10.3133/ofr7343","usgsCitation":"Cater, F., Pinckney, D.M., and Stotelmeyer, R., 1973, Mineral resources of the Clear Creek-Upper Big Deer Creek study area, contiguous to the Idaho Primitive Area, Lemhi County Idaho: U.S. Geological Survey Open-File Report 73-43, 79 p. :ill., maps (some folded) ;29 cm., https://doi.org/10.3133/ofr7343.","productDescription":"79 p. :ill., maps (some folded) ;29 cm.","costCenters":[],"links":[{"id":146716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db658922","contributors":{"authors":[{"text":"Cater, Fred W.","contributorId":26295,"corporation":false,"usgs":true,"family":"Cater","given":"Fred W.","affiliations":[],"preferred":false,"id":167000,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pinckney, D. M.","contributorId":33336,"corporation":false,"usgs":true,"family":"Pinckney","given":"D.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":167001,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stotelmeyer, R.B.","contributorId":62615,"corporation":false,"usgs":true,"family":"Stotelmeyer","given":"R.B.","affiliations":[],"preferred":false,"id":167002,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3001,"text":"wsp2029A - 1973 - Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:05:48","indexId":"wsp2029A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2029","chapter":"A","title":"Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota","docAbstract":"<p>Stratified fluvial sediments occur within the glacial drift at many places in the Mesabi Iron Range area. These sediments, which are important aquifers, occur extensively between the three main till units. The thickest and most extensive aquifer consists of glaciofluvial sediments that lie between the surficial till and the middle till unit, the bouldery till. Thickness of the glaciofluvial sediments at this stratigraphic interval is greater than 50 feet in much of the area, and transmissivity is greater than 100,000 gallons per day per foot in some places.</p>\n<p>Glaciofluvial sediments underlying the bouldery till occur largely in the western half of the area. These sediments are generally less than 50 feet thick, and transmissivity is generally less than 50,000 gallons per day per foot.</p>\n<p>Surficial glaciofluvial sediments are a source of ground water for high-yield wells only in the eastern part of the area in the vicinity of the Biwabik bedrock valley. Thickness of these sediments is greater than 100 feet in some places, but transmissivity is generally less than 50,000 gallons per day per foot.</p>\n<p>Practical sustained yield of aquifers in glacial drift is estimated to be as much as 40 million gallons per day from known aquifers. Assuming that the ratio of area underlain by aquifer to total area is constant for the study area (about 20 percent where mapped in detail), as much as 80 million gallons per day could be developed from glacial-drift aquifers.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2029A","collaboration":"Prepared in cooperation with the Minnesota Department of Iron Range Resources and Rehabilitation","usgsCitation":"Winter, T.C., 1973, Hydrogeology of glacial drift, Mesabi Iron Range, northeastern Minnesota: U.S. Geological Survey Water Supply Paper 2029, Document: iv, 23 p.; 3 Plates: 28.00 x 28.17 inches or smaller, https://doi.org/10.3133/wsp2029A.","productDescription":"Document: iv, 23 p.; 3 Plates: 28.00 x 28.17 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":29794,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2029a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139403,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2029a/report-thumb.jpg"},{"id":29791,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29792,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29793,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2029a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Minnesota","otherGeospatial":"Mesabi Iron Range","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -93.8,\n              47.625\n            ],\n            [\n              -93.8,\n              47\n            ],\n            [\n              -91.75,\n              47\n            ],\n            [\n              -91.75,\n              47.625\n            ],\n            [\n              -93.8,\n              47.625\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db624639","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":146127,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26192,"text":"wri7340 - 1973 - Base of fresh ground water approximately 3,000 micromhos in the Sacramento Valley and Sacramento-San Joaquin Delta, California","interactions":[],"lastModifiedDate":"2018-12-06T14:23:22","indexId":"wri7340","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-40","title":"Base of fresh ground water approximately 3,000 micromhos in the Sacramento Valley and Sacramento-San Joaquin Delta, California","docAbstract":"<p>The study area consists of about 6,600 square miles; about 5,500 square miles of the floor of the Sacramento Valley, and about 1,100 square miles of the Sacramento-San Joaquin Delta.&nbsp; The Sacramento Valley, as defined by Bryan (1923, p. 8), extends from Red Bluff 145 miles southward to Suisun Bay.&nbsp; It is bounded on the east by the Sierra Nevada, on the northeast by the Cascade Range, on the northwest by the Klamath Mountains, and the west by the Coast Ranges.&nbsp; Southward the valley merges with the Delta and the San Joaquin Valley.&nbsp; The width of the Sacramento Valley varies from about 30 miles near Red Bluff to about 60 miles on the south, and averages about 40 miles.&nbsp; The southern boundary of the study area coincides with the northern boundary used in an earlier study be Page (1971, 1973a).