Those of us who seek to explain the variations in hydrologic phenomena such as may be observed in the occurrence of floods or in changes in the shape of river channels are painfully aware of the lack of adequate data. Our existing data, collected mainly to serve immediate practical needs for water-resources development, usually are deficient in providing information useful for many kinds of scientific inquiry. Hydrologic records are usually obtained on streams that are highly regulated or otherwise put to use, to the neglect of headwater streams better suited to studies of the details of hydrologic processes.
","language":"English","publisher":"Taylor & Francis","doi":"10.1080/02626666209493250","usgsCitation":"Leopold, L.B., 1962, The Vigil Network: International Association of Scientific Hydrology - Bulletin , v. 7, no. 2, p. 5-9, https://doi.org/10.1080/02626666209493250.","productDescription":"5 p.","startPage":"5","endPage":"9","costCenters":[],"links":[{"id":338317,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"7","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d6304ce4b05ec799131147","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686124,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70176018,"text":"70176018 - 1961 - Geology and ground-water resources of Sumner County, Kansas","interactions":[],"lastModifiedDate":"2018-09-27T11:55:07","indexId":"70176018","displayToPublicDate":"2015-11-16T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Sumner County, Kansas","docAbstract":"This report describes the geography, geology, and ground-water resources of Sumner County in south-central Kansas. The hydrologic and geologic data upon which this report is based were obtained in the field during the summers of 1955 and 1956. Records of 300 wells and 2 springs, chemical analyses of 219 water samples from wells and test holes and of 15 from streams, and logs of 362 wells and test holes are included in tables.
Sumner County has an area of 1,183 square miles and lies in the Wellington Lowland and Arkansas River Lowlands of the Central Lowland physiographic province. It is drained by Arkansas River, Ninnescah River, and Chikaskia River and their tributaries. The land surface in general is a southeastward-sloping, gently rolling plain. The average annual precipitation at Wellington is about 31 inches. Wheat fanning is the principal industry of the county, and oil is the chief natural resource.
The Wellington Formation, of Permian age, crops out in the eastern two-thirds of the county except where it is covered by Pleistocene deposits. The Ninnescah Shale (Permian) overlies the Wellington Formation and crops out in parts of the western third of the county. The Permian rocks yield small quantities of hard water to wells. Pleistocene sand and gravel deposits of Nebraskan age are present in the northwestern corner of the county and yield moderate quantities of good water to wells. Discontinuous deposits of Kansan or Illinoisan age, locally mantled by colluvium, forms terraces in southern and eastern Sumner County, and may yield moderate quantities of water. Wisconsinan terrace deposits and Recent alluvium along the major streams yield large quantities of water. Colluvium and dune sand are unimportant as sources of water but may facilitate recharge.
Maps of Sumner County included in this report show the outcrop areas of the formations, geologic cross sections, the shape and slope of the water table, the locations of wells and test holes for which records are given, and the distribution of chloride in water samples.
The ground-water reservoir is recharged principally from rain and snow that fall within the county, by percolation from streams and other surface bodies of water, and by underflow from adjacent areas. Water is discharged from the ground-water reservoir by seepage into streams, by transpiration and evaporation, by movement into adjacent areas, and by wells. Water is pumped from wells for domestic, stock, municipal, industrial, and irrigation use. Irrigation from wells is most extensive in the valley of Arkansas River, in which area further development is most probable.
Chemical analyses of samples of water from Sumner County indicate that the quality varies greatly from place to place. Sulfate is common in water from the Wellington Formation and Ninnescah Shale. Water from Pleistocene deposits is generally suitable for most uses except in local areas where it contains excessive chloride.
","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Walters, K., 1961, Geology and ground-water resources of Sumner County, Kansas: Kansas Geological Survey Bulletin, v. 151, 198 p. .","productDescription":"198 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327735,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327734,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/Geology/Sumner/index.html"}],"volume":"151","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2ce7","contributors":{"authors":[{"text":"Walters, K.L.","contributorId":105765,"corporation":false,"usgs":true,"family":"Walters","given":"K.L.","affiliations":[],"preferred":false,"id":646804,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71747,"text":"tei791 - 1961 - Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions","interactions":[],"lastModifiedDate":"2018-10-03T09:25:01","indexId":"tei791","displayToPublicDate":"2013-07-16T09:38:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"791","title":"Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions","docAbstract":"The Appalachian basin is an elongate depression in the crystalline basement complex which contains a great volume of predominantly sedimentary stratified rocks. As defined in this paper it extends from the Adirondack Mountains in New York to central Alabama. From east to west it extends from the west flank of the Blue Ridge Mountains to the crest of the Findlay and Cincinnati arches and the Nashville dome. It encompasses an area of about 207,000 square miles, including all of West Virginia and parts of New York, New Jersey, Pennsylvania, Ohio, Maryland, Virginia, Kentucky, Tennessee, North Carolina, Georgia, and Alabama.
The stratified rocks that occupy the basin constitute a wedge-shaped mass whose axis of greatest thickness lies close to and parallel to the east edge of the basin. The maximum thickness of stratified rocks preserved in any one part of the basin today is between 35,000 and 40,000 feet. The volume of the sedimentary rocks is approximately 510,000 cubic miles and of volcanic rocks is a few thousand cubic miles. The sedimentary rocks are predominantly Paleozoic in age, whereas the volcanic rocks are predominantly Late Precambrian.
On the basis of gross lithology the stratified rocks overlying the crystalline basement complex can be divided into nine vertically sequential units, which are designated \"sequences\" in this report. The boundaries between contiguous sequences do not necessarily coincide with the commonly recognized boundaries between systems or series. All sequences are grossly wedge shaped, being thickest along the eastern margin of the basin and thinnest along the western margin.
