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,{"id":70210468,"text":"70210468 - 1952 - Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska","interactions":[],"lastModifiedDate":"2021-08-31T15:09:42.366714","indexId":"70210468","displayToPublicDate":"1952-01-01T11:08:23","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5963,"text":"Geological Investigations, Naval Petroleum Reserve No. 4, Alaska","active":false,"publicationSubtype":{"id":6}},"seriesNumber":"33","subseriesTitle":"Special Report","title":"Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska","docAbstract":"<p>A think complex sequence of olastic rocks, formerly named the Noatak formation, underlies the Lisburns formation (Mississippian) in the Brooks Range, northern Alaska. Five formations have been recognized as a result of of recent investigations by the author and other geologists of the Navy Oil Unit, U.S. Geological Survey. In the western Brooks Range, the three formations present below the Lisburns formation are: Utukok formation (Upper Touranisian to Lower Visean), Montak formation (restricted) (Upper Devonian to Lower Tournaisian (?)) and Hunt Fork (?) formation (Upper Devonian). In the central Brooks Range the Kayak formation (Lower to Upper Tournaisian), Kanayut formation (Upper Devonian to Lower Tournaisian (?)), and Hunt Fork formation (Upper Devonian) lie below the Lisburns formation.</p><p>Lithologic and faunal characteristics of these sedimentary units reveal the regional pattern of sedimentation and suggest specific paleoecologic environments. The chart conglomerates in the Kanayut and Noatuk formations are thought to have formed in a belt characterized by fluctuating marine and nonmarine conditions, the chart source being a mid-Devonian ragolith.</p><p>Analysis of formulas suggest certain correlations with the European, Siberian, and western Cordilleran sections.</p><p>Described faunas of the Utukok and Kayak formations include 40 braciopod species and varieties, 9 echinodera species, 2 bryzoan species, 8 molluscan species, and 1 tribute species, of which 13 are new.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70210468","usgsCitation":"Dutro, J.T., 1952, Stratigraphy and paleontology of the Noatak and associated formations, Brooks Range, Alaska: Geological Investigations, Naval Petroleum Reserve No. 4, Alaska 33, Report: iii, 144 p.; 3 Plates; 1 Table, https://doi.org/10.3133/70210468.","productDescription":"Report: iii, 144 p.; 3 Plates; 1 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,{"id":71245,"text":"tei176 - 1952 - The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado","interactions":[],"lastModifiedDate":"2014-04-03T14:45:54","indexId":"tei176","displayToPublicDate":"1952-01-01T10:56:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"176","title":"The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado","docAbstract":"Uranium deposits that contain uraniferous pyrobitumen of possible hydrothermal origin occur at the Weatherly and Robinson properties near Placerville, San Miguel County, Colo. These deposits were mined for copper, silver, and gold more than 50 years ago and were developed for uranium in 1950.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei176","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wilmarth, V., and Vickers, R., 1952, The Robinson and Weatherly uraniferous pyrobitumen deposits near Placerville, San Miguel County, Colorado: U.S. Geological Survey Trace Elements Investigations 176, 47 p., https://doi.org/10.3133/tei176.","productDescription":"47 p.","numberOfPages":"48","costCenters":[],"links":[{"id":283639,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei176.jpg"},{"id":285612,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0176/report.pdf"}],"country":"United States","state":"Colorado","county":"San Miguel County","city":"Placerville","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.04515,37.772072 ], [ -109.04515,38.153099 ], [ -107.73111,38.153099 ], [ -107.73111,37.772072 ], [ -109.04515,37.772072 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355959de4b0120853e8c26a","contributors":{"authors":[{"text":"Wilmarth, V.R.","contributorId":20803,"corporation":false,"usgs":true,"family":"Wilmarth","given":"V.R.","email":"","affiliations":[],"preferred":false,"id":283858,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Vickers, R.C.","contributorId":50583,"corporation":false,"usgs":true,"family":"Vickers","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":283859,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048431,"text":"tem500A - 1952 - Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","interactions":[{"subject":{"id":70048431,"text":"tem500A - 1952 - Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","indexId":"tem500A","publicationYear":"1952","noYear":false,"chapter":"A","title":"Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":66898,"text":"i178 - 1956 - Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah","indexId":"i178","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah"},"id":1}],"supersededBy":{"id":66898,"text":"i178 - 1956 - Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah","indexId":"i178","publicationYear":"1956","noYear":false,"title":"Photogeologic map of the Orange Cliffs-13 quadrangle, Garfield County, Utah"},"lastModifiedDate":"2014-03-04T13:39:52","indexId":"tem500A","displayToPublicDate":"1952-01-01T10:47:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"500","chapter":"A","title":"Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem500A","collaboration":"Prepared in cooperation with the U.S. Atomic Energy Commission","usgsCitation":"Ray, R., 1952, Photogeologic map, Orange Cliffs-13 quadrangle, Garfield county, Utah: U.S. Geological Survey Trace Elements Memorandum 500, Report: 3 p.; 1 Plate: 23.31 x 29.90 inches, https://doi.org/10.3133/tem500A.","productDescription":"Report: 3 p.; 1 Plate: 23.31 x 29.90 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278122,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0500-A/report-thumb.jpg"},{"id":283244,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0500-A/report.pdf"},{"id":283243,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0500-A/plate-1.pdf"}],"scale":"24000","country":"United States","state":"Utah","county":"Garfield County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.5,38.0 ], [ -110.5,38.125 ], [ -110.375,38.125 ], [ -110.375,38.0 ], [ -110.5,38.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"52455768e4b0b3d37307e1ab","contributors":{"authors":[{"text":"Ray, R.G.","contributorId":60664,"corporation":false,"usgs":true,"family":"Ray","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":484629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70098029,"text":"tei308 - 1952 - Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah","interactions":[],"lastModifiedDate":"2014-06-06T08:35:49","indexId":"tei308","displayToPublicDate":"1952-01-01T10:29:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"308","title":"Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah","docAbstract":"<p>Previous discoveries and studies of radioactive lignites of Tertiary age in North Dakota, South Dakota, Montana, and Wyoming led the Geological Survey in 1950 to do reconnaissance in the Green River and Uinta Basin of Wyoming and Utah, where similar lignites were believed to be present. Because of the common association of uranium with copper deposits and the presence of such deposits in the Uinta Basin, several areas containing copper-uranium minerals were also examined.