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,{"id":70156944,"text":"70156944 - 1972 - Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, January 13-April 5 , 1972","interactions":[],"lastModifiedDate":"2019-11-12T18:27:50","indexId":"70156944","displayToPublicDate":"2015-09-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, January 13-April 5 , 1972","docAbstract":"<p>The U.S. Geological Survey collected 110 water samples from Amchitka Island, Alaska, between January 13 and April 5, 1972. Tritium determinations were made on all samples collected and gross alpha and gross beta/gamma determinations were made on 92 samples. The gross alpha and gross beta determinations when compared with previously determined ranges for fresh waters on Amchitka Island show no trends.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70156944","usgsCitation":"Schroder, L., and Ballance, W.C., 1972, Radiochemical monitoring of water after the Cannikin event, Amchitka Island, Alaska, January 13-April 5 , 1972, i, 17 p., https://doi.org/10.3133/70156944.","productDescription":"i, 17 p.","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","temporalStart":"1972-01-13","temporalEnd":"2015-04-05","costCenters":[],"links":[{"id":307858,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70156944.JPG"},{"id":308548,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70156944/report.pdf","text":"Report","size":"3,074 KB","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Amchitka Island, Aleutian Islands","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              178.584136963,\n              51.63677159243599\n            ],\n            [\n              178.592376709,\n              51.61290019118336\n            ],\n            [\n              179.21585083,\n              51.3254629443313\n            ],\n            [\n             179.508361816,\n              51.37520943448463\n            ],\n            [\n              179.057922363,\n              51.587309751245456\n            ],\n            [\n              178.628082275,\n              51.67936786087718\n            ],\n            [\n              178.584136963,\n              51.63677159243599\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"55f2a9c0e4b0dacf699ec6c4","contributors":{"authors":[{"text":"Schroder, L.J.","contributorId":31767,"corporation":false,"usgs":true,"family":"Schroder","given":"L.J.","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571213,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ballance, Wilbur C.","contributorId":50436,"corporation":false,"usgs":true,"family":"Ballance","given":"Wilbur","email":"","middleInitial":"C.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":571214,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70157473,"text":"70157473 - 1972 - Trends in ground-water levels in Wisconsin, 1967-1971","interactions":[],"lastModifiedDate":"2018-01-08T19:39:05","indexId":"70157473","displayToPublicDate":"2015-05-12T02:15:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"21","title":"Trends in ground-water levels in Wisconsin, 1967-1971","docAbstract":"<p>This report supplements the Wisconsin Geological and Natural History Survey, Information Circular No.9, \"Trends in Ground-Water Levels in Wisconsin through 1966\". It describes, by hydrographs, the ground-water level trends in Wisconsin for the period 1967-1971. All current observation wells with more than three years of record are included; records of observation wells discontinued since 1967 and records of wells with less than three years of record are not included. 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56051ee9e4b058f706e51324","contributors":{"authors":[{"text":"Erickson, Robert M.","contributorId":147925,"corporation":false,"usgs":true,"family":"Erickson","given":"Robert","email":"","middleInitial":"M.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":573261,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70157472,"text":"70157472 - 1972 - Ground-water quality in Wisconsin through 1972","interactions":[],"lastModifiedDate":"2018-01-08T19:39:49","indexId":"70157472","displayToPublicDate":"2015-02-09T08:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5596,"text":"Wisconsin Geological & Natural History Survey Information Circular","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"22","title":"Ground-water quality in Wisconsin through 1972","docAbstract":"<p>Ground water, a plentiful and largely underdeveloped resource of Wisconsin, has good to excellent chemical quality in most places. This resource is readily available in most parts of the State for municipal, industrial, and rural uses. In 1970, about 0.5 billion gallons of ground water a day was pumped in Wisconsin for all uses (Murray and Reeves, 1972). In addition, underground reservoirs discharge an average of 16 billion gallons per day of water of relatively constant temperature and uniform quality, which maintains the base flow of streams and the level of lakes (Holt, 1964).