{"pageNumber":"6673","pageRowStart":"166800","pageSize":"25","recordCount":184652,"records":[{"id":45836,"text":"ofr64154 - 1964 - Location of geologic field projects as of June 30, 1964; Location of geologic field projects in Alaska as of June 30, 1964","interactions":[],"lastModifiedDate":"2012-02-02T00:04:59","indexId":"ofr64154","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":"64-154","title":"Location of geologic field projects as of June 30, 1964; Location of geologic field projects in Alaska as of June 30, 1964","language":"ENGLISH","doi":"10.3133/ofr64154","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Location of geologic field projects as of June 30, 1964; Location of geologic field projects in Alaska as of June 30, 1964: U.S. Geological Survey Open-File Report 64-154, 1 map on 2 sheets., https://doi.org/10.3133/ofr64154.","productDescription":"1 map on 2 sheets.","costCenters":[],"links":[{"id":135905,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63be98","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":531650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2253,"text":"wsp1777 - 1964 - Geology and ground-water resources of Washington County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1777","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":"1777","title":"Geology and ground-water resources of Washington County, Colorado","docAbstract":"Washington County, in northeastern Colorado, has an area of 2,520 square miles. The eastern two-thirds of the county, part of the High Plains physiographic section, is relatively flat and has been moderately altered by the deposition of loess and dune sand, and by stream erosion. The western one-third is a part of the South Platte River basin and has been deeply dissected by tributary streams. The soils and climate of the county are generally suited for agriculture, which is the principal industry. \r\n\r\nThe rocks that crop out in the county influence the availability of ground water. The Pierre Shale, of Late Cretaceous age, underlies the entire area and ranges in thickness from 2,000 to 4,500 feet. This dense shale is a barrier to the downward movement of water and yields little or no water to wells. The Chadron Formation, of Oligocene age, overlies the Pierre Shale in the northern and central parts of the area. The thickness of the formation ranges from a few feet to about 300 feet. Small to moderate quantities of water are available from the scattered sand lenses and from the highly fractured zones of the siltstone. The Ogallala Formation, of Pliocene age, overlies the Chadron Formation and in Washington County forms the High Plains section of the Great Plains province. The thickness of the Ogallala Formation ranges from 0 to about 400 feet, and the yield from wells ranges from a few gallons per hour to about 1,500 gpm. Peorian loess, of Pleistocene age, and dune sand, of Pleistocene to Recent age, mantle a large pan of the county and range in thickness from a few inches to about 120 feet Although the loess and dune sand yield little water to wells, they absorb much of the precipitation and conduct the water to underlying formations. Alluvium, of Pleistocene and Recent age, occupies most of the major stream valleys in thicknesses of a few feet to about 250 feet. The yield of wells tapping the alluvium ranges from a few gallons per minute to about 3,000 gpm, according to the thickness of saturated material. \r\n\r\nDevelopment of ground water for irrigation has been generally restricted to the South Platte, Arikaree, and Beaver valleys. There were 134 irrigation wells, 3 industrial wells, and 10 municipal wells in the county in 1959. The annual ground-water pumpage from Washington County is estimated to be 18,000 acre-ft; about 10,000 acre-ft is from the High Plains ground-water province. Although some ground water enters the county as underflow, most of the recharge to ground-water reservoirs is from precipitation on the land surface. Recharge to the Ogallala Formation in the county is assumed to be approximately equal to the natural discharge from the county by underflow because ground-water withdrawals are from storage, and no other significant amount of natural discharge is apparent. Undertow in the Ogallala was calculated to be 83,000 acre-ft per year and the rate of recharge from precipitation to be about 0.95 inch per year. Neither recharge nor discharge was calculated for that part of the county in the South Platte River basin. \r\n\r\nAll ground water in Washington County has a high proportion of carbonate and is classed as hard to very hard. The sodium-adsorption-ratio for all samples analyzed was below the limit recommended for irrigation water. All the water from the Ogallala Formation and most of the water from the Chadron Formation is suitable for domestic use. Some water from the alluvial deposits overlying the Pierre Shale was exceptionally high in calcium, magnesium, and sodium sulfates. \r\n\r\nGround water has been heavily developed for irrigation in the South Platte valley and in some parts of the Beaver and Arikaree valleys. Some additional areas, however, could be developed in the latter two valleys. Large quantities of ground water in the Ogallala Formation are available for future development. The quantity of water in storage in the High Plains ground-water province in Washington County is about 6.5 million