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,{"id":13417,"text":"ofr6142 - 1961 - Geology of uranium in the Chadron area, Nebraska and South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:06:50","indexId":"ofr6142","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-42","title":"Geology of uranium in the Chadron area, Nebraska and South Dakota","docAbstract":"The Chadron area covers 375 square miles about 25 miles southeast of the Black Hills. Recurrent mild tectonic activity and erosion on the Chadron arch, a compound anticlinal uplift of regional extent, exposed 1900 feet of Upper Cretaceous rocks, mostly marine shale containing pyrite and organic matter, and 600 feet of Oligocene and Miocene rocks, mostly terrestrial fine-grained sediment containing volcanic ash. Each Cretaceous formation truncated by the sub-Oligocene unconformity is stained yellow and red, leached, kaolinized, and otherwise altered to depths as great as 55 feet. The composition and profile of the altered material indicate lateritic soil; indirect evidence indicates Eocene(?) age. In a belt through the central part of the area, the Brule formation of Oligocene age is a sequence of bedded gypsum, clay, dolomite, and limestone more than 300 feet thick.\r\n\r\nUranium in Cretaceous shale in 58 samples averages 0.002 percent, ten times the average for the earth\u0019s crust. Association with pyrite and organic matter indicates low valency. The uranium probably is syngenetic or nearly so.\r\n\r\nUranium in Eocene(?) soil in 43 samples averages 0.054 percent, ranging up to 1.12 percent. The upper part of the soil is depleted in uranium; enriched masses in the basal part of the soil consist of remnants of bedrock shale and are restricted to the highest reaches of the ancient oxidation-reduction interface. The uranium is probably in the from of a low-valent mineral, perhaps uraninite. Modern weathering of Cretaceous shale is capable of releasing as much as 0.780 ppm uranium to water. Eocene(?) weathering probably caused enrichment of the ancient soil through 1) leaching of Cretaceous shale, 2) downward migration of uranyl complex ions, and 3) reduction of hydrogen sulfide at the water table.\r\n\r\nUranium minerals occur in the basal 25 feet of the gypsum facies of the Brule formation at the two localities where the gypsum is carbonaceous; 16 samples average 0.066 percent uranium and range up to 0.43 percent. Elsewhere uranium in dolomite and limestone in the basal 25 feet of the gypsum facies in 10 samples averages 0.007 percent, ranging up to 0.12 percent. Localization of the uranium at the base of the gypsum facies suggests downward moving waters; indirect evidence that the water from which the gypsum was deposited was highly alkaline suggests that the uranium was leached from volcanic ash in Oligocene time.","language":"ENGLISH","publisher":"U.S. Geological Survey],","doi":"10.3133/ofr6142","usgsCitation":"Dunham, R.J., 1961, Geology of uranium in the Chadron area, Nebraska and South Dakota: U.S. Geological Survey Open-File Report 61-42, viii, 243 p. :ill., maps ;29 cm., https://doi.org/10.3133/ofr6142.","productDescription":"viii, 243 p. :ill., maps ;29 cm.","costCenters":[],"links":[{"id":146083,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0042/report-thumb.jpg"},{"id":41852,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":41853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1961/0042/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c700","contributors":{"authors":[{"text":"Dunham, Robert Jacob","contributorId":74387,"corporation":false,"usgs":true,"family":"Dunham","given":"Robert","email":"","middleInitial":"Jacob","affiliations":[],"preferred":false,"id":167777,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64812,"text":"i332 - 1961 - Geologic map of a part of southwestern Wyoming and adjacent States","interactions":[],"lastModifiedDate":"2012-02-02T00:13:02","indexId":"i332","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"332","subseriesTitle":"NONE","title":"Geologic map of a part of southwestern Wyoming and adjacent States","language":"ENGLISH","doi":"10.3133/i332","usgsCitation":"Bradley, W.H., 1961, Geologic map of a part of southwestern Wyoming and adjacent States: U.S. Geological Survey IMAP 332, 1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i332.","productDescription":"1 map :col. ;86 x 131 cm. folded to 28 x 20 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102824,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1290.htm","linkFileType":{"id":5,"text":"html"},"description":"1290"},{"id":187277,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":91442,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0332/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2a5d","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":272197,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47386,"text":"b1082L - 1961 - Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado","interactions":[{"subject":{"id":47386,"text":"b1082L - 1961 - Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado","indexId":"b1082L","publicationYear":"1961","noYear":false,"chapter":"L","title":"Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado"},"predicate":"IS_PART_OF","object":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"id":1}],"isPartOf":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"lastModifiedDate":"2017-10-18T15:54:08","indexId":"b1082L","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1082","chapter":"L","title":"Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado","docAbstract":"<p>The area of the Piceance Creek basin between the Colorado and White Rivers includes approximately 1,600 square miles and is characterized by an extensive plateau that rises 1,000 to more than 4,000 feet above the surrounding lowlands. Relief is greatest in Naval Oil-Shale Reserves Nos. 1 and 3 near the south margin of the area, where the spectacular Roan Cliffs tower above the valley of the Colorado River. </p><p>The oldest rocks exposed in the mapped area are sandstone, shale, and coal beds of the Mesaverde group of Late Cretaceous age, which crop out along the east margin of the area. Overlying the Mesaverde is an unnamed sequence of dark-colored sandstone and shale, Paleocene in age. The Ohio Creek conglomerate, composed of black and red chert and quartzite pebbles in a white sandstone matrix, is probably the basal unit in the Paleocene sequence. The Wasatch formation of early Eocene age overlies the Paleocene sedimentary rocks. It is composed of brightly colored shale, lenticular beds of sandstone, and a few thin beds of fresh-water limestone. The Kasatch formation interfingers with and is overlain by the Green River formation of middle Eocene age. </p><p>The Green River formation has been divided into the Douglas Creek, Garden Gulch, Anvil Points, Parachute Creek, and Evacuation Creek members. The basal and uppermost members, the Douglas Creek and Evacuation Creek, respectively, are predominantly sandy units. The two middle members, the Garden Gulch and Parachute Creek, are composed principally of finer clastic rocks. The Anvil Points member is present only on the southeast, east, and northeast margins of the area. It is a nearshore facies composed principally of sandstone and is the equivalent of the Douglas Creek, Garden Gulch, and the lower part of the Parachute Creek members. </p><p>All of the richer exposed oil-shale beds are found in the Parachute Creek member, which is divided into two oil-shale zones by a series of low-grade oilshale beds. The upper oil-shale zone has several key beds and zones which can be traced throughout most of the mapped area. One of these, the Mahogany ledge or zone, is a group of very rich oil-shale beds at the base of the upper oil-shale zone. Drilling for oil and gas in the northeastern part of the area has revealed rich oil-shale zones in the Garden Gulch member also.</p><p>Local unconformities within and at the base of the Evacuation Creek member are exposed at several places along Piceance Creek and at one place near the mouth of Yellow Creek; otherwise, the rock sequence is conformable. </p><p>The mapped area is the major part of a large syncline, modified by numerous smaller structural features. Fractures, probably associated genetically with the minor structural features, are present in the central part of the area. These fractures are high-angle normal faults with small displacement. They occur in pairs with the intervening block downdropped. Two sets of joints are prominent, one trending northwest and the other northeast. The joint systems control the drainage pattern in the south-central part of the area. </p><p>More than 20,000 feet of sedimentary rocks underlies the area. Many of the formations yield oil or gas in northwestern Colorado, northeastern Utah, and southwestern Wyoming. The Piceance Creek gas field, in which gas occurs in the Douglas Creek member of the Green River formation, is the largest oil or gas field discovered thus far within the area. </p><p>About 7,000 million barrels of oil is contained in oil shale that yields an average of 45 gallons per ton from a continuous sequence 5 or more feet thick in the Mahogany zone. Oil shale in the Mahogany zone and adjacent beds that yields an average of 30 gallons of oil per ton from a continuous sequence 15 or more feet thick contains about 91,000 million barrels of oil. Similar shale in deeper zones in the northern part of the area, for which detailed estimates have not been prepared, are now known to contain at least an additional 72,000 million barrels of oil. Oil shale in a sequence 15 or more feet thick that yields an average of 25 gallons of oil per ton contains about 154,000 million barrels of oil in the Mahogany zone and adjacent beds; such shale in deeper zones in the northern part of the area probably contains at least an additional 157,000 million barrels of oil, although detailed estimates were not made. Oil shale in a sequence greater than 15 feet thick that yields an average of 15 gallons of oil per ton contains more than 900,000 million barrels of oil. These estimates of the oil content of the deposit do not take into account any loss in mining or processing of the shale.