</p>\n<br/>\n<p>No deposits commercially exploitable under present conditions were found. Samples of coal from the Bear River formation at Sage, Wyo., assayed 0.004 to 0.013 percent uranium in the ash; in the old Uteland copper mine in Uinta County, Utah, 0.007 to 0.017 percent uranium; in a freshwater limestone, Duchesne County, Utah, as much as 0.019 percent uranium; and in the Mesaverde formation at the Snow and Bonniebell claims near Jensen, Uintah County, Utah, 0.003 to 0.090 percent uranium. Maps were made and samples were taken at the Skull Creek carnotite deposits in Moffat County, Colo. (0.006 to 0.16 percent uranium); at the Fair-U claims in Routt County, Colo. (0.002 to 0.040 percent uranium); and at the Lucky Strike claims near Kremmling in Grand County, Colo. (0.006 to 0.018 percent uranium).</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei308","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Beroni, E., and McKeown, F.A., 1952, Reconnaissance for uraniferous rocks in northwestern Colorado, southwestern Wyoming, and northeastern Utah: U.S. Geological Survey Trace Elements Investigations 308, Report: 41 p.; 1 Plate: 16.75 x 15.21 inches, https://doi.org/10.3133/tei308.","productDescription":"Report: 41 p.; 1 Plate: 16.75 x 15.21 inches","numberOfPages":"42","costCenters":[],"links":[{"id":284054,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei308.jpg"},{"id":285633,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0308/report.pdf"},{"id":285632,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0308/figure-1.pdf"}],"country":"United States","state":"Colorado;Utah;Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.5,38.5 ], [ -111.5,42.5 ], [ -106.0,42.5 ], [ -106.0,38.5 ], [ -111.5,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53559532e4b0120853e8c193","contributors":{"authors":[{"text":"Beroni, E.P.","contributorId":13222,"corporation":false,"usgs":true,"family":"Beroni","given":"E.P.","affiliations":[],"preferred":false,"id":491545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McKeown, F. A.","contributorId":106100,"corporation":false,"usgs":true,"family":"McKeown","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":491546,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70274620,"text":"70274620 - 1952 - Hawaiian Volcano Observatory record book 1952","interactions":[],"lastModifiedDate":"2026-04-17T14:26:41.686143","indexId":"70274620","displayToPublicDate":"1952-01-01T10:23:19","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"title":"Hawaiian Volcano Observatory record book 1952","docAbstract":"<p>The Hawaiian Volcano Observatory (HVO) record books are annual journals in which field observations of eruptive activity at Kīlauea and Mauna Loa volcanoes, on the Island of Hawaiʻi, were compiled by HVO staff for most years from 1912 through early 1966. In addition to descriptive observations, the record books also contain hundreds of annotated photographs and sketches, as well as temperature and transit measurements. When photographs are included, the camera settings and film types used are noted. The field notes, sketches, and photographs used to compile the record books provide an unparalleled record of eruptive activity and were the basis for published newspaper reports and periodic bulletins, such as the <a href=\"../publication/70268164\" data-mce-href=\"../publication/70268164\">Hawaiian Volcano Observatory bulletins</a> and <a href=\"../publication/70246900\" data-mce-href=\"../publication/70246900\">The volcano letter</a>. &nbsp;</p><p>HVO staff also painstakingly prepared a second copy of each early record book, virtually identical to the original, complete with photographs and sketches. The original version of the record book was kept at HVO, while the duplicate went to the Hawaiian Volcano Research Association, which was created by a group of Honolulu, Hawaiʻi, businessmen to promote HVO’s work. The Hawaiian Volcano Research Association, which dissolved decades ago, held the duplicate books in Honolulu, where they were more readily accessible to the public. After 1923, HVO stopped duplicating the books—at least, no duplicate records for subsequent years have been found. During the decade of the 1940s, preparation of the record books stopped altogether. In 1952, compilation of the record books resumed and continued, with long gaps, until early 1966. Entries in these later volumes are sparse, and these books are little more than photo albums of the episodic eruptions of Kīlauea.&nbsp;</p><p>The original record books were held at HVO and, later, at Hawai‘i Volcanoes National Park. In 1972, the original record books for the years 1912 through 1939 were transferred to the Bishop Museum, in Honolulu, for safekeeping. These record books are now stored in archival boxes at that institution (accession number 172.265). The duplicate set of record books held by the Hawaiian Volcano Research Association were bound into volumes at an unknown date and turned over to the U.S. Geological Survey. This set of record books, spanning 1912 through 1923, is now housed in the rare book room of the U.S. Geological Survey Library in Reston, Virginia (catalog number 220(950) H3d). The record books for 1952 through early 1966 remain in storage at HVO. After 1955, typed annotations were no longer placed in the record books, and only photographs, most with captions, were included. Although the volumes titled “Record Book” end with the 1955 volume, the photograph albums that followed are similar, and the record book designation is retained for simplicity. 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,{"id":71319,"text":"tei265 - 1952 - The geology of the Florida land-pebble phosphate deposits","interactions":[],"lastModifiedDate":"2014-06-06T08:28:50","indexId":"tei265","displayToPublicDate":"1952-01-01T10:17:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"265","title":"The geology of the Florida land-pebble phosphate deposits","docAbstract":"<p>The land-pebble phosphate district is on the Gulf Coastal Plain of Florida. The phosphate deposits are in the Bone Valley formation, dated Pliocene by most writers. These strata overlie the Miocene Hawthorn formation and are overlain by consolidated sands 3 to 20 feet thick.