acre-f","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1777","usgsCitation":"McGovern, H.E., 1964, Geology and ground-water resources of Washington County, Colorado: U.S. Geological Survey Water Supply Paper 1777, iv, 46 p. :illus., maps (4 fold. 1 col., in pocket) ;24 cm., https://doi.org/10.3133/wsp1777.","productDescription":"iv, 46 p. :illus., maps (4 fold. 1 col., in pocket) ;24 cm.","costCenters":[],"links":[{"id":110015,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24953.htm","linkFileType":{"id":5,"text":"html"},"description":"24953"},{"id":137835,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1777/report-thumb.jpg"},{"id":28024,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28025,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28026,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28027,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1777/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28028,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1777/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68580b","contributors":{"authors":[{"text":"McGovern, Harold E.","contributorId":9634,"corporation":false,"usgs":true,"family":"McGovern","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144901,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61736,"text":"gq289 - 1964 - Geology of the Tygarts Valley quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:49","indexId":"gq289","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":"289","title":"Geology of the Tygarts Valley quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq289","usgsCitation":"Sheppard, R.A., 1964, Geology of the Tygarts Valley quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 289, 1 map., https://doi.org/10.3133/gq289.","productDescription":"1 map.","costCenters":[],"links":[{"id":102297,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_746.htm","linkFileType":{"id":5,"text":"html"},"description":"746"},{"id":248034,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0289/report.pdf","size":"31","linkFileType":{"id":1,"text":"pdf"}},{"id":252694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0289/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.11749999999999,38.3675 ], [ -83.11749999999999,38.5 ], [ -83,38.5 ], [ -83,38.3675 ], [ -83.11749999999999,38.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca77","contributors":{"authors":[{"text":"Sheppard, Richard A.","contributorId":41815,"corporation":false,"usgs":true,"family":"Sheppard","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63676,"text":"gp370 - 1964 - Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri","interactions":[{"subject":{"id":42556,"text":"ofr5159 - 1951 - Preliminary total-intensity aeromagnetic maps of three Arkansas quadrangles-Bald Knob, Pleasant Plains, and Cave City","indexId":"ofr5159","publicationYear":"1951","noYear":false,"title":"Preliminary total-intensity aeromagnetic maps of three Arkansas quadrangles-Bald Knob, Pleasant Plains, and Cave City"},"predicate":"SUPERSEDED_BY","object":{"id":63676,"text":"gp370 - 1964 - Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri","indexId":"gp370","publicationYear":"1964","noYear":false,"title":"Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri"},"id":1},{"subject":{"id":42557,"text":"ofr5161 - 1951 - Preliminary total-intensity aeromagnetic maps of three Arkansas quadrangles--Newport, Augusta, and Strawberry","indexId":"ofr5161","publicationYear":"1951","noYear":false,"title":"Preliminary total-intensity aeromagnetic maps of three Arkansas quadrangles--Newport, Augusta, and Strawberry"},"predicate":"SUPERSEDED_BY","object":{"id":63676,"text":"gp370 - 1964 - Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri","indexId":"gp370","publicationYear":"1964","noYear":false,"title":"Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri"},"id":2}],"lastModifiedDate":"2025-04-23T20:03:26.840641","indexId":"gp370","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"370","title":"Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp370","usgsCitation":"Jespersen, A., 1964, Aeromagnetic prospecting for bauxite deposits in the Mississippi embayment, Arkansas and Missouri: U.S. Geological Survey Geophysical Investigations Map 370, 1 Plate: 41.95 x 33.00 inches, https://doi.org/10.3133/gp370.","productDescription":"1 Plate: 41.95 x 33.00 inches","costCenters":[],"links":[{"id":484935,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3307.htm","linkFileType":{"id":5,"text":"html"}},{"id":260533,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0370/plate-1.pdf"},{"id":187106,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"25000","country":"United States","state":"Arkansas","otherGeospatial":"Mississippi embayment","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -91.25,\n              36\n            ],\n            [\n              -91.75,\n              36\n            ],\n            [\n              -91.75,\n              35.25\n            ],\n            [\n              -91.25,\n              35.25\n            ],\n            [\n              -91.25,\n              36\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689e2f","contributors":{"authors":[{"text":"Jespersen, Anna","contributorId":71264,"corporation":false,"usgs":true,"family":"Jespersen","given":"Anna","email":"","affiliations":[],"preferred":false,"id":269360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":97,"text":"wsp1781 - 1964 - Ground-water levels in the United States, 1957-61, North-central states","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1781","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":"1781","title":"Ground-water levels in the United States, 1957-61, North-central states","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1781","usgsCitation":"Hackett, O.M., 1964, Ground-water levels in the United States, 1957-61, North-central states: U.S. Geological Survey Water Supply Paper 1781, v, 148 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1781.","productDescription":"v, 148 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":136215,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1781/report-thumb.jpg"},{"id":24703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1781/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6675b6","contributors":{"authors":[{"text":"Hackett, O. M.","contributorId":38527,"corporation":false,"usgs":true,"family":"Hackett","given":"O.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":141925,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63533,"text":"gp450 - 1964 - Aeromagnetic map of part of the Canaan quadrangle, Berkshire County, Massachusetts, and Columbia and Rensselaer Counties, New York","interactions":[],"lastModifiedDate":"2025-05-05T18:34:44.458097","indexId":"gp450","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"450","title":"Aeromagnetic map of part of the Canaan quadrangle, Berkshire County, Massachusetts, and Columbia and Rensselaer Counties, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp450","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of part of the Canaan quadrangle, Berkshire County, Massachusetts, and Columbia and Rensselaer Counties, New York: U.S. Geological Survey Geophysical Investigations Map 450, 1 Plate: 21.43 x 27.35 inches, https://doi.org/10.3133/gp450.","productDescription":"1 Plate: 21.43 x 27.35 inches","costCenters":[],"links":[{"id":485036,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3395.htm","linkFileType":{"id":5,"text":"html"}},{"id":249678,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0450/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249679,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0450/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253171,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0450/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts, New York","county":"Berkshire County, Columbia County, Rensselaer County","otherGeospatial":"Canaan quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.5,\n              42.5\n            ],\n            [\n              -73.5,\n              42.375\n            ],\n            [\n              -73.375,\n              42.375\n            ],\n            [\n              -73.375,\n              42.5\n            ],\n            [\n              -73.5,\n              42.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6979bf","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269069,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269070,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269068,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63531,"text":"gp453 - 1964 - Aeromagnetic map of the Hancock quadrangle, Berkshire County, Massachusetts, and Rensselaer County, New York","interactions":[],"lastModifiedDate":"2025-04-24T20:52:25.297336","indexId":"gp453","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"453","title":"Aeromagnetic map of the Hancock quadrangle, Berkshire County, Massachusetts, and Rensselaer County, New York","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp453","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Hancock quadrangle, Berkshire County, Massachusetts, and Rensselaer County, New York: U.S. Geological Survey Geophysical Investigations Map 453, 1 Plate: 21.80 x 27.48 inches, https://doi.org/10.3133/gp453.","productDescription":"1 Plate: 21.80 x 27.48 inches","costCenters":[],"links":[{"id":485039,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3398.htm","linkFileType":{"id":5,"text":"html"}},{"id":253169,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0453/report-thumb.jpg"},{"id":249672,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0453/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249671,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0453/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts, New York","county":"Berkshire County, Rensselaer County","otherGeospatial":"Hancock quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.375,\n              42.625\n            ],\n            [\n              -73.375,\n              42.5\n            ],\n            [\n              -73.25,\n              42.5\n            ],\n            [\n              -73.25,\n              42.625\n            ],\n            [\n              -73.375,\n              42.