</p>","language":"English","publisher":"Wisconsin Geological & Natural History Survey","publisherLocation":"Madison, WI","usgsCitation":"Skinner, E., and Holt, C.L., 1972, Ground-water quality in Wisconsin through 1972: Wisconsin Geological & Natural History Survey Information Circular 22, 148 p.","productDescription":"148 p.","numberOfPages":"148","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":308484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":350397,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://wgnhs.uwex.edu/pubs/download_ic22/"}],"country":"United 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,{"id":70047462,"text":"70047462 - 1972 - Water resources of Lehigh County, Pennsylvania","interactions":[{"subject":{"id":56075,"text":"ofr70372 - 1970 - Water resources of Lehigh County, Pennsylvania","indexId":"ofr70372","publicationYear":"1970","noYear":false,"title":"Water resources of Lehigh County, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047462,"text":"70047462 - 1972 - Water resources of Lehigh County, Pennsylvania","indexId":"70047462","publicationYear":"1972","noYear":false,"title":"Water resources of Lehigh County, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T15:52:43","indexId":"70047462","displayToPublicDate":"2013-01-01T15:44:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"31","title":"Water resources of Lehigh County, Pennsylvania","docAbstract":"Lehigh County occupies an area of 347 square miles in southeastern Pennsylvania. The northern part of Lehigh County is underlain by the Martinsburg Formation, which consists chiefly of shale and slate. The central part of the county, where most of the population centers are located and much of the urbanization is occurring, is underlain by alternating beds of limestone and dolomite. From oldest to youngest, these carbonate rocks are the Leithsville Formation, the Allentown Formation, the Beekmantown Group, and the Jacksonburg Formation. The southern part of the county is underlain chiefly by the shales, sandstones, and conglomerates of the Brunswick Formation and by metamorphic and igneous rocks.","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the U. S. Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey and the Lehigh County Soil and Water Conservation District","usgsCitation":"Wood, C.R., Flippo, H.N., Lescinsky, J.B., and Barker, J.L., 1972, Water resources of Lehigh County, Pennsylvania: Water Resource Report 31, x, 263 p.","productDescription":"x, 263 p.","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276137,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047462.PNG"},{"id":276135,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016319.zip"}],"country":"United States","state":"Pennsylvania","county":"Lehigh County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.89003,40.419422 ], [ -75.89003,40.786114 ], [ -75.335381,40.786114 ], [ -75.335381,40.419422 ], [ -75.89003,40.419422 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021aebe4b0e21cafa49cb5","contributors":{"authors":[{"text":"Wood, Charles R.","contributorId":30259,"corporation":false,"usgs":true,"family":"Wood","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482096,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flippo, Herbert N. Jr.","contributorId":36597,"corporation":false,"usgs":true,"family":"Flippo","given":"Herbert","suffix":"Jr.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":482097,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lescinsky, Joseph B.","contributorId":53377,"corporation":false,"usgs":true,"family":"Lescinsky","given":"Joseph","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":482099,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Barker, James L.","contributorId":53000,"corporation":false,"usgs":true,"family":"Barker","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":482098,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70047461,"text":"70047461 - 1972 - Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania","interactions":[{"subject":{"id":55926,"text":"ofr69212 - 1969 - Progress report on the hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania","indexId":"ofr69212","publicationYear":"1969","noYear":false,"title":"Progress report on the hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania"},"predicate":"SUPERSEDED_BY","object":{"id":70047461,"text":"70047461 - 1972 - Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania","indexId":"70047461","publicationYear":"1972","noYear":false,"title":"Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania"},"id":1}],"lastModifiedDate":"2013-08-06T15:37:01","indexId":"70047461","displayToPublicDate":"2013-01-01T15:30:10","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":143,"text":"Water Resource Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"30","title":"Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania","docAbstract":"The Martinsburg Formation underlies the northern half of Lehigh and Northampton Counties, and is of Middle and LateOrdovician age. It is bounded on the south by older Ordovician limestone formations and on the north by a ridge-forming conglomerate of Silurian age. Recent mapping has supported a three-part division of the Martinsburg into a lower thin-bedded slate {Bushkill Member), a middle graywacke-bearing unit (Ramseyburg Member), and an upper thick-bedded slate (Pen Argyl Member).","language":"English","publisher":"Pennsylvania Geological Survey","publisherLocation":"Harrisburg, PA","collaboration":"Prepared by the United States Geological Survey, Water Resources Division, in cooperation with the Pennsylvania Geological Survey","usgsCitation":"Poth, C.W., 1972, Hydrology of the Martinsburg Formation in Lehigh and Northampton Counties, Pennsylvania: Water Resource Report 30, iv, 52 p.; Map: 1 Sheet.","productDescription":"iv, 52 p.; Map: 1 