</p>\n<br/>\n<p>The minable phosphate deposits, called “matrix” in the district, range from a featheredge to about 50 feet in thickness and consist of phosphatic pellets and nodules, quartz sand, and montmorillonitic clay in about equal proportions. Locally the matrix displays cross-bedding and horizontal laminations, but elsewhere it is structureless. The phosphorite particles, composed largely of carbonate-fluorapatite, range in diameter from less than 0.1 mm to about 60 cm and in P<sub>2</sub>O<sub>5<sub> content from 30 to 36 percent. Coarse-pebble deposits, containing 30 to 34 percent P<sub>2</sub>O<sub>5<sub>  are found mainly on basement highs; and fine-pebble deposits, containing 32 to 36 percent P<sub>2</sub>O<sub>5<sub> are, are found in basement lows. Deposits in the northern part of the field contain more phosphate particles and their P<sub>2</sub>O<sub>5<sub>  content is higher than those in the southern part.</p>\n<br/>\n<p>The upper part of the phosphatic strata is leached to an advanced degree and consists of quartz sand and clay-sized particules of pseudowavellite and wavellite. The leached zone ranges in thickness from a featheredge to 60 feet.</p>\n<br/>\n<p>The origin of the land-pebble deposits is incompletely known. Possible modes of origin are a residuum of Miocene age, or a reworked residuum of Pliocene or Quaternary age.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei265","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Cathcart, J., Blade, L., Davidson, D., and Ketner, K.B., 1952, The geology of the Florida land-pebble phosphate deposits: U.S. Geological Survey Trace Elements Investigations 265, 21 p., https://doi.org/10.3133/tei265.","productDescription":"21 p.","numberOfPages":"22","costCenters":[],"links":[{"id":284053,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei265.jpg"},{"id":285631,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0265/report.pdf"}],"country":"United States","state":"Florida","otherGeospatial":"Gulf Coastal Plain","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.5,27.0 ], [ -82.5,28.25 ], [ -81.5,28.25 ], [ -81.5,27.0 ], [ -82.5,27.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355959fe4b0120853e8c281","contributors":{"authors":[{"text":"Cathcart, J.B.","contributorId":83533,"corporation":false,"usgs":true,"family":"Cathcart","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":283986,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Blade, L.V.","contributorId":65093,"corporation":false,"usgs":true,"family":"Blade","given":"L.V.","email":"","affiliations":[],"preferred":false,"id":283984,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":283985,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ketner, K. B.","contributorId":23121,"corporation":false,"usgs":true,"family":"Ketner","given":"K.","email":"","middleInitial":"B.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":283983,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","interactions":[{"subject":{"id":70048427,"text":"tem446 - 1952 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"tem446","publicationYear":"1952","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"predicate":"SUPERSEDED_BY","object":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"id":1}],"supersededBy":{"id":3839,"text":"cir251 - 1953 - Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","indexId":"cir251","publicationYear":"1953","noYear":false,"title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana"},"lastModifiedDate":"2014-03-04T13:37:44","indexId":"tem446","displayToPublicDate":"1952-01-01T10:05:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"446","title":"Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana","docAbstract":"A reconnaissance search for uraniferous lignite and carbonaceous shale was made in western Montana and adjacent parts of Idaho during the summer of 1951. Particular emphasis in the examination was placed on coal and carbonaceous shale associated with volcanic rocks, as volcanic rocks in many area appear to have released uranium to circulating ground water from which it was concentrated in carbonaceous material. Twenty-two area in Montana and one area of Idaho were examine. The coal in five of these area is of Cretaceous age. The coal and carbonaceous shale in the remaining 18 area occur in Tertiary \"lake-bed\" deposits of Oligocene and younger age.  Both the Cretaceous and Tertiary coal and carbonaceous shale are associated with contemporaneous or younger volcanic rocks and pyroclastic sequences.  A sample of carbonaceous shale from the Prickly Pear Valley northeast of Helena, Montana, contained 0.013 percent uranium. A sample of carbonaceous shale from the Flint Creek Valley southwest of Drummond, Montana, contained 0.006 percent uranium. All other samples of both Cretaceous and Tertiary coal and carbonaceous shale were essentially non-radioactive. No further work is planned on the Cretaceous and Tertiary coal and carbonaceous shale in western Montana. A few localities in Idaho will be visited in the course of other work.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem446","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Hail, W.J., and Gill, J.R., 1952, Results of reconnaissance for uraniferous coal, lignite, and carbonaceous shale in western Montana: U.S. Geological Survey Trace Elements Memorandum 446, Report: 22 p.; 1 Plate: 23.48 x 13.76 inches, https://doi.org/10.3133/tem446.","productDescription":"Report: 22 p.; 1 Plate: 23.48 x 13.76 inches","numberOfPages":"24","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":278113,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0446/report-thumb.jpg"},{"id":283237,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0446/report.pdf"},{"id":283238,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0446/plate-1.pdf"}],"country":"United States","state":"Idaho;Montana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,44.3582 ], [ -116.05,47.4128 ], [ -109.6316,47.4128 ], [ -109.6316,44.3582 ], [ -116.05,44.3582 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5245576ae4b0b3d37307e1bc","contributors":{"authors":[{"text":"Hail, William J. Jr.","contributorId":99952,"corporation":false,"usgs":true,"family":"Hail","given":"William","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":484623,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gill, James R.","contributorId":44904,"corporation":false,"usgs":true,"family":"Gill","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":484622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25194,"text":"25194 - 1952 - Relative clauses","interactions":[],"lastModifiedDate":"2014-07-15T10:02:56","indexId":"25194","displayToPublicDate":"1952-01-01T10:01:38","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Relative clauses","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","doi":"10.3133/25194","issn":"0364-7064","usgsCitation":"Calkins, F.C., 1952, Relative clauses, 15 p., https://doi.org/10.3133/25194.","productDescription":"15 p.","numberOfPages":"15","costCenters":[],"links":[{"id":290100,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c64db0e4b0001bd51477a3","contributors":{"authors":[{"text":"Calkins, Frank Cathcart","contributorId":31734,"corporation":false,"usgs":true,"family":"Calkins","given":"Frank","email":"","middleInitial":"Cathcart","affiliations":[],"preferred":false,"id":193321,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70232383,"text":"70232383 - 1952 - Wildlife research: Or