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,{"id":2027,"text":"wsp1586J - 1972 - Tracer simulation study of potential solute movement in Port Royal Sound, South Carolina","interactions":[],"lastModifiedDate":"2019-12-30T09:39:10","indexId":"wsp1586J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"1586","chapter":"J","title":"Tracer simulation study of potential solute movement in Port Royal Sound, South Carolina","docAbstract":"A tracer study was conducted in Port Royal Sound to simulate the movement and ultimate pattern of concentration of a solute continuously injected into the flow. A total of 750 pounds of Rhodamine WT dye was injected by boat during a period of 24.8 hours in a line across the Colleton River. During the following 43 days, samples of water were taken at selected points in the sound, and the concentration of dye in the samples was determined by fluorometric analysis. \r\n\r\nThe data obtained in the field study were used with theoretical models to compute the ultimate pattern of concentration of nonconservative and conservative solutes for a hypothetical continuous injection at the site on the Colleton River.","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1586J","usgsCitation":"Kilpatrick, F.A., and Cummings, T.R., 1972, Tracer simulation study of potential solute movement in Port Royal Sound, South Carolina: U.S. Geological Survey Water Supply Paper 1586, iv, 27 p. , https://doi.org/10.3133/wsp1586J.","productDescription":"iv, 27 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":27500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137629,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586j/report-thumb.jpg"}],"country":"United States","state":"South Carolina","otherGeospatial":"Port Royal Sound","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -80.9637451171875,\n              32.16166284018013\n            ],\n            [\n              -80.321044921875,\n              32.16166284018013\n            ],\n            [\n              -80.321044921875,\n              32.648625783736726\n            ],\n            [\n              -80.9637451171875,\n              32.648625783736726\n            ],\n            [\n              -80.9637451171875,\n              32.16166284018013\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4de4b07f02db6271d5","contributors":{"authors":[{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144550,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cummings, T. Ray","contributorId":20722,"corporation":false,"usgs":true,"family":"Cummings","given":"T.","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":144549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12558,"text":"ofr7221 - 1972 - Tabulated gravity data from southeastern Alaska obtained during the 1969 field season","interactions":[],"lastModifiedDate":"2023-09-28T20:08:27.967524","indexId":"ofr7221","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-21","title":"Tabulated gravity data from southeastern Alaska obtained during the 1969 field season","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr7221","usgsCitation":"Barnes, D., Popenoe, P., Olson, R.C., MacKenzie, M., and Morin, R.L., 1972, Tabulated gravity data from southeastern Alaska obtained during the 1969 field season: U.S. 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,{"id":12557,"text":"ofr7220 - 1972 - Tabulated gravity data from southeastern Alaska obtained during the 1968 field season","interactions":[],"lastModifiedDate":"2013-08-01T15:29:54","indexId":"ofr7220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-20","title":"Tabulated gravity data from southeastern Alaska obtained during the 1968 field season","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr7220","usgsCitation":"Barnes, D., Olson, R., Holden, K.D., Morin, R.L., and Erwin, M., 1972, Tabulated gravity data from southeastern Alaska obtained during the 1968 field season: U.S. Geological Survey Open-File Report 72-20, 76 leaves ;21 x 27 cm., https://doi.org/10.3133/ofr7220.","productDescription":"76 leaves ;21 x 27 cm.","costCenters":[],"links":[{"id":111707,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0020/report.pdf","linkFileType":{"id":5,"text":"html"}},{"id":145397,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0020/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a25e4b07f02db60ee17","contributors":{"authors":[{"text":"Barnes, David F.","contributorId":72787,"corporation":false,"usgs":true,"family":"Barnes","given":"David F.","affiliations":[],"preferred":false,"id":166329,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olson, R.C.","contributorId":42596,"corporation":false,"usgs":true,"family":"Olson","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":166328,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Holden, K. D.","contributorId":30597,"corporation":false,"usgs":true,"family":"Holden","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":166327,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morin, R. L.","contributorId":95484,"corporation":false,"usgs":true,"family":"Morin","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":166330,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Erwin, M.J.","contributorId":95485,"corporation":false,"usgs":true,"family":"Erwin","given":"M.J.","email":"","affiliations":[],"preferred":false,"id":166331,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":2991,"text":"wsp1532F - 1972 - Appraisal of stream sedimentation in the Susquehanna River basin","interactions":[{"subject":{"id":55882,"text":"ofr68330 - 1968 - Preliminary appraisal of stream sedimentation in the Susquehanna River basin","indexId":"ofr68330","publicationYear":"1968","noYear":false,"title":"Preliminary appraisal of stream