{"pageNumber":"7059","pageRowStart":"176450","pageSize":"25","recordCount":185311,"records":[{"id":1000271,"text":"1000271 - 1953 - Technique for the application of a streamer-type fish tag","interactions":[],"lastModifiedDate":"2016-02-15T13:20:20","indexId":"1000271","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"Technique for the application of a streamer-type fish tag","docAbstract":"<p>Principal features of the technique are: attachment of the plastic tag by means of a nylon-thread loop prepared in advance of field work; use of a curved surgical needle with cutting edge and a split eye for application of the tag. The procedures for splitting the needle's eye and for applying the tag are described and illustrated by a series of photographs.</p>","language":"English","publisher":"Taylor & Francis","doi":"10.1577/1548-8659(1952)82[42:TFTAOA]2.0.CO;2","usgsCitation":"Joeris, L.S., 1953, Technique for the application of a streamer-type fish tag: Transactions of the American Fisheries Society, v. 82, no. 1, p. 42-47, https://doi.org/10.1577/1548-8659(1952)82[42:TFTAOA]2.0.CO;2.","productDescription":"6 p.","startPage":"42","endPage":"47","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133295,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"82","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c333","contributors":{"authors":[{"text":"Joeris, Leonard S.","contributorId":104430,"corporation":false,"usgs":true,"family":"Joeris","given":"Leonard","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":308319,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81350,"text":"81350 - 1953 - Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior","interactions":[],"lastModifiedDate":"2023-04-04T15:32:23.205022","indexId":"81350","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","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":"97","title":"Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Loeb, H.A., 1953, Sea lamprey spawning: Wisconsin and Minnesota streams of Lake Superior: Special Scientific Report - Fisheries 97, 36 p.","productDescription":"36 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198426,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101780,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/sea-lamprey-spawning-wisconsin-and-minnesota-streams-lake-superior"}],"country":"United States","state":"Minnesota, Wisconsin","otherGeospatial":"Lake Superior","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -90.2932442060535,\n              46.53801849599847\n            ],\n            [\n              -89.50894716491341,\n              48.02282639866175\n            ],\n            [\n              -91.15711887978152,\n              48.20234741183825\n            ],\n            [\n              -91.7057408913751,\n              48.15833881302618\n            ],\n            [\n              -92.48213634605524,\n              48.40319670473866\n            ],\n            [\n              -93.32900490043916,\n              46.61093869529458\n            ],\n            [\n              -93.55261656462791,\n              45.75903028146064\n            ],\n            [\n              -89.53197557881144,\n              45.82436185574744\n            ],\n            [\n              -90.2932442060535,\n              46.53801849599847\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc5e3","contributors":{"authors":[{"text":"Loeb, Howard A.","contributorId":63505,"corporation":false,"usgs":true,"family":"Loeb","given":"Howard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":295272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70194900,"text":"70194900 - 1953 - Biologists in the field of wildlife conservation","interactions":[],"lastModifiedDate":"2018-01-26T17:29:35","indexId":"70194900","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5610,"text":"AIBS Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Biologists in the field of wildlife conservation","docAbstract":"<p>We often hear comments such as \"people are funny\" and \"one meets the strangest people!\" Such sage remarks are not infrequently directed towards biologists, particularly those engaged in one of the many phases of wildlife conservation work. Bulletins of the \"love life\" of the raccoon or frog, and biologists who, for one reason or another, count the \"whiskers\" on a fox squirrel are held up for ridicule or dismissed with a shake of the head or a shrug of the shoulder and termed \"batty.\"</p>","language":"English","publisher":"Oxford University Press","doi":"10.2307/1292023","usgsCitation":"Leedy, D.L., 1953, Biologists in the field of wildlife conservation: AIBS Bulletin, v. 3, no. 2, p. 21-23, https://doi.org/10.2307/1292023.","productDescription":"3 p.","startPage":"21","endPage":"23","costCenters":[],"links":[{"id":350731,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5a6c4cb6e4b06e28e9cabb5a","contributors":{"authors":[{"text":"Leedy, Daniel L.","contributorId":37787,"corporation":false,"usgs":true,"family":"Leedy","given":"Daniel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":726045,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2507,"text":"wsp1136 - 1953 - Native and contaminated ground waters in the Long Beach-Santa Ana area, California","interactions":[],"lastModifiedDate":"2023-03-15T20:15:14.575742","indexId":"wsp1136","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1136","title":"Native and contaminated ground waters in the Long Beach-Santa Ana area, California","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1136","usgsCitation":"Piper, A., and Garrett, A.A., 1953, Native and contaminated ground waters in the Long Beach-Santa Ana area, California: U.S. Geological Survey Water Supply Paper 1136, Report: ix, 320 p.; 19 Plates: 20.00 x 15.50 inches or smaller, https://doi.org/10.3133/wsp1136.","productDescription":"Report: ix, 320 p.; 19 Plates: 20.00 x 15.50 inches or smaller","costCenters":[],"links":[{"id":28641,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28640,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28639,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28658,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1136/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":414254,"rank":22,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24224.htm","linkFileType":{"id":5,"text":"html"}},{"id":28657,"rank":21,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28656,"rank":20,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-18.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138888,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1136/report-thumb.jpg"},{"id":28655,"rank":19,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-17.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28654,"rank":18,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-16.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28653,"rank":17,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-15.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28652,"rank":16,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28651,"rank":15,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28650,"rank":14,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28649,"rank":13,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28648,"rank":12,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28647,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28646,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28645,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28644,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28643,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28642,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1136/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","city":"Long Beach, Santa Ana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -118.292,\n              33.602\n            ],\n            [\n              -117.698,\n              33.602\n            ],\n            [\n              -117.698,\n              34.031\n            ],\n            [\n              -118.292,\n              34.031\n            ],\n            [\n              -118.292,\n              33.602\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db698311","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":145310,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Garrett, A. A.","contributorId":44901,"corporation":false,"usgs":true,"family":"Garrett","given":"A.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":145309,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000150,"text":"1000150 - 1953 - Movement of tagged lake trout in Lake Superior, 1950-1952","interactions":[],"lastModifiedDate":"2012-02-02T00:04:34","indexId":"1000150","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3560,"text":"The Fisherman","active":true,"publicationSubtype":{"id":10}},"title":"Movement of tagged lake trout in Lake Superior, 1950-1952","docAbstract":"A total of 733 native lake trout was tagged at two widely separated localities in Lake Superior; subsequent recaptures numbered 155 fish (21.1 percent) during the year following marking.  In October 1950, 116 large lake trout (average total length, 27.3 inches) were tagged near Keweenaw Point, Michigan.  Fifteen (12.9 percent) were recovered during the first year at points as far west as the Gooseberry River, Minnesota (190 miles), north to the Slate Islands, Ontario (95 miles), and east to Grand Marais, Michigan (100 miles).  Nine fish (7.8 percent) were recovered during the second year after marking.  