{"pageNumber":"6903","pageRowStart":"172550","pageSize":"25","recordCount":184776,"records":[{"id":70216355,"text":"70216355 - 1957 - Water Analysis","interactions":[],"lastModifiedDate":"2020-11-12T21:09:43.831259","indexId":"70216355","displayToPublicDate":"1957-11-12T15:04:22","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Water Analysis","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60124a001","usgsCitation":"Love, S.K., and Thatcher, L.L., 1957, Water Analysis: Analytical Chemistry, v. 29, no. 4, p. 722-734, https://doi.org/10.1021/ac60124a001.","productDescription":"13 p.","startPage":"722","endPage":"734","costCenters":[],"links":[{"id":380486,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":804790,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":804791,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216354,"text":"70216354 - 1957 - Eastern and central Montana as a possible source area of uranium","interactions":[],"lastModifiedDate":"2020-11-12T21:03:58.228527","indexId":"70216354","displayToPublicDate":"1957-11-12T14:53:42","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Eastern and central Montana as a possible source area of uranium","docAbstract":"<p><span>Geologic settings in central and eastern Montana and in a few places in southwestern Montana are similar to the settings in areas favorable for the occurrence of uranium deposits. Several areas in Montana seem especially favorable for the occurrence of uranium.The alkalic igneous rock province of central Montana is similar to the one of the Colorado Plateau. On the basis of this analogy, certain areas in Montana, where the lithology and (or) structure are considered favorable for the occurrence of uranium, are suggested for prospecting. Seleniferous plants, similar to those that are uranium indicators on the Colorado Plateau, might be used as an aid in prospecting for uranium provided that the seleniferous shale areas are taken into account.Uranium deposits, similar to those in North and South Dakota, may be found in Cretaceous and Tertiary sandstones, lignites, and low-grade coals of eastern Montana; also, the magnetite-bearing beds of certain Cretaceoussandstones may contain fossil placer deposits of radioactive black minerals. Theoccurrence of uranium in basal conglomerates, quartzites, and sandstones in Africa and Ontario suggests that similar basal sedimentary rocks in central Montana may contain uranium.Many of the radioactivity anomalies in Montana found from the air are closely associated with the Eagle sandstone; others are associated with Precambrian basement rocks, Upper Cretaceous and Lower Tertiary igneous rocks, or sedimentary rocks of Jurassic and Cretaceous age. Glacial cover and lack of outcrops locally may hinder prospecting for uranium.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.52.3.211","usgsCitation":"Armstrong, F.C., 1957, Eastern and central Montana as a possible source area of uranium: Economic Geology, v. 52, no. 3, p. 211-224, https://doi.org/10.2113/gsecongeo.52.3.211.","productDescription":"14 p.","startPage":"211","endPage":"224","costCenters":[],"links":[{"id":480408,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc502288/","text":"External Repository"},{"id":380485,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Montana","otherGeospatial":"Central and eastern Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.0390625,\n              44.96479793033101\n            ],\n            [\n              -110.0390625,\n              48.980216985374994\n            ],\n            [\n              -116.3671875,\n              49.095452162534826\n            ],\n            [\n              -116.21337890625,\n              48.07807894349862\n            ],\n            [\n              -115.7080078125,\n              47.204642388766935\n            ],\n            [\n              -114.47753906249999,\n              46.5739667965278\n            ],\n            [\n              -114.60937499999999,\n              45.66012730272194\n            ],\n            [\n              -113.90625,\n              45.398449976304086\n            ],\n            [\n              -113.26904296874999,\n              44.26093725039923\n            ],\n            [\n              -111.09374999999999,\n              44.402391829093915\n            ],\n            [\n              -111.09374999999999,\n              44.96479793033101\n            ],\n            [\n              -110.0390625,\n              44.96479793033101\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"3","noUsgsAuthors":false,"publicationDate":"1957-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Armstrong, Frank Clarkson","contributorId":19559,"corporation":false,"usgs":true,"family":"Armstrong","given":"Frank","email":"","middleInitial":"Clarkson","affiliations":[],"preferred":false,"id":804789,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70216353,"text":"70216353 - 1957 - A truckmounted spectrographic laboratory for use in geochemical exploration","interactions":[],"lastModifiedDate":"2020-11-12T20:45:57.9405","indexId":"70216353","displayToPublicDate":"1957-11-12T14:33:41","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"A truckmounted spectrographic laboratory for use in geochemical exploration","docAbstract":"<p><span>A truck-mounted spectrographic laboratory has been designed and built by the U. S. Geological Survey to investigate the feasibility of using and transporting such equipment in the field as an aid in supplying rapid on-the-spot analytical data to geochemical exploration field parties.The laboratory is housed inside a 7- X 12-foot insulated and air-conditioned van-type truck body and carries complete equipment for making qualitative, semiquantitative, and quantitative analyses of geological materials. The spectrograph is a fixed-position 1.5-meter grating instrument of the Wadsworth type which records a range of spectra from 2063 to 4837A in the second order on a 20-inch strip of film. Companion units are a projection type comparator-densitometer, a film processor, and other accessory equipment. Trailer-mounted motor-generators supply 230 volts d-c for the arc source unit and 115 volts a-c for lights and accessories.Since its completion in May 1955, the truck-mounted laboratory has been driven over 4,000 miles. During this travel all the equipment remained in good adjustment; the laboratory was made ready for operation in less than 2 hours after arrival at the site of a field project.Because of the large number of elements that can be determined from a single spectrogram, the truck-mounted laboratory is useful in the early stages of a geochemical exploration project to determine diagnostic suites of elements, and later, to guide the day-to-day sampling.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.52.3.289","usgsCitation":"Canney, F.C., Myers, A., and Ward, F.N., 1957, A truckmounted spectrographic laboratory for use in geochemical exploration: Economic Geology, v. 52, no. 3, p. 289-306, https://doi.org/10.2113/gsecongeo.52.3.289.","productDescription":"18 p.","startPage":"289","endPage":"306","costCenters":[],"links":[{"id":380484,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"3","noUsgsAuthors":false,"publicationDate":"1957-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Canney, Frank C.","contributorId":91251,"corporation":false,"usgs":true,"family":"Canney","given":"Frank","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":804786,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Myers, A.T.","contributorId":8468,"corporation":false,"usgs":true,"family":"Myers","given":"A.T.","email":"","affiliations":[],"preferred":false,"id":804787,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ward, F. N.","contributorId":96254,"corporation":false,"usgs":true,"family":"Ward","given":"F.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":804788,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70216352,"text":"70216352 - 1957 - Ezcurrite (2Na 2 O.5B 2 O 3 .7H 2 O), a new sodium borate from Argentina; occurrence, mineralogy, and associated minerals","interactions":[],"lastModifiedDate":"2020-11-12T20:29:57.094966","indexId":"70216352","displayToPublicDate":"1957-11-12T14:24:24","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Ezcurrite (2Na 2 O.5B 2 O 3 .7H 2 O), a new sodium borate from Argentina; occurrence, mineralogy, and associated minerals","docAbstract":"<p><span>Describes ezcurrite from a pluglike deposit of recrystallized borax at the Tincalayu mine in Salta, Argentina, and attributes its origin, together with that of associated kernite which it closely resembles, to crystallization from solutions released by dehydration of borax at elevated temperatures during deformation.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.52.4.426","usgsCitation":"Muessig, S., and Allen, R., 1957, Ezcurrite (2Na 2 O.5B 2 O 3 .7H 2 O), a new sodium borate from Argentina; occurrence, mineralogy, and associated minerals: Economic Geology, v. 52, no. 4, p. 426-437, https://doi.org/10.2113/gsecongeo.52.4.426.","productDescription":"12 p.","startPage":"426","endPage":"437","costCenters":[],"links":[{"id":380483,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Argentina","otherGeospatial":"Tincalayu","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -67.09899902343749,\n              -25.477992320574803\n            ],\n            [\n              -66.7474365234375,\n              -25.477992320574803\n            ],\n            [\n              -66.7474365234375,\n              -25.14031191468073\n            ],\n            [\n              -67.09899902343749,\n              -25.14031191468073\n            ],\n            [\n              -67.09899902343749,\n              -25.477992320574803\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"4","noUsgsAuthors":false,"publicationDate":"1957-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Muessig, Siegfried","contributorId":22012,"corporation":false,"usgs":true,"family":"Muessig","given":"Siegfried","affiliations":[],"preferred":false,"id":804784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Allen, R.D.","contributorId":244851,"corporation":false,"usgs":false,"family":"Allen","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":804785,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216351,"text":"70216351 - 1957 - Some limitations on the possible composition of the ore-forming fluid","interactions":[],"lastModifiedDate":"2020-11-12T20:22:26.929129","indexId":"70216351","displayToPublicDate":"1957-11-12T14:16:24","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Some limitations on the possible composition of the ore-forming fluid","docAbstract":"<p><span>The activity ratios of various important anions (S (super =) , CO&nbsp;</span><sub>3</sub><span>&nbsp;(super =) , SO&nbsp;</span><sub>4</sub><span>&nbsp;(super =) , OH (super -) , F (super -) , and Cl (super -) ) in hydrothermal solutions at the time of deposition are evaluated using a simple thermodynamic technique. The ratios are interpreted in the light of the mineralogy of ore deposits and limits are placed on the variability of each ratio in hydrothermal solutions. All of the calculations are made for 25 degrees C and cautious extrapolation to higher temperatures seems justified; however, additional data for elevated temperatures and pressures are needed before more than approximate values may be assigned to these ratios in the ore-forming fluid.The calculated partial pressure of CO&nbsp;</span><sub>2</sub><span>&nbsp;in the ore fluid is generally less than one atmosphere, which suggests that a dense CO&nbsp;</span><sub>2</sub><span>&nbsp;phase cannot be considered an important ore fluid for most deposits. The partial pressure of H&nbsp;</span><sub>2</sub><span>&nbsp;S is usually less than 10 (super -4) atmosphere, which makes it extremely difficult to defend the theory that metals (other than the easily complexible mercury, arsenic, antimony, and perhaps gold and silver) are transported in quantity as complex sulfides or hydrosulfides. The sulfate to sulfide ratio is such that the oxidation potential at the time of deposition is defined by the following equation: Eh (in volts) = 0.22 + or - 0.04 - 0.059 pH.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.52.4.333","usgsCitation":"Barton, P., 1957, Some limitations on the possible composition of the ore-forming fluid: Economic Geology, v. 52, no. 4, p. 333-353, https://doi.org/10.2113/gsecongeo.52.4.333.","productDescription":"21 p.","startPage":"333","endPage":"353","costCenters":[],"links":[{"id":380482,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"4","noUsgsAuthors":false,"publicationDate":"1957-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Barton, Paul B.","contributorId":97128,"corporation":false,"usgs":true,"family":"Barton","given":"Paul B.","affiliations":[],"preferred":false,"id":804783,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70216350,"text":"70216350 - 1957 - Effects of radon in drill holes on gamma-ray logs","interactions":[],"lastModifiedDate":"2020-11-12T20:14:30.321964","indexId":"70216350","displayToPublicDate":"1957-11-12T14:03:39","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Effects of radon in drill holes on gamma-ray logs","docAbstract":"<p><span>Drill holes in uranium deposits in the Todilto limestone of Late Jurassic age near Grants, New Mexico, do not yield duplicate gamma-ray logs when probed at different times; some logs show equivalent uranium greatly in excess, in thickness and grade, of the chemical and laboratory radiometric analyses. Radon and its daughter products principally cause the discrepancies. Experimental work was undertaken by the writers to learn the relations of the radon to the uranium deposits and its behavior under different physical conditions. The work is based on the interpretation of about 600 gamma-ray logs, taken from 480 drill holes.Abnormally high amounts of radon, referred to here as contamination, ranged from barely detectable amounts to amounts that emitted as much radiation as ore-grade material. Most contaminated holes were in the higher-grade ore, and the contamination increased with elapsed time after drilling. Geologic conditions favorable for contamination by radon and its daughter products in drill holes are: proximity to uranium deposits and fractured or highly permeable rocks above the water table. Most drill holes can be decontaminated by blowing them out with compressed air or filling them with water. Water, however, tends to reduce the thickness-times-grade figures below the amounts determined in air.