sedimentation in the Susquehanna River basin"},"predicate":"SUPERSEDED_BY","object":{"id":2991,"text":"wsp1532F - 1972 - Appraisal of stream sedimentation in the Susquehanna River basin","indexId":"wsp1532F","publicationYear":"1972","noYear":false,"chapter":"F","title":"Appraisal of stream sedimentation in the Susquehanna River basin"},"id":1}],"lastModifiedDate":"2017-06-07T11:20:20","indexId":"wsp1532F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"F","title":"Appraisal of stream sedimentation in the Susquehanna River basin","docAbstract":"<p>The Susquehanna River presently transports about 3.0 million tons of sediment annually (110 tons per square mile). Only about 1.8 million tons of sediment enters the head of Chesapeake Bay annually because some sediment is trapped behind the power dams on the lower Susquehanna. Measured annual sediment yields from subbasins in the Susquehanna range from 40 to 440 tons per square mile. The highest yields are from parts of the glaciated section of the basin, in the anthracite coal region, and the Piedmont province. The lowest yields are from parts of the glaciated section of the basin and the Appalachian high plateau. Available data indicate that there has been a downward trend of sediment discharge in recent years. In the future, the high sediment yields associated with urbanization may offset this present downward trend.</p>","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp1532F","usgsCitation":"Williams, K.F., and Reed, L.A., 1972, Appraisal of stream sedimentation in the Susquehanna River basin: U.S. Geological Survey Water Supply Paper 1532, iv, 24 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1532F.","productDescription":"iv, 24 p. :ill. ;24 cm.","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":29764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1532f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139391,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1532f/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Susquehanna 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,{"id":56429,"text":"wdrAK711 - 1972 - Water resources data for Alaska, water year 1971","interactions":[],"lastModifiedDate":"2012-02-02T00:12:17","indexId":"wdrAK711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AK-71-1","title":"Water resources data for Alaska, water year 1971","language":"ENGLISH","doi":"10.3133/wdrAK711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Alaska, water year 1971: U.S. Geological Survey Water Data Report AK-71-1, 328 p., https://doi.org/10.3133/wdrAK711.","productDescription":"328 p.","costCenters":[],"links":[{"id":185004,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f7997","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":532610,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56486,"text":"wdrCO711 - 1972 - Water resources data for Colorado, water year 1971; Part 1, Surface water records","interactions":[],"lastModifiedDate":"2012-02-02T00:11:59","indexId":"wdrCO711","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"CO-71-1","title":"Water resources data for Colorado, water year 1971; Part 1, Surface water records","language":"ENGLISH","doi":"10.3133/wdrCO711","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Colorado, water year 1971; Part 1, Surface water records: U.S. Geological Survey Water Data Report CO-71-1, 425 p., https://doi.org/10.3133/wdrCO711.","productDescription":"425 p.","costCenters":[],"links":[{"id":181115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1971/co-71-1/report-thumb.jpg"},{"id":88133,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1971/co-71-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49ffe4b07f02db5f75c7","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":532667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6372,"text":"pp741 - 1972 - The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data","interactions":[],"lastModifiedDate":"2012-02-02T00:05:42","indexId":"pp741","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"741","title":"The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp741","usgsCitation":"Rowe, J.J., Morey, G.W., and Zen, C., 1972, The quinary reciprocal salt system Na, K, Mg, Ca/Cl, SO4; a review of the literature with new data: U.S. Geological Survey Professional Paper 741, 37 p., https://doi.org/10.3133/pp741.","productDescription":"37 p.","costCenters":[],"links":[{"id":117540,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0741/report-thumb.jpg"},{"id":33746,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0741/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a70e4b07f02db641223","contributors":{"authors":[{"text":"Rowe, Jack James","contributorId":73583,"corporation":false,"usgs":true,"family":"Rowe","given":"Jack","email":"","middleInitial":"James","affiliations":[],"preferred":false,"id":152598,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morey, George Washington","contributorId":62267,"corporation":false,"usgs":true,"family":"Morey","given":"George","email":"","middleInitial":"Washington","affiliations":[],"preferred":false,"id":152597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zen, C.S.","contributorId":26572,"corporation":false,"usgs":true,"family":"Zen","given":"C.S.","email":"","affiliations":[],"preferred":false,"id":152596,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":14875,"text":"ofr72239 - 1972 - Prototype and preliminary geologic mapping of Mars from Mariner 6 & 7 data; parts 1, 2 and 3","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr72239","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-239","title":"Prototype and preliminary geologic mapping of Mars from Mariner 6 & 7 data; parts 1, 2 and 