{"pageNumber":"6235","pageRowStart":"155850","pageSize":"25","recordCount":165658,"records":[{"id":1162,"text":"wsp1357 - 1955 - Computations of total sediment discharge, Niobrara River near Cody, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1357","title":"Computations of total sediment discharge, Niobrara River near Cody, Nebraska","docAbstract":"A natural chute in the Niobrara River near Cody, Nebr., constricts the flow of the river except at high stages to a narrow channel in which the turbulence is sufficient to suspend nearly the total sediment discharge. Because much of the flow originates in the sandhills area of Nebraska, the water discharge and sediment discharge are relatively uniform. \r\n\r\nSediment discharges based on depth-integrated samples at a contracted section in the chute and on streamflow records at a recording gage about 1,900 feet upstream are available for the period from April 1948 to September 1953 but are not given directly as continuous records in this report. Sediment measurements have been made periodically near the gage and at other nearby relatively unconfined sections of the stream for comparison with measurements at the contracted section. \r\n\r\nSediment discharge at these relatively unconfined sections was computed from formulas for comparison with measured sediment discharges at the contracted section. A form of the Du Boys formula gave computed tonnages of sediment that were unsatisfactory. Sediment discharges as computed from the Schoklitsch formula agreed well with measured sediment discharges that were low, but they were much too low at measured sediment discharges that were higher. The Straub formula gave computed discharges, presumably of bed material, that were several times larger than measured discharges of sediment coarser than 0.125 millimeter. All three of these formulas gave computed sediment discharges that increased with water discharges much less rapidly than the measured discharges of sediment coarser than 0.125 millimeter. \r\n\r\nThe Einstein procedure when applied to a reach that included 10 defined cross sections gave much better agreement between computed sediment discharge and measured sediment discharge than did anyone of the three other formulas that were used. This procedure does not compute the discharge of sediment that is too small to be found in the stream bed in appreciable quantities. Hence, total sediment discharges were obtained by adding computed discharges of sediment larger than 0.125 millimeter to measured discharges of sediment smaller than 0.125 millimeter. The size distributions of the computed sediment discharge compared poorly with the size distributions of sediment discharge at the contracted section. Ten sediment discharges computed from the Einstein procedure as applied to a single section averaged several times the measured sediment discharge for the contracted section and gave size distributions that were unsatisfactory.\r\n\r\nThe Einstein procedure was modified to compute total sediment discharge at an alluvial section from readily measurable field data. The modified procedure uses measurements of bed-material particle sizes, suspended-sediment concentrations and particle sizes from depth-integrated samples, streamflow, and water temperatures. Computations of total sediment discharge were made by using this modified procedure, some for the section at the gaging station and some for each of two other relatively unconfined sections. The size distributions of the computed and the measured sediment discharges agreed reasonably well. Major advantages of this modified procedure include applicability to a single section rather than to a reach of channel, use of measured velocity instead of water-surface slope, use of depth-integrated samples, and apparently fair accuracy for computing both total sediment discharge and approximate size distribution of the sediment. Because of these advantages this modified procedure is being further studied to increase its accuracy, to simplify the required computations, and to define its limitations. \r\n\r\nIn the development of the modified procedure, some relationships concerning theories of sediment transport were reviewed and checked against field data. Vertical distributions of suspended sediment at relatively unconfined sections did not agree well with theoretical dist","language":"ENGLISH","publisher":"U.S. Geological Survey ; for sale by U.S. G.P.O.,","doi":"10.3133/wsp1357","isbn":"pbk","usgsCitation":"Colby, B.R., and Hembree, C., 1955, Computations of total sediment discharge, Niobrara River near Cody, Nebraska: U.S. Geological Survey Water Supply Paper 1357, vii, 187 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1357.","productDescription":"vii, 187 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137363,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1357/report-thumb.jpg"},{"id":25989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25990,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25991,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25992,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25993,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25994,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25995,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1357/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25996,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6392","contributors":{"authors":[{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143282,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":143283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":807,"text":"wsp1222 - 1955 - Water levels and artesian pressures in observation wells in the United States in 1952, part 2. Southeastern states","interactions":[],"lastModifiedDate":"2024-01-24T19:35:33.499707","indexId":"wsp1222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1222","title":"Water levels and artesian pressures in observation wells in the United States in 1952, part 2. Southeastern states","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1222","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Water levels and artesian pressures in observation wells in the United States in 1952, part 2. Southeastern states: U.S. Geological Survey Water Supply Paper 1222, vi, 260 p., https://doi.org/10.3133/wsp1222.","productDescription":"vi, 260 p.","costCenters":[],"links":[{"id":424816,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24260.htm","text":"Virginia","linkFileType":{"id":5,"text":"html"}},{"id":424815,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24259.htm","text":"Tennessee","linkFileType":{"id":5,"text":"html"}},{"id":424814,"rank":9,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24258.htm","text":"South Carolina","linkFileType":{"id":5,"text":"html"}},{"id":424813,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24257.htm","text":"North