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,{"id":38890,"text":"pp485A - 1964 - Botanical evidence of floods and flood-plain deposition","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp485A","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":"485","chapter":"A","title":"Botanical evidence of floods and flood-plain deposition","language":"ENGLISH","doi":"10.3133/pp485A","usgsCitation":"Sigafoos, R., 1964, Botanical evidence of floods and flood-plain deposition: U.S. Geological Survey Professional Paper 485, p. A1-A35, https://doi.org/10.3133/pp485A.","productDescription":"p. A1-A35","costCenters":[],"links":[{"id":121993,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0485a/report-thumb.jpg"},{"id":65902,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0485a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602959","contributors":{"authors":[{"text":"Sigafoos, R.S.","contributorId":88014,"corporation":false,"usgs":true,"family":"Sigafoos","given":"R.S.","affiliations":[],"preferred":false,"id":220611,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38974,"text":"pp429B - 1964 - Ecology of benthonic species","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"pp429B","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":"429","chapter":"B","title":"Ecology of benthonic species","language":"ENGLISH","doi":"10.3133/pp429B","usgsCitation":"Smith, P., 1964, Ecology of benthonic species: U.S. Geological Survey Professional Paper 429, p. B1-B55, https://doi.org/10.3133/pp429B.","productDescription":"p. B1-B55","costCenters":[],"links":[{"id":120401,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0429b/report-thumb.jpg"},{"id":66077,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0429b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66078,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0429b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ee4b07f02db627aae","contributors":{"authors":[{"text":"Smith, P.B.","contributorId":83189,"corporation":false,"usgs":true,"family":"Smith","given":"P.B.","email":"","affiliations":[],"preferred":false,"id":220748,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"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":61622,"text":"gq311 - 1964 - Geology of the Tatman Mountain quadrangle, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq311","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":"311","title":"Geology of the Tatman Mountain quadrangle, Wyoming","language":"ENGLISH","doi":"10.3133/gq311","usgsCitation":"Rohrer, W.L., 1964, Geology of the Tatman Mountain quadrangle, Wyoming: U.S. Geological Survey Geologic Quadrangle 311, 1 map., https://doi.org/10.3133/gq311.","productDescription":"1 map.","costCenters":[],"links":[{"id":102323,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_772.htm","linkFileType":{"id":5,"text":"html"},"description":"772"},{"id":247928,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0311/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252353,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0311/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.61749999999999,44.25 ], [ -108.61749999999999,44.3675 ], [ -108.5,44.3675 ], [ -108.5,44.25 ], [ -108.61749999999999,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acbe4b07f02db67e393","contributors":{"authors":[{"text":"Rohrer, Willis L.","contributorId":93958,"corporation":false,"usgs":true,"family":"Rohrer","given":"Willis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266150,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63512,"text":"gp460 - 1964 - Aeromagnetic map of the Williamstown quadrangle, Berkshire County, Massachusetts, and Bennington County, Vermont","interactions":[],"lastModifiedDate":"2025-04-25T19:13:07.925377","indexId":"gp460","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":"460","title":"Aeromagnetic map of the Williamstown quadrangle, Berkshire County, Massachusetts, and Bennington County, Vermont","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp460","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Williamstown quadrangle, Berkshire County, Massachusetts, and Bennington County, Vermont: U.S. Geological Survey Geophysical Investigations Map 460, 1 Plate: 21.83 x 27.88 inches, https://doi.org/10.3133/gp460.","productDescription":"1 Plate: 21.83 x 27.88 inches","costCenters":[],"links":[{"id":253150,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0460/report-thumb.jpg"},{"id":249634,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0460/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249633,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0460/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485065,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3406.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Massachusetts, Vermont","county":"Bennington County, Berkshire County","otherGeospatial":"Williamstown quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.25,\n              42.75\n            ],\n            [\n              -73.25,\n              42.625\n            ],\n            [\n              -73.125,\n              42.625\n            ],\n            [\n              -73.125,\n              42.75\n            ],\n            [\n              -73.25,\n              42.75\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae6e4b07f02db68b7b6","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":269017,"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":269018,"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":269016,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":63513,"text":"gp461 - 1964 - Aeromagnetic map of the Windsor quadrangle, Berkshire County, Massachusetts","interactions":[],"lastModifiedDate":"2025-04-25T19:21:18.406056","indexId":"gp461","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":"461","title":"Aeromagnetic map of the Windsor quadrangle, Berkshire