{"pageNumber":"6327","pageRowStart":"158150","pageSize":"25","recordCount":165969,"records":[{"id":5220134,"text":"5220134 - 1952 - Molting of northern yellow-throat in southern Michigan","interactions":[],"lastModifiedDate":"2017-06-07T12:14:13","indexId":"5220134","displayToPublicDate":"2010-06-16T12:18:21","publicationYear":"1952","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3544,"text":"The Auk","onlineIssn":"1938-4254","printIssn":"0004-8038","active":true,"publicationSubtype":{"id":10}},"title":"Molting of northern yellow-throat in southern Michigan","docAbstract":"

During the summer of 1938, detailed studies were made of the molts of the Northern Yellow-throat, Geothlypis trichas brachidactyla, in southern Michigan. Observations of the post-natal molt were made each day on nestlings found near Geddes Pond, one mile east of Ann Arbor. Studies of the post-juvenal and post-nuptial molts were from fresh specimens collected at Portage Lake in Jackson County.

","language":"English","publisher":"American Ornithological Society","doi":"10.2307/4081292","usgsCitation":"Stewart, R.E., 1952, Molting of northern yellow-throat in southern Michigan: The Auk, v. 69, no. 1, p. 50-59, https://doi.org/10.2307/4081292.","productDescription":"10 p.","startPage":"50","endPage":"59","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":503068,"rank":1,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digitalcommons.usf.edu/auk/vol69/iss1/6","text":"External Repository"},{"id":194171,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Michigan","volume":"69","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699232","contributors":{"authors":[{"text":"Stewart, R. E.","contributorId":93426,"corporation":false,"usgs":true,"family":"Stewart","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":331386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70159078,"text":"tei161 - 1952 - Present and past ground-water conditions in the Morrison Formation in southwestern Colorado and southeastern Utah","interactions":[],"lastModifiedDate":"2017-06-17T12:59:28","indexId":"tei161","displayToPublicDate":"2010-02-02T05:15:00","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":"161","title":"Present and past ground-water conditions in the Morrison Formation in southwestern Colorado and southeastern Utah","docAbstract":"

Field and laboratory studies of ground-water conditions in the carnotite-bearing Morrison formation in southwestern Colorado and southeastern Utah were undertaken to determine possible relations between ground waters and the carnotite deposits.

\n

The ore-bearing sandstone consists of lenticular sandstone strata, interbedded within discontinuous layers of mudstone; these strata were deposited in a stream environment. The porosity and permeability of the ore-bearing sandstone in one area are relatively low, porosity averaging about 15 percent and permeability ranging between 30 and 3300 millidarcys. Permeability studies in this same area show that sandstone classed as favorable for ore is slightly more permeable than and has nearly twice the transmissibility of sandstone classed as semifavorable; outcrop studies also suggest a lower transmissibility for sandstone that is unfavorable.

\n

Samples of water from the ore-bearing and associated strata show considerable variation in chemical charter. These water samples are generally low in uranium, vanadium, copper, and lead, most samples containing less than 1 part per million (ppm) of each metal.

\n

General geologic relations suggest that ground-water movement probably was active through the ore-bearing strata during their deposition and shortly afterward. Movement during this time probably occurred largely through the more permeable sand strata and in the general direction of initial dip and stream flow. During Cretaceous time, when several thousand feet of marine sediments accumulated over the Morrison, the water contained in the ore-bearing strata probably was immobile or nearly so and was protected from escape or contamination. Following Tertiary deformation and erosion, active ground-water circulation no doubt was restored, but because of the low permeability and the lenticular character and therefore low transmissibility of the ore-bearing sandstone, ground-water movement probably was slow. Faulting probably also influenced the direction and rate of ground-water movement during Tertiary time.

\n

Movement and localization of ground water would permit the concentration of metal-bearing solutions during Salt Wash and early Brushy Basin time in the beds that now contain ore deposits. It is more difficult to explain the formation of these deposits, which have a wide geographic distribution at a restricted stratigraphic position, from solutions circulating through the rocks at a later date.

