{"pageNumber":"6319","pageRowStart":"157950","pageSize":"25","recordCount":184936,"records":[{"id":48064,"text":"ofr72300 - 1972 - An inventory of published and unpublished fluvial-sediment data for California, 1956-70","interactions":[],"lastModifiedDate":"2014-04-09T08:39:31","indexId":"ofr72300","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-300","title":"An inventory of published and unpublished fluvial-sediment data for California, 1956-70","docAbstract":"This inventory was prepared to provide a convenient reference to \npublished and unpublished fluvial-sediment data for water years 1956-70, \nand updates substantially previous inventories. Sediment stations are \nlisted in downstream order, and an alphabetical list of stations is also \nincluded. Figure 1 shows the approximate location of sediment stations \nin California. Most of the fluvial-sediment data in California were \ncollected by the U.S. Geological Survey, under cooperative agreements \nwith the following Federal, State, and local agencies: \nCalifornia Department of Water Resources, \nCalifornia Department of Navigation and Ocean Development, \nCalifornia Department of Fish and Game, \nBolinas Harbor District, \nMonterey County Flood Control and Water Conservation District, \nOrange County Flood Control District, \nRiverside County Flood Control and Water Conservation District, \nSan Diego County Department of Sanitation and Flood Control, \nSan Luis Obispo County, \nSan Mateo County, \nSanta Clara County Flood Control and Water District, \nSanta Cruz County Flood Control and Water Conservation District, \nSanta Cruz, city of, \nUniversity of California, \nVentura County Flood Control District, \nForest Service, U.S. Department of Agriculture, \nSoil Conservation Service, U.S. Department of Agriculture, \nCorps of Engineers, U.S. Army, \nBureau of Reclamation, U.S. Department of the Interior, \nNational Park Service, U.S. Department of the Interior. \nThis report was prepared by the Geological Survey under the general \nsupervision of R. Stanley Lord, district chief in charge of water-resources \ninvestigations in California.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Menlo Park, CA","doi":"10.3133/ofr72300","usgsCitation":"Porterfield, G., 1972, An inventory of published and unpublished fluvial-sediment data for California, 1956-70: U.S. Geological Survey Open-File Report 72-300, ii, 26 p., https://doi.org/10.3133/ofr72300.","productDescription":"ii, 26 p.","numberOfPages":"28","temporalStart":"1956-01-01","temporalEnd":"1970-12-31","costCenters":[],"links":[{"id":161968,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0300/report-thumb.jpg"},{"id":285917,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0300/report.pdf"}],"country":"United States","state":"California","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124.0,33.0 ], [ -124.0,42.0 ], [ -115.0,42.0 ], [ -115.0,33.0 ], [ -124.0,33.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db68434c","contributors":{"authors":[{"text":"Porterfield, George","contributorId":68719,"corporation":false,"usgs":true,"family":"Porterfield","given":"George","email":"","affiliations":[],"preferred":false,"id":236761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56584,"text":"wdrOK712 - 1972 - Water resources data for Oklahoma, water year 1971; Part 2, Water quality records","interactions":[],"lastModifiedDate":"2020-02-20T10:02:46","indexId":"wdrOK712","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"OK-71-2","title":"Water resources data for Oklahoma, water year 1971; Part 2, Water quality records","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrOK712","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Oklahoma, water year 1971; Part 2, Water quality records: U.S. Geological Survey Water Data Report OK-71-2, vi, 271 p., 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,{"id":1217,"text":"wsp1999H - 1972 - Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1999H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1999","chapter":"H","title":"Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California","docAbstract":"The study area, which includes about 5,000 square miles of the southern part of the San Joaquin Valley, is a broad structural trough of mostly interior drainage. The Sierra Nevada on the east is composed of consolidated igneous and metamorphic rocks of pre-Tertiary age. The surface of these rocks slopes 4?