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.52.4.438","usgsCitation":"Hilpert, L.S., and Bunker, C.M., 1957, Effects of radon in drill holes on gamma-ray logs: Economic Geology, v. 52, no. 4, p. 438-455, https://doi.org/10.2113/gsecongeo.52.4.438.","productDescription":"18 p.","startPage":"438","endPage":"455","costCenters":[],"links":[{"id":380481,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New Mexico","otherGeospatial":"Near Grants","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -107.7923583984375,\n              35.160336728130346\n            ],\n            [\n              -107.38037109375,\n              35.160336728130346\n            ],\n            [\n              -107.38037109375,\n              35.43381992014202\n            ],\n            [\n              -107.7923583984375,\n              35.43381992014202\n            ],\n            [\n              -107.7923583984375,\n              35.160336728130346\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"52","issue":"4","noUsgsAuthors":false,"publicationDate":"1957-06-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hilpert, Lowell Sinclair","contributorId":117367,"corporation":false,"usgs":true,"family":"Hilpert","given":"Lowell","email":"","middleInitial":"Sinclair","affiliations":[],"preferred":false,"id":804781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bunker, Carl Maurice","contributorId":77526,"corporation":false,"usgs":true,"family":"Bunker","given":"Carl","email":"","middleInitial":"Maurice","affiliations":[],"preferred":false,"id":804782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216346,"text":"70216346 - 1957 - Occurrence of selenium in sulfides from some sedimentary rocks of the western United States","interactions":[],"lastModifiedDate":"2021-04-07T13:37:54.138927","indexId":"70216346","displayToPublicDate":"1957-11-12T13:37:12","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Occurrence of selenium in sulfides from some sedimentary rocks of the western United States","docAbstract":"<div class=\"article-section-wrapper js-article-section js-content-section  \"><p>Investigations of the minor- and trace-element content of sulfides associated with uranium ore deposits from sandstone-type deposits have shown that selenium commonly substitutes for sulfur. The Morrison formation and Entrada sandstone of Jurassic age and the Wind River formation of Eocene age seem to be seleniferous stratigraphic zones; sulfides deposited within these formations generally contain abnormal amounts of selenium. The selenium content of the pyrite, marcasite, and chalcocite is much greater than that reported in previously published data.Under the prevailing temperatures and pressures of formation of the Colorado Plateau uranium deposits the maximum amount of Se substituting for S in the pyrite structure was found to be 3 percent by weight. Ferroselite, the iron selenide (FeSe<span>&nbsp;</span><sub>2</sub><span>&nbsp;</span>), was found in two deposits on the Colorado Plateau and it was also established that galena (PbS) forms an isomorphous series with clausthalite (PbSe) in nature.During oxidation of the selenium-bearing sulfides and selenides from the Colorado Plateau and Wyoming, the selenium forms pinkish crusts of either monoclinic or hexagonal native selenium intergrown with soluble sulfates, suggesting that under \"normal\" oxidizing conditions native selenium is more stable than selenites or selenates. The above-normal selenium content of these sulfides from sedimentary rocks of Mesozoic and Tertiary age is significant. The high selenium in these sulfides is related to periods of volcanic and intrusive activity penecontemporaneous with the formation of the containing sediments.</p></div>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.52.5.499","usgsCitation":"Coleman, R.G., and Delevaux, M.H., 1957, Occurrence of selenium in sulfides from some sedimentary rocks of the western United States: Economic Geology, v. 52, no. 5, p. 499-527, https://doi.org/10.2113/gsecongeo.52.5.499.","productDescription":"29 p.","startPage":"499","endPage":"527","costCenters":[],"links":[{"id":480409,"rank":0,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://digital.library.unt.edu/ark:/67531/metadc1050213/","text":"External Repository"},{"id":380471,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, Colorado, New Mexico, Utah, Wyoming","otherGeospatial":"Western 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,{"id":70213492,"text":"70213492 - 1957 - A definition of coal; reply","interactions":[],"lastModifiedDate":"2020-09-17T20:58:24.739663","indexId":"70213492","displayToPublicDate":"1957-08-01T15:56:52","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"A definition of coal; reply","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.52.5.585","usgsCitation":"Schopf, J., 1957, A definition of coal; reply: Economic Geology, v. 52, no. 5, p. 585-586, https://doi.org/10.2113/gsecongeo.52.5.585.","productDescription":"2 