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,{"id":5787,"text":"pp410 - 1964 - Stratigraphy and structure of part of the western Sierra Nevada metamorphic belt, California","interactions":[],"lastModifiedDate":"2012-02-02T00:06:02","indexId":"pp410","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":"410","title":"Stratigraphy and structure of part of the western Sierra Nevada metamorphic belt, California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp410","usgsCitation":"Clark, L., 1964, Stratigraphy and structure of part of the western Sierra Nevada metamorphic belt, California: U.S. Geological Survey Professional Paper 410, 70 p., https://doi.org/10.3133/pp410.","productDescription":"70 p.","costCenters":[],"links":[{"id":140767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0410/report-thumb.jpg"},{"id":112585,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0410/report.pdf","size":"13677","linkFileType":{"id":1,"text":"pdf"}},{"id":112586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-01.pdf","size":"2643","linkFileType":{"id":1,"text":"pdf"}},{"id":112587,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-02.pdf","size":"3799","linkFileType":{"id":1,"text":"pdf"}},{"id":112588,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-03.pdf","size":"5826","linkFileType":{"id":1,"text":"pdf"}},{"id":112589,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-04.pdf","size":"3424","linkFileType":{"id":1,"text":"pdf"}},{"id":112590,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-05.pdf","size":"4030","linkFileType":{"id":1,"text":"pdf"}},{"id":112591,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-06.pdf","size":"1975","linkFileType":{"id":1,"text":"pdf"}},{"id":112592,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-07.pdf","size":"3193","linkFileType":{"id":1,"text":"pdf"}},{"id":112593,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-08.pdf","size":"2023","linkFileType":{"id":1,"text":"pdf"}},{"id":112594,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-09.pdf","size":"682","linkFileType":{"id":1,"text":"pdf"}},{"id":112595,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-10.pdf","size":"1170","linkFileType":{"id":1,"text":"pdf"}},{"id":112596,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0410/plate-11.pdf","size":"657","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8687","contributors":{"authors":[{"text":"Clark, Lorin D.","contributorId":36931,"corporation":false,"usgs":true,"family":"Clark","given":"Lorin D.","affiliations":[],"preferred":false,"id":151585,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36011,"text":"b1123F - 1964 - Geology of the Rewey and Mifflin quadrangles, Wisconsin","interactions":[{"subject":{"id":46984,"text":"ofr58102 - 1958 - Geologic map of the Mifflin quadrangle, Wisconsin","indexId":"ofr58102","publicationYear":"1958","noYear":false,"title":"Geologic map of the Mifflin quadrangle, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":36011,"text":"b1123F - 1964 - Geology of the Rewey and Mifflin quadrangles, Wisconsin","indexId":"b1123F","publicationYear":"1964","noYear":false,"chapter":"F","title":"Geology of the Rewey and Mifflin quadrangles, Wisconsin"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:28","indexId":"b1123F","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":"1123","chapter":"F","title":"Geology of the Rewey and Mifflin quadrangles, Wisconsin","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1123F","usgsCitation":"Taylor, A.R., 1964, Geology of the Rewey and Mifflin quadrangles, Wisconsin: U.S. Geological Survey Bulletin 1123, p. 279-360, ill. ;24 cm., https://doi.org/10.3133/b1123F.","productDescription":"p. 279-360, ill. ;24 cm.","costCenters":[],"links":[{"id":97169,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1123f/plate-20.pdf","size":"10667","linkFileType":{"id":1,"text":"pdf"}},{"id":97170,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1123f/plate-21.pdf","size":"213","linkFileType":{"id":1,"text":"pdf"}},{"id":97168,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1123f/report.pdf","size":"5853","linkFileType":{"id":1,"text":"pdf"}},{"id":109372,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20835.htm","linkFileType":{"id":5,"text":"html"},"description":"20835"},{"id":163618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1123f/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e7a8","contributors":{"authors":[{"text":"Taylor, Alfred R.","contributorId":27024,"corporation":false,"usgs":true,"family":"Taylor","given":"Alfred","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":215614,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6025,"text":"pp483D - 1964 - Upper Jurassic mollusks from eastern Oregon and western Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:05:58","indexId":"pp483D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"483","chapter":"D","title":"Upper Jurassic mollusks from eastern Oregon and western Idaho","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp483D","usgsCitation":"Imlay, R.W., 1964, Upper Jurassic mollusks from eastern Oregon and western Idaho: U.S. Geological Survey Professional Paper 483, p. D1-D21, https://doi.org/10.3133/pp483D.","productDescription":"p. D1-D21","costCenters":[],"links":[{"id":118158,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0483d/report-thumb.jpg"},{"id":32972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0483d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a23e4b07f02db60d414","contributors":{"authors":[{"text":"Imlay, Ralph