3","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr72239","usgsCitation":"McCauley, J., West, M., Scott, D.H., Peterson, J.E., and Wilhelms, D.E., 1972, Prototype and preliminary geologic mapping of Mars from Mariner 6 & 7 data; parts 1, 2 and 3: U.S. Geological Survey Open-File Report 72-239, iii, 21 p. :2 folded maps ;27 cm.; 2 sheets, scale 1:5,000,000 and 1:500,000, https://doi.org/10.3133/ofr72239.","productDescription":"iii, 21 p. :2 folded maps ;27 cm.; 2 sheets, scale 1:5,000,000 and 1:500,000","costCenters":[],"links":[{"id":147217,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"500000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db6568ff","contributors":{"authors":[{"text":"McCauley, John F.","contributorId":54973,"corporation":false,"usgs":true,"family":"McCauley","given":"John F.","affiliations":[],"preferred":false,"id":170168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"West, Maretta","contributorId":48191,"corporation":false,"usgs":true,"family":"West","given":"Maretta","email":"","affiliations":[],"preferred":false,"id":170167,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Scott, David Holcomb 0000-0002-7925-7452 dscott@usgs.gov","orcid":"https://orcid.org/0000-0002-7925-7452","contributorId":37344,"corporation":false,"usgs":true,"family":"Scott","given":"David","email":"dscott@usgs.gov","middleInitial":"Holcomb","affiliations":[],"preferred":false,"id":170166,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Peterson, James E.","contributorId":32931,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":170165,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilhelms, Don E.","contributorId":28972,"corporation":false,"usgs":true,"family":"Wilhelms","given":"Don","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":170164,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":66862,"text":"i591M - 1972 - Map showing general availability of ground water in the Salina quadrangle, Utah","interactions":[],"lastModifiedDate":"2025-08-04T21:24:29.255847","indexId":"i591M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"591","chapter":"M","title":"Map showing general availability of ground water in the Salina quadrangle, Utah","docAbstract":"<p>The general availability of ground water was determined from well records collected by the U.S. Geological Survey and cooperating State, local, and Federal agencies. Data are for aquifers that in most places are less than 1,000 feet below the land surface. In areas of few or no wells, potential well yields are inferred from geologic data. Special investigations are needed to determine specific factors such as depths and sustained yields of aquifers, water levels, and suitability of water for use in any given area. More detailed information about principal aquifers for specific parts of the map area are obtainable from the district office of the Water Resources Division, U.S. Geological Survey, Salt Lake City, Utah.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i591M","usgsCitation":"Price, D., 1972, Map showing general availability of ground water in the Salina quadrangle, Utah: U.S. Geological Survey IMAP 591, 1 Plate: 40.03 x 27.60 inches; Cover: 9.17 x 11.78 inches, https://doi.org/10.3133/i591M.","productDescription":"1 Plate: 40.03 x 27.60 inches; Cover: 9.17 x 11.78 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":256125,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0591m/plate-1.pdf","text":"Map I-591-M","size":"10.13 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":493514,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9386.htm","linkFileType":{"id":5,"text":"html"}},{"id":256126,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0591m/report.pdf","text":"Folio Cover","size":"34 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":256127,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0591m/report-thumb.jpg"}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Salina quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38 ], [ -112,39 ], [ -110,39 ], [ -110,38 ], [ -112,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b14ff","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":275196,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15030,"text":"ofr72259 - 1972 - A computer program for creating keyword indexes to textual data files","interactions":[],"lastModifiedDate":"2017-06-18T22:02:36","indexId":"ofr72259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-259","title":"A computer program for creating keyword indexes to textual data files","docAbstract":"A keyword-in-context (KWIC) or out-of-context (KWOC) index is a convenient means of organizing information. This keyword index program can be used to create either KWIC or KWOC indexes of bibliographic references or other types of information punched on. cards, typed on optical scanner sheets, or retrieved from various Department of Interior data bases using the Generalized Information Processing System (GIPSY). The index consists of a 'bibliographic' section and a keyword-section based on the permutation of. document titles, project titles, environmental impact statement titles, maps, etc. or lists of descriptors. The program can also create a back-of-the-book index to documents from a list of descriptors. By providing the user with a wide range of input and output options, the program provides the researcher, manager, or librarian with a means of-maintaining a list and index to documents in. a small library, reprint collection, or office file.