Carolina","linkFileType":{"id":5,"text":"html"}},{"id":424812,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24256.htm","text":"Maryland","linkFileType":{"id":5,"text":"html"}},{"id":424811,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24255.htm","text":"Kentucky","linkFileType":{"id":5,"text":"html"}},{"id":424810,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24254.htm","text":"Georgia","linkFileType":{"id":5,"text":"html"}},{"id":424809,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24253.htm","text":"Florida","linkFileType":{"id":5,"text":"html"}},{"id":392395,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24252.htm","text":"Alabama","linkFileType":{"id":5,"text":"html"}},{"id":424817,"rank":12,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24261.htm","text":"West 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,{"id":2784,"text":"wsp1295 - 1955 - Chemical quality of surface waters in Devils Lake basin, North Dakota","interactions":[],"lastModifiedDate":"2018-03-16T13:46:22","indexId":"wsp1295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1295","title":"Chemical quality of surface waters in Devils Lake basin, North Dakota","docAbstract":"Devils Lake basin, a closed basin in northeastern North Dakota, covers about 3,900 square miles of land, the topography of which is morainal and of glacial origin. In this basin lies a chain of waterways, which begins with the Sweetwater group and extends successively through Mauvais Coulee, Devils Lake, East Bay Devils Lake, and East Devils Lake, to Stump Lake. In former years when lake levels were high, Mauvais Coulee drained the Sweetwater group and discharged considerable water into Devils Lake. Converging coulees also transported excess water to Stump Lake. For at least 70 years prior to 1941, Mauvais Coulee flowed only intermittently, and the levels of major lakes in this region gradually declined. Devils Lake, for example, covered an area of about 90,000 acres in 1867 but had shrunk to approximately 6,500 acres by 1941. Plans to restore the recreational appeal of Devils Lake propose the dilution and eventual displacement of the brackish lake water by fresh water that would be diverted from the Missouri River. Freshening of the lake water would permit restocking Devils Lake with fish. \r\n\r\nDevils and Stump Lake have irregular outlines and numerous windings and have been described as lying in the valley of a preglacial river, the main stem and tributaries of which are partly filled with drift. Prominent morainal hills along the south shore of Devils Lake contrast sharply with level farmland to the north. The mean annual temperature of Devils Lake basin ranges between 36 ? and 42 ? F. Summer temperatures above 100 ? F and winter temperatures below -30 ? Fare not uncommon. The annual precipitation for 77 years at the city of Devils Lake averaged 17.5 inches. Usually, from 75 to 80 percent of the precipitation in the basin falls during the growing season, April to September. \r\n\r\nFrom 1867 to 1941 the net fall of the water surface of Devils Lake was about 38 feet. By 1951 the surface had risen fully 14 feet from its lowest altitude, 1,400.9 feet. Since 1951, the level has fallen slowly. Hydrologic changes that may have caused Devils Lake to alter from a very large, moderately deep lake of fresh water to a small, shallow body of brackish water are discussed and evaluated on the basis of scanty information. During several years of average precipitation, temperature, and evaporation, Devils Lake and lakes upstream should receive nearly a quarter of an inch of runoff annually from the drainage area of about 3,000 square miles. Approximately 55 square miles of tributary area would be required to maintain each square mile of lake surface. However, runoff, expressed as percentage of the average, differs greatly from year to year. The amount of runoff retained in upstream lakes also Varies greatly. For these two reasons, annual inflow to Devils Lake is extremely variable. \r\n\r\nBecause many waterways in this basin have no surface outlets at normal stages, runoff collects in depressions, is concentrated by evaporation, and forms saline or alkaline lakes. The chemical and physical properties of the lake waters vary chiefly with changes in lake stage and volume of inflow. Scattered records from 1899 to 1923 and more comprehensive data from 1948 to 1952 show a range of salt concentration from 6,130 to 25,000 parts per million (ppm) in the water of Devils Lake. Although concentration has varied, the chemical composition of the dissolved solids has not changed appreciably. Lake waters are more concentrated in the lower part of the basin, downstream from Devils Lake. For periods of record the salt concentration ranged from 14,932 to 62,000 ppm in East Devils Lake and from 19,000 to 106,000 ppm in east Stump Lake. \r\n\r\nCurrent and past tonnages of dissolved solids in Devils Lake, East Bay Devils Lake, East Devils Lake, and east and west Stump Lakes were computed from concentrations and from altitude-capacity curves for each lake. Neither the average rate of diversion of water to restore Devils Lake to a higher level nor the quality of the divert","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1295","usgsCitation":"Swenson, H., and Colby, B.R., 1955, Chemical quality of surface waters in Devils Lake basin, North Dakota: U.S. Geological Survey Water Supply Paper 1295, Report: v, 81 p.; Plate: 17.5 x 17.1 inches, https://doi.org/10.3133/wsp1295.","productDescription":"Report: v, 81 p.; Plate: 17.5 x 17.1 inches","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":29259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1295/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138861,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1295/report-thumb.jpg"},{"id":29258,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1295/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e332f","contributors":{"authors":[{"text":"Swenson, Herbert","contributorId":54181,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","affiliations":[],"preferred":false,"id":145781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Colby, Bruce R.","contributorId":59775,"corporation":false,"usgs":true,"family":"Colby","given":"Bruce","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":660,"text":"wsp1276 - 1955 - Surface water supply of the United States, 1953, Part III-B, Ohio River basin, Cumberland and Tennessee River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp1276","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1276","title":"Surface water supply of the United States, 1953, Part III-B, Ohio River basin, Cumberland and Tennessee River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1276","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part III-B, Ohio River basin, Cumberland and Tennessee River basins: U.S. Geological Survey Water Supply Paper 1276, vii, 278 p. ;23 cm., https://doi.org/10.3133/wsp1276.","productDescription":"vii, 278 p. ;23 