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,{"id":22588,"text":"ofr5912 - 1959 - Ground-water movement in a rectangular aquifer bounded by four ditches or canals","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr5912","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-12","title":"Ground-water movement in a rectangular aquifer bounded by four ditches or canals","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey, Water Resources Division, Ground Water Branch,","doi":"10.3133/ofr5912","issn":"0094-9140","usgsCitation":"Brown, R.H., 1959, Ground-water movement in a rectangular aquifer bounded by four ditches or canals: U.S. Geological Survey Open-File Report 59-12, 14 p. :ill. ;27 cm., https://doi.org/10.3133/ofr5912.","productDescription":"14 p. :ill. ;27 cm.","costCenters":[],"links":[{"id":155341,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667445","contributors":{"authors":[{"text":"Brown, Russell H.","contributorId":106151,"corporation":false,"usgs":true,"family":"Brown","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188522,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22587,"text":"ofr5914 - 1959 - The development of the cone of depression around a pumped well in an infinite strip aquifer subject to uniform recharge","interactions":[],"lastModifiedDate":"2012-02-02T00:07:57","indexId":"ofr5914","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-14","title":"The development of the cone of depression around a pumped well in an infinite strip aquifer subject to uniform recharge","language":"ENGLISH","doi":"10.3133/ofr5914","issn":"0094-9140","usgsCitation":"Brown, R.H., 1959, The development of the cone of depression around a pumped well in an infinite strip aquifer subject to uniform recharge: U.S. Geological Survey Open-File Report 59-14, 15 p. (2 folded) :ill. ;28 cm., https://doi.org/10.3133/ofr5914.","productDescription":"15 p. (2 folded) :ill. ;28 cm.","costCenters":[],"links":[{"id":112997,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1959/0014/report.pdf","size":"1075","linkFileType":{"id":1,"text":"pdf"}},{"id":155340,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1959/0014/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668620","contributors":{"authors":[{"text":"Brown, Russell H.","contributorId":106151,"corporation":false,"usgs":true,"family":"Brown","given":"Russell","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":188521,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":53456,"text":"ofr5938 - 1959 - Geology and ground-water hydrology of the Mill Creek area, San Bernardino County, California","interactions":[],"lastModifiedDate":"2012-02-02T00:11:54","indexId":"ofr5938","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-38","title":"Geology and ground-water hydrology of the Mill Creek area, San Bernardino County, California","language":"ENGLISH","doi":"10.3133/ofr5938","usgsCitation":"Dutcher, L.C., and Burnham, W., 1959, Geology and ground-water hydrology of the Mill Creek area, San Bernardino County, California: U.S. Geological Survey Open-File Report 59-38, 229 p. : ill., maps (in pocket), fold. plates ; 27 cm., https://doi.org/10.3133/ofr5938.","productDescription":"229 p. : ill., maps (in pocket), fold. plates ; 27 cm.","costCenters":[],"links":[{"id":100365,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0038/plate-1.pdf","size":"6005","linkFileType":{"id":1,"text":"pdf"}},{"id":100366,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0038/plate-2.pdf","size":"4374","linkFileType":{"id":1,"text":"pdf"}},{"id":100367,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0038/plate-3.pdf","size":"2823","linkFileType":{"id":1,"text":"pdf"}},{"id":173927,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1959/0038/report-thumb.jpg"},{"id":87446,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1959/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685e04","contributors":{"authors":[{"text":"Dutcher, Lee Carlton","contributorId":32229,"corporation":false,"usgs":true,"family":"Dutcher","given":"Lee","email":"","middleInitial":"Carlton","affiliations":[],"preferred":false,"id":247650,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Burnham, W.L.","contributorId":58668,"corporation":false,"usgs":true,"family":"Burnham","given":"W.L.","email":"","affiliations":[],"preferred":false,"id":247651,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":46960,"text":"ofr5959 - 1959 - Geologic and structure map of the Sage Spring Creek oil field and vicinity, Natrona and Converse Counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:42","indexId":"ofr5959","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"59-59","title":"Geologic and structure map of the Sage Spring Creek oil field and vicinity, Natrona and Converse Counties, Wyoming","language":"ENGLISH","doi":"10.3133/ofr5959","usgsCitation":"Horn, G.H., 1959, Geologic and structure map