disaster!","interactions":[],"lastModifiedDate":"2022-07-19T16:30:16.911678","indexId":"70232383","displayToPublicDate":"1952-01-01T10:01:32","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":688,"text":"Alabama Conservation","active":true,"publicationSubtype":{"id":10}},"title":"Wildlife research: Or disaster!","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Alabama Department of Conservation","usgsCitation":"Haugen, A.O., 1952, Wildlife research: Or disaster!: Alabama Conservation, v. 24, no. 3, p. 6-7.","productDescription":"2 p.","startPage":"6","endPage":"7","costCenters":[{"id":104,"text":"Alabama Cooperative Fish & Wildlife Unit","active":false,"usgs":true}],"links":[{"id":404037,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Haugen, Arnold O.","contributorId":292651,"corporation":false,"usgs":false,"family":"Haugen","given":"Arnold","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":846926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71301,"text":"tei242 - 1952 - Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products","interactions":[],"lastModifiedDate":"2014-06-06T07:50:28","indexId":"tei242","displayToPublicDate":"1952-01-01T09:53:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"242","title":"Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products","docAbstract":"<p>In 1942 the Geological Survey began to collect, in response to a request made by the War Production Board, samples of mine, mill, and smelter products. About 1,400 such samples were collected and analyzed spectrographically for about 20 elements that were of strategic importance, in order to determine whether any of the products analyzed might be possible sources of some of the needed elements. When attention was directed to radioactive elements in 1943, most of the samples were scanned for radioactivity. Part of the work was done on behalf of the Division of Raw Materials of the Atomic Energy Commission.</p>\n<br/>\n<p>The sources, mine mill, smelter, or prospect, from which these samples were collected, the kind of material sampled, i.e. ores, concentrates, middlings, tailings, flue dusts, and so forth, and the radioactivity of the samples are listed in this report. Samples of the materials collected in the course of the Geological Survey’s investigations for uranium are excluded, but about 500 such samples were analyzed spectrographically for some or all of the same 20 elements sought in the samples that are the subject of this report. Most of the samples were tested only for their radioactivity, but a few were analyzed chemically for uranium. The radioactivity of many of the samples tested in the early screening was determined only qualitatively. Several samples were tested at one time, and if the count obtained did not exceed a predetermined minimum above background, the samples were not tested individually. If the count was more than this minimum, the samples were tested individually to identify the radioactive sample or samples and to obtain a quantitative value for the radioactivity. In general, the rough screening served as a basis for separating samples in which the radioactivity amount to less than 0.003 percent equivalent uranium from those in which it exceeded that amount. Some aspects of various phases of the investigation of radioactivity in these samples have been reported in various other reports, as follows.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei242","collaboration":"This report concerns work done partly on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Hall, M.L., and Butler, A.P., 1952, Compilation of data on the uranium and equivalent uranium content of samples analyzed by U.S. Geological Survey during a program of sampling mine, mill, and smelter products: U.S. Geological Survey Trace Elements Investigations 242, 46 p., https://doi.org/10.3133/tei242.","productDescription":"46 p.","numberOfPages":"47","costCenters":[],"links":[{"id":284051,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei242.jpg"},{"id":285625,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0242/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53558ffce4b0120853e8be90","contributors":{"authors":[{"text":"Hall, Marlene Louise","contributorId":40516,"corporation":false,"usgs":true,"family":"Hall","given":"Marlene","email":"","middleInitial":"Louise","affiliations":[],"preferred":false,"id":283961,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, Arthur Pierce Jr.","contributorId":88826,"corporation":false,"usgs":true,"family":"Butler","given":"Arthur","suffix":"Jr.","email":"","middleInitial":"Pierce","affiliations":[],"preferred":false,"id":283962,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70048313,"text":"tem397 - 1952 - Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah","interactions":[],"lastModifiedDate":"2014-02-28T14:46:17","indexId":"tem397","displayToPublicDate":"1952-01-01T09:42:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":338,"text":"Trace Elements Memorandum","code":"TEM","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"397","title":"Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem397","collaboration":"Prepared in cooperation with the Atomic Energy Commission","usgsCitation":"Bates, C., 1952, Photogeological map, Stinking Spring Creek-13 Quadrangle, Emery County, Utah: U.S. Geological Survey Trace Elements Memorandum 397, Report: 3 p.; 1 Plate: 23.33 x 25.45 inches, https://doi.org/10.3133/tem397.","productDescription":"Report: 3 p.; 1 Plate: 23.33 x 25.45 inches","numberOfPages":"3","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":277955,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tem/0397/report-thumb.jpg"},{"id":283118,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tem/0397/plate-1.pdf"},{"id":283117,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tem/0397/report.pdf"}],"country":"United States","state":"Utah","county":"Emery County","otherGeospatial":"Stinking Spring Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0,38.5 ], [ -111.0,38.625 ], [ -110.875,38.625 ], [ -110.875,38.5 ], [ -111.0,38.