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Off.,","doi":"10.3133/wsp1384","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1957, Surface water supply of the United States, 1955, Part II-B, South Atlantic slope and eastern Gulf of Mexico basins, Ogeechee River to Pearl River: U.S. Geological Survey Water Supply Paper 1384, x, 388 p. :ill. ;25 cm., https://doi.org/10.3133/wsp1384.","productDescription":"x, 388 p. :ill. ;25 cm.","costCenters":[],"links":[{"id":139123,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1384/report-thumb.jpg"},{"id":29651,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1384/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcce0","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":528045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2646,"text":"wsp1407 - 1957 - Water levels and artesian pressures in observation wells in the United States in 1955, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2019-06-13T08:32:32","indexId":"wsp1407","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1407","title":"Water levels and artesian pressures in observation wells in the United States in 1955, Part 4, South-Central States","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wsp1407","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1957, Water levels and artesian pressures in observation wells in the United States in 1955, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 1407, vi, 216 p., https://doi.org/10.3133/wsp1407.","productDescription":"vi, 216 p.","costCenters":[],"links":[{"id":28965,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1407/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138180,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1407/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa159","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":528029,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2941,"text":"wsp1383 - 1957 - Surface water supply of the United States, 1955, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1383","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1383","title":"Surface water supply of the United States, 1955, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River","language":"ENGLISH","publisher":"U.S. Government Printing Office,","doi":"10.3133/wsp1383","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1957, Surface water supply of the United States, 1955, Part II-A, South Atlantic slope and eastern Gulf of Mexico basins, James River to Savannah River: U.S. Geological Survey Water Supply Paper 1383, viii, 314 p. : tables ;25 cm., https://doi.org/10.3133/wsp1383.","productDescription":"viii, 314 p. : tables ;25 cm.","costCenters":[],"links":[{"id":138684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1383/report-thumb.jpg"},{"id":29650,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1383/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69605e","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":528044,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2562,"text":"wsp1377 - 1957 - Geology and ground-water resources of Goshen County Wyoming with a section on chemical quality of the ground water","interactions":[{"subject":{"id":51788,"text":"ofr54322 - 1954 - Geology and groundwater resources of the North Platte Irrigation Project area in Goshen County, Wyoming","indexId":"ofr54322","publicationYear":"1954","noYear":false,"title":"Geology and groundwater resources of the North Platte Irrigation Project area in Goshen County, Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":2562,"text":"wsp1377 - 1957 - Geology and ground-water resources of Goshen County Wyoming with a section on chemical quality of the ground water","indexId":"wsp1377","publicationYear":"1957","noYear":false,"title":"Geology and ground-water resources of Goshen County Wyoming with a section on chemical quality of the ground water"},"id":1}],"lastModifiedDate":"2022-02-17T20:03:36.844362","indexId":"wsp1377","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"1377","title":"Geology and ground-water resources of Goshen County Wyoming with a section on chemical quality of the ground water","docAbstract":"