The lowermost unit the Late Precambrian stratified sequence is present only along part of the eastern margin of the basin, where it lies unconformably on the basement complex. It consists largely of volcanic tuffs and flows but contains some interbedded sedimentary rocks. The Late Precambrian sequence is overlain by the Early Cambrian clastic sequence. Where the older sequence is absent, the Early Cambrian sequence rests on the basement complex. Interbedded fine- to coarse-grained noncarbonate detrital rocks comprise the bulk of the sequence, but some volcanic and carbonate rocks are included. Next above is the Cambrian-Ordovician carbonate sequence which consists largely of limestone and dolomite. Some quartzose sandstone is present in the lower part in the western half of the basin, and much shale is present in the upper part in the southeast part of the basin. The next higher sequence is the Late Ordovician clastic sequence, which consists largely of shale, siltstone, and sandstone. Coarse-grained light-gray to red rocks are common in the sequence along the eastern side of the basin, whereas fine-grained dark-gray to black calcareous rocks are common along the west side. The Late Ordovician clastic sequence is overlain unconformably in many places by the Early Silurian clastic sequence. The latter comprises a relatively thin wedge of coarse-grained clastic rocks. Some of the most prolific oil- and gas-producing sandstones in the Appalachian basin are included. Among these are the \"Clinton\" sands of Ohio, the Medina Sandstones of New York and Pennsylvania, and the Keefer or \"Big Six\" Sandstone of West Virginia and Kentucky. Conformably overlying the Early Silurian clastic sequence is the Silurian-Devonian carbonate sequence, which consists predominantly of limestone and dolomite. It also contains a salt-bearing unit in the north-central part of the basin and a thick wedge of coarse-grained red beds in the northeastern part. The sequence is absent in much of the southern part of the basin. Large volumes of gas and much oil are obtained from some of its rocks, especially from the Oriskany Sandstone and the Huntersville Ghert. The Silurian-Devonian carbonate sequence is abruptly overlain by the Devonian clastic sequence a thick succession of interbedded shale, mudrock, siltstone, and sandstone. Colors range from predominantly purple and red in the northeastern part of the basin to predominantly dark gray and black in the southwestern part. Many rocks in the upper part contain hydrocarbons in commercial quantities. The next higher sequence is a heterogeneous succession that comprises most rocks of Mississippian age in the basin. It is composed largely of fine-grained to very coarse-grained noncalcareous clastic rocks in the northern half of the basin, and largely of carbonate rocks in the southern part. Large quantities of oil and gas are produced from the sequence. The youngest sequence consists of coarse-grained clastic rocks largely of Pennsylvanian age. In the center of the basin a relatively small volume of lithologically similar rocks of Permian age are included. The sequence has been intensively mined for coal throughout most of its extent.
The waste-disposal possibilities of the stratified rocks in the Appalachian basin are considered in terms of the following: 1) gross lithology of the sequences; 2) general lithology of the rock units composing the sequences; and 3) the structural attitudes of the sequences in different parts of the basin. The degree of exploitation of economically significant mineral* resources is considered briefly where such exploitation may affect waste-disposal possibilities. Hydrologic aspects are not in general considered. Based largely on consideration of the above geologic factors the following types of reservoirs associated with particular geologic environments offer some prospects for the disposal of radioactive waste solutions. They are: 1) artificially created cavities in thick salt beds; 2) artificially fractured thin lenticular sandstone bodies isolated in shale or mudrock sequences; 3) portions of thick noncarbonate clastic sequences possessing appreciable natural porosity and permeability; 4) thin clastic units (with natural or artificially created openings) in the plate of a thrust fault overlain by impermeable strata.
Considered in its entirety the Late Ordovician clastic sequence appears to have a greater number of favorable geologic factors for waste-disposal purposes than the others. The Early Silurian clastic sequence, the Silurian-Devonian carbonate sequence, and the Devonian clastic sequence offer fewer possibilities. The Late Precambrian stratified sequence, Early Cambrian, and the Cambrian-Ordovician carbonate sequence offer few possibilities. The Mississippian and Pennsylvanian sequences appear to be generally unsuitable.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei791","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Colton, G.W., 1961, Geologic summary of the Appalachian basin, with reference to the subsurface disposal of radioactive waste solutions: U.S. Geological Survey Trace Elements Investigations 791, Report: 121 p.; 15 Maps; 1 Illustration, https://doi.org/10.3133/tei791.","productDescription":"Report: 121 p.; 15 Maps; 1 Illustration","costCenters":[],"links":[{"id":358066,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358065,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358067,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358068,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358069,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358070,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358071,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358072,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358073,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358074,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358075,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358076,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358077,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358078,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358079,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358080,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":358081,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":290249,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0028/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.71,35.8 ], [ -84.71,43.91 ], [ -74.13,43.91 ], [ -74.13,35.8 ], [ -84.71,35.