\n

Whatever mode of origin is used to explain the deposits, geologists almost without exception, agree that the metals were transported by solutions that have migrated through the sediments for considerable distances. For this reason, a study of the horizontal and vertical transmissibility characteristics of all exposed sedimentary formations on the Colorado Plateau is planned.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei161","usgsCitation":"Phoenix, D.A., 1952, Present and past ground-water conditions in the Morrison Formation in southwestern Colorado and southeastern Utah: U.S. Geological Survey Trace Elements Investigations 161, Report: 42 p.; 6 Plates: 31 x 21 inches or smaller, https://doi.org/10.3133/tei161.","productDescription":"Report: 42 p.; 6 Plates: 31 x 21 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":309904,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":309910,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-4.pdf","text":"Plate 4","size":"5.61 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 4"},{"id":309909,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-3.pdf","text":"Plate 3","size":"1.54 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":309911,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-5.pdf","text":"Plate 5","size":"5.55 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 5"},{"id":309912,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-6.pdf","text":"Plate 6","size":"2.81 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 6"},{"id":309902,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/161/report.pdf","text":"Report","size":"23.08 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":309908,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-2.pdf","text":"Plate 2","size":"4.83 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":309907,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/161/plate-1.pdf","text":"Plate 1","size":"4.54 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"country":"United States","state":"Colorado, Utah","county":"Mesa County, Montrose County, San Miguel County","otherGeospatial":"Calamity Mesa, Atkinson Mesa, Slick Rock area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -109.5941162109375,\n 37.735969208590504\n ],\n [\n -109.5941162109375,\n 39.08530414503412\n ],\n [\n -108.2373046875,\n 39.08530414503412\n ],\n [\n -108.2373046875,\n 37.735969208590504\n ],\n [\n -109.5941162109375,\n 37.735969208590504\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5620ce93e4b06217fc478b0b","contributors":{"authors":[{"text":"Phoenix, D. A.","contributorId":92665,"corporation":false,"usgs":true,"family":"Phoenix","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":577563,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5230010,"text":"5230010 - 1952 - Venomous Snakes of the United States and Treatment of Their Bites","interactions":[],"lastModifiedDate":"2012-02-02T00:15:25","indexId":"5230010","displayToPublicDate":"2009-06-09T11:33:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":98,"text":"Wildlife Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"339","title":"Venomous Snakes of the United States and Treatment of Their Bites","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Stickel, W.H., 1952, Venomous Snakes of the United States and Treatment of Their Bites: Wildlife Leaflet 339, 29.","productDescription":"29","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":112338,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015007538047?urlappend=%3Bseq=3"},{"id":202534,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602321","contributors":{"authors":[{"text":"Stickel, W. H.","contributorId":23239,"corporation":false,"usgs":true,"family":"Stickel","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":343360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":5210487,"text":"5210487 - 1952 - Where are the ducks?","interactions":[],"lastModifiedDate":"2012-02-02T00:15:19","indexId":"5210487","displayToPublicDate":"2009-06-09T09:23:17","publicationYear":"1952","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Where are the ducks?","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The Potomac Valley: History and Prospect","largerWorkSubtype":{"id":4,"text":"Other Government Series"},"language":"English","publisher":"Audubon Society of the District of Columbia, Inc.","publisherLocation":"Washington, DC","collaboration":"reprinted from ATLANTIC NATURALIST 6(4):143-150, 1951","usgsCitation":"Slavik, W., and Uhler, F., 1952, Where are the ducks?, chap. of The Potomac Valley: History and Prospect, p. 23-30.","productDescription":"44","startPage":"23","endPage":"30","numberOfPages":"44","costCenters":[{"id":531,"text":"Patuxent Wildlife Research Center","active":true,"usgs":true}],"links":[{"id":200514,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a49fc","contributors":{"editors":[{"text":"Briggs, Shirley A.","contributorId":111850,"corporation":false,"usgs":true,"family":"Briggs","given":"Shirley","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":506528,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Slavik, W.","contributorId":9744,"corporation":false,"usgs":true,"family":"Slavik","given":"W.","email":"","affiliations":[],"preferred":false,"id":328524,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Uhler, F.M.","contributorId":81965,"corporation":false,"usgs":true,"family":"Uhler","given":"F.M.","email":"","affiliations":[],"preferred":false,"id":328525,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":24330,"text":"ofr98166 - 1952 - Geologic reconnaissance and test-well drilling program, Marine Corps Training Center, Twentynine Palms, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"ofr98166","displayToPublicDate":"2002-05-01T00:00:00","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":"98-166","title":"Geologic reconnaissance and test-well drilling program, Marine Corps Training Center, Twentynine Palms, California","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nInformation Services [distributor],","doi":"10.3133/ofr98166","issn":"0094-9140","usgsCitation":"Riley, F.S., and Worts, G.F., 1952, Geologic reconnaissance and test-well drilling program, Marine Corps Training Center, Twentynine Palms, California (Retyped 2001): U.S. Geological Survey Open-File Report 98-166, vi, 64 p. :maps ;28 cm., https://doi.org/10.3133/ofr98166.","productDescription":"vi, 64 p. :maps ;28 cm.","costCenters":[],"links":[{"id":157425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1998/0166/report-thumb.jpg"},{"id":53436,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1998/0166/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"Retyped 2001","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db6883b3","contributors":{"authors":[{"text":"Riley, Francis S.","contributorId":93028,"corporation":false,"usgs":true,"family":"Riley","given":"Francis","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":191702,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Worts, George Frank Jr.","contributorId":90322,"corporation":false,"usgs":true,"family":"Worts","given":"George","suffix":"Jr.","email":"","middleInitial":"Frank","affiliations":[],"preferred":false,"id":191701,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70197598,"text":"70197598 - 1952 - Ground-water data collected in the Missouri River basin units in Kansas during 1951","interactions":[],"lastModifiedDate":"2022-05-25T18:52:09.980244","indexId":"70197598","displayToPublicDate":"1999-12-26T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Ground-water data collected in the Missouri River basin units in Kansas during 1951","docAbstract":"

