{"pageNumber":"6762","pageRowStart":"169025","pageSize":"25","recordCount":184880,"records":[{"id":39045,"text":"pp323 - 1962 - Stratigraphy and paleontology of the uppermost Pennsylvanian and lowermost Permian Rocks in Kansas","interactions":[],"lastModifiedDate":"2021-09-13T18:41:02.826629","indexId":"pp323","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"323","title":"Stratigraphy and paleontology of the uppermost Pennsylvanian and lowermost Permian Rocks in Kansas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp323","usgsCitation":"Mudge, M.R., Yochelson, E.L., Douglass, R.C., Duncan, H., Strimple, H.L., Gordon, M., and Dunkle, D.H., 1962, Stratigraphy and paleontology of the uppermost Pennsylvanian and lowermost Permian Rocks in Kansas: U.S. Geological Survey Professional Paper 323, Report: v, 213 p.; 7 Plates: 26.00 × 47.00 inches or smaller, https://doi.org/10.3133/pp323.","productDescription":"Report: v, 213 p.; 7 Plates: 26.00 × 47.00 inches or smaller","costCenters":[],"links":[{"id":66257,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66256,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66255,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66254,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66253,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66252,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119930,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0323/report-thumb.jpg"},{"id":389165,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4321.htm"},{"id":66259,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0323/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66258,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0323/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -96.8333,\n              37.0\n            ],\n            [\n              -95.3667,\n              37.0\n            ],\n            [\n              -95.3667,\n              40\n            ],\n            [\n              -96.8333,\n              40\n            ],\n            [\n              -96.8333,\n              37.0\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8b2d","contributors":{"authors":[{"text":"Mudge, M. R.","contributorId":51805,"corporation":false,"usgs":true,"family":"Mudge","given":"M.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220854,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yochelson, E. L.","contributorId":50948,"corporation":false,"usgs":true,"family":"Yochelson","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220853,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Douglass, R. C.","contributorId":43827,"corporation":false,"usgs":true,"family":"Douglass","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":220851,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Duncan, Helen","contributorId":70822,"corporation":false,"usgs":true,"family":"Duncan","given":"Helen","email":"","affiliations":[],"preferred":false,"id":220855,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Strimple, H. L.","contributorId":17484,"corporation":false,"usgs":true,"family":"Strimple","given":"H.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":220850,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":220849,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Dunkle, D. H.","contributorId":48442,"corporation":false,"usgs":true,"family":"Dunkle","given":"D.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":220852,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"id":39062,"text":"pp341A - 1962 - Geology and ore deposits of the Nova Lima and Rio Acima quadrangles, Minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2012-02-02T00:09:59","indexId":"pp341A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"341","chapter":"A","title":"Geology and ore deposits of the Nova Lima and Rio Acima quadrangles, Minas Gerais, Brazil","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and mineral resources of parts of Minas Gerais, Brazil","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp341A","usgsCitation":"Gair, J., 1962, Geology and ore deposits of the Nova Lima and Rio Acima quadrangles, Minas Gerais, Brazil: U.S. Geological Survey Professional Paper 341, p. A1-A67, https://doi.org/10.3133/pp341A.","productDescription":"p. A1-A67","costCenters":[],"links":[{"id":119941,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0341a/report-thumb.jpg"},{"id":66314,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66315,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66316,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66317,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66318,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66319,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66320,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66321,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66322,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0341a/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66323,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0341a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db6843d7","contributors":{"authors":[{"text":"Gair, J. E.","contributorId":50891,"corporation":false,"usgs":true,"family":"Gair","given":"J. E.","affiliations":[],"preferred":false,"id":220881,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":33809,"text":"b1122A - 1962 - Geology of the Spruce Pine district, Avery, Mitchell, and Yancey Counties, North Carolina","interactions":[{"subject":{"id":14551,"text":"ofr53143 - 1953 - Geologic map of the Spruce Pine district, North Carolina","indexId":"ofr53143","publicationYear":"1953","noYear":false,"title":"Geologic map of the Spruce Pine district, North Carolina"},"predicate":"SUPERSEDED_BY","object":{"id":33809,"text":"b1122A - 1962 - Geology of the Spruce Pine district, Avery, Mitchell, and Yancey Counties, North Carolina","indexId":"b1122A","publicationYear":"1962","noYear":false,"chapter":"A","title":"Geology of the Spruce Pine district, Avery, Mitchell, and Yancey Counties, North Carolina"},"id":1}],"lastModifiedDate":"2021-10-21T11:52:04.898019","indexId":"b1122A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1122","chapter":"A","title":"Geology of the Spruce Pine district, Avery, Mitchell, and Yancey Counties, North Carolina","docAbstract":"The Spruce Pine pegmatite district, a northeastward-trending belt 25 miles \r\nlong and 10 miles wide, lies in parts of Avery, Mitchell, and Yancey Counties in the Blue Ridge Province of western North Carolina. The most abundant \r\nrocks in the district are interlayered mica and amphibole gneisses and schists, all of which are believed to be of Precambrian age. These rocks are cut by small bodies of dunite and associated rocks of Precambrian (?) age, large bodies of alaskite and associated pegmatite of early Paleozoic age, and basaltic and diabasic dikes and sills of Triassic (?) age. The rocks of the district have been weathered to saprolite that is locally 50 feet thick.\r\n\r\nThe major structure in the area is a southwestward-plunging asymmetrical \r\nsynclinorium that has its steeper limb on the northwest side.\r\n\r\nFeldspar, muscovite as sheet and scrap (ground) mica, and kaolin from the \r\nalaskite and associated pegmatite account for over 90 percent of the total \r\nmineral production of the district. Amounts of other pegmatite minerals, \r\nincluding quartz, beryl, columbite-tantalite, rare-earth and uranium minerals \r\nare an extremely small part of the mineral resources. Actual or potential \r\nproducts from other rocks are olivine, vermiculite, asbestos, talc, chromium and nickel, soapstone, mica schist, garnet, kyanite, dolomite marble, and construction materials.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to Economic Geology (1960)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1122A","isbn":"0607643226","usgsCitation":"Brobst, D.A., 1962, Geology of the Spruce Pine district, Avery, Mitchell, and Yancey Counties, North Carolina: U.S. Geological Survey Bulletin 1122, Report: iv, 26 p.; 2 Plates 52 x 30 inches and 52 x 27 inches, https://doi.org/10.3133/b1122A.","productDescription":"Report: iv, 26 p.; 2 Plates 52 x 30 inches and 52 x 27 inches","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":61716,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61715,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122a/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":61714,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165925,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122a/report-thumb.jpg"},{"id":109360,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20822.htm","linkFileType":{"id":5,"text":"html"},"description":"20822"}],"scale":"24000","country":"United States","state":"North Carolina","county":"Avery County, Mitchell County, Yancey County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.292,35.822 ], [ -82.292,36.078 ], [ -81.938,36.078 ], [ -81.938,35.822 ], [ -82.292,35.822 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e47e","contributors":{"authors":[{"text":"Brobst, Donald Albert","contributorId":36117,"corporation":false,"usgs":true,"family":"Brobst","given":"Donald","email":"","middleInitial":"Albert","affiliations":[],"preferred":false,"id":211971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2392,"text":"wsp1604 - 1962 - Geology and ground-water resources of Fond du Lac County, Wisconsin","interactions":[{"subject":{"id":57717,"text":"ofr5989 - 1959 - Geology and ground-water resources of Fond De Lac County, Wisconsin","indexId":"ofr5989","publicationYear":"1959","noYear":false,"title":"Geology and ground-water resources of Fond De Lac County, Wisconsin"},"predicate":"SUPERSEDED_BY","object":{"id":2392,"text":"wsp1604 - 1962 - Geology and ground-water resources of Fond du Lac County, Wisconsin","indexId":"wsp1604","publicationYear":"1962","noYear":false,"title":"Geology and ground-water resources of Fond du Lac County, Wisconsin"},"id":1}],"lastModifiedDate":"2015-10-02T15:01:34","indexId":"wsp1604","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1604","title":"Geology and ground-water resources of Fond du Lac