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,{"id":2783,"text":"wsp1418 - 1957 - Geology and ground water, Heart Mountain and Chapman Bench Divisions, Shoshone irrigation project, Wyoming","interactions":[],"lastModifiedDate":"2022-01-11T22:52:16.660418","indexId":"wsp1418","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":"1418","title":"Geology and ground water, Heart Mountain and Chapman Bench Divisions, Shoshone irrigation project, Wyoming","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1418","usgsCitation":"Swenson, F.A., and Swenson, H., 1957, Geology and ground water, Heart Mountain and Chapman Bench Divisions, Shoshone irrigation project, Wyoming: U.S. Geological Survey Water Supply Paper 1418, Report: iv, 55 p.;  5 Plates: 20.50 × 24.00 inches or smaller, https://doi.org/10.3133/wsp1418.","productDescription":"Report: iv, 55 p.;  5 Plates: 20.50 × 24.00 inches or smaller","costCenters":[],"links":[{"id":29257,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1418/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29256,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1418/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29255,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1418/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29254,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1418/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247248,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1418/plate-7.pdf","size":"1262","linkFileType":{"id":1,"text":"pdf"}},{"id":247247,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1418/plate-6.pdf","size":"822","linkFileType":{"id":1,"text":"pdf"}},{"id":138854,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1418/report-thumb.jpg"},{"id":394229,"rank":8,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24372.htm"}],"country":"United States","state":"Wyoming","otherGeospatial":"Heart Mountain and Chapman Bench divisions","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.136,\n              44.51\n            ],\n            [\n              -108.842,\n              44.51\n            ],\n            [\n              -108.842,\n              44.783\n            ],\n            [\n              -109.136,\n              44.783\n            ],\n            [\n              -109.136,\n              44.51\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685fde","contributors":{"authors":[{"text":"Swenson, Frank Albert","contributorId":71958,"corporation":false,"usgs":true,"family":"Swenson","given":"Frank","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":145780,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, Herbert","contributorId":54181,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","affiliations":[],"preferred":false,"id":145779,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2393,"text":"wsp1360I - 1957 - Reconnaissance of the ground-water resources of the Elkhorn River Basin above Pilger, Nebraska, with a section on chemical quality of the water","interactions":[],"lastModifiedDate":"2022-07-06T21:12:19.504709","indexId":"wsp1360I","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":"1360","chapter":"I","title":"Reconnaissance of the ground-water resources of the Elkhorn River Basin above Pilger, Nebraska, with a section on chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1360I","usgsCitation":"Newport, T.G., and Krieger, R.A., 1957, Reconnaissance of the ground-water resources of the Elkhorn River Basin above Pilger, Nebraska, with a section on chemical quality of the water: U.S. Geological Survey Water Supply Paper 1360, Report: iv, 40 p.; 2 Plates: 35.50 × 19.50 inches and 15.00 × 13.50 inches, https://doi.org/10.3133/wsp1360I.","productDescription":"Report: iv, 40 p.; 2 Plates: 35.50 × 19.50 inches and 15.00 × 13.50 inches","startPage":"715","endPage":"754","costCenters":[],"links":[{"id":403103,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24344.htm"},{"id":139188,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360i/report-thumb.jpg"},{"id":28370,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247207,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360i/plate-45.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247206,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360i/plate-44.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","city":"Pilger","otherGeospatial":"Elkhorn River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -99.554,\n              41.688\n            ],\n            [\n              -97,\n              41.688\n            ],\n            [\n              -97,\n              42.548\n            ],\n            [\n              -99.554,\n              42.548\n            ],\n            [\n              -99.554,\n              41.688\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636be9","contributors":{"authors":[{"text":"Newport, Thomas Gwyn","contributorId":39353,"corporation":false,"usgs":true,"family":"Newport","given":"Thomas","email":"","middleInitial":"Gwyn","affiliations":[],"preferred":false,"id":145128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krieger, R. A.","contributorId":11202,"corporation":false,"usgs":true,"family":"Krieger","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145127,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2049,"text":"wsp1360E - 1957 - Geology and ground-water resources of the Kaycee irrigation project, Johnson County, Wyoming","interactions":[],"lastModifiedDate":"2024-11-27T16:02:15.632063","indexId":"wsp1360E","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":"1360","chapter":"E","title":"Geology and ground-water resources of the Kaycee irrigation project, Johnson County, Wyoming","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1955","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1360E","usgsCitation":"Kohout, F.A., and Rainwater, F.H., 1957, Geology and ground-water resources of the Kaycee irrigation project, Johnson County, Wyoming: U.S. Geological Survey Water Supply Paper 1360, Report: iv, 54 p.; 4 Plates: 49.36 × 26.00 inches or smaller, https://doi.org/10.3133/wsp1360E.","productDescription":"Report: iv, 54 p.; 4 Plates: 49.36 × 26.00 inches or smaller","costCenters":[],"links":[{"id":27575,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360e/chart-1.pdf","text":"Chart 1","linkFileType":{"id":1,"text":"pdf"}},{"id":394254,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24340.htm"},{"id":27576,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360e/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27574,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360e/plate-23.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27573,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360e/plate-22-2.pdf","text":"Plate 22-2","linkFileType":{"id":1,"text":"pdf"}},{"id":27572,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360e/plate-22-1.pdf","text":"Plate 22-1","linkFileType":{"id":1,"text":"pdf"}},{"id":137730,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360e/report-thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Johnson County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.9533,\n              43.5994\n            ],\n            [\n              -106.1758,\n              43.5994\n            ],\n            [\n              -106.1758,\n              43.8783\n            ],\n            [\n              -106.9533,\n              43.8783\n            ],\n            [\n              -106.9533,\n              43.5994\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685509","contributors":{"authors":[{"text":"Kohout, Francis Anthony","contributorId":11200,"corporation":false,"usgs":true,"family":"Kohout","given":"Francis","email":"","middleInitial":"Anthony","affiliations":[],"preferred":false,"id":144592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rainwater, F. H.","contributorId":41402,"corporation":false,"usgs":true,"family":"Rainwater","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3065,"text":"wsp1396 - 1957 - Surface water supply of the United States, 1955, Part XII, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"wsp1396","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":"1396","title":"Surface water supply of the United States, 1955, Part XII, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1396","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1957, Surface water supply of the United States, 1955, Part XII, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Water Supply Paper 1396, ix, 333 p. ;23 cm., https://doi.org/10.3133/wsp1396.","productDescription":"ix, 333 p. ;23 cm.","costCenters":[],"links":[{"id":139437,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1396/report-thumb.jpg"},{"id":29923,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1396/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db6961e1","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":528053,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2113,"text":"wsp1421 - 1957 - Geology and ground-water resources of Outagamie County, Wisconsin","interactions":[],"lastModifiedDate":"2015-10-05T09:02:03","indexId":"wsp1421","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":"1421","title":"Geology and ground-water resources of Outagamie County, Wisconsin","docAbstract":"<p>Outagamie County is in east-central Wisconsin. It has no serious groundwater problem at present, but the county is important as a recharge area for the principal aquifers supplying water to Brown County and industrial Green Bay to the east.</p>\n<p>The county is covered by glacial drift and lake deposits of the Wisconsin stage of glaciation. In the northwestern quarter of the county these deposits rest upon Precambrian crystalline rocks; throughout the remainder of the county they are underlain by sandstone, limestone, dolomite, and shale of Cambrian and Ordovician age. &middot;where they are sufficiently thick, and where more productive formations are absent, glacial sand and gravel are an important source of ground water. The major sources, however, are the St. Peter sandstone, of Ordovician age, and the sandstones of the Upper Cambrian series. The Precambrian crystalline rocks, which underlie all the county, yield little or no water to wells.</p>\n<p>The regional dip of the Paleozoic bedrocks is 25 to 30 feet per mile eastward and southeastward. There are no major folds, but the thickness of each geologic unit may change from place to place because of predepositional or postdepositional erosion. There is no conclusive evidence of major faulting in the area.