Returns from 617 tagged lake trout of smaller size released in the Apostle Island region of Wisconsin during the period June 12 to August 6, 1951, numbered 140 (22.7 percent) during the first year.  Of these fish, 90 percent were recaptured within a radius of 50 miles of the point of release.  Seventy-six percent were caught in Wisconsin, 14 percent in Minnesota, and 9 percent in Michigan waters.  The fish retaken in Michigan had moved 120 to 255 miles between the time of release and recapture, traveling as far east as Grand Marais.  Lake trout recaptured at distances of more than 50 miles from the tagging locality were of larger average size than marked fish caught within this radius.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"The Fisherman","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Eschmeyer, P.H., Daly, R., and Erkkila, L.F., 1953, Movement of tagged lake trout in Lake Superior, 1950-1952: The Fisherman, v. 21, no. 3.","productDescription":"p. 4, 11","startPage":"4, 11","numberOfPages":"-4","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":132929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"21","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4816","contributors":{"authors":[{"text":"Eschmeyer, Paul H.","contributorId":86719,"corporation":false,"usgs":true,"family":"Eschmeyer","given":"Paul","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":308148,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daly, Russell","contributorId":97857,"corporation":false,"usgs":true,"family":"Daly","given":"Russell","email":"","affiliations":[],"preferred":false,"id":308150,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Erkkila, Leo F.","contributorId":92197,"corporation":false,"usgs":true,"family":"Erkkila","given":"Leo","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":308149,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70189740,"text":"70189740 - 1953 - The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","interactions":[],"lastModifiedDate":"2017-07-22T13:01:12","indexId":"70189740","displayToPublicDate":"1953-01-01T00:00:00","publicationYear":"1953","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"seriesTitle":{"id":5468,"text":"Research Council of Israel Special Publication","active":false,"publicationSubtype":{"id":19}},"seriesNumber":"2","title":"The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions","docAbstract":"<p>The study of modern surface soils, and ancient weathering zones, which occur either buried or as surface relicts, has contributed materially to understanding the complex events of the glacial and post-glacial period both in glaciated areas and in regions not influenced by glaciation. Most work of this kind in the United States has been done by geologists.</p><p>Numerous Pleistocene geologists have noted weathered zones between sheets of glacial drift or loess in the middle western United States. These include Condra, et al<sup>5</sup>; Frye<sup>7</sup>; Frye and Leonard<sup>8</sup>; Kay and Pearce<sup>13</sup>; Leighton and MacClintock<sup>15</sup>; Leverett<sup>16</sup>,<sup>17</sup>,<sup>18</sup>; Lugn<sup>19</sup>; Peltier<sup>23</sup>; Schultz and Stout<sup>26</sup>; Schultz, et al<sup>27</sup>; and Simonson<sup>28</sup>. Kay and Pearce<sup>13</sup> interpreted the weathered zones between sheets of glacial drift as profiles of ancient soils which they referred to as gumbotil. Hseung, Marshall and Krusekopf<sup>10</sup> have recently questioned the pedogenic character of gumbotil, but have failed to offer a satisfactory alternative explanation. Thorp, and coworkers<sup>30</sup>, in a general review of buried soils, apparently consider gumbotil a product of ancient soil-forming processes.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Desert research: Proceedings (Research Council of Israel Special Publication No. 2)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Desert Research","conferenceDate":"May 7-14, 1952","conferenceLocation":"Jerusalem, Israel","language":"English","publisher":"Research Council of Israel","publisherLocation":"Jerusalem, Israel","usgsCitation":"Miller, J., and Leopold, L.B., 1953, The use of soils and paleosols for interpreting geomorphic and climatic history of arid regions, <i>in</i> Desert research: Proceedings (Research Council of Israel Special Publication No. 2), Jerusalem, Israel, May 7-14, 1952, p. 453-462.","productDescription":"10 p.","startPage":"453","endPage":"462","costCenters":[],"links":[{"id":344223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59746421e4b0ec1a48878495","contributors":{"authors":[{"text":"Miller, John","contributorId":190242,"corporation":false,"usgs":false,"family":"Miller","given":"John","email":"","affiliations":[],"preferred":false,"id":706049,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":706050,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70178712,"text":"70178712 - 1952 - Status of development of selected ground-water basins in Utah","interactions":[],"lastModifiedDate":"2016-12-09T11:28:53","indexId":"70178712","displayToPublicDate":"2016-11-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":4,"text":"Other Government Series"},"seriesTitle":{"id":294,"text":"Technical Publication","active":false,"publicationSubtype":{"id":4}},"seriesNumber":"7","title":"Status of development of selected ground-water basins in Utah","docAbstract":"<p>This technical publication consists essentially of abstracts of more detailed reports which have been published. Reference to existing reports are given in the text and in the bibliography, page 114.</p>","language":"English","publisher":"Utah Department of Natural Resources, Division of Water Rights","publisherLocation":"Salt Lake City, UT","usgsCitation":"Thomas, H.E., Nelson, W., Lofgren, B.E., and Butler, R., 1952, Status of development of selected ground-water basins in Utah: Technical Publication 7, 96 p.","productDescription":"96 p.","numberOfPages":"97","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":331494,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":331492,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/libview.exe?Modinfo=Viewpub&LIBNUM=20-4-170"},{"id":331493,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://waterrights.utah.gov/docSys/v920/w920/w9200086.pdf"}],"country":"United States","state":"Utah","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-111.046551,41.251716],[-111.046723,40.997959],[-110.750727,40.996847],[-110.715026,40.996347],[-110.539819,40.996346],[-110.500718,40.994746],[-110.375714,40.994947],[-110.250709,40.996089],[-110.237848,40.995427],[-110.125709,40.99655],[-110.121639,40.997101],[-110.048476,40.997555],[-110.006495,40.997815],[-110.000708,40.997352],[-109.999838,40.99733],[-109.97553,40.997912],[-109.855299,40.997614],[-109.854302,40.997661],[-109.715409,40.998191],[-109.713877,40.998266],[-109.676421,40.998395],[-109.534926,40.998143],[-109.500694,40.999127],[-109.250735,41.001009],[-109.231985,41.002059],[-109.173682,41.000859],[-109.050076,41.000659],[-109.048455,40.826081],[-109.049088,40.714562],[-109.048373,40.662602],[-109.048249,40.653601],[-109.048044,40.619231],[-109.050074,40.540358],[-109.049955,40.539901],[-109.050698,40.499963],[-109.050314,40.495092],[-109.050946,40.444368],[-109.050969,40.222662],[-109.050973,40.180849],[-109.050944,40.180712],[-109.050813,40.059579],[-109.050873,40.058915],[-109.050615,39.87497],[-109.05104,39.660472],[-109.051363,39.497674],[-109.050765,39.366677],[-109.051512,39.126095],[-109.052436,38.999985],[-109.053292,38.942878],[-109.053233,38.942467],[-109.053797,38.905284],[-109.053943,38.904414],[-109.054189,38.874984],[-109.057388,38.795456],[-109.059541,38.719888],[-109.060253,38.599328],[-109.059962,38.499987],[-109.060062,38.275489],[-109.054648,38.244921],[-109.041762,38.16469],[-109.041837,38.153022],[-109.04282,37.999301],[-109.042819,37.997068],[-109.043121,37.97426],[-109.041058,37.907236],[-109.041653,37.88117],[-109.041844,37.872788],[-109.041723,37.842051],[-109.041754,37.835826],[-109.041461,37.800105],[-109.042098,37.74999],[-109.041636,37.74021],[-109.04176,37.713182],[-109.041732,37.711214],[-109.042269,37.666067],[-109.042089,37.623795],[-109.042131,37.617662],[-109.041806,37.604171],[-109.041865,37.530726],[-109.041915,37.530653],[-109.043137,37.499992],[-109.043464,37.484711],[-109.04581,37.374993],[-109.046039,37.249993],[-109.045584,37.249351],[-109.045487,37.210844],[-109.045978,37.201831],[-109.045995,37.177279],[-109.045156,37.112064],[-109.045203,37.111958],[-109.045173,37.109464],[-109.045189,37.096271],[-109.044995,37.086429],[-109.045058,37.074661],[-109.045166,37.072742],[-109.045223,36.999084],[-109.181196,36.999271],[-109.233848,36.999266],[-109.246917,36.999346],[-109.26339,36.999263],[-109.268213,36.999242],[-109.270097,36.999266],[-109.378039,36.999135],[-109.381226,36.999148],[-109.495338,36.999105],[-109.625668,36.998308],[-109.875673,36.998504],[-110.000677,36.997968],[-110.000876,36.998502],[-110.021778,36.998602],[-110.47019,36.997997],[-110.490908,37.003566],[-110.50069,37.00426],[-110.599512,37.003448],[-110.625605,37.003416],[-110.62569,37.003721],[-110.75069,37.003197],[-111.066496,37.002389],[-111.133718,37.000779],[-111.254853,37.001077],[-111.278286,37.000465],[-111.405517,37.001497],[-111.405869,37.001481],[-111.412784,37.001478],[-112.35769,37.001025],[-112.368946,37.001125],[-112.534545,37.000684],[-112.538593,37.000674],[-112.540368,37.000669],[-112.545094,37.000734],[-112.558974,37.000692],[-112.609787,37.000753],[-112.899366,37.000319],[-112.966471,37.000219],[-113.965907,36.999976],[-113.965907,37.000025],[-114.0506,37.000396],[-114.051749,37.088434],