County, Wisconsin","docAbstract":"<p>The principal water-bearing rocks underlying Fond du Lac County, Wis., are sandstones of Cambrian and Ordovician age and dolomite of Silurian age. Other aquifers include dolomite of Ordovician age and sand. and gravel of Quaternary age. Crystalline rocks of Precambrian age, which underlie all the water-bearing formations, form a practically impermeable basement complex and yield little or no water to wells. Ground water is the source of all public and most private and industrial water supplies in the county. The municipalities and industries obtain water chiefly from wells that penetrate the sandstones of Cambrian and Ordorician age. The Platteville formation and Galena dolomite of Ordovician age and the Niagara dolomite of Silurian age supply water to most domestic and stock wells and to a few industrial wells. Several buried valleys in the bedrock surface contain water-bearing deposits of sand and gravel. The source of the ground water in Fond du Lac County is local precipitation. Recharge to the water-bearing beds occurs in most of the county but is greatest where the bedrock formations are near the surface. Ground water is discharged by seeps and springs, by evaporation and transpiration, and by wells. Ground-water levels in wells fluctuate in response to recharge and to natural discharge and pumping. In areas not affected by pumping, water levels generally decline through the summer months because of natural discharge and lack of recharge, recover slightly in the fall after the first killing frost, decline during the winter, and recover in the spring when recharge is greatest. In areas of heavy pumping, the water levels are lowest in late summer and highest in late winter. Water levels in wells in the Fond du Lac area were about 5 to 50 feet above the land surface in 1885, but they had declined to as low as 185 feet below the land surface by 1957. Coefficients of transmissibility and storage of the sandstones of Cambrian and Ordovician age were determined by making controlled aquifer tests at Fond du Lac. The coefficients were verified by comparing computed water-level declines with actual declines. The computed values were within about 30 percent of the actual values, a reasonable agreement for coefficients of this type. Probable declines of water levels by 1966 were computed, using the same coefficients of transmissibility and storage. If the distribution of wells and the rate of pumping remain the same in 1957-66 as they were in 1956, the water levels will decline about 5 feet more by 1966. If, however, the distribution of pumped wells remains the same but the pumping by the city of Fond du Lac increases at a uniform rate from the 3 mgd (million gallons per day) pumped in 1956 to 5 mgd in 1966, the water levels in 1966 will be at least 60 feet below those of 1956. Dispersal of wells to the northwest toward the recharge area would reduce the water-level declines. The results of pumping tests, of test holes tapping the Niagara dolomite indicate that wells producing at least 200 gpm (gallons per minute) could be developed east of the Niagara escarpment. 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]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698992","contributors":{"authors":[{"text":"Pierce, William Gamewell","contributorId":105361,"corporation":false,"usgs":true,"family":"Pierce","given":"William","email":"","middleInitial":"Gamewell","affiliations":[],"preferred":false,"id":214714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rich, Ernest Isaac","contributorId":31451,"corporation":false,"usgs":true,"family":"Rich","given":"Ernest","email":"","middleInitial":"Isaac","affiliations":[],"preferred":false,"id":214713,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":68233,"text":"ha58 - 1962 - Emergency water supplies in the Wichita area, Kansas","interactions":[],"lastModifiedDate":"2012-10-30T16:17:44","indexId":"ha58","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"58","title":"Emergency water supplies in the Wichita area, Kansas","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha58","usgsCitation":"Lane, C.W., Reavis, E., and Stramel, G.J., 1962, Emergency water supplies in the Wichita area, Kansas: U.S. Geological Survey Hydrologic Atlas 58, 36 p.; 2 col. maps on one sheet: 32 x 42 inches, https://doi.org/10.3133/ha58.","productDescription":"36 p.; 2 col. maps on one sheet: 32 x 42 inches","costCenters":[],"links":[{"id":262850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/058/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":190296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/058/report-thumb.jpg"},{"id":89610,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -98,37 ], [ -98,38.25 ], [ -96.5,38.25 ], [ -96.5,37 ], [ -98,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66dd7b","contributors":{"authors":[{"text":"Lane, Charles W.","contributorId":103526,"corporation":false,"usgs":true,"family":"Lane","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reavis, E.L.","contributorId":70246,"corporation":false,"usgs":true,"family":"Reavis","given":"E.L.","email":"","affiliations":[],"preferred":false,"id":277885,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stramel, Gilbert