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"523d6e66e4b097188d6c76ed","contributors":{"authors":[{"text":"Bates, C.E.","contributorId":48237,"corporation":false,"usgs":true,"family":"Bates","given":"C.E.","email":"","affiliations":[],"preferred":false,"id":484299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221604,"text":"70221604 - 1952 - Geology of the Iron King Mine, Yavapai county, Arizona","interactions":[],"lastModifiedDate":"2021-06-25T12:17:52.193622","indexId":"70221604","displayToPublicDate":"1952-01-01T07:09:55","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Geology of the Iron King Mine, Yavapai county, Arizona","docAbstract":"<p><span>The&nbsp;</span>Iron<span>&nbsp;</span>King<span>&nbsp;</span>mine<span>&nbsp;is about 2,000 feet west-northwest of the intersection of the 112 15 west meridian and the 34 30 north parallel in the Humboldt region in central&nbsp;</span>Yavapai<span>&nbsp;</span>County<span>,&nbsp;</span>Arizona<span>. The&nbsp;</span>mine<span>&nbsp;is approximately in the geographical center of the Humboldt region. Precambrian rocks form the bedrock. Late Cenozoic unconsolidated river wash and valley fill with some interbedded basalt locally mantle the Precambrian rocks, especially in the north-central part of the region. The Precambrian rocks consist of two metamorphosed volcanic formations and intrusive rocks that range in composition from quartz porphyry to gabbro. The volcanic formations originally were flows, volcanic breccias, and tuffaceous sedimentary rocks. Dynamothermal metamorphism of these rocks formed textures, structures, and mineral assemblages characteristic of low-grade ;riietamorphic rocks, but sufficient relict textures and structures remain to permit delineation of formations on the bases of their original nature. All the Precambrian rocks are foliated, except those in the interior parts of the larger intrusive masses. This foliation has two major trends, (1) north to N 20° W, and (2) N 20° E. The northeast-trending foliation is younger and locally is superimposed on the north- to northwest-trending foliation. The Precambrian rocks strike north to northwest and dip steeply, chiefly westward. Duplication of stratigraphic units and determination of tops suggest two major northeast-trending folds, which probably plunge southward. The northeast-trending foliation appears to bear an axial-plane relationship to these folds. Some masses of igneous rock probably were intruded during development of foliation. The&nbsp;</span>Iron<span>&nbsp;</span>King<span>&nbsp;deposit supports the only active&nbsp;</span>mine<span>&nbsp;in the Humboldt region. It consists of 12 steeply plunging echelon veins arranged along the footwall of a sheared and altered zone in the metamorphosed andesitic tuffaceous sedimentary rocks. Narrow zones of more intense shear probably localized the veins. Solutions first introduced quartz, pyrite, ankerite, and sericite, forming a sporadically mineralized zone (in the hanging wall of the deposit) and probably veins in the&nbsp;</span>Iron<span>&nbsp;</span>King<span>&nbsp;fracture system. Intra-mineralization shear strongly brecciated these early minerals and formed the structures that localized and distributed the ore minerals in the veins. After this deformation, sphalerite, galena, chalcopyrite, tennantite, arsenopyrite, pyrite, quartz, and ankerite were deposited; the last three minerals may have formed through solution and the redeposition of earlier minerals. Formation of sericite either accompanied or followed the deposition of ore-forming minerals. Silver is related closely in distribution to copper and probably is in the tennantite. Gold occurs chiefly in the pyrite. Banding, mimetic after foliation and planes developed by shearing, is pronounced in much of the vein material. Mineral zoning, generally similar in each vein, is a characteristic of the deposit. High-angle reverse faults of about 100 feet in maximum vertical separation offset the veins. These faults are nearly parallel to the veins in strike and dip.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.47.1.24","usgsCitation":"Creasey, S., 1952, Geology of the Iron King Mine, Yavapai county, Arizona: Economic Geology, v. 47, no. 1, p. 24-56, https://doi.org/10.2113/gsecongeo.47.1.24.","productDescription":"33 p.","startPage":"24","endPage":"56","costCenters":[],"links":[{"id":386727,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Iron King Mine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.25418090820312,\n              34.49693681996495\n            ],\n            [\n              -112.21572875976561,\n              34.49693681996495\n            ],\n            [\n              -112.21572875976561,\n              34.526358599757465\n            ],\n            [\n              -112.25418090820312,\n              34.526358599757465\n            ],\n            [\n              -112.25418090820312,\n              34.49693681996495\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"47","issue":"1","noUsgsAuthors":false,"publicationDate":"1952-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Creasey, S.C.","contributorId":36109,"corporation":false,"usgs":true,"family":"Creasey","given":"S.C.","email":"","affiliations":[],"preferred":false,"id":818257,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39241,"text":"pp242 - 1952 - Larger invertebrate fossils of the Woodbine formation (Cenomanian) of Texas, with decapod crustaceans from the Woodbine formation of Texas","interactions":[],"lastModifiedDate":"2023-04-13T21:59:54.279189","indexId":"pp242","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","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":"242","title":"Larger invertebrate fossils of the Woodbine formation (Cenomanian) of Texas, with decapod crustaceans from the Woodbine formation of Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp242","usgsCitation":"Stephenson, L.W., and Stenzel, H.B., 1952, Larger invertebrate fossils of the Woodbine formation (Cenomanian) of Texas, with decapod crustaceans from the Woodbine formation of Texas: U.S. Geological Survey Professional Paper 242, Report: iv, 226; 4 Plates: 36.50 x 35.41 inches or smaller, https://doi.org/10.3133/pp242.","productDescription":"Report: iv, 226; 4 Plates: 36.50 x 35.41 inches or smaller","costCenters":[],"links":[{"id":104397,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4228.htm","linkFileType":{"id":5,"text":"html"},"description":"4228"},{"id":66977,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0242/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66976,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0242/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":66975,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0242/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0242/report.pdf"},{"id":66974,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0242/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":170274,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0242/report-thumb.jpg"}],"country":"United States","state":"Texas","otherGeospatial":"Woodbine formation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -97.1308,\n              33.9183\n            ],\n            [\n              -97.1308,\n              33.3933\n            ],\n            [\n              -96.25,\n              33.3933\n            ],\n            [\n              -96.25,\n              33.9183\n            ],\n            [\n              -97.1308,\n              33.9183\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a91ca","contributors":{"authors":[{"text":"Stephenson, L. W.","contributorId":70349,"corporation":false,"usgs":true,"family":"Stephenson","given":"L.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221189,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stenzel, H. B.","contributorId":64944,"corporation":false,"usgs":true,"family":"Stenzel","given":"H.