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72259","usgsCitation":"Moody, D.W., 1972, A computer program for creating keyword indexes to textual data files: U.S. Geological Survey Open-File Report 72-259, i, 27 leaves ;1972., https://doi.org/10.3133/ofr72259.","productDescription":"i, 27 leaves ;1972.","costCenters":[],"links":[{"id":43943,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0259/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0259/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b09c6","contributors":{"authors":[{"text":"Moody, David W.","contributorId":84729,"corporation":false,"usgs":true,"family":"Moody","given":"David","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170444,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16672,"text":"ofr72454 - 1972 - Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","interactions":[],"lastModifiedDate":"2024-03-27T17:56:09.862376","indexId":"ofr72454","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-454","title":"Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards","docAbstract":"<p>A program to study the engineering geology of most of the larger Alaska coastal communities and to evaluate their earthquake and other geologic hazards was started promptly after the 1964 Alaska earthquake; this report is a product of that program. Field-study methods were largely reconnaissance, and thus the interpretations in the report are subject to revision as further information becomes available. The report provides broad guidelines for planners and engineers when considering geologic factors during preparation of land-use plans. The use of this information should lead to minimizing future loss of life and property, especially during major earthquakes.</p><p>Skagway was established in 1897 as a seaport near the head of Taiya Inlet fiord in the northern part of southeastern Alaska. Rugged mountains, steep-walled valleys, fiords, and numerous glaciers and icefields characterize the landscape of the area. Valley floors are narrow and most carry large streams, which end in tidewater deltas. Skagway is situated on the delta and lower valley floor of the Skagway River.</p><p>Glaciers became vastly enlarged during the Pleistocene Epoch and presumably covered the area at least several times. The last major deglaciation probably occurred about 10,000 years ago. Subsequently, there was minor expansion and then partial retreat of glaciers; land rebound because of glacial melting is still going on today.</p><p>Bedrock is composed predominantly of plutonic intrusive rocks, chiefly quartz diorite and granodiorite, some metamorphic rocks and a few dikes are present. Most bedrock is of Jurassic and Cretaceous age.</p><p>An assortment of surficial deposits of Quaternary age form the valley bottoms and locally part of the valley walls. Thick deposits of sand and gravel have accumulated as deltas at the heads of fiords and as alluvium in the main stream valleys; deposits may be as much as S8S feet thick at Skagway. Locally, thin deposits mantle some of the steep bedrock slopes and also form some moderately to gently sloping ground. Manmade fill covers much of the top of the delta and floor of the Skagway valley. The fill is composed chiefly of gravel and sand. Quarried blocks of granodiorite are used as riprap to face river dikes and on fill areas exposed to waves of Taiya Inlet.</p><p>The geologic structure of the area is imperfectly known. However, it appears that plutonic rocks intruded metamorphic rocks in Jurassic and Cretaceous time. Extensive faulting is strongly indicated by the strikingly linear or curvilinear pattern of fiords and many large and small valleys, but no major faults have been positively identified because of concealment by water or surficial deposits. Inferred faults include those coincident with the lower Skagway valley, Taiya Inlet-Taiya valley, and the Katzehin River delta-Upper Dewey Lake. Principal fault movements probably occurred in middle Tertiary time but some movement might have been in late Tertiary or possibly early Quaternary time. Local faults appear to join the Chilkat River fault, a segment of the important Denali fault system, one of the major tectonic elements of southeastern Alaska. One fault segment of this system shows evidence of movement within the last several hundred years. Southeastern Alaska's other major fault system is the active Fairweather-Queen Charlotte Islands fault system'near the coast of the Pacific Ocean. This fault system passes to within about 100 miles of Skagway. At its northwest end the fault system merges with the Chugach-St. Elias fault.</p><p>One hundred twenty-two earthquakes, some of them strong, have been felt or possibly felt at Skagway during the years 1898 through 1969. The closest large earthquake (magnitude about 8) causing some damage at Skagway occurred July 10, 1958. Its epicenter was about 100 miles to the southwest. Other earthquakes, as much as 150 miles away, also have caused slight to moderate damage. The closest instrumentally recorded earthquake (magnitude 6) had its epicenter about 30 miles to the west of Skagway.</p><p>Most earthquakes in southeastern Alaska have occurred southwest, west, or northwest of Skagway, near the coast of the Pacific Ocean. They appear to be related to movement along the Fairweather-Queen Charlotte Islands fault system or the Chugach-St. Elias fault. Most have had their epicenters offshore. Some earthquakes may be related to movement at depth along the Denali fault system.</p><p>The probability of destructive earthquakes at Skagway is unknown because the tectonics of the region have not been studied in detail. However, on the basis of the seismic record and limited tectonic evidence, we suggest that sometime in the future an earthquake of at least magnitude 6 probably will occur very close to the city, a magnitude 7 earthquake might occur in the general area, and an earthquake of magnitude 8 probably will occur at some distance to the southwest, west, or northwest.