{"pageNumber":"6675","pageRowStart":"166850","pageSize":"25","recordCount":184644,"records":[{"id":61989,"text":"mr41 - 1964 - Industrial minerals and construction materials occurrences in Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:36","indexId":"mr41","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"41","title":"Industrial minerals and construction materials occurrences in Alaska","language":"ENGLISH","doi":"10.3133/mr41","usgsCitation":"Cobb, E.H., 1964, Industrial minerals and construction materials occurrences in Alaska: U.S. Geological Survey Mineral Investigations Resource Map 41, 1 map :col. ;83 x 118 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mr41.","productDescription":"1 map :col. ;83 x 118 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":180519,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260440,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/41/plate-1.pdf"}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -170,53.5 ], [ -170,70 ], [ -130,70 ], [ -130,53.5 ], [ -170,53.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eec4e","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":266657,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2896,"text":"wsp1783 - 1964 - Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"wsp1783","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":"1783","title":"Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1783","usgsCitation":"Weeks, E.P., 1964, Hydrologic conditions in the Wheatland Flats area, Platte County, Wyoming: U.S. Geological Survey Water Supply Paper 1783, v, 79 p. :illus., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1783.","productDescription":"v, 79 p. :illus., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":138377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1783/report-thumb.jpg"},{"id":29548,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29549,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29550,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29551,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29552,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29553,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29554,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29555,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1783/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29556,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1783/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db68325e","contributors":{"authors":[{"text":"Weeks, Edwin P. epweeks@usgs.gov","contributorId":2576,"corporation":false,"usgs":true,"family":"Weeks","given":"Edwin","email":"epweeks@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":145972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61990,"text":"mr40 - 1964 - Iron occurrences in Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:36","indexId":"mr40","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"40","title":"Iron occurrences in Alaska","language":"ENGLISH","doi":"10.3133/mr40","usgsCitation":"Cobb, E.H., 1964, Iron occurrences in Alaska: U.S. Geological Survey Mineral Investigations Resource Map 40, 1 map :col. ;79 x 115 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/mr40.","productDescription":"1 map :col. ;79 x 115 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":180520,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260441,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/40/plate-1.pdf"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -172,52 ], [ -172,68.25 ], [ -137.25,68.25 ], [ -137.25,52 ], [ -172,52 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6672d7","contributors":{"authors":[{"text":"Cobb, Edward Huntington","contributorId":25916,"corporation":false,"usgs":true,"family":"Cobb","given":"Edward","email":"","middleInitial":"Huntington","affiliations":[],"preferred":false,"id":266658,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":161,"text":"wsp1942 - 1964 - Quality of surface waters of the United States, 1962, Parts 3 and 4, Ohio River basin and St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp1942","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":"1942","title":"Quality of surface waters of the United States, 1962, Parts 3 and 4, Ohio River basin and St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1942","usgsCitation":"Love, S.K., 1964, Quality of surface waters of the United States, 1962, Parts 3 and 4, Ohio River basin and St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 1942, x, 322 p. ;23 cm., https://doi.org/10.3133/wsp1942.","productDescription":"x, 322 p. ;23 cm.","costCenters":[],"links":[{"id":137266,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1942/report-thumb.jpg"},{"id":24772,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1942/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651b1b","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":142032,"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":63534,"text":"gp448 - 1964 - Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts","interactions":[],"lastModifiedDate":"2022-08-17T21:56:10.085185","indexId":"gp448","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":"448","title":"Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp448","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Beckett quadrangle, Berkshire, Hampshire, and Hampden Counties, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 448, 1 Plate: 21.75 × 27.74 inches, https://doi.org/10.3133/gp448.","productDescription":"1 Plate: 21.75 × 27.74 inches","costCenters":[],"links":[{"id":405290,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3392.htm","linkFileType":{"id":5,"text":"html"}},{"id":253172,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0448/report-thumb.jpg"},{"id":249681,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0448/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249680,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0448/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Berkshire County, Hampshire County, Hampden County","otherGeospatial":"Beckett quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.125,\n              42.25\n            ],\n            [\n              -73,\n              42.25\n            ],\n            [\n              -73,\n              42.375\n            ],\n            [\n              -73.125,\n              42.375\n            ],\n            [\n              -73.125,\n              42.