-6? southwestward from the foothills and underlies the valley. The Coast Ranges on the west consist mostly of complexly folded and faulted consolidated marine and nonmarine sedimentary rocks of Jurassic, Cretaceous, and Tertiary age, which dip eastward and overlie the basement complex. Unconsolidated deposits, of late Pliocene to Holocene age, blanket the underlying consolidated rocks in the valley and are the source of most of the fresh ground water. The unconsolidated deposits, the subject of this report, are divided into informal stratigraphic units on the basis of source of sediment, environment of deposition, and texture. \r\n\r\nFlood-basin, lacustrine, and marsh deposits are fine grained and underlie the valley trough. They range in age from late Pliocene to Holocene. These deposits, consisting of nearly impermeable gypsiferous fine sand, silt, and clay, are more than 3,000 feet thick beneath parts of Tulare Lake bed. In other parts of the trough, flood-basin, lacustrine, and marsh deposits branch into clayey or silty clay tongues designated by the letter symbols A to F. Three of these tongues, the E, C, and A clays, lie beneath large areas of the southern part of the valley. \r\n\r\nThe E clay includes the Corcoran Clay Member of the Tulare Formation, the most extensive hydrologic confining layer in the valley. The E clay underlies about 3,500 square miles of bottom land and western slopes. The beds generally are dark-greenish-gray mostly diatomaceous silty clay of Pleistocene age. Marginally, the unit bifurcates into an upper and a lower stratum that contains thin beds of moderately yellowish-brown silt and sand. The E clay is warped into broad, gentle northwesterly trending anticlines and synclines. \r\n\r\nThe C clay, of Pleistocene age, is a fine-grained lacustrine or paludal deposit occurring 220-300 feet beneath Tulare Lake bed and parts of Fresno Slough. The beds consist of bluish-gray silty clay. Structural contours indicate that the C clay has been extensively warped and folded. \r\n\r\nThe A clay of Pleistocene and Holocene (?) age is a fine-grained lacustrine or paludal deposit occurring 10-60 feet beneath Buena Vista, Kern, and Tulare Lake beds, and parts of Fresno Slough. The clay is mainly blue or dark greenish gray, plastic, and highly organic. In some areas the unit is separated into an upper and a lower stratum by several feet of sand. A radiocarbon date of 26,780 ? 600 years was obtained from wood cored 3 feet beneath the clay. \r\n\r\nContinental deposits are arkosic beds of late Pliocene and Pleistocene (?) age and were derived from the Sierra Nevada, Tehachapi, and San Emigdio Mountains. In places, a reduced-oxidized contact transgresses the deposits derived from the Sierra Nevada. The reduced deposits consist of moderately permeable bluish-green or bluish-gray fine to medium sand, silt, and clay. The oxidized deposits consist mainly of poorly permeable yellowish-brown silt and fine sand. Deposits derived from the Tehachapi and the San Emigdio Mountains consist of poorly to moderately permeable yellowish-brown sand and silt. Continental and alluvial deposits of Tertiary and Quaternary age that were derived from the Coast Ranges consist mainly of poorly to moderately permeable yellowish-brown gravel, sand, silt, and clay. They include the Tulare Formation and overlying alluvial deposits. \r\n\r\nAlluvium is composed of coarse arkosic deposits derived from the Sierra Nevada, Tehachapi, and San Emigdio Mountains. A reduced-oxidized contact also transgresses the alluvial deposits derived from the Sierra Nevada. The oxidized deposits consist of poorly to highly permeable yellowish-brown gravel, sand, silt, and clay. The reduc","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1999H","usgsCitation":"Croft, M., 1972, Subsurface geology of the late Tertiary and Quaternary water-bearing deposits of the southern part of the San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 1999, iv, 29 p. :illus. and portfolio (6 plates) ;24 cm., https://doi.org/10.3133/wsp1999H.","productDescription":"iv, 29 p. :illus. and portfolio (6 plates) ;24 cm.","costCenters":[],"links":[{"id":137986,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999h/report-thumb.jpg"},{"id":26116,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26117,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26118,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26119,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26120,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26121,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999h/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26122,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699a52","contributors":{"authors":[{"text":"Croft, M.G.","contributorId":55413,"corporation":false,"usgs":true,"family":"Croft","given":"M.G.","email":"","affiliations":[],"preferred":false,"id":143384,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68820,"text":"oc65 - 1972 - Chart showing correlation of selected key units in the organic-rich sequence of the Green River Formation, Piceance Creek basin, Colorado, and Uinta Basin, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:24","indexId":"oc65","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":328,"text":"Oil and Gas Investigation Chart","code":"OC","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"65","title":"Chart showing correlation of selected key units in the organic-rich sequence of the Green River Formation, Piceance Creek basin, Colorado, and Uinta Basin, Utah","language":"ENGLISH","doi":"10.3133/oc65","isbn":"0607823682","usgsCitation":"Cashion, W.B., and Donnell, J., 1972, Chart showing correlation of selected key units in the organic-rich sequence of the Green River Formation, Piceance Creek basin, Colorado, and Uinta Basin, Utah: U.S. Geological Survey Oil and Gas Investigation Chart 65, 1 map. 22 1/2 by 35 inches, https://doi.org/10.3133/oc65.","productDescription":"1 map. 22 1/2 by 35 