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":221188,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":81349,"text":"81349 - 1952 - Twenty five years of Federal fishery research on the Great Lakes","interactions":[],"lastModifiedDate":"2016-02-18T10:32:40","indexId":"81349","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"85","title":"Twenty five years of Federal fishery research on the Great Lakes","docAbstract":"<p>The major purpose of this publication is to present an annotated bibliography of papers resulting from Federal investigations on the Great Lakes fish and fisheries since the formal initiation of a continuing research program by the Fish and Wildlife Service. It is believed that this purpose can be served best by prefacing that bibliography with a brief account of the origins of Great Lakes Fishery Investigations, of the circumstances that have guided their course, and of the scientists who have participated in the several studies.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Hile, R., 1952, Twenty five years of Federal fishery research on the Great Lakes: Special Scientific Report - Fisheries 85, 48 p.","productDescription":"48 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101776,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045825877?urlappend=%3Bseq=319"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a49e4b07f02db623d86","contributors":{"authors":[{"text":"Hile, Ralph","contributorId":48510,"corporation":false,"usgs":true,"family":"Hile","given":"Ralph","email":"","affiliations":[],"preferred":false,"id":295271,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39213,"text":"pp248A - 1952 - Mica deposits of the southeastern Piedmont, Part 1, General features","interactions":[],"lastModifiedDate":"2023-11-13T19:45:49.567698","indexId":"pp248A","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","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":"248","chapter":"A","title":"Mica deposits of the southeastern Piedmont, Part 1, General features","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/pp248A","usgsCitation":"Jahns, R.H., Griffitts, W.R., and Heinrich, E.W., 1952, Mica deposits of the southeastern Piedmont, Part 1, General features: U.S. Geological Survey Professional Paper 248, vi, 102 p.; 1 Plate: 22.74 x 19.77 inches, https://doi.org/10.3133/pp248A.","productDescription":"vi, 102 p.; 1 Plate: 22.74 x 19.77 inches","numberOfPages":"109","costCenters":[],"links":[{"id":104405,"rank":4,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_98134.htm","linkFileType":{"id":5,"text":"html"}},{"id":264251,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0248a/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":268937,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0248a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":169688,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0248a/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Piedmont Province","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,32 ], [ -89,41.5 ], [ -73,41.5 ], [ -73,32 ], [ -89,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a56e4b07f02db62db2e","contributors":{"authors":[{"text":"Jahns, R. H.","contributorId":97961,"corporation":false,"usgs":true,"family":"Jahns","given":"R.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":221150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffitts, W. R.","contributorId":10428,"corporation":false,"usgs":true,"family":"Griffitts","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":221148,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heinrich, E. W.","contributorId":81963,"corporation":false,"usgs":true,"family":"Heinrich","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70011124,"text":"70011124 - 1952 - Radiochemical preparation of heptadecene-81","interactions":[],"lastModifiedDate":"2019-12-12T08:21:00","indexId":"70011124","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Radiochemical preparation of heptadecene-81","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Science","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","doi":"10.1126/science.116.3018.477","issn":"00368075","usgsCitation":"Burton, V., and Breger, I.A., 1952, Radiochemical preparation of heptadecene-81: Science, v. 116, no. 3018, p. 477-479, https://doi.org/10.1126/science.116.3018.477.","startPage":"477","endPage":"479","numberOfPages":"3","costCenters":[],"links":[{"id":221731,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"116","issue":"3018","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a93f0e4b0c8380cd810f8","contributors":{"authors":[{"text":"Burton, V.L.","contributorId":85329,"corporation":false,"usgs":true,"family":"Burton","given":"V.L.","email":"","affiliations":[],"preferred":false,"id":360333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Breger, Irving A.","contributorId":65205,"corporation":false,"usgs":true,"family":"Breger","given":"Irving","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":360332,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011125,"text":"70011125 - 1952 - Fluorometric analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:19:07","indexId":"70011125","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Fluorometric analysis","docAbstract":"[No abstract available]","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Analytical Chemistry","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","issn":"00032700","usgsCitation":"Fletcher, M.H., Friedemann, T., Kavanagh, F., Leininger, E., and Murata, J., 1952, Fluorometric analysis: Analytical Chemistry, v. 24, no. 12, p. 1965-1968.","startPage":"1965","endPage":"1968","numberOfPages":"4","costCenters":[],"links":[{"id":221732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a128fe4b0c8380cd5435d","contributors":{"authors":[{"text":"Fletcher, M. H.","contributorId":53438,"corporation":false,"usgs":true,"family":"Fletcher","given":"M.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":360337,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friedemann, T.E.","contributorId":7002,"corporation":false,"usgs":true,"family":"Friedemann","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":360334,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kavanagh, F.","contributorId":37898,"corporation":false,"usgs":true,"family":"Kavanagh","given":"F.","email":"","affiliations":[],"preferred":false,"id":360336,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Leininger, E.E.","contributorId":95200,"corporation":false,"usgs":true,"family":"Leininger","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":360338,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Murata, J.K.","contributorId":35463,"corporation":false,"usgs":true,"family":"Murata","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":360335,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":1013775,"text":"1013775 - 1952 - A rapid presemptive test for furunculosis in fish","interactions":[],"lastModifiedDate":"2025-07-31T15:51:48.374268","indexId":"1013775","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3196,"text":"Progressive Fish-Culturist","active":true,"publicationSubtype":{"id":10}},"title":"A rapid presemptive test for furunculosis in fish","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Oxford