Willard","contributorId":19155,"corporation":false,"usgs":true,"family":"Imlay","given":"Ralph","email":"","middleInitial":"Willard","affiliations":[],"preferred":false,"id":151976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7812,"text":"ofr649 - 1964 - Preliminary report on tests of the application of geophysical methods to Arctic ground water problems","interactions":[],"lastModifiedDate":"2023-11-20T23:37:43.02624","indexId":"ofr649","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":"64-9","title":"Preliminary report on tests of the application of geophysical methods to Arctic ground water problems","docAbstract":"<p>Seismic refraction and electrical resistivity surveys were made during the summer and fall of 1952 in the Tanana Valley near Fairbanks, Alaska, as part of the studies of the application of geophysical techniques to ground-water problems in Alaska instigated in 1951 by the U.S. Army Engineer Research and Development Laboratories. Work centered around the highway junctions at Fairbanks, Big Delta, and Tok. It was found that both survey methods defined the horizontal extent of the frozen ground and both were capable of determining the depth to the top of the permafrost but neither regularly yielded reliable information on the material beneath the top of the permafrost. The greatest need at present is for a thorough examination of data obtained in the field seasons of 1948 and 1952. Two fundamental theoretical investigations are desirable: (1) examination of the attenuation of longitudinal waves traveling through a thin layer, and (2) further development of the theoretical multilayer resistivity interpretation of problems in which the second layer has a very high resistivity. Further field work should include: (1) tests of the U.S. Geological Survey's new shallow-reflection seismograph; (2) a brief test of electromagnetic equipment; (3) additional resistivity measurements with commutated current; and (4) both seismic and resistivity measurements in areas where the bedrock possesses different physical properties from the schist usually found in interior Alaska. 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,{"id":66941,"text":"i399 - 1964 - Geologic map of the Bozeman Pass quadrangle, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:11:04","indexId":"i399","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"399","subseriesTitle":"NONE","title":"Geologic map of the Bozeman Pass quadrangle, Montana","language":"ENGLISH","doi":"10.3133/i399","usgsCitation":"Roberts, A.E., 1964, Geologic map of the Bozeman Pass quadrangle, Montana: U.S. Geological Survey IMAP 399, 1 map., https://doi.org/10.3133/i399.","productDescription":"1 map.","costCenters":[],"links":[{"id":102833,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1299.htm","linkFileType":{"id":5,"text":"html"},"description":"1299"},{"id":190447,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.86749999999999,45.6175 ], [ -110.86749999999999,45.75 ], [ -110.75,45.75 ], [ -110.75,45.6175 ], [ -110.86749999999999,45.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69d966","contributors":{"authors":[{"text":"Roberts, A. E.","contributorId":89194,"corporation":false,"usgs":true,"family":"Roberts","given":"A.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":275340,"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":68629,"text":"ha120 - 1964 - Water-table, surface-drainage, and engineering soils map of the Trap Pond area, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha120","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"120","title":"Water-table, surface-drainage, and engineering soils map of the Trap Pond area, Delaware","language":"ENGLISH","doi":"10.3133/ha120","usgsCitation":"Adams, J.K., and Boggess, D.H., 1964, Water-table, surface-drainage, and engineering soils map of the Trap Pond area, Delaware: U.S. Geological Survey Hydrologic Atlas 120, 1 map., https://doi.org/10.3133/ha120.","productDescription":"1 map.","costCenters":[],"links":[{"id":185775,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90290,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/120/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":90291,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/120/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.5,38.45055555555556 ], [ -75.5,38.6175 ], [ -75.36749999999999,38.6175 ], [ -75.36749999999999,38.45055555555556 ], [ -75.5,38.45055555555556 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c80","contributors":{"authors":[{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278599,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278600,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":68625,"text":"ha143 - 1964 - Floods in Lombard quadrangle, Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha143","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"143","title":"Floods in Lombard quadrangle, Illinois","language":"ENGLISH","doi":"10.3133/ha143","usgsCitation":"Allen, H., and May, V.J., 1964, Floods in Lombard quadrangle, Illinois: U.S. Geological Survey Hydrologic Atlas 143, col. map ;58 x 44 cm. on sheet 80 x 84 cm. fold. in envelope 30 x 24 cm., https://doi.org/10.3133/ha143.","productDescription":"col. map ;58 x 44 cm. on sheet 80 x 84 cm. fold. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":186141,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90286,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/143/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,41.8675 ], [ -88.11749999999999,42 ], [ -88,42 ], [ -88,41.8675 ], [ -88.11749999999999,41.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e705a","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278591,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":278592,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":68623,"text":"ha89 - 1964 - Floods in Joliet quadrangle, Illinois","interactions":[],"lastModifiedDate":"2022-09-14T21:25:11.02932","indexId":"ha89","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"89","title":"Floods in Joliet quadrangle, Illinois","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha89","usgsCitation":"Allen, H., and Wyerman, T.A., 1964, Floods in Joliet quadrangle, Illinois: U.S. Geological Survey Hydrologic Atlas 89, 1 Plate: 53.00 × 32.50 inches, https://doi.org/10.3133/ha89.","productDescription":"1 Plate: 53.00 × 32.50 inches","costCenters":[],"links":[{"id":185647,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":406732,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_16187.htm","linkFileType":{"id":5,"text":"html"}},{"id":90284,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/089/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinios","otherGeospatial":"Joliet quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -88.125,\n              41.5\n            ],\n            [\n              -88,\n              41.5\n            ],\n            [\n              -88,\n              41.625\n            ],\n            [\n              -88.125,\n              41.625\n            ],\n            [\n              -88.125,\n              41.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e5e4b07f02db5e70ba","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278588,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wyerman, Theodore A.","contributorId":23222,"corporation":false,"usgs":true,"family":"Wyerman","given":"Theodore","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":278589,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":63338,"text":"gq295 - 1964 - Geology of the Fordsville quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:40","indexId":"gq295","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":"295","title":"Geology of the Fordsville quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq295","usgsCitation":"Bergendahl, M., and Smith, A.E., 1964, Geology of the Fordsville quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 295, 1 map :col. ;76 x 84 cm., https://doi.org/10.3133/gq295.","productDescription":"1 map :col. ;76 x 84 cm.","costCenters":[],"links":[{"id":102304,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_753.htm","linkFileType":{"id":5,"text":"html"},"description":"753"},{"id":249440,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0295/report.pdf","size":"36","linkFileType":{"id":1,"text":"pdf"}},{"id":252839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0295/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -86.75,37.6175 ], [ -86.75,37.75 ], [ -86.61749999999999,37.75 ], [ -86.61749999999999,37.6175 ], [ -86.75,37.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68050c","contributors":{"authors":[{"text":"Bergendahl, M.H.","contributorId":23538,"corporation":false,"usgs":true,"family":"Bergendahl","given":"M.H.","affiliations":[],"preferred":false,"id":268694,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Avery E.","contributorId":82383,"corporation":false,"usgs":true,"family":"Smith","given":"Avery","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":268695,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":68407,"text":"ha129 - 1964 - Geology and hydrology of alluvial deposits along the Ohio River between the Uniontown area and Wickliffe, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"ha129","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"129","title":"Geology and hydrology of alluvial deposits along the Ohio River between the Uniontown area and Wickliffe, Kentucky","language":"ENGLISH","doi":"10.3133/ha129","usgsCitation":"Gallaher, J.T., 1964, Geology and hydrology of alluvial deposits along the Ohio River between the Uniontown area and Wickliffe, Kentucky: U.S. Geological Survey Hydrologic Atlas 129, 2 maps :col. ;on sheets 81 x 76 cm. and 51 x 41 cm., https://doi.org/10.3133/ha129.","productDescription":"2 maps :col. ;on sheets 81 x 76 cm. and 51 x 41 cm.","costCenters":[],"links":[{"id":190007,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89922,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/129/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89923,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/129/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,37.5 ], [ -88.25,37.5 ], [ -88.25,37.5 ], [ -88.25,37.5 ], [ -88.25,37.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db685254","contributors":{"authors":[{"text":"Gallaher, John T.","contributorId":11585,"corporation":false,"usgs":true,"family":"Gallaher","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":278165,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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