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1960 - Generalized geologic map of the Nelchina area, Alaska, showing igneous rocks and larger faults","interactions":[],"lastModifiedDate":"2012-02-10T00:10:57","indexId":"i312","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"312","subseriesTitle":"NONE","title":"Generalized geologic map of the Nelchina area, Alaska, showing igneous rocks and larger faults","language":"ENGLISH","doi":"10.3133/i312","usgsCitation":"Grantz, A., 1960, Generalized geologic map of the Nelchina area, Alaska, showing igneous rocks and larger faults: U.S. Geological Survey IMAP 312, 1 map., https://doi.org/10.3133/i312.","productDescription":"1 map.","costCenters":[],"links":[{"id":102798,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1262.htm","linkFileType":{"id":5,"text":"html"},"description":"1262"},{"id":187237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"96000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -148.13333333333333,61.75 ], [ -148.13333333333333,62.31722222222223 ], [ -147,62.31722222222223 ], [ -147,61.75 ], [ -148.13333333333333,61.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af1ed","contributors":{"authors":[{"text":"Grantz, Arthur agrantz@usgs.gov","contributorId":2585,"corporation":false,"usgs":true,"family":"Grantz","given":"Arthur","email":"agrantz@usgs.gov","affiliations":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":273872,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":16458,"text":"ofr60151 - 1960 - Selected logs of borings on the east side of San Francisco Bay, California","interactions":[],"lastModifiedDate":"2012-02-02T00:07:16","indexId":"ofr60151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-151","title":"Selected logs of borings on the east side of San Francisco Bay, California","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr60151","usgsCitation":"Weaver, M.A., and Radbruch, D.H., 1960, Selected logs of borings on the east side of San Francisco Bay, California: U.S. Geological Survey Open-File Report 60-151, 465 p. :map ;29 cm., https://doi.org/10.3133/ofr60151.","productDescription":"465 p. :map ;29 cm.","costCenters":[],"links":[{"id":150200,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a04e4b07f02db5f8594","contributors":{"authors":[{"text":"Weaver, Mary A.","contributorId":85611,"corporation":false,"usgs":true,"family":"Weaver","given":"Mary","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":172884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Radbruch, Dorothy H.","contributorId":65874,"corporation":false,"usgs":true,"family":"Radbruch","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":172883,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":13580,"text":"ofr6051 - 1960 - Surficial geology of the Hope Valley quadrangle, Rhode Island","interactions":[{"subject":{"id":13580,"text":"ofr6051 - 1960 - Surficial geology of the Hope Valley quadrangle, Rhode Island","indexId":"ofr6051","publicationYear":"1960","noYear":false,"title":"Surficial geology of the Hope Valley quadrangle, Rhode Island"},"predicate":"SUPERSEDED_BY","object":{"id":63062,"text":"gq166 - 1962 - Surficial geology of the Hope Valley quadrangle, Rhode Island","indexId":"gq166","publicationYear":"1962","noYear":false,"title":"Surficial geology of the Hope Valley quadrangle, Rhode Island"},"id":1}],"supersededBy":{"id":63062,"text":"gq166 - 1962 - Surficial geology of the Hope Valley quadrangle, Rhode Island","indexId":"gq166","publicationYear":"1962","noYear":false,"title":"Surficial geology of the Hope Valley quadrangle, Rhode Island"},"lastModifiedDate":"2012-02-02T00:06:52","indexId":"ofr6051","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"60-51","title":"Surficial geology of the Hope Valley quadrangle, Rhode Island","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6051","usgsCitation":"Feininger, T.G., 1960, Surficial geology of the Hope Valley quadrangle, Rhode Island: U.S. Geological Survey Open-File Report 60-51, 34 p. ill., folded map ;27 cm., https://doi.org/10.3133/ofr6051.","productDescription":"34 p. ill., folded map ;27 cm.","costCenters":[],"links":[{"id":147250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688aa5","contributors":{"authors":[{"text":"Feininger, Tomas Gustaf","contributorId":38577,"corporation":false,"usgs":true,"family":"Feininger","given":"Tomas","email":"","middleInitial":"Gustaf","affiliations":[],"preferred":false,"id":168058,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2859,"text":"wsp1455A - 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Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1487","title":"Geology and ground-water resources of the lower Little Bighorn River Valley, Big Horn County, Montana, with special reference to the drainage of waterlogged lands","docAbstract":"The lower Little Bighorn River valley, Montana, is in the unglaciated part of the Missouri Plateau section of the Great Plains physiographic province. The river and its principal tributaries rise in the Bighorn Mountains, and the confluence of this northward-flowing stream with the Bighorn River is near the east edge of Hardin, Mont. The normal annual precipitation ranges from about 12 inches in the northern part of the area to 15 inches in the southern part. The economy of the area is founded principally on farming, much of the low-lying land adjacent to the river being irrigated. The irrigated land is within the Crow Indian Reservation, although a part is privately owned. The bedrock formations exposed in the area are of Cretaceous age and include the Parkman sandstone, Claggett shale, Eagle sandstone, Telegraph Creek shale, and Cody shale. The Cloverly formation, Tensleep sandstone, and Madison limestone, which underlie but are not exposed in the area, and the Parkman sandstone in the southern half of the area appear to be the principal bedrock aquifers. All except the Parkman lie at depths ranging from a few feet to several thousand feet, and all appear to be capable of yielding water in commercial quantities. Some