Goshen County, which has an area of 2,186 square miles, lies in southeastern Wyoming. The purpose of this study was to evaluate the ground-water resources of the county by determining the character, thickness, and extent of the waterbearing materials; the source, occurrence, movement, quantity, and quality of the ground water; and the possibility of developing additional ground water. The rocks exposed in the area are sedimentary and range in age from Precambrian to Recent. A map that shows the areas of outcrop and a generalized section that summarizes the age, thickness, physical character, and water supply of these formations are included in the report. Owing to the great depths at which they lie beneath most of the county, the formations older than the Lance formation of Late Cretaceous age are not discussed in detail. The Lance formation, of Late Cretaceous age, which consists mainly of beds of fine-grained sandstone and shale, has a maximum thickness of about 1,400 feet. It yields water, which usually is under artesian pressure, to a large number of domestic and stock wells in the south-central part of the county. Tertiary rocks in the area include the Chadron and Brule formations of Oligocene age, the Arikaree formation of Miocene age, and channel deposits of Pliocene age. The Chadron formation is made up of two distinct units: a lower unit of highly variegated fluviatile deposits that has been found only in the report area; and an upper unit that is typical of the formation as it occurs in adjacent areas. The lower unit, which ranges in thickness from a knife edge to about 95 feet, is not known to yield water to wells, but its coarse-grained channel deposits probably would yield small quantities of water to wells. The upper unit, which ranges in thickness from a knife edge to about 150 feet, yields sufficient quantities of water for domestic and stock uses from channel deposits of sandstone under artesian pressure. The Brule formation, which is mainly a siltstone, ranges in thickness from a knife edge to about 450 feet and yields water to domestic and stock wells from fractures and from lenses of sandstone. The Arikaree formation ranges in thickness from a knife edge to about 1,000 feet, and yields water to several domestic and stock wells in the northwestern part of the area. The Pliocene channel deposits, which probably do not exceed 25 feet in thickness, are not a source of water for wells in Goshen County. The upland deposits, which are mainly of Pleistocene age, generally are dry and do not serve as aquifers; however, test drilling revealed several deep, buried channels occupied by deposits which probably would yield moderate quantities of water to wells if a sufficient saturated thickness were penetrate The deposits of the third terrace, which are of Pleistocene age, range in thickness from a knife edge to about 210 feet and yield water to a large number of irrigation wells in the area. The flood-plain deposits, which are of Pleistocene and Recent age, range in thickness from a knife edge to about 200 feet. Those in the valley of the North Platte River yield abundant water to many large supply wells. The flood-plain deposits along the valley of Rawhide Creek consist mainly of fine-grained materials and yield large supplies of water to well only in the lower stretches of the creek valley near its confluence with the valley of the North Platte River. The deposits along the valleys of Horse and Bear Creeks generally are relatively thin and fine grained. In the vicinity of Ls grange, however, the deposits, which are about 45 feet thick, yield moderate, supplies of water to several irrigation wells. Other Recent deposits in the area--dune sand, loesslike deposits, and slope wash--generally are fine grained and relatively thin and, hence, are not important sources of ground water. The unconsolidated sand and gravel of the flood-plain and terrace deposits are the principal aquifers in the area.

","language":"English","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1377","usgsCitation":"Rapp, J.R., Visher, F.N., Littleton, R., and Durum, W.H., 1957, Geology and ground-water resources of Goshen County Wyoming with a section on chemical quality of the ground water: U.S. Geological Survey Water Supply Paper 1377, Report: vi, 145 p.; 4 Plates: 30.00 × 51.00 inches or smaller, https://doi.org/10.3133/wsp1377.","productDescription":"Report: vi, 145 p.; 4 Plates: 30.00 × 51.00 inches or smaller","costCenters":[],"links":[{"id":28825,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1377/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":109940,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24359.htm","linkFileType":{"id":5,"text":"html"},"description":"24359"},{"id":28824,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1377/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28823,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1377/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28822,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1377/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28821,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1377/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138658,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1377/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Goshen County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-104.0525,42.6128],[-104.0525,42.0879],[-104.0525,42.0024],[-104.0525,41.998],[-104.0522,41.7004],[-104.0522,41.6975],[-104.0521,41.5654],[-104.6491,41.5656],[-104.6506,41.651],[-104.6513,41.8418],[-104.6544,42.2159],[-104.6546,42.5228],[-104.6516,42.61],[-104.616,42.6105],[-104.5967,42.6104],[-104.4777,42.6104],[-104.3598,42.6117],[-104.1247,42.6113],[-104.0525,42.6128]]]},\"properties\":{\"name\":\"Goshen\",\"state\":\"WY\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685b7f","contributors":{"authors":[{"text":"Rapp, J. R.","contributorId":29394,"corporation":false,"usgs":true,"family":"Rapp","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145399,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Visher, F. N.","contributorId":52554,"corporation":false,"usgs":true,"family":"Visher","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145400,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Littleton, R. T.","contributorId":25136,"corporation":false,"usgs":true,"family":"Littleton","given":"R. T.","affiliations":[],"preferred":false,"id":145398,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145401,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":55751,"text":"ofr5713 - 1957 - Ground-water conditions in the Aberdeen-Columbus area, Mississippi","interactions":[],"lastModifiedDate":"2026-01-21T17:12:15.059309","indexId":"ofr5713","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-13","title":"Ground-water conditions in the Aberdeen-Columbus area, Mississippi","docAbstract":"