County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp461","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Windsor quadrangle, Berkshire County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 461, 1 Plate: 21.73 x 27.69 inches, https://doi.org/10.3133/gp461.","productDescription":"1 Plate: 21.73 x 27.69 inches","costCenters":[],"links":[{"id":485066,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3407.htm","linkFileType":{"id":5,"text":"html"}},{"id":253151,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0461/report-thumb.jpg"},{"id":249636,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0461/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249635,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0461/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Berkshire County","otherGeospatial":"Windsor quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.125,\n              42.625\n            ],\n            [\n              -73.125,\n              42.5\n            ],\n            [\n              -73,\n              42.5\n            ],\n            [\n              -73,\n              42.625\n            ],\n            [\n              -73.125,\n              42.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae7e4b07f02db68bd37","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":269020,"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":269021,"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":269019,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":63514,"text":"gp445 - 1964 - Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland","interactions":[],"lastModifiedDate":"2025-04-24T20:18:45.86874","indexId":"gp445","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":"445","title":"Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp445","usgsCitation":"Popenoe, P., Petty, A.J., and Tyson, N., 1964, Aeromagnetic map of western Pennsylvania and parts of eastern Ohio, northern West Virginia, and western Maryland: U.S. Geological Survey Geophysical Investigations Map 445, 1 Plate: 37.08 x 37.06 inches, https://doi.org/10.3133/gp445.","productDescription":"1 Plate: 37.08 x 37.06 inches","costCenters":[],"links":[{"id":485034,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3389.htm","linkFileType":{"id":5,"text":"html"}},{"id":253152,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0445/report-thumb.jpg"},{"id":249638,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0445/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249637,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0445/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Maryland, Ohio, Pennsylvania, West Virginia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -81.4167,\n              41.25\n            ],\n            [\n              -81.4167,\n              39.5833\n            ],\n            [\n              -78.8333,\n              39.5833\n            ],\n            [\n              -78.8333,\n              41.25\n            ],\n            [\n              -81.4167,\n              41.25\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db689ea0","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":269024,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Petty, A. J.","contributorId":35384,"corporation":false,"usgs":true,"family":"Petty","given":"A.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":269023,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Tyson, N.S.","contributorId":28674,"corporation":false,"usgs":true,"family":"Tyson","given":"N.S.","email":"","affiliations":[],"preferred":false,"id":269022,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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":62504,"text":"gq307 - 1964 - Geology of the Kelly quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq307","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":"307","title":"Geology of the Kelly quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq307","usgsCitation":"Miller, T.P., 1964, Geology of the Kelly quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 307, 1 map :col. ;81 x 89 cm., https://doi.org/10.3133/gq307.","productDescription":"1 map :col. ;81 x 89 cm.","costCenters":[],"links":[{"id":102318,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_767.htm","linkFileType":{"id":5,"text":"html"},"description":"767"},{"id":248667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0307/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":253894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0307/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.5,36.8675 ], [ -87.5,37 ], [ -87.36749999999999,37 ], [ -87.36749999999999,36.8675 ], [ -87.5,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67fbfc","contributors":{"authors":[{"text":"Miller, Thomas P. tmiller@usgs.gov","contributorId":4183,"corporation":false,"usgs":true,"family":"Miller","given":"Thomas","email":"tmiller@usgs.gov","middleInitial":"P.","affiliations":[{"id":121,"text":"Alaska Volcano Observatory","active":false,"usgs":true}],"preferred":false,"id":267468,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61621,"text":"gq310 - 1964 - Geology of the Sheep Mountain quadrangle, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq310","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":"310","title":"Geology of the Sheep Mountain quadrangle, Wyoming","language":"ENGLISH","doi":"10.3133/gq310","usgsCitation":"Rohrer, W.L., 1964, Geology of the Sheep Mountain quadrangle, Wyoming: U.S. Geological Survey Geologic Quadrangle 310, 1 map., https://doi.org/10.3133/gq310.","productDescription":"1 map.","costCenters":[],"links":[{"id":102322,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_771.htm","linkFileType":{"id":5,"text":"html"},"description":"771"},{"id":247927,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0310/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252352,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0310/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.5,44.25 ], [ -108.5,44.3675 ], [ -108.36749999999999,44.3675 ], [ -108.36749999999999,44.25 ], [ -108.5,44.