cm.","costCenters":[],"links":[{"id":136892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1276/report-thumb.jpg"},{"id":25223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1276/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696361","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":527632,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":663,"text":"wsp1283 - 1955 - Surface water supply of the United States, 1953, Part IX, Colorado River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp1283","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1283","title":"Surface water supply of the United States, 1953, Part IX, Colorado River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1283","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part IX, Colorado River basin: U.S. Geological Survey Water Supply Paper 1283, x, 472 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1283.","productDescription":"x, 472 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136895,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1283/report-thumb.jpg"},{"id":25226,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1283/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69639b","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":527635,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":657,"text":"wsp1284 - 1955 - Surface water supply of the United States, 1953, Part X, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1284","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1284","title":"Surface water supply of the United States, 1953, Part X, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1284","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part X, The Great Basin: U.S. Geological Survey Water Supply Paper 1284, viii, 227 p. :ill., map ;24 cm., https://doi.org/10.3133/wsp1284.","productDescription":"viii, 227 p. :ill., map ;24 cm.","costCenters":[],"links":[{"id":136073,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1284/report-thumb.jpg"},{"id":25220,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1284/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6962ea","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":527629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2159,"text":"wsp1187 - 1955 - Quality of surface waters of the United States, 1950 : Parts 5 and 6, surface waters of Hudson Bay, upper Mississippi, Missouri River Basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1187","title":"Quality of surface waters of the United States, 1950 : Parts 5 and 6, surface waters of Hudson Bay, upper Mississippi, Missouri River Basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1187","usgsCitation":"Love, S.K., 1955, Quality of surface waters of the United States, 1950 : Parts 5 and 6, surface waters of Hudson Bay, upper Mississippi, Missouri River Basins: U.S. Geological Survey Water Supply Paper 1187, ix, 478 p. :tables ;25 cm., https://doi.org/10.3133/wsp1187.","productDescription":"ix, 478 p. :tables ;25 cm.","costCenters":[],"links":[{"id":137851,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1187/report-thumb.jpg"},{"id":27770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6548ce","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144754,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2433,"text":"wsp1255 - 1955 - Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area","interactions":[],"lastModifiedDate":"2024-02-22T23:08:50.440875","indexId":"wsp1255","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1255","title":"Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area","docAbstract":"<p>The circulation of water, in any form, from the surface of the earth to the atmosphere and back again is called the hydrologic cycle. A comprehensive study of the water resources of any area must, therefore, include data on the climate of the area.</p><p>The humid subtropical climate of southeastern Florida is characterized by relatively high temperatures, alternating semi-annual wet and dry seasons, and usually light but persistent winds.</p><p>The recurrence of drought in an area having relatively large rainfall such as southeastern Florida indicates that the agencies that remove water are especially effective. Two of the most important of the agencies associated with climate are evaporation and transpiration, or \"evapotranspiration\". Evaporation losses from permanent water areas are believed to average between about 40 and 45 inches per year. Over land areas indirect methods must be used to determine losses by evapotranspiration; necessarily, these values are not precise.</p><p>Because of their importance in the occurrence and movement of both surface and ground waters, detailed studies were made of the geology and geomorphology of southern Florida.</p><p>As a result of widespread crustal movements, southern Florida emerged from the sea in late Pliocene time and probably was slightly tilted to the west. At the beginning of the Pleistocene the continent emerged still farther as a result of the lowering of sea level attending the first widespread glaciation. During this epoch, southern Florida may have stood several hundred feet above sea level.</p><p>During the interglacial ages the sea repeatedly flooded southern Florida. The marine members of the Fort Thompson formation in the Lake Okeechobee-Everglades depression and the Caloosahatchee River Valley apparently are the deposits of these interglacial invasions by the sea. The fresh-water marls, sands, and organic deposits of the Fort Thompson formation appear to have accumulated during glacial ages when sea level was low and the area was a land surface partly occupied by fresh-water lakes and marshes. Elsewhere in southern Florida the deposits are mainly marine limestones and sandy terrace deposits.</p><p>The Pliocene surface upon which these Pleistocene sediments were deposited was highest to the north and west of the present Everglades and Kissimmee River basin, and it sloped gently to the south, southeast, and east. On this slightly sloping floor, alternately submerged and emerged, the later materials were built; these materials modified by wind, rain, and surface and ground waters, have largely determined the present topographic and ecologic character of southern Florida.</p><p>The most important aquifer in southern Florida, and the one in which most of the wells are developed, is the Biscayne aquifer. It is composed of parts of the Tamiami formation (Miocene), Caloosahatchee marl (Pliocene), Fort Thompson formation, Anastasia formation, Key Largo limestone, Miami oolite, and Pamlico sand (Pleistocene). In some parts of southern Florida, the Pamlico sand and the Anastasia formation are not a part of the Biscayne aquifer; however, they are utilized in the development of small water supplies. Most of the Caloosahatchee marl and the Fort Thompson formation in the Lake Okeechobee area is of very low permeability. In the northern Everglades their less permeable parts contain highly mineralized waters, which appear to have been trapped since the invasions by the Pleistocene seas. These waters have been modified by dilution with fresh ground water and by chemical reactions with surrounding materials.