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ef3e4b0194841642446","contributors":{"authors":[{"text":"Colton, George Willis","contributorId":12015,"corporation":false,"usgs":true,"family":"Colton","given":"George","email":"","middleInitial":"Willis","affiliations":[],"preferred":false,"id":284696,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71744,"text":"tei787 - 1961 - Hydrologic significance of six core holes in carbonate rocks of the Nevada test site","interactions":[],"lastModifiedDate":"2014-07-16T09:31:07","indexId":"tei787","displayToPublicDate":"2013-07-16T09:29:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"787","title":"Hydrologic significance of six core holes in carbonate rocks of the Nevada test site","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei787","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Schoff, S.L., and Winograd, I.J., 1961, Hydrologic significance of six core holes in carbonate rocks of the Nevada test site: U.S. Geological Survey Trace Elements Investigations 787, 97 p., https://doi.org/10.3133/tei787.","productDescription":"97 p.","costCenters":[],"links":[{"id":290247,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.01,35.0 ], [ -120.01,42.0 ], [ -114.04,42.0 ], [ -114.04,35.0 ], [ -120.01,35.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79efce4b019484164245f","contributors":{"authors":[{"text":"Schoff, Stuart Leeson","contributorId":57951,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart","email":"","middleInitial":"Leeson","affiliations":[],"preferred":false,"id":284693,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":284692,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70047041,"text":"70047041 - 1961 - Water utilization in the Anchorage area, Alaska, 1958-59","interactions":[{"subject":{"id":52142,"text":"ofr60150 - 1960 - Water utilization in the Anchorage area, Alaska, 1958-59","indexId":"ofr60150","publicationYear":"1960","noYear":false,"title":"Water utilization in the Anchorage area, Alaska, 1958-59"},"predicate":"SUPERSEDED_BY","object":{"id":70047041,"text":"70047041 - 1961 - Water utilization in the Anchorage area, Alaska, 1958-59","indexId":"70047041","publicationYear":"1961","noYear":false,"title":"Water utilization in the Anchorage area, Alaska, 1958-59"},"id":1}],"lastModifiedDate":"2013-07-15T15:10:16","indexId":"70047041","displayToPublicDate":"2013-01-01T15:05:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":258,"text":"Hydrological Data","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"12","title":"Water utilization in the Anchorage area, Alaska, 1958-59","language":"English","publisher":"Alaska Department of Health and Welfare","collaboration":"Issued in cooperation with the U.S. Geological Survey, Water Resources Division","usgsCitation":"Waller, R., 1961, Water utilization in the Anchorage area, Alaska, 1958-59: Hydrological Data 12, 19 p.","productDescription":"19 p.","costCenters":[],"links":[{"id":275007,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Anchorage","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153.25,59.75 ], [ -153.25,62.5 ], [ -145.75,62.5 ], [ -145.75,59.75 ], [ -153.25,59.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51e519f5e4b069f8d27ccb72","contributors":{"authors":[{"text":"Waller, R.M.","contributorId":13659,"corporation":false,"usgs":true,"family":"Waller","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":480917,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70040438,"text":"70040438 - 1961 - Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York","interactions":[],"lastModifiedDate":"2012-10-19T17:16:26","indexId":"70040438","displayToPublicDate":"2012-01-01T13:59:30","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":242,"text":"Bulletin","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"GW-45","title":"Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York","language":"English","publisher":"New York State Water Resources Commission","publisherLocation":"Albany, NY","usgsCitation":"Hoffman, J., 1961, Hydrology of the shallow ground-water reservoir of the Town of Southold, Suffolk County, Long Island, New York: Bulletin GW-45, 49 p., 1 Plate.","productDescription":"49 p., 1 Plate","numberOfPages":"49","costCenters":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"links":[{"id":262740,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -79.760000,40.480000 ], [ -79.760000,45.020000 ], [ -71.860000,45.020000 ], [ -71.860000,40.480000 ], [ -79.760000,40.480000 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"50df0563e4b0dfbe79e686de","contributors":{"authors":[{"text":"Hoffman, J.F.","contributorId":37413,"corporation":false,"usgs":true,"family":"Hoffman","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":468327,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68391,"text":"ha43 - 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1961 - Studies of the hydrology of the lower Colorado River area","interactions":[],"lastModifiedDate":"2012-02-02T00:11:14","indexId":"ofr6192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-92","title":"Studies of the hydrology of the lower Colorado River area","language":"ENGLISH","doi":"10.3133/ofr6192","usgsCitation":"McDonald, C.C., 1961, Studies of the hydrology of the lower Colorado River area: U.S. Geological Survey Open-File Report 61-92, 8 p., https://doi.org/10.3133/ofr6192.","productDescription":"8 p.","costCenters":[],"links":[{"id":176827,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dc9","contributors":{"authors":[{"text":"McDonald, C. 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Some of the basic hydrologic data has been collected by the Geological Survey during the early investigations of ground-water conditions in the Quincy Basin (Henshaw, written communication, 1917; Schwennesen and Meinzer, 1918). Most of the data, however, were obtained by the Geological Survey since 1941, in cooperation with the U.S. Bureau of Reclamation and the Washington State Department of Conservation under continuing programs in the area of the Columbia Basin Project of the Bureau of Reclamation. Some preliminary geologic field work in the Moses Lake North quadrangle was done by the Geological Survey in 1954 in cooperation with the Washington State Department of Conservation.