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,{"id":34607,"text":"b1181D - 1964 - Curecanti pluton, an unusual intrusive body in the Black Canyon of the Gunnison, Colorado","interactions":[],"lastModifiedDate":"2024-07-31T18:54:48.075062","indexId":"b1181D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1181","chapter":"D","title":"Curecanti pluton, an unusual intrusive body in the Black Canyon of the Gunnison, Colorado","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1181D","usgsCitation":"Hansen, W.R., 1964, Curecanti pluton, an unusual intrusive body in the Black Canyon of the Gunnison, Colorado: U.S. Geological Survey Bulletin 1181, iii, 15 p., https://doi.org/10.3133/b1181D.","productDescription":"iii, 15 p.","costCenters":[],"links":[{"id":431729,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_92574.htm","linkFileType":{"id":5,"text":"html"}},{"id":163007,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1181d/report-thumb.jpg"},{"id":96515,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1181d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"Black Canyon of the Gunnison","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.455,\n              38.4697\n            ],\n            [\n              -107.455,\n              38.4208\n            ],\n            [\n              -107.3756,\n              38.4208\n            ],\n            [\n              -107.3756,\n              38.4697\n            ],\n            [\n              -107.455,\n              38.4697\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ec97","contributors":{"authors":[{"text":"Hansen, W. R.","contributorId":59378,"corporation":false,"usgs":true,"family":"Hansen","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":213254,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62319,"text":"gq262 - 1964 - Pre-quaternary geology of the Pemberton quadrangle, New Jersey","interactions":[],"lastModifiedDate":"2012-02-10T00:10:56","indexId":"gq262","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"262","title":"Pre-quaternary geology of the Pemberton quadrangle, New Jersey","language":"ENGLISH","doi":"10.3133/gq262","usgsCitation":"Owens, J.P., and Minard, J.P., 1964, Pre-quaternary geology of the Pemberton quadrangle, New Jersey: U.S. Geological Survey Geologic Quadrangle 262, 1 map :col. ;58 x 45 cm., on sheet 73 x 92 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq262.","productDescription":"1 map :col. ;58 x 45 cm., on sheet 73 x 92 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102267,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_716.htm","linkFileType":{"id":5,"text":"html"},"description":"716"},{"id":248501,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0262/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253562,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0262/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.75,39.8675 ], [ -74.75,40 ], [ -74.61749999999999,40 ], [ -74.61749999999999,39.8675 ], [ -74.75,39.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db6811a9","contributors":{"authors":[{"text":"Owens, James Patrick","contributorId":105706,"corporation":false,"usgs":true,"family":"Owens","given":"James","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":267223,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Minard, James P.","contributorId":84761,"corporation":false,"usgs":true,"family":"Minard","given":"James","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":267222,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":71100,"text":"wdrMN641 - 1964 - Surface water records of Minnesota, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:14:03","indexId":"wdrMN641","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"MN-64-1","title":"Surface water records of Minnesota, 1964","language":"ENGLISH","doi":"10.3133/wdrMN641","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of Minnesota, 1964: U.S. Geological Survey Water Data Report MN-64-1, vii, 160 p., https://doi.org/10.3133/wdrMN641.","productDescription":"vii, 160 p.","costCenters":[],"links":[{"id":101518,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1964/mn-64-1/report.pdf","size":"11947","linkFileType":{"id":1,"text":"pdf"}},{"id":192933,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1964/mn-64-1/report-thumb.jpg"}],"scale":"100000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697906","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":534719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3226,"text":"cir483 - 1964 - Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","interactions":[],"lastModifiedDate":"2012-02-02T00:05:34","indexId":"cir483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"483","title":"Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62","docAbstract":"Estimates of potential waterpower and historical data on waterpower developments in various parts of the world are assembled in this report. Salient characteristics of the period studied, 1955-62, include increased use of the underground powerhouse, multiple -purpose developments, and use of storage (including pumped storage) to increase the value of waterpower for peaking purposes. High-voltage long-distance transmission has been improved, especially in the United States, Sweden, and the U.S.S.R., and generating facilities tend to be larger than ever before. Asia leads the continents in total potential waterpower; Europe is first in use of waterpower. In rate of increase of waterpower installations and in percent of hydroelectric to total installations Africa is first among the continents. The 1955-62 period saw a great increase in per capita consumption of electric energy. Norway leads all countries with annual consumption of about 9,000 kwhr per capita. Waterpower development was carried on in a majority of the countries of the world and in most of them at an accelerated rate.