No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5713","usgsCitation":"Boswell, E.H., and Lang, J., 1957, Ground-water conditions in the Aberdeen-Columbus area, Mississippi: U.S. Geological Survey Open-File Report 57-13, 17 p., https://doi.org/10.3133/ofr5713.","productDescription":"17 p.","costCenters":[],"links":[{"id":369475,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0013/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174171,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0013/report-thumb.jpg"}],"country":"United States","state":"Mississippi","otherGeospatial":"Aberdeen-Columbus area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.604736328125,\n 33.46925353734004\n ],\n [\n -88.31085205078125,\n 33.46925353734004\n ],\n [\n -88.31085205078125,\n 33.87953701355924\n ],\n [\n -88.604736328125,\n 33.87953701355924\n ],\n [\n -88.604736328125,\n 33.46925353734004\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d35a","contributors":{"authors":[{"text":"Boswell, E. H.","contributorId":38954,"corporation":false,"usgs":true,"family":"Boswell","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":254192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lang, J.W.","contributorId":89593,"corporation":false,"usgs":true,"family":"Lang","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":254193,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66491,"text":"i252 - 1957 - Photogeologic map of the Hurricane Cliffs-2 NE quadrangle, Mohave County, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"252","subseriesTitle":"NONE","title":"Photogeologic map of the Hurricane Cliffs-2 NE quadrangle, Mohave County, Arizona","language":"ENGLISH","doi":"10.3133/i252","usgsCitation":"Marshall, C.H., 1957, Photogeologic map of the Hurricane Cliffs-2 NE quadrangle, Mohave County, Arizona: U.S. Geological Survey IMAP 252, 1 map., https://doi.org/10.3133/i252.","productDescription":"1 map.","costCenters":[],"links":[{"id":103036,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1520.htm","linkFileType":{"id":5,"text":"html"},"description":"1520"},{"id":187772,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.36749999999999,36.8675 ], [ -113.36749999999999,37 ], [ -113.25,37 ], [ -113.25,36.8675 ], [ -113.36749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6868ad","contributors":{"authors":[{"text":"Marshall, C. H.","contributorId":31050,"corporation":false,"usgs":true,"family":"Marshall","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274607,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":66085,"text":"i245 - 1957 - Photogeologic map of the Johnson NE quadrangle, Kane County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:11:07","indexId":"i245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"245","subseriesTitle":"NONE","title":"Photogeologic map of the Johnson NE quadrangle, Kane County, Utah","language":"ENGLISH","doi":"10.3133/i245","usgsCitation":"Hackman, R., 1957, Photogeologic map of the Johnson NE quadrangle, Kane County, Utah: U.S. Geological Survey IMAP 245, 1 map., https://doi.org/10.3133/i245.","productDescription":"1 map.","costCenters":[],"links":[{"id":103040,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1524.htm","linkFileType":{"id":5,"text":"html"},"description":"1524"},{"id":190371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.36749999999999,37.1175 ], [ -112.36749999999999,37.25 ], [ -112.25,37.25 ], [ -112.25,37.1175 ], [ -112.36749999999999,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa5b3","contributors":{"authors":[{"text":"Hackman, R.J.","contributorId":95086,"corporation":false,"usgs":true,"family":"Hackman","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":273953,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55757,"text":"ofr5724 - 1957 - Construction and use of special drawdown scales for use in prediction of water-level changes throughout heavily pumped areas","interactions":[],"lastModifiedDate":"2014-05-21T08:01:49","indexId":"ofr5724","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-24","title":"Construction and use of special drawdown scales for use in prediction of water-level changes throughout heavily pumped areas","docAbstract":"