inches","costCenters":[],"links":[{"id":104856,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5225.htm","linkFileType":{"id":5,"text":"html"},"description":"5225"},{"id":188520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90434,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/oc/065/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2484706","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,39 ], [ -111.5,41 ], [ -107.70083333333334,41 ], [ -107.70083333333334,39 ], [ -111.5,39 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c9c","contributors":{"authors":[{"text":"Cashion, W. B.","contributorId":75525,"corporation":false,"usgs":true,"family":"Cashion","given":"W.","middleInitial":"B.","affiliations":[],"preferred":false,"id":278981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Donnell, John R.","contributorId":84330,"corporation":false,"usgs":true,"family":"Donnell","given":"John R.","affiliations":[],"preferred":false,"id":278982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63656,"text":"gp830 - 1972 - Aeromagnetic and geologic map of part of northwestern Montana and northern Idaho","interactions":[],"lastModifiedDate":"2025-09-23T19:07:07.352151","indexId":"gp830","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"830","title":"Aeromagnetic and geologic map of part of northwestern Montana and northern Idaho","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp830","usgsCitation":"Kleinkopf, M.D., Harrison, J.E., and Zartman, R., 1972, Aeromagnetic and geologic map of part of northwestern Montana and northern Idaho: U.S. Geological Survey Geophysical Investigations Map 830, Report: 5 p.; 1 Plate: 34.14 x 30.52 inches, https://doi.org/10.3133/gp830.","productDescription":"Report: 5 p.; 1 Plate: 34.14 x 30.52 inches","costCenters":[],"links":[{"id":253341,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0830/report-thumb.jpg"},{"id":249871,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0830/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249870,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0830/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":495936,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6183.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Idaho, Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -116.5,\n              48.5\n            ],\n            [\n              -116.5,\n              47\n            ],\n            [\n              -114.4167,\n              47\n            ],\n            [\n              -114.4167,\n              48.5\n            ],\n            [\n              -116.5,\n              48.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db6989cc","contributors":{"authors":[{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":269314,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":269316,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zartman, R. E.","contributorId":15632,"corporation":false,"usgs":true,"family":"Zartman","given":"R. E.","affiliations":[],"preferred":false,"id":269315,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63657,"text":"gp837 - 1972 - Aeromagnetic, Bouguer gravity, and generalized geologic maps of the central part of the Little Belt Mountains, Montana","interactions":[],"lastModifiedDate":"2025-07-08T21:26:56.00563","indexId":"gp837","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"837","title":"Aeromagnetic, Bouguer gravity, and generalized geologic maps of the central part of the Little Belt Mountains, Montana","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp837","usgsCitation":"Kleinkopf, M.D., Witkind, I.J., and Keefer, W.R., 1972, Aeromagnetic, Bouguer gravity, and generalized geologic maps of the central part of the Little Belt Mountains, Montana: U.S. Geological Survey Geophysical Investigations Map 837, Report: 4 p.; 1 Plate: 46.13 x 39.34 inches, https://doi.org/10.3133/gp837.","productDescription":"Report: 4 p.; 1 Plate: 46.13 x 39.34 inches","costCenters":[],"links":[{"id":491876,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6190.htm","linkFileType":{"id":5,"text":"html"}},{"id":253342,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0837/report-thumb.jpg"},{"id":249873,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0837/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249872,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0837/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"62500","country":"United States","state":"Montana","otherGeospatial":"Little Belt Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.5,\n              46.75\n            ],\n            [\n              -110.5,\n              47.25\n            ],\n            [\n              -110.75,\n              47.25\n            ],\n            [\n              -110.75,\n              46.75\n            ],\n            [\n              -110.5,\n              46.