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db69208a","contributors":{"authors":[{"text":"Popenoe, Peter","contributorId":62206,"corporation":false,"usgs":true,"family":"Popenoe","given":"Peter","email":"","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":269064,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boynton, G. R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":269065,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zandle, G. L.","contributorId":39863,"corporation":false,"usgs":true,"family":"Zandle","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":269063,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35276,"text":"b1142L - 1964 - Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b1142L","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":"1142","chapter":"L","title":"Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1142L","usgsCitation":"Morris, H.T., 1964, Geology of the Tintic Junction quadrangle, Tooele, Juab, and Utah Counties, Utah: U.S. Geological Survey Bulletin 1142, p. L1-L23, :fold. col. map (in pocket) ;24 cm., https://doi.org/10.3133/b1142L.","productDescription":"p. L1-L23, :fold. col. map (in pocket) ;24 cm.","costCenters":[],"links":[{"id":109414,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20885.htm","linkFileType":{"id":5,"text":"html"},"description":"20885"},{"id":166972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1142l/report-thumb.jpg"},{"id":63135,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1142l/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63136,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1142l/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cab4","contributors":{"authors":[{"text":"Morris, H. T.","contributorId":15585,"corporation":false,"usgs":true,"family":"Morris","given":"H.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":214362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2186,"text":"wsp1747 - 1964 - Geology and hydrology of the West Milton area, Saratoga County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp1747","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":"1747","title":"Geology and hydrology of the West Milton area, Saratoga County, New York","docAbstract":"This report describes the geology, ground-water conditions, streamflow characteristics, and quality of water in the West Milton area, Saratoga County, N.Y. The West Milton area is in the east-central part of New York in the hilly region that forms a transition zone between the Adirondack Mountains and the Hudson-Mohawk valley lowland. Bedrock underlying the area consists of crystalline rocks of Precambrian age and sandstone, dolomite, limestone, and shale formations of Cambrian and Ordovician age. The formations have been moderately folded and have been displaced as much as several hundred feet' along at least three northeast-trending normal faults. The bedrock is overlain in nearly all parts of the area by a layer of unconsolidated deposits which ranges in thickness from a few feet to more than 200 feet. The unconsolidated deposits are of Pleistocene age and consist of unstratified materials (till) laid down by glacial ice at stratified sediments deposited by glacial meltwaters. The topography of the bedrock surface differs greatly from the topography of the land surface. Although not evident in the present topography, at least two channels, cut in bedrock by preglacial streams, pass through the area. \r\n\r\nGround-water supplies adequate to satisfy domestic requirements can be obtained from wells in any part of the area. Large ground-water supplies may be taken from coarse-grained stratified deposits comprising two aquifers in the valley of Kayaderosseras Creek. The Atomic Energy Commission has pumped as much as 1 mgd from a horizontal well drawing from the uppermost aquifer which is composed of flood-plain deposits. Part of the water yielded by this well during extended periods of pumping is induced flow from the creek. Three nearby vertical wells drilled by the Commission comprise a separate well field capable of yielding at least 2 mgd and possibly as much as 3 mgd from the deeper stratified deposits underlying the valley. A pumping test showed that at near the center of this well field the coefficient of transmissibility is about 125,000 gpd per ft and the coefficient of storage is about 0.0003. The water obtained from the sand and gravel has a hardness of about 125 ppm and contains about 150 ppm of dissolved solids. \r\n\r\nMost of the Government reservation is drained by Glowegee Creek, one of the larger tributaries of Kayaderosseras Creek. The average streamflow of Kayaderosseras Creek at West Milton is 141 cfs or about 1.5 cfs per sq. mi. The monthly mean discharge has ranged from a low of 21.7 cfs in September 1958 to a high of 866 cfs in March 1936, and the annual mean discharge has ranged from 94.5 cfs in 1941 to 198 cfs in 1952. The mean annual flood is 1,740 cfs and the 50-year flood is 5,300 cfs. \r\n\r\nStreamflow data have been collected on Glowegee Creek since 1948 at a station 0.5 mile south of West Milton. The average streamflow of Glowegee Creek at this station is 41 cfs or about 1.5 cfs per sq mi. The mean annual flood is 740 cfs and the 50-year flood is 2,250 cfs. \r\n\r\nThe quality of the water in both Kayaderosseras Creek and Glowegee Creek is satisfactory for public supply and most industrial purposes. The mineral content of both streams is low--the dissolved-solids content averaging about 93 ppm in Kayaderosseras Creek and about 131 ppm in Glowegee Creek. The average hardness of water in Kayaderosseras Creek and Glowegee Creek is 68 ppm and 102 ppm, respectively. During periods of low flow, suspended sediment discharge in both streams is less than 10 tons per day, but during periods of high flow, the sediment discharge has been as great as 163 tons per day in Glowegee Creek and 437 tons per day in Kayaderosseras Creek.