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i330","collaboration":"Prepared in cooperation with the Washington State Department of Conservation","usgsCitation":"Grolier, M.J., and Foxworthy, B.L., 1961, Geology of the Moses Lake North quadrangle, Washington: U.S. Geological Survey IMAP 330, Plate: 37.73 x 40.60 inches, https://doi.org/10.3133/i330.","productDescription":"Plate: 37.73 x 40.60 inches","costCenters":[],"links":[{"id":102912,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1379.htm","linkFileType":{"id":5,"text":"html"},"description":"1379"},{"id":189540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0330/report-thumb.jpg"},{"id":279958,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0330/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Washington","otherGeospatial":"Moses Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.375,47.125 ], [ -119.375,47.25 ], [ -119.25,47.25 ], [ -119.25,47.125 ], [ -119.375,47.125 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e98d","contributors":{"authors":[{"text":"Grolier, Maurice J.","contributorId":98292,"corporation":false,"usgs":true,"family":"Grolier","given":"Maurice","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":273889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Foxworthy, Bruce L.","contributorId":88815,"corporation":false,"usgs":true,"family":"Foxworthy","given":"Bruce","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":273888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68325,"text":"ha42 - 1961 - Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","interactions":[],"lastModifiedDate":"2022-06-03T20:40:02.242302","indexId":"ha42","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"42","title":"Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha42","usgsCitation":"Herrick, E.H., 1961, Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells: U.S. Geological Survey Hydrologic Atlas 42, 1 Plate: 27.50 × 21.00 inches, https://doi.org/10.3133/ha42.","productDescription":"1 Plate: 27.50 × 21.00 inches","costCenters":[],"links":[{"id":185963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":401720,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15804.htm"},{"id":89786,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"680","country":"United States","state":"New Mexico","county":"Dona Ana County","otherGeospatial":"White Sands Missile Range headquarters area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.622314453125,\n 32.287132632616384\n ],\n [\n -106.383,\n 32.287132632616384\n ],\n [\n -106.383,\n 32.465743313283596\n ],\n [\n -106.622314453125,\n 32.465743313283596\n ],\n [\n -106.622314453125,\n 32.287132632616384\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2aef","contributors":{"authors":[{"text":"Herrick, Eugene H.","contributorId":80360,"corporation":false,"usgs":true,"family":"Herrick","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68695,"text":"ha41 - 1961 - Floods at Boulder, Colorado","interactions":[{"subject":{"id":52181,"text":"ofr6177 - 1961 - Preliminary report on floods on Boulder Creek below Boulder, Colorado","indexId":"ofr6177","publicationYear":"1961","noYear":false,"title":"Preliminary report on floods on Boulder Creek below Boulder, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":68695,"text":"ha41 - 1961 - Floods at Boulder, Colorado","indexId":"ha41","publicationYear":"1961","noYear":false,"title":"Floods at Boulder, Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"ha41","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","title":"Floods at Boulder, Colorado","language":"ENGLISH","doi":"10.3133/ha41","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Floods at Boulder, Colorado: U.S. Geological Survey Hydrologic Atlas 41, 3 col. maps ;30 x 52 cm. on sheet 74 x 105 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/ha41.","productDescription":"3 col. maps ;30 x 52 cm. on sheet 74 x 105 cm. folded to 26 x 19 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":188615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90417,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"6000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e7097","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":534515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68664,"text":"ha11 - 1961 - Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","interactions":[],"lastModifiedDate":"2012-02-02T00:13:41","indexId":"ha11","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"11","title":"Precipitation, water loss, and runoff in the Delaware River basin and New Jersey","language":"ENGLISH","doi":"10.3133/ha11","usgsCitation":"Hely, A.G., Nordenson, T.J., and and others, 1961, Precipitation, water loss, and runoff in the Delaware River basin and New Jersey: U.S. Geological Survey Hydrologic Atlas 11, 1 map :illus., maps (part col.) ;69 cm., https://doi.org/10.3133/ha11.","productDescription":"1 map :illus., maps (part col.) ;69 cm.","costCenters":[],"links":[{"id":186048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad0e4b07f02db6808b8","contributors":{"authors":[{"text":"Hely, Allen Grant","contributorId":41902,"corporation":false,"usgs":true,"family":"Hely","given":"Allen","email":"","middleInitial":"Grant","affiliations":[],"preferred":false,"id":278668,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nordenson, T. J.","contributorId":95116,"corporation":false,"usgs":true,"family":"Nordenson","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":534512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":52156,"text":"ofr6128 - 1961 - Floods in Pennsylvania, frequency and magnitude","interactions":[],"lastModifiedDate":"2016-06-23T10:52:55","indexId":"ofr6128","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-28","title":"Floods in Pennsylvania, frequency and magnitude","docAbstract":"This report outlines a method of determining the magnitude of floods having frequencies up to 50 years for any stream in Pennsylvania except regulated streams and streams whose drainage basins are smaller than 10 square miles. On the main stems of the Schuylkill, Delaware, Susquehanna, and Chemung Rivers the magnitude of floods can be determined for frequencies up to 100 years.
\nSix composite frequency curves show the relation of the mean annual flood to floods having recurrence interval up to 50 to 100 years. Curves for fourteen hydrologic areas show the variation of mean annual flood with drainage area. This report explains how to select the proper curves for any chosen point in the State and how to compute a flood-frequency curve for that point.
\nA tabulation of peak gage heights and discharges for most gaging stations in the State is included. In general, the tabulations contain all peaks above a specific base discharge, although for some stations only annual peaks are shown.
