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Low- and intermediate-elevation snow melted, bringing many streams to record-high level. Large diurnal fluctuations of discharge were evident on smaller streams. The temperature remained high until mid-May. As high-elevation snow became primed for runoff, the temperature dropped enough to refreeze and alter the structure of snow cover, thus reducing the effectiveness of the subsequent melting temperature. Had there been no respite from melting temperatures much greater peak discharges would have occurred, with damage greatly exceeding that experienced. Streams remained at high levels for several weeks.
Record peaks were reached on Strawberry River, lower Weber River, Ogden River, Spanish Fork, lower Provo River, and Jordan River in Utah; Humboldt River and its tributaries draining the north area of the basin in Nevada; and the central Bear River in Idaho and Wyoming. Record volumes for the water year were measured on many streams in the northcentral part of Utah, the northeastern part of Nevada, and the central part of the Bear River basin in Idaho and Wyoming.
Damage in the Great Basin reached \\$10 million and in the Green River basin, more than$300,000. Two lives were lost on Ogden River. The greatest urban damage, in Salt Lake City, totaled \\$1.9 million; the greatest single damage, to Denver and Rio Grande Western Railroad, was \\$510,000.
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","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":2134,"text":"wsp1460D - 1957 - Ground-water geology of the Bruneau–Grand View area, Owyhee County, Idaho","interactions":[],"lastModifiedDate":"2022-01-19T20:27:04.38033","indexId":"wsp1460D","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":"1460","chapter":"D","title":"Ground-water geology of the Bruneau–Grand View area, Owyhee County, Idaho","docAbstract":"The Bruneau-Grand View area is part of an artesian basin in northern Owyhee \nCounty, Idaho. The area described in this report comprises about 600 square \nmiles, largely of undeveloped public domain, much of which is open, or may be \nopened, for desert-entry filing. Many irrigation-entry applications to the Federal \nGovernment are pending, and information about ground-water geology is needed \nby local citizens and well drillers, by Federal agencies that have custody of the \nland, and by local and State agencies that administer water rights. The areal \ngeology and ground-water conditions in the Bruneau-Grand View area seemingly \ntypify several basins in southwestern Idaho, and this study is a step toward \ndefinition and analysis of regional problems in ground-water geology and the \noccurrence and availability of ground water for irrigation or other large-scale \nuses.
\nOwyhee County is subdivided physiographically into a plateau area, the Owyhee uplift, and the Snake River valley. The Bruneau-Grand View area is largely \nwithin the Snake River valley. The climate is arid and irrigation is essential \nfor stable agricultural development. Nearly all usable indigenous surface water \nin the area is appropriated, including freshet flow in the Bruneau River, which \nis used for power generation at the C. J. Strike Dam. However, with storage \nfacilities additional land could be irrigated, and some land may be irrigated with \nSnake River water if suitable reclamation projects are constructed.
\nSedimentary and igneous rocks exposed in the area range in age from Miocene \nto Recent. The igneous rocks include silicic and basic intrusive and extrusive \nbodies, and the sedimentary rocks are compacted stream and lake sediments. \nThe rocks contain economically important artesian aquifers; the principal ones \nare volcanic rocks in which ground water is imperfectly confined beneath sediments of the Idaho formation, thus forming a leaky artesian system. The altitude \nof the piezometric surface of the artesian water does not exceed about 2,700 \nfeet above mean sea level. In some areas, where the land surface is below \nthat altitude, the artesian system discharges water through springs and seeps \nand locally causes waterlogging and development of alkali soil.
\nIn chemical quality much of the water is unsuitable for irrigation and domestic \nuse. The water contains a relatively moderate amount of dissolved solids, but \nthe percent sodium and the concentration of fluoride are excessive for some \nuses. The quality of the water for irrigation ranges from excellent in the southern part of the artesian system to unsuitable in the northern part. All the \nartesian ground water that was sampled contained excessive amounts of fluoride.
\nThere is a substantial supply of undeveloped artesian water in the area, but\nsustained use of the water for irrigation may not be feasible unless provisions \ncan be made for adequate soil drainage and soil amendment, because of the high \npercentage of sodium in the water. Detailed hydrologic and geologic study of \nthe area should precede development.
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G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":144717,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":2150,"text":"wsp1380 - 1957 - Quality of surface waters for irrigation, western United States, 1953","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1380","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":"1380","title":"Quality of surface waters for irrigation, western United States, 1953","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1380","usgsCitation":"Love, S.K., 1957, Quality of surface waters for irrigation, western United States, 1953: U.S. Geological Survey Water Supply Paper 1380, viii, 203 p. :ill., map ;25 cm., https://doi.org/10.3133/wsp1380.","productDescription":"viii, 203 p. :ill., map ;25 cm.","costCenters":[],"links":[{"id":137821,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1380/report-thumb.jpg"},{"id":27760,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1380/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ee4b07f02db6549f9","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":144745,"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.
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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":49,"text":"wsp1320B - 1957 - Floods of May-June 1953 in Missouri River basin in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1320B","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":"1320","chapter":"B","title":"Floods of May-June 1953 in Missouri River basin in Montana","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1320B","usgsCitation":"Wells, J.V., 1957, Floods of May-June 1953 in Missouri River basin in Montana: U.S. Geological Survey Water Supply Paper 1320, p. 69-153 :ill., maps ;24 cm., https://doi.org/10.3133/wsp1320B.","productDescription":"p. 69-153 :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137532,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1320b/report-thumb.jpg"},{"id":24678,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1320b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24679,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1320b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1320b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df91f","contributors":{"authors":[{"text":"Wells, J. 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