p.","startPage":"585","endPage":"586","costCenters":[],"links":[{"id":378549,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"5","noUsgsAuthors":false,"publicationDate":"1957-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Schopf, James M.","contributorId":94297,"corporation":false,"usgs":true,"family":"Schopf","given":"James M.","affiliations":[],"preferred":false,"id":799137,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70213491,"text":"70213491 - 1957 - A definition of coal","interactions":[],"lastModifiedDate":"2020-09-17T20:56:10.150794","indexId":"70213491","displayToPublicDate":"1957-08-01T15:53:21","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"A definition of coal","docAbstract":"<p><span>In reply to critical discussion, restates and clarifies the definition of coal given in a glossary of terms pertaining to coals, bitumens, and related carbonaceous materials.</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.52.5.584","usgsCitation":"Tomkeieff, S.I., 1957, A definition of coal: Economic Geology, v. 52, no. 5, p. 584-585, https://doi.org/10.2113/gsecongeo.52.5.584.","productDescription":"2 p.","startPage":"584","endPage":"585","costCenters":[],"links":[{"id":378548,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"52","issue":"5","noUsgsAuthors":false,"publicationDate":"1957-08-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Tomkeieff, S. I.","contributorId":240921,"corporation":false,"usgs":false,"family":"Tomkeieff","given":"S.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":799136,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37804,"text":"37804 - 1957 - Availability of surplus big-game animals on National Wildlife Refuges","interactions":[],"lastModifiedDate":"2014-07-24T09:22:04","indexId":"37804","displayToPublicDate":"1957-08-01T09:21:35","publicationYear":"1957","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":"390","title":"Availability of surplus big-game animals on National Wildlife Refuges","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1957, Availability of surplus big-game animals on National Wildlife Refuges (Supersedes Wildlife Leaflet 341 (1952).): Wildlife Leaflet 390, 6 p.","productDescription":"6 p.","numberOfPages":"6","costCenters":[],"links":[{"id":290856,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Supersedes Wildlife Leaflet 341 (1952).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f3e4b0824b2d177086","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221450,"text":"70221450 - 1957 - Hypothesis regarding the origin of thinolite tufa at Pyramid Lake, Nevada","interactions":[],"lastModifiedDate":"2021-06-16T13:14:30.698161","indexId":"70221450","displayToPublicDate":"1957-06-16T08:10:39","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Hypothesis regarding the origin of thinolite tufa at Pyramid Lake, Nevada","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1957)68[1683:HRTOOT]2.0.CO;2","usgsCitation":"Radbruch, D.H., 1957, Hypothesis regarding the origin of thinolite tufa at Pyramid Lake, Nevada: GSA Bulletin, v. 68, no. 12, p. 1683-1688, https://doi.org/10.1130/0016-7606(1957)68[1683:HRTOOT]2.0.CO;2.","productDescription":"6 p.","startPage":"1683","endPage":"1688","costCenters":[],"links":[{"id":386527,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Pyramid Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -119.83337402343749,\n              39.82119422647453\n            ],\n            [\n              -119.2950439453125,\n              39.82119422647453\n            ],\n            [\n              -119.2950439453125,\n              40.225024210604964\n            ],\n            [\n              -119.83337402343749,\n              40.225024210604964\n            ],\n            [\n              -119.83337402343749,\n              39.82119422647453\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"68","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Radbruch, Dorothy H.","contributorId":65874,"corporation":false,"usgs":true,"family":"Radbruch","given":"Dorothy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":817749,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221359,"text":"70221359 - 1957 - Thermal waters of volcanic origin","interactions":[],"lastModifiedDate":"2021-06-11T13:23:35.475772","indexId":"70221359","displayToPublicDate":"1957-06-11T08:20:28","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Thermal waters of volcanic origin","docAbstract":"<p>Waters of widely differing chemical compositions have been considered at least in part volcanic in origin, and are commonly associated with each other in the same area. Do any or all of these types contain volcanic components, and if so, how are the different types derived?