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F.","contributorId":67968,"corporation":false,"usgs":true,"family":"Busch","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":244886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shaw, E.C.","contributorId":94737,"corporation":false,"usgs":true,"family":"Shaw","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":244887,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52183,"text":"ofr6180 - 1961 - Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","interactions":[],"lastModifiedDate":"2013-11-26T11:28:10","indexId":"ofr6180","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-80","title":"Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho","language":"English","doi":"10.3133/ofr6180","usgsCitation":"Jones, P., 1961, Hydrology of radioactive waste disposal at the Idaho Chemical Processing Plant National Reactor Testing Station, Idaho: U.S. Geological Survey Open-File Report 61-80, 8 p., https://doi.org/10.3133/ofr6180.","productDescription":"8 p.","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":176727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Idaho","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f22","contributors":{"authors":[{"text":"Jones, P.H.","contributorId":50963,"corporation":false,"usgs":true,"family":"Jones","given":"P.H.","email":"","affiliations":[],"preferred":false,"id":244923,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71752,"text":"tei796 - 1961 - Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","interactions":[],"lastModifiedDate":"2012-02-02T00:13:52","indexId":"tei796","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"796","title":"Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal","language":"ENGLISH","doi":"10.3133/tei796","usgsCitation":"Twenhofel, W., Moore, J.E., and Black, R.A., 1961, Preliminary evaluation of the seismicity, geology, and hydrology of the northern Sand Springs Range, Churchill County, Nevada, as a possible site for Project Shoal: U.S. Geological Survey Trace Elements Investigations 796, 21 p. : ill., maps ; 27 cm.; 10 figs.; 1 table, https://doi.org/10.3133/tei796.","productDescription":"21 p. : ill., maps ; 27 cm.; 10 figs.; 1 table","costCenters":[],"links":[{"id":191640,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/796/report-thumb.jpg"},{"id":90982,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/796/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c36b","contributors":{"authors":[{"text":"Twenhofel, William S.","contributorId":47876,"corporation":false,"usgs":true,"family":"Twenhofel","given":"William S.","affiliations":[],"preferred":false,"id":284704,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, John Ezra","contributorId":93582,"corporation":false,"usgs":true,"family":"Moore","given":"John","email":"","middleInitial":"Ezra","affiliations":[],"preferred":false,"id":284706,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Black, Rudolph Allen","contributorId":60724,"corporation":false,"usgs":true,"family":"Black","given":"Rudolph","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":284705,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":52228,"text":"ofr6228 - 1961 - Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","interactions":[],"lastModifiedDate":"2018-10-03T09:24:58","indexId":"ofr6228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"62-28","title":"Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions","docAbstract":"The Appalachian basin is an elongate depression in the crystalline basement complex which contains a great volume of predominantly sedimentary stratified rocks. As defined in this paper it extends from the Adirondack Mountains in New York to central Alabama. From east to west it extends from the west flank of the Blue Ridge Mountains to the crest of the Findlay and Cincinnati arches and the Nashville dome. It encompasses an area of about 207,000 square miles, including all of West Virginia and parts of New York, New Jersey, Pennsylvania, Ohio, Maryland, Virginia, Kentucky, Tennessee, North Carolina, Georgia, and Alabama.
The stratified rocks that occupy the basin constitute a wedge-shaped mass whose axis of greatest thickness lies close to and parallel to the east edge of the basin. The maximum thickness of stratified rocks preserved in any one part of the basin today is between 35,000 and 40,000 feet. The volume of the sedimentary rocks is approximately 510,000 cubic miles and of volcanic rocks is a few thousand cubic miles. The sedimentary rocks are predominantly Paleozoic in age, whereas the volcanic rocks are predominantly Late Precambrian.
On the basis of gross lithology the stratified rocks overlying the crystalline basement complex can be divided into nine vertically sequential units, which are designated \"sequences\" in this report. The boundaries between contiguous sequences do not necessarily coincide with the commonly recognized boundaries between systems or series. All sequences are grossly wedge shaped, being thickest along the eastern margin of the basin and thinnest along the western margin.
The lowermost unit the Late Precambrian stratified sequence is present only along part of the eastern margin of the basin, where it lies unconformably on the basement complex. It consists largely of volcanic tuffs and flows but contains some interbedded sedimentary rocks. The Late Precambrian sequence is overlain by the Early Cambrian clastic sequence. Where the older sequence is absent, the Early Cambrian sequence rests on the basement complex. Interbedded fine- to coarse-grained noncarbonate detrital rocks comprise the bulk of the sequence, but some volcanic and carbonate rocks are included. Next above is the Cambrian-Ordovician carbonate sequence which consists largely of limestone and dolomite. Some quartzose sandstone is present in the lower part in the western half of the basin, and much shale is present in the upper part in the southeast part of the basin. The next higher sequence is the Late Ordovician clastic sequence, which consists largely of shale, siltstone, and sandstone. Coarse-grained light-gray to red rocks are common in the sequence along the eastern side of the basin, whereas fine-grained dark-gray to black calcareous rocks are common along the west side. The Late Ordovician clastic sequence is overlain unconformably in many places by the Early Silurian clastic sequence. The latter comprises a relatively thin wedge of coarse-grained clastic rocks. Some of the most prolific oil- and gas-producing sandstones in the Appalachian basin are included. Among these are the \"Clinton\" sands of Ohio, the Medina Sandstones of New York and Pennsylvania, and the Keefer or \"Big Six\" Sandstone of West Virginia and Kentucky. Conformably overlying the Early Silurian clastic sequence is the Silurian-Devonian carbonate sequence, which consists predominantly of limestone and dolomite. It also contains a salt-bearing unit in the north-central part of the basin and a thick wedge of coarse-grained red beds in the northeastern part. The sequence is absent in much of the southern part of the basin. Large volumes of gas and much oil are obtained from some of its rocks, especially from the Oriskany Sandstone and the Huntersville Ghert. The Silurian-Devonian carbonate sequence is abruptly overlain by the Devonian clastic sequence a thick succession of interbedded shale, mudrock, siltstone, and sandstone. Colors range from predominantly purple and red in the northeastern part of the basin to predominantly dark gray and black in the southwestern part. Many rocks in the upper part contain hydrocarbons in commercial quantities. The next higher sequence is a heterogeneous succession that comprises most rocks of Mississippian age in the basin. It is composed largely of fine-grained to very coarse-grained noncalcareous clastic rocks in the northern half of the basin, and largely of carbonate rocks in the southern part. Large quantities of oil and gas are produced from the sequence. The youngest sequence consists of coarse-grained clastic rocks largely of Pennsylvanian age. In the center of the basin a relatively small volume of lithologically similar rocks of Permian age are included. The sequence has been intensively mined for coal throughout most of its extent.