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/cir483","usgsCitation":"Young, L.L., 1964, Summary of developed and potential waterpower of the United States and other countries of the world, 1955-62: U.S. Geological Survey Circular 483, iv, 38 p. ;26cm., https://doi.org/10.3133/cir483.","productDescription":"iv, 38 p. ;26cm.","costCenters":[],"links":[{"id":123048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0483/report-thumb.jpg"},{"id":30219,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0483/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6992c4","contributors":{"authors":[{"text":"Young, Loyd L.","contributorId":14805,"corporation":false,"usgs":true,"family":"Young","given":"Loyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":146469,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3221,"text":"cir489 - 1964 - A magnetic anomaly of possible economic significance in southeastern Minnesota","interactions":[],"lastModifiedDate":"2018-01-02T19:49:02","indexId":"cir489","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"489","title":"A magnetic anomaly of possible economic significance in southeastern Minnesota","docAbstract":"An aeromagnetic survey in southeastern Minnesota by the U. S. Geological Survey in cooperation with the State of Minnesota has revealed a high-amplitude, linear, and narrow magnetic feature that suggests a possible source of Precambrian iron-formation of economic value. \r\n\r\nFor the past few years the U. S. Geological Survey has been conducting detailed geophysical studies of the midcontinent gravity anomaly--a broad, high-amplitude feature that extends from Lake Superior through the States of Minnesota, Iowa, Nebraska, and part of Kansas. As part of this study an aeromagnetic survey of the southern part of the State was made in cooperation with the State of Minnesota during the summer of 1963, in which a linear high-amplitude anomaly of the order of 4,000 gammas was discovered. Because of the high amplitude, the linearity, and the narrowness of the magnetic feature, it is believed the source may be Precambrian iron-formation of possible economic value. \r\n\r\nThe anomalous area is in Fillmore County, approximately between the towns of Lanesboro and Peterson in the extreme southeastern part of the State. (See figures 1 and 2.) At the site of the anomaly, Cambrian sedimentary rocks occur in the valley of the Root River, and Ordovician rocks (nearly flat lying) mantle the upland areas. \r\n\r\nThe uplands are largely covered by glacial deposits, which are relatively thin (Paul K. Sims, written communication, 1964). Depths to the Precambrian are estimated to range from 500 feet to 1,000 feet below the surface. \r\n\r\nThe aeromagnetic map shown in figure 2 was compiled from continuous magnetic profiles made along east-west flight lines 1,000 feet above ground, and spaced approximately 1 mile apart. Contour intervals of 20, 100, and 500 gammas were used depending on the intensity. The instrument for the survey was a flux-gate type magnetometer (AN/ASQ-3A) which measures total-field variations. The contour map displays variations in magnetic pattern which are typical of shallow Precambrian rocks. Anomalies of the order of 1,000 gammas are shown along the east and west edges of the map. The outstanding feature is the previously mentioned linear positive anomaly that trends northeast and reaches a peak of 3,960 gammas. The positive anomaly is contoured from data on four consecutive profiles, but only two show high amplitudes. The high-amplitude anomalies along traverses 1 and 2 are shown in figure 3. \r\n\r\nDepth calculations suggest that the source of the anomaly lies about 1,000 feet below the surface. Assuming a dikelike source and magnetization resulting entirely from induction in the earth's field, several calculations were made in an attempt to fit the magnetic profile taken along the line AA' (see figs. 2 and 4), considered to be a typical cross-section of the magnetic anomaly. Comparisons are shown between observed and computed profiles. The fixed parameters used were (a) distance from detector to source of 2,000 ft; width of dike of 5,000 ft; dip of dike of 75?, 90?, 105? , and 120? , as shown. The best fit occurs when the dike is vertical or dips 75? to the southwest. For these cases, the susceptibility, k, is computed to be 0.016 c.g.s, units, and is comparable to k = 0.02+ calculated by Bath (1962) for the relatively unmetamorphosed iron-formation of the Main Megabi district in Minnesota where the induced magnetization was most likely the dominant magnetization. If the dominant magnetization for the anomaly in Fillmore County were remanent rather than induced, the economic importance of the anomaly would be greatly reduced. \r\n\r\nThis anomaly seems sufficiently promising to warrant further geologic and geophysical investigation. Detailed ground magnetic and electrical studies would be useful to delineate the feature. In the final analysis, however, the presence of iron-formation can be determined only by the drill.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir489","usgsCitation":"Zietz, I., 1964, A magnetic anomaly of possible economic significance in southeastern Minnesota: U.S. Geological Survey Circular 489, 5 p. :maps ;27 cm., https://doi.org/10.3133/cir489.","productDescription":"5 p. :maps ;27 cm.","costCenters":[],"links":[{"id":138944,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0489/report-thumb.jpg"},{"id":30214,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0489/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae1de","contributors":{"authors":[{"text":"Zietz, Isidore","contributorId":76708,"corporation":false,"usgs":true,"family":"Zietz","given":"Isidore","affiliations":[],"preferred":false,"id":146462,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62486,"text":"gq355 - 1964 - Geology of the South Butte quadrangle New Mexico-Valencia County","interactions":[],"lastModifiedDate":"2021-11-10T19:56:51.078882","indexId":"gq355","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"355","title":"Geology of the South Butte quadrangle New Mexico-Valencia County","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq355","usgsCitation":"Moench, R.H., 1964, Geology of the South Butte quadrangle New Mexico-Valencia County: U.S. Geological Survey Geologic Quadrangle 355, Report: 1 p.; Plate, https://doi.org/10.3133/gq355.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102367,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_816.htm","linkFileType":{"id":5,"text":"html"},"description":"816"},{"id":248649,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0355/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":253876,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0355/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"New Mexico","county":"Valencia County","otherGeospatial":"South Butte quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.5,34.8675 ], [ -107.5,35 ], [ -107.36749999999999,35 ], [ -107.36749999999999,34.8675 ], [ -107.5,34.