{"pageNumber":"6757","pageRowStart":"168900","pageSize":"25","recordCount":184617,"records":[{"id":57723,"text":"ofr62162 - 1962 - Surface water of Beaver Creek Basin, in South-Central Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr62162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-162","title":"Surface water of Beaver Creek Basin, in South-Central Oklahoma","docAbstract":"Annual discharge from Beaver Creek basin is estimated to have averaged 217,000 acre-feet during a 19-year base period, water years 1938-56, equivalent to an average annual runoff depth of 4.7 inches over the 857 square-mile drainage area. About 55,000 acre-feet per year comes from Little Beaver Creek basin, a tributary drainage of 195 square miles.\r\nYearly streamflow is highly variable. The discharge of Little Beaver Creek near Duncan during 13-year period of record (water years 1949-61) has ranged from 86,530 acre-feet in calendar year 1957 to 4,880 acre-feet in 1956, a ratio of almost 18 to 1.\r\n\r\nHighest runoff within a year tends to occur in the spring months of May and June, a 2-month period that, on the average, accounts for more than half of the annual discharge of Little Beaver Creek near Duncan. The average monthly runoff during record was lowest in January. Variation in daily streamflow is such that while the average discharge for the 13-year period of record was 50.1 cfs (cubic feet per second), the daily discharge was more than 6 cfs only about half of the time. There was no flow at the site 19 percent of the time during the period.\r\n\r\nSome base runoff usually exists in the headwaters of Beaver and Little Beaver Creeks, and in the lower reaches of Beaver Creek. Low flow in Cow Creek tends to be sustained by waste water from Duncan, where water use in 1961 averaged 4 million gallons per day. In the remainder of the basin, periods of no flow occur in most years.\r\n\r\nThe surface water of Beaver Creek basin is very hard but in general is usable for municipal, agricultural and industrial purposes. The chemical character of the water is predominantly a calcium, magnesium bicarbonate type of water in the lower three quarters of the basin, except in Cow Creek where oil-field brines induce a distinct sodium, calcium chloride characteristic at low and medium flows. A calcium sulfate type of water occurs in most of the northern part of the basin except in headwater areas underlain by the Rush Springs Sandstone, where quality is similar to that in the lower basin.\r\n\r\nThe report gives an estimate of the average discharge at several sites in Beaver Creek basin for a 19-year base period, October 1937 to September 1956. Duration curves of daily discharge for Little Beaver Creek near Duncan and Beaver Creek near Waurika are shown for the period of record. Monthly and annual discharge records for these gaging stations are presented. The results of 52 discharge measurements at 17 other sites in the basin are tabulated, with 5 groups being plotted as discharge profiles. Storage requirements for regulated discharge at the two gaging stations are shown.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr62162","usgsCitation":"Laine, L., and Murphy, J., 1962, Surface water of Beaver Creek Basin, in South-Central Oklahoma: U.S. Geological Survey Open-File Report 62-162, 28 p., https://doi.org/10.3133/ofr62162.","productDescription":"28 p.","costCenters":[],"links":[{"id":184243,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698203","contributors":{"authors":[{"text":"Laine, L.L.","contributorId":100464,"corporation":false,"usgs":true,"family":"Laine","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":257642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Murphy, J.J.","contributorId":69144,"corporation":false,"usgs":true,"family":"Murphy","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":257641,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71759,"text":"tei805 - 1962 - Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei805","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"805","title":"Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes","language":"ENGLISH","doi":"10.3133/tei805","usgsCitation":"LeGrand, H.E., 1962, Geology and ground-water hydrology of the Atlantic and Gulf coastal plain as related to disposal of radioactive wastes: U.S. Geological Survey Trace Elements Investigations 805, 170 p., 33 fig. 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,{"id":34931,"text":"b1107E - 1962 - Uranium and other trace elements in Devonian and Mississippian black shales in the central midcontinent area","interactions":[],"lastModifiedDate":"2019-05-10T09:05:51","indexId":"b1107E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1107","chapter":"E","title":"Uranium and other trace elements in Devonian and Mississippian black shales in the central midcontinent area","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1107E","usgsCitation":"Landis, E.R., 1962, Uranium and other trace elements in Devonian and Mississippian black shales in the central midcontinent area: U.S. Geological Survey Bulletin 1107, p. 289-336, ill. (3 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1107E.","productDescription":"p. 289-336, ill. (3 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":62883,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1107e/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62884,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1107e/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62885,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1107e/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1107e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":164346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1107e/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d571","contributors":{"authors":[{"text":"Landis, Edwin R.","contributorId":48553,"corporation":false,"usgs":true,"family":"Landis","given":"Edwin","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":213831,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2837,"text":"wsp1619V - 1962 - Alluvial aquifer in northeastern Louisiana — A large source of water","interactions":[],"lastModifiedDate":"2022-01-13T22:37:26.8892","indexId":"wsp1619V","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1619","chapter":"V","title":"Alluvial aquifer in northeastern Louisiana — A large source of water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1619V","usgsCitation":"Turcan, A., and Meyer, R.R., 1962, Alluvial aquifer in northeastern Louisiana — A large source of water: U.S. Geological Survey Water Supply Paper 1619, iv, 28 p., https://doi.org/10.3133/wsp1619V.