[-114.051822,37.090976],[-114.052827,37.103961],[-114.051867,37.134292],[-114.052179,37.14711],[-114.051673,37.172368],[-114.051405,37.233854],[-114.051974,37.283848],[-114.051974,37.284511],[-114.0518,37.293044],[-114.0518,37.293548],[-114.051927,37.370459],[-114.051927,37.370734],[-114.051765,37.418083],[-114.052448,37.43144],[-114.052701,37.492014],[-114.052685,37.502513],[-114.052718,37.517264],[-114.052689,37.517859],[-114.052962,37.592783],[-114.052472,37.604776],[-114.051728,37.745997],[-114.051785,37.746249],[-114.05167,37.746958],[-114.051109,37.756276],[-114.049919,37.765586],[-114.048473,37.809861],[-114.049677,37.823645],[-114.049928,37.852508],[-114.049658,37.881368],[-114.050423,37.999961],[-114.049903,38.148601],[-114.050138,38.24996],[-114.049417,38.2647],[-114.05012,38.404536],[-114.050091,38.404673],[-114.050485,38.499955],[-114.049834,38.543784],[-114.049862,38.547764],[-114.050154,38.57292],[-114.049883,38.677365],[-114.049749,38.72921],[-114.049168,38.749951],[-114.049465,38.874949],[-114.048521,38.876197],[-114.048054,38.878693],[-114.049104,39.005509],[-114.047079,39.499943],[-114.047728,39.542742],[-114.047273,39.759413],[-114.047783,39.79416],[-114.047214,39.821024],[-114.047134,39.906037],[-114.046555,39.996899],[-114.046835,40.030131],[-114.046386,40.097896],[-114.046741,40.104231],[-114.046683,40.116931],[-114.046153,40.231971],[-114.046178,40.398313],[-114.045826,40.424823],[-114.045218,40.430282],[-114.045518,40.494474],[-114.045577,40.495801],[-114.045281,40.506586],[-114.043505,40.726292],[-114.043831,40.758666],[-114.043803,40.759205],[-114.043176,40.771675],[-114.042145,40.999926],[-114.041447,41.207752],[-114.042553,41.210923],[-114.041396,41.219958],[-114.040231,41.49169],[-114.040942,41.499921],[-114.040437,41.615377],[-114.039968,41.62492],[-114.039901,41.753781],[-114.041152,41.850595],[-114.041107,41.850573],[-114.039648,41.884816],[-114.041723,41.99372],[-113.993903,41.992698],[-113.893261,41.988057],[-113.822163,41.988479],[-113.796082,41.989104],[-113.76453,41.989459],[-113.500837,41.992799],[-113.496548,41.993305],[-113.431563,41.993799],[-113.40223,41.994161],[-113.396497,41.99425],[-113.357611,41.993859],[-113.340072,41.994747],[-113.250829,41.99561],[-113.249159,41.996203],[-113.000821,41.998223],[-113.00082,41.998223],[-112.979218,41.998263],[-112.909587,41.998791],[-112.882367,41.998922],[-112.880619,41.998921],[-112.833125,41.999345],[-112.833084,41.999305],[-112.788542,41.999681],[-112.709375,42.000309],[-112.648019,42.000307],[-112.450814,42.000953],[-112.450567,42.001092],[-112.38617,42.001126],[-112.264936,42.000991],[-112.239107,42.001217],[-112.192976,42.001167],[-112.173352,41.996568],[-112.163956,41.996708],[-112.109532,41.997598],[-112.01218,41.99835],[-111.915837,41.998519],[-111.915622,41.998496],[-111.876491,41.998528],[-111.750778,41.99933],[-111.507264,41.999518],[-111.471381,41.999739],[-111.425535,42.00084],[-111.420898,42.000793],[-111.415873,42.000748],[-111.046689,42.001567],[-111.045818,41.579845],[-111.045789,41.565571],[-111.046264,41.377731],[-111.0466,41.360692],[-111.046551,41.251716]]]},\"properties\":{\"name\":\"Utah\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58468aeee4b04fc80e5236d9","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":654900,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, W.B.","contributorId":30282,"corporation":false,"usgs":true,"family":"Nelson","given":"W.B.","email":"","affiliations":[],"preferred":false,"id":654901,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lofgren, B. E.","contributorId":42579,"corporation":false,"usgs":true,"family":"Lofgren","given":"B.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":654902,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, R.G.","contributorId":60706,"corporation":false,"usgs":true,"family":"Butler","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":654903,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70160626,"text":"70160626 - 1952 -  An interim report on gill disease","interactions":[],"lastModifiedDate":"2016-01-04T09:20:00","indexId":"70160626","displayToPublicDate":"2015-12-28T00:00:00","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":" An interim report on gill disease","docAbstract":"<p><span><strong>GILL DISEASE among fish, a disease which is characterized by a proliferation of the gill epithelium, has been attributed to a number of different causes. Generally, there are two recognized types: the eastern or bacterial type, in which long filamentous bacteria can always be demonstrated; and the western type, in which, by definition, bacteria cannot be demonstrated.</strong></span></p>","language":"English","publisher":"Department of Commerce, Bureau of Fisheries","doi":"10.1577/1548-8640(1952)14[10:AIROGD]2.0.CO;2","usgsCitation":"Rucker, R., Johnson, H., and Kaydas, G., 1952,  An interim report on gill disease: Progressive Fish-Culturist, v. 14, no. 1, p. 10-14, https://doi.org/10.1577/1548-8640(1952)14[10:AIROGD]2.0.CO;2.","productDescription":"5 p.","startPage":"10","endPage":"14","numberOfPages":"5","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":654,"text":"Western Fisheries Research Center","active":true,"usgs":true}],"links":[{"id":312873,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"14","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56825d27e4b0a04ef4925af1","contributors":{"authors":[{"text":"Rucker, R.R.","contributorId":104000,"corporation":false,"usgs":true,"family":"Rucker","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":583372,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Johnson, H.E.","contributorId":56757,"corporation":false,"usgs":true,"family":"Johnson","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":583373,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Kaydas, G.M.","contributorId":150875,"corporation":false,"usgs":false,"family":"Kaydas","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":583374,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70175968,"text":"70175968 - 1952 - Geology and ground-water resources of Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum","interactions":[],"lastModifiedDate":"2016-08-23T09:02:48","indexId":"70175968","displayToPublicDate":"2015-10-20T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Berry, D., and Durum, W.H., 1952, Geology and ground-water resources of Lincoln County, Kansas, with a chapter on The chemical quality of ground water, by W.H. Durum: Kansas Geological Survey Bulletin, v. 95, 96 p. .","productDescription":"96 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327430,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327429,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"95","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dbe4b03fd6b7df2cd9","contributors":{"authors":[{"text":"Berry, D.W.","contributorId":24842,"corporation":false,"usgs":true,"family":"Berry","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":646719,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Durum, W. H.","contributorId":78311,"corporation":false,"usgs":true,"family":"Durum","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":646720,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175967,"text":"70175967 - 1952 - Geology and ground-water resources of the Kansas River Valley between Lawrence and Topeka, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T09:00:14","indexId":"70175967","displayToPublicDate":"2015-08-12T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of the Kansas River Valley between Lawrence and Topeka, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Davis, S., and Carlson, W.A., 1952, Geology and ground-water resources of the Kansas River Valley between Lawrence and Topeka, Kansas: Kansas Geological Survey Bulletin, v. 96, no. 5, p. 201-276.","productDescription":"75 p. ","startPage":"201","endPage":"276","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327424,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327423,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"96","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dce4b03fd6b7df2ced","contributors":{"authors":[{"text":"Davis, S.N.","contributorId":51918,"corporation":false,"usgs":true,"family":"Davis","given":"S.N.","email":"","affiliations":[],"preferred":false,"id":646717,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlson, W. A.","contributorId":173967,"corporation":false,"usgs":false,"family":"Carlson","given":"W.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":646718,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70159230,"text":"tei138 - 1952 - Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado","interactions":[],"lastModifiedDate":"2015-10-30T10:48:25","indexId":"tei138","displayToPublicDate":"2015-07-06T08:00:00","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":"138","title":"Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado","docAbstract":"<p>The Quartz Creek pegmatite district includes an area about 29 square miles in the vicinity of Quartz Creek in Gunnison County,. Colo. This area contains 1,803 pegmatites that are intruded into pre-Cambrian rocks.</p>\n<p>The rocks exposed in the district range in age from pre-Cambrian to Recent. The oldest pre-Cambrian rocks are chiefly quartzites interbedded with a few arkoses and conglomerates. These rocks are surrounded by more abundant hornblende gneiss and tonalite. A small body of biotite tonalite was intruded and two thin layers of dacitic pillow lava were extruded into this series. The hornblende gneiss and tonalite have the same composition and differ only in texture. The older material (hornblende gneiss) has a well-marked lineation, whereas the younger (tonalite) is equigranular. Subsequently, a large body of quartz monzonite was intruded along the northern boundary of the mapped area. Later, coarse-grained granite was intruded into the southern part of the area. Dikes of fine-grained granite cut the coarse-grained variety.