</p><p>Effects from nearby large earthquakes could cause extensive damage at Skagway. Nine principal effects are considered.</p><p>1. Surface&nbsp;displacement. Displacement of ground caused by fault movement would affect only structures built athwart the fault. However, a sudden tectonic uplift of land of as much as a few feet might affect a wide area and necessitate extensive dredging and wharf rebuilding. On the other hand, a subsidence of several feet would allow tidewater to reach inland and flood part of the harbor facilities and the business district.</p><p>2. Ground shaking. Because intensity of ground shaking during earthquakes largely depends on type and water content of the geologic material being shaken, the geologic materials are separated into three categories. Those considered susceptible to strongest shaking are grouped into category 1 (containing materials that are saturated, loose, and of medium- to fine-grain sizes); those of intermediate susceptibility in category 2; and those least susceptible to shaking in category 3.</p><p>3. Compaction of some medium-grained sediments during strong earthquake shaking could cause local settling of alluvial and deltaic surfaces. Also, some manmade fills near the harbor might undergo marked differential settling.</p><p>4. Liquefaction of saturated beds of uniform, fine sand commonly occurs during strong earthquakes. Few such beds, however, are positively identified at Skagway; some may occur within deltaic and alluvial deposits. If present, these beds might liquefy and cause local settling or trigger landslides.</p><p>5. Ejection of water-sediment mixtures from earthquake-induced fractures or from point sources, plus some associated ground subsidence, is common during major earthquakes where saturated sand and fine gravel deposits are confined beneath generally impermeable beds. Some alluvial and deltaic deposits at Skagway probably are susceptible to these processes. Locally, ejecta might cover roads and areas between buildings and fill low-lying areas. Associated ground fracturing might damage roadways, foundations of buildings, and other facilities.</p><p>6. Subaerial and subaqueous slides occur frequently during earthquakes. Saturated loose sediments on steep slopes are especially susceptible to sliding. During a major earthquake, surficial deposits forming such slopes along the southeast side of the Skagway valley probably would be subject to sliding or earthflowing on an extensive scale. Some sliding might extend onto the valley floor and damage or destroy buildings and part of the railroad. Rockfalls would be numerous and locally very large rockslides might occur.</p><p>Subaqueous sliding of the Skagway delta is potentially the most damaging of earthquake effects. Sliding may have occurred there during the earthquake of September 16, 1899; any future major earthquake close to the city would cause extensive sliding, possibly triggered in part by liquefaction. If shaking continued for several minutes, successive slides might progressively remove large portions of the delta and allow extensive land spreading and fracturing of Skagway River alluvium as much as several thousand feet landward from the shoreline.</p><p>7. Glacier surfaces commonly receive extensive snow avalanches and rockslides during seismic shaking. In the Skagway area, glaciers may be disrupted at their margins, and resulting blocked streams might form lakes in a few places. If these lakes drained suddenly, downstream areas would he flooded. No long-term effects, such as glacier expansion, are expected.</p><p>8. Ground- and surface-water levels often are affected during and after strong earthquake shaking. At Skagway, ground-water levels probably would be lowered, but there would be no permanent change in water quality. Earthquake-triggered landslides could dam the Skagway River; the sudden failure of the dams might cause severe flooding.</p><p>9. Waves generated by earthquakes include tsunamis, seiche waves, and waves caused by subaerial and submarine sliding and tectonic displacement of land. Damage in the Skagway area would depend on wave height, tidal stage, and warning time. Some waves triggered by subaerial and subaqueous slides have a strong possibility of reaching heights of as much as 60 feet--or possibly even higher. Tsunamis from the open ocean must travel 160 miles of fiords before reaching Skagway, which allows sufficient time for appraisal of expectable wave height and, if necessary, evacuation of the harbor area and other low-lying ground.</p><p>Geologic hazards other than those hazards associated with earthquakes include nonearthquake-induced subaerial and subaqueous slides, floods, and slow uplift (rebound) of land. Landslides of moderate size are known to have occurred from time to time during heavy rains such as those of September 1967. Subaqueous slides happen intermittently during the normal growth of deltas. Submarine cables on the floor of northern Taiya Inlet presumably were broken by such slides on September 10, 1927. Flooding by the Skagway River has inundated parts of the city many times, usually during heavy rains in the fall. Two floods were reported to have been caused by the sudden draining of glacier-dammed lakes. Dikes protect the city from many smaller floods, but heightening and broadening is needed to give full protection. Slow land uplift at Skagway, because of regional glacioisostatic rebound, averages 0.059 foot per year. On this basis, the shoreline theoretically shifted seaward 500 feet and the harbor shoaled 4.4 feet between 1897 and 1972.</p><p>It is recommended that future geologic study of the Skagway area include: detailed geologic mapping and collection of data on geologic materials, joints, faults, and slope stability; complete evaluation of earthquake probability and response of materials to shaking; and collection and evaluation of periodic soundings and sediment data from Skagway and Taiya deltas to assist in forecasting the stability of the delta front.