of the other formations arc capable of yielding enough water for domestic and stock needs. The river alluvium of Recent age and the Pleistocene terrace deposits are the principal unconsolidated formations in the area with respect to water supply and drainage. Wells yielding as much as 100 gallons per minute may be developed in favorable areas. Pumping tests reveal that the transmissibility of the coarser unconsolidated materials probably ranges from about 15,000 to 30,000 gallons per day per foot. Two tests of the Parkman sandstone showed transmissibilities of 6,000 and 20,000 gallons per day per foot. Although a test of the Cloverly formation showed a transmissibility of only 3,000 gallons per day per foot, the high artesian pressure--80 pounds per square inch at the land surface--in the Cloverly caused the tested well to yield about 200 gallons per minute by natural flow; this is greater than the yield of any other single well in the area. Textural properties were compared with the hydraulic properties determined by laboratory tests to show the relation between different types of waterbearing materials. Materials classified as heavy soils-normally somewhat dense and impervious-had an average permeability of 7.2 gallons per day per square foot, which was more than expected. One sample of very coarse alluvial material had a permeability of 6,000 gallons per day per square foot. The depth to water beneath irrigation units was mapped, thus showing the waterlogged areas. Waterlogging is not a serious problem where the water table is more than 6 feet below the land surface. For the drainage studies the unconsolidated deposits are classified in two zones-coarse-grained sediments resting on the relatively impermeable bedrock floor and overlying fine-grained sediments which extend to the land surface. The transmissibility of the coarse-sediment zone generally is many times greater than that of the fine-sediment zone. Because in many places drains could not be economically dug deep enough to enter the coarse zone, the study of the effectiveness of drainage completed in the fine zone received much attention. The studies showed that, despite a considerable thickness of fine-grained sediments between the bottom of the drain and the top of the coarse zone, drainage ditches frequently were effective in relieving waterlogging of fields nearby. Pilot relief wells installed in existing drains showed that the effectiveness of some drains could be increased appreciably by installing a series of relief wells. Records of fluctuations of water levels in 196 observation wells and water-level contour maps were studied to show the principal areas of recharge and discharge in the irrigable areas.
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A.","contributorId":78719,"corporation":false,"usgs":true,"family":"Moulder","given":"E.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145043,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Klug, M. F.","contributorId":97372,"corporation":false,"usgs":true,"family":"Klug","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":145044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Morris, D. A.","contributorId":56204,"corporation":false,"usgs":true,"family":"Morris","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145041,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Swenson, F. A.","contributorId":71622,"corporation":false,"usgs":true,"family":"Swenson","given":"F.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":145042,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Krieger, R. A.","contributorId":11202,"corporation":false,"usgs":true,"family":"Krieger","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145040,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":3053,"text":"wsp1636 - 1960 - Surface water supply of the United States, 1959, Part 12, Pacific slope basins in Washington and upper Columbia River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1636","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1636","title":"Surface water supply of the United States, 1959, Part 12, Pacific slope basins in Washington and upper Columbia River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1636","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 12, Pacific slope basins in Washington and upper Columbia River Basin: U.S. Geological Survey Water Supply Paper 1636, x, 402 p. :tables ;23 cm., https://doi.org/10.3133/wsp1636.","productDescription":"x, 402 p. :tables ;23 cm.","costCenters":[],"links":[{"id":139334,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1636/report-thumb.jpg"},{"id":29907,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1636/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6943ca","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146211,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3052,"text":"wsp1633 - 1960 - Surface water supply of the United States, 1959, Part 9, Colorado River Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:36","indexId":"wsp1633","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1633","title":"Surface water supply of the United States, 1959, Part 9, Colorado River Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1633","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 9, Colorado River Basin: U.S. Geological Survey Water Supply Paper 1633, xi, 506 p. :tables ;23 cm., https://doi.org/10.3133/wsp1633.","productDescription":"xi, 506 p. :tables ;23 cm.","costCenters":[],"links":[{"id":139333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1633/report-thumb.jpg"},{"id":29906,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1633/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db694361","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146210,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2840,"text":"wsp1481 - 1960 - Geology and ground-water resources of the Winter Garden district, Texas, 1948","interactions":[],"lastModifiedDate":"2016-08-22T10:51:28","indexId":"wsp1481","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1481","title":"Geology and ground-water resources of the Winter Garden district, Texas, 1948","docAbstract":"The Winter Garden district, as described in this report, includes all of Dimmit and Zavala Counties and the eastern part of Maverick County a total of about 3,200 square miles. The fleldwork for the investigation was completed in 1948.