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri7340","usgsCitation":"Berkstresser, C.F., 1973, Base of fresh ground water approximately 3,000 micromhos in the Sacramento Valley and Sacramento-San Joaquin Delta, California: U.S. Geological Survey Water-Resources Investigations Report 73-40, 22.51 x 33.21 inches, https://doi.org/10.3133/wri7340.","productDescription":"22.51 x 33.21 inches","costCenters":[],"links":[{"id":157918,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1973/0040/report-thumb.jpg"},{"id":359986,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1973/0040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"Sacramento Valley, San Joaquin Delta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.7008056640625,\n              37.75334401310656\n            ],\n            [\n              -120.838623046875,\n              37.75334401310656\n            ],\n            [\n              -120.838623046875,\n              40.734770989672406\n            ],\n            [\n              -122.7008056640625,\n              40.734770989672406\n            ],\n            [\n              -122.7008056640625,\n              37.75334401310656\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db6489a3","contributors":{"authors":[{"text":"Berkstresser, Charles F. Jr.","contributorId":43390,"corporation":false,"usgs":true,"family":"Berkstresser","given":"Charles","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":195963,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56541,"text":"wdrND722 - 1973 - Water resources data for North Dakota, water year 1972; Part 2, water quality records","interactions":[],"lastModifiedDate":"2019-09-30T16:26:39","indexId":"wdrND722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"ND-72-2","title":"Water resources data for North Dakota, water year 1972; Part 2, water quality records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrND722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for North Dakota, water year 1972; Part 2, water quality records: U.S. Geological Survey Water Data Report ND-72-2, 175 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,{"id":15247,"text":"ofr73207 - 1973 - Geologic map of the Cotuit quadrangle, Barnstable County, Massachusetts","interactions":[{"subject":{"id":15247,"text":"ofr73207 - 1973 - Geologic map of the Cotuit quadrangle, Barnstable County, Massachusetts","indexId":"ofr73207","publicationYear":"1973","noYear":false,"title":"Geologic map of the Cotuit quadrangle, Barnstable County, Massachusetts"},"predicate":"SUPERSEDED_BY","object":{"id":62358,"text":"gq1213 - 1975 - Geologic map of the Cotuit quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1213","publicationYear":"1975","noYear":false,"title":"Geologic map of the Cotuit quadrangle, Barnstable County, Cape Cod, Massachusetts"},"id":1}],"supersededBy":{"id":62358,"text":"gq1213 - 1975 - Geologic map of the Cotuit quadrangle, Barnstable County, Cape Cod, Massachusetts","indexId":"gq1213","publicationYear":"1975","noYear":false,"title":"Geologic map of the Cotuit quadrangle, Barnstable County, Cape Cod, Massachusetts"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr73207","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-207","title":"Geologic map of the Cotuit quadrangle, Barnstable County, Massachusetts","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr73207","usgsCitation":"Oldale, R.N., 1973, Geologic map of the Cotuit quadrangle, Barnstable County, Massachusetts: U.S. Geological Survey Open-File Report 73-207, 9 p. :ill., (1 folded), folded map ;28 cm.; 1 sheet, scale 1:24,000, https://doi.org/10.3133/ofr73207.","productDescription":"9 p. :ill., (1 folded), folded map ;28 cm.; 1 sheet, scale 1:24,000","costCenters":[],"links":[{"id":147154,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c1a6","contributors":{"authors":[{"text":"Oldale, Robert N.","contributorId":38953,"corporation":false,"usgs":true,"family":"Oldale","given":"Robert","email":"","middleInitial":"N.","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":170814,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61272,"text":"mf501 - 1973 - Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska to Canadian border, part III, Arctic Quadrangle (north half), Alaska","interactions":[],"lastModifiedDate":"2023-04-05T18:38:54.516702","indexId":"mf501","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"501","title":"Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska to Canadian border, part III, Arctic Quadrangle (north half), Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf501","usgsCitation":"1973, Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska to Canadian border, part III, Arctic Quadrangle (north half), Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 501, 2 Plates: 34.57 x 22.63 inches and 20.05 x 25.09 inches, https://doi.org/10.3133/mf501.","productDescription":"2 Plates: 34.57 x 22.63 inches and 20.05 x 25.09 inches","costCenters":[],"links":[{"id":415271,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0501/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415270,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0501/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406014,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2947.htm","linkFileType":{"id":5,"text":"html"}},{"id":180622,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0501/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Arctic Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -146.3125,\n              68.5\n            ],\n            [\n              -144,\n              68.5\n            ],\n            [\n              -144,\n              69\n            ],\n            [\n              -146.3125,\n              69\n            ],\n            [\n              -146.3125,\n              68.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf1f","contributors":{"compilers":[{"text":"Yeend, Warren","contributorId":91559,"corporation":false,"usgs":true,"family":"Yeend","given":"Warren","email":"","affiliations":[],"preferred":false,"id":868582,"contributorType":{"id":3,"text":"Compilers"},"rank":1},{"text":"Brosge, William P.","contributorId":287895,"corporation":false,"usgs":false,"family":"Brosge","given":"William","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":868583,"contributorType":{"id":3,"text":"Compilers"},"rank":2}]}}