J.","contributorId":95327,"corporation":false,"usgs":true,"family":"Stramel","given":"Gilbert","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":277886,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":33750,"text":"b1140B - 1962 - Use of cesium-137 in the determination of cation exchange capacity","interactions":[],"lastModifiedDate":"2012-02-02T00:09:24","indexId":"b1140B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1140","chapter":"B","title":"Use of cesium-137 in the determination of cation exchange capacity","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1140B","usgsCitation":"Beetem, W., Janzer, V.J., and Wahlberg, J., 1962, Use of cesium-137 in the determination of cation exchange capacity: U.S. Geological Survey Bulletin 1140, p. B1-B8 ;24 cm., https://doi.org/10.3133/b1140B.","productDescription":"p. B1-B8 ;24 cm.","costCenters":[],"links":[{"id":163952,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1140b/report-thumb.jpg"},{"id":61623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1140b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6047c6","contributors":{"authors":[{"text":"Beetem, W.A.","contributorId":19173,"corporation":false,"usgs":true,"family":"Beetem","given":"W.A.","email":"","affiliations":[],"preferred":false,"id":211874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Janzer, Victor J.","contributorId":36119,"corporation":false,"usgs":true,"family":"Janzer","given":"Victor","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":211875,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wahlberg, J.S.","contributorId":59850,"corporation":false,"usgs":true,"family":"Wahlberg","given":"J.S.","affiliations":[],"preferred":false,"id":211876,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":35472,"text":"b1122F - 1962 - Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","interactions":[],"lastModifiedDate":"2021-12-23T19:56:45.980641","indexId":"b1122F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"1122","chapter":"F","title":"Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources","docAbstract":"The Haldeman and Wrigley 7th-minute quadrangles are near the western edge of the eastern Kentucky coal field and cover an area of approximately 117 square miles in parts of Carter, Rowan, Elliott, and Morgan Counties, Ky. The rocks exposed in the two quadrangles are of Early and Late Mississippian and Early and Middle Pennsylvanian age. The Mississippian rocks are composed of the thick Brodhead formation, which consists of siltstone and shale, and eleven thin marine limestone and shale formations, having an aggregate thickness of about 150 feet. The Lee and Breathitt formations, of Pennsylvanian age, consist of sandstone, siltstone, and shale; they also contain thin beds of coal and several beds of underclay, including the economically important Olive Hill clay bed of Crider, 1913. Pennsylvanian rocks include beds of both continental and marine origin. The eleven thin Mississippian formations and the upper-most part of the thick Brodhead formation are truncated by a prominent unconformity on which rocks of Pennsylvanian age rest. The rocks occupy a region of gentle dips between the Cincinnati arch and the Appalachian Mountains.\r\n\r\nRefractory clay deposits are in the Olive Hill clay bed, which occurs in the \r\nlower part of the Lee formation. The Olive Hill clay bed is discontinuous and \r\nconsists of a series of irregularly shaped lenses. The bed is approximately \r\ntwo-thirds semifiint clay and one-third flint clay, and it contains minor amounts of plastic clay. Some of the flint clay is nearly pure kaolinite, but the semi flint and plastic clay consists of mixtures of kaolinite, illite, and mixed-layer clay minerals. The structure of the kaolinite ranges from highly crystalline to very poorly crystalline 'fireclay' type. The degree of crystallinity of the kaolinite and the hardness of the clay vary inversely with the amount of illite and mixed-layer clay minerals present. The nearly pure kaolinite is believed to have formed by the removal of alkalies and some silica fram mixtures of kaolinite, illite, and mixed-layer clays by leaching in swamps to the deposition of the beds overlying the clay. The refractory properties of the clay vary directly with the purity of the kaolinite, and refractoriness decreases as the proportions of illite and mixed-layer clays increase. Certain nonclay minerals, chiefly siderite, pyrite, and iron oxide-bearing minerals, also act as fiuxes, reducing the refractory properties of the clay. The entire resources of clay in the Olive Hill clay bed are roughly and tentatively estimated to include 105,000,000 tons in the Haldeman quadrangle and 175,000,000 tons in the Wrigley quadrangle. Much of this clay is of poor quality and the amount that is better than the minimum requirements for use in refractories is probably about 30,000,000 tons. Only a fraction of this tonnage is suitable for superheat-duty products.