{"pageNumber":"6781","pageRowStart":"169500","pageSize":"25","recordCount":184858,"records":[{"id":1304,"text":"wsp1475D - 1961 - Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota","interactions":[],"lastModifiedDate":"2016-04-05T09:49:55","indexId":"wsp1475D","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":"D","title":"Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota","docAbstract":"<p>Jewel Cave National Monument occupies 2 square miles of a broad plateau of sedimentary rocks in western Custer County, S. Dak., and is at an altitude of about 5,400 feet above mean sea level. The sedimentary rocks that constitute the plateau range in age from Cambrian to Pennsylvanian. Rocks of Silurian and Devonian age are absent. The presence of rocks of Ordovician age has not been established definitely but they may be represented by 10 feet of sandstone directly beneath the Englewood limestone of Mississippian age. The sedimentary formations are underlain by schist of Precambrian age.</p>\n<p>Study of outcrops in the vicinity of the monument confirms the existence of a fault about 1,500 feet north of the entrance to Jewel Cave. The fault trends generally east-west across the monument and has a displacement of about 120 feet about 1 mile west of the entrance to the cave. The effect of the fault on the occurrence of ground water near the cave is not known. In addition to the spring that furnishes the present (1959) water supply for the facilities at Jewel Cave, three springs outside the monument were visited during the study. Combined yield of the 3 springs is less than 2 gpm (gallons per minute).</p>\n<p>A single test well indicates that the monument at the well site is underlain by 665 feet of limestone, dolomite, and sandstone of Paleozoic age and an undetermined thickness of quartzbiotite schist of Precambrian age. Pumping tests using a cylinder pump indicate that the test well is capable of producing 15 to 18 gpm for a short time from 2 zones of sandstone below the Englewood limestone. These sandstones are believed to present the best possibilities for development of a permanent water supply at the monument.</p>","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/wsp1475D","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Dyer, C., 1961, Geology and occurrence of ground water at Jewel Cave National Monument, South Dakota: U.S. Geological Survey Water Supply Paper 1475, 23 p., https://doi.org/10.3133/wsp1475D.","productDescription":"23 p.","startPage":"139","endPage":"157","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":137886,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1475d/report-thumb.jpg"},{"id":26336,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1475d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","otherGeospatial":"Jewel Cave National Monument","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.85478973388672,\n              43.71057158566884\n            ],\n            [\n              -103.85478973388672,\n              43.74381677850666\n            ],\n            [\n              -103.81153106689452,\n              43.74381677850666\n            ],\n            [\n              -103.81153106689452,\n              43.71057158566884\n            ],\n            [\n              -103.85478973388672,\n              43.71057158566884\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64986f","contributors":{"authors":[{"text":"Dyer, C.F.","contributorId":23917,"corporation":false,"usgs":true,"family":"Dyer","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":143533,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37042,"text":"naf64 - 1961 - Pelage and surface topography of the northern fur seal","interactions":[],"lastModifiedDate":"2012-02-02T00:10:00","indexId":"naf64","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":58,"text":"North American Fauna","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"64","title":"Pelage and surface topography of the northern fur seal","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Scheffer, V.B., 1961, Pelage and surface topography of the northern fur seal: North American Fauna 64, v, 206 p. illus., plates, diagrs., tables 23 cm.","productDescription":"v, 206 p. illus., plates, diagrs., tables 23 cm.","costCenters":[],"links":[{"id":22653,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.fwspubs.org/toc/nafa//64","linkFileType":{"id":5,"text":"html"}},{"id":164644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68893b","contributors":{"authors":[{"text":"Scheffer, Victor B.","contributorId":91548,"corporation":false,"usgs":true,"family":"Scheffer","given":"Victor","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":217400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33737,"text":"b1084H - 1961 - An evaluation of whole-order, 1/2-order, and 1/3-order reporting in semiquantitative spectrochemical analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:09:24","indexId":"b1084H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1084","chapter":"H","title":"An evaluation of whole-order, 