of the Sage Spring Creek oil field and vicinity, Natrona and Converse Counties, Wyoming: U.S. Geological Survey Open-File Report 59-59, 1 map, https://doi.org/10.3133/ofr5959.","productDescription":"1 map","costCenters":[],"links":[{"id":171568,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":99849,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1959/0059/plate-1.pdf","size":"8668","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8041","contributors":{"authors":[{"text":"Horn, George Henry","contributorId":91475,"corporation":false,"usgs":true,"family":"Horn","given":"George","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":234397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34998,"text":"b1072F - 1959 - Mineral occurrences of New York State with selected references to each locality","interactions":[],"lastModifiedDate":"2021-08-31T21:10:49.6029","indexId":"b1072F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1072","chapter":"F","title":"Mineral occurrences of New York State with selected references to each locality","docAbstract":"<p>References and locations were compiled for more than 1,000 mineral occurrences in New York State. Each occurrence is shown on an accompanying map and is given by commodity and county in a locality list. 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,{"id":61435,"text":"mf182 - 1959 - Bedrock geology of the northern and eastern parts of the North Range, Cuyuna district, Minnesota","interactions":[],"lastModifiedDate":"2019-05-28T08:25:02","indexId":"mf182","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"182","title":"Bedrock geology of the northern and eastern parts of the North Range, Cuyuna district, Minnesota","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf182","usgsCitation":"Schmidt, R.G., 1959, Bedrock geology of the northern and eastern parts of the North Range, Cuyuna district, Minnesota: U.S. Geological Survey Miscellaneous Field Studies Map 182, 1 map on 5 sheets, https://doi.org/10.3133/mf182.","productDescription":"1 map on 5 sheets","costCenters":[],"links":[{"id":182872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0182/report-thumb.jpg"},{"id":364160,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0182/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364161,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0182/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364159,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0182/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364163,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0182/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":364162,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0182/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"7200","country":"United States","state":"Minnesota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.1,46.45 ], [ -94.1,46.55 ], [ -93.81694444444445,46.55 ], [ -93.81694444444445,46.45 ], [ -94.1,46.45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633f4b","contributors":{"authors":[{"text":"Schmidt, R. G.","contributorId":107690,"corporation":false,"usgs":true,"family":"Schmidt","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":265637,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","interactions":[{"subject":{"id":22843,"text":"ofr5636 - 1956 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"ofr5636","publicationYear":"1956","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"predicate":"SUPERSEDED_BY","object":{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"wsp1469","publicationYear":"1959","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"id":1},{"subject":{"id":44087,"text":"ofr5466 - 1954 - Table showing estimated ground-water storage capacity of the San Joaquin Valley, California, and map showing ground-water storage units in the San Joaquin Valley","indexId":"ofr5466","publicationYear":"1954","noYear":false,"title":"Table showing estimated ground-water storage capacity of the San Joaquin Valley, California, and map showing ground-water storage units in the San Joaquin Valley"},"predicate":"SUPERSEDED_BY","object":{"id":3095,"text":"wsp1469 - 1959 - Ground-water conditions and storage capacity in the San Joaquin Valley, California","indexId":"wsp1469","publicationYear":"1959","noYear":false,"title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"wsp1469","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1469","title":"Ground-water conditions and storage capacity in the San Joaquin Valley, California","docAbstract":"The San Joaquin Valley includes roughly the southern two-thirds of the Great \r\nCentral Valley of California. It is a broad structural trough surrounded by \r\nmountains. The northern part of the valley drains through the San Joaquin \r\nRiver northward to San Francisco Bay ; the southern part of the valley normally \r\nis a basin of interior drainage tributary