,{"id":2898,"text":"wsp2029C - 1973 - Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp2029C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"2029","chapter":"C","title":"Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado","docAbstract":"A method to determine evapotranspiration from ground water was tested at four sites in the flood plain of the Arkansas River in Colorado. Approximate ground-water budgets were obtained by analyzing water-level data from observation wells installed in five-point arrays. The analyses were based on finite difference approximations of the differential equation describing ground-water flow. \r\n\r\nData from the sites were divided into two groups by season. It was assumed that water levels during the dormant season were unaffected by evapotranspiration of ground water or by recharge, collectively termed 'accretion.' Regression analyses of these data were made to provide an equation for separating the effects of changes in aquifer storage and of aquifer heterogeneity from those due to accretion during the growing season. The data collected during the growing season were thus analyzed to determine accretion.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp2029C","usgsCitation":"Weeks, E.P., and Sorey, M., 1973, Use of finite-difference arrays of observation wells to estimate evapotranspiration from ground water in the Arkansas River Valley, Colorado: U.S. Geological Survey Water Supply Paper 2029, iii, 27 p. ;24 cm., https://doi.org/10.3133/wsp2029C.","productDescription":"iii, 27 p. ;24 cm.","costCenters":[],"links":[{"id":138379,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2029c/report-thumb.jpg"},{"id":29564,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2029c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6046a9","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145976,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":145977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24979,"text":"pp850 - 1973 - Geological Survey research 1973","interactions":[],"lastModifiedDate":"2025-01-07T17:39:30.968268","indexId":"pp850","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"850","title":"Geological Survey research 1973","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp850","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Geological Survey research 1973: U.S. Geological Survey Professional Paper 850, viii, 366 p., https://doi.org/10.3133/pp850.","productDescription":"viii, 366 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":421216,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92939.htm","text":"Biostratigraphic record extended to Early Silurian or Ordovician in western Brooks Range","linkFileType":{"id":5,"text":"html"}},{"id":53964,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0850/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118859,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0850/report-thumb.jpg"},{"id":465772,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92944.htm","text":"Upper Lower Permian rocks discovered in northeastern Alaska","linkFileType":{"id":5,"text":"html"}},{"id":465773,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92945.htm","text":"New evidence bearing on age of Wales Group","linkFileType":{"id":5,"text":"html"}},{"id":465774,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92947.htm","text":"Late Ordovician (Ashgillian) age of volcanic rocks, north-central Maine","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6876ee","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":529140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15243,"text":"ofr73204 - 1973 - Reconnaissance geology of the Mansehra quadrangle, Hazara district, Pakistan","interactions":[{"subject":{"id":15243,"text":"ofr73204 - 1973 - Reconnaissance geology of the Mansehra quadrangle, Hazara district, Pakistan","indexId":"ofr73204","publicationYear":"1973","noYear":false,"title":"Reconnaissance geology of the Mansehra quadrangle, Hazara district, Pakistan"},"predicate":"SUPERSEDED_BY","object":{"id":5811,"text":"pp716C - 1975 - Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas","indexId":"pp716C","publicationYear":"1975","noYear":false,"chapter":"C","title":"Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas"},"id":1}],"supersededBy":{"id":5811,"text":"pp716C - 1975 - Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas","indexId":"pp716C","publicationYear":"1975","noYear":false,"title":"Geology of the southern Himalaya in Hazara, Pakistan, and adjacent areas"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr73204","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-204","title":"Reconnaissance geology of the Mansehra quadrangle, Hazara district, Pakistan","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr73204","usgsCitation":"Offield, T.W., Abdullah, S., and Zafar, M., 1973, Reconnaissance geology of the Mansehra quadrangle, Hazara district, Pakistan: U.S. Geological Survey Open-File Report 73-204, 31 leaves :folded col. maps ;27 cm.; 41 p., https://doi.org/10.3133/ofr73204.","productDescription":"31 leaves :folded col. maps ;27 cm.; 41 p.","costCenters":[],"links":[{"id":147126,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6de4b07f02db63ed20","contributors":{"authors":[{"text":"Offield, Terry W.","contributorId":15196,"corporation":false,"usgs":true,"family":"Offield","given":"Terry","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170805,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Abdullah, S.K.M.","contributorId":67896,"corporation":false,"usgs":true,"family":"Abdullah","given":"S.K.M.","email":"","affiliations":[],"preferred":false,"id":170806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zafar, M.S.","contributorId":93067,"corporation":false,"usgs":true,"family":"Zafar","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":170807,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":56532,"text":"wdrNC722 - 1973 - Water resources data for North Carolina, water year 1972; Part 2, water quality records","interactions":[],"lastModifiedDate":"2020-08-12T20:34:07.224943","indexId":"wdrNC722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NC-72-2","title":"Water resources data for North Carolina, water year 1972; Part 2, water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNC722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for North Carolina, water year 1972; Part 2, water quality records: U.S. Geological Survey Water Data 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,{"id":56445,"text":"wdrAR721 - 1973 - Water resources data for Arkansas, water year 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrAR721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-72-1","title":"Water resources data for Arkansas, water year 1972","language":"ENGLISH","doi":"10.3133/wdrAR721","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Arkansas, water year 1972: U.S. Geological Survey Water Data Report AR-72-1, 149 p., https://doi.org/10.3133/wdrAR721.","productDescription":"149 p.","costCenters":[],"links":[{"id":184128,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f7558","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":532626,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56446,"text":"wdrAR722 - 1973 - Water resources data for Arkansas, water year 1972","interactions":[],"lastModifiedDate":"2012-02-02T00:12:22","indexId":"wdrAR722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-72-2","title":"Water resources data for Arkansas, water year 1972","language":"ENGLISH","doi":"10.3133/wdrAR722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Arkansas, water year 1972: U.S. Geological Survey Water Data Report AR-72-2, 178 p., https://doi.org/10.3133/wdrAR722.","productDescription":"178 p.","costCenters":[],"links":[{"id":184129,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f763e","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":532627,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","interactions":[{"subject":{"id":56068,"text":"ofr70352 - 1970 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"ofr70352","publicationYear":"1970","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"predicate":"SUPERSEDED_BY","object":{"id":2861,"text":"wsp1974 - 1973 - Water resources of the New Jersey part of the Ramapo River basin","indexId":"wsp1974","publicationYear":"1973","noYear":false,"title":"Water resources of the New Jersey part of the Ramapo River basin"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1974","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1974","title":"Water resources of the New Jersey part of the Ramapo River basin","docAbstract":"The Ramapo River, a major stream in the Passaic River basin, drains an area of 161 square miles, 70 percent of which is in Orange and Rockland Counties, N.Y., and 30 percent is in Bergen and Passaic Counties, N.J. This report describes the hydrology of the New Jersey part of the basin and evaluates the feasibility of developing large ground-water supplies from the stratified drift in the Ramapo River valley by inducing recharge to the aquifer from the river. The ground water and surface water of the basin are considered as a single resource because the development of either ground water or surface water affects the availability of the other. \r\n\r\nPrecambrian gneiss, sparsely mantled with Pleistocene glacial drift, underlies the basin west of the Ramapo River in New Jersey. To the east, bedrock consists of the Watchung Basalt and of shale, sandstone, and conglomerate of the Brunswick Formation of Triassic age. Glacial drift occurs nearly everywhere in the eastern part of the basin, and deposits of stratified drift more than 100 feet thick occur in the Ramapo valley. Average annual runoff at Pompton Lakes accounts for 25 inches of the 45 inches of annual precipitation in the New Jersey part of the basin, and the remaining 20 inches is accounted for by evapotranspiration. Streamflow is highly variable--particularly in the area underlain by gneissic rocks-because of the low storage capacity of the rocks and the rough topography. \r\n\r\nMany of the small tributaries go dry during extended periods of no precipitation. Small domestic supplies of ground water can be obtained nearly everywhere, but the Brunswick Formation is the only consolidated-rock aquifer in the basin that can be depended upon to yield 100-200 gallons per minute to wells. Supplies of more than 1,000 gallons per minute are available from wells tapping the stratified drift in the Ramapo valley. The drift supplies 75 percent of the ground water pumped for public supply in the basin. Sustained ground-water yield in upland areas, based on stream base-flow recession, is estimated to be 200,000-300,000 gallons per day per square mile for the drift-covered Brunswick Formation and about 100,000-200,000 gallons per day per square mile for the gneiss and basalt. Potential sustained yield of the stratified drift in the valley depends on the availability of the streamflow and on the induced rate of infiltration. \r\n\r\nPumping from the stratified drift results in a reduction in streamflow, which may be undesirable, mainly because of prior downstream water rights. On the basis of the storage available in the stratified drift and an analysis of daily flow during the drought period of October 1964 to September 1967 at Pompton Lakes, 20-25 million gallons per day of Ramapo River water are available for development after existing downstream water requirements are supplied. However, some low-flow augmentation will be. necessary to insure downstream rights. Rates of infiltration computed