Ground-water studies in the Missouri River Basin were begun by the United States Geological Survey during the fall of 1945 as a part of the program for development of the resources of the basin by the U.S. Bureau of Reclamation and other Federal Agencies. The studies of the ground-water resources in the part of Kansas that lies within the Basin have been coordinated with the cooperative program of ground-water studies already being made in Kansas by the U.S. Geological Survey, the State Geological Survey of Kansas, the Division of Sanitation of the Kansas State Board of Health, and the Division of Water Resources of the Kansas State Board of Agriculture.

Areas in which ground-water data have been collected for the Missouri Basin program include the Almena Unit in Norton and Phillips Counties; the Bostwick Unit in Jewell, Republic, and Cloud Counties; the Cedar Bluff Unit in Ellis, Rush, and Trego Counties; the Glen Elder Unit in Mitchell County; Kanopolis unit in Ellsworth, McPherson, and Saline Counties; Kirwin unit in Phillips, Smith, and Osborne Counties; the Ladder Creek project in Greeley, Gove, Lane, Logan, Scott, Wallace, and Wichita Counties; the St. Francis unit in Cheyenne County; the Webster Unit in Osborne County; and the Wilson Unit in Lincoln County. Data relating to the Ladder Creek project will be published later in a separate report.

This report is the fifth of a series of annual reports on ground-water in the above-named units in Kansas and contains the data collected mostly during 1951.  An index to the data that were collected and presented in the 1947, 1948, 1949, 1950, and 1951 reports is given in table 1.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70197598","collaboration":"Compiled in cooperation with the State Geological Survey of Kansas, the Division of Sanitation of the Kansas State Board of Health, and the Division of Water Resources of the Kansas State Board of Agriculture.","usgsCitation":"Mason, B., and Berry, D.W., 1952, Ground-water data collected in the Missouri River basin units in Kansas during 1951: Open-File Report, iv, 119 p., https://doi.org/10.3133/70197598.","productDescription":"iv, 119 p.","costCenters":[],"links":[{"id":401065,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70197598/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":354995,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70197598/report-thumb.jpg"}],"country":"United States","state":"Kansas","otherGeospatial":"Missouri River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -102.030029296875,\n 38.44498466889473\n ],\n [\n -97.415771484375,\n 38.44498466889473\n ],\n [\n -97.415771484375,\n 40.002371935876475\n ],\n [\n -102.030029296875,\n 40.002371935876475\n ],\n [\n -102.030029296875,\n 38.44498466889473\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Mason, B.J.","contributorId":53029,"corporation":false,"usgs":true,"family":"Mason","given":"B.J.","email":"","affiliations":[],"preferred":false,"id":737874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":737875,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71360,"text":"tei311 - 1952 - Geology of the Copper King Mine area, Prairie Divide, Larimer County, Colorado (Part 1)","interactions":[],"lastModifiedDate":"2014-06-11T11:01:28","indexId":"tei311","displayToPublicDate":"1994-01-01T07:00:00","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":"311","title":"Geology of the Copper King Mine area, Prairie Divide, Larimer County, Colorado (Part 1)","docAbstract":"

The Copper King mine, in Larimer County, Colo., in the northern part of the Front Range of Colorado, was operated for a short time prior to World War II for copper and zino, but since 1949, when pitchblende was discovered on the mine dump, it has been worked for uranium.

\n
\n

The bedrock in the mine area consists predominantly of pre-Cambrian (Silver Plums) granite with minor migmatite and metasediments--biotite-quartz-plagioclase gneiss, biotite schist, quartzite, amphibolite, amphibole skarn, and biotite skols. The metasediments occur as inclusions that trend northeast in the granite. This trend is essentially parallel to the prevailing foliation in the granite. At places the metasediments are crosscut sharply by the granite to form angular, partly discordant, steep-walled bodies in the granite. Faults, confined to a narrow zone that extends through the mine, cut both the pre-Cambrian rocks and the contained sulfide deposits. The Copper King fault, a breccia zone, contains a deposit of pitchblende; the other faults are believed to be later than the ore.

\n
\n

The two types of mineral deposits--massive sulfide and pitchblende deposits--in the mine area, are of widely different mineralogy, age, and origin. The massive sulfide deposits are small and consist of pyrite, sphalerite, chalcopyrite, pyrrhotite, and in places magnetite in amphibole skarn, mice skols, and quartzite. The deposit at the Copper King mine has yielded small quantities of high-grade sphalerite ore. The massive sulfides are pyrometasomatic deposits of pre-Cambrian age.