</p><p>To determine the probable characteristics of volcanic waters, the writer has selected hot-spring groups that are particularly high in temperature and associated heat flow, are associated with late Tertiary or Quaternary volcanism, and are therefore most likely to contain some water and chemical components of direct volcanic origin. Of the different types of water that occur in these groups, one of the most common is characterized chemically by a dominance of sodium chloride.</p><p>Isotopic evidence indicates that the contribution of water of direct volcanic origin is not large and is probably no more than 5 per cent in typical sodium-chloride springs.</p><p>The compositions of volcanic waters are believed to be determined by: [1] type of magma and stage of crystallization; [2] temperature and pressure of the emanation at different stages during and after departure from the magma; [3] chemical composition, relative quantity, and depth of penetration of mixing meteoric water and water of other origin; and [4] reactions with wall rocks. Although the type of magma and its stage of crystallization are of major interest and have been emphasized in the past, the outstanding characteristics of volcanic emanations at and near the surface of the earth seem to be controlled for the most part by the other factors.</p><p>Nonvolatile compounds are slightly to highly soluble in steam at high pressure, and high-density steam has solvent properties similar to those of liquid water. In the volcanic sodium-chloride waters, the high ratio of lithium to sodium and potassium is shown to indicate that alkalies were transported as alkali halides dissolved in a dense vapor. This in turn demands a deep circulation of meteoric water for steam to condense at high pressure and for the halides to remain in solution. The depth of circulation of meteoric water in the sodium-chloride spring systems is believed to be in the order of 2 miles. Where circulation of meteoric water is shallow, the vapors rise and expand at low pressure, which does not permit transport of substances of low volatility; some type of water other than the sodium-chloride type is formed. The common volcanic sodium-chloride waters are therefore concluded to be the diluted product of high-density emanations, modified by reactions with wall rocks and by precipitation of the less soluble components.</p><p>Emanations at high temperature and relatively low pressure consist almost entirely of steam and volatile components. Their compositions are therefore relatively simple, and their ability to transport matter of low volatility is very limited.</p><p>The sodium-chloride type is probably gradational into acid-sulfate-chloride waters. There is some evidence that, under conditions not well understood, sulfur may be emitted as SO<sub>2</sub>, SO<sub>3</sub>, or other sulfur species of intermediate valence, rather than as H<sub>2</sub>S or S. Other major types of volcanic waters are called sodium bicarbonate, acid sulfate, and calcium bicarbonate; the first two tend to be distinct, but the calcium-bicarbonate type clearly grades into the sodium-chloride type. The writer concludes that, in general, all these are derived from the sodium-chloride waters as a result of physical environment or of reactions with wall rocks.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1957)68[1637:TWOVO]2.0.CO;2","usgsCitation":"White, D.E., 1957, Thermal waters of volcanic origin: GSA Bulletin, v. 68, no. 12, p. 1637-1658, https://doi.org/10.1130/0016-7606(1957)68[1637:TWOVO]2.0.CO;2.","productDescription":"22 p.","startPage":"1637","endPage":"1658","costCenters":[],"links":[{"id":386422,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817420,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221358,"text":"70221358 - 1957 - Magmatic, connate, and metamorphic waters","interactions":[],"lastModifiedDate":"2021-06-11T13:17:43.45072","indexId":"70221358","displayToPublicDate":"1957-06-11T08:14:41","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Magmatic, connate, and metamorphic waters","docAbstract":"<p>Some major types of water of “deep” origin are believed to be recognizable from their chemical and isotopic compositions. Oil-field brines dominated by sodium and calcium chlorides differ markedly from average ocean water. In general, the brines are believed to be connate in origin (“fossil” sea water) with a negligible to high proportion of meteoric water. Many brines, particularly in pre-Tertiary rocks, are much higher in salinity than sea water and are greatly enriched in calcium as well as sodium chloride. Brines near the salinity of sea water are generally higher, relative to sea water, in bicarbonate, iodine, boron, lithium, silica, ammonium, and water-soluble organic compounds, and lower in sulfate, potassium, and magnesium.