from seepage losses observed near Mahwah indicate that at least 11 million gallons per day, on an average basis, can be infiltrated from the river by the pumping of wells tapping the stratified drift. The use of recharge pits and spreading areas would increase the rate of infiltration. Losses from the Ramapo River could be minimized by returning treated sewage effluent directly to the river or, preferably, by recharging the stratified-drift aquifer with the treated effluent. \r\n\r\nGround-water quality and surface-water quality at times of low-flow vary according to the type of rock from which the water is obtained. Water from the gneiss is low in dissolved solids--less than 127 mg/l (milligrams per liter)--and soft to moderately hard--less than 94 rag/l. Water from the Brunswick Formation is more mineralized--total dissolved-solids content is as much as 278 mg/1 and hardness as much as 188 mg/1. Water from the stratified drift is generally intermediate in quality--that is, total dissolved-solids content is as ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1974","usgsCitation":"Vecchioli, J., and Miller, E., 1973, Water resources of the New Jersey part of the Ramapo River basin: U.S. Geological Survey Water Supply Paper 1974, vi, 77 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1974.","productDescription":"vi, 77 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":138982,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1974/report-thumb.jpg"},{"id":29456,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29457,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29458,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29459,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1974/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29460,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1974/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef13d","contributors":{"authors":[{"text":"Vecchioli, John","contributorId":36113,"corporation":false,"usgs":true,"family":"Vecchioli","given":"John","email":"","affiliations":[],"preferred":false,"id":145920,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, E.G.","contributorId":44132,"corporation":false,"usgs":true,"family":"Miller","given":"E.G.","email":"","affiliations":[],"preferred":false,"id":145921,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56561,"text":"wdrNE722 - 1973 - Water resources data for Nebraska, water year 1972; part 2, water quality records","interactions":[],"lastModifiedDate":"2019-09-30T14:25:13","indexId":"wdrNE722","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"NE-72-2","title":"Water resources data for Nebraska, water year 1972; part 2, water quality records","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNE722","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Nebraska, water year 1972; part 2, water quality records: U.S. Geological Survey Water Data Report NE-72-2, 175 p., 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,{"id":23312,"text":"ofr73102 - 1973 - Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:08:01","indexId":"ofr73102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-102","title":"Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington","docAbstract":"A model of the circulation and quality of water in the Duwamish River estuary has been sufficiently developed to allow prediction of the effects of a proposed widening and deepening of waterways on residence time and dissolved oxygen in the estuary's salt wedge. For a low river-discharge period in August 1970, use of the model yielded an estimated residence time of wedge water to be 6.3 days in the present waterways estuary and 8.6 days in the wider and deeper proposed-waterways estuary--a 37-percent increase. June-September 1970 and for the estuary about 4 miles upstream from its mouth, the model estimates indicate that dissolved-oxygen values in the wedge of the proposed-waterways estuary would be as much as 1.4 milligrams per liter lower and would average 0.4 milligram per liter lower than (average difference significant at 95-percent confidence level) dissolved-oxygen values in the wedge of the present-waterways estuary. \r\n\r\nExtrapolation to low dissolved-oxygen values of a regression between the predicted dissolved oxygen for both the proposed and present-waterways estuaries suggests that 4 miles upstream of the estuary mouth oxygen would be completely depleted from the proposed-waterways estuary wedge whereas there still would be 0.2 milligram of oxygen per liter of water in the wedge of the present-waterways estuary.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr73102","issn":"0094-9140","usgsCitation":"Haushild, W., and Stoner, J., 1973, Predicted effects of proposed navigation improvements on residence time and dissolved oxygen of the salt wedge in the Duwamish River estuary, King County, Washington: U.S. Geological Survey Open-File Report 73-102, 13 p. :ill., map ;27 cm., https://doi.org/10.3133/ofr73102.","productDescription":"13 p. :ill., map ;27 cm.","costCenters":[],"links":[{"id":155134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0102/report-thumb.jpg"},{"id":52612,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0102/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fde2","contributors":{"authors":[{"text":"Haushild, W.L.","contributorId":48953,"corporation":false,"usgs":true,"family":"Haushild","given":"W.L.","affiliations":[],"preferred":false,"id":189874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":189875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":24797,"text":"ofr73358 - 1973 - Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"ofr73358","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-358","title":"Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California","docAbstract":"This is a study of the feasibility of recharging, in the Waterman Canyon-East Twin Creek area, imported water from northern California