\n
\n

The pitchblende at the Copper King mine is principally in the Copper King vein, a tight, hard breccia zone that cuts through both granite and the massive sulfide deposit. A small part of the pitchblende is in small fractures near the vein and in boxwork pyrite adjacent to the vein; the post-ore faults, close to their intersection with the Copper King vein, contain some radioactive material, but elsewhere, so far as is known, they are barren. The pitchblende in the deposit forms a steeply plunging ore shoot that has a horizontal length of more than 50 feet and a vertical height of about 85 feet. The thickness of the ore shoot averages about 2 feet, but it ranges from a feather edge to about 4 feet. The hard pitch-blende is intimately intergrown with siderite; other gangue minerals include pyrite, quartz, and finely comminuted fragments of the wall rocks. The vein was repeatedly reopened during mineral deposition as shown by several stages of brecciation and recommended by the vein matter. The pitchblende deposit probably formed at intermediate temperatures and depths and, according to the Pb/U ratio, is about 60 million years old--an early Tertiary age.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei311","collaboration":"This report concerns work done on behalf of the Division of Raw Materials of the U.S. Atomic Energy Commission.","usgsCitation":"Sims, P.K., and Phair, G., 1952, Geology of the Copper King Mine area, Prairie Divide, Larimer County, Colorado (Part 1): U.S. Geological Survey Trace Elements Investigations 311, 44 p.; Plate 1: 19.44 x 14.66 inches; Plate 2: 19.39 x 14.74 inches; Plate 3: 10.33 x 19.71 inches, https://doi.org/10.3133/tei311.","productDescription":"44 p.; Plate 1: 19.44 x 14.66 inches; Plate 2: 19.39 x 14.74 inches; Plate 3: 10.33 x 19.71 inches","costCenters":[],"links":[{"id":258776,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/311/plate-1.pdf","size":"1063","linkFileType":{"id":1,"text":"pdf"}},{"id":258777,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/311/plate-2.pdf","size":"821","linkFileType":{"id":1,"text":"pdf"}},{"id":258778,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/311/plate-3.pdf","size":"500","linkFileType":{"id":1,"text":"pdf"}},{"id":258779,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/311/report.pdf","size":"5408","linkFileType":{"id":1,"text":"pdf"}},{"id":258780,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/311/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Larimer County","otherGeospatial":"Copper King Mine;Prairie Divide","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.1954,40.2578 ], [ -106.1954,40.9984 ], [ -104.9431,40.9984 ], [ -104.9431,40.2578 ], [ -106.1954,40.2578 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae758","contributors":{"authors":[{"text":"Sims, Paul Kibler","contributorId":26759,"corporation":false,"usgs":true,"family":"Sims","given":"Paul","email":"","middleInitial":"Kibler","affiliations":[],"preferred":false,"id":284046,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Phair, George","contributorId":91512,"corporation":false,"usgs":true,"family":"Phair","given":"George","email":"","affiliations":[],"preferred":false,"id":284047,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71207,"text":"tei173 - 1952 - Uranium in the metal-mining districts of Colorado","interactions":[],"lastModifiedDate":"2014-04-03T14:43:14","indexId":"tei173","displayToPublicDate":"1994-01-01T07:00:00","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":"173","title":"Uranium in the metal-mining districts of Colorado","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/tei173","usgsCitation":"King, R., Leonard, B.F., Moore, F.B., and Pierson, C.T., 1952, Uranium in the metal-mining districts of Colorado: U.S. Geological Survey Trace Elements Investigations 173, Plate 1: 20.80 x 20.11 inches; Plate 2: 8.27 x 11.73 inches; Plate 3: 9.62 x 11.79 inches, https://doi.org/10.3133/tei173.","productDescription":"Plate 1: 20.80 x 20.11 inches; Plate 2: 8.27 x 11.73 inches; Plate 3: 9.62 x 11.79 inches","costCenters":[],"links":[{"id":192992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/173/report-thumb.jpg"},{"id":90601,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/173/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":285604,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0173/figure-1.pdf"},{"id":285605,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0173/figure-2.pdf"},{"id":285606,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/tei/0173/figure-3.pdf"}],"country":"United States","state":"Colorado","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -109.0603,36.9924 ], [ -109.0603,41.0034 ], [ -102.0409,41.0034 ], [ -102.0409,36.9924 ], [ -109.0603,36.9924 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60540d","contributors":{"authors":[{"text":"King, R.U.","contributorId":7692,"corporation":false,"usgs":true,"family":"King","given":"R.U.","email":"","affiliations":[],"preferred":false,"id":283804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leonard, B. 