</p><p>Sea-level fluctuations, starting at the close of the Pliocene with the highest levels and progressing toward the Recent with successively lower levels, have built a series of nearly flat marine terrances abutting against one another much like a series of broad stearsteps. Erosion and solution have defaced and, in places, have obliterated the original surficial forms of these old sea bottoms, shores, and shoreline features, but their remnants today are widespread and, in some places, are easily recognizable.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1255","collaboration":"Prepared in cooperation with the Florida Geological Survey, Dade County, cities of Miami and Miami Beach, and other agencies","usgsCitation":"Parker, G., Ferguson, G., and Love, S.K., 1955, Water resources of southeastern Florida, with special reference to the geology and ground water of the Miami area: U.S. Geological Survey Water Supply Paper 1255, Report: xxv, 965 p.; 24 Plates: 19.50 x 30.25 inches or smaller, https://doi.org/10.3133/wsp1255.","productDescription":"Report: xxv, 965 p.; 24 Plates: 19.50 x 30.25 inches or smaller","costCenters":[],"links":[{"id":425904,"rank":28,"type":{"id":36,"text":"NGMDB Index 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K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":145189,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2782,"text":"wsp1263 - 1955 - Geology and ground-water resources of the Missouri River valley in northeastern Montana, with a section on the quality of the ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1263","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1263","title":"Geology and ground-water resources of the Missouri River valley in northeastern Montana, with a section on the quality of the ground water","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1263","usgsCitation":"Swenson, F.A., and Durum, W.H., 1955, Geology and ground-water resources of the Missouri River valley in northeastern Montana, with a section on the quality of the ground water: U.S. Geological Survey Water Supply Paper 1263, iv, 128 p. :illus., maps (2 fold., col. in pocket) diagrs., tables. ;23 cm., https://doi.org/10.3133/wsp1263.","productDescription":"iv, 128 p. :illus., maps (2 fold., col. in pocket) diagrs., tables. ;23 cm.","costCenters":[],"links":[{"id":138853,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1263/report-thumb.jpg"},{"id":29251,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1263/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29252,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1263/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29253,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1263/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6854ef","contributors":{"authors":[{"text":"Swenson, Frank Albert","contributorId":71958,"corporation":false,"usgs":true,"family":"Swenson","given":"Frank","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":145777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2309,"text":"wsp1296 - 1955 - Geology and ground-water resources of the Baton Rouge area, Louisiana","interactions":[{"subject":{"id":23882,"text":"ofr53192 - 1953 - Summary report on the geology and ground-water resources of the Baton Rouge Area, Louisiana","indexId":"ofr53192","publicationYear":"1953","noYear":false,"title":"Summary report on the geology and ground-water resources of the Baton Rouge Area, Louisiana"},"predicate":"SUPERSEDED_BY","object":{"id":2309,"text":"wsp1296 - 1955 - Geology and ground-water resources of the Baton Rouge area, Louisiana","indexId":"wsp1296","publicationYear":"1955","noYear":false,"title":"Geology and ground-water resources of the Baton Rouge area, Louisiana"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1296","title":"Geology and ground-water resources of the Baton Rouge area, Louisiana","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1296","usgsCitation":"Meyer, R.R., and Turcan, A., 1955, Geology and ground-water resources of the Baton Rouge area, Louisiana: U.S. Geological Survey Water Supply Paper 1296, v, 138 p. :plates, map, diagrs., tables. ;23 cm., https://doi.org/10.3133/wsp1296.","productDescription":"v, 138 p. :plates, map, diagrs., tables. ;23 cm.","costCenters":[],"links":[{"id":137718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1296/report-thumb.jpg"},{"id":28134,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1296/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28135,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1296/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28136,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1296/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28137,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1296/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6857f1","contributors":{"authors":[{"text":"Meyer, Rex Rupert","contributorId":39015,"corporation":false,"usgs":true,"family":"Meyer","given":"Rex","email":"","middleInitial":"Rupert","affiliations":[],"preferred":false,"id":144988,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Turcan, A. N.","contributorId":34114,"corporation":false,"usgs":true,"family":"Turcan","given":"A. N.","affiliations":[],"preferred":false,"id":144987,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2845,"text":"wsp1298 - 1955 - Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water","interactions":[],"lastModifiedDate":"2016-04-05T09:11:18","indexId":"wsp1298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1298","title":"Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water","docAbstract":"<p>The area described in this report is the flood plain of the Grand River and the bordering benchlands in Perkins and Corson Counties, S. Dak., from a point about 6 miles west of the town of Shadehill to the confluence of the Grand and Missouri Rivers near Mobridge.</p>\n<p>The exposed bedrock formations include the Pierre shale, the Fox Hills sandstone, and the Hell Creek formation of Late Cretaceous age, and-the Ludlow member of the Fort Union formation of Tertiary (Paleocene) age. Some stringers of the Cannonball formation probably interfinger with beds of the Ludlow member but none of the former was identified during the field investigations. The Pierre shale is exposed from the mouth of the Grand River to approximately the center of the area. Although a few wells in the area obtain water from this formation, it is not generally considered to be a source of supply. The Fox Hills sandstone, the Hell Creek formation, and the Ludlow member of the Fort Union formation are exposed successively upstream and, where saturated, yield small to moderate quantities of water to wells.</p>\n<p>Unconsolidated deposits of silt, sand, and gravel occur in several physiographic positions; they underlie the high benchland on both sides of the river, the poorly defined terraces along the river, and the flood plain throughout its entire length. Possibly all these unconsolidated deposits are water bearing; however, where the deposits on the benchland and in the terraces are dissected by streams, they probably contain little or no water.