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689c18","contributors":{"authors":[{"text":"Kleinkopf, M. D.","contributorId":10036,"corporation":false,"usgs":true,"family":"Kleinkopf","given":"M.","middleInitial":"D.","affiliations":[],"preferred":false,"id":269317,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witkind, I. J.","contributorId":54221,"corporation":false,"usgs":true,"family":"Witkind","given":"I.","middleInitial":"J.","affiliations":[],"preferred":false,"id":269319,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Keefer, W. R.","contributorId":21538,"corporation":false,"usgs":true,"family":"Keefer","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":269318,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":64284,"text":"gp815 - 1972 - Aeromagnetic reconnaissance and generalized geologic map of the San Andreas fault between San Francisco and San Bernardino, California","interactions":[],"lastModifiedDate":"2025-07-08T20:11:03.570688","indexId":"gp815","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"815","title":"Aeromagnetic reconnaissance and generalized geologic map of the San Andreas fault between San Francisco and San Bernardino, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp815","usgsCitation":"Hanna, W.F., Brown, R., Ross, D.C., and Griscom, A., 1972, Aeromagnetic reconnaissance and generalized geologic map of the San Andreas fault between San Francisco and San Bernardino, California: U.S. Geological Survey Geophysical Investigations Map 815, 1 Plate: 44.32 x 32.31 inches, https://doi.org/10.3133/gp815.","productDescription":"1 Plate: 44.32 x 32.31 inches","costCenters":[],"links":[{"id":491865,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_6168.htm","linkFileType":{"id":5,"text":"html"}},{"id":254316,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0815/report-thumb.jpg"},{"id":250898,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0815/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250897,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0815/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"California","city":"San Bernardino, San Francisco","otherGeospatial":"San Andreas fault","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -122.5,\n              37.5417\n            ],\n            [\n              -122.5,\n              34.1\n            ],\n            [\n              -117.4667,\n              34.1\n            ],\n            [\n              -117.4667,\n              37.5417\n            ],\n            [\n              -122.5,\n              37.5417\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689d67","contributors":{"authors":[{"text":"Hanna, W. F.","contributorId":6835,"corporation":false,"usgs":true,"family":"Hanna","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":270431,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brown, R.D. Jr.","contributorId":19997,"corporation":false,"usgs":true,"family":"Brown","given":"R.D.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":270432,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ross, D. C.","contributorId":103681,"corporation":false,"usgs":true,"family":"Ross","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":270434,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griscom, Andrew","contributorId":23520,"corporation":false,"usgs":true,"family":"Griscom","given":"Andrew","email":"","affiliations":[],"preferred":false,"id":270433,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":36307,"text":"b1335 - 1972 - Sedimentary and igneous rocks of the Grays River Quadrangle, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1335","title":"Sedimentary and igneous rocks of the Grays River Quadrangle, Washington","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1335","usgsCitation":"Wolfe, E.W., and McKee, E.H., 1972, Sedimentary and igneous rocks of the Grays River Quadrangle, Washington: U.S. Geological Survey Bulletin 1335, v, 70 p. :illus., maps. ;23 cm., https://doi.org/10.3133/b1335.","productDescription":"v, 70 p. :illus., maps. ;23 cm.","costCenters":[],"links":[{"id":166622,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1335/report-thumb.jpg"},{"id":64239,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbe2e","contributors":{"authors":[{"text":"Wolfe, Edward W.","contributorId":79878,"corporation":false,"usgs":true,"family":"Wolfe","given":"Edward","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":216110,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKee, Edwin H. mckee@usgs.gov","contributorId":3728,"corporation":false,"usgs":true,"family":"McKee","given":"Edwin","email":"mckee@usgs.gov","middleInitial":"H.","affiliations":[],"preferred":true,"id":216109,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1144,"text":"wsp1757M - 1972 - Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1757M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1757","chapter":"M","title":"Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia","docAbstract":"Nine ground-water samples from the principal shallow and deep North Sahara aquifers of Algeria and Tunisia were examined to determine the relation of their chemical composition to corrosion and mineral encrustation thought to be contributing to observed decline in well capacities within a UNESCO/UNDP Special Fund Project area. Although the shallow and deep waters differ significantly in certain quality factors, all are sulfochloride types with corrosion potentials ranging from moderate to extreme. None appear to be sufficiently supersaturated