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697245","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":269072,"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":269073,"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":269071,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61782,"text":"gq316 - 1964 - Geology of the Boltsfork quadrangle and part of the Burnaugh quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:29","indexId":"gq316","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":"316","title":"Geology of the Boltsfork quadrangle and part of the Burnaugh quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq316","usgsCitation":"Spencer, F.D., 1964, Geology of the Boltsfork quadrangle and part of the Burnaugh quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 316, 1 map., https://doi.org/10.3133/gq316.","productDescription":"1 map.","costCenters":[],"links":[{"id":102328,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_777.htm","linkFileType":{"id":5,"text":"html"},"description":"777"},{"id":248074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0316/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0316/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.75,38.25 ], [ -82.75,38.3675 ], [ -82.61749999999999,38.3675 ], [ -82.61749999999999,38.25 ], [ -82.75,38.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68341b","contributors":{"authors":[{"text":"Spencer, Frank Darwyn","contributorId":22330,"corporation":false,"usgs":true,"family":"Spencer","given":"Frank","email":"","middleInitial":"Darwyn","affiliations":[],"preferred":false,"id":266359,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2337,"text":"wsp1785 - 1964 - An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico","interactions":[{"subject":{"id":52356,"text":"ofr63102 - 1963 - An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico","indexId":"ofr63102","publicationYear":"1963","noYear":false,"title":"An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":2337,"text":"wsp1785 - 1964 - An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico","indexId":"wsp1785","publicationYear":"1964","noYear":false,"title":"An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1785","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":"1785","title":"An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/wsp1785","usgsCitation":"Motts, W.S., and Cushman, R., 1964, An appraisal of the possibilities of artificial recharge to ground-water supplies in part of the Roswell basin, New Mexico: U.S. Geological Survey Water Supply Paper 1785, v, 85 p. :illus., maps (1 col.) ;24 cm., https://doi.org/10.3133/wsp1785.","productDescription":"v, 85 p. :illus., maps (1 col.) ;24 cm.","costCenters":[],"links":[{"id":138574,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1785/report-thumb.jpg"},{"id":28202,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28203,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28204,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28205,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28206,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28207,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28208,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1785/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1785/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db68564f","contributors":{"authors":[{"text":"Motts, Ward Sundt","contributorId":68708,"corporation":false,"usgs":true,"family":"Motts","given":"Ward","email":"","middleInitial":"Sundt","affiliations":[],"preferred":false,"id":145039,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushman, Robert L.","contributorId":22751,"corporation":false,"usgs":true,"family":"Cushman","given":"Robert L.","affiliations":[],"preferred":false,"id":145038,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61574,"text":"gq258 - 1964 - Geology of the Hoppers quadrangle, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:28","indexId":"gq258","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":"258","title":"Geology of the Hoppers quadrangle, Montana","language":"ENGLISH","doi":"10.3133/gq258","usgsCitation":"Roberts, A.E., 1964, Geology of the Hoppers quadrangle, Montana: U.S. Geological Survey Geologic Quadrangle 258, 1 map :col. ;58 x 41 cm., on sheet 66 x 70 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq258.","productDescription":"1 map :col. ;58 x 41 cm., on sheet 66 x 70 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102263,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_712.htm","linkFileType":{"id":5,"text":"html"},"description":"712"},{"id":247884,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0258/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0258/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.75,45.6175 ], [ -110.75,45.75 ], [ -110.61749999999999,45.75 ], [ -110.61749999999999,45.6175 ], [ -110.75,45.