\r\n\r\nLimestone is the only nonmetallic mineral resource other than refractory clay \r\nthat has been developed in the two quadrangles, but 1arge amounts of shale \r\nsuitable for use in making lightweight aggregate and structural clay products \r\nmay also be present. Most of the limestone, which is quarried. in both quadrangles, is used for road-metal, concrete aggregate, and agriculture stone, but some of the limestone is of the quality that would be suitable for other uses. Virtually all the Mississippian Beech Creek limestone of Malott, 1919 which is as much as 18 feet thick, consists of high-calcium limestone. Shale beds that appear most favoralble for making lightweight aggregate are in the shale facies of the Lee formation of Pennsylvanian age. Shale that is probably suitable for structural clay products is present in the shale flacles of the Lee formation and in the Muldraugh formation of Mississippian age.\r\n\r\nSeveral dry holes have been drilled in search for oil and gas within the area \r\nof the two quadrangles. Though no commercial production was ever attained, one well furnished a supply of gas f","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to economic geology (1960)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1122F","usgsCitation":"Patterson, S.H., Hosterman, J.W., and Huddle, J.W., 1962, Geology and refractory clay deposits of the Haldeman and Wrigley quadrangles, Kentucky, with a section on coal resources: U.S. Geological Survey Bulletin 1122, Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller, https://doi.org/10.3133/b1122F.","productDescription":"Report: vi, 113 p.; 8 Plates: 28 x 18 inches or smaller","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":109365,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_20827.htm","linkFileType":{"id":5,"text":"html"},"description":"20827"},{"id":63375,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63374,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63373,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63372,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63371,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63376,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1122f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63370,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63369,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63368,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1122f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1122f/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"Kentucky","otherGeospatial":"Haldeman and Wrigley quadrangles","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.375,\n              38.25\n            ],\n            [\n              -83.25,\n              38.25\n            ],\n            [\n              -83.25,\n              38.0\n            ],\n            [\n              -83.375,\n              38.0\n            ],\n            [\n              -83.375,\n              38.25\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6863e2","contributors":{"authors":[{"text":"Patterson, Sam H.","contributorId":62996,"corporation":false,"usgs":true,"family":"Patterson","given":"Sam","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214698,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hosterman, John W.","contributorId":48962,"corporation":false,"usgs":true,"family":"Hosterman","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":214697,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Huddle, John Warfield","contributorId":23932,"corporation":false,"usgs":true,"family":"Huddle","given":"John","email":"","middleInitial":"Warfield","affiliations":[],"preferred":false,"id":214696,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":15931,"text":"ofr62124 - 1962 - Influences of the soil on boreal and arctic plant communities","interactions":[],"lastModifiedDate":"2025-06-03T16:40:34.974652","indexId":"ofr62124","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-124","title":"Influences of the soil on boreal and arctic plant communities","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr62124","usgsCitation":"Shacklette, H.T., 1962, Influences of the soil on boreal and arctic plant communities: U.S. Geological Survey Open-File Report 62-124, x, 349 p., https://doi.org/10.3133/ofr62124.","productDescription":"x, 349 p.","costCenters":[],"links":[{"id":489483,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0124/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149048,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0124/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f1e4b07f02db5ee54c","contributors":{"authors":[{"text":"Shacklette, Hansford Threlkeld","contributorId":94660,"corporation":false,"usgs":true,"family":"Shacklette","given":"Hansford","email":"","middleInitial":"Threlkeld","affiliations":[],"preferred":false,"id":171967,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":15727,"text":"ofr62113 - 1962 - The crystallography, crystal structure, and crystal chemistry of various