1/2-order, and 1/3-order reporting in semiquantitative spectrochemical analysis","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/b1084H","usgsCitation":"Barnett, P.R., 1961, An evaluation of whole-order, 1/2-order, and 1/3-order reporting in semiquantitative spectrochemical analysis: U.S. Geological Survey Bulletin 1084, p. 183-206 :graphs ;24 cm., https://doi.org/10.3133/b1084H.","productDescription":"p. 183-206 :graphs ;24 cm.","costCenters":[],"links":[{"id":163415,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1084h/report-thumb.jpg"},{"id":61606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1084h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684829","contributors":{"authors":[{"text":"Barnett, Paul R.","contributorId":29801,"corporation":false,"usgs":true,"family":"Barnett","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":211853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38993,"text":"pp352C - 1961 - Effect of sediment characteristics on erosion and deposition in ephemeral-stream channels","interactions":[],"lastModifiedDate":"2012-02-02T00:10:14","indexId":"pp352C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"352","chapter":"C","title":"Effect of sediment characteristics on erosion and deposition in ephemeral-stream channels","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Erosion and sedimentation in a semiarid environment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp352C","usgsCitation":"Schumm, S.A., 1961, Effect of sediment characteristics on erosion and deposition in ephemeral-stream channels: U.S. Geological Survey Professional Paper 352, p. 31-70, https://doi.org/10.3133/pp352C.","productDescription":"p. 31-70","costCenters":[],"links":[{"id":120410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0352c/report-thumb.jpg"},{"id":66106,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0352c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625508","contributors":{"authors":[{"text":"Schumm, S. A.","contributorId":71957,"corporation":false,"usgs":true,"family":"Schumm","given":"S.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":220780,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39012,"text":"pp366 - 1961 - Ash-flow tuffs: Their origin, geologic relations, and identification","interactions":[],"lastModifiedDate":"2013-11-07T10:52:43","indexId":"pp366","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"366","title":"Ash-flow tuffs: Their origin, geologic relations, and identification","docAbstract":"Pyroclastic materials, which are interpreted as having been deposited by flowage as a suspension of ash in volcanic gas, are becoming widely recognized as major geologic episodes. These may be unconsolidated, indurated by partial welding, or welded into a compact rock. Many students are working on these materials and the interest in them is so widespread that need for a coordinated treatise on them has developed. This report deals with the history of the concept of their origin; gives detailed descriptions of their character and mode of occurrence; gives criteria for their recognition; and considers their distribution and consolidation.","language":"English","publisher":"United States Government Printing Office","doi":"10.3133/pp366","usgsCitation":"Ross, C., and Smith, R.L., 1961, Ash-flow tuffs: Their origin, geologic relations, and identification: U.S. Geological Survey Professional Paper 366, vi, 80 p., https://doi.org/10.3133/pp366.","productDescription":"vi, 80 p.","numberOfPages":"87","costCenters":[],"links":[{"id":172491,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0366/report-thumb.jpg"},{"id":268972,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0366/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672ba8","contributors":{"authors":[{"text":"Ross, Clarence S.","contributorId":7251,"corporation":false,"usgs":true,"family":"Ross","given":"Clarence S.","affiliations":[],"preferred":false,"id":220802,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Robert L.","contributorId":90803,"corporation":false,"usgs":true,"family":"Smith","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220803,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38970,"text":"pp424B - 1961 - Short papers in the geologic and hydrologic sciences; Articles 1-146","interactions":[],"lastModifiedDate":"2023-09-25T21:08:19.50785","indexId":"pp424B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"424","chapter":"B","title":"Short papers in the geologic and hydrologic sciences; Articles 1-146","docAbstract":"<p>The scientific and economic results of work by the United States Geological Survey during the fiscal year 1961, the 12 months ending June 30, 1961, will be summarized in four volumes of which this is the first. This volume includes 146 short papers on a variety of subjects in the fields of geology, hydrology, and related sciences, prepared by members of the Geologic, Water Resources, and Conservation Divisions of the Survey. These papers are of two kinds. Some are announcements of new discoveries or observations on problems of limited scope, which may or may not be described in greater detail subsequently. Others summarize conclusions drawn from more extensive or continuing investigations, which in large part will be described in greater detail in reports to be published at a· later date.