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67ff3d","contributors":{"authors":[{"text":"Roberts, Albert Eugene","contributorId":77126,"corporation":false,"usgs":true,"family":"Roberts","given":"Albert","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":266085,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62003,"text":"mr38 - 1964 - Placer gold occurrences in Alaska","interactions":[],"lastModifiedDate":"2025-05-09T13:28:20.950341","indexId":"mr38","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"38","title":"Placer gold occurrences in Alaska","docAbstract":"<p>The following references give data on localities of placer gold by quadrangle and are keyed by number within each quadrangle to locations shown on map. The quadrangle boundaries and names used on the map are those selected by the U. S. Geological Survey for topographic mapping in Alaska on a scale of 1:250,000. 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,{"id":1054,"text":"wsp1695 - 1964 - Geology and ground-water resources of southeastern New Hampshire","interactions":[{"subject":{"id":51806,"text":"ofr5516 - 1955 - Preliminary report on the investigation of ground-water resources of the seacoast region of New Hampshire","indexId":"ofr5516","publicationYear":"1955","noYear":false,"title":"Preliminary report on the investigation of ground-water resources of the seacoast region of New Hampshire"},"predicate":"SUPERSEDED_BY","object":{"id":1054,"text":"wsp1695 - 1964 - Geology and ground-water resources of southeastern New Hampshire","indexId":"wsp1695","publicationYear":"1964","noYear":false,"title":"Geology and ground-water resources of southeastern New Hampshire"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:17","indexId":"wsp1695","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":"1695","title":"Geology and ground-water resources of southeastern New Hampshire","docAbstract":"The continued growth and development of southeastern New Hampshire, an area of about 390 square miles adjacent to the Atlantic Ocean, will depend partly on effectively satisfying the demand for water, which has increased rapidly since World War II. \r\n\r\nThe report identifies and describes the principal geologic units with respect to the occurrence of ground water. These units include bedrock and the various unconsolidated deposits that mantle the bedrock surface discontinuously throughout the area. \r\n\r\nThe bedrock formations, consisting of igneous and metamorphic rocks, chiefly of Paleozoic age, form a single water-bearing unit. Ground water is in joints and fractures. The fractures are small and scattered and therefore impart only a low permeability to the rocks. Wells in the bedrock commonly produce small but reliable supplies of ground water at depths of less than 150 feet. The yields of about 80 wells inventoried for this report ranged from 1? to 100 gpm (gallons per minute) and the median was 912 gpm. Depths ranged from 45 to 600 feet. The unconsolidated deposits consist of glacial drift of Pleistocene age; swamp deposits, alluvium, and beach deposits of Recent age; and eolian deposits of Pleistocene -and Recent age. For this report the glacial drift is divided into till, ice-contact deposits, marine deposits, and outwash and shore deposits. Glacial till forms a discontinuous blanket, commonly less than 15 but in some hills (drumlins) as much as about 200 feet thick. It has a low permeability but, because of its widespread outcrop area, it has been utilized as a source of water for numerous domestic supplies. Because most wells in till are shallow, many fail to meet modern demands during dry summers. \r\n\r\nIce-contact deposits locally form kames, kame terraces, kame plains, and ice-channel fillings throughout the area. They overlie bedrock and till and range in thickness from less than 1 foot to as much as 190 feet. In general, the ice-contact deposits are coarse textured and permeable, but variations in- the physical and hydrologic properties of a single deposit and from deposit to deposit are common. Ice-contact deposits are the source of the larger ground-water supplies in southeastern New Hampshire. \r\n\r\nMarine deposits underlie lowlands and valleys to a distance of about 20 miles inland from the present coastline. They commonly overlie bedrock and till and at places overlie or are interbedded with ice-contact deposits. Marine deposits range in thickness from less than 1 foot to possibly 75 feet. They are fine textured and impermeable; they do not yield water to wells in southeastern New Hampshire but generally act as a barrier to ground-water movement. Outwash and shore deposits form broad sand plains or gently sloping terraces of small extent. At most places the outwash and shore deposits, which range in thickness from less than 1 foot to about 50 feet, overlie marine deposits, but at some places they overlie bedrock, till, or ice-contact deposits. The outwash and shore deposits are fine textured and moderately permeable. They commonly yield enough ground water to meet the needs of farms, homes, and small industries. Alluvium underlies the flood plains and channels of the principal streams and overlies bedrock and older unconsolidated deposits wherever streams cross the older units. The alluvium generally is not tapped by wells. \r\n\r\nBeach deposits occupy areas along the Atlantic Ocean between promontories of bedrock or till. In general beach deposits are permeable and are a source of water supplies for domestic use. Yields of wells are limited, however, by the danger of drawing in salty water. \r\n\r\nRecharge in southeastern New Hampshire is derived principally from precipitation on outcrop areas of ice-contact deposits and outwash and shore deposits during the nongrowing season. Ground water is discharged naturally by springs, by effluent seepage to streams and other bodies of surface water, and by evapotranspiration. It ","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1695","usgsCitation":"Bradley, E., 