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1481","usgsCitation":"Turner, S.F., Robinson, T.W., and White, W.N., 1960, Geology and ground-water resources of the Winter Garden district, Texas, 1948: U.S. Geological Survey Water Supply Paper 1481, Report: v, 247 p.; 4 Plates: 24.50 x 31.13 inches or smaller, https://doi.org/10.3133/wsp1481.","productDescription":"Report: v, 247 p.; 4 Plates: 24.50 x 31.13 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1481/report-thumb.jpg"},{"id":29406,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29407,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29408,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29409,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1481/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29410,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1481/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685323","contributors":{"authors":[{"text":"Turner, Samuel Foster","contributorId":26287,"corporation":false,"usgs":true,"family":"Turner","given":"Samuel","email":"","middleInitial":"Foster","affiliations":[],"preferred":false,"id":145884,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, T. W.","contributorId":82285,"corporation":false,"usgs":true,"family":"Robinson","given":"T.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":145886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2930,"text":"wsp1569 - 1960 - Surface water supply of Hawaii, 1956-58","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"wsp1569","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1569","title":"Surface water supply of Hawaii, 1956-58","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1569","usgsCitation":"Wells, J.V., 1960, Surface water supply of Hawaii, 1956-58: U.S. Geological Survey Water Supply Paper 1569, vii, 295 p. ;24 cm., https://doi.org/10.3133/wsp1569.","productDescription":"vii, 295 p. ;24 cm.","costCenters":[],"links":[{"id":139017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1569/report-thumb.jpg"},{"id":29639,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1569/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69769a","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. B.","affiliations":[],"preferred":false,"id":146016,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3194,"text":"wsp1541B - 1960 - Double-mass curves, with a section fitting curves to cyclic data","interactions":[],"lastModifiedDate":"2019-03-27T07:59:56","indexId":"wsp1541B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1541","chapter":"B","title":"Double-mass curves, with a section fitting curves to cyclic data","docAbstract":"The double.-mass curve is used to check the consistency of many kinds of hydrologic data by comparing data for a single station with that of a pattern composed of the data from several other stations in the area The double-mass curve can be used to adjust inconsistent precipitation data. \r\n\r\nThe graph of the cumulative data of one variable versus the cumulative data of a related variable is a straight line so long as the relation between the variables is a fixed ratio. Breaks in the double-mass curve of such variables are caused by changes in the relation between the variables. These changes may be due to changes in the method of data collection or to physical changes that affect the relation. \r\n\r\nApplications of the double-mass curve to precipitation, streamflow, and sediment data, and to precipitation-runoff relations are described. A statistical test for significance of an apparent break in the slope of the double-mass curve is described by an example. Poor correlation between the variables can prevent detection of inconsistencies in a record, but an increase in the length of record tends to offset the effect of poor correlation. \r\n\r\nThe residual-mass curve, which is a modification of the double-mass curve, magnifies imperceptible breaks in the double-mass curve for detailed study. Of the several methods of fitting a smooth curve to cyclic or periodic data, the moving-arc method and the double-integration method deserve greater use in hydrology. Both methods are described in this manual. The moving-arc method has general applicability, and the double integration method is useful in fitting a curve to cycles of sinusoidal form.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1541B","usgsCitation":"Searcy, J., Hardison, C.H., and Langbein, W., 1960, Double-mass curves, with a section fitting curves to cyclic data: U.S. Geological Survey Water Supply Paper 1541, iv, 36 p., https://doi.org/10.3133/wsp1541B.","productDescription":"iv, 36 p.","startPage":"31","endPage":"66","numberOfPages":"41","costCenters":[],"links":[{"id":138111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1541b/report-thumb.jpg"},{"id":30179,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1541b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db496791","contributors":{"authors":[{"text":"Searcy, James K.","contributorId":44519,"corporation":false,"usgs":true,"family":"Searcy","given":"James K.","affiliations":[],"preferred":false,"id":146412,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardison, Clayton H.","contributorId":46073,"corporation":false,"usgs":true,"family":"Hardison","given":"Clayton","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":146413,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langbein, Walter B.","contributorId":98294,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter B.","affiliations":[],"preferred":false,"id":759856,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":3195,"text":"wsp1541C - 1960 - Graphical correlation of