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":394362,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24836.htm"},{"id":138973,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1619v/report-thumb.jpg"},{"id":29403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1619v/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Louisiana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.2840,\n              32.275\n            ],\n            [\n              -90.9790,\n              32.275\n            ],\n            [\n              -90.9790,\n              32.495\n            ],\n            [\n              -91.2840,\n              32.495\n            ],\n            [\n              -91.2840,\n              32.275\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db6879ea","contributors":{"authors":[{"text":"Turcan, A. N.","contributorId":34114,"corporation":false,"usgs":true,"family":"Turcan","given":"A. N.","affiliations":[],"preferred":false,"id":145879,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, R. R.","contributorId":20725,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145878,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63521,"text":"gp366 - 1962 - Aeromagnetic map of the Newtown quadrangle, Fairfield, Litchfield and New Haven Counties, Connecticut","interactions":[],"lastModifiedDate":"2021-11-18T21:26:42.644764","indexId":"gp366","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"366","title":"Aeromagnetic map of the Newtown quadrangle, Fairfield, Litchfield and New Haven Counties, Connecticut","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp366","usgsCitation":"Popenoe, P., Bromery, R.W., and Kirby, J., 1962, Aeromagnetic map of the Newtown quadrangle, Fairfield, Litchfield and New Haven Counties, Connecticut: U.S. Geological Survey Geophysical Investigations Map 366, 1 Plate: 23.24 × 27.56 inches, https://doi.org/10.3133/gp366.","productDescription":"1 Plate: 23.24 × 27.56 inches","costCenters":[],"links":[{"id":391893,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_436.htm"},{"id":253159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0366/report-thumb.jpg"},{"id":249652,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0366/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249651,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0366/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Connecticut","county":"Fairfield County, Litchfield County, New Haven County","otherGeospatial":"Newtown quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -73.375,41.375 ], [ -73.375,41.5 ], [ -73.25,41.5 ], [ -73.25,41.375 ], [ -73.375,41.375 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691c1f","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":269035,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kirby, J.R.","contributorId":6428,"corporation":false,"usgs":true,"family":"Kirby","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":269034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71758,"text":"tei804 - 1962 - Selected logs and drilling records of wells and test holes drilled at the Nevada test site prior to 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei804","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"804","title":"Selected logs and drilling records of wells and test holes drilled at the Nevada test site prior to 1960","language":"ENGLISH","doi":"10.3133/tei804","usgsCitation":"Moore, J.E., 1962, Selected logs and drilling records of wells and test holes drilled at the Nevada test site prior to 1960: U.S. Geological Survey Trace Elements Investigations 804, 54 p. : ill., map ; 27 cm.; 4 figs.; 4 tables, https://doi.org/10.3133/tei804.","productDescription":"54 p. : ill., map ; 27 cm.; 4 figs.; 4 tables","costCenters":[],"links":[{"id":191693,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/804/report-thumb.jpg"},{"id":90985,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/804/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a04e4b07f02db5f853c","contributors":{"authors":[{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":47242,"text":"ofr6298 - 1962 - Geologic map of Butler County, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:54","indexId":"ofr6298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-98","title":"Geologic map of Butler County, Pennsylvania","language":"ENGLISH","doi":"10.3133/ofr6298","usgsCitation":"Patterson, E., and Van Lieu, J., 1962, Geologic map of Butler County, Pennsylvania: U.S. Geological Survey Open-File Report 62-98, 1 map, https://doi.org/10.3133/ofr6298.","productDescription":"1 map","costCenters":[],"links":[{"id":168387,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":84213,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0098/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a323a","contributors":{"authors":[{"text":"Patterson, E. D.","contributorId":56278,"corporation":false,"usgs":true,"family":"Patterson","given":"E. D.","affiliations":[],"preferred":false,"id":234889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Van