to evaporation sumps in the trough of \r\nthe valley, chiefly Tulare and Buena Vista Lake beds. \r\nIn years of normal discharge most of the streamflow in the southern part of \r\nthe valley not diverted for irrigation finds its way to Tulare and Buena Vista \r\nLake beds. In the historic past, however, during years of heavy floods the low \r\ndivide between Buena Vista and Tulare Lakes and the low divide between \r\nTulare Lake and the San Joaquin River were overtopped and through-flowing \r\ndrainage occurred over the full length of the valley. Because the Tulare Lake \r\nbed is the lowest point and also the largest sump, this whole basin of interior \r\ndrainage is commonly referred to as the Tulare Lake drainage basin. \r\nAverage annual precipitation ranges from more than 15 inches in the north- \r\neastern part of the valley to less than 4 inches in the southwestern part. The \r\nprecipitation decreases from north to south and from east to west across the \r\nvalley. Streamflow, the critical quantity in the water supply, depends almost \r\nwholly on the amount and distribution of precipitation in the Sierra Nevada to \r\nthe east. Much of this precipitation falls as snow, and the snowpack acts as a \r\nnatural reservoir retaining much of the annual runoff until late spring and early \r\nsummer. \r\nThe mean seasonal runoff to the San Joaquin Valley is nearly 10 million acre- \r\nfeet, of which about two-thirds is tributary to the San Joaquin River; the remaining third is tributary to Tulare Lake drainage basin. In 1952 about 8.5 \r\nmillion acre-feet of surface water was diverted for irrigation. Withdrawals of \r\nground water for irrigation in 1952 approximated 7.5 million acre-feet. \r\nThe surface of the San Joaquin Valley is not a featureless plain but is characterized by various types of physiography such as dissected uplands, low \r\nalluvial plains and fans, river flood plains and channels, and overflow lands \r\nand lake bottoms. \r\nThe dissected uplands fringe the valley along its mountain borders. They are \r\nunderlain by unconsolidated to semiconsolidated continental deposits of late \r\nTertiary and early Quaternary age which have been moderately tilted and \r\nfolded. The topography of these uplands ranges from deeply dissected hill land \r\nhaving a relief of several hundred feet to gently rolling land whose relief Is only \r\na few feet. \r\nThe low plains and fans border the dissected uplands along their valley- \r\nward margins. They are generally fiat to gently undulating and featureless and are underlain by undeformed to slightly deformed alluvial deposits of \r\nQuaternary age. \r\nThe river flood plains and channels lie along the San Joaquia and Kings \r\nRivers in the axial part of the valley and along the major east-side streams. \r\nWhere the rivers are incised below the general land surface, the flood plains are \r\nwell defined; but in the axial trough of the valley, where the rivers are flanked \r\nby low-lying overflow lands, the flood-plain and channel deposits are confined to \r\nthe stream channel and to the natural levees that slope away from the river. \r\nOverflow lands and lake bottoms include the historic beds of Tulare, Buena \r\nVista, and Kern Lakes in the southern part of the valley, and the low-lying lands \r\nin the axial trough between the low alluvial plains and fans and the natural \r\nlevees of the San Joaquin River and its major tributaries. They are level and \r\nfeatureless and are underlain by lake and swamp deposits of Recent age. \r\nThe San Joaquin Valley is a great structural downwarp between the tilted \r\nblock of the Sierra Nevada on the east and the complexly folded and faulted \r\nCoast Ranges on the we","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1469","usgsCitation":"Davis, G.H., Green, J.H., Olmsted, F.H., and Brown, D.W., 1959, Ground-water conditions and storage capacity in the San Joaquin Valley, California: U.S. Geological Survey Water Supply Paper 1469, viii, 287 p. :diagrs., tables. and portfolio (fold. maps (part col.) diagrs., profiles) ;24 cm., https://doi.org/10.3133/wsp1469.","productDescription":"viii, 287 p. :diagrs., tables. and portfolio (fold. maps (part col.) diagrs., profiles) ;24 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,{"id":61460,"text":"mf211 - 1959 - Preliminary geologic and structure map of the southwest part of the Cascade Springs quadrangle, Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2018-12-14T11:09:53","indexId":"mf211","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"211","title":"Preliminary geologic and structure map of the southwest part of the Cascade Springs quadrangle, Fall River County, South Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf211","usgsCitation":"Post, E., 1959, Preliminary geologic and structure map of the southwest part of the Cascade Springs quadrangle, Fall River County, South Dakota: U.S. Geological Survey Miscellaneous Field Studies Map 211, 36.57 x 30.77 inches, https://doi.org/10.3133/mf211.","productDescription":"36.57 x 30.77 inches","costCenters":[],"links":[{"id":360301,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0211/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182778,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0211/report-thumb.jpg"}],"country":"United States","state":"South Dakota","county":"Fall River County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -130.5511111111111,43.25 ], [ -130.5511111111111,43.284166666666664 ], [ -103.61749999999999,43.284166666666664 ], [ -103.61749999999999,43.25 ], [ -130.5511111111111,43.