with troublesome mineral species to cause rapid or severe encrustation of filter pipes or other well parts. However, calcium carbonate encrustation of deep-well cooling towers and related irrigation pipes can be expected because of loss of carbon dioxide and water during evaporative cooling. \r\n\r\nCorrosion products, particularly iron sulfide, can be expected to deposit in wells producing waters from the deep aquifers. This could reduce filterpipe openings and increase casing roughness sufficiently to cause significant reduction in well capacity. It seems likely, however, that normal pressure reduction due to exploitation of the artesian systems is a more important control of well performance. If troublesome corrosion and related encrustation are confirmed by downhole inspection, use of corrosion-resisting materials, such as fiber-glass casing and saw-slotted filter pipe (shallow wells only), or stainless-steel screen, will minimize the effects of the waters represented by these samples. A combination of corrosion-resisting stainless steel filter pipe electrically insulated from the casing with a nonconductive spacer and cathodic protection will minimize external corrosion of steel casing, if this is found to be a problem. However, such installations are difficult to make in very deep wells and difficult to control in remote areas. Both the shallow waters and the deep waters examined in this study will tend to cause soil salinization because their salt contents are relatively high, and both have sodium absorption ratios which are unfavorable to sodium-sensitive soils and vegetation. Proper drainage and soil treatment are the only means of overcoming these problems during irrigation.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1757M","usgsCitation":"Clarke, F., and Jones, B.F., 1972, Significance of ground-water chemistry in performance of North Sahara Tube wells in Algeria and Tunisia: U.S. Geological Survey Water Supply Paper 1757, vi, M1-M39 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1757M.","productDescription":"vi, M1-M39 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":137623,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1757m/report-thumb.jpg"},{"id":25925,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1757m/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f9e4b07f02db5f3ccc","contributors":{"authors":[{"text":"Clarke, Frank Eldridge","contributorId":107255,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank Eldridge","affiliations":[],"preferred":false,"id":143252,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, Blair F. bfjones@usgs.gov","contributorId":2784,"corporation":false,"usgs":true,"family":"Jones","given":"Blair","email":"bfjones@usgs.gov","middleInitial":"F.","affiliations":[{"id":436,"text":"National Research Program - Eastern Branch","active":true,"usgs":true}],"preferred":true,"id":143251,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1786,"text":"wsp1999I - 1972 - Water for cranberry culture in the Cranmoor area of central Wisconsin","interactions":[],"lastModifiedDate":"2015-10-02T13:26:50","indexId":"wsp1999I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1999","chapter":"I","title":"Water for cranberry culture in the Cranmoor area of central Wisconsin","docAbstract":"<p>The Cranmoor area of central Wisconsin is the principal cranberry producing area of the State. Cranberries are grown in only about 2.5 square miles of an 80-square-mile marsh and swamp in the Cranberry Creek basin. Cranberry growers have built reservoirs and ditches throughout 25 square miles of marsh for better management of the area's natural water supply. Additional water is diverted into the basin to supplement the cranberry needs. In the 1966-67 hydrologic budget for Cranberry Creek basin, annual inputs were 27.8 inches of precipitation, 3.8 inches of surface-water diversion into the basin, and 1.1 inches decrease in stored water. Annual outputs were. 20.8 inches of evapotranspiration, 11.7 inches of runoff, and 0.2 inch of groundwater outflow. During the 1966-67 period, precipitation averaged about 3 inches per year below normal. The water used for cranberry culture is almost exclusively surface water. Efficient management of the basin's water supply, plus intermittent diversions of about 100 cubic feet per second from outside the basin, provide cranberry growers with a sufficient quantity of water. Although the quantity of surface water is adequate, the pH (generally 5.7-6.7) is slightly high for optimum use. Dissolved oxygen is slightly low, generally between 4 and 10 milligrams per liter. The water is soft; iron and manganese contents vary seasonally, being high in winter and summer and low in spring. Additional supplies of surface water can be obtained by increasing diversions from outside the basin and by increasing reservoir capacity within the basin. Ground water, although not presently used for cranberries, is available in the central, southern, and eastern parts of the basin, where the thickness of the saturated alluvium exceeds 50 feet. Well yields in these areas might be as much as 1,000 gpm (gallons per minute). Additionally, well yields of as much as 1,000 gpm may be expected from saturated alluvium southeast of Cranberry Creek basin. Where saturated alluvium is less than 50 feet thick, in the northern and western parts of the basin, well yields generally are less than 50 gpm. Ground water is also available from sandstone in the western part of the basin. Where the sandstone is thickest (about 60 ft.), well yields may be as much as 200 gpm. The quality of ground water is similar to that of surface water. The pH of water from the shallow alluvium ranges between 6.0 and 6,6; the pH of water from the deep alluvium is about 7.0. Ground water is soft to moderately hard, 22 to 88 milligrams per liter, and contains excessive amounts of iron and manganese.