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72454","usgsCitation":"Yehle, L.A., and Lemke, R.W., 1972, Reconnaissance engineering geology of the Skagway area, Alaska, with emphasis on evaluation of earthquake and other geologic hazards: U.S. Geological Survey Open-File Report 72-454, Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller, https://doi.org/10.3133/ofr72454.","productDescription":"Report: iv, 108 p.; 4 Plates: 35.77 x 18.67 inches or smaller","costCenters":[],"links":[{"id":427161,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427160,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427159,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427158,"rank":3,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1972/0454/figure-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":427153,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150379,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0454/report-thumb.jpg"}],"scale":"9600","country":"United States","state":"Alaska","city":"Skagway","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.40680330286153\n            ],\n            [\n              -135.22164285027563,\n              59.48810534833572\n            ],\n            [\n              -135.3463249696411,\n              59.48810534833572\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db6443d4","contributors":{"authors":[{"text":"Yehle, Lynn A. yehle@usgs.gov","contributorId":3794,"corporation":false,"usgs":true,"family":"Yehle","given":"Lynn","email":"yehle@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":173260,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lemke, Richard Walter","contributorId":105280,"corporation":false,"usgs":true,"family":"Lemke","given":"Richard","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":173261,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14835,"text":"ofr72251 - 1972 - Geochemical data from the Nabesna B-3 quadrangle, Alaska","interactions":[],"lastModifiedDate":"2012-03-02T17:16:06","indexId":"ofr72251","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-251","title":"Geochemical data from the Nabesna B-3 quadrangle, Alaska","language":"ENGLISH","publisher":"U.S Geological Survey],","doi":"10.3133/ofr72251","usgsCitation":"Matson, N.A., and Richter, D.H., 1972, Geochemical data from the Nabesna B-3 quadrangle, Alaska: U.S. Geological Survey Open-File Report 72-251, 41 leaves :folded map ;27 cm.; 1 sheet, scale 1:63,360, https://doi.org/10.3133/ofr72251.","productDescription":"41 leaves :folded map ;27 cm.; 1 sheet, scale 1:63,360","costCenters":[],"links":[{"id":106530,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8690.htm","linkFileType":{"id":5,"text":"html"},"description":"8690"},{"id":147565,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0251/report-thumb.jpg"},{"id":43623,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0251/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43624,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0251/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"63360","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae7f1","contributors":{"authors":[{"text":"Matson, Neal A. Jr.","contributorId":18779,"corporation":false,"usgs":true,"family":"Matson","given":"Neal","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":170093,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Richter, Donald H.","contributorId":61021,"corporation":false,"usgs":true,"family":"Richter","given":"Donald","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":170094,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":56471,"text":"wdrFL7112 - 1972 - Water resources data for Florida, water year 1971; Part 1, Subsurface water records; Volume 2, Streams, southern Florida, Lake Okeechobee, and the Everglades","interactions":[],"lastModifiedDate":"2012-02-02T00:12:20","indexId":"wdrFL7112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"FL-71-1-2","title":"Water resources data for Florida, water year 1971; Part 1, Subsurface water records; Volume 2, Streams, southern Florida, Lake Okeechobee, and the Everglades","language":"ENGLISH","doi":"10.3133/wdrFL7112","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Water resources data for Florida, water year 1971; Part 1, Subsurface water records; Volume 2, Streams, southern Florida, Lake Okeechobee, and the Everglades: U.S. Geological Survey Water Data Report FL-71-1-2, 245 p., https://doi.org/10.3133/wdrFL7112.","productDescription":"245 p.","costCenters":[],"links":[{"id":184116,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f73c2","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":532652,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48088,"text":"ofr72420 - 1972 - Compilation of hydrologic data, Little Elm Creek, Trinity River basin, Texas, 1968","interactions":[],"lastModifiedDate":"2017-06-14T14:35:53","indexId":"ofr72420","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-420","title":"Compilation of hydrologic data, Little Elm Creek, Trinity River basin, Texas, 1968","docAbstract":"<p>The U.S. Soil Conservation Service is actively engaged in the installation of flood and soil erosion reducing measures in Texas under the authority of \"The Flood Control Act ot 1936 and 1944\" and ''Watershed Protection and Flood Prevention Act\" (Public Law 566), as amended. In June 1968, the Soil Conservation Service estimated approximately 3,500 structures to be physically and economically feasible for installation in Texas. As of September 30, 1968, 1,271 of these structures had been built. </p><p>This watershed-development