</p>\n<p>The average depth to ground water along the lower Grand River valley is about 17 feet. Probably, the flow of ground water in the bottom lands is nearly parallel to and slightly toward the surface stream. The measurements of the water level in observation wells for the period 1946-48 indicate that the fluctuations of the water table are small.</p>\n<p>The results of analyses of 13 samples of ground water from the alluvium and the Hell Creek formation show that the suitability of the ground water for use varies because of the considerable range in mineralization and composition. Dissolved solids ranged from 343 to 4,250 parts per million (ppm), hardness from 11 to 1,130 ppm, and percentage of sodium from 25 to 98. Concentrations of some of the individual constituents exceed standards of the United States Public Health Service. The water is moderately hard and contains undesirable amounts of iron and moderate to large amounts of dissolved solids. In general, the water quality ranges from excellent to unsuitable for irrigation use. The result of the mixing of the ground water with recharge water from Shadehill Reservoir cannot be predicted on the basis of available data.</p>\n<p>The geologic and hydrologic data in this report were obtained from earlier reports and from field observations during the period 1946-48. The report includes a geologic map and tabulated well records.</p>","language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, DC","doi":"10.3133/wsp1298","usgsCitation":"Tychsen, P.C., Vorhis, R., and Jochens, E.R., 1955, Reconnaissance of geology and ground water in the lower Grand River valley, South Dakota, with a section on Chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1298, Report: iv, 33 p.; 2 Plates: 30.00 x 18.15 inches and 27.50 x 9.69 inches, https://doi.org/10.3133/wsp1298.","productDescription":"Report: iv, 33 p.; 2 Plates: 30.00 x 18.15 inches and 27.50 x 9.69 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":138696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1298/report-thumb.jpg"},{"id":29415,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1298/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29416,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1298/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29417,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1298/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Grand River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -102.23876953125,\n              45.336701909968106\n            ],\n            [\n              -102.23876953125,\n              45.73685954736049\n            ],\n            [\n              -100.30517578125,\n              45.73685954736049\n            ],\n            [\n              -100.30517578125,\n              45.336701909968106\n            ],\n            [\n              -102.23876953125,\n              45.336701909968106\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c389","contributors":{"authors":[{"text":"Tychsen, Paul C.","contributorId":82683,"corporation":false,"usgs":true,"family":"Tychsen","given":"Paul","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145896,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vorhis, R.C.","contributorId":32512,"corporation":false,"usgs":true,"family":"Vorhis","given":"R.C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145894,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jochens, Eugene R.","contributorId":55804,"corporation":false,"usgs":true,"family":"Jochens","given":"Eugene","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145895,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":169,"text":"wsp1197 - 1955 - Quality of surface waters of the United States, 1951. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1197","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1197","title":"Quality of surface waters of the United States, 1951. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1197","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Quality of surface waters of the United States, 1951. Parts 1-4, North Atlantic slope basins to St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1197, xi, 373 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1197.","productDescription":"xi, 373 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137344,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1197/report-thumb.jpg"},{"id":24780,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1197/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6548bd","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":527209,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2935,"text":"wsp1279 - 1955 - Surface water supply of the United States, 1953, Part VI-A, Missouri River basin, Missouri River basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1279","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1279","title":"Surface water supply of the United States, 1953, Part VI-A, Missouri River basin, Missouri River basin above Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Government Printing Office,","doi":"10.3133/wsp1279","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part VI-A, Missouri River basin, Missouri River basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1279, x, 458 p. : tables ;25 cm., https://doi.org/10.3133/wsp1279.","productDescription":"x, 458 p. : tables ;25 cm.","costCenters":[],"links":[{"id":138672,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1279/report-thumb.jpg"},{"id":29644,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1279/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696333","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":528038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2473,"text":"wsp1240 - 1955 - Surface water supply of the United States, 1952, Part VI-B, Missouri River basin, Missouri River basin below Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1240","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1240","title":"Surface water supply of the United States, 1952, Part VI-B, Missouri River basin, Missouri River basin below Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1240","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1952, Part VI-B, Missouri River basin, Missouri River basin below Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1240, x, 455 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1240.","productDescription":"x, 455 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":138736,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1240/report-thumb.jpg"},{"id":28549,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1240/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696464","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":528025,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":662,"text":"wsp1278 - 1955 - Surface water supply of the United States, 1953, Part V, Hudson Bay and upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp1278","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1278","title":"Surface water supply of the United States, 1953, Part V, Hudson Bay and upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1278","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part V, Hudson Bay and upper Mississippi River basins: U.S. Geological Survey Water Supply Paper 1278, xii, 539 p. ;23 cm., https://doi.org/10.3133/wsp1278.","productDescription":"xii, 539 p. ;23 cm.","costCenters":[],"links":[{"id":136894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1278/report-thumb.jpg"},{"id":25225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1278/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69631d","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":527634,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":810,"text":"wsp1226 - 1955 - Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii","interactions":[{"subject":{"id":51582,"text":"ofr53266 - 1953 - Water levels in observation wells in Santa Barbara County, California, in 1952","indexId":"ofr53266","publicationYear":"1953","noYear":false,"title":"Water levels in observation wells in Santa Barbara County, California, in 1952"},"predicate":"SUPERSEDED_BY","object":{"id":810,"text":"wsp1226 - 1955 - Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of Hawaii","indexId":"wsp1226","publicationYear":"1955","noYear":false,"title":"Water levels and artesian pressures in observation wells in the United States in 1952: Part 6, southwestern states and territory of 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,{"id":2156,"text":"wsp1362 - 1955 - Quality of surface waters for irrigation, western United States, 1952","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1362","title":"Quality of surface waters for irrigation, western United States, 1952","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1362","usgsCitation":"Love, S.K., 1955, Quality of surface waters for irrigation, western United States, 1952: U.S. Geological Survey Water Supply Paper 1362, viii, 179 p. :ill., map ;25 cm., https://doi.org/10.3133/wsp1362.","productDescription":"viii, 179 p. :ill., map ;25 cm.","costCenters":[],"links":[{"id":27766,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1362/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137848,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1362/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6868ae","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144751,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":661,"text":"wsp1277 - 1955 - Surface water supply of the United States, 1953, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp1277","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1277","title":"Surface water supply of the United States, 1953, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1277","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1277, ix, 361 p. ;23 cm., https://doi.org/10.3133/wsp1277.","productDescription":"ix, 361 p. ;23 cm.","costCenters":[],"links":[{"id":136893,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1277/report-thumb.jpg"},{"id":25224,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1277/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696366","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":527633,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2923,"text":"wsp1320A - 1955 - Floods of June 1953 in northwestern Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1320A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1320","chapter":"A","title":"Floods of June 1953 in northwestern Iowa","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1320A","usgsCitation":"Wells, J.V., 1955, Floods of June 1953 in northwestern Iowa: U.S. Geological Survey Water Supply Paper 1320, vi, 68 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp1320A.","productDescription":"vi, 68 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":139010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1320a/report-thumb.jpg"},{"id":29630,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1320a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29631,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1320a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29632,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1320a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfaa4","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146007,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1069,"text":"wsp1258 - 1955 - Ground-water resources of the Middle Loup division of the lower Platte River basin, Nebraska, with a section on Chemical quality of the ground water","interactions":[],"lastModifiedDate":"2013-01-08T12:59:02","indexId":"wsp1258","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1258","title":"Ground-water resources of the Middle Loup division of the lower Platte River basin, Nebraska, with a section on Chemical quality of the ground water","docAbstract":"The Middle Loup division of the lower Platte River basin is an area of 650 square miles which includes the Middle Loup River valley from the confluence of the Middle and North Loup Rivers in Howard County, Nebr., to the site of the diversion dam that the U. S. Bureau of Reclamation proposes to construct in Blaine County near Milburn, Nebr. It also includes land in Howard and Sherman Counties designated by the Bureau of Reclamation as the Farwell unit. Irrigable land in this division is present on both sides of the Middle Loup River and along its tributaries. Most of the Middle Loup River valley is already irrigated by the Middle Loup Public Power and Irrigation District, which is strictly an irrigation enterprise. The uplands are not irrigated. \n\nLoess, dune sand, gravel, silt, and clay of Pleistocene or Recent age are exposed in the report area. These unconsolidated sediments rest on bedrock consisting of alternating layers of shale, mudstone, sandstone, and limestone, which are essentially fiat lying or slightly warped. The Ogallala formation, of Tertiary (Pliocene) age, immediately underlies the Pleistocene sediments and rests on the Pierre shale of Cretaceous age. Belts of alluvium occupy the Middle Loup River valley and the valleys of the principal streams in the area. The soils, dune sand, and terrace deposits are the most recent deposits. \n\nThe Ogallala formation is water bearing and is the source of supply for some domestic and livestock wells. The saturated part of the sand and gravel formations of Pleistocene age, which yields water freely to wells, is the most important aquifer in the Middle Loup division. The water generally is under water-table conditions. The yields of properly constructed wells range from a few gallons per minute (gpm) to as much as 1,800 gpm. Some wells tap water in both the sand and gravel of Pleistocene age and in the underlying Ogallala formation. No wells are known to penetrate into formations older than the Ogallala. \n\nFluctuations of the water table indicate