1964, Geology and ground-water resources of southeastern New Hampshire: U.S. Geological Survey Water Supply Paper 1695, v, 80 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1695.","productDescription":"v, 80 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":25720,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25721,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25722,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25723,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25724,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25725,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25726,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1695/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1695/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137945,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1695/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685601","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":143098,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":243,"text":"wsp1530 - 1964 - Summary of floods in the United States during 1956","interactions":[],"lastModifiedDate":"2012-02-02T00:05:06","indexId":"wsp1530","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":"1530","title":"Summary of floods in the United States during 1956","language":"ENGLISH","publisher":"U.S. G.P.O,","doi":"10.3133/wsp1530","usgsCitation":"Hendricks, E.L., 1964, Summary of floods in the United States during 1956: U.S. Geological Survey Water Supply Paper 1530, vi, 85 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1530.","productDescription":"vi, 85 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1530/report-thumb.jpg"},{"id":24850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1530/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6992b4","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":63539,"text":"gp451 - 1964 - Aeromagnetic map of the Cheshire quadrangle, Berkshire County, Massachusetts","interactions":[],"lastModifiedDate":"2025-04-24T20:40:12.799206","indexId":"gp451","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":"451","title":"Aeromagnetic map of the Cheshire quadrangle, Berkshire County, Massachusetts","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp451","usgsCitation":"Popenoe, P., Boynton, G.R., and Zandle, G.L., 1964, Aeromagnetic map of the Cheshire quadrangle, Berkshire County, Massachusetts: U.S. Geological Survey Geophysical Investigations Map 451, 1 Plate: 21.53 x 27.51 inches, https://doi.org/10.3133/gp451.","productDescription":"1 Plate: 21.53 x 27.51 inches","costCenters":[],"links":[{"id":485037,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3396.htm","linkFileType":{"id":5,"text":"html"}},{"id":249691,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0451/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":249690,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0451/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253260,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0451/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Massachusetts","county":"Berkshire County","otherGeospatial":"Cheshire quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -73.25,\n              42.625\n            ],\n            [\n              -73.25,\n              42.5\n            ],\n            [\n              -73.125,\n              42.5\n            ],\n            [\n              -73.125,\n              42.625\n            ],\n            [\n              -73.25,\n              42.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ff4","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":269087,"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":269088,"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":269086,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":68018,"text":"ha196 - 1964 - Synopsis of water resources of the Ipswich River Basin, Massachusetts","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha196","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":"196","title":"Synopsis of water resources of the Ipswich River Basin, Massachusetts","language":"ENGLISH","doi":"10.3133/ha196","usgsCitation":"Sammel, E.A., Brackley, R.A., and Palmquist, W., 1964, Synopsis of water resources of the Ipswich River Basin, Massachusetts: U.S. Geological Survey Hydrologic Atlas 196, 2 col. maps ;53-64 x 63-75 cm., https://doi.org/10.3133/ha196.","productDescription":"2 col. maps ;53-64 x 63-75 cm.","costCenters":[],"links":[{"id":190194,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89265,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/196/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89266,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/196/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"2500000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -71.20083333333334,42.5 ], [ -71.20083333333334,42.75 ], [ -70.75,42.75 ], [ -70.75,42.5 ], [ -71.20083333333334,42.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687d1d","contributors":{"authors":[{"text":"Sammel, Edward A.","contributorId":78320,"corporation":false,"usgs":true,"family":"Sammel","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277513,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brackley, Richard A.","contributorId":61792,"corporation":false,"usgs":true,"family":"Brackley","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":277511,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Palmquist, Wilbur Nathaniel","contributorId":69122,"corporation":false,"usgs":true,"family":"Palmquist","given":"Wilbur Nathaniel","affiliations":[],"preferred":false,"id":277512,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"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}]}}