&nbsp; The last period of intrusive activity in pre-Cambrian time is marked by a large number of pegmatites.</p>\n<p>The pre-Cambrian rocks were tilted and eroded, and the flatlying&nbsp; Jurassic Morrison formation was deposited on the irregular surface. This formation is conformably overlain by the Cretaceous Dakota sandstone. Faulting produced a vertical offset of 410 feet in the Mesozoic sediments along the only large fault in the area. At the end of Mesozoic time there was another period of erosion. Tertiary (?) tuff is exposed in small, scattered areas in the southern part of the district. It overlies both the Dakota sandstone and pre-Cambrian formations. Glacial till occurs along the edges of Quartz Creek and Wood Gulch. Quaternary alluvium fills the valley bottoms.</p>\n<p>&nbsp;Although the composition of the country rock has little effect on the shape of the pegmatites, the foliation imposed on this rock has a localizing effect and in part controls the ultimate shape of pegmatites.&nbsp; &nbsp;Zoned and related internal structures are not well developed in the pegmatites of this region. &nbsp;Many of the pegmatites are homogeneous and those that are zoned usually contain a large wall zone and small discontinuous cores. In addition to the more common homogeneous and zoned pegmatites, 7 percent of the pegmatites show a layered structure of textural and mineralogical units not repeated on the opposite side of the pegmatite. Other internal structural units include pegmatites which vary in composition along strike, multiple or &ldquo;line-rock pegmatites&rdquo; and fracture fillings.</p>\n<p>The mineralogy of the pegmatites is described in detail. &nbsp;Specific attention was given to most of the 27 observed minerals. A study of the index of refraction of 439 specimens of plagioclase showed that the variation from zone to zone and layer to layer is minor and that there is no systematic variation in respect to the entire district. No correlation could be found between the refractive index of plagioclase in the pegmatites and the type country rock, or the presence of various accessory minerals.</p>\n<p>Index of refraction determinations on 95 specimens of muscovite showed no constant variation from wall zone to core or from layer to layer. &nbsp;Curved muscovite has identical optical properties with the flat variety. The index of refraction was determined for 189 beryl specimens. The beryl in the pegmatites containing only a wall zone and a core showed no difference between zones, but in pegmatites that have intermediate zones, the indices of refraction of the beryl showed an inward increase in the alkali content from the contact. Beryl occurs with almost all of the pegmatite minerals and is not restricted in its mineral associations.</p>\n<p>Tourmaline, except the black variety, is associated with lepidolite. Dark green and blue tourmaline is found in the outer zones of pegmatites containing lepidolite, and the pink and light green varieties are found in direct contact with lepidolite.</p>\n<p>Lepidolite occurs in aggregates of fine grains, in flat plates, and in curved plates; the three varieties are optically identical. The lighter-colored varieties have higher indices of refraction and contain less lithia than the darker varieties.</p>\n<p>In addition, the occurrence of the following minerals is described in detail: perthite, quartz, martite, biotite, garnet, columbite-tantalite, monazite, microlite, topaz, gahnite, allanite, and an unidentified mineral.</p>\n<p>The lack of alteration in the wall rocks adjacent to the pegmatites is interpreted as indicating that the original pegmatite&nbsp; magma did not have an excess of materials such as B, OH-, and P that are needed to form alteration minerals. Because of their low concentration, the above materials were available only in the pegmatitic magma during its crystallization. Pegmatites that contain the rare minerals such as beryl, tourmaline, curved muscovite, biotite, magnetite, monazite, columbite-tantalite, cleavelandite, topaz, lepidolite, and microlite show a grouping in clusters within the district.</p>\n<p>Beryl-bearing pegmatites occur most abundantly in hornblende gneiss and are only rarely found in either granite or quartz monzonite. The types of minerals that form in a pegmatite appear to be determined by the character of the material segregated from the original magma and the period in which it segregated. The elements escape at one period and may be from only-a specific pocket in the magma. These liquids tend to form groups of pegmatites in which the later bodies contain a high proportion of volatiles.</p>\n<p>&nbsp;</p>\n<p>&nbsp;</p>\n<p>Inferred reserves of the district are estimated for beryl, scrap mica, both hand-cobbing and milling feldspar, lepidolite, columbite-tantalite, topaz, monazite, and microlite. No sheet mica was found. Reserves are small and transportation costs are high so substantial production of low-priced feldspar and scrap mica will depend on the adoption of economica milling techniques for recovering the large quantities of feldspar available.&nbsp; Beryl is irregularly distributed and its recovery as a byproduct will depend on the establishment of a stable market for feldspar and scrap mica.&nbsp; Lepidolite reserves are small low grade.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei138","usgsCitation":"Staatz, M.H., and Trites, A., 1952, Geology of the Quartz Creek Pegmatite District, Gunnison County Colorado: U.S. Geological Survey Trace Elements Investigations 138, Report: 288 p.; 11 Plates: 29.61 x 46.75 inches or smaller, https://doi.org/10.3133/tei138.","productDescription":"Report: 288 p.; 11 Plates: 29.61 x 46.75 inches or smaller","numberOfPages":"297","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":310072,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei138.PNG"},{"id":310797,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/138/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":310796,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/138/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":310798,"rank":4,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-9.pdf","text":"Figure 9","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 9"},{"id":310799,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-16.pdf","text":"Figure 16","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 16"},{"id":310800,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-17.pdf","text":"Figure 17","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 17"},{"id":310801,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-18.pdf","text":"Figure 18","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 18"},{"id":310802,"rank":8,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-19.pdf","text":"Figure 19","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 19"},{"id":310803,"rank":9,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-20.pdf","text":"Figure 20","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 20"},{"id":310804,"rank":10,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-21.pdf","text":"Figure 21","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 21"},{"id":310805,"rank":11,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-22.pdf","text":"Figure 22","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 22"},{"id":310806,"rank":12,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-27.pdf","text":"Figure 27","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 27"},{"id":310807,"rank":13,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/tei/138/figure-28.pdf","text":"Figure 28","linkFileType":{"id":1,"text":"pdf"},"description":"Figure 28"}],"country":"United States","state":"Colorado","county":"Gunnison County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-107.3944,39.2565],[-107.39,39.2503],[-107.3785,39.2471],[-107.3711,39.2388],[-107.3761,39.2368],[-107.3793,39.2311],[-107.3767,39.2199],[-107.3806,39.2102],[-107.3766,39.1985],[-107.3607,39.186],[-107.3561,39.1787],[-107.3531,39.1729],[-107.3432,39.1685],[-107.3325,39.1659],[-107.3185,39.1653],[-107.3076,39.1572],[-107.2959,39.1542],[-107.2936,39.1448],[-107.2864,39.1369],[-107.2824,39.1187],[-107.2486,39.1188],[-107.2174,39.1188],[-107.1864,39.1187],[-107.1542,39.1189],[-107.1225,39.1189],[-107.0923,39.1188],[-107.066,39.1188],[-107.0601,39.1118],[-107.0528,39.1105],[-107.0405,39.0989],[-107.0399,39.0975],[-107.0364,39.0948],[-107.0194,39.0894],[-107.0116,39.082],[-106.9971,39.0695],[-106.9886,39.0708],[-106.9866,39.0665],[-106.9863,39.0625],[-106.9907,39.06],[-106.9897,39.052],[-106.9969,39.049],[-107.0016,39.0424],[-106.9959,39.0338],[-106.9878,39.0305],[-106.9643,39.0296],[-106.9647,39.0174],[-106.9446,39.0145],[-106.9345,39.0058],[-106.9174,38.999],[-106.9099,39.0001],[-106.9082,38.9925],[-106.9002,38.9925],[-106.8927,38.9894],[-106.8839,38.9904],[-106.8779,38.9943],[-106.8772,39.0064],[-106.8606,39.0093],[-106.8564,38.9989],[-106.8455,38.9859],[-106.8273,38.9774],[-106.8072,38.979],[-106.8001,38.9797],[-106.7966,38.9841],[-106.7879,38.9843],[-106.7835,38.9876],[-106.7821,38.9995],[-106.7746,39.006],[-106.7687,39.0084],[-106.7513,39.0257],[-106.744,39.0269],[-106.7485,39.0419],[-106.7403,39.046],[-106.7227,39.045],[-106.7