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c2f7","contributors":{"authors":[{"text":"Post, Edwin V.","contributorId":80330,"corporation":false,"usgs":true,"family":"Post","given":"Edwin V.","affiliations":[],"preferred":false,"id":265692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60050,"text":"mf200 - 1959 - Preliminary geologic map of the Elk Ridge 1 SW quadrangle, San Juan County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:39","indexId":"mf200","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"200","title":"Preliminary geologic map of the Elk Ridge 1 SW quadrangle, San Juan County, Utah","language":"ENGLISH","doi":"10.3133/mf200","usgsCitation":"Lewis, R., and Campbell, R.H., 1959, Preliminary geologic map of the Elk Ridge 1 SW quadrangle, San Juan County, Utah: U.S. Geological Survey Miscellaneous Field Studies Map 200, 1 map., https://doi.org/10.3133/mf200.","productDescription":"1 map.","costCenters":[],"links":[{"id":104003,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2619.htm","linkFileType":{"id":5,"text":"html"},"description":"2619"},{"id":179959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.75,37.75 ], [ -109.75,37.8675 ], [ -109.61749999999999,37.8675 ], [ -109.61749999999999,37.75 ], [ -109.75,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b747","contributors":{"authors":[{"text":"Lewis, R.Q.","contributorId":91910,"corporation":false,"usgs":true,"family":"Lewis","given":"R.Q.","affiliations":[],"preferred":false,"id":263056,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, R. H.","contributorId":52160,"corporation":false,"usgs":true,"family":"Campbell","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":263055,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35048,"text":"b1019M - 1959 - Annotated bibliography on the geology of selenium","interactions":[],"lastModifiedDate":"2012-02-02T00:09:44","indexId":"b1019M","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1019","chapter":"M","title":"Annotated bibliography on the geology of selenium","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1019M","usgsCitation":"Luttrell, G., 1959, Annotated bibliography on the geology of selenium: U.S. Geological Survey Bulletin 1019, p. 867-972, maps (1 fold. in pocket) ;24 cm., https://doi.org/10.3133/b1019M.","productDescription":"p. 867-972, maps (1 fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":247527,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1019m/report.pdf","size":"6055","linkFileType":{"id":1,"text":"pdf"}},{"id":247528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1019m/plate-5.pdf","size":"2026","linkFileType":{"id":1,"text":"pdf"}},{"id":252038,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1019m/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd78","contributors":{"authors":[{"text":"Luttrell, Gwendolyn Lewise Werth","contributorId":80658,"corporation":false,"usgs":true,"family":"Luttrell","given":"Gwendolyn Lewise Werth","affiliations":[],"preferred":false,"id":214035,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35565,"text":"b1072I - 1959 - Beryl deposits of the Beecher No. 3-Black Diamond pegmatite, Custer County, South Dakota","interactions":[],"lastModifiedDate":"2022-01-14T20:02:42.917949","indexId":"b1072I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1072","chapter":"I","title":"Beryl deposits of the Beecher No. 3-Black Diamond pegmatite, Custer County, South Dakota","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1957","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1072I","usgsCitation":"Redden, J.A., 1959, Beryl deposits of the Beecher No. 3-Black Diamond pegmatite, Custer County, South Dakota: U.S. Geological Survey Bulletin 1072, Report: 23 p.; 2 Plates: 26.82 × 48.90 iniches and  22.76 × 15.35 inches, https://doi.org/10.3133/b1072I.","productDescription":"Report: 23 p.; 2 Plates: 26.82 × 48.90 iniches and  22.76 × 15.35 