minerals and compounds belonging to the torbernite mineral group","interactions":[],"lastModifiedDate":"2025-06-03T18:23:00.909354","indexId":"ofr62113","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-113","title":"The crystallography, crystal structure, and crystal chemistry of various minerals and compounds belonging to the torbernite mineral group","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr62113","usgsCitation":"Ross, M., 1962, The crystallography, crystal structure, and crystal chemistry of various minerals and compounds belonging to the torbernite mineral group: U.S. Geological Survey Open-File Report 62-113, viii, 179 p., https://doi.org/10.3133/ofr62113.","productDescription":"viii, 179 p.","costCenters":[],"links":[{"id":489489,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0113/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":146460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0113/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db668882","contributors":{"authors":[{"text":"Ross, Malcolm","contributorId":100372,"corporation":false,"usgs":true,"family":"Ross","given":"Malcolm","email":"","affiliations":[],"preferred":false,"id":171605,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60556,"text":"mf253 - 1962 - Preliminary geologic map of the western part of the Superior quadrangle, Pinal County, Arizona","interactions":[],"lastModifiedDate":"2018-12-17T14:17:31","indexId":"mf253","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"253","title":"Preliminary geologic map of the western part of the Superior quadrangle, Pinal County, Arizona","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf253","usgsCitation":"Peterson, D.W., 1962, Preliminary geologic map of the western part of the Superior quadrangle, Pinal County, Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 253, 41.13 x 49.73 inches, https://doi.org/10.3133/mf253.","productDescription":"41.13 x 49.73 inches","costCenters":[],"links":[{"id":182601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/0253/report-thumb.jpg"},{"id":360382,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/0253/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Arizona","county":"Pinal County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.11749999999999,33.25 ], [ -111.11749999999999,33.3675 ], [ -111.03416666666666,33.3675 ], [ -111.03416666666666,33.25 ], [ -111.11749999999999,33.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db6740c7","contributors":{"authors":[{"text":"Peterson, Donald W.","contributorId":11209,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":263976,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37114,"text":"rr61 - 1962 - Bioassay and use of pituitary materials to spawn warm-water fishes","interactions":[],"lastModifiedDate":"2012-02-02T00:09:52","indexId":"rr61","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"61","title":"Bioassay and use of pituitary materials to spawn warm-water fishes","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Clemens, H., and Sneed, K., 1962, Bioassay and use of pituitary materials to spawn warm-water fishes: Research Report 61, 30 p.","productDescription":"30 p.","costCenters":[],"links":[{"id":164983,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db625e30","contributors":{"authors":[{"text":"Clemens, H.P.","contributorId":39837,"corporation":false,"usgs":true,"family":"Clemens","given":"H.P.","email":"","affiliations":[],"preferred":false,"id":217504,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sneed, K.E.","contributorId":44858,"corporation":false,"usgs":true,"family":"Sneed","given":"K.E.","email":"","affiliations":[],"preferred":false,"id":217505,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":22804,"text":"ofr6234 - 1962 - Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","interactions":[],"lastModifiedDate":"2013-11-22T15:37:23","indexId":"ofr6234","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"62-34","title":"Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho","docAbstract":"This reports evaluates the ground-water resources of about 1,000 square miles in the semiarid uplands south of the Snake River between Bruneau River and Salmon Falls Creek. The outcropping rocks are the Idavada Volcanics of Pliocene age, and the Idaho Group of Pliocene and Plieistocene age, consisting of the Banbury Basalt of middle Pliocene age and overlying predominantly sedimentary deposits of middle Pliocene through middle Pleistocene age. These rocks dip gently northward. The volcanic rocks are the best aquifers, but the yield of water from the sedimentary deposits is adequate for domestic and stock use. About 6,000 acre-feet of water is withdrawn annually from the Idavada Volcanics by 9 irrigation wells to irrigate about 3,000 acres. Only a few tends of acre-feet of water withdrawn from the other formations. The regional dip of the rocks induces weak artesian conditions in the volcanic rocks and somewhat higher artesian head in the sedimentary rocks. Estimated depth to water ranges from less than 250 feet to more than 750 feet, as shown in an accompanying map. The eastern part of the area appears to be more favorable for the development of ground water for irrigation than the western part because of better aquifers at shallower depth.