Problem and Proposed Method of Solution

\n
\n

Frequently the Theis nonequilibrium formula is use din the quantitative analyses that are part of many-ground-water investigations. The computations associated therewith may become quite involved and tedious, especially when dealing with predictions of the decline of water levels throughout large areas in which there are many discharging wells. The process of predicting future water-level declines can be greatly simplified and shortened by preparing a special draw-down scale for given conditions. Through use of such a scale much of the computation can be reduced to scaling the values sought from a map, on which the pumped wells have been spotted. The net drawdown effect, which is the sum of the water-level declines caused by the many individual pumped wells, can be determined readily for any desired point in the area. If the net drawdown effect is desired, a summation of the effects of all the pumped wells can be repeated for each point. By determining the water-level change at a number of points, for a given period of time, a contour map of predicted water-level changes for the multiple-well system can be drawn.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5724","usgsCitation":"Conover, C., and Reeder, H., 1957, Construction and use of special drawdown scales for use in prediction of water-level changes throughout heavily pumped areas: U.S. Geological Survey Open-File Report 57-24, 9 p., https://doi.org/10.3133/ofr5724.","productDescription":"9 p.","numberOfPages":"9","costCenters":[],"links":[{"id":287369,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287368,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0024/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2f07","contributors":{"authors":[{"text":"Conover, C.S.","contributorId":79862,"corporation":false,"usgs":true,"family":"Conover","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":254201,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reeder, H.O.","contributorId":108169,"corporation":false,"usgs":true,"family":"Reeder","given":"H.O.","email":"","affiliations":[],"preferred":false,"id":254202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":55760,"text":"ofr5729 - 1957 - Tennessee section of 1956 annual water-level report","interactions":[{"subject":{"id":55760,"text":"ofr5729 - 1957 - Tennessee section of 1956 annual water-level report","indexId":"ofr5729","publicationYear":"1957","noYear":false,"title":"Tennessee section of 1956 annual water-level report"},"predicate":"SUPERSEDED_BY","object":{"id":92,"text":"wsp1538 - 1962 - Ground-water levels in the United States, 1956-58, southeastern States","indexId":"wsp1538","publicationYear":"1962","noYear":false,"title":"Ground-water levels in the United States, 1956-58, southeastern States"},"id":1}],"supersededBy":{"id":92,"text":"wsp1538 - 1962 - Ground-water levels in the United States, 1956-58, southeastern States","indexId":"wsp1538","publicationYear":"1962","noYear":false,"title":"Ground-water levels in the United States, 1956-58, southeastern States"},"lastModifiedDate":"2012-02-02T00:11:49","indexId":"ofr5729","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-29","title":"Tennessee section of 1956 annual water-level report","language":"ENGLISH","doi":"10.3133/ofr5729","usgsCitation":"Criner, J., 1957, Tennessee section of 1956 annual water-level report: U.S. Geological Survey Open-File Report 57-29, 92 p., https://doi.org/10.3133/ofr5729.","productDescription":"92 p.","costCenters":[],"links":[{"id":174253,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db6851fa","contributors":{"authors":[{"text":"Criner, J.H. Jr.","contributorId":24018,"corporation":false,"usgs":true,"family":"Criner","given":"J.H.","suffix":"Jr.","affiliations":[],"preferred":false,"id":254205,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5945,"text":"pp260V - 1957 - Larger Foraminifera from Eniwetok Atoll drill holes","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"pp260V","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"260","chapter":"V","title":"Larger Foraminifera from Eniwetok Atoll drill holes","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp260V","usgsCitation":"Cole, W.S., 1957, Larger Foraminifera from Eniwetok Atoll drill holes: U.S. Geological Survey Professional Paper 260, p. 743-784, https://doi.org/10.3133/pp260V.","productDescription":"p. 743-784","costCenters":[],"links":[{"id":126464,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0260v/report-thumb.jpg"},{"id":32827,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0260v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":32828,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0260v/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8ee1","contributors":{"authors":[{"text":"Cole, W. Storrs","contributorId":97487,"corporation":false,"usgs":true,"family":"Cole","given":"W.","email":"","middleInitial":"Storrs","affiliations":[],"preferred":false,"id":151852,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55754,"text":"ofr5717 - 1957 - Occurrence of ground water near Ana Springs, Summer Lake Basin, Lake County, Oregon","interactions":[],"lastModifiedDate":"2014-05-21T07:55:07","indexId":"ofr5717","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-17","title":"Occurrence of ground water near Ana Springs, Summer Lake Basin, Lake County, Oregon","docAbstract":"