inches","costCenters":[],"links":[{"id":96969,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1072i/plate-18.pdf","size":"214","linkFileType":{"id":1,"text":"pdf"}},{"id":109282,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20721.htm","linkFileType":{"id":5,"text":"html"},"description":"20721"},{"id":63463,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1072i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166901,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1072i/report-thumb.jpg"},{"id":96968,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1072i/plate-17.pdf","size":"4406","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"South Dakota","county":"Custer County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -103.562,\n              43.711\n            ],\n            [\n              -103.572,\n              43.711\n            ],\n            [\n              -103.572,\n              43.697\n            ],\n            [\n              -103.562,\n              43.697\n            ],\n            [\n              -103.562,\n              43.711\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a52e4b07f02db62aaed","contributors":{"authors":[{"text":"Redden, Jack Allison","contributorId":107676,"corporation":false,"usgs":true,"family":"Redden","given":"Jack","email":"","middleInitial":"Allison","affiliations":[],"preferred":false,"id":214861,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":34836,"text":"b1046R - 1959 - Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:27","indexId":"b1046R","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1046","chapter":"R","title":"Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1046R","usgsCitation":"Kepferle, R.C., 1959, Uranium in Sharon Springs member of Pierre shale, South Dakota and northeastern Nebraska: U.S. Geological Survey Bulletin 1046, p. 577-604, ill., maps (fold. in pocket) ;24 cm., https://doi.org/10.3133/b1046R.","productDescription":"p. 577-604, ill., maps (fold. in pocket) ;24 cm.","costCenters":[],"links":[{"id":109228,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20656.htm","linkFileType":{"id":5,"text":"html"},"description":"20656"},{"id":163976,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1046r/report-thumb.jpg"},{"id":62785,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62786,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62787,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62788,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1046r/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":62789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1046r/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db6054ce","contributors":{"authors":[{"text":"Kepferle, Roy Clark","contributorId":46072,"corporation":false,"usgs":true,"family":"Kepferle","given":"Roy","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":213667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39068,"text":"pp314H - 1959 - Pre-Atoka rocks of northern Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:09:59","indexId":"pp314H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"314","chapter":"H","title":"Pre-Atoka rocks of northern Arkansas","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1957","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp314H","usgsCitation":"Frezon, S., and Glick, E., 1959, Pre-Atoka rocks of northern Arkansas: U.S. Geological Survey Professional Paper 314, p. 171-189, https://doi.org/10.3133/pp314H.","productDescription":"p. 171-189","costCenters":[],"links":[{"id":120125,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0314h/report-thumb.jpg"},{"id":66330,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66331,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66332,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66333,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66334,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66335,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66336,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66337,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66338,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66339,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66340,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66341,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0314h/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0314h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf01","contributors":{"authors":[{"text":"Frezon, S. E.","contributorId":83904,"corporation":false,"usgs":true,"family":"Frezon","given":"S. E.","affiliations":[],"preferred":false,"id":220891,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Glick, E.E.","contributorId":12060,"corporation":false,"usgs":true,"family":"Glick","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":220890,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35218,"text":"b1093 - 1959 - Surficial geology of Anchorage and vicinity, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"b1093","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1093","title":"Surficial geology of Anchorage and