105,39.0478],[-106.7078,39.0536],[-106.7029,39.0559],[-106.6931,39.0552],[-106.6846,39.045],[-106.6741,39.0457],[-106.6644,39.0417],[-106.6553,39.0446],[-106.6467,39.0334],[-106.6498,39.0261],[-106.6483,39.0218],[-106.6383,39.0194],[-106.6375,39.0144],[-106.6145,39.0001],[-106.6129,38.9955],[-106.5989,38.998],[-106.5949,38.991],[-106.5798,38.9918],[-106.5773,38.9905],[-106.5684,38.9943],[-106.5624,38.9967],[-106.5592,38.9986],[-106.5538,38.9986],[-106.551,38.9915],[-106.5414,38.9879],[-106.5338,38.9822],[-106.5302,38.9782],[-106.5255,38.9737],[-106.5221,38.9674],[-106.5273,38.9609],[-106.5264,38.9558],[-106.5193,38.953],[-106.5138,38.9479],[-106.5046,38.9448],[-106.5044,38.9374],[-106.4925,38.9309],[-106.488,38.9254],[-106.4791,38.918],[-106.4668,38.9123],[-106.46,38.9104],[-106.4501,38.9124],[-106.4393,38.9156],[-106.4348,38.9148],[-106.4298,38.9243],[-106.4201,38.9278],[-106.4171,38.9272],[-106.4154,38.9188],[-106.4113,38.9152],[-106.4053,38.9143],[-106.402,38.9104],[-106.3932,38.9118],[-106.3919,38.9185],[-106.3798,38.9253],[-106.3757,38.9226],[-106.3752,38.9113],[-106.3742,38.9062],[-106.367,38.9066],[-106.3613,38.9119],[-106.3556,38.9127],[-106.3442,38.9069],[-106.3365,38.9086],[-106.3316,38.9114],[-106.3255,38.9108],[-106.3244,38.9097],[-106.3226,38.8993],[-106.3196,38.8944],[-106.325,38.8892],[-106.3252,38.8839],[-106.3348,38.879],[-106.3357,38.8743],[-106.3356,38.8714],[-106.3447,38.8678],[-106.3487,38.8633],[-106.348,38.8548],[-106.3526,38.8559],[-106.3647,38.8531],[-106.3641,38.8442],[-106.3683,38.8414],[-106.3695,38.8384],[-106.3776,38.8359],[-106.3823,38.8311],[-106.3824,38.8245],[-106.3902,38.8225],[-106.3956,38.8226],[-106.3994,38.8259],[-106.406,38.8292],[-106.4152,38.8237],[-106.4142,38.8145],[-106.4178,38.8122],[-106.4184,38.8057],[-106.418,38.8024],[-106.4133,38.7951],[-106.412,38.7901],[-106.4121,38.79],[-106.416,38.7877],[-106.4139,38.7744],[-106.4166,38.7696],[-106.4179,38.7656],[-106.4135,38.7582],[-106.4146,38.7565],[-106.4187,38.751],[-106.4167,38.7408],[-106.4196,38.7383],[-106.416,38.7284],[-106.4169,38.7254],[-106.4229,38.7205],[-106.4244,38.7099],[-106.4311,38.7085],[-106.4436,38.7074],[-106.4492,38.7023],[-106.4523,38.6982],[-106.4468,38.6914],[-106.4457,38.6908],[-106.4451,38.6899],[-106.4415,38.6862],[-106.4368,38.6822],[-106.435,38.6799],[-106.4332,38.6718],[-106.4314,38.6677],[-106.4297,38.6654],[-106.4285,38.6569],[-106.4292,38.6516],[-106.4259,38.6504],[-106.4242,38.6482],[-106.4201,38.6451],[-106.4174,38.6446],[-106.409,38.6476],[-106.4064,38.6474],[-106.403,38.6468],[-106.4003,38.6444],[-106.4007,38.6425],[-106.4007,38.6399],[-106.3965,38.6397],[-106.3892,38.6407],[-106.3838,38.6386],[-106.3785,38.6385],[-106.3825,38.6336],[-106.3846,38.632],[-106.3849,38.6261],[-106.3793,38.62],[-106.375,38.6209],[-106.368,38.6185],[-106.3631,38.614],[-106.3632,38.6108],[-106.3627,38.6095],[-106.3627,38.6058],[-106.3621,38.6027],[-106.3603,38.5995],[-106.3591,38.5977],[-106.3586,38.5941],[-106.3568,38.5904],[-106.355,38.5877],[-106.3502,38.58],[-106.349,38.5764],[-106.3467,38.5732],[-106.3443,38.571],[-106.3437,38.5687],[-106.3431,38.566],[-106.3437,38.5624],[-106.3466,38.5587],[-106.3484,38.5542],[-106.3507,38.5497],[-106.353,38.5465],[-106.3542,38.5424],[-106.3542,38.5392],[-106.3541,38.5361],[-106.3506,38.5293],[-106.3453,38.5266],[-106.3423,38.5239],[-106.3411,38.5198],[-106.3423,38.5148],[-106.3446,38.5107],[-106.3452,38.508],[-106.3434,38.5048],[-106.3387,38.5003],[-106.3334,38.4981],[-106.3322,38.4962],[-106.3304,38.494],[-106.3292,38.4931],[-106.3245,38.4949],[-106.321,38.4958],[-106.3175,38.4954],[-106.3134,38.4949],[-106.3104,38.4931],[-106.3075,38.4881],[-106.3039,38.4795],[-106.3015,38.4773],[-106.2986,38.4755],[-106.2933,38.4741],[-106.2904,38.4723],[-106.2892,38.4701],[-106.2874,38.4637],[-106.2862,38.4587],[-106.2832,38.4551],[-106.2819,38.4543],[-106.275,38.4543],[-106.2715,38.4552],[-106.2711,38.45],[-106.2714,38.4482],[-106.2712,38.446],[-106.2669,38.4432],[-106.2656,38.442],[-106.2614,38.4402],[-106.2562,38.4402],[-106.2515,38.4402],[-106.2485,38.4398],[-106.2467,38.4389],[-106.245,38.438],[-106.2444,38.4371],[-106.2438,38.4353],[-106.245,38.4325],[-106.245,38.4298],[-106.2455,38.4266],[-106.2449,38.4212],[-106.5045,38.4204],[-106.5134,38.4204],[-106.5416,38.4203],[-106.5603,38.4202],[-106.615,38.4199],[-106.6338,38.4198],[-106.6714,38.4196],[-106.7841,38.4185],[-106.8247,38.4182],[-106.9979,38.4165],[-106.9979,38.3263],[-106.9975,38.2973],[-106.9976,38.2184],[-106.998,38.2039],[-106.9978,38.1468],[-107.0458,38.1464],[-107.1043,38.1464],[-107.2617,38.1457],[-107.2986,38.1454],[-107.5192,38.1451],[-107.5666,38.1445],[-107.5638,38.1495],[-107.5621,38.1545],[-107.5617,38.1595],[-107.5629,38.1636],[-107.5659,38.1672],[-107.5665,38.1694],[-107.5679,38.1794],[-107.5698,38.1866],[-107.5736,38.197],[-107.5755,38.2038],[-107.5774,38.2137],[-107.5777,38.2255],[-107.5789,38.2286],[-107.5844,38.2372],[-107.5862,38.2412],[-107.5881,38.2476],[-107.5894,38.2512],[-107.5918,38.253],[-107.6024,38.256],[-107.6077,38.2582],[-107.6101,38.26],[-107.6113,38.2627],[-107.618,38.2739],[-107.6265,38.2888],[-107.6333,38.3005],[-107.5213,38.301],[-107.4995,38.3008],[-107.4995,38.3248],[-107.4997,38.3656],[-107.4993,38.4033],[-107.4994,38.4096],[-107.4991,38.4246],[-107.4995,38.4404],[-107.4989,38.4445],[-107.4991,38.4504],[-107.4991,38.4531],[-107.4989,38.4717],[-107.499,38.5356],[-107.4992,38.5737],[-107.4989,38.6172],[-107.4992,38.6304],[-107.5011,38.6657],[-107.5011,38.6942],[-107.5011,38.7804],[-107.5012,38.7822],[-107.5005,38.8384],[-107.5,38.8683],[-107.5003,38.8828],[-107.4994,38.9241],[-107.4994,38.9263],[-107.4994,38.9544],[-107.4993,39.0351],[-107.5002,39.1389],[-107.5001,39.2201],[-107.4884,39.2252],[-107.4854,39.2275],[-107.4837,39.2298],[-107.4825,39.2307],[-107.4808,39.2316],[-107.4784,39.2317],[-107.476,39.2303],[-107.4742,39.229],[-107.4706,39.2272],[-107.4682,39.2263],[-107.4652,39.2268],[-107.4617,39.2269],[-107.4551,39.2283],[-107.4445,39.2312],[-107.4363,39.2344],[-107.4339,39.2358],[-107.4298,39.2395],[-107.4275,39.2427],[-107.4264,39.245],[-107.4258,39.2477],[-107.4259,39.2531],[-107.4248,39.2545],[-107.423,39.255],[-107.42,39.255],[-107.4123,39.2542],[-107.4004,39.253],[-107.3944,39.2565]]]},\"properties\":{\"name\":\"Gunnison\",\"state\":\"CO\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"56261470e4b0fb9a11dd762d","contributors":{"authors":[{"text":"Staatz, Mortimer H.","contributorId":55494,"corporation":false,"usgs":true,"family":"Staatz","given":"Mortimer","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":577873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trites, A.F.","contributorId":25196,"corporation":false,"usgs":true,"family":"Trites","given":"A.F.","affiliations":[],"preferred":false,"id":577874,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175965,"text":"70175965 - 1952 - Geology and ground-water resources of the North Fork Solomon River in Mitchell, Osborne, Smith, and Phillips Counties, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T08:53:54","indexId":"70175965","displayToPublicDate":"2015-06-25T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of the North Fork Solomon River in Mitchell, Osborne, Smith, and Phillips Counties, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Leonard, A., 1952, Geology and ground-water resources of the North Fork Solomon River in Mitchell, Osborne, Smith, and Phillips Counties, Kansas: Kansas Geological Survey Bulletin, v. 98, 150 p. .","productDescription":"150 p. ","costCenters":[],"links":[{"id":327403,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327402,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"98","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73dce4b03fd6b7df2cef","contributors":{"authors":[{"text":"Leonard, A.R.","contributorId":101669,"corporation":false,"usgs":true,"family":"Leonard","given":"A.R.","email":"","affiliations":[],"preferred":false,"id":646715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70159220,"text":"tei155 - 1952 - Geology and pegmatites of part of the Fourmile area, Custer County, South Dakota","interactions":[],"lastModifiedDate":"2015-10-30T11:03:16","indexId":"tei155","displayToPublicDate":"2015-06-01T05:15:00","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":"155","title":"Geology and pegmatites of part of the Fourmile area, Custer County, South Dakota","docAbstract":"<p>The Fourmile area, Custer County, S. Dak., is in pre-Cambrian metamorphic rocks that surround the granitic core of the Black Hills. The area is on the upright limb of an overturned anticline that plunges about 30&deg; S. 10&deg; E.</p>\n<p>Three new formations of metamorphic rocks are described that have a total thickness of at least 7, 700 feet. The oldest of these formations, the Ruby Creek quartz-mica schist, is more than 6,500 feet thick. The overlying Raver formation, about 200 feet thick, is composed of thin beds of amphibolite and hornblende schist, lime-silicate rock, cordierite-biotite schist, microcline-biotite schist, and other types of rock. The youngest formation, the Ruddock quartz-mica-feldspar schist, is more than 1,000 feet thick. The presence of kyanite, staurolite, cordierite, and sillimanite in the rocks indicate that they have been subjected to high-grade metamorphism.</p>\n<p>About 420 pegmatites were mapped in the Ruby Creek quartz-mica--schist and the Ruddock quartz-mica-feldspar schist. A few thin pegmatites in the Raver formation were not mapped. Most of the pegmatites are concordant with the schistosity and relict (?) bedding of the enclosing metamorphic rocks. They are as much as 250 feet thick and range from 10 to 2,600 feet in length. Nine pegmatites are zoned and are classified as heterogeneous pegmatites. The remainder are homogeneous pegmatites that are poorly zoned. The major constituents of the pegmatites are plagioclase, quartz perthite, and muscovite. The accessory minerals are tourmaline, apatite, garnet, and biotite. Beryl was observed in 15 of the pegmatites.