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1747","usgsCitation":"Mack, F., Pauszek, F.H., and Crippen, J.R., 1964, Geology and hydrology of the West Milton area, Saratoga County, New York: U.S. Geological Survey Water Supply Paper 1747, viii, 110 p. :illus., maps, diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1747.","productDescription":"viii, 110 p. :illus., maps, diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":137741,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1747/report-thumb.jpg"},{"id":27816,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27817,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27818,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27819,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27820,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27821,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1747/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27815,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1747/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4691","contributors":{"authors":[{"text":"Mack, Frederick K.","contributorId":95858,"corporation":false,"usgs":true,"family":"Mack","given":"Frederick K.","affiliations":[],"preferred":false,"id":144794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pauszek, F. H.","contributorId":61399,"corporation":false,"usgs":true,"family":"Pauszek","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":144793,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crippen, John R.","contributorId":13208,"corporation":false,"usgs":true,"family":"Crippen","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":144792,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61289,"text":"mf292 - 1964 - Geologic map of the Continental Peak quadrangle, Fremont and Sweetwater Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf292","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"292","title":"Geologic map of the Continental Peak quadrangle, Fremont and Sweetwater Counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf292","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Continental Peak quadrangle, Fremont and Sweetwater Counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 292, 1 map., https://doi.org/10.3133/mf292.","productDescription":"1 map.","costCenters":[],"links":[{"id":104063,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2712.htm","linkFileType":{"id":5,"text":"html"},"description":"2712"},{"id":182974,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,42.25 ], [ -108.75,42.3675 ], [ -108.61749999999999,42.3675 ], [ -108.61749999999999,42.25 ], [ -108.75,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c85a","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265331,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265330,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61292,"text":"mf294 - 1964 - Geologic map of the Pacific Springs quadrangle, Fremont and Sweetwater Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf294","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"294","title":"Geologic map of the Pacific Springs quadrangle, Fremont and Sweetwater Counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf294","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Pacific Springs quadrangle, Fremont and Sweetwater Counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 294, 1 map ;58 x 43 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf294.","productDescription":"1 map ;58 x 43 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104065,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2714.htm","linkFileType":{"id":5,"text":"html"},"description":"2714"},{"id":183756,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109,42.25 ], [ -109,42.3675 ], [ -108.86749999999999,42.3675 ], [ -108.86749999999999,42.25 ], [ -109,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db6921e4","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265336,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61293,"text":"mf296 - 1964 - Geologic map of the Parting of the Ways quadrangle, Sublette and Sweetwater Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf296","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"296","title":"Geologic map of the Parting of the Ways quadrangle, Sublette and Sweetwater Counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf296","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Parting of the Ways quadrangle, Sublette and Sweetwater Counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 296, 1 map ;58 x 43 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf296.","productDescription":"1 map ;58 x 43 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104067,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2716.htm","linkFileType":{"id":5,"text":"html"},"description":"2716"},{"id":182273,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.25,42.25 ], [ -109.25,42.3675 ], [ -109.11749999999999,42.3675 ], [ -109.11749999999999,42.25 ], [ -109.25,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d35","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265339,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265338,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61295,"text":"mf297 - 1964 - Geologic map of the Tule Butte quadrangle, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf297","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"297","title":"Geologic map of the Tule Butte quadrangle, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/mf297","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Tule Butte quadrangle, Sweetwater County, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 297, 1 map ;58 x 43 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf297.","productDescription":"1 map ;58 x 43 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104068,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2717.htm","linkFileType":{"id":5,"text":"html"},"description":"2717"},{"id":182980,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.25,42.1175 ], [ -109.25,42.25 ], [ -109.11749999999999,42.25 ], [ -109.11749999999999,42.1175 ], [ -109.25,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635bb3","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265341,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61296,"text":"mf288 - 1964 - Geology of the NE1/4 of Freighter Gap quadrangle, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf288","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"288","title":"Geology of the NE1/4 of Freighter Gap quadrangle, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/mf288","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geology of the NE1/4 of Freighter Gap quadrangle, Sweetwater County, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 288, 1 map ;58 x 43 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf288.","productDescription":"1 map ;58 x 43 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104059,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2707.htm","linkFileType":{"id":5,"text":"html"},"description":"2707"},{"id":182981,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.86749999999999,42.1175 ], [ -108.86749999999999,42.25 ], [ -108.75,42.25 ], [ -108.75,42.1175 ], [ -108.86749999999999,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e933","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265343,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61299,"text":"mf286 - 1964 - Geology of the Pinnacles NW quadrangle, Sweetwater County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf286","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"286","title":"Geology of the Pinnacles NW quadrangle, Sweetwater County, Wyoming","language":"ENGLISH","doi":"10.3133/mf286","usgsCitation":"Zeller, H.D., and Stephens, E.V., 1964, Geology of the Pinnacles NW quadrangle, Sweetwater County, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 286, 1 map ;58 x 43 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf286.","productDescription":"1 map ;58 x 43 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104057,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2705.htm","linkFileType":{"id":5,"text":"html"},"description":"2705"},{"id":182984,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,42.1175 ], [ -108.75,42.25 ], [ -108.61749999999999,42.25 ], [ -108.61749999999999,42.1175 ], [ -108.75,42.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e864","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265350,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. Vernon","contributorId":89588,"corporation":false,"usgs":true,"family":"Stephens","given":"E.","email":"","middleInitial":"Vernon","affiliations":[],"preferred":false,"id":265349,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3487,"text":"cir484 - 1964 - Exploratory laboratory study of lateral turbulent diffusion at the surface of an alluvial channel","interactions":[],"lastModifiedDate":"2018-01-02T19:49:07","indexId":"cir484","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":"484","title":"Exploratory laboratory study of lateral turbulent diffusion at the surface of an alluvial channel","docAbstract":"In natural streams turbulent diffusion is one of the principal mechanisms by which liquid and suspended-particulate contaminants are dispersed in the flow. A knowledge of turbulence characteristics is therefore essential in predicting the dispersal rates of contaminants in streams. In this study the theory of diffusion by continuous movements for homogeneous turbulence is applied to lateral diffusion at the surface of an open channel in which there is uniform flow. An exploratory-laboratory investigation was conducted in which the lateral dispersion at the water surface of a sand-Led flume was studied by measuring the lateral spread from a point source of small floating polyethylene articles. The experiment was restricted to a single set of low and channel geometry conditions. \r\n\r\nThe results of the study indicate that with certain restrictions lateral dispersion in alluvial channels may be successfully described by the theory of diffusion by continuous movements. The experiment demonstrates a means for evaluating the lateral diffusion coefficient and also methods for quantitatively estimating fundamental turbulence properties, such as the intensity and the Lagrangian integral scale of turbulence in an alluvial channel. \r\n\r\nThe experimental results show that with increasing distance from the source the coefficient of lateral turbulent diffusion increases initially but tends toward a constant limiting value. This result is in accordance with turbulent diffusion theory. Indications are that the distance downstream from the source required for the diffusion coefficient to reach its limiting value is actually very small when compared to the length scale of most diffusion phenomena in natural streams which are of practical interest.