gaging-station records","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp1541C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1541","chapter":"C","title":"Graphical correlation of gaging-station records","docAbstract":"A gaging-station record is a sample of the rate of flow of a stream at a given site. This sample can be used to estimate the magnitude and distribution of future flows if the record is long enough to be representative of the long-term flow of the stream. The reliability of a short-term record for estimating future flow characteristics can be improved through correlation with a long-term record. Correlation can be either numerical or graphical, but graphical correlation of gaging-station records has several advantages. \r\n\r\nThe graphical correlation method is described in a step-by-step procedure with an illustrative problem of simple correlation, illustrative problems of three examples of multiple correlation--removing seasonal effect--and two examples of correlation of one record with two other records. Except in the problem on removal of seasonal effect, the same group of stations is used in the illustrative problems. The purpose of the problems is to illustrate the method--not to show the improvement that can result from multiple correlation as compared with simple correlation. \r\n\r\nHydrologic factors determine whether a usable relation exists between gaging-station records. Statistics is only a tool for evaluating and using an existing relation, and the investigator must be guided by a knowledge of hydrology.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1541C","usgsCitation":"Searcy, J., 1960, Graphical correlation of gaging-station records: U.S. Geological Survey Water Supply Paper 1541, 1 v.(Issued as three seperate chapters) :ill. ;24 cm. ;67-100 p., https://doi.org/10.3133/wsp1541C.","productDescription":"1 v.(Issued as three seperate chapters) :ill. ;24 cm. ;67-100 p.","costCenters":[],"links":[{"id":138112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1541c/report-thumb.jpg"},{"id":30180,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1541c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db6723b4","contributors":{"authors":[{"text":"Searcy, James K.","contributorId":44519,"corporation":false,"usgs":true,"family":"Searcy","given":"James K.","affiliations":[],"preferred":false,"id":146415,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3324,"text":"cir427 - 1960 - A field instrument for quantitative determination of beryllium by activation analysis","interactions":[],"lastModifiedDate":"2018-01-02T20:38:35","indexId":"cir427","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"427","title":"A field instrument for quantitative determination of beryllium by activation analysis","docAbstract":"A low-cost instrument has been developed for quantitative determinations of beryllium in the field by activation analysis. The instrument makes use of the gamma-neutron reaction between gammas emitted by an artificially radioactive source (Sb124) and beryllium as it occurs in nature. The instrument and power source are mounted in a panel-type vehicle. Samples are prepared by hand-crushing the rock to approximately ?-inch mesh size and smaller. Sample volumes are kept constant by means of a standard measuring cup. Instrument calibration, made by using standards of known BeO content, indicates the analyses are reproducible and accurate to within ? 0.25 percent BeO in the range from 1 to 20 percent BeO with a sample counting time of 5 minutes. Sensitivity of the instrument maybe increased somewhat by increasing the source size, the sample size, or by enlarging the cross-sectional area of the neutron-sensitive phosphor normal to the neutron flux.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir427","usgsCitation":"Vaughn, W., Wilson, E., and Ohm, J., 1960, A field instrument for quantitative determination of beryllium by activation analysis: U.S. Geological Survey Circular 427, 9 p. :illus. ;27cm., https://doi.org/10.3133/cir427.","productDescription":"9 p. :illus. ;27cm.","costCenters":[],"links":[{"id":30333,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1960/0427/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1960/0427/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec8d","contributors":{"authors":[{"text":"Vaughn, William W.","contributorId":107267,"corporation":false,"usgs":true,"family":"Vaughn","given":"William W.","affiliations":[],"preferred":false,"id":146669,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, E.E.","contributorId":68299,"corporation":false,"usgs":true,"family":"Wilson","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":146667,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ohm, J.M.","contributorId":83508,"corporation":false,"usgs":true,"family":"Ohm","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":146668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2959,"text":"wsp1629 - 1960 - Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","interactions":[],"lastModifiedDate":"2012-02-02T00:05:39","indexId":"wsp1629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1960","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":"1629","title":"Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1629","usgsCitation":"Wells, J.V., 1960, Surface water supply of the United States, 1959, Part 6-A, Missouri River Basin above Sioux City, Iowa: U.S. Geological Survey Water Supply Paper 1629, x, 415 p. :ill., tables ;25 cm., https://doi.org/10.3133/wsp1629.","productDescription":"x, 415 p. :ill., tables ;25 cm.","costCenters":[],"links":[{"id":139282,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1629/report-thumb.jpg"},{"id":29668,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1629/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69437f","contributors":{"authors":[{"text":"Wells, J. V. B.","contributorId":57037,"corporation":false,"usgs":true,"family":"Wells","given":"J.","email":"","middleInitial":"V. 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