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei215","usgsCitation":"Waring, C.L., and Annell, C., 1952, A semiquantitative spectrographic method for the analysis of minerals, rocks, and ores (II): U.S. Geological Survey Trace Elements Investigations 215, 32 p., https://doi.org/10.3133/tei215.","productDescription":"32 p.","costCenters":[],"links":[{"id":188448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/215/report-thumb.jpg"},{"id":90665,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/215/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6545","contributors":{"authors":[{"text":"Waring, C. 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S.","contributorId":94286,"corporation":false,"usgs":true,"family":"Grimaldi","given":"F.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":283871,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71281,"text":"tei217 - 1952 - Wagon-drill sampling by U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:13:36","indexId":"tei217","displayToPublicDate":"1994-01-01T00:00:00","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":"217","title":"Wagon-drill sampling by U.S. Geological Survey","language":"ENGLISH","doi":"10.3133/tei217","usgsCitation":"Huleatt, W.P., 1952, Wagon-drill sampling by U.S. Geological Survey: U.S. Geological Survey Trace Elements Investigations 217, 11 leaves : ill. ; 27 cm.; 2 figs., https://doi.org/10.3133/tei217.","productDescription":"11 leaves : ill. ; 27 cm.; 2 figs.","costCenters":[],"links":[{"id":188527,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/217/report-thumb.jpg"},{"id":90667,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd4e6","contributors":{"authors":[{"text":"Huleatt, William Penn","contributorId":97575,"corporation":false,"usgs":true,"family":"Huleatt","given":"William","email":"","middleInitial":"Penn","affiliations":[],"preferred":false,"id":283946,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":71306,"text":"tei247 - 1952 - Radioactive tertiary porphyries in the Central City district, Colorado, and their bearing upon pitchblende deposition","interactions":[],"lastModifiedDate":"2012-02-02T00:13:33","indexId":"tei247","displayToPublicDate":"1994-01-01T00:00:00","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":"247","title":"Radioactive tertiary porphyries in the Central City district, Colorado, and their bearing upon pitchblende deposition","language":"ENGLISH","doi":"10.3133/tei247","usgsCitation":"Phair, G., 1952, Radioactive tertiary porphyries in the Central City district, Colorado, and their bearing upon pitchblende deposition: U.S. Geological Survey Trace Elements Investigations 247, 53 p. : maps ; 27 cm., https://doi.org/10.3133/tei247.","productDescription":"53 p. : maps ; 27 cm.","costCenters":[],"links":[{"id":188249,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/247/report-thumb.jpg"},{"id":90679,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/247/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649d51","contributors":{"authors":[{"text":"Phair, George","contributorId":91512,"corporation":false,"usgs":true,"family":"Phair","given":"George","email":"","affiliations":[],"preferred":false,"id":283968,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":60854,"text":"mf4 - 1952 - Geologic map of bastnaesite deposits, Birthday claims, San Bernardino County, California","interactions":[{"subject":{"id":15942,"text":"ofr52137 - 1952 - Geologic map of bastnaesite deposits of the Birthday claims, San Bernardino County, California","indexId":"ofr52137","publicationYear":"1952","noYear":false,"title":"Geologic map of bastnaesite deposits of the Birthday claims, San Bernardino County, California"},"predicate":"SUPERSEDED_BY","object":{"id":60854,"text":"mf4 - 1952 - Geologic map of bastnaesite deposits, Birthday claims, San Bernardino County, California","indexId":"mf4","publicationYear":"1952","noYear":false,"title":"Geologic map of bastnaesite deposits, Birthday claims, San Bernardino County, California"},"id":1}],"lastModifiedDate":"2018-07-18T14:17:58","indexId":"mf4","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"4","title":"Geologic map of bastnaesite deposits, Birthday claims, San Bernardino County, California","docAbstract":"