The waste-disposal possibilities of the stratified rocks in the Appalachian basin are considered in terms of the following: 1) gross lithology of the sequences; 2) general lithology of the rock units composing the sequences; and 3) the structural attitudes of the sequences in different parts of the basin. The degree of exploitation of economically significant mineral* resources is considered briefly where such exploitation may affect waste-disposal possibilities. Hydrologic aspects are not in general considered. Based largely on consideration of the above geologic factors the following types of reservoirs associated with particular geologic environments offer some prospects for the disposal of radioactive waste solutions. They are: 1) artificially created cavities in thick salt beds; 2) artificially fractured thin lenticular sandstone bodies isolated in shale or mudrock sequences; 3) portions of thick noncarbonate clastic sequences possessing appreciable natural porosity and permeability; 4) thin clastic units (with natural or artificially created openings) in the plate of a thrust fault overlain by impermeable strata.
Considered in its entirety the Late Ordovician clastic sequence appears to have a greater number of favorable geologic factors for waste-disposal purposes than the others. The Early Silurian clastic sequence, the Silurian-Devonian carbonate sequence, and the Devonian clastic sequence offer fewer possibilities. The Late Precambrian stratified sequence, Early Cambrian, and the Cambrian-Ordovician carbonate sequence offer few possibilities. The Mississippian and Pennsylvanian sequences appear to be generally unsuitable.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr6228","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Colton, G.W., 1961, Geologic summary of the Appalachian Basin, with reference to the subsurface disposal of radioactive waste solutions: U.S. Geological Survey Open-File Report 62-28, Report: 121 p.; 15 Maps; 1 Illustration, https://doi.org/10.3133/ofr6228.","productDescription":"Report: 121 p.; 15 Maps; 1 Illustration","costCenters":[],"links":[{"id":86729,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86730,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":177170,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0028/report-thumb.jpg"},{"id":86731,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86732,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86733,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86734,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86735,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86736,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86737,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86738,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86739,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86740,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86741,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86742,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86743,"rank":414,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86744,"rank":415,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0028/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Appalachian Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.71,35.8 ], [ -84.71,43.91 ], [ -74.13,43.91 ], [ -74.13,35.8 ], [ -84.71,35.8 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688132","contributors":{"authors":[{"text":"Colton, George Willis","contributorId":12015,"corporation":false,"usgs":true,"family":"Colton","given":"George","email":"","middleInitial":"Willis","affiliations":[],"preferred":false,"id":244999,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57721,"text":"ofr61177 - 1961 - Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:12:12","indexId":"ofr61177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-177","title":"Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma","docAbstract":"Unconsolidated water-bearing alluvial deposits border the Canadian River in the vicinity of Norman, Oklahoma. These Quaternary materials are divided on the basis of topgraphic position into 'high terrace deposits' and 'alluvium.' The high terrace lies at an elevation of 50 to 60 feet above the alluvium, which in turn lies 7 to 15 feet above the channel of the Canadian River. Southwest of Norman a relatively thick section of these deposits occur as a hydrologic unit and overlie impermeable Permian shale. The high terrace deposits contain thick beds of clay, silt, and fine sand, whereas the alluvium contains a higher percentage of coarse sand and gravel.\r\nGround-water recharge is estimated to be 23 percent of the normal annual precipitation of 33.22 inches; the specific yield is about 15 percent, and the coefficient of permeability is about 1,000 gpd/ft2. Using these figures 17,000 acre-feet of water is computed to be in storage within the area acting as a hydrologic unit. About 3.6 million gallons of water is discharged daily from the high terrace deposits through a 16,000-foot section of alluvium having a saturated thickness of 40 feet along the river.\r\n\r\nThe quality of water in the high terrace deposits meets the standards of the U.S. Public Health Service for domestic water used by Interstate carriers but nitrate content of one well is higher than recommended by the Oklahoma Department of Public Health. Water in the alluvium is of poorer quality because the water is concentrated by evapotranspiration.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr61177","usgsCitation":"Stacy, B.L., 1961, Ground water in the alluvial deposits of the Canadian River valley near Norman, Oklahoma: U.S. Geological Survey Open-File Report 61-177, 61 p., https://doi.org/10.3133/ofr61177.","productDescription":"61 p.","costCenters":[],"links":[{"id":184149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d7fe","contributors":{"authors":[{"text":"Stacy, Bill L.","contributorId":99637,"corporation":false,"usgs":true,"family":"Stacy","given":"Bill","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":257637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68452,"text":"ha40 - 1961 - Floods at Mount Vernon, Ohio","interactions":[],"lastModifiedDate":"2022-04-29T20:48:06.30266","indexId":"ha40","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"40","title":"Floods at Mount Vernon, Ohio","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha40","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Floods at Mount Vernon, Ohio: U.S. Geological Survey Hydrologic Atlas 40, 1 Plate: 22.50 × 29.00 inches, https://doi.org/10.3133/ha40.","productDescription":"1 Plate: 22.50 × 29.00 inches","costCenters":[],"links":[{"id":186274,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":399951,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15782.htm"},{"id":89989,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"12000","country":"United States","state":"Ohio","city":"Mount Vernon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.517,\n 40.358\n ],\n [\n -82.45,\n 40.358\n ],\n [\n -82.45,\n 40.425\n ],\n [\n -82.517,\n 40.425\n ],\n [\n -82.517,\n 