,{"id":1999,"text":"wsp1651 - 1964 - Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:22","indexId":"wsp1651","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":"1651","title":"Chemical quality of surface waters and sedimentation in the Saline River basin, Kansas","docAbstract":"This report gives the results of an investigation of the sediment and dissolved minerals that are transported by the Saline River and its tributaries. The Saline River basin is in western and central Kansas; it is long and narrow and covers 3,420 square miles of rolling plains, which is broken in some places by escarpments and small areas of badlands. In the western part the uppermost bedrock consists predominantly of calcareous elastic sedimentary rocks of continental origin of Pliocene age and in most places is covered by eolian deposits of Pleistocene and Recent age. In the central part the ex posed bedrock consists predominantly of calcareous marine sedimentary rocks of Late Cretaceous age. In the eastern part the exposed bedrock consists mainly of noncalcareous continental and littoral elastic sedimentary rocks of Early Cretaceous and Permian age. Fluvial deposits are in the valleys, and eolian materials are present over much of the uplands. \r\n\r\nAverage precipitation increases rather uniformly from about 18 inches per year in the west to almost 28 inches per year in the east. Runoff is not affected by irrigation nor regulated by large structures, but it is closely related to precipitation. Average runoff increases from less than 0.2 inch per year in the west to more than 1.5 inches per year in the east. Aquifers of the flood-plain and terrace deposits and of the Cretaceous Dakota Sandstone are the major sources of ground-water accretion to the streams. In the upper reaches of the Saline River, the water is only slightly mineralized; during the period of record the specific conductance near Wakeeney never exceeded 750 micromhos per centimeter. In the lower reaches, however, the water is slightly mineralized during periods of high flow and is highly mineralized during periods of low flow; the specific conductance near Russell exceeded 1,500 micromhos per centimeter more than 80 percent of the time. Near Russell, near Wilson, and at Tescott the water is of the calcium bicarbonate type when the specific conductance is less than about 1,000 micromhos per centimeter, but it is of the sodium chloride type when the specific conductance is more than about 1,500 micromhos per centimeter. The water is off the calcium bicarbonate, sodium bicarbonate, or sodium chloride type when the conductance is between 1,000 and 1,500 micromhos per centimeter. Most of the increase in mineralization of the water is caused by inflow of highly mineralized ground water. The ground-water inflow was estimated to be 22 percent of the total streamflow at Tescott in 1948 and 60 percent in 1952. Mineralization increases and water quality deteriorates progressively downstream along nearly the entire Saline River, especially in the part of the area directly underlain by the Dakota Sandstone between the vicinities of Fairport and Wilson: sodium and chloride are the principal constituents of water contributed by the Dakota. The total percentage of the salt in the Saline River that comes from oil-field brines is considered to be small. The water in the upper Saline River is of good quality for domestic use except that it is hard; the water in the lower Saline River is of poor quality for domestic use because most of the time it is highly mineralized, is hard, and contains high concentrations of chloride and sulfate. In the upper reaches of the river, the water is of good quality for irrigation. In the lower reaches, if the water were impounded in a reservoir, it would be of good quality for irrigation during years of high flow and of very poor quality during years of low flow. The water in the lower reaches is of poor quality for industrial use because it is highly mineralized most of the tinge. Relations of suspended-sediment discharge to water discharge were used with the long-term streamflow duration curves to compute the long-term aver age suspended-sediment discharges and concentrations at five indications. Sediment discharge is closely related to runoff. 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R.","contributorId":82276,"corporation":false,"usgs":true,"family":"Boynton","given":"G.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":225221,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, Francis P.","contributorId":42574,"corporation":false,"usgs":true,"family":"Gilbert","given":"Francis","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":225220,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":14077,"text":"ofr6476 - 1964 - Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies","interactions":[],"lastModifiedDate":"2017-05-19T18:32:38","indexId":"ofr6476","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":"64-76","title":"Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6476","usgsCitation":"Henderson, R.G., and Wilson, A., 1964, Polar charts for calculating aeromagnetic anomalies of three-dimensional bodies: U.S. Geological Survey Open-File Report 64-76, 13 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr6476.","productDescription":"13 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":42714,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42715,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42716,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42717,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42718,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42719,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42720,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1964/0076/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":42721,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0076/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db684a33","contributors":{"authors":[{"text":"Henderson, Roland