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e5de","contributors":{"authors":[{"text":"Rohrer, Willis L.","contributorId":93958,"corporation":false,"usgs":true,"family":"Rohrer","given":"Willis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":266149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1122,"text":"wsp1773 - 1964 - Geology and ground-water resources of the Anchorage area, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1773","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":"1773","title":"Geology and ground-water resources of the Anchorage area, Alaska","docAbstract":"The Anchorage area, at the head of Cook Inlet in south-central Alaska, \r\noccupies 150 square miles of a glaciated lowland and lies between two estuaries and the Chugach Mountains. Two military bases are in the area; \r\nAnchorage is the largest city in Alaska and the chief transportation center \r\nfor this part of the State. \r\nThe bedrock in the Anchorage area is chiefly Tertiary shale in the lowland \r\nand metamorphic rocks of Mesozoic age beneath the adjacent mountain \r\nslopes. Glacial drift which underlies nearly the entire area has an average \r\nthickness of several hundred feet and appears to include at least five sheets \r\nof deposits, two of which are exposed. The drift consists of till, outwash stream and lake deposits (sand and gravel), and estuarine (and lake) deposits \r\n(clay and silt). The stratigraphy and lateral distribution of the deposits are \r\ncomplex, but data at hand s, how that the thickest deposits, including all the \r\nestuarine and lake sediment and most of the stream-deposited sediment, \r\nare beneath the lowland away from the mountain wall, and that the deposits \r\nnear the mountains are till and subordinate outwash sediments. \r\nDeposits of sand and gravel laid down by outwash streams in channels and \r\non outwash plains are the most important aquifers, and the only \r\nones which yield large quantities of ground water from single beds. Thin \r\nlayers of sandy or gravelly material in till are also important aquifers although they yield relatively small quantities of water. Bedded sand and \r\nsilt associated with the estuarine and lake(?) clay commonly becomes unstable during drilling and pumping, and has been successfully developed in \r\nonly a few wells. Unconfined aquifers are extensive, but permeable saturated \r\nmaterial is thin in many places and water supplies available from them are \r\nsmall or undependable in those places. The most important aquifers are confined or artesian. Clay and till form the confining beds: the till is somewhat 'leaky' in many places. Near Anchorage the buried water-bearing \r\nbeds appear to be interconnected and to form a single artesian system. The \r\nwater table and piezometric surface slope from the mountain wall of the \r\nlowland toward the estuaries, and the flow of the ground water is in that \r\ndirection. The aquifers are recharged by the infiltration of precipitation \r\nat the land surface and of surface water through stream beds: near the mountains the artesian aquifers are probably recharged in part by percolation from \r\nthe water-table aquifer, and far from the mountains the water-table aquifer \r\nis probably recharged in part by upward flow from the underlying artesian \r\naquifers. In several valleys and in a few other places, in the lowland, artesian wells flow at the land surface. \r\nThe outwash sand and gravel are moderately to very permeable; most \r\nof the other water-bearing material are much less permeable. The co- efficient of transmissibility for some single beds of sandy gravel is as high \r\nas 60,000 to I00,000 gpd per ft (gallons per day per foot); for the entire \r\nsection of glacial drift at and near Anchorage it is believed to be of the \r\norder of 200,000 gpd per ft. Calculations based on this value for the total \r\nsection and on the slope of the piezometric surface indicate that in the \r\nimmediate vicinity of Anchorage about 5 million gpd flows through each \r\nmile-wide section of the drift (measured in a northeast-southwest direction, perpendicular to the direction of flow), under normal (nonpumping) conditions. Under conditions of continuous heavy pumping the slope of the piezometric surface is steepened, flow is increased, and additional recharge is induced. \r\n\r\nThe highest yield reported from a well in this area is 2.600 gpm (gallons per minute) with 35 feet of drawdown: the highest reported specific capacity is 180 gpm per ft of drawdown, for a well pumped at. 270 gpm. \r\n\r\nOnly a few wells in the area have been developed for high yields. Well screens have been used ","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1773","usgsCitation":"Cederstrom, D.J., Trainer, F.W., and Waller, R.M., 1964, Geology and ground-water resources of the Anchorage area, Alaska: U.S. Geological Survey Water Supply Paper 1773, vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm., https://doi.org/10.3133/wsp1773.","productDescription":"vi, 108 p. :illus., maps (1 col.) diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":138014,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1773/report-thumb.jpg"},{"id":25887,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25888,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25889,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25890,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1773/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25891,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1773/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6855f4","contributors":{"authors":[{"text":"Cederstrom, Dagfin