Sheet","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":276134,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047461.PNG"},{"id":276133,"type":{"id":11,"text":"Document"},"url":"https://www.dcnr.state.pa.us/cs/groups/public/documents/document/dcnr_016318.zip"}],"country":"United States","state":"Pennsylvania","county":"Lehigh County;Northampton County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0,40.5 ], [ -76.0,41.0 ], [ -75.0,41.0 ], [ -75.0,40.5 ], [ -76.0,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52021ae6e4b0e21cafa49c6a","contributors":{"authors":[{"text":"Poth, Charles W.","contributorId":80168,"corporation":false,"usgs":true,"family":"Poth","given":"Charles","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482095,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047580,"text":"70047580 - 1972 - Evaporite deposits of Bogota area, Cordillera Oriental, Colombia","interactions":[{"subject":{"id":20084,"text":"ofr70207 - 1970 - The evaporite deposits of the Bogota area, Cordillera Oriental, Colombia","indexId":"ofr70207","publicationYear":"1970","noYear":false,"title":"The evaporite deposits of the Bogota area, Cordillera Oriental, Colombia"},"predicate":"SUPERSEDED_BY","object":{"id":70047580,"text":"70047580 - 1972 - Evaporite deposits of Bogota area, Cordillera Oriental, Colombia","indexId":"70047580","publicationYear":"1972","noYear":false,"title":"Evaporite deposits of Bogota area, Cordillera Oriental, Colombia"},"id":1}],"lastModifiedDate":"2023-01-31T17:46:06.022842","indexId":"70047580","displayToPublicDate":"2013-01-01T15:10:00","publicationYear":"1972","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":701,"text":"American Association of Petroleum Geologists Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Evaporite deposits of Bogota area, Cordillera Oriental, Colombia","docAbstract":"<p>Four evaporite-bearing stratigraphic zones are known in Cretaceous strata of the Cordillera Oriental of Colombia north and east of Bogota. The easternmost and oldest zone is probably of Berriasian to Valanginian age. The next oldest is probably late Barremian to early Aptian in age. The third appears to be Aptian. The westernmost and best known sequence in the Sabana de Bogota is Turonian to early Coniacian in age. This youngest sequence contains the thickest salt deposits known in Colombia and is probably the most widespread geographically.</p><p>Most of the rock salt exposed in the three accessible mines (at Zipaquira, Nemocon, and Upin) has a characteristic lamination of alternating slightly argillaceous and highly argillaceous salt layers of varied but moderate thickness. Black, calcareous claystone, commonly very pyritic, is interbedded conformably with the laminated salt in many places throughout the deposits. Fragments of black claystone derived from the thinner interbeds are ubiquitous in all deposits, both as concordant breccia zones and as isolated clasts.</p><p>Anhydrite is scarce at Zipaquira and apparently even rarer at Nemocon and Upin. Gypsum is produced at three small deposits in the oldest evaporite zone where it probably was concentrated by leaching of salt initially associated with it.</p><p>The two intervening evaporite zones are not exposed, but their existence and distribution are indicated by brine springs and locally by \"rute,\" a distinctive black, calcareous mud formed by the leaching of salt beds.</p><p>Fossils show that the youngest salt-claystone zone, in the Sabana de Bogota, is contemporary with associated hematitic sandstone and siltstone, and with carbonaceous and locally coaly claystone. Although evidence is poor, this same facies relation probably exists within the other three evaporite zones.</p><p>All salt deposits in this study probably are associated with anticlines, a relation best exemplified by the deposits on the Sabana de Bogota. Within these anticlines the salt deposits appear to be contained stratigraphically in fault-bound crestal, claystone cores that have not been mobilized over great vertical distances. The deposits of this study are not salt domes.</p>","language":"English","publisher":"American Association of Petroleum Geologists","doi":"10.1306/819A41FE-16C5-11D7-8645000102C1865D","usgsCitation":"McLaughlin, D.H., 1972, Evaporite deposits of Bogota area, Cordillera Oriental, Colombia: American Association of Petroleum Geologists Bulletin, v. 56, no. 11, p. 2240-2259, https://doi.org/10.1306/819A41FE-16C5-11D7-8645000102C1865D.","productDescription":"20 p.","startPage":"2240","endPage":"2259","costCenters":[],"links":[{"id":276548,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Colombia","city":"Bogota","otherGeospatial":"Cordillera Oriental","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -71.73591768051784,\n              6.43270960214528\n            ],\n            [\n              -75.52600833049453,\n              6.43270960214528\n            ],\n            [\n              -75.52600833049453,\n              2.387732778963965\n            ],\n            [\n              -71.73591768051784,\n              2.387732778963965\n            ],\n            [\n              -71.73591768051784,\n              6.43270960214528\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"56","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"520a03e8e4b0026c2bc11b15","contributors":{"authors":[{"text":"McLaughlin, Donald H. Jr.","contributorId":73215,"corporation":false,"usgs":true,"family":"McLaughlin","given":"Donald","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482446,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047772,"text":"70047772 - 1972 - Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington","interactions":[{"subject":{"id":8894,"text":"ofr70129 - 1972 - Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington","indexId":"ofr70129","publicationYear":"1972","noYear":false,"title":"Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington"},"predicate":"SUPERSEDED_BY","object":{"id":70047772,"text":"70047772 - 1972 - Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington","indexId":"70047772","publicationYear":"1972","noYear":false,"title":"Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington"},"id":1}],"lastModifiedDate":"2019-11-12T17:31:40","indexId":"70047772","displayToPublicDate":"2013-01-01T15:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"65","title":"Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington","docAbstract":"A geochemical exploration program aimed at determining regional patterns of metal distribution as well as pinpointing areas likely to contain undiscovered ore deposits was carried out in north-central Okanogan County, Washington. About 1,000 gully and stream sediment samples were collected from a rectangular area of about 800 square miles. The area includes two contiguous, virtually dormant, mining districts that had yielded nearly $1.4 million in gold, silver, lead, copper, and zinc prior to the end of World War I, mostly from quartz lodes.","language":"English","publisher":"Washington Department of Natural Resources","publisherLocation":"Olympia, Washington","collaboration":"Prepared cooperatively by the United States Geological Survey","usgsCitation":"Fox, K.F., and Rinehart, C.D., 1972, Distribution of copper and other metals in gully sediments of part of Okanogan County, Washington: Bulletin 65, v, 38 p.","productDescription":"v, 38 p.","numberOfPages":"48","costCenters":[],"links":[{"id":276914,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047772.JPG"},{"id":276913,"type":{"id":11,"text":"Document"},"url":"https://www.dnr.wa.gov/publications/ger_b65_metals_seds_okanogan_co.pdf"}],"country":"United States","state":"Washington","county":"Okanogan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.8352,47.9408 ], [ -120.8857, 47.9408 ], [ -120.8857, 49.0006 ], [ -118.8352, 49.0006 ], [ -118.8352, 47.9408 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521732e4e4b043bae8d2e5d7","contributors":{"authors":[{"text":"Fox, Kenneth F. Jr.","contributorId":82269,"corporation":false,"usgs":true,"family":"Fox","given":"Kenneth","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":482938,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rinehart, C. Dean","contributorId":88326,"corporation":false,"usgs":true,"family":"Rinehart","given":"C.","email":"","middleInitial":"Dean","affiliations":[],"preferred":false,"id":482939,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047829,"text":"70047829 - 1972 - Geology and mineral deposits of the Loomis quadrangle, Okanogan County, Washington","interactions":[],"lastModifiedDate":"2013-08-26T12:41:48","indexId":"70047829","displayToPublicDate":"2013-01-01T12:32:00","publicationYear":"1972","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":105,"text":"Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"64","title":"Geology and mineral deposits of the Loomis quadrangle, Okanogan County, Washington","language":"English","publisher":"Washington Division of Mines and Geology","publisherLocation":"Olympia, WA","collaboration":"Prepared cooperatively by the U.S. Geological Survey","usgsCitation":"Rinehart, C., and Fox, K., 1972, Geology and mineral deposits of the Loomis quadrangle, Okanogan County, Washington: Bulletin 64, vii, 124 p.; Map: 1 Sheet.","productDescription":"vii, 124 p.; Map: 1 Sheet","costCenters":[],"links":[{"id":276997,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047829.gif"},{"id":276996,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_30845.htm"}],"scale":"62500","country":"United States","state":"Washington","county":"Okanogan County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.5,48.75 ], [ -119.5,49.0 ], [ -119.75,49.0 ], [ -119.75,48.75 ], [ -119.5,48.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"521c78e7e4b01458f7842943","contributors":{"authors":[{"text":"Rinehart, C.D.","contributorId":94310,"corporation":false,"usgs":true,"family":"Rinehart","given":"C.D.","email":"","affiliations":[],"preferred":false,"id":483083,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fox, K. F. Jr.","contributorId":46554,"corporation":false,"usgs":true,"family":"Fox","given":"K. F.","suffix":"Jr.","affiliations":[],"preferred":false,"id":483082,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047241,"text":"70047241 - 1972 - Hydrochemical study of the National Reactor Testing Station, Idaho","interactions":[],"lastModifiedDate":"2013-07-26T09:58:45","indexId":"70047241","displayToPublicDate":"2013-01-01T09:52:00","publicationYear":"1972","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Hydrochemical study of the National Reactor Testing Station, Idaho","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Hydrogeology: section 11 of the 24th International Geological Congress, Montreal 1972","largerWorkSubtype":{"id":12,"text":"Conference publication"},"language":"English","publisher":"International Geological Congress","publisherLocation":"Montreal, Canada","usgsCitation":"Schoen, R., 