George","contributorId":43787,"corporation":false,"usgs":true,"family":"Henderson","given":"Roland","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":168892,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilson, Alphonso","contributorId":57467,"corporation":false,"usgs":true,"family":"Wilson","given":"Alphonso","email":"","affiliations":[],"preferred":false,"id":168893,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2544,"text":"wsp1586F - 1964 - On determining pollutant distribution in tidal estuaries","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1586F","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":"1586","chapter":"F","title":"On determining pollutant distribution in tidal estuaries","language":"ENGLISH","publisher":"U.S. Govt. Printing Off.,","doi":"10.3133/wsp1586F","usgsCitation":"Pyatt, E., 1964, On determining pollutant distribution in tidal estuaries: U.S. Geological Survey Water Supply Paper 1586, iv, 56 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1586F.","productDescription":"iv, 56 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":138659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1586f/report-thumb.jpg"},{"id":28787,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1586f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28788,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1586f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1586f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691be1","contributors":{"authors":[{"text":"Pyatt, E.E.","contributorId":31740,"corporation":false,"usgs":true,"family":"Pyatt","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":145376,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2016,"text":"wsp1779BB - 1964 - Ground-water resources of Mirage Flats, Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1779BB","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":"1779","chapter":"BB","title":"Ground-water resources of Mirage Flats, Nebraska","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1779BB","usgsCitation":"Keech, C.F., 1964, Ground-water resources of Mirage Flats, Nebraska: U.S. Geological Survey Water Supply Paper 1779, iii, 36 p. :ill., maps ;24 cm., https://doi.org/10.3133/wsp1779BB.","productDescription":"iii, 36 p. :ill., maps ;24 cm.","costCenters":[],"links":[{"id":137584,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1779bb/report-thumb.jpg"},{"id":27482,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1779bb/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27483,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1779bb/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d617","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144534,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":245,"text":"wsp1660B - 1964 - Summary of floods in the United States during 1958","interactions":[],"lastModifiedDate":"2017-09-06T17:48:22","indexId":"wsp1660B","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":"1660","chapter":"B","title":"Summary of floods in the United States during 1958","docAbstract":"<p>This report describes the most outstanding floods that occurred in the United States during 1958.</p><p>A series of storms from January 23 to February 16 brought large amounts of precipitation to northern California and produced damaging floods, particularly in the Lower Sacramento Valley where losses totaled about \\$12 million.</p><p>Major floods, notable because of the large area affected, occurred on many small streams in central and south Texas, following heavy general rains in late February. Extensive flooding occurred along the Gulf Coastal plain on the lower reaches of the major streams from the Brazos River to the Nueces River. Two lives were lost, and property damage exceeded \\$1 million.</p><p>Damaging floods of April 1-7 followed one of the wettest winters in California history. Swollen streams overflowed their banks throughout the central part of the State, and discharge peaks on many streams exceeded those .of the floods of December 1955. Most severely flooded was the San Francisco Bay area. Total flood damage was estimated at \\$23 million.</p><p>The storms and floods of April-May in Louisiana and adjacent States outranked all other floods in the United States during 1958 with respect to intensity of rain over a large area, number of streams having maximum discharge of record, rare occurrence of peaks, and great amount (\\$21 million) of resultant damage.</p><p>Heavy rains on June 8-15 caused one of the greatest summer floods of record in central Indiana. Peak discharges were high and of rare occurrences. Failure of numerous levees along the Wabash River caused great damage. Crop damage alone was estimated at \\$48 million.</p><p>Intense rains of July 1-2 caused record-breaking floods in southwestern Iowa. Rapid rises and the great magnitude of the floods on small streams resulted in 18 deaths and many injuries. Six towns and cities along the East Nishnabotna River and its tributaries were particularly hard hit; rural damage was also high. Total damage was estimated at \\$15 million.</p><p>Heavy rains (as much as 40 inches during the last 2 weeks in September) from the middle of September to the middle of October caused destructive floods along the Rio Grande in Texas and Mexico. Many communities were isolated by the flood waters, and damage to crops was great.</p><p>In addition to the 7 floods mentioned above, 21 others of lesser magnitude are reported in this annual summary.