40.358\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df767","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":534511,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2307,"text":"wsp1475C - 1961 - Geology in relation to availability of water along the south rim, Grand Canyon National Park, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp1475C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1475","chapter":"C","title":"Geology in relation to availability of water along the south rim, Grand Canyon National Park, Arizona","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1475C","usgsCitation":"Metzger, D.G., 1961, Geology in relation to availability of water along the south rim, Grand Canyon National Park, Arizona: U.S. Geological Survey Water Supply Paper 1475, iv, 105-138 p. :ill., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1475C.","productDescription":"iv, 105-138 p. :ill., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":137716,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475c/report-thumb.jpg"},{"id":28130,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28131,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1475c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28132,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683ff9","contributors":{"authors":[{"text":"Metzger, Donald George","contributorId":36915,"corporation":false,"usgs":true,"family":"Metzger","given":"Donald","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":144985,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3204,"text":"wsp1591A - 1961 - Urban growth and the water regimen","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1591A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1591","chapter":"A","title":"Urban growth and the water regimen","docAbstract":"The continuing growth and concentration of population and industry in urban and suburban areas in recent decades has caused a complex merging of social, economic, and physical problems, The interrelationships of man and his use and development of the land and water resources is a particularly significant aspect of urbanization, but there has been relatively little study to date of the effect of urban man upon natural hydrologic conditions. \r\n\r\nAs urban man changes an area from one of field and forest to one of buildings and streets, he covers land where water once entered the soil, and thus creates or aggravates problems of drainage, including storm-water runoff. As he requires increasing amounts of water for home and factory, he drills deeper wells, and builds longer aqueducts and larger dams and reservoirs. As he disposes of un- wanted waste materials, he either treats them by using water or pollutes the receiving body of water. As he dredges and deepens coastal streams carrying salt water, and he pumps greater quantities of water from wells in coastal areas, he increases the likelihood of salt-water contamination. These and many other urban effects upon hydrology deserve increasing study if we are to provide for the best use of the water and land resources available to the Nation's urban centers.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1591A","usgsCitation":"Savini, J., and Kammerer, J., 1961, Urban growth and the water regimen: U.S. Geological Survey Water Supply Paper 1591, 1 v. (issued as seperate chapters) :ill. ;24 cm. ;43 p. , https://doi.org/10.3133/wsp1591A.","productDescription":"1 v. (issued as seperate chapters) :ill. ;24 cm. ;43 p. ","costCenters":[],"links":[{"id":138116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1591a/report-thumb.jpg"},{"id":30191,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1591a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30192,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1591a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f7e4b07f02db5f238b","contributors":{"authors":[{"text":"Savini, John","contributorId":67491,"corporation":false,"usgs":true,"family":"Savini","given":"John","email":"","affiliations":[],"preferred":false,"id":146428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammerer, J.C.","contributorId":24762,"corporation":false,"usgs":true,"family":"Kammerer","given":"J.C.","email":"","affiliations":[],"preferred":false,"id":146427,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3275,"text":"cir443 - 1961 - Availability of ground water in the Gallup area, New Mexico","interactions":[],"lastModifiedDate":"2013-07-29T14:45:31","indexId":"cir443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"443","title":"Availability of ground water in the Gallup area, New Mexico","docAbstract":"A thick succession of sedimentary rocks (about 6,000 feet) underlies the town of Gallup and crops out nearby. Although all the sedimentary rocks are capable of yielding some water, only a few units of sandstone and limestone yield water in sufficient quantity and of acceptable quality to be considered as sources of large supplies. The five stratigraphic units that are most productive of ground water form three aquifers, as follows: (a) the Glorieta sandstone and San Andres limestone, (b) the Westwater Canyon member of the Morrison formation and the Dakota sandstone, and (e) the Gallup sandstone. The Glorieta sandstone yields only small amounts of water to wells, except where it is intensely fractured. It probably contributes large amounts of water to the overlying, more permeable San Andres limestone by slow vertical leakage over large areas, as water is withdrawn from the San Andres. The San Andres limestone is discontinuous in the eastern part of the area, wedging out entirely a few miles east of Gallup. Its permeability varies widely because locally the permeability has been greatly increased by fractures and solution channels. On the north flank of the Zuni Mountains, near its outcrop, the San Andres yields as much as 1,100 gpm (gallons per minute) of water to wells. The specific capacity of wells that tap the aquifer formed by this Glorieta sandstone and San Andres limestone ranges from 0.1 to 29 gpm per foot of drawdown. \n\nIn general, the water in the Glorieta sandstone and San Andres limestone is hard, because it contains much calcium. Both bicarbonate and sulfate anions are abundant. The chemical quality of the water deteriorates with increasing distance from the outcrop. \n\nThe Westwater Canyon member of the Morrison formation and the Dakota sandstone form a single hydrologic unit extending from about 5 miles east of Gallup westward into Arizona. To the east they are separated by shale of the Brushy Basin member of the Morrison formation. The water-bearing properties of the Westwater Canyon member and the Dakota sandstone are ill defined, because few wells in the area tap either of them exclusively. The specific capacity of wells that tap the Westwater Canyon member, the Dakota sandstone, or both ranges from 0.02 to 2.3 gpm per foot of drawdown. \n\nWater in this aquifer generally contains less that 1,000 ppm (parts per million) of dissolved solids. The concentration of sodium and bicarbonate typically is high, and the concentration of sulfate is high locally. The Gallup sandstone is the principal aquifer in the immediate vicinity of, and to the north and south of, Gallup. It yields as much as 260 gpm of water to wells; the specific capacity of