Lieu, J. A.","contributorId":21203,"corporation":false,"usgs":true,"family":"Van Lieu","given":"J. A.","affiliations":[],"preferred":false,"id":234888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2392,"text":"wsp1604 - 1962 - Geology and ground-water resources of Fond du Lac County, Wisconsin","interactions":[{"subject":{"id":57717,"text":"ofr5989 - 1959 - Geology and ground-water resources of Fond De Lac County, Wisconsin","indexId":"ofr5989","publicationYear":"1959","noYear":false,"title":"Geology and ground-water resources of Fond De Lac County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":2392,"text":"wsp1604 - 1962 - Geology and ground-water resources of Fond du Lac County, Wisconsin","indexId":"wsp1604","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of Fond du Lac County, Wisconsin"},"id":1}],"lastModifiedDate":"2015-10-02T15:01:34","indexId":"wsp1604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1604","title":"Geology and ground-water resources of Fond du Lac County, Wisconsin","docAbstract":"<p>The principal water-bearing rocks underlying Fond du Lac County, Wis., are sandstones of Cambrian and Ordovician age and dolomite of Silurian age. Other aquifers include dolomite of Ordovician age and sand. and gravel of Quaternary age. Crystalline rocks of Precambrian age, which underlie all the water-bearing formations, form a practically impermeable basement complex and yield little or no water to wells. Ground water is the source of all public and most private and industrial water supplies in the county. The municipalities and industries obtain water chiefly from wells that penetrate the sandstones of Cambrian and Ordorician age. The Platteville formation and Galena dolomite of Ordovician age and the Niagara dolomite of Silurian age supply water to most domestic and stock wells and to a few industrial wells. Several buried valleys in the bedrock surface contain water-bearing deposits of sand and gravel. The source of the ground water in Fond du Lac County is local precipitation. Recharge to the water-bearing beds occurs in most of the county but is greatest where the bedrock formations are near the surface. Ground water is discharged by seeps and springs, by evaporation and transpiration, and by wells. Ground-water levels in wells fluctuate in response to recharge and to natural discharge and pumping. In areas not affected by pumping, water levels generally decline through the summer months because of natural discharge and lack of recharge, recover slightly in the fall after the first killing frost, decline during the winter, and recover in the spring when recharge is greatest. In areas of heavy pumping, the water levels are lowest in late summer and highest in late winter. Water levels in wells in the Fond du Lac area were about 5 to 50 feet above the land surface in 1885, but they had declined to as low as 185 feet below the land surface by 1957. Coefficients of transmissibility and storage of the sandstones of Cambrian and Ordovician age were determined by making controlled aquifer tests at Fond du Lac. The coefficients were verified by comparing computed water-level declines with actual declines. The computed values were within about 30 percent of the actual values, a reasonable agreement for coefficients of this type. Probable declines of water levels by 1966 were computed, using the same coefficients of transmissibility and storage. If the distribution of wells and the rate of pumping remain the same in 1957-66 as they were in 1956, the water levels will decline about 5 feet more by 1966. If, however, the distribution of pumped wells remains the same but the pumping by the city of Fond du Lac increases at a uniform rate from the 3 mgd (million gallons per day) pumped in 1956 to 5 mgd in 1966, the water levels in 1966 will be at least 60 feet below those of 1956. Dispersal of wells to the northwest toward the recharge area would reduce the water-level declines. The results of pumping tests, of test holes tapping the Niagara dolomite indicate that wells producing at least 200 gpm (gallons per minute) could be developed east of the Niagara escarpment. The ground water in Fond do Lac County is, in general, a hard calcium and magnesium bicarbonate water, which contains excessive iron in some areas.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1604","collaboration":"Prepared in cooperation with Geological and Natural History Survey, University of Wisconsin, and the city of Fond Du Lac","usgsCitation":"Newport, T., 1962, Geology and ground-water resources of Fond du Lac County, Wisconsin: U.S. Geological Survey Water Supply Paper 1604, Report: iv, 52 p.; 5 Plates: 22.00 x 29.69 inches or smaller, https://doi.org/10.3133/wsp1604.","productDescription":"Report: iv, 52 p.; 5 Plates: 22.00 x 29.69 inches or smaller","numberOfPages":"62","onlineOnly":"Y","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":28369,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1604/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1604/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Fond Du Lac County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.4033,43.9388],[-88.315,43.938],[-88.2826,43.9377],[-88.1619,43.9379],[-88.1622,43.8914],[-88.1608,43.8044],[-88.1599,43.7197],[-88.1597,43.6305],[-88.1601,43.6132],[-88.1608,43.5431],[-88.2808,43.5429],[-88.4008,43.5435],[-88.4013,43.6309],[-88.522,43.6323],[-88.6124,43.6325],[-88.6238,43.6326],[-88.6447,43.6332],[-88.6763,43.6334],[-88.7654,43.633],[-88.8862,43.6336],[-88.8854,43.721],[-88.8859,43.808],[-88.8857,43.8954],[-88.7651,43.8953],[-88.6446,43.895],[-88.524,43.8941],[-88.4561,43.8932],[-88.404,43.8923],[-88.4033,43.9388]]]},\"properties\":{\"name\":\"Fond Du