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1958","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1082L","usgsCitation":"Donnell, J., 1961, Tertiary geology and oil-shale resources of the Piceance Creek basin between the Colorado and White Rivers, northwestern Colorado: U.S. Geological Survey Bulletin 1082, Report: v, 56 p.; 7 Plates: 33.54 x 39.62 inches or smaller, https://doi.org/10.3133/b1082L.","productDescription":"Report: v, 56 p.; 7 Plates: 33.54 x 39.62 inches or smaller","startPage":"835","endPage":"891","costCenters":[],"links":[{"id":100042,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1082l/report.pdf","text":"Report","size":"5.76 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,{"id":47154,"text":"ofr61124 - 1961 - Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil","interactions":[{"subject":{"id":47154,"text":"ofr61124 - 1961 - Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil","indexId":"ofr61124","publicationYear":"1961","noYear":false,"title":"Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil"},"predicate":"SUPERSEDED_BY","object":{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","indexId":"pp341E","publicationYear":"1966","noYear":false,"chapter":"E","title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil"},"id":1}],"supersededBy":{"id":39027,"text":"pp341E - 1966 - Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil","indexId":"pp341E","publicationYear":"1966","noYear":false,"title":"Geology and mineral resources of the Monlevade and Rio Piracicaba quadrangles, Minas Gerais, Brazil"},"lastModifiedDate":"2019-06-21T15:17:34","indexId":"ofr61124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"61-124","title":"Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr61124","usgsCitation":"Reeves, R.G., 1961, Geologic map and sections of the Andrade mine, Monlevade quadrangle, Minas Gerais, Brazil: U.S. Geological Survey Open-File Report 61-124, 1 Plate: 23.38 x 35.40 inches, https://doi.org/10.3133/ofr61124.","productDescription":"1 Plate: 23.38 x 35.40 inches","costCenters":[],"links":[{"id":134526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1961/0124/report-thumb.jpg"},{"id":364918,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1961/0124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"Brazil","state":"Minas Gerais","otherGeospatial":"Andrade mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -43.205623626708984,\n              -19.796102330463036\n            ],\n            [\n              -43.175411224365234,\n              -19.796102330463036\n            ],\n            [\n              -43.175411224365234,\n              -19.779626760060168\n            ],\n            [\n              -43.205623626708984,\n              -19.779626760060168\n            ],\n            [\n              -43.205623626708984,\n              -19.796102330463036\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4847","contributors":{"authors":[{"text":"Reeves, Robert G.","contributorId":72770,"corporation":false,"usgs":true,"family":"Reeves","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":234722,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39059,"text":"pp335 - 1961 - Characteristic Lower Cretaceous megafossils from northern Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:59","indexId":"pp335","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"335","title":"Characteristic Lower Cretaceous megafossils from northern Alaska","language":"ENGLISH","doi":"10.3133/pp335","usgsCitation":"Imlay, R.W., 1961, Characteristic Lower Cretaceous megafossils from northern Alaska: U.S. Geological Survey Professional Paper 335, 74 p., https://doi.org/10.3133/pp335.","productDescription":"74 p.","costCenters":[],"links":[{"id":119938,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0335/report-thumb.jpg"},{"id":66289,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0335/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66290,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0335/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66291,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0335/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66292,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0335/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66293,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e3e4b07f02db5e542e","contributors":{"authors":[{"text":"Imlay, R. W.","contributorId":23118,"corporation":false,"usgs":true,"family":"Imlay","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220877,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47382,"text":"b1082H - 1961 - Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah","interactions":[{"subject":{"id":47382,"text":"b1082H - 1961 - Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah","indexId":"b1082H","publicationYear":"1961","noYear":false,"chapter":"H","title":"Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah"},"predicate":"IS_PART_OF","object":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"id":1}],"isPartOf":{"id":33208,"text":"b1082 - 1962 - Contributions to economic geology, 1958","indexId":"b1082","publicationYear":"1962","noYear":false,"title":"Contributions to economic geology, 1958"},"lastModifiedDate":"2017-10-18T15:15:22","indexId":"b1082H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1082","chapter":"H","title":"Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah","docAbstract":"<p>The Drum Mountains are in west-central Utah 30 miles northwest of Delta, between the Sevier Desert on the east and Whirlwind Valley on the west. It is a typically barren desert range comprising a westward-tilted structural unit in which is exposed as much as 9,000 feet of quartzite (Cambrian and Precambrian?) and 3,000 feet of carbonate rocks of Cambrian age. These beds, which strike northward and dip west, are cut by myriad east- to northeast-trending faults with displacements of a few feet to a few thousand feet. Quartz monzonite dikes, pebble dikes, and vein deposits are present locally along the faults. The Cambrian rocks are overlain unconformably by volcanic rocks of probable Tertiary age. </p><p>Bodies of manganese carbonate ore were formed by replacement of two 20-foot beds of impure dolomite at the base of the sequence of carbonate rocks, along their intersection with certain preore faults. The feeding fissures locally contain veins in which rhodochrosite is associated with base metal sulfides. Downward- moving meteoric water has oxidized the ore bodies to a depth of 100 to 200 feet except where they are sealed off by structural or stratigraphic traps.<br></p><p>From 1925 to 1953, 72,462 long tons of manganese ore with an average grade of about 25 percent Mn were shipped.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology, 1958","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/b1082H","usgsCitation":"Crittenden, M.D., Straczek, J.A., and Roberts, R.J., 1961, Manganese deposits in the Drum Mountains, Juab and Millard Counties, Utah: U.S. Geological Survey Bulletin 1082, Report: iv, 51 p.; 5 Plates: 21.87 x 22.85 inches or smaller, https://doi.org/10.3133/b1082H.","productDescription":"Report: iv, 51 p.; 5 Plates: 21.87 x 22.85 inches or smaller","startPage":"493","endPage":"544","costCenters":[],"links":[{"id":100019,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1082h/plate-24.pdf","text":"Plate 24","size":"753 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 24"},{"id":100018,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1082h/plate-23.pdf","text":"Plate 23","size":"832 kB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 23"},{"id":172970,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1082h/report-thumb.jpg"},{"id":109306,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20749.htm","linkFileType":{"id":5,"text":"html"},"description":"20749"},{"id":100014,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1082h/report.pdf","text":"Report","size":"4.26 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":100015,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1082h/plate-20.pdf","text":"Plate 20","size":"2.77 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 20"},{"id":100016,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1082h/plate-21.pdf","text":"Plate 21","size":"3.8 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 21"},{"id":100017,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1082h/plate-22.pdf","text":"Plate 22","size":"1.25 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 22"}],"country":"United States","state":"Utah","county":"Juab County, Millard County","otherGeospatial":"Drum Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -113.3184814453125,\n              39.45316112807394\n            ],\n            [\n              -112.6812744140625,\n              39.45316112807394\n            ],\n            [\n              -112.6812744140625,\n              39.829631721333726\n            ],\n            [\n              -113.3184814453125,\n              39.829631721333726\n            ],\n            [\n              -113.3184814453125,\n              39.45316112807394\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64aca4","contributors":{"authors":[{"text":"Crittenden, Max D. Jr.","contributorId":28951,"corporation":false,"usgs":true,"family":"Crittenden","given":"Max","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":235192,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Straczek, John A.","contributorId":87194,"corporation":false,"usgs":true,"family":"Straczek","given":"John","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":235191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Roberts, Ralph Jackson","contributorId":63010,"corporation":false,"usgs":true,"family":"Roberts","given":"Ralph","email":"","middleInitial":"Jackson","affiliations":[],"preferred":false,"id":235193,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":968,"text":"wsp1535D - 1961 - Calcium carbonate saturation in ground water, from routine