In April 1949 a deposit containing considerable quantities of the rare mineral bastnaesite - the fluorocarbonate of cerium, lanthanum, and other rare earths - was discovered near Mountain Pass, San Bernardino County, Calif.  Small quantities of bastnaesite have been found in several places in the United States, but this area is the first that offers promise of being a commercial source of cerium, lanthanum, and other rare earths.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf4","usgsCitation":"Sharp, W.N., and Pray, L., 1952, Geologic map of bastnaesite deposits, Birthday claims, San Bernardino County, California: U.S. Geological Survey Miscellaneous Field Studies Map 4, 47.39 x 41.05 inches, https://doi.org/10.3133/mf4.","productDescription":"47.39 x 41.05 inches","costCenters":[],"links":[{"id":183505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"600","country":"United States","state":"California","county":"San Bernardino County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -115.5,35.5 ], [ -115.5,35.5 ], [ -115.5,35.5 ], [ -115.5,35.5 ], [ -115.5,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b12e4b07f02db6a29f3","contributors":{"authors":[{"text":"Sharp, W. N.","contributorId":21958,"corporation":false,"usgs":true,"family":"Sharp","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":264508,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pray, L.C.","contributorId":49433,"corporation":false,"usgs":true,"family":"Pray","given":"L.C.","affiliations":[],"preferred":false,"id":264509,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71295,"text":"tei236 - 1952 - A theoretical treatment of the absorption characteristics of the dithizone mixed-color system","interactions":[],"lastModifiedDate":"2012-02-02T00:13:33","indexId":"tei236","displayToPublicDate":"1994-01-01T00:00:00","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":"236","title":"A theoretical treatment of the absorption characteristics of the dithizone mixed-color system","language":"ENGLISH","doi":"10.3133/tei236","usgsCitation":"Milkey, R.G., 1952, A theoretical treatment of the absorption characteristics of the dithizone mixed-color system: U.S. Geological Survey Trace Elements Investigations 236, 12 p. : ill. ; 27 cm., https://doi.org/10.3133/tei236.","productDescription":"12 p. : ill. ; 27 cm.","costCenters":[],"links":[{"id":188161,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/tei/236/report-thumb.jpg"},{"id":90673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/236/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a5af3","contributors":{"authors":[{"text":"Milkey, Robert G.","contributorId":84006,"corporation":false,"usgs":true,"family":"Milkey","given":"Robert","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":283954,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2377,"text":"wsp1135 - 1952 - Ground-water resources of Snohomish County, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:19","indexId":"wsp1135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1952","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":"1135","title":"Ground-water resources of Snohomish County, Washington","docAbstract":"Snohomish County comprises an east-west strip, six townships wide, extending 60 miles from the eastern shore of Puget Sound to the drainage divide of the Cascade Mountains. Topographically, the eastern two-thirds of the county varies frown hills and low mountain spurs at the west to the continuous high, maturely carved mountains of the Cascade Range at the east. The western third of the county lies in the Puget Sound lowland section: it is made up largely of unconsolidated deposits, as contrasted with the hard rocks of the mountain section. High-level deposits of glacial debris in some places form a transitional ramp from the lowlands to the mountain topography; in other places the transition is abrupt. The principal rivers--the Snohomish, Skykomish, Stillaguamish, and Sauk--drain westward and northwestward to Puget Sound.\r\n\r\nThe Puget Sound lowland, with its extensions up the river valleys, is economically the important part. of the county. Within that part., ground-water development is of particular importance. The climate is equable and dominantly oceanic, with an average of about 32 h. of rainfall annually, but with a pronounced dry season from June to September. A mean annual temperature of 52 F, a growing season of more than 200 days, and a variety of good soils form a setting in which supplemental irrigation can at least double the average crop production. \r\n\r\nWithin the coastal lowland, plateau segments 200 to 600 ft or more in altitude are separated by flat-bottomed, alluviated river gorges. The river flats in some eases represent the surface of as much as 500 to 600 ft of glacial and alluvial deposits backfilled into canyonlike arms of the aneestral drainage system. The plateau segments are formed of the till-smoothed remnants of bedrock or the tabular segments of Pleistocene deposits. The Pleistocene deposits consist, above sea level, of about 200 ft of Admiralty clay and as much as 1,000 ft of deposits of the Vashon glaciation. The latter include as much as 300 ft of either clay or sand units of advance outwash, up to 150 ft of till, and variable thicknesses of outwash-terrace and train material. The Admiralty clay is composed largely of clayey materials without