by way of the State Water Project beginning in 1972. \r\n\r\nThe feasibility of recharging 30,000 acre-feet of water a year in the Waterman Canyon-East Twin Creek area will depend on the effectiveness of fault K as a barrier to ground-water movement near the land surface. The results of test drilling and an infiltration test indicate that the subsurface material at the spreading grounds is permeable enough to allow recharged water to percolate to the water table. The data indicate that fault K extends into the Waterman Canyon-East Twin Creek area and may impede the lateral movement of recharged water. Fault K has no known surface expression and therefore probably does not affect the highly permeable younger alluvium. If that is so, fault K will be less effective as a barrier to ground-water movement as the recharge mound rises. Monitoring of the observation wells near the spreading grounds as the planned recharge operation proceeds should provide data about the hydrologic effects of fault K near the land surface.","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/ofr73358","issn":"0094-9140","usgsCitation":"Warner, J.W., and Moreland, J.A., 1973, Artificial recharge in the Waterman Canyon-East Twin Creek area, San Bernardino County, California: U.S. Geological Survey Open-File Report 73-358, iv, 44 p. :ill., maps ;27 cm., https://doi.org/10.3133/ofr73358.","productDescription":"iv, 44 p. :ill., maps ;27 cm.","costCenters":[],"links":[{"id":157510,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0358/report-thumb.jpg"},{"id":53810,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0358/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":53811,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0358/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c47","contributors":{"authors":[{"text":"Warner, J. W.","contributorId":42996,"corporation":false,"usgs":true,"family":"Warner","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":192582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moreland, J. A.","contributorId":71994,"corporation":false,"usgs":true,"family":"Moreland","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":192583,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2858,"text":"wsp1969 - 1973 - Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","interactions":[],"lastModifiedDate":"2017-02-06T11:55:59","indexId":"wsp1969","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"1969","title":"Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan","docAbstract":"<p>The Tri-County region, consisting of Clinton, Eaton, and Ingham Counties, is an area of 1,697 square miles in Michigan's Lower Peninsula and has as its hub the Lansing metropolitan area. The land surface ranges in altitude from about 700 to about 1,000 feet. The region receives an average of about 31 inches of precipitation each year. </p><p>The population is nearing 400,000 and by 1990 will be near 600,000. Average daily water use is slightly more than 30 million gallons today; by 1980 it will be about 50 million gallons, and by 1990 it will probably be about 70 million gallons. </p><p>The Tri-County region is drained by seven river systems. The median annual 7 -day mean low flows of the principal streams in these systems were measured at the point farthest downstream within the region. These values, in cubic feet per second, are as follows: Grand River, 180; Maple River, 34; Looking Glass River, 28; Red Cedar River, 30; Portage Creek, 15; Battle Creek, 20; and Thornapple River, 24-a total of 331 cubic feet per second or about 220 million gallons per day. The areal variance in 7-day low-flow runoff ranges from 0 to 0.15 cubic foot per second per square mile. </p><p>The principal source of ground water in the Tri-County region is a complex aquifer system composed of the Saginaw and Grand River Formations and some of the overlying glacial sediments. This aquifer yields between 300 and 700 gallons per minute to individual wells in much of the western half of Ingham County, in the eastern half of Clinton County, in a small area in southeastern Clinton County, and in northeastern Eaton County. In some parts of the region, the glacial sediments are favorable for development of moderate to large supplies of water. Minor aquifers in the region are the Bayport, Michigan, and Marshall Formations. </p><p>Providing water supplies in the future requires complete and comprehensive water-management programs. Such management programs involve determining which of several alternative water-development systems is the best. Some of the chief factors and methods that must be considered when planning these systems are combined use of ground and surface water, artificial recharge, treatment of wastes, use of storage reservoirs, and importation of water from the Great Lakes.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1969","usgsCitation":"Vanlier, K.E., Wood, W., and Brunett, J.O., 1973, Water-supply development and management alternatives for Clinton, Eaton, and Ingham Counties, Michigan: U.S. Geological Survey Water Supply Paper 1969, Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller, https://doi.org/10.3133/wsp1969.","productDescription":"Document: vii, 111 p.; 3 Plates: 35.70 x 31.97 inches or smaller","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":139081,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1969/report-thumb.jpg"},{"id":247253,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-1.pdf","size":"5337","linkFileType":{"id":1,"text":"pdf"}},{"id":247254,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-2.pdf","size":"10148","linkFileType":{"id":1,"text":"pdf"}},{"id":247255,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1969/plate-3.pdf","size":"13282","linkFileType":{"id":1,"text":"pdf"}},{"id":29452,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1969/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Michigan","county":"Clinton County, Eaton