wells that tap the Gallup sandstone ranges from 0.08 to 4.7 gpm per foot of drawdown. In general, the water in the Gal]up sandstone is potable, although in places it yields water high in iron, sulfate, and dissolved solids; the concentration of dissolved solids generally is less than 1,000 ppm. \n\nBecause the yields of all the formations tested at Gallup are small, the town needs a better source of water. The San Juan River discharges annually a larger volume of water than is available from any other source in northwestern New Mexico. Gallup has applied for 15,000 acre-feet of San Juan River water a year, an average of 13,400,000 gpd (gallons per day). This water would be expensive, because about 50 miles of pipeline would be required to transport the water, and it would have to be liked about 1,000 feet over a high ridge north of town. \n\nDespite the expense involved, at this time the San Juan River seems to offer the most secure long-term supply of water for the Gallup area.","language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/cir443","collaboration":"Prepared in cooperation with the New Mexico State Engineer and the town of Gallup","usgsCitation":"West, S.W., 1961, Availability of ground water in the Gallup area, New Mexico: U.S. Geological Survey Circular 443, Report: iv, 21 p.; 1 Plate: 16.40 x 18.09 inches, https://doi.org/10.3133/cir443.","productDescription":"Report: iv, 21 p.; 1 Plate: 16.40 x 18.09 inches","numberOfPages":"26","costCenters":[],"links":[{"id":124367,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0443/report-thumb.jpg"},{"id":30272,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0443/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271084,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0443/plate-1.pdf"}],"country":"United States","state":"New Mexico","city":"Gallup","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.847,35.493 ], [ -108.847,35.55 ], [ -108.59,35.55 ], [ -108.59,35.493 ], [ -108.847,35.493 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d8c6","contributors":{"authors":[{"text":"West, Samuel Wilson","contributorId":24763,"corporation":false,"usgs":true,"family":"West","given":"Samuel","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":146559,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1761,"text":"wsp1532A - 1961 - Hydrologic effects of water spreading in Box Creek basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1532A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1532","chapter":"A","title":"Hydrologic effects of water spreading in Box Creek basin, Wyoming","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/wsp1532A","usgsCitation":"Hadley, R.F., and McQueen, I., 1961, Hydrologic effects of water spreading in Box Creek basin, Wyoming: U.S. Geological Survey Water Supply Paper 1532, iv, 47, [1] p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1532A.","productDescription":"iv, 47, [1] p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532a/report-thumb.jpg"},{"id":26874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606e92","contributors":{"authors":[{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":144100,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McQueen, I.S.","contributorId":59774,"corporation":false,"usgs":true,"family":"McQueen","given":"I.S.","email":"","affiliations":[],"preferred":false,"id":144101,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1705,"text":"wsp1475F - 1961 - Ground Water at Grant Village Site, Yellowstone National Park, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:06","indexId":"wsp1475F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1475","chapter":"F","title":"Ground Water at Grant Village Site, Yellowstone National Park, Wyoming","docAbstract":"On behalf of the National Park Service, the U.S. Geological Survey during the summer of 1959 made a study of ground-water conditions in the area of the Grant Village site, along the shore of the West Thumb of Yellowstone Lake, 1 to 2 miles south of the present facilities at West Thumb. The water supply for the present development at West Thumb is obtained from Duck Lake, but the quantity of water available from this source probably will be inadequate for the planned development at Grant Village.\r\n\r\nDuring the investigation, 11 auger holes were bored and 6 test wells were drilled. Aquifer tests by pumping and bailing methods were made at two of the test wells. All material penetrated in the auger holes and test wells is of Quaternary age except the welded tuff of possible Pliocene age that was penetrated in the lower part of test well 4.\r\n\r\nSmall to moderate quantities of water were obtained from the test wells in the area. Test well 2 yielded 35 gpm (gallons per minute) at a temperature of nearly 100 deg F. Test well 6 yielded about 15 gpm at a temperature of 48 deg F. The yield of this well might be increased by perforation of additional sections of casing, followed by further development of the well. Water from the other four test wells was of inadequate quantity, too highly mineralized, or too warm to be effectively utilized.\r\n\r\nMost of the ground water sampled had high concentrations of silica and iron, and part of the water was excessively high in fluoride content. Otherwise, the ground water was of generally suitable quality for most uses.\r\n\r\nThe most favorable area for obtaining water supplies from wells is near the lakeshore, where a large part of the water pumped would be ground-water flow diverted from its normal discharge into the lake. Moderate quantities of relatively cool water of fairly good quality may be available near the lakeshore between test wells 5 and 6 and immediately east of test well 6.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Hydrology of the Public Domain","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1475F","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Gordon, E.D., McCullough, R.A., and Weeks, E.P., 1961, Ground Water at Grant Village Site, Yellowstone National Park, Wyoming: U.S. Geological Survey Water Supply Paper 1475, 173-200 p., https://doi.org/10.3133/wsp1475F.","productDescription":"173-200 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":12519,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/wsp/1475-F/","linkFileType":{"id":5,"text":"html"}},{"id":137092,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475f/report-thumb.jpg"},{"id":26783,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.66666666666667,44.25 ], [ -110.66666666666667,44.5 ], [ -110.33333333333333,44.5 ], [ -110.33333333333333,44.25 ], [ -110.66666666666667,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abae4b07f02db671f58","contributors":{"authors":[{"text":"Gordon, Ellis D.","contributorId":12451,"corporation":false,"usgs":true,"family":"Gordon","given":"Ellis","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":143995,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McCullough, Richard A.","contributorId":78712,"corporation":false,"usgs":true,"family":"McCullough","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":143996,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":143994,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}