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1999I","collaboration":"Prepared in cooperation with University Extension-the University of Wisconsin Geological and Natural History Survey","usgsCitation":"Hamilton, L.J., 1972, Water for cranberry culture in the Cranmoor area of central Wisconsin: U.S. Geological Survey Water Supply Paper 1999, Report: iii, 20 p.; 2 Plates: 34.50 x 24.00 inches and 17.00 x 27.00 inches, https://doi.org/10.3133/wsp1999I.","productDescription":"Report: iii, 20 p.; 2 Plates: 34.50 x 24.00 inches and 17.00 x 27.00 inches","numberOfPages":"26","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":138497,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1999i/report-thumb.jpg"},{"id":26922,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1999i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26921,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1999i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","city":"Cranmoor","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -90.3131103515625,\n              44.50825885600572\n            ],\n            [\n              -90.450439453125,\n              44.308126684886126\n            ],\n            [\n              -90.3570556640625,\n              44.05601169578525\n            ],\n            [\n              -90.164794921875,\n              44.07969327425713\n            ],\n            [\n              -90.02197265625,\n              44.24126379833979\n            ],\n            [\n              -89.9615478515625,\n              44.296332880058706\n            ],\n            [\n              -89.9176025390625,\n              44.37098696297173\n            ],\n            [\n              -89.945068359375,\n              44.46123053905882\n            ],\n            [\n              -90.0164794921875,\n              44.53175879707938\n            ],\n            [\n              -90.142822265625,\n              44.57873024377564\n            ],\n            [\n              -90.3131103515625,\n              44.50825885600572\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48d1e4b07f02db547e08","contributors":{"authors":[{"text":"Hamilton, Louis J.","contributorId":53768,"corporation":false,"usgs":true,"family":"Hamilton","given":"Louis","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":144154,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37435,"text":"ssrw154 - 1972 - Use of banding data in migratory game bird research and management","interactions":[],"lastModifiedDate":"2012-02-02T00:09:39","indexId":"ssrw154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"154","title":"Use of banding data in migratory game bird research and management","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Geis, A.D., 1972, Use of banding data in migratory game bird research and management: Special Scientific Report  - Wildlife 154, ii, 47 p.","productDescription":"ii, 47 p.","costCenters":[],"links":[{"id":112142,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785148?urlappend=%3Bseq=3"},{"id":167704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b7c","contributors":{"authors":[{"text":"Geis, Aelred D.","contributorId":86401,"corporation":false,"usgs":true,"family":"Geis","given":"Aelred","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":218074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48107,"text":"ofr7315 - 1972 - Feasibility study of East Coast Triassic basins for waste storage","interactions":[],"lastModifiedDate":"2012-02-02T00:10:04","indexId":"ofr7315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"73-15","title":"Feasibility study of East Coast Triassic basins for waste storage","language":"ENGLISH","doi":"10.3133/ofr7315","usgsCitation":"Bain, G.L., 1972, Feasibility study of East Coast Triassic basins for waste storage: U.S. Geological Survey Open-File Report 73-15, 113 p. ill., maps, https://doi.org/10.3133/ofr7315.","productDescription":"113 p. ill., maps","costCenters":[],"links":[{"id":100087,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-1_sheet_1.pdf","size":"8545","linkFileType":{"id":1,"text":"pdf"}},{"id":100088,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-1_sheet_2.pdf","size":"11902","linkFileType":{"id":1,"text":"pdf"}},{"id":100089,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-1_sheet_3.pdf","size":"5560","linkFileType":{"id":1,"text":"pdf"}},{"id":100090,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-figure_02.pdf","size":"2357","linkFileType":{"id":1,"text":"pdf"}},{"id":100091,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-figure_12.pdf","size":"506","linkFileType":{"id":1,"text":"pdf"}},{"id":100092,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1973/0015/plate-figure_24.pdf","size":"1878","linkFileType":{"id":1,"text":"pdf"}},{"id":162113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1973/0015/report-thumb.jpg"},{"id":84841,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1973/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9ba7","contributors":{"authors":[{"text":"Bain, George