</p><p>Professional Papers 424-C and -D include additional short papers of the same character as those in the present volume. Professional Paper 424-A provides a synopsis of the more important new findings resulting from work during the fiscal year.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1961 (Professional Paper 424)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp424B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1961, Short papers in the geologic and hydrologic sciences; Articles 1-146: U.S. Geological Survey Professional Paper 424, viii, 344 p., https://doi.org/10.3133/pp424B.","productDescription":"viii, 344 p.","numberOfPages":"352","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true},{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":336128,"rank":2,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424A","text":"Chapter A","linkHelpText":"Synopsis of geologic and hydrologic results"},{"id":113313,"rank":5,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0424b/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":173313,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0424b/report-thumb.jpg"},{"id":336129,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424C","text":"Chapter C","linkHelpText":"Articles 147-292"},{"id":336130,"rank":4,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.er.usgs.gov/publication/pp424D","text":"Chapter D","linkHelpText":"Articles 293-435"},{"id":421142,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_28432.htm","linkFileType":{"id":5,"text":"html"}}],"publicComments":"Scientific notes and summaries of investigations prepared by me1nbers of the Geologic, Water Resources, and Conservation Divisions in the fields of geology, hydrology, and allied sciences.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db648567","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":529898,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64812,"text":"i332 - 1961 - Geologic map of a part of southwestern Wyoming and adjacent States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:02","indexId":"i332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"332","subseriesTitle":"NONE","title":"Geologic map of a part of southwestern Wyoming and adjacent States","language":"ENGLISH","doi":"10.3133/i332","usgsCitation":"Bradley, W.H., 1961, Geologic map of a part of southwestern Wyoming and adjacent States: U.S. Geological Survey IMAP 332, 1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i332.","productDescription":"1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102824,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1290.htm","linkFileType":{"id":5,"text":"html"},"description":"1290"},{"id":187277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91442,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2a5d","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":272197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3411,"text":"cir439 - 1961 - Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","interactions":[],"lastModifiedDate":"2017-06-09T08:32:55","indexId":"cir439","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":"439","title":"Time of travel of water in the Ohio River, Pittsburgh to Cincinnati","docAbstract":"This report presents a procedure for estimating the time of travel of water in the Ohio River from Pittsburgh, Pa., to Cincinnati, Ohio, under various river stage conditions. This information is primarily for use by civil defense officials and by others concerned with problems involving travel time of river water. \r\n\r\nTables and charts are presented to show, for a particular stage or discharge at Cincinnati, the average time it would take for water to travel through the entire reach from Pittsburgh, or through successive intermediate segments of the reach. For example, when the discharge at Cincinnati is 200,000 cfs, travel time from Pittsburgh to Cincinnati, a distance of 470 miles, averages about 7 days; and for discharges of more than 200,000 cfs, the travel time decreases very slowly with increasing discharge. When the discharge is 30,000 cfs, travel time is about 28 days; and for discharges of less than 30,000 cfs, the travel time increases very rapidly with decreasing discharge. Estimates of travel time at low discharge are subject to large errors. Statistical analysis of the possible variations of upstream discharge for a given discharge at Cincinnati indicates that the shortest probable travel time from Pittsburgh to Cincinnati ranges from 56 percent of that under average conditions when the discharge at Cincinnati is 15,000 cfs to 93 percent of that under average conditions when the discharge at Cincinnati is 894,000 cfs. \r\n\r\nA chart showing the time distribution of flow at Cincinnati is presented so that the probable travel