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e4b9","contributors":{"authors":[{"text":"Moench, Robert Hadley","contributorId":28238,"corporation":false,"usgs":true,"family":"Moench","given":"Robert","email":"","middleInitial":"Hadley","affiliations":[],"preferred":false,"id":267440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14011,"text":"ofr6473 - 1964 - Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York","interactions":[],"lastModifiedDate":"2025-06-17T13:50:40.301139","indexId":"ofr6473","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-73","title":"Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6473","usgsCitation":"Hartshorn, J.H., and Atherton, J.S., 1964, Preliminary surficial geology of the Bashbish Falls quadrangle, Massachusetts-Connecticut-New York: U.S. Geological Survey Open-File Report 64-73, Report: 16 p.; 1 Plate: 33.60 x 27.47 inches, https://doi.org/10.3133/ofr6473.","productDescription":"Report: 16 p.; 1 Plate: 33.60 x 27.47 inches","costCenters":[],"links":[{"id":490821,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0073/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":490820,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0073/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397538,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8071.htm"},{"id":146640,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0073/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Connecticut, Massachusetts, New York","otherGeospatial":"Bashbish Falls quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              42\n            ],\n            [\n              -73.375,\n              42\n            ],\n            [\n              -73.375,\n              42.125\n            ],\n            [\n              -73.5,\n              42.125\n            ],\n            [\n              -73.5,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aabe4b07f02db66998c","contributors":{"authors":[{"text":"Hartshorn, Joseph H.","contributorId":89862,"corporation":false,"usgs":true,"family":"Hartshorn","given":"Joseph","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":168786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Atherton, J. S.","contributorId":98737,"corporation":false,"usgs":true,"family":"Atherton","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":168787,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":17901,"text":"ofr6461 - 1964 - Water resources of Van Buren County, Michigan","interactions":[{"subject":{"id":17901,"text":"ofr6461 - 1964 - Water resources of Van Buren County, Michigan","indexId":"ofr6461","publicationYear":"1964","noYear":false,"title":"Water resources of Van Buren County, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":70047876,"text":"70047876 - 1964 - Water resources of Van Buren County, Michigan","indexId":"70047876","publicationYear":"1964","noYear":false,"title":"Water resources of Van Buren County, Michigan"},"id":1}],"supersededBy":{"id":70047876,"text":"70047876 - 1964 - Water resources of Van Buren County, Michigan","indexId":"70047876","publicationYear":"1964","noYear":false,"title":"Water resources of Van Buren County, Michigan"},"lastModifiedDate":"2013-08-28T14:38:22","indexId":"ofr6461","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-61","title":"Water resources of Van Buren County, Michigan","language":"ENGLISH","publisher":"Michigan Geological Survey Division,","doi":"10.3133/ofr6461","usgsCitation":"Giroux, P., Hendrickson, G.E., Stoimenoff, L., and Whetstone, G., 1964, Water resources of Van Buren County, Michigan: U.S. Geological Survey Open-File Report 64-61, 140 p., 45 figs., vii, 144 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr6461.","productDescription":"140 p., 45 figs., vii, 144 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":149159,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634afd","contributors":{"authors":[{"text":"Giroux, P.R.","contributorId":59055,"corporation":false,"usgs":true,"family":"Giroux","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":178150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hendrickson, G. E.","contributorId":99958,"corporation":false,"usgs":true,"family":"Hendrickson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":178152,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoimenoff, L.E.","contributorId":34157,"corporation":false,"usgs":true,"family":"Stoimenoff","given":"L.E.","email":"","affiliations":[],"preferred":false,"id":178149,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Whetstone, G.W.","contributorId":94680,"corporation":false,"usgs":true,"family":"Whetstone","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":178151,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":1022,"text":"wsp1545C - 1964 - Shortcuts and special problems in aquifer tests","interactions":[{"subject":{"id":51150,"text":"ofr5291 - 1952 - Graphic method for plotting field pumping-test data","indexId":"ofr5291","publicationYear":"1952","noYear":false,"title":"Graphic method for plotting field pumping-test data"},"predicate":"SUPERSEDED_BY","object":{"id":1022,"text":"wsp1545C - 1964 - Shortcuts and special problems in aquifer tests","indexId":"wsp1545C","publicationYear":"1964","noYear":false,"chapter":"C","title":"Shortcuts and special problems in aquifer tests"},"id":1},{"subject":{"id":56096,"text":"ofr57108 - 1957 - The spacing of pumped wells","indexId":"ofr57108","publicationYear":"1957","noYear":false,"title":"The spacing of pumped wells"},"predicate":"SUPERSEDED_BY","object":{"id":1022,"text":"wsp1545C - 1964 - Shortcuts and special problems in aquifer tests","indexId":"wsp1545C","publicationYear":"1964","noYear":false,"chapter":"C","title":"Shortcuts and special problems in aquifer tests"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp1545C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1545","chapter":"C","title":"Shortcuts and special problems in aquifer tests","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1545C","usgsCitation":"Bentall, R., 1964, Shortcuts and special problems in aquifer tests: U.S. Geological Survey Water Supply Paper 1545, ix, 117 p., [4] leaves of plates :ill. ;24 cm., https://doi.org/10.3133/wsp1545C.","productDescription":"ix, 117 p., [4] leaves of plates :ill. ;24 cm.","costCenters":[],"links":[{"id":137934,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1545c/report-thumb.jpg"},{"id":25636,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1545c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25637,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1545c/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25638,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1545c/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25639,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1545c/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25640,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1545c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f3ec9","contributors":{"authors":[{"text":"Bentall, Ray","contributorId":78711,"corporation":false,"usgs":true,"family":"Bentall","given":"Ray","email":"","affiliations":[],"preferred":false,"id":143041,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6142,"text":"pp454F - 1964 - Smaller Foraminifera from the late Tertiary of southern Okinawa","interactions":[],"lastModifiedDate":"2026-02-18T20:37:09.038803","indexId":"pp454F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"454","chapter":"F","title":"Smaller Foraminifera from the late Tertiary of southern Okinawa","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp454F","usgsCitation":"LeRoy, L., 1964, Smaller Foraminifera from the late Tertiary of southern Okinawa: U.S. Geological Survey Professional Paper 454, 58 p., https://doi.org/10.3133/pp454F.","productDescription":"58 p.","costCenters":[],"links":[{"id":33216,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0454f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117823,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0454f/report-thumb.jpg"}],"country":"Japan","otherGeospatial":"southern Okinawa","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              127.72328672550105,\n              26.506872948334575\n            ],\n            [\n              127.60737120655202,\n              26.216323136732505\n            ],\n            [\n              127.61653661967887,\n              26.05342949150092\n            ],\n            [\n              127.71681702211973,\n              26.068436464138607\n            ],\n            [\n              127.96805717016713,\n              26.177360242761907\n            ],\n            [\n              128.02951935230834,\n              26.43351653434496\n            ],\n            [\n              127.72328672550105,\n              26.506872948334575\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f0e4b07f02db5ee073","contributors":{"authors":[{"text":"LeRoy, L.W.","contributorId":91851,"corporation":false,"usgs":true,"family":"LeRoy","given":"L.W.","email":"","affiliations":[],"preferred":false,"id":152189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3092,"text":"wsp1941 - 1964 - Quality of surface waters of the United States, 1962, Parts 1 and 2, North Atlantic slope basins and South Atlantic and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1941","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1941","title":"Quality of surface waters of the United States, 1962, Parts 1 and 2, North Atlantic slope basins and South Atlantic and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1941","usgsCitation":"Love, S.K., 1964, Quality of surface waters of the United States, 1962, Parts 1 and 2, North Atlantic slope basins and South Atlantic and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1941, xi, 434 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1941.","productDescription":"xi, 434 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138644,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1941/report-thumb.jpg"},{"id":29974,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1941/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651ad7","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146261,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13,"text":"wsp1739 - 1964 - Compilation of records of surface waters of Hawaii, July 1950 to June 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1739","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1739","title":"Compilation of records of surface waters of Hawaii, July 1950 to June 1960","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1739","usgsCitation":"Hendricks, E.L., 1964, Compilation of records of surface waters of Hawaii, July 1950 to June 1960: U.S. Geological Survey Water Supply Paper 1739, vii, 136 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1739.","productDescription":"vii, 136 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1739/report-thumb.jpg"},{"id":24612,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24613,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24614,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24615,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24616,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1739/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":24617,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1739/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9087","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":141816,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5794,"text":"pp483E - 1964 - Multinodose scaphitid cephalopods from the lower part of the Pierre Shale and equivalent rocks in the conterminous United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"pp483E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"483","chapter":"E","title":"Multinodose scaphitid cephalopods from the lower part of the Pierre Shale and equivalent rocks in the conterminous United States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp483E","usgsCitation":"Cobban, W.A., and Scott, G.R., 1964, Multinodose scaphitid cephalopods from the lower part of the Pierre Shale and equivalent rocks in the conterminous United States: U.S. Geological Survey Professional Paper 483, p. E1-E13, https://doi.org/10.3133/pp483E.","productDescription":"p. E1-E13","costCenters":[],"links":[{"id":121310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0483e/report-thumb.jpg"},{"id":32477,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0483e/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698b45","contributors":{"authors":[{"text":"Cobban, William Aubrey","contributorId":78317,"corporation":false,"usgs":true,"family":"Cobban","given":"William","email":"","middleInitial":"Aubrey","affiliations":[],"preferred":false,"id":151592,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Glenn R.","contributorId":102046,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":151593,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1335,"text":"wsp1535J - 1964 - Chemical composition of snow in the northern Sierra Nevada and other areas","interactions":[],"lastModifiedDate":"2017-09-06T17:45:05","indexId":"wsp1535J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1535","chapter":"J","title":"Chemical composition of snow in the northern Sierra Nevada and other areas","docAbstract":"<p>Melting snow provides a large part of the water used throughout the western conterminous United States for agriculture, industry, and domestic supply. It is an active agent in chemical weathering, supplies moisture for forest growth, and sustains fish and wildlife. Despite its importance, virtually nothing has been known of the chemical character of snow in the western mountains until the present study.