John","contributorId":90287,"corporation":false,"usgs":true,"family":"Cederstrom","given":"Dagfin","email":"","middleInitial":"John","affiliations":[],"preferred":false,"id":143212,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trainer, Frank W.","contributorId":103655,"corporation":false,"usgs":true,"family":"Trainer","given":"Frank","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":143213,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":143211,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":39025,"text":"pp391C - 1964 - Quantitative interpretation of mineralogical composition from X-ray and chemical data for the Pierre Shale","interactions":[],"lastModifiedDate":"2012-02-02T00:10:36","indexId":"pp391C","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":"391","chapter":"C","title":"Quantitative interpretation of mineralogical composition from X-ray and chemical data for the Pierre Shale","language":"ENGLISH","doi":"10.3133/pp391C","usgsCitation":"Schultz, L., 1964, Quantitative interpretation of mineralogical composition from X-ray and chemical data for the Pierre Shale: U.S. Geological Survey Professional Paper 391, p. C1-C31, https://doi.org/10.3133/pp391C.","productDescription":"p. C1-C31","costCenters":[],"links":[{"id":120530,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0391c/report-thumb.jpg"},{"id":66166,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0391c/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0391c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ea5","contributors":{"authors":[{"text":"Schultz, L.G.","contributorId":62617,"corporation":false,"usgs":true,"family":"Schultz","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":220822,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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,{"id":1947,"text":"wsp1748 - 1964 - Apparatus and techniques for measuring bedload","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1748","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":"1748","title":"Apparatus and techniques for measuring bedload","docAbstract":"The need for accurate determinations of the total sediment discharge of particles of bedload size has prompted this investigation of available and possible measuring apparatus and procedures. The accuracy of measurements of sediment discharge made with trap-type samplers is affected by the variability of sampler efficiency, by the oscillatory variation of bedload discharge, and by sampler placement. Equations that were developed for determining total discharge from measured bedioad discharge and measured suspended-sediment discharge are simplest if the bedload apparatus measures only the true bedload. \r\n\r\nEarly bedload samplers are generally unsatisfactory. Recently developed or suggested apparatus include various improved samplers of the pressure-difference type, a pumping sampler, a magnetic sampler, acoustical instruments that measure the magnitude of the sound of particle collisions, an ultrasonic bedload sampler designed to measure and integrate electronically the concentration and velocity, and a tiltmeter designed to measure the total sediment discharge from the ground tilt that results from the passage of flow. All the pressure-difference samplers are improvements over early samplers, but none are void of the inherent shortcomings of trap-type apparatus; probably the Sphinx (Dutch) and VUV (Hungarian) samplers are the most satisfactory. The acoustical instruments are capable of measuring only the relative discharge. The ultrasonic sampler and the tiltmeter are not adequate without further development. \r\n\r\nSome new possible apparatus and means for measuring or aiding in measuring bedload discharge are small pit samplers, ultrasonic sounders, pressure transducers, and photography. A small pit sampler for measuring bedload discharge was designed to provide self-placement and portability ; however, its practicability and efficiency are undetermined. Exploratory films show that by using slowmotion photography the discharge of particles larger than about pea size can be determined provided the flow is clear; however, photography generally is not practical. Ultrasonic sounders provide continuous and accurate data on bed configuration and dune movement for use in equations that were developed for computing the bedload discharge. Computations with the equations indicate that the interpretation of the sounding data needs further study. Pressure transducers placed beneath the bed surface possibly can be used to provide information on dune movement; however, their installation would be difficult. The time required for collecting data on bed configuration and dune movement throughout a cross section could be substantially reduced by using several transducers simultaneously in conjunction with an ultrasonic sounder. A modified ultrasonic sounder that provides information on the shape and velocity of large particles and a method for determining the discharge of such particles were proposed; the method seems most feasible for particles of high sphericity.","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1748","usgsCitation":"Hubbell, D.W., 1964, Apparatus and techniques for measuring bedload: U.S. Geological Survey Water Supply Paper 1748, v, 74 p. :illus. ;24 cm., https://doi.org/10.3133/wsp1748.","productDescription":"v, 74 p. :illus. ;24 cm.","costCenters":[],"links":[{"id":27278,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1748/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138418,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1748/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4883e4b07f02db51824d","contributors":{"authors":[{"text":"Hubbell, David Wellington","contributorId":88330,"corporation":false,"usgs":true,"family":"Hubbell","given":"David","email":"","middleInitial":"Wellington","affiliations":[],"preferred":false,"id":144417,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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