</p>\n<p>Ground water in Outagamie County occurs under both water-table (unconfined) and artesian (confined) conditions. The source of the ground water is precipitation which falls on the surface and percolates downward into the underlying permeable materials. Regional movement of ground water in the eastern third of the county is controlled by the bedrock structure, and the discharge is toward the east and south. Throughout the rest of the county the movement of water is controlled mainly by bedrock and surface topography, and the water moves toward the streams and bedrock valleys.</p>\n<p>Water-level :fluctuations follow definite patterns. Where the effects of pumping are at a minimum, water levels reach a high in April or May, decline through the summer months owing to natural discharge, and lack of recharge, and do not begin to recover until after the ground thaws in the spring. In areas of heavy pumping where this pattern is distorted, the lowest water levels occur in the early fall and recoveries begin in October or November after the period of heaviest pumping.</p>\n<p>Pumpage in the county was estimated to be about 9.0 million gallons per day (mgd) in 1951 and 1952. Nearly half of this was for industrial, commercial, and public-supply use along the Fox River. Wells, most of which are drilled by the cable-tool method, range in diameter from 3 to 16 inches and in depth from 10 or 20 feet to 804 feet. In the alluvium and glacial drift 1~- to 2&yen;2-inch driven wells are common.</p>\n<p>Pumping tests were made to determine the hydraulic characteristics of the aquifers at Seymour, Appleton, and Hortonville. The average coefficient of transmissibility at Seymour is about 18,000 gpd per foot; at Appleton it is about 19,000 gpd per foot. The coefficients of storage are 0.00022 and 0.00015 at Seymour and Appleton, respectively. Movement of ground water out of the county, assuming an average transmissibility of 18,000 gpd per foot, was calculated to be more than 10 mgd toward the southeast.</p>\n<p>The ground water differs greatly in chemical quality from well to well, but it is generally a very hard calcium magnesium bicarbonate water, some of it high in iron. To aid in determining the source of well waters, 22 chemical analyses were plotted on a logarithmic diagram to obtain characteristic patterns for waters from several geologic sources.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1421","usgsCitation":"LeRoux, E.F., 1957, Geology and ground-water resources of Outagamie County, Wisconsin: U.S. Geological Survey Water Supply Paper 1421, Report: 57 p.; 7 Plates: 26.60 x 19.80 inches or smaller, https://doi.org/10.3133/wsp1421.","productDescription":"Report: 57 p.; 7 Plates: 26.60 x 19.80 inches or smaller","numberOfPages":"57","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":138327,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1421/report-thumb.jpg"},{"id":27696,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1421/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27695,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27689,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27693,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27694,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27690,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27691,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27692,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1421/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wisconsin","county":"Outagamie County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-88.6062,44.5903],[-88.4889,44.5894],[-88.3671,44.5875],[-88.2453,44.5846],[-88.2203,44.5858],[-88.1908,44.5864],[-88.1918,44.5016],[-88.1921,44.4167],[-88.1921,44.3871],[-88.1919,44.3288],[-88.193,44.2421],[-88.2536,44.2432],[-88.2835,44.243],[-88.3754,44.2443],[-88.4041,44.244],[-88.4966,44.2443],[-88.5247,44.2441],[-88.6185,44.2438],[-88.6453,44.2435],[-88.7397,44.2432],[-88.7381,44.3307],[-88.7365,44.4164],[-88.7368,44.5021],[-88.7371,44.5906],[-88.6152,44.5903],[-88.6062,44.5903]]]},\"properties\":{\"name\":\"Outagamie\",\"state\":\"WI\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f8","contributors":{"authors":[{"text":"LeRoux, E. F.","contributorId":29795,"corporation":false,"usgs":true,"family":"LeRoux","given":"E.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":144693,"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":"<p>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.</p>","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":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":2942,"text":"wsp1384 - 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","interactions":[],"lastModifiedDate":"2012-02-02T00:05:33","indexId":"wsp1384","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":"1384","title":"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","language":"ENGLISH","publisher":"U.S. Govt. Print. 