County, Ingham County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-84.3681,43.1172],[-84.3675,42.9561],[-84.3679,42.9439],[-84.3666,42.861],[-84.3668,42.8561],[-84.3649,42.7746],[-84.1593,42.7779],[-84.1519,42.685],[-84.146,42.5999],[-84.1402,42.4239],[-84.2539,42.4236],[-84.2607,42.4242],[-84.3676,42.4242],[-84.3677,42.4224],[-84.4864,42.4215],[-84.6026,42.4215],[-84.7207,42.4209],[-84.83,42.421],[-84.8375,42.4215],[-84.9561,42.4221],[-85.0667,42.4215],[-85.0736,42.4211],[-85.0738,42.5956],[-85.0745,42.7707],[-84.9577,42.7712],[-84.8391,42.7706],[-84.8376,42.857],[-84.8393,42.9434],[-84.8382,43.1199],[-84.6022,43.1185],[-84.3681,43.1172]]]},\"properties\":{\"name\":\"Clinton\",\"state\":\"MI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99fe","contributors":{"authors":[{"text":"Vanlier, Kenneth Eugene","contributorId":6840,"corporation":false,"usgs":true,"family":"Vanlier","given":"Kenneth","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":145915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, Warren W.","contributorId":47770,"corporation":false,"usgs":false,"family":"Wood","given":"Warren W.","affiliations":[{"id":6601,"text":"Michigan State University","active":true,"usgs":false}],"preferred":false,"id":145916,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brunett, Jilann O.","contributorId":92230,"corporation":false,"usgs":true,"family":"Brunett","given":"Jilann","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":145917,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61276,"text":"mf502 - 1973 - Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska, to Canadian border, part V, Coleen Quadrangle (north half), Alaska","interactions":[],"lastModifiedDate":"2023-04-05T16:30:14.990942","indexId":"mf502","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"502","title":"Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska, to Canadian border, part V, Coleen Quadrangle (north half), Alaska","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf502","usgsCitation":"1973, Preliminary geologic map of a prospective transportation route from Prudhoe Bay, Alaska, to Canadian border, part V, Coleen Quadrangle (north half), Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 502, 2 Plates: 43.51 x 22.08 inches and 19.19 x 24.73 inches, https://doi.org/10.3133/mf502.","productDescription":"2 Plates: 43.51 x 22.08 inches and 19.19 x 24.73 inches","costCenters":[],"links":[{"id":415248,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0502/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":415247,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0502/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":408937,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2948.htm","linkFileType":{"id":5,"text":"html"}},{"id":180626,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0502/report-thumb.jpg"}],"country":"United States","state":"Alaska","otherGeospatial":"Coleen Quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -144,\n              68.8\n            ],\n            [\n              -144,\n              68\n            ],\n            [\n              -141,\n              68\n            ],\n            [\n              -141,\n              68.8\n            ],\n            [\n              -144,\n              68.8\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db69924f","contributors":{"compilers":[{"text":"Yeend, Warren","contributorId":20405,"corporation":false,"usgs":true,"family":"Yeend","given":"Warren","affiliations":[],"preferred":false,"id":868584,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}}
,{"id":48199,"text":"ofr73264 - 1973 - Geohydrology and artificial-recharge potential of the Irvine area, Orange County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:10:41","indexId":"ofr73264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-264","title":"Geohydrology and artificial-recharge potential of the Irvine area, Orange County, California","docAbstract":"The Irvine area is in hydraulic continuity with the rest of the coastal plain in Orange County. Factors that distinguish the aquifer section of the Irvine area from that in other parts of the coastal plain are a low permeability, a high clay and silt content, and a thin alluvial sequence. Rapid facies change and the large percentage of silt and clay in the section locally result in confining conditions. The aquifer, most of which is included in the Fernando Formation, is as much as 1,300 feet thick beneath parts of the plain. The alluvium overlying the Fernando Formation averages about 200-250 feet in thickness and also contains significant amounts of silt and clay.\r\n\r\nTransmissivities range from 25,000 to 100,000 gallons per day per foot in the Irvine area, values which are much lower than those in the rest of the coastal plain in Orange County. \r\n\r\nWater levels have recovered as much as 60 feet from the low levels of the early 1950's. Water-level maps indicate that in the winter non-pumping season water tends to move toward upper Newport Bay and the rest of the coastal plain. During the summer pumping season a cone of depression develops, reversing the winter gradient. \r\n\r\nThe average dissolved-solids content of the ground water is about 800 milligrams per liter. The most prevalent cations are sodium and calcium; the most prevalent anions are bicarbonate and sulfate. No long-term degradation of water quality has occurred, with the exception of a slight increase in dissolved solids. \r\n\r\nNo areas in the Irvine area are suitable for the large-scale spreading of water for artificial recharge. Clay and silt predominate in the section beneath the Tustin plain, and in the foothill areas either bedrock is close to the surface or the alluvium is fine grained.","language":"ENGLISH","doi":"10.3133/ofr73264","usgsCitation":"Singer, J.A., 1973, Geohydrology and artificial-recharge potential of the Irvine area, Orange County, California: U.S. Geological Survey Open-File Report 73-264, 44 p.  ill., maps ; 27 cm., https://doi.org/10.3133/ofr73264.","productDescription":"44 p.  ill., maps ; 27 cm.","costCenters":[],"links":[{"id":171456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0264/report-thumb.jpg"},{"id":84913,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8d7e","contributors":{"authors":[{"text":"Singer, John A.","contributorId":48976,"corporation":false,"usgs":true,"family":"Singer","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":236956,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48189,"text":"ofr73237 - 1973 - Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal","interactions":[],"lastModifiedDate":"2020-05-12T17:40:47.892257","indexId":"ofr73237","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-237","title":"Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr73237","usgsCitation":"Robertson, J., 1973, Comments on the use of numerical model by Kerr-McGee Corporation in appraising effects of subsurface liquid waste disposal: U.S. Geological Survey Open-File Report 73-237, 5 p., https://doi.org/10.3133/ofr73237.","productDescription":"5 p.","costCenters":[],"links":[{"id":171829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0237/report-thumb.jpg"},{"id":374695,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0237/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae654","contributors":{"authors":[{"text":"Robertson, J.B.","contributorId":85173,"corporation":false,"usgs":true,"family":"Robertson","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":236943,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48184,"text":"ofr73228 - 1973 - Wolf River at Memphis, Tennessee: floodflow characteristics along proposed Interstate Highway 240, Shelby County","interactions":[],"lastModifiedDate":"2014-04-09T13:11:27","indexId":"ofr73228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","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":"73-228","title":"Wolf River at Memphis, Tennessee: floodflow characteristics along proposed Interstate Highway 240, Shelby County","docAbstract":"This report has been prepared by the U.S. Geological Survey at the request of Mr. Henry Derthick, Engineer of Structures of the Tennessee Department of Transportation, under the authority of a cooperative agreement between the two agencies. It supplements information contained in a report with the same title dated September 1966. The Department of Transportation proposes to construct a segment of Interstate Highway 240 and several bridges across the Wolf River on the northern side off Memphis, Shelby Count. Mt. Derthick has requested an analysis of the 50-year flood or the maximum flood of record to determine the possible effect of the proposed construction on flood profiles along the Wolf River.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr73228","usgsCitation":"Randolph, W.J., and Gamble, C.R., 1973, Wolf River at Memphis, Tennessee: floodflow characteristics along proposed Interstate Highway 240, Shelby County: U.S. Geological Survey Open-File Report 73-228, Report: 5 p.; 1 Plate: 26.26 x 21.23 inches, https://doi.org/10.3133/ofr73228.","productDescription":"Report: 5 p.; 1 Plate: 26.26 x 21.23 inches","numberOfPages":"7","costCenters":[],"links":[{"id":286002,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0228/plate-1.pdf"},{"id":286000,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0228/report-thumb.jpg"},{"id":286001,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0228/report.pdf"}],"country":"United States","state":"Tennessee","county":"Shelby County","city":"Memphis","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -90.310298,34.994185 ], [ -90.310298,35.409483 ], [ -89.632779,35.409483 ], [ -89.632779,34.994185 ], [ -90.310298,34.994185 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b4d","contributors":{"authors":[{"text":"Randolph, William J.","contributorId":35645,"corporation":false,"usgs":true,"family":"Randolph","given":"William","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":236938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":236937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56788,"text":"wdrLA721 - 1973 - Water resources data for Louisiana, water year 1972","interactions":[],"lastModifiedDate":"2025-05-22T20:04:46.06827","indexId":"wdrLA721","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1973","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"LA-72-1","title":"Water resources data for Louisiana, water year 1972","docAbstract":"<p>Water-resources data for the 1972 water year for Louisiana, including records of streamflow or reservoir storage at gaging stations, partial-record stations, and miscellaneous sites, and records of water-quality data on the chemical and physical characteristics of surface water are given in this report. Records for a few pertinent gaging stations in bordering States are also included. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey under the direction of Albert N. Cameron, district chief. These data represent that portion of the National Water Data System collected by the U.S. Geological Survey and cooperating State and federal agencies in Louisiana.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA721","collaboration":"Prepared in cooperation with the Louisiana Department of Public Works and with other State and Federal agencies","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1973, Water resources data for Louisiana, water year 1972: U.S. Geological Survey Water Data Report LA-72-1, x, 226 p., https://doi.org/10.3133/wdrLA721.","productDescription":"x, 226 p.","costCenters":[],"links":[{"id":175201,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1972/la-72-1/report-thumb.jpg"},{"id":486440,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1972/la-72-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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