Academic","doi":"10.1577/1548-8640(1952)14[74:ARPTFF]2.0.CO;2","usgsCitation":"Griffin, P.J., 1952, A rapid presemptive test for furunculosis in fish: Progressive Fish-Culturist, v. 14, no. 2, p. 74-75, https://doi.org/10.1577/1548-8640(1952)14[74:ARPTFF]2.0.CO;2.","productDescription":"2 p.","startPage":"74","endPage":"75","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132073,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a879f","contributors":{"authors":[{"text":"Griffin, P. J.","contributorId":50111,"corporation":false,"usgs":true,"family":"Griffin","given":"P.","middleInitial":"J.","affiliations":[],"preferred":false,"id":319238,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1014506,"text":"1014506 - 1952 - Further studies on factors determining tissue levels of sulfamerazine in trout","interactions":[],"lastModifiedDate":"2026-04-20T16:11:29.629401","indexId":"1014506","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Further studies on factors determining tissue levels of sulfamerazine in trout","docAbstract":"<p><span>There is considerable variation in the tissue level of sulfamerazine among individual trout in a treated population. This fact may be the reason why prolonged sulfonamide therapy sometimes fails to free all trout from Bacterium salmonicida. The quantity of food given with a standard dosage of sulfamerazine has a pronounced effect on the tissue concentration of sulfamerazine; the concentration increased when the quantity of food decreased. It appears therefore, that trout should be fed at a rate very closely adjusted to their optimum feeding requirements for the best practical results. The start of treatment with high initial doses of sulfamerazine had no effect on the tissue concentration sustained by the maintenance dosage. The relative distribution of sulfamerazine in various organs and tissues of rainbow trout was about the same as in brown and brook trout. The only difference noticed was the lack of peak levels of short duration between the 8 and 10 days of treatment, which is characteristic for brook and brown trout.</span></p>","language":"English","publisher":"American Fisheries Society","doi":"10.1577/1548-8659(1951)81[101:FSOFDT]2.0.CO;2","usgsCitation":"Snieszko, S.F., and Friddle, S.B., 1952, Further studies on factors determining tissue levels of sulfamerazine in trout: Transactions of the American Fisheries Society, v. 81, no. 1, p. 101-110, https://doi.org/10.1577/1548-8659(1951)81[101:FSOFDT]2.0.CO;2.","productDescription":"10 p.","startPage":"101","endPage":"110","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":131568,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a846a","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320492,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Friddle, S. B.","contributorId":18299,"corporation":false,"usgs":true,"family":"Friddle","given":"S.","middleInitial":"B.","affiliations":[],"preferred":false,"id":320493,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70011127,"text":"70011127 - 1952 - Silicate analysis","interactions":[],"lastModifiedDate":"2012-03-12T17:18:26","indexId":"70011127","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Silicate analysis","docAbstract":"[No abstract available]","largerWorkTitle":"Analytical Chemistry","language":"English","issn":"00032700","usgsCitation":"Fowler, R., Hazel, W., Highfill, J., and Stevens, R., 1952, Silicate analysis, <i>in</i> Analytical Chemistry, v. 24, no. 1, p. 196-197.","startPage":"196","endPage":"197","numberOfPages":"2","costCenters":[],"links":[{"id":220685,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b8f34e4b08c986b318db9","contributors":{"authors":[{"text":"Fowler, R.M.","contributorId":74139,"corporation":false,"usgs":true,"family":"Fowler","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":360342,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hazel, W.M.","contributorId":108247,"corporation":false,"usgs":true,"family":"Hazel","given":"W.M.","email":"","affiliations":[],"preferred":false,"id":360343,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Highfill, J.P.","contributorId":14112,"corporation":false,"usgs":true,"family":"Highfill","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":360340,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stevens, R.E.","contributorId":62954,"corporation":false,"usgs":true,"family":"Stevens","given":"R.E.","email":"","affiliations":[],"preferred":false,"id":360341,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70011111,"text":"70011111 - 1952 - Absorption characteristics of the dithizone mixed color system: A theoretical treatment","interactions":[],"lastModifiedDate":"2012-03-12T17:19:09","indexId":"70011111","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Absorption characteristics of the dithizone mixed color system: A theoretical treatment","docAbstract":"[No abstract available]","largerWorkTitle":"Analytical Chemistry","language":"English","issn":"00032700","usgsCitation":"Milkey, R., 1952, Absorption characteristics of the dithizone mixed color system: A theoretical treatment, <i>in</i> Analytical Chemistry, v. 24, no. 10, p. 1675-1676.","startPage":"1675","endPage":"1676","numberOfPages":"2","costCenters":[],"links":[{"id":221572,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"24","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e64de4b0c8380cd47324","contributors":{"authors":[{"text":"Milkey, R.G.","contributorId":89125,"corporation":false,"usgs":true,"family":"Milkey","given":"R.G.","affiliations":[],"preferred":false,"id":360301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000314,"text":"1000314 - 1952 - Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950","interactions":[],"lastModifiedDate":"2016-02-15T14:12:53","indexId":"1000314","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3624,"text":"Transactions of the American Fisheries Society","active":true,"publicationSubtype":{"id":10}},"title":"Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950","docAbstract":"<div class=\"paragraph\">To obtain information on the post-spawning movements of yellow perch that spawn in southern Green Bay, Lake Michigan, 4,172 fish caught in drop nets were marked by tagging with monel-metal strap tags attached to the right operculum and 24,799 were marked by clipping off the second or membranous dorsal fin. Marking was done during the period from May 3 to 17, 1950, at six main stations, all located in the southern end of Green Bay.</div>\n<div class=\"paragraph\">The average length of the tagged perch was 7.3 inches and all fell within the range 5.5&ndash;14.4 inches. Most (90.9 percent) of the fish were below the minimum legal length of 8.0 inches. The follow-up procedure consisted of informing commercial and sports fishermen of the program and enlisting their cooperation in watching for marked fish; accounts of the investigation were released through newspapers and descriptive posters were distributed. The personnel connected with the investigation examined catches frequently.