</p><p>Analysis of more than 100 samples, most from the northern Sierra Nevada, but some from Utah, Denver, Colo., and scattered points, shows that melted snow is a dilute solution containing measurable amounts of some or all of the inorganic constituents commonly found in natural water. There are significant regional differences in chemical composition; the progressive increase in calcium content with increasing distance eastward from the west slope of the Sierra Nevada is the most pronounced. The chemical character of individual snowfalls is variable. Some show predominant influence of oceanic salt; others show strong effects of mineralization from continental sources, probably largely dust. Silica and boron were found in about half the samples analyzed for these constituents; precipitation is seldom analyzed for these substances.</p><p>Results of the chemical analyses for major constituents in snow samples are summarized in the following table. The median and mean values for individual constituents are derived from 41-78 samples of Sierra Nevada snow, 6-18 samples of Utah snow, and 6-17 samples of Denver, Colo., snow.</p><p>The sodium, chloride, and perhaps boron found in snow are probably incorporated in moisture-laden air masses as they move over the Pacific Ocean. Silica, although abundant in the silicate-mineral nuclei found in some snowflakes, may be derived in soluble form largely from dust. Calcium, magnesium, and some bicarbonate are probably added by dust of continental origin. The sources of the other constituents remain unknown.</p><p>When snowmelt comes in contact with the lithosphere, the earlier diversity of chemical type largely disappears. The melt water rapidly increases its content of dissolved solids and becomes calcium magnesium bicarbonate in type. Silica, whose concentration increases more than tenfold, shows the largest gain; calcium and bicarbonate contents also increase markedly. Most of the additional mineral matter is from soft and weathered rock; bicarbonate, however, is largely from the soil atmosphere.</p><p>Investigators, some reporting as much as a century ago, concentrated attention largely on nitrogen compounds and seldom reported other constituents except chloride and sulfate. The Northern European precipitation-sampling network provides the most comprehensive collection of data on precipitation chemistry, but it does not segregate snow from other forms of precipitation. The present study establishes with confidence the chemical character of snow in the Sierra Nevada, and suggests that the dissolved-solids content of precipitation increases with increasing distance inland from the Pacific Coast.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1535J","usgsCitation":"Feth, J.H., Rogers, S.M., and Roberson, C.E., 1964, Chemical composition of snow in the northern Sierra Nevada and other areas: U.S. Geological Survey Water Supply Paper 1535, Report: iii, 39 p.; Plate: 28.00 x 21.15 inches, https://doi.org/10.3133/wsp1535J.","productDescription":"Report: iii, 39 p.; Plate: 28.00 x 21.15 inches","numberOfPages":"45","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":26389,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1535j/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26390,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535j/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137406,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535j/report-thumb.jpg"},{"id":109971,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24719.htm","linkFileType":{"id":5,"text":"html"},"description":"24719"}],"country":"United States","state":"Arizona, California, Colorado, Nevada, Oregon, Utah","city":"Denver","otherGeospatial":"Sierra Nevada","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e3c6a","contributors":{"authors":[{"text":"Feth, John Henry Frederick","contributorId":37310,"corporation":false,"usgs":true,"family":"Feth","given":"John","email":"","middleInitial":"Henry Frederick","affiliations":[],"preferred":false,"id":143582,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rogers, S. M.","contributorId":101637,"corporation":false,"usgs":true,"family":"Rogers","given":"S.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":143584,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roberson, Charles Elmer","contributorId":79451,"corporation":false,"usgs":true,"family":"Roberson","given":"Charles","email":"","middleInitial":"Elmer","affiliations":[],"preferred":false,"id":143583,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2796,"text":"wsp1608D - 1964 - Artesian water in the Malabar coastal plain of southern Kerala, India","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"wsp1608D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1608","chapter":"D","title":"Artesian water in the Malabar coastal plain of southern Kerala, India","docAbstract":"The present report is based on a geological and hydrological reconnaissance during 1954 of the Malabar Coastal Plain and adjacent island area of southern Kerala to evaluate the availability of ground water for coastal villages and municipalities and associated industries and the potentialities for future development. The work was done in cooperation with the Geological Survey of India and under the auspices of the U.S. Technical Cooperation Mission to India. The State of Kerala, which lies near the southern tip of India and along the eastern shore of the Caspian Sea, contains a total area of 14,937 square miles. The eastern part of the state is s rugged mountainous highland which attains \r\naltitudes of more than 6,000 feet. This highland descends westward through piedmont upland to s narrow coastal plain, which reaches a maximum width of about 16 miles in the latitude of Shertalli. A tropical monsoon rain-forest climate prevails in most of Kerala, and annual rainfall ranges from 65 to 130 inches in the southern part of the coastal plain to as much a 200 inches in the highland. \r\n\r\nThe highland and piedmont upland tracts of Kerala are underlain by Precambrian meamorphic and igneous rocks belonging in large parabola-the so-called Charnockite