vicinity, Alaska","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1093","usgsCitation":"Miller, R.D., and Dobrovolny, E., 1959, Surficial geology of Anchorage and vicinity, Alaska: U.S. Geological Survey Bulletin 1093, 128 p. illus., col. map, diagrs., tables. ;24 cm., https://doi.org/10.3133/b1093.","productDescription":"128 p. illus., col. map, diagrs., tables. ;24 cm.","costCenters":[],"links":[{"id":109322,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20778.htm","linkFileType":{"id":5,"text":"html"},"description":"20778"},{"id":93194,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93195,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93196,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93197,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93198,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93199,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1093/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":93200,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1093/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166439,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1093/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d1e","contributors":{"authors":[{"text":"Miller, Robert D.","contributorId":85168,"corporation":false,"usgs":true,"family":"Miller","given":"Robert","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":214270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dobrovolny, Ernest","contributorId":45288,"corporation":false,"usgs":true,"family":"Dobrovolny","given":"Ernest","affiliations":[],"preferred":false,"id":214269,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":33740,"text":"b1077 - 1959 - Geology of the Lake Mary quadrangle, Iron County, Michigan","interactions":[{"subject":{"id":12610,"text":"ofr565 - 1956 - Preliminary report on the geology of Lake Mary quadrangle, Iron County, Michigan","indexId":"ofr565","publicationYear":"1956","noYear":false,"title":"Preliminary report on the geology of Lake Mary quadrangle, Iron County, Michigan"},"predicate":"SUPERSEDED_BY","object":{"id":33740,"text":"b1077 - 1959 - Geology of the Lake Mary quadrangle, Iron County, Michigan","indexId":"b1077","publicationYear":"1959","noYear":false,"title":"Geology of the Lake Mary quadrangle, Iron County, Michigan"},"id":1}],"lastModifiedDate":"2016-08-26T14:32:11","indexId":"b1077","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1959","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":"1077","title":"Geology of the Lake Mary quadrangle, Iron County, Michigan","docAbstract":"<p>The Lake Mary quadrangle is in eastern Iron County, in the west part of the Upper Peninsula of Michigan. The quadrangle is underlain by Lower and Middle Precambrian rocks, formerly designated Archean and Algonkian rocks, and is extensively covered by Pleistocene glacial deposits. A few Upper Precambrian (Keweenawan) diabase dikes and two remnants of sandstone and dolomite of early Paleozoic age are also found in the area. </p><p>The major structural feature is the Holmes Lake anticline, the axis of which strikes northwest through the northeast part of the quadrangle. Most of the quadrangle, therefore, is underlain by rock of the west limb of the anticline. To the northwest along the fold axis, the Holmes Lake anticline is separated from the Amasa oval by a saddle of transverse folds in the vicinity of Michigamme Mountain in the Kiernan quadrangle. </p><p>The Lower Precambrian rocks are represented by the Dickinson group and by porphyritic red granite whose relation to the Dickinson group is uncertain, but which may be older. The rocks of the Dickinson group are chiefly green to black metavolcanic schist and red felsite, some of the latter metarhyolite. The dark schist is commonly magnetic. The Dickinson group underlies the core area of the Holmes Lake anticline, which is flanked by steeply dipping Middle Precambrian formations of the Animikie series. </p><p>A major unconformity separates the Lower Precambrian rocks from the overlying Middle Precambrian rocks. In ascending order the formations of the Middle Precambrian are the Randville dolomite, the Hemlock formation, which includes the Mansfield iron-bearing slate member, and the Michigamme slate. An unconformity occurs between the Hemlock formation and Michigamme slate. The post-Hemlock unconformity is thought to be represented in the Lake Mary quadrangle by the absence of iron-formation of the Amasa formation, which is known to lie between the Hemlock and the Michigamme to the northwest of the Lake Mary quadrangle in the Crystal Falls quadrangle. Post-Hemlock erosion may account also for the absence of iron-formation of the Fence River formation on the east limb of the Holmes Lake anticline within the Lake Mary quadrangle. </p><p>The Randville dolomite is not exposed and is known only from diamond drilling in the northeast part of the area where it occurs in the east and west limbs of the Holmes Lake