</div>\n<div class=\"paragraph\">The large majority (101 or 79.5 percent) of the 127 tagged perch recaptured in the experimental nets during the marking operations were retaken at the tagging station at which they were released.</div>\n<div class=\"paragraph\">Of the 108 tagged perch captured by commercial fishermen and anglers following the opening of the season on May 20, 96 were taken by drop nets, 6 by gill nets, and 6 by hook and line. The mean lengths for the three groups were 7.7, 7.1, and 9.25 inches, respectively. All recoveries were made in the Wisconsin waters of Green Bay.</div>\n<div class=\"paragraph\">Most of the &ldquo;open-season&rdquo; recoveries (86 fish; 79.6 percent) were made during the period May 20-May 31. Recaptures during subsequent months were: June&ndash;14; July&ndash;7; August&ndash;none; September&ndash;1. Of the 86 perch recaptured May 20&ndash;31, 70 were retaken inside and 16 outside the tagging area. The majority (14 of 22) of those recovered after May 31 were retaken outside the tagging area.</div>\n<div class=\"paragraph\">The average length of the 20 tagged yellow perch recaptured by drop nets (data restricted to fish from a single type of net to avoid bias from gear selectivity) outside the tagging area (8.42 inches) was 0.96 inch greater than the mean length (7.46 inches) of the 76 fish retaken inside the area. This statistically highly significant difference lends support to the belief of commercial fishermen that the larger of the yellow perch that spawn in southern Green Bay move out soon after spawning.</div>\n<div class=\"paragraph\">The percentage of recapture of tagged perch increased sharply with increase in the size of the fish. Not one of 169 tagged fish less than 6.5 inches long was recovered. The rates of recapture at greater lengths were: 6.5 to 8.9 inches&ndash;2.5 percent; 9.0 to 9.9 inches&ndash;11.4 percent; 10.0 to 14.4 inches&ndash;16.7 percent. Among the several factors suggested in explanation of this relationship, the most important appear to be the lesser ability of the smaller fish to survive the rigors of handling and tagging, greater loss of tags from the smaller fish, and the greater likelihood of overlooking the smaller of the tagged fish in the sorting of the catch.</div>\n<div class=\"paragraph\">The factors just mentioned and the lack of knowledge of the efficiency of measures taken to obtain records of recoveries preclude the 2.6-percent return of all tagged fish from being accepted as an approximation of the rate of recapture. Neither should the 6.6-percent return of tagged fish of legal size (8 inches and longer) be taken as an estimate of the rate of exploitation.</div>\n<div class=\"paragraph\">Although 465 fin-clipped perch were recovered in the experimental nets during the marking operations, only 68 of 24,799 fish so marked were recovered after the fishing season opened. All but one of these 68 were retaken near the point of marking. The difficulty of detecting a perch with a missing membranous dorsal is believed to be a major cause of the poor returns from fin-clipped fish.</div>\n<div class=\"paragraph\">These investigations have demonstrated that for studying migration of yellow perch, tagging is superior to fin-clipping as a method of marking. The technique of the tagging, however, needs to be improved, and better means must be found to trace tagged fish of small size. Furthermore certain small regions in the bay not at present open to commercial fishing must be explored in order to obtain more comprehensive information as to migration.</div>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1951)81[150:MOYPMI]2.0.CO;2","usgsCitation":"Mraz, D., 1952, Movements of yellow perch marked in southern Green Bay, Lake Michigan, in 1950: Transactions of the American Fisheries Society, v. 81, no. 1, p. 150-161, https://doi.org/10.1577/1548-8659(1951)81[150:MOYPMI]2.0.CO;2.","productDescription":"12 p.","startPage":"150","endPage":"161","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":131664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"81","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b482f","contributors":{"authors":[{"text":"Mraz, Donald","contributorId":21502,"corporation":false,"usgs":true,"family":"Mraz","given":"Donald","email":"","affiliations":[],"preferred":false,"id":308377,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70195898,"text":"70195898 - 1952 - Ground water in the Litchville area, Barnes County, North Dakota","interactions":[],"lastModifiedDate":"2018-03-07T13:42:34","indexId":"70195898","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5646,"text":"North Dakota Ground Water Studies","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"18","title":"Ground water in the Litchville area, Barnes County, North Dakota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"North Dakota State Water Conservation Commission","usgsCitation":"Akin, P., 1952, Ground water in the Litchville area, Barnes County, North Dakota: North Dakota Ground Water Studies 18, 51 p.","productDescription":"51 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":352291,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5aff6b45e4b0da30c1bfe4e6","contributors":{"authors":[{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":730420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171409,"text":"70171409 - 1952 - Origin of the Mima Mounds, Thurston County region, Washington","interactions":[],"lastModifiedDate":"2016-05-31T10:54:39","indexId":"70171409","displayToPublicDate":"1952-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2309,"text":"Journal of Geology","active":true,"publicationSubtype":{"id":10}},"title":"Origin of the Mima Mounds, Thurston County region, Washington","docAbstract":"<p><span>There has been recent favorable consideration of the idea that the Mima mounds were made by gophers. The writer believes the evidence indicates that gophers function only in the reworking of the mound material, not in the primary construction. The plausibility of the earlier glacial or periglacial theory has been increased by recent knowledge of permafrost and of the deposits made by combined water and ice in cold climates. The gopher theory, as it has been applied to the Mima mounds, contains internal disharmonies and ignores significant field evidence supporting the earlier idea.</span></p>","language":"English","publisher":"University of Chicago Press","doi":"10.1086/625998","usgsCitation":"Newcomb, R.C., 1952, Origin of the Mima Mounds, Thurston County region, Washington: Journal of Geology, v. 60, no. 5, p. 461-472, https://doi.org/10.1086/625998.","productDescription":"12 p.","startPage":"461","endPage":"472","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":622,"text":"Washington Water Science Center","active":true,"usgs":true}],"links":[{"id":321897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"60","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574eb5dae4b0ee97d51a83e6","contributors":{"authors":[{"text":"Newcomb, R. C.","contributorId":77907,"corporation":false,"usgs":true,"family":"Newcomb","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":630909,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}