program will have varying but important effects on the surface- and ground-water resources of river basins, especially where a large number of the floodwater-retarding structures are built. Basic hydrologic data are needed to appraise the effects of the structures on water yield and the mode of occurrence of runoff. </p><p>Hydrologic investigations of these small watersheds were begun by the Geological Survey in 1951 and are now being made in 11 areas (fig. 1). These studies are being made in cooperation with t he Texas Water Development Board, the Soil Conservation Service, the San Antonio River Authority, the city of Dallas, and the Tarrant County Water Control and Improvement District No. 1. The 11 study areas were choson to sample watersheds having different rainfall, topography, geology, and soils. In four of the study areas (Mukewater, North, Little Elm, and Pin Oak Creeks), streamflow and rainfall records were collected prior to construction of the floodwater-retarding structures, thus affording the opportunity for analyses to the conditions before and after\" development. Structures have now been built in three of these study areas. A summary of the development of the floodwater-retarding structures on each study area as of September 30, 1968, is shown in table 1. <u></u></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr72420","collaboration":"Prepared in cooperation with the City of Dallas and the Texas Water Development Board","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, Compilation of hydrologic data, Little Elm Creek, Trinity River basin, Texas, 1968: U.S. Geological Survey Open-File Report 72-420, v, 83 p., https://doi.org/10.3133/ofr72420.","productDescription":"v, 83 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":327730,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr72420.JPG"},{"id":287745,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0420/report.pdf","text":"Report","size":"38.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"}],"country":"United States","state":"Texas","otherGeospatial":"Little Elm Creek, Trinity River basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -97.1612,32.745 ], [ -97.1612,33.6619 ], [ -96.1234,33.6619 ], [ -96.1234,32.745 ], [ -97.1612,32.745 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ee4b07f02db6a9e8a","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":531780,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48086,"text":"ofr72404 - 1972 - High-resolution shallow focus geophysical data from offshore western Louisiana","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr72404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-404","title":"High-resolution shallow focus geophysical data from offshore western Louisiana","language":"ENGLISH","doi":"10.3133/ofr72404","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1972, High-resolution shallow focus geophysical data from offshore western Louisiana: U.S. Geological Survey Open-File Report 72-404, NA, https://doi.org/10.3133/ofr72404.","productDescription":"NA","costCenters":[],"links":[{"id":162468,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db68875b","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":531778,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":66062,"text":"i591N - 1972 - Map showing drainage basins and historic cloudburst floods in the Salina quadrangle, Utah","interactions":[],"lastModifiedDate":"2025-08-04T21:26:18.999749","indexId":"i591N","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"591","chapter":"N","title":"Map showing drainage basins and historic cloudburst floods in the Salina quadrangle, Utah","docAbstract":"<p>In the Salina quadrangle, as in most of the arid West, summer precipitation commonly occurs as thunderstorms. Suring these storms, rain falls as a torrential downpour, or cloudburst, in a local area. An inch of rain or more may fall in half an hour; U.S. Weather Bureau records show that o.4 inch of rain has fallen in a period of 5 minutes (Woolley, 1946). Such a fall of water far exceeds the absorptive capacity of the ground surface, and in areas of steep sparsely vegetated terrain the runoff forms a cloudburst flood in which loose rock, soil, and alluvium combine with water to form a debris-laden mudflow. The mudflow then moves rapidly down gullies and canyons with power great enough to erode and to transport debris, and to destroy the works of man lying in its path. When the mudflow pours from the canyon mount into an open valley, solid debris separates from the water and is added to the alluvial fan built by numerous previous floods. Because many towns in Utah are built on fans at the mouths of canyons, there has been loss of life and considerable damage to buildings, streets, and crops since 1847, when white men first settled in Utah.</p><p>This map shows historical cloudburst floods for which records exist; data were taken from the sources listed below. Most of the flooded areas shown are in or near populated places, and so the floods were observed and recorded. Actually, no part of the quadrangle is exempt from cloudburst floods; every canyon, dry wash, and swale is visited sooner or later by a cloudburst and becomes, briefly, the site of a destructive mudflow. The traveler is advised to exercise caution in all drainageways, especially during July and August, when 80 percent of the cloudbursts occur.