Series. Beneath ahe coastal plain are semiconsolidated asunconsolidated sedimentary deposits whose age ranges from Miocene to Recent. These deposits include sofa sandstone and clay shale containing some marl or limestone and sand, and clay and pea containing some gravel. The sofa sandstone, sand, and gravel beds constitute important aquifers a depths ranging from a few tens of feet to 400 feet or more below the land surface. The shallow ground war is under water-able or unconfined conditions, but the deeper aquifers contain water under artesian pressure. Near the coast, drilled wells tapping the deeper aquifers commonly flow with artesian heads as much as 10 to 12 feet above the land surface. \r\n\r\nThe draft from existing wells in the coastal belt between Quilon and Alleppy was estimated at 1 to 1 1/2 million imperial gallons a day. However, favorable conations exist for considerable further ground-water development in the coastal plain provided that sufficient attention is given to the potential hazards of saltwater encroachment and local overdevelopment. It is estimated that the overall potential for development of water from wells is probably at least several tens of millions of gallons a day, and perhaps more, in the Malabar Coastal Plain of southern Kera. Such a draft would have to be well dispersed to avoid overdevelopment and salt-war encroachment.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1608D","usgsCitation":"Taylor, G., and Ghosh, P., 1964, Artesian water in the Malabar coastal plain of southern Kerala, India: U.S. Geological Survey Water Supply Paper 1608, iii, 14 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1608D.","productDescription":"iii, 14 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":138615,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1608d/report-thumb.jpg"},{"id":29292,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29293,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1608d/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29294,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1608d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abbe4b07f02db672c6d","contributors":{"authors":[{"text":"Taylor, George C.","contributorId":45693,"corporation":false,"usgs":true,"family":"Taylor","given":"George C.","affiliations":[],"preferred":false,"id":145806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ghosh, P.K.","contributorId":53771,"corporation":false,"usgs":true,"family":"Ghosh","given":"P.K.","email":"","affiliations":[],"preferred":false,"id":145807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68146,"text":"ha117 - 1964 - Availability of ground water in the Elva quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"117","title":"Availability of ground water in the Elva quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/ha117","usgsCitation":"Morgan, J.H., 1964, Availability of ground water in the Elva quadrangle, Kentucky: U.S. Geological Survey Hydrologic Atlas 117, col. map ;92 x 120 cm., https://doi.org/10.3133/ha117.","productDescription":"col. map ;92 x 120 cm.","costCenters":[],"links":[{"id":101448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/117/report.pdf","size":"46","linkFileType":{"id":1,"text":"pdf"}},{"id":101449,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/117/plate-1.pdf","size":"10186","linkFileType":{"id":1,"text":"pdf"}},{"id":186456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/117/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,36.8675 ], [ -88.5,37 ], [ -88.36749999999999,37 ], [ -88.36749999999999,36.8675 ], [ -88.5,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dd81","contributors":{"authors":[{"text":"Morgan, J. H.","contributorId":9243,"corporation":false,"usgs":true,"family":"Morgan","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32718,"text":"pp448I - 1964 - Low-flow characteristics of streams in the Mississippi embayment in Mississippi and Alabama, with a section on quality of the water","interactions":[],"lastModifiedDate":"2021-09-02T19:22:47.501234","indexId":"pp448I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"448","chapter":"I","title":"Low-flow characteristics of streams in the Mississippi embayment in Mississippi and Alabama, with a section on quality of the water","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of the Mississippi embayment","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp448I","usgsCitation":"Speer, P.R., Golden, H.G., Patterson, J.F., and Welborne, W.J., 1964, Low-flow characteristics of streams in the Mississippi embayment in Mississippi and Alabama, with a section on quality of the water: U.S. Geological Survey Professional Paper 448, Report: iv, 47 p.; 3 Plates; 45.50 × 30.50 inches or smaller, https://doi.org/10.3133/pp448I.","productDescription":"Report: iv, 47 p.; 3 Plates; 45.50 × 30.50 inches or smaller","costCenters":[],"links":[{"id":388461,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4452.htm"},{"id":60636,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448i/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60635,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448i/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60634,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0448i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":60637,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0448i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0448i/report-thumb.jpg"}],"country":"United States","state":"Alabama, Mississippi","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -91.2306,\n              32.00\n            ],\n            [\n              -87.0,\n              32.00\n            ],\n            [\n              -87.0,\n              35.00\n            ],\n            [\n              -91.2306,\n              35.00\n            ],\n            [\n              -91.2306,\n              32.00\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602c7d","contributors":{"authors":[{"text":"Speer, P. R.","contributorId":104948,"corporation":false,"usgs":true,"family":"Speer","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":209020,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Golden, H. G.","contributorId":56280,"corporation":false,"usgs":true,"family":"Golden","given":"H.