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":2343,"text":"wsp1412 - 1957 - Water consumption by water-loving plants in the Malad Valley, Oneida County, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1412","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":"1412","title":"Water consumption by water-loving plants in the Malad Valley, Oneida County, Idaho","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1412","usgsCitation":"Mower, R.W., and Nace, R.L., 1957, Water consumption by water-loving plants in the Malad Valley, Oneida County, Idaho: U.S. Geological Survey Water Supply Paper 1412, iv, 33 p. :illus., maps. ;24 cm., https://doi.org/10.3133/wsp1412.","productDescription":"iv, 33 p. :illus., maps. ;24 cm.","costCenters":[],"links":[{"id":138339,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1412/report-thumb.jpg"},{"id":28257,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1412/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28258,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1412/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1412/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa235","contributors":{"authors":[{"text":"Mower, Reed W.","contributorId":32503,"corporation":false,"usgs":true,"family":"Mower","given":"Reed","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145051,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145052,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2873,"text":"wsp1411 - 1957 - The deep channel and alluvial deposits of the Ohio Valley in Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:35","indexId":"wsp1411","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":"1411","title":"The deep channel and alluvial deposits of the Ohio Valley in Kentucky","docAbstract":"The alluvial deposits of Pleistocene age in the Ohio Valley form a ground-water reservoir of large storage capacity and yield. In this region it is the only source of large supplies of water that are both cool and of good quality the year round. The reservoir is heavily drawn upon, yet has very large potentialities for future development because of the favorable conditions for both natural and artificially induced infiltration of water from the river into the alluvial deposits. \r\n\r\nThe principal features of the Ohio Valley were formed during the Pleistocene, or glacial, epoch. The drainage area upriver from Cincinnati was added when ice first advanced south, blocked rivers draining northwestward off the Appalachians, and diverted their waters southwest into the headwaters of the early Ohio River. A deep channel, the bottom of which is at a lower altitude than the present river bed, was excavated before the third (Illinoian) glacial stage. The thick body of sand and gravel that now lies in the deep channel was deposited by floods of melt water as the ice sheet of the Wisconsin stage melted away from the Ohio basin. \r\n\r\nThe vertical distance between river pool level and the base of the old channel increases from 25 feet at Ashland, Ky., to 110 feet at the mouth of the river, for the old channel has a steeper gradient than the present river. The width of the bedrock valley ranges from half a mile at one point near Cincinnati to almost 10 miles near Uniontown, Ky. Where the valley is narrow, the flat-floored deep channel extends from one side of the valley to. the other. Where the valley is wide, the deep channel occupies only part of the width of the valley, the rest being underlain by rock benches mantled with alluvium. The alluvium consists of a sheet of sand and gravel overlain by a thinner layer of silt and clay. The sheet of sand and gravel is continuous across and up and down the valley, and at most places along the valley it is exposed in part of the river channel. The gravel is coarse and cobbly near Cincinnati but finer downstream, and near Paducah most of it is no larger than pea size. The thickness of water-saturated sand and gravel increases downvalley in the same way as does the distance between river level and the base of the old channel, roughly from 2b to 110 feet. The storage coefficient is likely to about 0.2, or 1.5 gallons of water per cubic foot of sand and gravel.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1411","usgsCitation":"Walker, E.H., 1957, The deep channel and alluvial deposits of the Ohio Valley in Kentucky: U.S. Geological Survey Water Supply Paper 1411, iii, 25 p. :maps, diagrs. ;23 cm., https://doi.org/10.3133/wsp1411.","productDescription":"iii, 25 p. :maps, diagrs. ;23 cm.","costCenters":[],"links":[{"id":138976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1411/report-thumb.jpg"},{"id":29495,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29496,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29497,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29498,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29499,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29500,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1411/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29501,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1411/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668811","contributors":{"authors":[{"text":"Walker, Eugene H.","contributorId":24761,"corporation":false,"usgs":true,"family":"Walker","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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