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr6234","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Crosthwaite, E., 1962, Ground-water reconnaissance of the Sailor Creek area, Owyhee, Elmore, and Twin Falls Counties, Idaho: U.S. Geological Survey Open-File Report 62-34, Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller, https://doi.org/10.3133/ofr6234.","productDescription":"Report: ii, 53 p.; 3 Plates: 32.94 x 21.57 inches and smaller","numberOfPages":"56","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":155706,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1962/0034/report-thumb.jpg"},{"id":52232,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52233,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52234,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1962/0034/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":52235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1962/0034/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Idaho","county":"Elmore County;Owyhee County;Twin Falls County","otherGeospatial":"Sailor Creek Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4626,42.0584 ], [ -116.4626,44.1361 ], [ -112.07,44.1361 ], [ -112.07,42.0584 ], [ -116.4626,42.0584 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a81e4b07f02db64a0c5","contributors":{"authors":[{"text":"Crosthwaite, E. G.","contributorId":83098,"corporation":false,"usgs":true,"family":"Crosthwaite","given":"E. G.","affiliations":[],"preferred":false,"id":188903,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37113,"text":"rr60 - 1962 - Limnological organic analyses by quantitative dichromate oxidation","interactions":[],"lastModifiedDate":"2012-02-02T00:09:52","indexId":"rr60","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":74,"text":"Research Report","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"60","title":"Limnological organic analyses by quantitative dichromate oxidation","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Maciolek, J.A., 1962, Limnological organic analyses by quantitative dichromate oxidation: Research Report 60, 61 p.","productDescription":"61 p.","costCenters":[],"links":[{"id":164896,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a51cf","contributors":{"authors":[{"text":"Maciolek, J. A.","contributorId":62655,"corporation":false,"usgs":true,"family":"Maciolek","given":"J.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":217503,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":59791,"text":"mf247 - 1962 - Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:10:13","indexId":"mf247","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"247","title":"Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska","language":"ENGLISH","doi":"10.3133/mf247","usgsCitation":"Hummel, C., 1962, Preliminary geologic map of the Nome C-1 quadrangle, Seward Peninsula, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 247, 1 map ;44 x 39 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf247.","productDescription":"1 map ;44 x 39 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":104026,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2663.htm","linkFileType":{"id":5,"text":"html"},"description":"2663"},{"id":184549,"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\": [ [ [ -165.5,64.5 ], [ -165.5,64.75 ], [ -165,64.75 ], [ -165,64.5 ], [ -165.5,64.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67af2d","contributors":{"authors":[{"text":"Hummel, C. H.","contributorId":29065,"corporation":false,"usgs":true,"family":"Hummel","given":"C. H.","affiliations":[],"preferred":false,"id":262599,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68696,"text":"ha47 - 1962 - Floods at Fremont, Ohio","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha47","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1962","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":"47","title":"Floods at Fremont, Ohio","language":"ENGLISH","doi":"10.3133/ha47","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1962, Floods at Fremont, Ohio: U.S. Geological Survey Hydrologic Atlas 47, 1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches)), https://doi.org/10.3133/ha47.","productDescription":"1 map :col. ;on sheet 72 x 84 in folder 30 x 24.  (Contour interval 5 feet.  30 by 31 inches))","costCenters":[],"links":[{"id":188097,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90418,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/047/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.18333333333334,41.25 ], [ -83.18333333333334,41.3675 ], [ -83.05,41.3675 ], [ -83.05,41.25 ], [ -83.18333333333334,41.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7280","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":534516,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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