</p>\n<p>The heterogeneous pegmatites contain commercial deposits of potash feldspar, mica (sheet and scrap), and beryl.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei155","usgsCitation":"Lang, A., and Redden, J., 1952, Geology and pegmatites of part of the Fourmile area, Custer County, South Dakota: U.S. Geological Survey Trace Elements Investigations 155, Report: 60 p.; 4 Plates: 19.73 x 23.88 inches or smaller, https://doi.org/10.3133/tei155.","productDescription":"Report: 60 p.; 4 Plates: 19.73 x 23.88 inches or smaller","numberOfPages":"61","onlineOnly":"N","additionalOnlineFiles":"Y","costCenters":[],"links":[{"id":310060,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/tei155.jpg"},{"id":310808,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/155/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":310809,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/155/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":310810,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/155/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":310811,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/155/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":310812,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/155/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"}],"country":"United States","state":"South Dakota","county":"Custer County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-102.8114,43.6852],[-102.8137,43.6792],[-102.818,43.675],[-102.8167,43.6719],[-102.8152,43.6664],[-102.8282,43.6589],[-102.8352,43.6588],[-102.8436,43.665],[-102.8481,43.6649],[-102.8572,43.6557],[-102.863,43.6583],[-102.8646,43.6669],[-102.8773,43.6689],[-102.8812,43.6702],[-102.8863,43.6711],[-102.8964,43.6722],[-102.9072,43.6725],[-102.9115,43.6688],[-102.9107,43.6642],[-102.9164,43.6641],[-102.9194,43.6595],[-102.918,43.6555],[-102.9223,43.654],[-102.9241,43.6494],[-102.9246,43.6471],[-102.9214,43.6454],[-102.92,43.6422],[-102.9243,43.6385],[-102.9275,43.6375],[-102.9323,43.6315],[-102.9314,43.6252],[-102.9325,43.6201],[-102.9356,43.6178],[-102.9412,43.6163],[-102.9526,43.6143],[-102.9563,43.6138],[-102.9626,43.6123],[-102.9664,43.6136],[-102.9709,43.6158],[-102.9822,43.6115],[-102.9854,43.6128],[-102.9922,43.6104],[-103.0016,43.607],[-103.0016,43.5897],[-103.0013,43.4763],[-103.0675,43.476],[-103.1496,43.4762],[-103.4594,43.4764],[-103.484,43.4763],[-103.5017,43.4763],[-103.6311,43.4765],[-103.6551,43.4764],[-103.6936,43.4764],[-103.8627,43.4763],[-103.8741,43.4769],[-103.9315,43.4768],[-103.9537,43.4771],[-104.0539,43.4772],[-104.0541,43.4827],[-104.0542,43.5037],[-104.0546,43.5674],[-104.0546,43.5742],[-104.0546,43.6466],[-104.0547,43.6713],[-104.0548,43.7132],[-104.0549,43.7251],[-104.0549,43.7377],[-104.0547,43.757],[-104.0546,43.7669],[-104.0547,43.8012],[-104.0548,43.8509],[-104.0548,43.853],[-103.5743,43.8564],[-103.455,43.8568],[-103.4239,43.8571],[-103.3407,43.8561],[-102.9834,43.8538],[-102.9612,43.8542],[-102.8749,43.8544],[-102.7473,43.8543],[-102.7086,43.8545],[-102.6877,43.8544],[-102.6876,43.8517],[-102.6918,43.8452],[-102.6886,43.8426],[-102.6886,43.8412],[-102.6885,43.8403],[-102.6884,43.838],[-102.6902,43.8343],[-102.692,43.8311],[-102.6951,43.8283],[-102.6973,43.8187],[-102.6985,43.8137],[-102.6945,43.8101],[-102.6957,43.8083],[-102.6963,43.8069],[-102.6988,43.8041],[-102.6987,43.8014],[-102.6966,43.7969],[-102.6972,43.795],[-102.7055,43.7958],[-102.7073,43.7926],[-102.7078,43.7903],[-102.7134,43.7857],[-102.7177,43.7815],[-102.7232,43.7764],[-102.7308,43.7735],[-102.7357,43.7712],[-102.7357,43.7693],[-102.735,43.7666],[-102.7348,43.763],[-102.736,43.7611],[-102.7385,43.7588],[-102.7404,43.7583],[-102.7435,43.7574],[-102.7491,43.7532],[-102.7546,43.7481],[-102.7582,43.7425],[-102.7638,43.7397],[-102.7751,43.7363],[-102.7718,43.7323],[-102.7718,43.7296],[-102.7767,43.7254],[-102.7779,43.7231],[-102.7791,43.7208],[-102.7841,43.7207],[-102.7898,43.7206],[-102.7972,43.7132],[-102.7984,43.7118],[-102.8033,43.7058],[-102.8005,43.7008],[-102.8011,43.6985],[-102.8061,43.6953],[-102.8098,43.6929],[-102.8129,43.691],[-102.8153,43.6878],[-102.8114,43.6852]]]},\"properties\":{\"name\":\"Custer\",\"state\":\"SD\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5626146ee4b0fb9a11dd7629","contributors":{"authors":[{"text":"Lang, A.J. Jr.","contributorId":84844,"corporation":false,"usgs":true,"family":"Lang","given":"A.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":577859,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redden, J. A.","contributorId":62215,"corporation":false,"usgs":true,"family":"Redden","given":"J. A.","affiliations":[],"preferred":false,"id":577860,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13965,"text":"ofr172 - 1952 - Ground water in the Gila River Basin and adjacent areas, Arizona: a summary","interactions":[],"lastModifiedDate":"2018-08-29T08:13:56","indexId":"ofr172","displayToPublicDate":"2013-08-04T14:49:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"172","title":"Ground water in the Gila River Basin and adjacent areas, Arizona: a summary","docAbstract":"<p>This report is a resume' of the principal facts collected by the Geological Survey in the period 1890-1952 about the ground-water resources of the Gila River basin and certain other areas in Arizona. Since 1939 the Geological Survey has been making ground-water investigations on a continuing basis in cooperation with the State of Arizona. Since 1940 the cooperating agency has been the State Land Department.</p><p>The occurrence of ground water in fifteen areas that form a part of the Gila River drainage basin is described in this report. The areas are denoted by the name of a town or geographic feature, and are as follows: Duncan, Safford, San Simon, Upper San Pedro, Lower San Pedro, Aravaipa Creek, Upper Santa Cruz, Lower Santa Cruz, Salt River Valley, Rainbow ValleyWaterman Wash, McMullen Valley, Harquahala Plain, Gila Bend, Palomas Plain, and Wellton-Mohawk. Data also are presented for several areas not in the Gila River system, including Ranegras Plain and the Willcox and Douglas basins. A summary of the data is given following the ground-water discussion in each area.</p><p>A series of maps accompany the report, including an index map and maps of the principal areas of ground-water development. The mar,z, show the geology, the location of most of the irrigation wells and irrigated lands, and, where data were available, contours of the water table, depth to the water table, and changes in its position over a period of years.</p><p>Ground water occurs in the region primarily in alluvial fill consisting of gravel, sand, silt, and clay which was deposited in structural troughs between mountain ranges. Ground water stored in these alluvial basins is derived from many sources. The principal sources are infiltration from runoff along the mountain fronts and seepage from irrigation water applied to cultivated lands.</p><p>Of great interest in Arizona at the present time is the rate of depletion of ground-water reserves by withdrawals from storage. Use of ground water in Arizona increased by more than 50 percent in the 6-year period 1'46-51, from 2,400,000 acre-feet in 1946 to 3,750,000 acre-feet in 1951. The areas of greatest withdrawal are in Pinal and Maricopa Counties, in the southcentral part of the State. Maps and hydrographs accompanying this report show that the water table is declining in the heavily pumped areas, indicating that ground water is being withdrawn in excess of replenishment. The rate of decline has been as much as 10 feet per year in the most intensively pumped areas, and has been greatest during the past few years.</p><p>In an effort to compensate for decreased well yields resulting from the decline of the water table in some areas, many deep wells have been drilled within the past few years. The deep aquifers do not represent a new source of water; their water is a part of the common supply of the structural basins in which they lie. The aquifers tapped by these deep wells generally yield less water per foot of drawdown than the shallower aquifers. The water in the deeper aquifers is variable in quality, ranging from water too high in dissolved solids to be usable for irrigation to water lower in concentration than that in the overlying aquifers.</p><p>The quality of the ground waters in most of the region is considered suitable for irrigation. In local areas, however, the ground waters are naturally unsuitable for irrigation and, in other areas, the concentration of dissolved solids has increased sufficiently to make the waters harmful to some crops. The problem of salt balance is becoming increasingly important, not only in the Salt River Valley area, but also in other parts of the Gila River Basin. A discussion of the salt-balance problem is given in Part II of this report.&nbsp;</p><p>It should be emphasized that ground waters in each of the individual areas in the Gila River drainage system are interrelated with ground waters in adjacent areas upstream and downstream. The connection is tenuous between some areas, but in central Arizona the ground waters in the different areas are closely related. Although subsurface barriers to ground-water movement exist in places, they are not everywhere fully effective.