time of Ohio River water can be determined for any time of the year. This chart provides information which, when applied to the time-of-travel chart, shows that the most probable travel time of water from Pittsburgh to Cincinnati ranges from 160 hours in February to 1,250 hours in September. Also presented is a flow-duration curve that can be used to predict future discharges and, subsequently, times of travel, for use in long-range planning. The procedure used to compute time of travel is described in sufficient detail to make it usable as a guide for similar studies of other rivers that have deans and pools in the reach being studied. \r\n\r\nThe computations for the time-of-travel charts were made as follows: (a) by dividing the reach between Pittsburgh and Cincinnati into four subreaches with a full-range streamgaging station at or near the ends of each; (b) by computing for each subreach mean velocities corresponding to various discharges at Cincinnati, using data obtained from river survey maps and data available from gaging station operations; (c) by assuming that any mass of contaminated water would travel at a rate equal to that of the mean velocity of the river water.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir439","usgsCitation":"Steacy, R.E., 1961, Time of travel of water in the Ohio River, Pittsburgh to Cincinnati: U.S. Geological Survey Circular 439, iii, 14 p. :map, diagrs., tables. ;27cm., https://doi.org/10.3133/cir439.","productDescription":"iii, 14 p. :map, diagrs., tables. ;27cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":30428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0439/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0439/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Ohio River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.957275390625,\n              38.272688535980976\n            ],\n            [\n              -79.8046875,\n              38.272688535980976\n            ],\n            [\n              -79.8046875,\n              40.73893324113601\n            ],\n            [\n              -84.957275390625,\n              40.73893324113601\n            ],\n            [\n              -84.957275390625,\n              38.272688535980976\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48b6e4b07f02db533c35","contributors":{"authors":[{"text":"Steacy, Robert E.","contributorId":71162,"corporation":false,"usgs":true,"family":"Steacy","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146848,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3282,"text":"cir448 - 1961 - Reports and maps of the Geological Survey released only in the open files, 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:29","indexId":"cir448","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":"448","title":"Reports and maps of the Geological Survey released only in the open files, 1960","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir448","usgsCitation":"Weld, B., Asselstine, E.S., and Johnson, A., 1961, Reports and maps of the Geological Survey released only in the open files, 1960: U.S. Geological Survey Circular 448, 15 p. ;26 cm., https://doi.org/10.3133/cir448.","productDescription":"15 p. ;26 cm.","costCenters":[],"links":[{"id":126478,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0448/report-thumb.jpg"},{"id":30278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f42f","contributors":{"authors":[{"text":"Weld, Betsy A.","contributorId":68714,"corporation":false,"usgs":true,"family":"Weld","given":"Betsy A.","affiliations":[],"preferred":false,"id":146577,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Asselstine, Erwin S.","contributorId":104034,"corporation":false,"usgs":true,"family":"Asselstine","given":"Erwin","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146579,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Johnson, Arthur","contributorId":76720,"corporation":false,"usgs":true,"family":"Johnson","given":"Arthur","affiliations":[],"preferred":false,"id":146578,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3692,"text":"cir449 - 1961 - Preliminary estimate of water used in southeast river basins, 1960","interactions":[],"lastModifiedDate":"2018-01-02T20:09:44","indexId":"cir449","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":"449","title":"Preliminary estimate of water used in southeast river basins, 1960","docAbstract":"The estimated withdrawal use of water in the Southeast River Basins during 1960 was about 3,900 mgd exclusive of water used to develop waterpower and exclusive of water used by the Savannah River Plant of the U.S. Atomic Energy Commission. This estimated use amounts to 770 gallons per capita per day. \r\n\r\nWithdrawal use of water requires that the water be removed from the ground or diverted from a stream or lake. In this report the use is divided into four types: public supplies, rural, irrigation, and self-supplied industrial. An estimate of water used for waterpower is not included in this report. Consumptive use is the quantity of water discharged to the atmosphere or incorporated in the products of the process in which it was used. Only about 290 million of the 3,900 mgd withdrawn was consumed. \r\n\r\nOf the water withdrawn in 1960, 3,200 mgd was taken from surface sources and 710 mgd from underground sources. Withdrawal of water has increased 31 percent in South Carolina, Alabama, and Georgia since 1955. The use of saline water was almost three times as great in 1960 as in 1955.