</p><p>Many changes take place after sea water is entrapped in newly deposited marine sediments: (1) Iodine, silicon, boron, nitrogen, and other elements have been selectively concentrated in organisms that decompose during and after burial in sediments. Many of the elements may redissolve in the interstitial water. (2) Bacteria are active in the sediments and reduce sulfate to sulfide and produce methane, ammonia, carbon dioxide, and other products. (3) Some elements have been selectively removed from sea water by inorganic processes, such as adsorption on clays and colloidal matter. When this matter is reconstituted by diagenetic and other changes, some components are redissolved. The abundance of lithium and possibly boron and other elements may be controlled to a considerable extent by these inorganic processes. (4) The interstitial water may react chemically with enclosing sediments and produce dolomite, reconstituted clays, and other minerals. The high loss of magnesium relative to calcium in most connate waters is probably caused by such reactions.</p><p>Volcanic hot-spring waters of different compositions have been discussed in an accompanying paper (White, 1957). The most significant type is believed to be dominated by sodium chloride, and is best explained as originating from dense gases driven at high temperature and pressure from magma and containing much matter of low volatility that is in solution because of the solvent properties of high-density steam. This dense vapor is condensed in and greatly diluted by deeply circulating meteoric water. Most other types of volcanic water are believed to be derived from the sodium-chloride type.</p><p>Volcanic sodium-chloride waters are similar in many respects to connate waters but are believed to be distinguishable by relatively high lithium, fluorine, silica, boron, sulfur, CO<sub>2</sub>, arsenic, and antimony; by relatively low calcium and magnesium; and by lack of hydrocarbons, water-soluble organic compounds, and perhaps ammonia and nitrate. Relatively high boron and combined CO<sub>2</sub><span>&nbsp;</span>are alone not reliable indicators of a volcanic origin.</p><p>During compaction, rocks lose most of their interstitial high-chloride water; much additional water may then be lost during progressive metamorphism, and the content changes from about 5 per cent in shale to perhaps 1 per cent in gneiss. This expelled water is here called metamorphic. Because of pressure and permeability gradients, it must normally escape upward and mix with connate and meteoric water. Even though large quantities must exist, no example of metamorphic water has been positively identified.</p><p>Some thermal springs in California are high in salinity and relatively low in temperature and apparent associated heat flow. Some are clearly connate in origin. Other springs are characterized by very high combined carbon dioxide and boron, relative to chloride. Their compositions are considerably different from known connate and volcanic waters and are believed to be best explained by a metamorphic origin.</p><p>Although some major types of deep water seem to be recognizable, there is much danger of oversimplifying the problems. Many waters are no doubt mixtures of different types, and some of high salinity result from dissolution of salts by meteoric water.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1957)68[1659:MCAMW]2.0.CO;2","usgsCitation":"White, D.E., 1957, Magmatic, connate, and metamorphic waters: GSA Bulletin, v. 68, no. 12, p. 1659-1682, https://doi.org/10.1130/0016-7606(1957)68[1659:MCAMW]2.0.CO;2.","productDescription":"24 p.","startPage":"1659","endPage":"1682","costCenters":[],"links":[{"id":386420,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"White, Donald E.","contributorId":76787,"corporation":false,"usgs":true,"family":"White","given":"Donald","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":817419,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221356,"text":"70221356 - 1957 - Thermal effects of the ocean on permafrost","interactions":[],"lastModifiedDate":"2021-06-11T13:04:31.142961","indexId":"70221356","displayToPublicDate":"1957-06-11T08:01:44","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Thermal effects of the ocean on permafrost","docAbstract":"<p>In high latitudes the large difference between the mean annual temperature at the ground surface and in the unfrozen sediments beneath bodies of water can affect ground temperatures to depths of several hundred feet. The effect is of particular interest near the edge of the ocean where it depends upon the magnitude of the temperature difference between the land surface and ocean bottom, the thermal properties of the ground materials, and past changes in climate and/or shore-line configuration. Theoretical considerations suggest that, except where there are transgressing shore lines, permafrost to depths greater than about 100 feet beneath the ocean bottom is not to be expected at points farther than a few thousand feet offshore. Similar considerations indicate that geothermal installations along the Arctic coast can give information regarding post-Pleistocene shore-line changes.