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1660B","collaboration":"Prepared in cooperation with Federal, State, and local agencies","usgsCitation":"Hendricks, E.L., 1964, Summary of floods in the United States during 1958: U.S. Geological Survey Water Supply Paper 1660, vi, 97 p., https://doi.org/10.3133/wsp1660B.","productDescription":"vi, 97 p.","numberOfPages":"104","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":136589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1660b/report-thumb.jpg"},{"id":24852,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1660b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db6992a6","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2029,"text":"wsp1617A - 1964 - Discharge characteristics of embankment-shaped weirs","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1617A","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":"1617","chapter":"A","title":"Discharge characteristics of embankment-shaped weirs","docAbstract":"An embankment-shaped weir is an embankment overtopped by flood waters. Among the engineering problems frequently resulting from. this occurrence is the need to compute the peak discharge from postflood yield observations. The research described in this. report was concerned with the theoretical and experimental bases for the computation procedure. \r\n\r\nThe research had two main objectives. One was to determine the relationship between embankment form and roughness and some of the more important discharge characteristics. The second was to define, theoretically and experimentally, the relationship between free-flow discharge and the boundary layer on the roadway. The first objective was accomplished with the experimental determination of coefficients of discharge and other significant flow characteristics for a variety of boundary and flow conditions. The second objective was accomplished with the development and experimental verification of a discharge equation which involved the boundary layer displacement thickness. This phase of the research included a general investigation of boundary layer growth on the roadway. \r\n\r\nIt is included that both free- and submerged-flow discharge are virtually independent of the influence of embankment shape and relative height. The influence of boundary resistance is appreciable only for smaller heads. The most practical solution for discharge is one which is based on. the simple weir equation and experimentally determined coefficients. A completely analytical equation of discharge is impractical. \r\n\r\nThe report contains the results of 936 experiments on the discharge characteristics of 17 different models; plus 106 boundary-layer velocity traverses on 4 different models. The data are summarized in both graphical and tabular form.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1617A","usgsCitation":"Kindsvater, C.E., 1964, Discharge characteristics of embankment-shaped weirs: U.S. Geological Survey Water Supply Paper 1617, v, 11 p. :tables, graphs, diagrs, illus. ;24 cm., https://doi.org/10.3133/wsp1617A.","productDescription":"v, 11 p. :tables, graphs, diagrs, illus. ;24 cm.","costCenters":[],"links":[{"id":137646,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1617a/report-thumb.jpg"},{"id":27502,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1617a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae939","contributors":{"authors":[{"text":"Kindsvater, Carl E.","contributorId":73182,"corporation":false,"usgs":true,"family":"Kindsvater","given":"Carl","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144552,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":24825,"text":"ofr64170 - 1964 - Floods in Oklahoma: magnitude and frequency","interactions":[],"lastModifiedDate":"2017-09-29T08:11:18","indexId":"ofr64170","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":"64-170","title":"Floods in Oklahoma: magnitude and frequency","docAbstract":"<p>This report presents methods by which the magnitude and frequency of expected floods for most streams in Oklahoma can be determined. Flood data were used to define flood-frequency curves applicable to the State. Composite frequency curves were drawn showing the relation of mean annual floods to floods having recurrence intervals from 1.2 to 50 years. In some areas, it was found that the slope of the composite frequency curve varies with the drainage area. An adjustment curve was defined for use in conjunction with the composite curve for these areas. Other curves express the relation of the mean annual flood to drainage basin characteristics. By combining data from the composite and mean annual flood curves, flood-frequency curves can be drawn for streams in Oklahoma not materially affected by the works of man. Neither of the above two types of curves should be extrapolated beyond the range defined by base data. Frequency curves presented in this report were based on analysis of flood records collected at gaging stations having 5 or more years of record not materially affected by regulation or diversion.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr64170","issn":"0094-9140","collaboration":"Prepared in cooperation with the State of Oklahoma Department of Highways and United States Department of Commerce Bureau of Public Roads","usgsCitation":"Westfall, A., and Patterson, J., 1964, Floods in Oklahoma: magnitude and frequency: U.S. Geological Survey Open-File Report 64-170, ix, 105 p., https://doi.org/10.3133/ofr64170.","productDescription":"ix, 105 p.","costCenters":[],"links":[{"id":157115,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1964/0170/report-thumb.jpg"},{"id":346204,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1964/0170/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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