1972, Hydrochemical study of the National Reactor Testing Station, Idaho, <i>in</i> Hydrogeology: section 11 of the 24th International Geological Congress, Montreal 1972, p. 306-314.","productDescription":"9 p.","startPage":"306","endPage":"314","costCenters":[{"id":343,"text":"Idaho Water Science Center","active":true,"usgs":true}],"links":[{"id":275425,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Idaho","otherGeospatial":"Idaho National Laboratory","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.1355,43.4243 ], [ -113.1355,43.8876 ], [ -112.6011,43.8876 ], [ -112.6011,43.4243 ], [ -113.1355,43.4243 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51f39a65e4b0a32220222f7d","contributors":{"authors":[{"text":"Schoen, Robert","contributorId":22418,"corporation":false,"usgs":true,"family":"Schoen","given":"Robert","email":"","affiliations":[],"preferred":false,"id":481485,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70042895,"text":"70042895 - 1972 - Photogeology: Part X: calibration of radar data from Apollo 16 results","interactions":[],"lastModifiedDate":"2013-01-28T13:27:41","indexId":"70042895","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"315","title":"Photogeology: Part X: calibration of radar data from Apollo 16 results","docAbstract":"Orbital and surface photography collected during the Apollo 16 mission can be used to calibrate existing Earth-based, high-resolution radar maps of the lunar surface. The absence of any theoretical treatment of the radar backscatter from irregular rocks has prevented the assignment of radar-echo cross sections to specific size distributions of rocks. This gap will now be filled with the use of ground truth provided by metric and panoramic camera photographs and by surface photographic data collected by the astronauts.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 16 preliminary science report (NASA SP 315)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Zisk, S., and Moore, H., 1972, Photogeology: Part X: calibration of radar data from Apollo 16 results, chap. <i>of</i> Apollo 16 preliminary science report (NASA SP 315), p. 29-110-29-113.","productDescription":"4 p.","startPage":"29-110","endPage":"29-113","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":266623,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266622,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a16/as16psr.pdf"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5107ac1ce4b0df796f216e96","contributors":{"authors":[{"text":"Zisk, S.H.","contributorId":35311,"corporation":false,"usgs":true,"family":"Zisk","given":"S.H.","email":"","affiliations":[],"preferred":false,"id":472524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, H. J.","contributorId":71962,"corporation":false,"usgs":true,"family":"Moore","given":"H. J.","affiliations":[],"preferred":false,"id":472525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70042874,"text":"70042874 - 1972 - Photogeology: Part B: Cayley Formation interpreted as basin ejecta","interactions":[],"lastModifiedDate":"2013-01-27T18:30:49","indexId":"70042874","displayToPublicDate":"2013-01-01T00:00:00","publicationYear":"1972","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"seriesNumber":"315","title":"Photogeology: Part B: Cayley Formation interpreted as basin ejecta","docAbstract":"The discovery that samples returned from the Cayley Formation at the Apollo 16 landing site consist mainly of nonvolcanic breccias (secs. 6 and 7 of this report) suggests that the hypothesis in which light plains-forming materials may be ejecta from multi-ring basins should be reevaluated (refs 29-15 to 29-17). Improved information on the morphology and distribution of the Cayley Formation, provided by Apollo 16 orbital photography, leads to a concept in which the Cayley Formation was deposited as fluidized debris that traveled beyond the presently recognizable extent of the Imbrium Basin ejecta. An elaboration of this genetic model is in preparation; the description, a summary of the model, and its implications are presented in this subsection.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Apollo 16 preliminary science report (NASA SP 315)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"National Aeronautics and Space Administration","publisherLocation":"Washington, D.C.","usgsCitation":"Eggleton, R.E., and Schaber, G.G., 1972, Photogeology: Part B: Cayley Formation interpreted as basin ejecta, chap. <i>of</i> Apollo 16 preliminary science report (NASA SP 315), p. 29-7-29-16.","productDescription":"10 p.","startPage":"29-7","endPage":"29-16","costCenters":[{"id":131,"text":"Astrogeology Science Center","active":true,"usgs":true}],"links":[{"id":266580,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266579,"type":{"id":11,"text":"Document"},"url":"https://www.hq.nasa.gov/alsj/a16/as16psr.pdf"}],"otherGeospatial":"Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"51065a82e4b0f227c1e454c0","contributors":{"authors":[{"text":"Eggleton, R. E.","contributorId":75154,"corporation":false,"usgs":true,"family":"Eggleton","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":472487,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schaber, G. G.","contributorId":68300,"corporation":false,"usgs":true,"family":"Schaber","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":472486,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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