</p><p>The ground-water--surface-water interrelationship is important in some areas. Those basins occupied by perennial streams, or by streams having large influent seepage losses, have not shown large, perennial declines of water levels in wells. Effluent seepage of ground water contributes to stream flow in the lower reaches of several basins. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr172","usgsCitation":"Halpenny, L.C., 1952, Ground water in the Gila River Basin and adjacent areas, Arizona: a summary: U.S. Geological Survey Open-File Report 172, xxii, 224 p., https://doi.org/10.3133/ofr172.","productDescription":"xxii, 224 p.","costCenters":[],"links":[{"id":356900,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/0172/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":291630,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/0172/report-thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Gila River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -114.5581,32.6315 ], [ -114.5581,33.3923 ], [ -108.2049,33.3923 ], [ -108.2049,32.6315 ], [ -114.5581,32.6315 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53e09e59e4b0beb42bdca43a","contributors":{"authors":[{"text":"Halpenny, Leonard Cameron","contributorId":66698,"corporation":false,"usgs":true,"family":"Halpenny","given":"Leonard","email":"","middleInitial":"Cameron","affiliations":[],"preferred":false,"id":168710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16406,"text":"ofr169 - 1952 - Perlite deposit near Healy, Alaska","interactions":[],"lastModifiedDate":"2014-08-01T13:36:41","indexId":"ofr169","displayToPublicDate":"2013-08-01T13:33:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"169","title":"Perlite deposit near Healy, Alaska","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ofr169","usgsCitation":"Wahrhaftig, C., and Eckhart, R.A., 1952, Perlite deposit near Healy, Alaska: U.S. Geological Survey Open-File Report 169, Report: 6 p.; 2 Maps, https://doi.org/10.3133/ofr169.","productDescription":"Report: 6 p.; 2 Maps","costCenters":[],"links":[{"id":291524,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","city":"Healy","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -149.664,63.6642 ], [ -149.664,64.2342 ], [ -148.1798,64.2342 ], [ -148.1798,63.6642 ], [ -149.664,63.6642 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53dca9cce4b0761578637761","contributors":{"authors":[{"text":"Wahrhaftig, Clyde","contributorId":102473,"corporation":false,"usgs":true,"family":"Wahrhaftig","given":"Clyde","email":"","affiliations":[],"preferred":false,"id":172793,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Eckhart, Richard A.","contributorId":23551,"corporation":false,"usgs":true,"family":"Eckhart","given":"Richard","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":172792,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72202,"text":"tem445 - 1952 - Reconnaissance for uraniferous rocks in northeastern Wind River Basin, Wyoming","interactions":[],"lastModifiedDate":"2014-07-23T13:10:15","indexId":"tem445","displayToPublicDate":"2013-07-23T13:07:00","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":"445","title":"Reconnaissance for uraniferous rocks in northeastern Wind River Basin, Wyoming","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem445","collaboration":"Prepared for the U.S. Atomic Energy Commission, Technical Information Service.","usgsCitation":"Tourtelot, H.A., 1952, Reconnaissance for uraniferous rocks in northeastern Wind River Basin, Wyoming: U.S. Geological Survey Trace Elements Memorandum 445, 14 p., https://doi.org/10.3133/tem445.","productDescription":"14 p.","costCenters":[],"links":[{"id":290811,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.22823,43.573028 ], [ -108.22823,43.589193 ], [ -108.196215,43.589193 ], [ -108.196215,43.573028 ], [ -108.22823,43.573028 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd76ae4b0824b2d177d34","contributors":{"authors":[{"text":"Tourtelot, Harry Allison","contributorId":77937,"corporation":false,"usgs":true,"family":"Tourtelot","given":"Harry","email":"","middleInitial":"Allison","affiliations":[],"preferred":false,"id":285185,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72172,"text":"tem362 - 1952 - Grain size distribution in the surface sands and the economic phosphate deposits of the land-pebble phosphate district, Florida","interactions":[],"lastModifiedDate":"2014-07-23T12:51:33","indexId":"tem362","displayToPublicDate":"2013-07-23T12:48:00","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":"362","title":"Grain size distribution in the surface sands and the economic phosphate deposits of the land-pebble phosphate district, Florida","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem362","collaboration":"Prepared for the United States Atomic Energy Commission, Technical Information Service.","usgsCitation":"Davidson, D.F., 1952, Grain size distribution in the surface sands and the economic phosphate deposits of the land-pebble phosphate district, Florida: U.S. Geological Survey Trace Elements Memorandum 362, 16 p., https://doi.org/10.3133/tem362.","productDescription":"16 p.","costCenters":[],"links":[{"id":290800,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.6349,24.5211 ], [ -87.6349,31.001 ], [ -80.0311,31.001 ], [ -80.0311,24.5211 ], [ -87.6349,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd76ae4b0824b2d177d36","contributors":{"authors":[{"text":"Davidson, David Francis","contributorId":86399,"corporation":false,"usgs":true,"family":"Davidson","given":"David","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":285182,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72168,"text":"tem341A - 1952 - Summary of uranium-bearing coal, lignite, and carbonaceous shale investigations in the Rocky Mountain region during 1951","interactions":[],"lastModifiedDate":"2014-07-23T12:45:33","indexId":"tem341A","displayToPublicDate":"2013-07-23T12:38:00","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":"341","chapter":"A","title":"Summary of uranium-bearing coal, lignite, and carbonaceous shale investigations in the Rocky Mountain region during 1951","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tem341A","collaboration":"Prepared by the Geological Survey for the U.S. Atomic Energy Commission.","usgsCitation":"Denson, N.M., and Bachman, G.O., 1952, Summary of uranium-bearing coal, lignite, and carbonaceous shale investigations in the Rocky Mountain region during 1951: U.S. Geological Survey Trace Elements Memorandum 341, 44 p., https://doi.org/10.3133/tem341A.","productDescription":"44 p.","temporalStart":"1951-01-01","temporalEnd":"1951-12-31","costCenters":[],"links":[{"id":290796,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"state":"Colorado;Idaho;Montana;Wyoming;Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.93,37.04 ], [ -116.93,48.97 ], [ -102.11,48.97 ], [ -102.11,37.04 ], [ -116.93,37.04 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd76ae4b0824b2d177d38","contributors":{"authors":[{"text":"Denson, Norman MacLaren","contributorId":29321,"corporation":false,"usgs":true,"family":"Denson","given":"Norman","email":"","middleInitial":"MacLaren","affiliations":[],"preferred":false,"id":285179,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bachman, George Odell","contributorId":64249,"corporation":false,"usgs":true,"family":"Bachman","given":"George","email":"","middleInitial":"Odell","affiliations":[],"preferred":false,"id":285180,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72163,"text":"tem337 - 1952 - Relation of the \"topography\" of the Hawthorn formation to size of phosphate particles in the deposits, and to topography, in the northern part of the land-pebble phosphate field, Florida","interactions":[],"lastModifiedDate":"2014-07-23T11:55:10","indexId":"tem337","displayToPublicDate":"2013-07-23T11:54:00","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":"337","title":"Relation of the \"topography\" of the Hawthorn formation to size of phosphate particles in the deposits, and to topography, in the northern part of the land-pebble phosphate field, Florida","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem337","usgsCitation":"Davidson, D.F., 1952, Relation of the \"topography\" of the Hawthorn formation to size of phosphate particles in the deposits, and to topography, in the northern part of the land-pebble phosphate field, Florida: U.S. Geological Survey Trace Elements Memorandum 337, 17 p., https://doi.org/10.3133/tem337.","productDescription":"17 p.","costCenters":[],"links":[{"id":290791,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.6349,24.5211 ], [ -87.6349,31.001 ], [ -80.0311,31.001 ], [ -80.0311,24.5211 ], [ -87.6349,24.5211 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd76ae4b0824b2d177d3a","contributors":{"authors":[{"text":"Davidson, David Francis","contributorId":86399,"corporation":false,"usgs":true,"family":"Davidson","given":"David","email":"","middleInitial":"Francis","affiliations":[],"preferred":false,"id":285177,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72156,"text":"tem327 - 1952 - Radioactivity and mineralogy of placer concentrates from the Wiseman and Chandalar districts, Upper Yukon Region, northeastern Alaska","interactions":[],"lastModifiedDate":"2014-07-23T11:18:43","indexId":"tem327","displayToPublicDate":"2013-07-23T11:18:00","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":"327","title":"Radioactivity and mineralogy of placer concentrates from the Wiseman and Chandalar districts, Upper Yukon Region, northeastern