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":209017,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Patterson, J. F.","contributorId":98776,"corporation":false,"usgs":true,"family":"Patterson","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":209019,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Welborne, W. J.","contributorId":59857,"corporation":false,"usgs":true,"family":"Welborne","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":209018,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":2046,"text":"wsp1499G - 1964 - Water resources of the Green Bay area, Wisconsin","interactions":[],"lastModifiedDate":"2021-08-16T21:39:30.070959","indexId":"wsp1499G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"1499","chapter":"G","title":"Water resources of the Green Bay area, Wisconsin","docAbstract":"<p>The Green Bay area comprises an area of about 525 square miles in eastern Wisconsin at the south end of Green Bay. It includes the western three-fourths of Brown County and the eastern one-ninth of Outagamie County. In 1960, the population of the area was estimated at 124,000.</p>\n<p>The most prominent topographic feature is the northwest-facing, southwestward trending Niagara escarpment. The area northwest of the escarpment drains into Green Bay via the Fox River, Suamico River, Duck Creek, and their tributaries. The area southeast of the escarpment is drained by streams that flow into Lake Michigan.</p>\n<p>The chief sources of surface water in the Green Bay area are the Fox River, Green Bay, and Lake Michigan. Smaller amounts of water are available from the East and Suamico Rivers and other streams. A sandstone aquifer is the principal source of the ground-water supply. The Niagara dolomite, although largely undeveloped, is potentially an important aquifer in the eastern part of the area. Small amounts of water are obtained also from the Platteville formation and from deposits of Pleistocene and Recent age. Water from the surfaceand ground-water sources is moderately hard to very hard.</p>\n<p>The Fox River, tributary to Lake Michigan at Green Bay, is a significant source of water for industrial use in the Green Bay area. The Menasha Dam, which controls release of water from the Lake Winnebago pool, is the major regulation on the Fox River, and it has considerable effect in reducing peak flows and supplementing low flows in the lower Fox River. The average discharge of the lower Fox River for the period 1898-1959, as measured at the gaging station at Rapide Croche Dam, was 2,687 mgd (million gallons per day). The longest consecutive period during which the discharge averaged less than 500 mgd was 80 days. The average discharge can be expected to fall below 700 mgd about once every 5 years for a 7-day period. In 1959, the average withdrawal of water from the Fox River was about 62 mgd. The water in the river is of the calcium magnesium bicarbonate type and is hard.</p>\n<p>The small streams in the area are utilized chiefly for stock watering; some of the water, however, is used for irrigation. The water in the small streams is more highly mineralized than the water in the Fox River and is very hard.</p>\n<p>Large quantities of water are available from Green Bay, but the disposal of industrial waste into the bay has restricted the use of the water. The major withdrawal is for condenser cooling, and, in 1959, it averaged about 415 mgd. The water from Green Bay is moderately hard but is of better chemical quality than the water from the Fox River and the small streams in the area.</p>\n<p>The only withdrawals of water from Lake Michigan for use in the Green Bay area are made by the city of Green Bay. In 1959, these withdrawals averaged 7.8 mgd.</p>\n<p>The lower Fox River is not subject to extremes of flow owing to the dampening effect of the Lake Winnebago pool and the regulation of flow at Menasha Dam. Cloudbursts over the lower Fox River valley below Menasha Dam, however, have occasionally caused extremely high water, as in 1922, when the discharge at the mouth of the Fox River was estimated to be about 50,000 mgd. Daily discharges greater than about 13,000 mgd occurred only 7 times in the period 1918-59. The 50-year flood of 15,500 mgd represents an average runoff of less than 2.6 mgd per square mile of drainage area, a relatively low runoff for a 50-year flood in Wisconsin.</p>\n<p>The sandstone aquifer is the principal source of ground water in the Green Bay area and furnishes water for public supply and industrial use. This aquifer includes rocks of Late Cambrian age, and the Prairie du Chien group and St. Peter sandstone of Ordovician age; it ranges in thickness from 550 to 640 feet. Ground water is found in openings along fractures and bedding planes and in the interstices between sand grains.</p>\n<p>The sandstone aquifer can support additional development of large supplies of ground water. Wells can be developed in most of the area that will yield 500 gpm (gallons per minute) or more, provided they are properly spaced and penetrate the entire thickness of the aquifer. It is estimated that the perennial yield of the sandstone in the Green Bay area could be at least 30 mgd if the aquifer is properly developed; only 5.4 mgd was withdrawn in 1959. The water from this sandstone aquifer is of the calcium magnesium bicarbonate type, is very hard, and, at a few places, contains objectionable amounts of iron.</p>\n<p>The Niagara dolomite, potentially a source of moderate to large quantities of water in the eastern part of the area, probably will yield 500 gpm or more to wells.</p>\n<p>In 1959, the average withdrawal of water for all uses was estimated at 495 mgd, of which 98.2 percent was from surface-water sources and 1.8 percent was from wells. About 485 mgd of water was withdrawn for industrial use, 6 mgd for public supply, and 4 mgd for rural use. The industrial use of water averaged 441 mgd for condenser cooling, 38 mgd fot processing by the paper industry, and 6 mgd for other industrial uses. The city of Green Bay used 7.8 mgd of water from Lake Michigan; other public supplies in the area used 2.6 mgd from wells. Of the withdrawals of water for rural use, about 75 percent was from wells and about 25 percent was from streams.</p>\n<p>The discharge of wastes into the lower Fox River and its tributary streams has altered the quality of the natural water. The wastes consist chiefly of treated municipal sewage and treated and untreated wastes from the paper industry, rendering plants, a sugar mill, and other industries. The industrial waste makes up about 90 percent of the oxygen-demand loading in the lower Fox River, and treated municipal sewage accounts for about 10 percent. The dissolved-oxygen concentration of water in the lower Fox River decreases rapidly in the vicinity of Green Bay during the summer when the river water is warm. If the periods when the river water is warmest, generally during July and early August, were to coincide with periods of lowest annual streamflow, generally in late August, the river would be unable to assimilate the loading of decomposable organic matter.