analyses","interactions":[],"lastModifiedDate":"2013-01-08T13:01:31","indexId":"wsp1535D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1535","chapter":"D","title":"Calcium carbonate saturation in ground water, from routine analyses","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1535D","usgsCitation":"Back, W., 1961, Calcium carbonate saturation in ground water, from routine analyses: U.S. Geological Survey Water Supply Paper 1535, iii, 14 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1535D.","productDescription":"iii, 14 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":137552,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1535d/report-thumb.jpg"},{"id":25505,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1535d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":265372,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1535d/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f9759","contributors":{"authors":[{"text":"Back, William","contributorId":59007,"corporation":false,"usgs":true,"family":"Back","given":"William","email":"","affiliations":[],"preferred":false,"id":142940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":723,"text":"wsp1714 - 1961 - Surface water supply of the United States, 1960, Part 10, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1714","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1714","title":"Surface water supply of the United States, 1960, Part 10, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1714","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 10, The Great Basin: U.S. Geological Survey Water Supply Paper 1714, viii, 270 p. :tables ;23 cm., https://doi.org/10.3133/wsp1714.","productDescription":"viii, 270 p. :tables ;23 cm.","costCenters":[],"links":[{"id":136291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1714/report-thumb.jpg"},{"id":25286,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1714/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db6942d6","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142651,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":722,"text":"wsp1701 - 1961 - Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1701","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"1701","title":"Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut","language":"ENGLISH","publisher":"U.S. Govt. Printing Office,","doi":"10.3133/wsp1701","usgsCitation":"Hendricks, E.L., 1961, Surface water supply of the United States, 1960, Part 1-A, North Atlantic Slope basins, Maine to Connecticut: U.S. Geological Survey Water Supply Paper 1701, v., 286 p. ;23 cm., https://doi.org/10.3133/wsp1701.","productDescription":"v., 286 p. ;23 cm.","costCenters":[],"links":[{"id":136290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1701/report-thumb.jpg"},{"id":25285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1701/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db69436e","contributors":{"authors":[{"text":"Hendricks, E. L.","contributorId":50126,"corporation":false,"usgs":true,"family":"Hendricks","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":142650,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68325,"text":"ha42 - 1961 - Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","interactions":[],"lastModifiedDate":"2022-06-03T20:40:02.242302","indexId":"ha42","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1961","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":"42","title":"Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha42","usgsCitation":"Herrick, E.H., 1961, Geologic map of White Sands Missile Range headquarters area, Dona Ana County, New Mexico, showing location of wells, contours on the water table, and location of proposed dams, reservoirs and recharge-discharge wells: U.S. Geological Survey Hydrologic Atlas 42, 1 Plate: 27.50 × 21.00 inches, https://doi.org/10.3133/ha42.","productDescription":"1 Plate: 27.50 × 21.00 inches","costCenters":[],"links":[{"id":185963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":401720,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15804.htm"},{"id":89786,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/042/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"680","country":"United States","state":"New Mexico","county":"Dona Ana County","otherGeospatial":"White Sands Missile Range headquarters area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -106.622314453125,\n              32.287132632616384\n            ],\n            [\n              -106.383,\n              32.287132632616384\n            ],\n            [\n              -106.383,\n              32.465743313283596\n            ],\n            [\n              -106.622314453125,\n              32.465743313283596\n            ],\n            [\n              -106.622314453125,\n              32.287132632616384\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a2aef","contributors":{"authors":[{"text":"Herrick, Eugene H.","contributorId":80360,"corporation":false,"usgs":true,"family":"Herrick","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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