Alaska","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem327","collaboration":"Performed for the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"White, M.G., 1952, Radioactivity and mineralogy of placer concentrates from the Wiseman and Chandalar districts, Upper Yukon Region, northeastern Alaska: U.S. Geological Survey Trace Elements Memorandum 327, 14 p., https://doi.org/10.3133/tem327.","productDescription":"14 p.","costCenters":[],"links":[{"id":290781,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Alaska","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -148.4949600803,67.3649 ], [ -148.4949600803,67.5292 ], [ -149.9243,67.5292 ], [ -149.9243,67.3649 ], [ -148.4949600803,67.3649 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd76ae4b0824b2d177d3c","contributors":{"authors":[{"text":"White, Max Gregg","contributorId":91841,"corporation":false,"usgs":true,"family":"White","given":"Max","email":"","middleInitial":"Gregg","affiliations":[],"preferred":false,"id":285172,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":72076,"text":"tem152 - 1952 - The carnotite prospects of the Craven Canyon Area, Fall River County, South Dakota","interactions":[],"lastModifiedDate":"2014-07-21T13:41:03","indexId":"tem152","displayToPublicDate":"2013-07-21T13:37:00","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":"152","title":"The carnotite prospects of the Craven Canyon Area, Fall River County, South Dakota","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem152","collaboration":"Performed for the Division of Raw Materials, U.S. Atomic Energy Commission.","usgsCitation":"Page, L.R., and Redden, J., 1952, The carnotite prospects of the Craven Canyon Area, Fall River County, South Dakota: U.S. Geological Survey Trace Elements Memorandum 152, Report: 36 p.; 2 Maps, https://doi.org/10.3133/tem152.","productDescription":"Report: 36 p.; 2 Maps","costCenters":[],"links":[{"id":290592,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":8506,"type":{"id":17,"text":"Plate"},"url":"https://onlinepubs.er.usgs.gov/djvu/TEM/tem_152_plt.djvu"}],"country":"United States","state":"South Dakota","county":"Fall River County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.054709,43.000481 ], [ -104.054709,43.4771 ], [ -102.998992,43.4771 ], [ -102.998992,43.000481 ], [ -104.054709,43.000481 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7772e4b0b2908510b8de","contributors":{"authors":[{"text":"Page, Lincoln Ridler","contributorId":75228,"corporation":false,"usgs":true,"family":"Page","given":"Lincoln","email":"","middleInitial":"Ridler","affiliations":[],"preferred":false,"id":285084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Redden, J. A.","contributorId":62215,"corporation":false,"usgs":true,"family":"Redden","given":"J. A.","affiliations":[],"preferred":false,"id":285083,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":72069,"text":"tem145A - 1952 - The Papsy's Hope Autunite Prospect, Marysville District, Piute County, Utah","interactions":[],"lastModifiedDate":"2014-07-21T11:24:12","indexId":"tem145A","displayToPublicDate":"2013-07-21T11:20:00","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":"145","chapter":"A","title":"The Papsy's Hope Autunite Prospect, Marysville District, Piute County, Utah","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tem145A","collaboration":"Prepared for the United States Atomic Energy Commission, Technical Information Service.","usgsCitation":"Kaiser, E., 1952, The Papsy's Hope Autunite Prospect, Marysville District, Piute County, Utah: U.S. Geological Survey Trace Elements Memorandum 145, 10 p., https://doi.org/10.3133/tem145A.","productDescription":"10 p.","costCenters":[],"links":[{"id":290556,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","county":"Piute County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.520432,38.146545 ], [ -112.520432,38.511395 ], [ -111.765839,38.511395 ], [ -111.765839,38.146545 ], [ -112.520432,38.146545 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7724e4b0b2908510b5f1","contributors":{"authors":[{"text":"Kaiser, Edward P.","contributorId":90216,"corporation":false,"usgs":true,"family":"Kaiser","given":"Edward P.","affiliations":[],"preferred":false,"id":285069,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":71872,"text":"tei158 - 1952 - Uranophane at the Silver Cliff Mine near Lusk, Niobrara County, Wyoming","interactions":[],"lastModifiedDate":"2014-07-18T10:28:37","indexId":"tei158","displayToPublicDate":"2013-07-18T10:26:00","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":"158","title":"Uranophane at the Silver Cliff Mine near Lusk, Niobrara County, Wyoming","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei158","collaboration":"Performed for the Division of Raw Materials of the U.S. Atomic Energy Commission","usgsCitation":"Wilmarth, V., 1952, Uranophane at the Silver Cliff Mine near Lusk, Niobrara County, Wyoming: U.S. Geological Survey Trace Elements Investigations 158, Report: 22 p.; 3 Maps, https://doi.org/10.3133/tei158.","productDescription":"Report: 22 p.; 3 Maps","costCenters":[],"links":[{"id":290436,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Wyoming","county":"Niobrara County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.9019,42.6098 ], [ -104.9019,43.5037 ], [ -104.0526,43.5037 ], [ -104.0526,42.6098 ], [ -104.9019,42.6098 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd7a73e4b0b2908510d817","contributors":{"authors":[{"text":"Wilmarth, Verl R.","contributorId":89951,"corporation":false,"usgs":true,"family":"Wilmarth","given":"Verl R.","affiliations":[],"preferred":false,"id":284844,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70047531,"text":"70047531 - 1952 - Geology and ground-water resources of the Baltimore area","interactions":[{"subject":{"id":50997,"text":"ofr5199 - 1951 - Geologic cross section of the Sparrows Point district, Maryland","indexId":"ofr5199","publicationYear":"1951","noYear":false,"title":"Geologic cross section of the Sparrows Point district, Maryland"},"predicate":"SUPERSEDED_BY","object":{"id":70047531,"text":"70047531 - 1952 - Geology and ground-water resources of the Baltimore area","indexId":"70047531","publicationYear":"1952","noYear":false,"title":"Geology and ground-water resources of the Baltimore area"},"id":1}],"lastModifiedDate":"2013-08-08T13:39:41","indexId":"70047531","displayToPublicDate":"2013-01-01T13:32:00","publicationYear":"1952","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":"4","title":"Geology and ground-water resources of the Baltimore area","language":"English","publisher":"Maryland Geological Survey","publisherLocation":"Baltimore, MD","usgsCitation":"Bennett, R.R., and Meyer, R.R., 1952, Geology and ground-water resources of the Baltimore area: Bulletin 4, xi, 573 p.","productDescription":"xi, 573 p.","costCenters":[],"links":[{"id":276226,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Maryl","city":"Baltimore","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.917,38.89 ], [ -76.917,39.717 ], [ -76.083,39.717 ], [ -76.083,38.89 ], [ -76.917,38.89 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5204bde7e4b0403aa6262a07","contributors":{"authors":[{"text":"Bennett, Robert Raymond","contributorId":8369,"corporation":false,"usgs":true,"family":"Bennett","given":"Robert","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":482285,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meyer, R. R.","contributorId":20725,"corporation":false,"usgs":true,"family":"Meyer","given":"R.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":482286,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70047843,"text":"70047843 - 1952 - Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota","interactions":[{"subject":{"id":50949,"text":"ofr5190 - 1951 - Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota","indexId":"ofr5190","publicationYear":"1951","noYear":false,"title":"Preliminary report on ground-water conditions in the Cloquet area, Carlton County, Minnesota"},"predicate":"SUPERSEDED_BY","object":{"id":70047843,"text":"70047843 - 1952 - Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota","indexId":"70047843","publicationYear":"1952","noYear":false,"title":"Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota"},"id":1}],"lastModifiedDate":"2016-04-11T12:38:28","indexId":"70047843","displayToPublicDate":"2013-01-01T10:36:37","publicationYear":"1952","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":"6","title":"Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","collaboration":"Prepared in cooperation Division of Waters, Minnesota Department of Conservation","usgsCitation":"Akin, P., and Jones, J., 1952, Geology and ground-water resources of the Cloquet area, Carlton County, Minnesota: Bulletin 6, 63 p.","productDescription":"63 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":277045,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Minnesota","county":"Carlton County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -93.061233,46.768737 ], [ -93.061233,46.41722 ], [ -92.291597,46.41722 ], [ -92.291597,46.768737 ], [ -93.061233,46.768737 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd5dcfe4b0b290850fb4c5","contributors":{"authors":[{"text":"Akin, P.D.","contributorId":104471,"corporation":false,"usgs":true,"family":"Akin","given":"P.D.","email":"","affiliations":[],"preferred":false,"id":483119,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, J.R.","contributorId":15967,"corporation":false,"usgs":true,"family":"Jones","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":483118,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}