changes in the amount of ground water stored in the water-bearing formations. The principal factors controlling the rise of the water table are the amount of precipitation within the area, the quantity of water coming into the area as underflow from the west and northwest, seepage from the Middle Loup River at times when the water surface in the river is higher than the adjoining water table, and the infiltration of irrigation water not utilized by vegetation or lost by runoff or evaporation. The principal factors controlling the decline of the water table are the discharge as effluent seepage into the Middle Loup River and its tributaries, the amount of water pumped from wells, evapotranspiration losses, and the amount of water leaving the area as underflow. \n\nPeriodic water-level measurements were made in a total of 241 observation wells during the period 1948-50. Hydrographs of three observation wells having a longer period of record (1934-50) indicate that the water table rose slightly from 1934 until 1950 and that it remained nearly constant during the 1950 water year. \n\nThe configuration of the water table in the Middle Loup division shows that, except north and northwest of Sargent, the Middle Loup River is an effluent, or gaining, stream throughout its entire length in this area. Thus any rise or fall in the ground-water level will increase or decrease the discharge of the river. The river recharges the ground- water reservoir only during periods when it is at flood stage. The depth to the water table from the land surface is governed largely by irregularities in topography. The depth to water is less than 10 feet near the river and increases to as much as 60 feet near the valley margins and the bordering intermediate slopes. In the Far- well unit the depth to water is more than 100 feet and in some parts more than 150 feet. Ground water pumped from wells is the source of supply for the principal municipalities in th","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1258","usgsCitation":"Brown, D.W., and Rainwater, F.H., 1955, Ground-water resources of the Middle Loup division of the lower Platte River basin, Nebraska, with a section on Chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1258, iv, 85 p. :maps (2 fold. in pocket) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1258.","productDescription":"iv, 85 p. :maps (2 fold. in pocket) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138020,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1258/report-thumb.jpg"},{"id":25749,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1258/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265374,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1258/plate-2.pdf"},{"id":265373,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1258/plate-1.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a808","contributors":{"authors":[{"text":"Brown, Delbert Wayne","contributorId":95753,"corporation":false,"usgs":true,"family":"Brown","given":"Delbert","email":"","middleInitial":"Wayne","affiliations":[],"preferred":false,"id":143129,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rainwater, Frank Hays","contributorId":38967,"corporation":false,"usgs":true,"family":"Rainwater","given":"Frank","email":"","middleInitial":"Hays","affiliations":[],"preferred":false,"id":143128,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2931,"text":"wsp1234 - 1955 - Surface water supply of the United States, 1952 Part II-B, South Atlantic slope and eastern Gulf of Mexico basins, Ogeechee River to Pearl River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1234","title":"Surface water supply of the United States, 1952 Part II-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/wsp1234","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1952 Part II-B, South Atlantic slope and eastern Gulf of Mexico basins, Ogeechee River to Pearl River: U.S. Geological Survey Water Supply Paper 1234, ix, 364 p. : ill., tables ;25 cm., https://doi.org/10.3133/wsp1234.","productDescription":"ix, 364 p. : ill., tables ;25 cm.","costCenters":[],"links":[{"id":138927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1234/report-thumb.jpg"},{"id":29640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1234/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd399","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":528034,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":659,"text":"wsp1286 - 1955 - Surface water supply of the United States, 1953, Part XII, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp1286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1286","title":"Surface water supply of the United States, 1953, Part XII, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1286","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1955, Surface water supply of the United States, 1953, Part XII, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Water Supply Paper 1286, x, 407 p. ;23 cm., https://doi.org/10.3133/wsp1286.","productDescription":"x, 407 p. ;23 cm.","costCenters":[],"links":[{"id":136891,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1286/report-thumb.jpg"},{"id":25222,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1286/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696328","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":527631,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":45,"text":"wsp1260B - 1955 - Floods of April 1952 in the Missouri River basin","interactions":[],"lastModifiedDate":"2019-12-30T08:58:02","indexId":"wsp1260B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1260","chapter":"B","title":"Floods of April 1952 in the Missouri River basin","docAbstract":"<p>The floods of April 1952 in the Milk River basin, along the Missouri River from the mouth of the Little Missouri River to the mouth of the Kansas River, and for scattered tributaries of the Missouri River in North and South Dakota were the greatest ever observed. The damage amounted to an estimated $179 million. The outstanding featur6 of the floods was the extraordinary peak discharge generated in the Missouri River at and downstream from Bismarck, N. Dak., on April 6 when a large ice jam upstream from the city was suddenly released. Inflow from flooding tributaries maintained the peak discharge at approximately the same magnitude in the transit of the flood across South Dakota; downstream from Yankton, S. Dak., attenuation of the peak discharge was continuous because of natural storage in the wide flood plains. The outstanding characteristic of floods in the Milk River basin was their duration--the flood crested at Havre, Mont., on April 3 and at Nashua, Mont.. on April 18. The floods were caused by an abnormally heavy accumulation of snow that was converted into runoff in a few days of very warm weather at the end of March. The heaviest water content of the snow pack at breakup was in a narrow arc extending through Aberdeen, S. Dak., Pierre, S. Dak.. and northwestward toward the southwest corner of North Dakota. The water content