</p>\n<p>In an emergency, industrial and public supply wells could supply at least 6 mgd for a sustained period and probably as much as 10 mgd for a period of several days. Six of the wells that formerly supplied the city of Green Bay are maintained in operating condition and could furnish about the same quantity of water as the industrial and other public supply wells. Small streams in the area would be supplemental sources of water, and the water in the Fox River and Green Bay is easily accessible.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water resources of industrial regions: A summary of the source, occurrence, availability, and use of water in the area","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1499G","usgsCitation":"Knowles, D.B., Dreher, F.C., and Whetstone, G.W., 1964, Water resources of the Green Bay area, Wisconsin: U.S. Geological Survey Water Supply Paper 1499, Report: v, 67 p.; 1 Plate: 23.50 x 31.95 inches, https://doi.org/10.3133/wsp1499G.","productDescription":"Report: v, 67 p.; 1 Plate: 23.50 x 31.95 inches","numberOfPages":"78","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[{"id":677,"text":"Wisconsin Water Science Center","active":true,"usgs":true}],"links":[{"id":27567,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1499g/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27568,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1499g/report.pdf"},{"id":387952,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24443.htm"},{"id":137727,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1499g/report-thumb.jpg"}],"country":"United States","state":"Wisconsin","county":"Brown County, Oconto County, Outagamie County","city":"Green Bay","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.25,\n              44.25\n            ],\n            [\n              -88.25,\n              44.6670\n            ],\n            [\n              -87.90,\n              44.6670\n            ],\n            [\n              -87.90,\n              44.25\n            ],\n            [\n              -88.25,\n              44.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634ad6","contributors":{"authors":[{"text":"Knowles, Doyle Blewer","contributorId":9633,"corporation":false,"usgs":true,"family":"Knowles","given":"Doyle","email":"","middleInitial":"Blewer","affiliations":[],"preferred":false,"id":144585,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dreher, F. C.","contributorId":93878,"corporation":false,"usgs":true,"family":"Dreher","given":"F.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144587,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whetstone, George Walter","contributorId":30603,"corporation":false,"usgs":true,"family":"Whetstone","given":"George","email":"","middleInitial":"Walter","affiliations":[],"preferred":false,"id":144586,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":62381,"text":"gq299 - 1964 - Geology of the Adolphus quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2012-02-10T00:10:45","indexId":"gq299","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"299","title":"Geology of the Adolphus quadrangle, Kentucky-Tennessee","language":"ENGLISH","doi":"10.3133/gq299","usgsCitation":"Nelson, W.H., 1964, Geology of the Adolphus quadrangle, Kentucky-Tennessee: U.S. Geological Survey Geologic Quadrangle 299, 1 map., https://doi.org/10.3133/gq299.","productDescription":"1 map.","costCenters":[],"links":[{"id":102308,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_757.htm","linkFileType":{"id":5,"text":"html"},"description":"757"},{"id":248556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0299/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253700,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0299/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.36749999999999,36.6175 ], [ -86.36749999999999,36.75 ], [ -86.25,36.75 ], [ -86.25,36.6175 ], [ -86.36749999999999,36.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db683651","contributors":{"authors":[{"text":"Nelson, Willis H.","contributorId":84777,"corporation":false,"usgs":true,"family":"Nelson","given":"Willis","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":267305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52396,"text":"ofr6443 - 1964 - Availability of ground water for irrigation on the Pojoaque Pueblo Grant, Santa Fe County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr6443","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-43","title":"Availability of ground water for irrigation on the Pojoaque Pueblo Grant, Santa Fe County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr6443","usgsCitation":"Dinwiddie, G., 1964, Availability of ground water for irrigation on the Pojoaque Pueblo Grant, Santa Fe County, New Mexico: U.S. Geological Survey Open-File Report 64-43, 14 p., https://doi.org/10.3133/ofr6443.","productDescription":"14 p.","costCenters":[],"links":[{"id":100169,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0043/report.pdf","size":"8000","linkFileType":{"id":1,"text":"pdf"}},{"id":177687,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0043/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667e5f","contributors":{"authors":[{"text":"Dinwiddie, G.A.","contributorId":49798,"corporation":false,"usgs":true,"family":"Dinwiddie","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":245278,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":52395,"text":"ofr6442 - 1964 - Geology of the 410 area, Nevada Test Site, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr6442","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","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":"64-42","title":"Geology of the 410 area, Nevada Test Site, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr6442","usgsCitation":"Davis, R.E., 1964, Geology of the 410 area, Nevada Test Site, Nye County, Nevada: U.S. Geological Survey Open-File Report 64-42, 24 p., https://doi.org/10.3133/ofr6442.","productDescription":"24 p.","costCenters":[],"links":[{"id":177241,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68357e","contributors":{"authors":[{"text":"Davis, R. E.","contributorId":77153,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":245277,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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