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir484","usgsCitation":"Sayre, W., and Chamberlain, A., 1964, Exploratory laboratory study of lateral turbulent diffusion at the surface of an alluvial channel: U.S. Geological Survey Circular 484, iv, 18 p. :illus. ;27cm., https://doi.org/10.3133/cir484.","productDescription":"iv, 18 p. :illus. ;27cm.","costCenters":[],"links":[{"id":30496,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0484/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124792,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0484/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db60238e","contributors":{"authors":[{"text":"Sayre, William W.","contributorId":93894,"corporation":false,"usgs":true,"family":"Sayre","given":"William W.","affiliations":[],"preferred":false,"id":147017,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chamberlain, A.R.","contributorId":11597,"corporation":false,"usgs":true,"family":"Chamberlain","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":147016,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3486,"text":"cir485 - 1964 - Lithologic variations in slope development theory","interactions":[],"lastModifiedDate":"2018-01-02T19:49:05","indexId":"cir485","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":"485","title":"Lithologic variations in slope development theory","docAbstract":"This paper presents a comprehensive review and amplification of the writer's earlier slope development theory. In particular, the influence of lithology on evolving slope profiles is investigated and calculations are made for various conditions, such as presence of caprock, soft bottom, and hard and soft intermediate layers.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir485","usgsCitation":"Scheidegger, A.E., 1964, Lithologic variations in slope development theory: U.S. Geological Survey Circular 485, iii, 8 p. :diagrs., tables. ;26 cm., https://doi.org/10.3133/cir485.","productDescription":"iii, 8 p. :diagrs., tables. ;26 cm.","costCenters":[],"links":[{"id":30495,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1964/0485/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118010,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1964/0485/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635ad6","contributors":{"authors":[{"text":"Scheidegger, Adrian E.","contributorId":100370,"corporation":false,"usgs":true,"family":"Scheidegger","given":"Adrian","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":147015,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":13159,"text":"ofr6440 - 1964 - Principal facts for gravity stations along the central and southern Wasatch Front, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr6440","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":"64-40","title":"Principal facts for gravity stations along the central and southern Wasatch Front, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr6440","usgsCitation":"Cook, K.L., and Berg, J.W., 1964, Principal facts for gravity stations along the central and southern Wasatch Front, Utah: U.S. Geological Survey Open-File Report 64-40, 23 p. ;29 x 38 cm., https://doi.org/10.3133/ofr6440.","productDescription":"23 p. ;29 x 38 cm.","costCenters":[],"links":[{"id":146088,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0040/report-thumb.jpg"},{"id":41559,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0040/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6680ba","contributors":{"authors":[{"text":"Cook, Kenneth L.","contributorId":91099,"corporation":false,"usgs":true,"family":"Cook","given":"Kenneth","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":167330,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berg, Joseph Wilbur Jr.","contributorId":78337,"corporation":false,"usgs":true,"family":"Berg","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"Wilbur","affiliations":[],"preferred":false,"id":167329,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38880,"text":"pp501C - 1964 - Geological Survey research 1964, Chapter C","interactions":[],"lastModifiedDate":"2025-09-17T19:04:26.585446","indexId":"pp501C","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":"501","chapter":"C","title":"Geological Survey research 1964, Chapter C","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geological Survey research 1964","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/pp501C","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, 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,{"id":61291,"text":"mf295 - 1964 - Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"mf295","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"295","title":"Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf295","usgsCitation":"Zeller, H.D., and Stephens, E., 1964, Geologic map of the Hay Meadow Reservoir quadrangle, Sublette, Fremont, and Sweetwater Counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 295, 1 map ;58 x 44 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf295.","productDescription":"1 map ;58 x 44 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104066,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2715.htm","linkFileType":{"id":5,"text":"html"},"description":"2715"},{"id":182976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.11749999999999,42.25 ], [ -109.11749999999999,42.3675 ], [ -109,42.3675 ], [ -109,42.25 ], [ -109.11749999999999,42.