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/i591N","usgsCitation":"Hackman, R., and Williams, P., 1972, Map showing drainage basins and historic cloudburst floods in the Salina quadrangle, Utah: U.S. Geological Survey IMAP 591, 1 Plate: 40.26 x 27.93 inches; Cover: 9.23 x 11.74 inches, https://doi.org/10.3133/i591N.","productDescription":"1 Plate: 40.26 x 27.93 inches; Cover: 9.23 x 11.74 inches","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":255580,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0591n/plate-1.pdf","text":"Map I-591-N","size":"8.75 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":255582,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0591n/report-thumb.jpg"},{"id":255581,"rank":2,"type":{"id":8,"text":"Cover"},"url":"https://pubs.usgs.gov/imap/0591n/report.pdf","text":"Folio Cover","size":"389 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":493515,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9387.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"250000","country":"United States","state":"Utah","otherGeospatial":"Salina quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112,38 ], [ -112,39 ], [ -110,39 ], [ -110,38 ], [ -112,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c95b","contributors":{"authors":[{"text":"Hackman, Robert J.","contributorId":30999,"corporation":false,"usgs":true,"family":"Hackman","given":"Robert J.","affiliations":[],"preferred":false,"id":273928,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Williams, Paul L.","contributorId":91086,"corporation":false,"usgs":true,"family":"Williams","given":"Paul L.","affiliations":[],"preferred":false,"id":273927,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":48036,"text":"ofr72164 - 1972 - Low flows and temperatures of streams in the Seattle-Tacoma urban complex and adjacent areas, Washington","interactions":[],"lastModifiedDate":"2012-07-19T01:01:48","indexId":"ofr72164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","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":"72-164","title":"Low flows and temperatures of streams in the Seattle-Tacoma urban complex and adjacent areas, Washington","docAbstract":"Data on the minimum flows of streams and water temperature are necessary for the proper planning and development of the water resources of urban Seattle-Tacoma and adjacent areas. The data on low flows are needed for such purposes as (1) designing and operating municipal and industrial water-supply systems; (2) classifying streams as to their potential for waste disposal; (3) defining the amount of water available for irrigation, for maintaining streamflow as required by law or agreement, and for fish propagation; and (4) designing water-storage facilities. Data on stream temperatures are important to many water users because of the many biological, chemical, and physical properties of water that are dependent on temperature. Agricultural and domestic users as well as municipal, industrial and fishery agencies are concerned with water temperatures. In this report, low-flow data are accompanied by information on seasonal variations in water temperatures at sites selected as representing regional stream-temperature patterns. Because low flows and high water temperatures commonly occur together, they may impose constraints on various uses of the region's streams. The following discussion deals first with low-flow trends in the region, then with stream temperatures, and finally with some of the resulting constraints.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tacoma, WA","doi":"10.3133/ofr72164","usgsCitation":"Hidaka, F., 1972, Low flows and temperatures of streams in the Seattle-Tacoma urban complex and adjacent areas, Washington: U.S. Geological Survey Open-File Report 72-164, 11 p.; 1 Plate: 58 x 77 cm., https://doi.org/10.3133/ofr72164.","productDescription":"11 p.; 1 Plate: 58 x 77 cm.","costCenters":[],"links":[{"id":170293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1972/0164/report-thumb.jpg"},{"id":84806,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1972/0164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":84807,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1972/0164/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Washington","city":"Seattle;Tacoma","otherGeospatial":"Cedar River;Deschutes River;Flett Creek;Green River;Nisqually River;North Creek;Puyallup River;Quilceda Creek;Sammamish River;Skykomish River;Snoqualmie River;Sultan River;Taylor Creek;White River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,46.666666666666664 ], [ -123,48.166666666666664 ], [ -121.58333333333333,48.166666666666664 ], [ -121.58333333333333,46.666666666666664 ], [ -123,46.666666666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644921","contributors":{"authors":[{"text":"Hidaka, F.T.","contributorId":48542,"corporation":false,"usgs":true,"family":"Hidaka","given":"F.T.","email":"","affiliations":[],"preferred":false,"id":236709,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37435,"text":"ssrw154 - 1972 - Use of banding data in migratory game bird research and management","interactions":[],"lastModifiedDate":"2012-02-02T00:09:39","indexId":"ssrw154","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":83,"text":"Special Scientific Report  - Wildlife","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"154","title":"Use of banding data in migratory game bird research and management","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Geis, A.D., 1972, Use of banding data in migratory game bird research and management: Special Scientific Report  - Wildlife 154, ii, 47 p.","productDescription":"ii, 47 p.","costCenters":[],"links":[{"id":112142,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/uc1.31822009785148?urlappend=%3Bseq=3"},{"id":167704,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db604b7c","contributors":{"authors":[{"text":"Geis, Aelred D.","contributorId":86401,"corporation":false,"usgs":true,"family":"Geis","given":"Aelred","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":218074,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}