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir449","usgsCitation":"MacKichan, K.A., and Kammerer, J.C., 1961, Preliminary estimate of water used in southeast river basins, 1960: U.S. Geological Survey Circular 449, iii, 10 p. :map, tables. ;27 cm., https://doi.org/10.3133/cir449.","productDescription":"iii, 10 p. :map, tables. ;27 cm.","costCenters":[],"links":[{"id":30744,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0449/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0449/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c43a","contributors":{"authors":[{"text":"MacKichan, Kenneth Allen","contributorId":70372,"corporation":false,"usgs":true,"family":"MacKichan","given":"Kenneth","email":"","middleInitial":"Allen","affiliations":[],"preferred":false,"id":147418,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kammerer, John Craig","contributorId":90701,"corporation":false,"usgs":true,"family":"Kammerer","given":"John","email":"","middleInitial":"Craig","affiliations":[],"preferred":false,"id":147419,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4171,"text":"cir451 - 1961 - Floods of September 6, 1960, in eastern Puerto Rico","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"cir451","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":"451","title":"Floods of September 6, 1960, in eastern Puerto Rico","docAbstract":"The floods of September 6, 1960, were the greatest known on many streams in eastern Puerto Rico. There were 117 lives lost, 30 persons missing, and 136 injured. Total damage was estimated in excess of $7 million. Several thousand persons were forced from their homes by the floods as 484, houses were destroyed and more than 3,600 others were. damaged. All main highways and most secondary roads were impassable for a short period during the floods and damage to them was heavy. \r\n\r\nFollowing the passage of Hurricane Donna off the northeast coast, rains of very high intensity fell over parts of the eastern half of the island, beginning about 9 p.m. September 5. By dawn September 6, rains totaling more than 10 inches over a large area produced floods in every river basin from the Rio Grande de Manati eastward. Flood discharges on the Rio Humacao, Rio Turabo, and Rio Valenciano were the greatest known and rank high among the notable floods on streams that drain from 6 to ]5 square miles. \r\n\r\nAn outstanding feature of the floods was the unusually high magnitude of peak discharges--9 of the 24 peak discharges determined had Myers ratings greater than 80 percent.","language":"ENGLISH","publisher":"United States Government Printing Office,","doi":"10.3133/cir451","usgsCitation":"Barnes, H.H., and Bogart, D.B., 1961, Floods of September 6, 1960, in eastern Puerto Rico: U.S. Geological Survey Circular 451, 13 p. :ill. ;27 cm., https://doi.org/10.3133/cir451.","productDescription":"13 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":117874,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0451/report-thumb.jpg"},{"id":31280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0451/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df7ca","contributors":{"authors":[{"text":"Barnes, Harry Hawthorne","contributorId":64630,"corporation":false,"usgs":true,"family":"Barnes","given":"Harry","email":"","middleInitial":"Hawthorne","affiliations":[],"preferred":false,"id":148338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bogart, Dean Butler","contributorId":85157,"corporation":false,"usgs":true,"family":"Bogart","given":"Dean","email":"","middleInitial":"Butler","affiliations":[],"preferred":false,"id":148339,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3693,"text":"cir456 - 1961 - Estimated use of water in the United States, 1960","interactions":[],"lastModifiedDate":"2018-03-12T14:12:43","indexId":"cir456","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":"456","title":"Estimated use of water in the United States, 1960","docAbstract":"<p>The estimated overage withdrawal use of water in the United States during 1960 was almost 270,000 mgd (million gallons per day), exclusive of water used to develop water power. This estimated use amounts to about 1,500 gpd (galIons per day) per capita. An additional 2,000,000 mgd were used to develop waterpower.</p><p>Withdrawal use of water requires that the water be removed from the ground or diverted from a stream or lake. In this report the use is divided into five types: public supplies, rural, irrigation, self-supplied industrial, and waterpower. Consumptive use of water is the quantity discharged to the atmosphere or incorporated in the products of the process in which it was used. Only 61,000 mgd of the 270,000 mgd withdrawn was consumed.