L.","contributorId":95114,"corporation":false,"usgs":true,"family":"Bain","given":"George","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":236821,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38731,"text":"pp724A - 1972 - Huntington Lake Quadrangle, central Sierra Nevada, California; analytic data","interactions":[],"lastModifiedDate":"2012-02-02T00:09:54","indexId":"pp724A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"724","chapter":"A","title":"Huntington Lake Quadrangle, central Sierra Nevada, California; analytic data","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1971","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp724A","usgsCitation":"Bateman, P.C., and Wones, D.R., 1972, Huntington Lake Quadrangle, central Sierra Nevada, California; analytic data: U.S. Geological Survey Professional Paper 724, 17 p., https://doi.org/10.3133/pp724A.","productDescription":"17 p.","costCenters":[],"links":[{"id":119576,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0724a/report-thumb.jpg"},{"id":65591,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0724a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62a59d","contributors":{"authors":[{"text":"Bateman, P. C.","contributorId":27851,"corporation":false,"usgs":true,"family":"Bateman","given":"P.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wones, D. R.","contributorId":104079,"corporation":false,"usgs":true,"family":"Wones","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220359,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35006,"text":"b1314D - 1972 - Distribution of minor elements in biotite samples from felsic intrusive rocks as a tool for correlation","interactions":[],"lastModifiedDate":"2012-02-02T00:09:46","indexId":"b1314D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1314","chapter":"D","title":"Distribution of minor elements in biotite samples from felsic intrusive rocks as a tool for correlation","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1314D","usgsCitation":"Lovering, T., 1972, Distribution of minor elements in biotite samples from felsic intrusive rocks as a tool for correlation: U.S. Geological Survey Bulletin 1314, iii, 29 p. :illus. ;24 cm., https://doi.org/10.3133/b1314D.","productDescription":"iii, 29 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":165490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1314d/report-thumb.jpg"},{"id":62947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1314d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640944","contributors":{"authors":[{"text":"Lovering, T.G.","contributorId":55014,"corporation":false,"usgs":true,"family":"Lovering","given":"T.G.","affiliations":[],"preferred":false,"id":213968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":42571,"text":"ofr72155 - 1972 - Saturated thickness of unconsolidated stratified deposits, Ellington Quadrangle, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:11:04","indexId":"ofr72155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-155","title":"Saturated thickness of unconsolidated stratified deposits, Ellington Quadrangle, Connecticut","language":"ENGLISH","doi":"10.3133/ofr72155","usgsCitation":"Handman, E., 1972, Saturated thickness of unconsolidated stratified deposits, Ellington Quadrangle, Connecticut: U.S. Geological Survey Open-File Report 72-155, 1 map, https://doi.org/10.3133/ofr72155.","productDescription":"1 map","costCenters":[],"links":[{"id":168760,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":80340,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0155/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fdbda","contributors":{"authors":[{"text":"Handman, E. H.","contributorId":63407,"corporation":false,"usgs":true,"family":"Handman","given":"E.","middleInitial":"H.","affiliations":[],"preferred":false,"id":226732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68142,"text":"ha459 - 1972 - Floods in Hampshire Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha459","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"459","title":"Floods in Hampshire Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha459","usgsCitation":"Mycyk, R.T., and Duerk, M.D., 1972, Floods in Hampshire Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 459, 1 col. map ;58 x 43 cm., on sheet 76 x 112 cm., https://doi.org/10.3133/ha459.","productDescription":"1 col. map ;58 x 43 cm., on sheet 76 x 112 cm.","costCenters":[],"links":[{"id":186373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89443,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/459/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.61749999999999,42 ], [ -88.61749999999999,42.1175 ], [ -88.5,42.1175 ], [ -88.5,42 ], [ -88.61749999999999,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e713c","contributors":{"authors":[{"text":"Mycyk, Roman T.","contributorId":58331,"corporation":false,"usgs":true,"family":"Mycyk","given":"Roman","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":277722,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Duerk, Marvin D.","contributorId":96768,"corporation":false,"usgs":true,"family":"Duerk","given":"Marvin","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":277723,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":6530,"text":"pp785 - 1972 - Petrology and stratigraphy of the Fra Mauro Formation at the Apollo 14 site","interactions":[],"lastModifiedDate":"2012-02-02T00:06:01","indexId":"pp785","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"785","title":"Petrology and stratigraphy of the Fra Mauro Formation at the Apollo 14 site","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp785","usgsCitation":"Wilshire, H.G., and Jackson, E., 1972, Petrology and stratigraphy of the Fra Mauro Formation at the Apollo 14 site: U.S. Geological Survey Professional Paper 785, 26 p., https://doi.org/10.3133/pp785.","productDescription":"26 p.","costCenters":[],"links":[{"id":118153,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0785/report-thumb.jpg"},{"id":34009,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0785/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d45","contributors":{"authors":[{"text":"Wilshire, Howard Gordon","contributorId":102479,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":152875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jackson, E.D.","contributorId":99524,"corporation":false,"usgs":true,"family":"Jackson","given":"E.D.","email":"","affiliations":[],"preferred":false,"id":152874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68059,"text":"ha476 - 1972 - Ground-water resources of Benson and Pierce Counties, north-central North Dakota","interactions":[],"lastModifiedDate":"2018-06-04T10:38:20","indexId":"ha476","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"476","title":"Ground-water resources of Benson and Pierce Counties, north-central North Dakota","docAbstract":"<p>The purpose of this investigation is to provide information about the ground-water resources in Benson and Pierce Counties that is sufficient for planning the safe and intelligent development of water supplies for irrigation, domestic, stock, industrial, and municipal purposes.&nbsp; The investigation is part of a statewide program to determine the location and extent of ground-water aquifers; to evaluate the occurrence and movement of ground water within the aquifers, including sources of recharge and discharge; to determine potential yields to wells developed in the aquifers; and to determine the chemical quality of ground water.</p><p>Benson and Pierce Counties cover an area of 2,512 square miles in north-central North Dakota.&nbsp; This study, which began in July 1967 and was completed in June 1971, was made cooperatively by the U.S. Geological Survey, the North Dakota State Water Commission, the North Dakota Geological Survey, and the Benson and Pierce Counties Water Management Districts.&nbsp; This interim report presents only the major conclusions of the study.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha476","usgsCitation":"Randich, P., 1972, Ground-water resources of Benson and Pierce Counties, north-central North Dakota: U.S. Geological Survey Hydrologic Atlas 476, 43.0 x 34.5 inches, 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,{"id":68232,"text":"ha383 - 1972 - Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas","interactions":[],"lastModifiedDate":"2012-02-10T00:11:15","indexId":"ha383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"383","title":"Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas","language":"ENGLISH","doi":"10.3133/ha383","usgsCitation":"Lamonds, A.G., 1972, Water-resources reconnaissance of the Ozark plateaus province, northern Arkansas: U.S. Geological Survey Hydrologic Atlas 383, 2 maps. ;99 x 112 cm. fold. to 30 x 20 cm., https://doi.org/10.3133/ha383.","productDescription":"2 maps. ;99 x 112 cm. fold. to 30 x 20 cm.","costCenters":[],"links":[{"id":188039,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89602,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89603,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89604,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89605,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89606,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89607,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89608,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89609,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/383/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,35.5 ], [ -94,36.5 ], [ -91,36.5 ], [ -91,35.5 ], [ -94,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9b55","contributors":{"authors":[{"text":"Lamonds, A. G.","contributorId":8450,"corporation":false,"usgs":true,"family":"Lamonds","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":277884,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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