Ana Springs are near the north end of Summer Lake Basin, a closed fault-block basin in Lake County Oregon. The water of the springs rises by artesian pressure from lava-rock aquifers through about 150 feet of overlying thinly bedded lake deposits to discharge at the bottom of an impounding reservoir, the spring orifices being beneath 30 to 36 feet of water. On the valley floor less than a mile south and southwest of the reservoir artesian wells appear to tap the same lava rock from which the waters of the springs arise.

\n
\n

Observations of the piesometric surface of the artesian water during flow tests show that three artesian wells, 30/16-1R1, 30/17-7D1, and -7F1, are hydraulically connected with a fourth, 30/16-1R2, and that well 30/16-1R2 is hydraulically connected with Ana Springs. A fifth artesian well, 30/16-12A1, did not show hydraulic connection with the other four wells during the short-term tests made.

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\n

Mathematical constant derived from the tests permit calculations which indicate that the four wells, 30/16-1R1, -1R2, 30/17-7D1, and -7F1, when flowing at a combined rate of 4,600 gpm for 100 days, may lower the pressure head on Ana Springs by an amount equal to 2.7 feet of water, This lowering in pressure may cause a decrease in the rate of discharge of Ana Springs by about 4.4 cubic feet per second, or about 5 percent of the present wintertime rate of discharge. This diversion (5 percent) would be within the limit of error of single measurement of the the spring discharge. Chemical and temperature characteristics of thew Ana Spring water indicate it is similar to the water of the five lava-rock wells.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5717","collaboration":"Prepared in cooperation with the Oregon State Engineer","usgsCitation":"Brown, S., 1957, Occurrence of ground water near Ana Springs, Summer Lake Basin, Lake County, Oregon: U.S. Geological Survey Open-File Report 57-17, ii, 26 p., https://doi.org/10.3133/ofr5717.","productDescription":"ii, 26 p.","numberOfPages":"40","costCenters":[],"links":[{"id":287364,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287363,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0017/report.pdf"}],"country":"United States","state":"Oregon","county":"Lake County","otherGeospatial":"Ana Springs;Summer Lake Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -121.0,42.25 ], [ -121.0,43.25 ], [ -120.0,43.25 ], [ -120.0,42.25 ], [ -121.0,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692459","contributors":{"authors":[{"text":"Brown, S. G.","contributorId":46914,"corporation":false,"usgs":true,"family":"Brown","given":"S. G.","affiliations":[],"preferred":false,"id":254196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55761,"text":"ofr5731 - 1957 - Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California","interactions":[],"lastModifiedDate":"2014-05-21T08:06:20","indexId":"ofr5731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-31","title":"Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California","docAbstract":"

At the request of the United States Forest Service, the Ground Water Branch of the United Stated Geological Survey made a reconnaissance of the geologic features and water resources of the Dora Belle Campground in Sierra National Forest on the shore of Shaver Lake, Fresno County, California.

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\n

Basically, the water-supply problem at Dora Belle Campground is that the present supply obtained from a spring is not adequate to meet the present summer demand, and is of poor quality. Plans call for a considerable increase in camping facilities.. This, it is imperative that the present supply be augmented or, preferably, be replaced entirely. the Forest Service estimated the future peak demand to be about 25,00 gallons per day.