</p><p>Of the water withdrawn in 1960, 220,000 mgd (including irrigation conveyance losses) was taken from surface sources and 47,000 from underground sources. Withdrawal of water for uses other than waterpower has increased 12 percent since 1955. The amount of water used for generation of waterpower has! increased 33 percent since 1955. The use of saline water was almost twice as great in 1960 as in 1955.</p><p>The upper limit of our water supply is the average annual runoff, nearly 1,200,000 mgd. The supply in 1960 was depleted by 61,000 mgd, the amount of water consumed. However, a large part of the water withdrawn but not consumed was deteriorated in quality.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir456","usgsCitation":"MacKichan, K., and Kammerer, J., 1961, Estimated use of water in the United States, 1960: U.S. Geological Survey Circular 456, iii, 44 p., https://doi.org/10.3133/cir456.","productDescription":"iii, 44 p.","numberOfPages":"50","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":117668,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1961/0456/report-thumb.jpg"},{"id":30745,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1961/0456/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc71","contributors":{"authors":[{"text":"MacKichan, K.A.","contributorId":48163,"corporation":false,"usgs":true,"family":"MacKichan","given":"K.A.","affiliations":[],"preferred":false,"id":147421,"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":147420,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":19553,"text":"ofr6178 - 1961 - Glacier observations, Glacier National Park, Montana, 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:07:37","indexId":"ofr6178","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":"61-78","title":"Glacier observations, Glacier National Park, Montana, 1960","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/ofr6178","usgsCitation":"Johnson, A., 1961, Glacier observations, Glacier National Park, Montana, 1960: U.S. Geological Survey Open-File Report 61-78, iii, 15 p., [1] leaf of plates :ill. ;29 cm., https://doi.org/10.3133/ofr6178.","productDescription":"iii, 15 p., [1] leaf of plates :ill. ;29 cm.","costCenters":[],"links":[{"id":152371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a54b2","contributors":{"authors":[{"text":"Johnson, Arthur","contributorId":76720,"corporation":false,"usgs":true,"family":"Johnson","given":"Arthur","affiliations":[],"preferred":false,"id":181108,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71746,"text":"tei789 - 1961 - Geology of the 410 area, Nevada test site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:13:45","indexId":"tei789","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":"789","title":"Geology of the 410 area, Nevada test site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/tei789","usgsCitation":"Davis, R.E., 1961, Geology of the 410 area, Nevada test site, Nye County, Nevada: U.S. Geological Survey Trace Elements Investigations 789, 25 p. : ill., maps ; 27 cm.; 2 figs. (1 in pocket); 1 table, https://doi.org/10.3133/tei789.","productDescription":"25 p. : ill., maps ; 27 cm.; 2 figs. (1 in pocket); 1 table","costCenters":[],"links":[{"id":186241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/789/report-thumb.jpg"},{"id":90978,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/789/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90979,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/789/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db6834fe","contributors":{"authors":[{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":284695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66188,"text":"i339 - 1961 - Geologic map of the Goodnews quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:17","indexId":"i339","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"339","subseriesTitle":"NONE","title":"Geologic map of the Goodnews quadrangle, Alaska","language":"ENGLISH","doi":"10.3133/i339","usgsCitation":"Hoare, J., and Coonrad, W.L., 1961, Geologic map of the Goodnews quadrangle, Alaska: U.S. Geological Survey IMAP 339, 1 map., https://doi.org/10.3133/i339.","productDescription":"1 map.","costCenters":[],"links":[{"id":102849,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1315.htm","linkFileType":{"id":5,"text":"html"},"description":"1315"},{"id":188476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -162,59 ], [ -162,60 ], [ -159,60 ], [ -159,59 ], [ -162,59 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69863c","contributors":{"authors":[{"text":"Hoare, J. M.","contributorId":52143,"corporation":false,"usgs":true,"family":"Hoare","given":"J. M.","affiliations":[],"preferred":false,"id":274128,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Coonrad, W. L.","contributorId":69946,"corporation":false,"usgs":true,"family":"Coonrad","given":"W.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":274129,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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