important quantities of ground water. Similar clayey sediments are known to continue downward for more than 1,000 ft below sea level. The sand unit and, to a lesser extent, the clay unit, are largely advance outwash of the Vashon glaciation. They are water bearing, and the position of their ground-water reservoirs--in flat-shaped bodies perched on the Admiralty clay beneath the plateau surfaces and slopes--makes them particularly susceptible to useful development. The till is a persistent ground-moraine deposit that mantles most of the area of the plateau segments and passes beneath much of the outwash and alluvium of the valleys. The till is a great vaster of precipitation; it. sheds off to the creeks much water that would otherwise recharge the ground-water reservoirs. A small amount of water percolates irregularly into and through the till or accumulates in the soil zones on top, where it is tapped by a great many 'hardpan' wells of small yield. Outwash terraces of gravels and sands, where they lie below the local water table, carry large quantities of ground water. The alluvial materials of the river valleys are good aquifers, but the water is iron bearing in many places and is saline in places in the lower parts of the Snohomish and Stillaguamish Valleys. \r\n\r\nAt present, no good aquifers are known to exist in the bedrock formations. The metamorphic, granitic, and volcanic rocks of the mountainous parts of the county are largely nonpermeable. The Tertiary strata, which underlie the coastal lowland at depth and crop out about its inner margin, contain little or no water, and that which is present is usually of poor quality. \r\n\r\nThe chemical quality of the ground waters is in general excellent. The iron- bearing water of the alluvial valleys is the princ","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1135","usgsCitation":"Newcomb, R.C., 1952, Ground-water resources of Snohomish County, Washington: U.S. Geological Survey Water Supply Paper 1135, v, 133 p. :ill., maps ;24 cm. + plates folded in pocket., https://doi.org/10.3133/wsp1135.","productDescription":"v, 133 p. :ill., maps ;24 cm. + plates folded in pocket.","costCenters":[],"links":[{"id":137762,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1135/report-thumb.jpg"},{"id":28332,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1135/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28333,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1135/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28334,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1135/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c4b","contributors":{"authors":[{"text":"Newcomb, Reuben Clair","contributorId":37712,"corporation":false,"usgs":true,"family":"Newcomb","given":"Reuben","email":"","middleInitial":"Clair","affiliations":[],"preferred":false,"id":145106,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":41300,"text":"ofr52122 - 1952 - Photogeologic maps of the Stinking Spring Creek 11 and 12 quadrangles, Emery County, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:10:49","indexId":"ofr52122","displayToPublicDate":"1994-01-01T00:00:00","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":"52-122","title":"Photogeologic maps of the Stinking Spring Creek 11 and 12 quadrangles, Emery County, Utah","language":"ENGLISH","doi":"10.3133/ofr52122","usgsCitation":"Ray, R.G., and Fischer, W.A., 1952, Photogeologic maps of the Stinking Spring Creek 11 and 12 quadrangles, Emery County, Utah: U.S. Geological Survey Open-File Report 52-122, 1 map, https://doi.org/10.3133/ofr52122.","productDescription":"1 map","costCenters":[],"links":[{"id":171633,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79076,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0122/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79077,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1952/0122/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685ec0","contributors":{"authors":[{"text":"Ray, Richard G.","contributorId":29802,"corporation":false,"usgs":true,"family":"Ray","given":"Richard","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":224795,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fischer, William August","contributorId":68305,"corporation":false,"usgs":true,"family":"Fischer","given":"William","email":"","middleInitial":"August","affiliations":[],"preferred":false,"id":224796,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":41302,"text":"ofr5263 - 1952 - Photogeologic maps of the Verdure 1, 2, 4, 6, 7, and 8 quadrangles, Utah and Colorado","interactions":[],"lastModifiedDate":"2016-02-03T10:24:45","indexId":"ofr5263","displayToPublicDate":"1994-01-01T00:00:00","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":"52-63","title":"Photogeologic maps of the Verdure 1, 2, 4, 6, 7, and 8 quadrangles, Utah and Colorado","docAbstract":"

Base maps compiled by Soil Conservation Service, U.S. Department of Agriculture. These maps are compilations of photogeology and surface geology, Colorado Plateau area, United States. They are also known as:

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Base maps compiled by Soil Conservation Service, U.S. Department of Agriculture. These maps are compilations of photogeology and surface geology, Colorado Plateau area, United States. 

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