in part of this concentrated cover exceeded 6 inches. The winter of 1951-52, which followed a wet cold fall that made the ground impervious, was one of the most severe ever experienced in South Dakota and northern Montana. Depths of snow and low temperatures combined to produce, at the end of March, one of the heaviest snow covers in the history of the Great Plains. The Missouri River ice was intact upstream from Chamberlain, S. Dak., at the end of March, and the breakup of the ice with inflow of local runoff was one of the spectacular features of the flood. Runoff from the Yellowstone River combining with the flood pouring from the Little Missouri River caused the Missouri River to crest at an all-time high at Elbowoods, N. Dak., on April 4. As this crest moved downstream to Bismarck, its intensity was increased by the alternate storing and release of ice jams plus the inflow from the Knife River. The crest discharge of 500,000 cfs came at Bismarck at 6 p. m. on April 6. following a very sharp rise from 80,000 cfs at 11 a.m. Overflow occurred along the Missouri River from Elbowoods to the mouth with high damage to cities. farmland, and installations located in the flood plain. Cleanup and repair operations following the flood continued for many weeks. Few of the flooded farms produced a crop during 1952. This report presents detailed records of stage and discharge for the flood period on the Missouri River and tributaries from Fort Peck. Mont., to the mouth. Information on damages and river stages collected by other agencies is also presented.</p>","language":"English","publisher":"U.S. Government Print Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1260B","usgsCitation":"Wells, J.V., 1955, Floods of April 1952 in the Missouri River basin: U.S. Geological Survey Water Supply Paper 1260, Report: x, 302 p.; 3 Plates: 16.50 x 19.00 inches or smaller, https://doi.org/10.3133/wsp1260B.","productDescription":"Report: x, 302 p.; 3 Plates: 16.50 x 19.00 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":24669,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24670,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137523,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1260b/report-thumb.jpg"},{"id":24671,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1260b/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24672,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1260b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Missouri River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.345703125,\n              49.38237278700955\n            ],\n            [\n              -113.90625,\n              47.57652571374621\n            ],\n            [\n              -110.56640625,\n              42.35854391749705\n            ],\n            [\n              -104.32617187499999,\n              37.78808138412046\n            ],\n            [\n              -96.94335937499999,\n              36.1733569352216\n            ],\n            [\n              -89.033203125,\n              37.50972584293751\n            ],\n            [\n              -88.9453125,\n              38.13455657705411\n            ],\n            [\n              -92.63671875,\n              43.197167282501276\n            ],\n            [\n              -93.955078125,\n              45.706179285330855\n            ],\n            [\n              -99.228515625,\n              49.26780455063753\n            ],\n            [\n              -102.919921875,\n              49.32512199104001\n            ],\n            [\n              -114.345703125,\n              49.38237278700955\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e478ee4b07f02db4899d8","contributors":{"authors":[{"text":"Wells, J. 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,{"id":973,"text":"wsp1257 - 1955 - Geology and ground-water resources of the Paintsville area, Kentucky","interactions":[{"subject":{"id":50953,"text":"ofr5193 - 1951 - Structure map with contours on the Van Lear coal, Paintsville quadrangle, Kentucky","indexId":"ofr5193","publicationYear":"1951","noYear":false,"title":"Structure map with contours on the Van Lear coal, Paintsville quadrangle, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":973,"text":"wsp1257 - 1955 - Geology and ground-water resources of the Paintsville area, Kentucky","indexId":"wsp1257","publicationYear":"1955","noYear":false,"title":"Geology and ground-water resources of the Paintsville area, Kentucky"},"id":1},{"subject":{"id":50954,"text":"ofr5194 - 1951 - Areal geologic map of the Paintsville quadrangle, Kentucky","indexId":"ofr5194","publicationYear":"1951","noYear":false,"title":"Areal geologic map of the Paintsville quadrangle, Kentucky"},"predicate":"SUPERSEDED_BY","object":{"id":973,"text":"wsp1257 - 1955 - Geology and ground-water resources of the Paintsville area, Kentucky","indexId":"wsp1257","publicationYear":"1955","noYear":false,"title":"Geology and ground-water resources of the Paintsville area, Kentucky"},"id":2}],"lastModifiedDate":"2022-03-22T18:08:44.428443","indexId":"wsp1257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1955","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":"1257","title":"Geology and ground-water resources of the Paintsville area, Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1257","usgsCitation":"Baker, J.A., 1955, Geology and ground-water resources of the Paintsville area, Kentucky: U.S. Geological Survey Water Supply Paper 1257, Report: iv, 123 p.;  3 Plates: 20.00 × 20.00 inches or smaller, https://doi.org/10.3133/wsp1257.","productDescription":"Report: iv, 123 p.;  3 Plates: 20.00 × 20.00 inches or smaller","costCenters":[],"links":[{"id":397407,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24291.htm"},{"id":25526,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1257/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25525,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1257/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25524,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1257/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137057,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1257/report-thumb.jpg"}],"scale":"31700","country":"United States","state":"Kentucky","otherGeospatial":"Paintsville area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82.875,\n              37.75\n            ],\n            [\n              -82.75,\n              37.75\n            ],\n            [\n              -82.75,\n              37.875\n            ],\n            [\n              -82.875,\n              37.875\n            ],\n            [\n              -82.875,\n              37.75\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68550f","contributors":{"authors":[{"text":"Baker, John Augustus","contributorId":48159,"corporation":false,"usgs":true,"family":"Baker","given":"John","email":"","middleInitial":"Augustus","affiliations":[],"preferred":false,"id":142948,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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