Lac\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cee4b07f02db54572c","contributors":{"authors":[{"text":"Newport, Thomas G.","contributorId":93462,"corporation":false,"usgs":true,"family":"Newport","given":"Thomas G.","affiliations":[],"preferred":false,"id":145126,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1856,"text":"wsp1704 - 1962 - Surface water supply of the United States, 1960, part 2-B, South Atlantic slope and Eastern Gulf of Mexico Basins, Ogeechee River to Pearl River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1704","title":"Surface water supply of the United States, 1960, part 2-B, South Atlantic slope and Eastern Gulf of Mexico Basins, Ogeechee River to Pearl River","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1704","usgsCitation":"Hendricks, E.L., 1962, Surface water supply of the United States, 1960, part 2-B, South Atlantic slope and Eastern Gulf of Mexico Basins, Ogeechee River to Pearl River: U.S. Geological Survey Water Supply Paper 1704, x, 465 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1704.","productDescription":"x, 465 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1704/report-thumb.jpg"},{"id":27075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69429a","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":144255,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1809,"text":"wsp1547 - 1962 - Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60","interactions":[],"lastModifiedDate":"2017-09-07T10:08:46","indexId":"wsp1547","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1547","title":"Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60","docAbstract":"<p>This inventory of published and unpublished sediment-load data contains a list of the sediment-transport measurements in the United States and Puerto Rico during October 1950 to September 1960, made by the agencies associated with the Subcommittee on Sedimentation. Some of the agencies have miscellaneous sediment data, such as single observations at scattered stations or observations on very small watersheds, which are not listed in this inventory. Each entry contains the following: drainage area above station, period of record, number or frequency of observations, sampling equipment and method in which it was used, units of expression for load, particle-size analyses, and source of basic data or published results. </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1547","collaboration":"Prepared in cooperation with Sub-committee on Sedimentation, Agency Committee on Water Resources","usgsCitation":"Harris, K.F., 1962, Inventory of published and unpublished sediment-load data, United States and Puerto Rico, 1950-60: U.S. Geological Survey Water Supply Paper 1547, v, 117 p., https://doi.org/10.3133/wsp1547.","productDescription":"v, 117 p.","numberOfPages":"126","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1547/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1547/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c6e4b07f02db53fe24","contributors":{"authors":[{"text":"Harris, Kerry F.","contributorId":31732,"corporation":false,"usgs":true,"family":"Harris","given":"Kerry","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144191,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68386,"text":"ha49 - 1962 - Floods at Barberton, Ohio","interactions":[],"lastModifiedDate":"2022-12-12T20:13:05.34242","indexId":"ha49","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"49","title":"Floods at Barberton, Ohio","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha49","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Floods at Barberton, Ohio: U.S. Geological Survey Hydrologic Atlas 49, 1 Plate: 30.50 × 30.00 inches, https://doi.org/10.3133/ha49.","productDescription":"1 Plate: 30.50 × 30.00 inches","costCenters":[],"links":[{"id":185615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89886,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/049/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":410303,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15879.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Ohio","city":"Barberton","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -81.625,41 ], [ -81.625,41.125 ], [ -81.5,41.125 ], [ -81.5,41 ], [ -81.625,41 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7345","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":534503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34585,"text":"b1147A - 1962 - Reconnaissance study of uranium deposits in Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:09:20","indexId":"b1147A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1147","chapter":"A","title":"Reconnaissance study of uranium deposits in Arizona","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1147A","usgsCitation":"Granger, H.C., and Raup, R., 1962, Reconnaissance study of uranium deposits in Arizona: U.S. Geological Survey Bulletin 1147, p. A1-A54  :fig. ;24 cm., https://doi.org/10.3133/b1147A.","productDescription":"p. A1-A54  :fig. ;24 cm.","costCenters":[],"links":[{"id":164296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1147a/report-thumb.jpg"},{"id":62482,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1147a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db6364d4","contributors":{"authors":[{"text":"Granger, Harry Clifford","contributorId":8832,"corporation":false,"usgs":true,"family":"Granger","given":"Harry","email":"","middleInitial":"Clifford","affiliations":[],"preferred":false,"id":213220,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raup, Robert B.","contributorId":67880,"corporation":false,"usgs":true,"family":"Raup","given":"Robert B.","affiliations":[],"preferred":false,"id":213221,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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