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\n

On October 28, 1957, the writer examined the are in the company of C. H. Fankboner, Assistant Forest Engineer, Sierra National Forest, and Ben Dix, Construction and Maintenance Foreman, Pine Ridge District. Field work, done on October 28th and 29th, consisted of a brief geologic reconnaissance to determine the rock types and geologic structure, and a hydrologic reconnaissance consisting of a partial inventory of water walls and springs in the vicinity of the campground. A spring box near the western edge of Bell Diamond Meadow was pumped out with a Forest Service pump truck to determine its rate of recovery and potential production.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/ofr5731","collaboration":"Prepared at the request of the Department of Agriculture, Forest Service","usgsCitation":"Davis, G.H., 1957, Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California: U.S. Geological Survey Open-File Report 57-31, 17 p., https://doi.org/10.3133/ofr5731.","productDescription":"17 p.","numberOfPages":"22","costCenters":[],"links":[{"id":287371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287370,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0031/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Shaver Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.374409,37.035345 ], [ -119.374409,37.158277 ], [ -119.242267,37.158277 ], [ -119.242267,37.035345 ], [ -119.374409,37.035345 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eba4","contributors":{"authors":[{"text":"Davis, G. H.","contributorId":40963,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":254206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55762,"text":"ofr5732 - 1957 - Records of selected artesian wells in South Dakota","interactions":[{"subject":{"id":55762,"text":"ofr5732 - 1957 - Records of selected artesian wells in South Dakota","indexId":"ofr5732","publicationYear":"1957","noYear":false,"title":"Records of selected artesian wells in South Dakota"},"predicate":"SUPERSEDED_BY","object":{"id":1260,"text":"wsp1534 - 1961 - Progress report on wells penetrating artesian aquifers in South Dakota","indexId":"wsp1534","publicationYear":"1961","noYear":false,"title":"Progress report on wells penetrating artesian aquifers in South Dakota"},"id":1}],"supersededBy":{"id":1260,"text":"wsp1534 - 1961 - Progress report on wells penetrating artesian aquifers in South Dakota","indexId":"wsp1534","publicationYear":"1961","noYear":false,"title":"Progress report on wells penetrating artesian aquifers in South Dakota"},"lastModifiedDate":"2012-02-02T00:11:49","indexId":"ofr5732","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-32","title":"Records of selected artesian wells in South Dakota","language":"ENGLISH","doi":"10.3133/ofr5732","usgsCitation":"Davis, R.W., 1957, Records of selected artesian wells in South Dakota: U.S. Geological Survey Open-File Report 57-32, 53 p.; 3 plates, https://doi.org/10.3133/ofr5732.","productDescription":"53 p.; 3 plates","costCenters":[],"links":[{"id":174254,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635759","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":254207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55765,"text":"ofr5740 - 1957 - Water quality: a factor in Arkansas River development","interactions":[],"lastModifiedDate":"2019-06-11T15:26:25","indexId":"ofr5740","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-40","title":"Water quality: a factor in Arkansas River development","docAbstract":"

One of the first requisites for intelligent planning of the utilization and control of water and for the administration of laws relating to its use, is data on the quantity, quality, and mode of occurrence of water supplies. The collections, evaluation, interpretation, and publication of such data constitute the primary function of the Water Resources Division of the United States Geological Survey. Since 1895 the Congress has made appropriations to this agency for investigations of the water resources of the Nation. In 1929 the Congress adopted the policy of dollar-for-dollar cooperation with State and local governmental agencies for water-resources investigations. The Geological Survey's Federal-State cooperative program of quality-of-water investigations in Oklahoma was started in 1944 in cooperation with the Oklahoma Planning and Resources Board. Since July of this year the program has been carried on cooperatively with the newly created Oklahoma Water Resources Board.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr5740","usgsCitation":"Dover, T., 1957, Water quality: a factor in Arkansas River development: U.S. Geological Survey Open-File Report 57-40, 14 p., https://doi.org/10.3133/ofr5740.","productDescription":"14 p.","numberOfPages":"17","costCenters":[],"links":[{"id":287375,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287374,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0040/report.pdf"}],"country":"United States","state":"Oklahoma","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -103.0025,33.6158 ], [ -103.0025,37.0023 ], [ -94.4307,37.0023 ], [ -94.4307,33.6158 ], [ -103.0025,33.6158 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3ab3","contributors":{"authors":[{"text":"Dover, T.B.","contributorId":90293,"corporation":false,"usgs":true,"family":"Dover","given":"T.B.","email":"","affiliations":[],"preferred":false,"id":254212,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}