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db69808b","contributors":{"authors":[{"text":"Zeller, H. D.","contributorId":104872,"corporation":false,"usgs":true,"family":"Zeller","given":"H.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":265335,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stephens, E. V.","contributorId":31054,"corporation":false,"usgs":true,"family":"Stephens","given":"E. V.","affiliations":[],"preferred":false,"id":265334,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":15550,"text":"ofr64129 - 1964 - Log for field trip through Caldecott Tunnel, Berkeley Hills, California","interactions":[],"lastModifiedDate":"2018-03-19T14:01:35","indexId":"ofr64129","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":"64-129","title":"Log for field trip through Caldecott Tunnel, Berkeley Hills, California","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64129","usgsCitation":"Radbruch, D.H., 1964, Log for field trip through Caldecott Tunnel, Berkeley Hills, California: U.S. Geological Survey Open-File Report 64-129, 3 p., https://doi.org/10.3133/ofr64129.","productDescription":"3 p.","costCenters":[],"links":[{"id":352639,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0129/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148394,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0129/report-thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Caldecott Tunnel","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -122.75,\n              37.6\n            ],\n            [\n              -122.1,\n              37.6\n            ],\n            [\n              -122.1,\n              38.25\n            ],\n            [\n              -122.75,\n              38.25\n            ],\n            [\n              -122.75,\n              37.6\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63c060","contributors":{"authors":[{"text":"Radbruch, Dorothy H.","contributorId":65874,"corporation":false,"usgs":true,"family":"Radbruch","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":171316,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":46986,"text":"ofr64121 - 1964 - Geologic map of the Mine Mountain quadrangle, Nye County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:39","indexId":"ofr64121","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":"64-121","title":"Geologic map of the Mine Mountain quadrangle, Nye County, Nevada","language":"ENGLISH","doi":"10.3133/ofr64121","usgsCitation":"Orkild, P.P., 1964, Geologic map of the Mine Mountain quadrangle, Nye County, Nevada: U.S. Geological Survey Open-File Report 64-121, 1 map, https://doi.org/10.3133/ofr64121.","productDescription":"1 map","costCenters":[],"links":[{"id":172314,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696999","contributors":{"authors":[{"text":"Orkild, Paul P.","contributorId":14441,"corporation":false,"usgs":true,"family":"Orkild","given":"Paul","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":234439,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16451,"text":"ofr64161 - 1964 - Seismic refraction survey in the Great Miami River Valley and vicinity, Montgomery, Warren, and Butler Counties, Ohio","interactions":[],"lastModifiedDate":"2025-07-24T16:32:53.565544","indexId":"ofr64161","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":"64-161","title":"Seismic refraction survey in the Great Miami River Valley and vicinity, Montgomery, Warren, and Butler Counties, Ohio","docAbstract":"<p>As part of a continuing program to define the thickness and extent of water-bearing sand and gravel deposits in southwestern Ohio, the U.S. Geological Survey, in cooperation with the Ohio Division of Water and The Miami Conservancy District, completed a seismic refraction survey of the Great Miami River valley and adjacent areas between Dayton and Hamilton, Ohio, in the fall of 1963. A similar survey of the adjoining lower Great Miami River and Whitewater River valleys was completed in 1962 (Watkins, 1963; Spieker and Watkins, unpublished data).</p><p>The area of the survey includes known or inferred portions of an interglacial drainage system which is deeply entrenched into bedrock. Ohio was covered by glaciers at least three times during the Pleistocene epoch. As each glacier melted, rock fragments absorbed by the glacier were transported and deposited in these buried valleys by torrents of meltwater. The total thickness of glacial drift is over 300 feet in some places. </p><p>Much of the glacial material is highly permeable and saturated with large quantities of water of good quality. The underlying bedrock is virtually impermeable and yields only meager quantities of water. The cities of Dayton, Middletown, Hamilton, and many industries in the Miami River valley rely on wells in the glacial deposits as their principal source of water. The purpose of the present survey is to define the thickness and extent of these important water-bearing formations. 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