anticline. The formation has a maximum thickness of about 2,100 feet; this includes a lower arkosic phase, some of which is quartz pebble conglomerate, a medial dolomitic phase, and an upper slate phase. The triad is gradational. Included within the formation are a few beds of chloritic schist thought to be of volcanic origin. An&nbsp;unconformity between the Randville and the succeeding Hemlock is not indicated in the quadrangle, but is probably present. </p><p>The Hemlock formation is best exposed in the northwest and south-central parts of the area. The apparent thickness of the formation is 10,000- 17,000 feet. It is composed mainly of mafic metavolcanic rocks and intercalated slate and iron-formation. In the north part of the quadrangle the volcanic rocks are greenstone, which includes altered basaltic flow rocks, volcanic breccia, tuff, and slate. Pillow structures are common in the metabasalt. It is not certain if any Hemlock rocks are present in the east limb of the Holmes Lake anticline. In the south part of the quadrangle, the rocks of the Hemlock are chiefly chlorite and hornblende schist and hornfels. Pyroxene hornfels is sparingly present. </p><p>At least two sedimentary slate belts are included in the Hemlock formation. One of these, the Mansfield iron-bearing slate member, includes in its upper part an altered chert-siderite iron-formation 30 to over 150 feet thick from which iron ore has been mined at the Mansfield location. The position of the iron-bearing rocks has been determined magnetically, and past explorations for iron ore are discussed. </p><p>Though probably; unconformable, the contact between the Hemlock and the Michigamme formations appears conformable. The Michigamme slate consists of at least 4,000 feet of interbedded mica schist and granulite, the altered equivalents of the slate and graywacke characteristic of the Michigamme in adjacent areas. The Michigamme rocks are best exposed in the south part of the quadrangle in the vicinity of Peavy Pond. </p><p>Two periods of regional metamorphism have resulted in the alteration of almost all of the rocks of the quadrangle. The Lower Precambrian rocks underwent at least one period of metamorphism, uplift, and erosion before the deposition of the Randville dolomite. After the deposition of the Michigamme slate, a post-Middle Precambrian period of regional metamorphism occurred with attending deformation and igneous intrusion. The grade of metamorphism rises toward the south in the area. The rocks in the northern two-thirds of the quadrangle are representative of greenschist facies of regional metamorphism, whereas the rocks in the southern onethird of the quadrangle are representative of the albite-epidote-amphibolite, the amphibolite, and the pyroxene hornfels facies, the metamorphic node centering about the intrusive Peavy Pond complex in the Peavy Pond area. </p><p>The Precambrian sedimentary and volcanic rocks are cut by intrusive igneous rocks of different types and several different ages. Gabbroic sills and dikes invaded the Hemlock rocks at some time after the Hemlock was deposited and before the post-Middle Precambrian orogeny and metamorphism. Some contact metamorphism attended the intrusion of the major sills. One of the sills, the West Kiernan sill, is well differentiated. A syntectonic igneous body, composed of gabbro and minor ultramafic parts and fringed with intermediate and felsic differentiates and hybrids, the Peavy; Pond complex, was intruded into the Hemlock and Michigamme formations during the post-Middle Precambrian orogeny. The complex is situated in the Peavy Pond area at the crest of the regional metamorphic node. Contact-altered sedimentary and volcanic rocks margin the complex. </p><p>The effects of regional metamorphism have been superposed on the contact metamorphic rocks peripheral to the complex and on the igneous rocks of the complex as well. The mafic augite-bearing rocks of the complex emplaced early in the orogeny were deformed by granulation at the peak of the deformation and subsequently metamorphosed to hornblende rocks. Some of the intermediate and felsic rocks of the complex were foliated by the deformation, while the more fluid, felsic parts of the complex were intruded under orogenic stress and crystallized after the peak of deformation. The deformation culminated in major faulting during which the formations were dislocated, and some of the granite of the complex was extremely brecciated. </p><p>A few diabase dikes, probably of Keweenawan age, have intruded the deformed and altered Animikie rocks. </p><p>The only known metallic resource is iron ore. The Mansfield mine produced 1¥2 million tons of high-grade iron ore between the years 1890 and 1913. Sporadic exploration since 1913 has failed to reveal other ore deposits of economic importance.</p>","language":"English","publisher":"U. S. 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