</p><p>The geothermal effects of bodies of water offer an explanation for the anomalously large outward earth-heat flow recently reported by A. D. Misener for Resolute Bay, Cornwallis Island, N. W. T., Canada.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1957)68[1515:TEOTOO]2.0.CO;2","usgsCitation":"Lachenbruch, A.H., 1957, Thermal effects of the ocean on permafrost: GSA Bulletin, v. 68, no. 11, p. 1515-1530, https://doi.org/10.1130/0016-7606(1957)68[1515:TEOTOO]2.0.CO;2.","productDescription":"16 p.","startPage":"1515","endPage":"1530","costCenters":[],"links":[{"id":386416,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"68","issue":"11","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Lachenbruch, Arthur H.","contributorId":27850,"corporation":false,"usgs":true,"family":"Lachenbruch","given":"Arthur","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":817416,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70221173,"text":"70221173 - 1957 - Colorimetric estimation of milligram quantities of inorganic azides","interactions":[],"lastModifiedDate":"2021-06-04T13:17:45.382283","indexId":"70221173","displayToPublicDate":"1957-06-04T08:16:20","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Colorimetric estimation of milligram quantities of inorganic azides","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"American Chemical Society","doi":"10.1021/ac60125a037","usgsCitation":"Roberson, C.E., and Austin, C., 1957, Colorimetric estimation of milligram quantities of inorganic azides: Analytical Chemistry, v. 29, no. 5, p. 854-855, https://doi.org/10.1021/ac60125a037.","productDescription":"2 p.","startPage":"854","endPage":"855","costCenters":[],"links":[{"id":386203,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"5","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Roberson, Charles Elmer","contributorId":79451,"corporation":false,"usgs":true,"family":"Roberson","given":"Charles","email":"","middleInitial":"Elmer","affiliations":[],"preferred":false,"id":816950,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Austin, Calvin","contributorId":259279,"corporation":false,"usgs":false,"family":"Austin","given":"Calvin","email":"","affiliations":[],"preferred":false,"id":816951,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37803,"text":"37803 - 1957 - Nutrias in the United States","interactions":[],"lastModifiedDate":"2014-07-24T13:54:33","indexId":"37803","displayToPublicDate":"1957-06-01T13:54:03","publicationYear":"1957","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":"389","title":"Nutrias in the United States","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1957, Nutrias in the United States (Revises and updates Wildlife Leaflet 319 (1949).): Wildlife Leaflet 389, 11 p.","productDescription":"11 p.","numberOfPages":"11","costCenters":[],"links":[{"id":290936,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises and updates Wildlife Leaflet 319 (1949).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f3e4b0824b2d177088","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529730,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37802,"text":"37802 - 1957 - Fur Catch in the United States, 1956","interactions":[],"lastModifiedDate":"2014-07-24T09:19:17","indexId":"37802","displayToPublicDate":"1957-06-01T09:18:30","publicationYear":"1957","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":"388","title":"Fur Catch in the United States, 1956","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled in Section of Wild Fur Animal Investigations, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"U.S. Branch of Wildlife Research, 1957, Fur Catch in the United States, 1956 (Succeeds Wildlife Leaflet 380 (1956).): Wildlife Leaflet 388, 3 p.","productDescription":"3 p.","numberOfPages":"3","costCenters":[],"links":[{"id":290855,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Succeeds Wildlife Leaflet 380 (1956).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f3e4b0824b2d17708a","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529729,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37801,"text":"37801 - 1957 - Big game inventory for 1955","interactions":[],"lastModifiedDate":"2014-07-24T09:16:17","indexId":"37801","displayToPublicDate":"1957-06-01T09:15:14","publicationYear":"1957","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":"387","title":"Big game inventory for 1955","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Compiled by Denver Wildlife Research Laborary, Branch of Wildlife Research, Bureau of Sport Fisheries and Wildlife.","usgsCitation":"Wildlife Research Laboratory, 1957, Big game inventory for 1955 (Reissued from Wildlife Leaflet 376 (1956) to fit 1955.): Wildlife Leaflet 387, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290854,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet 376 (1956) to fit 1955.","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f3e4b0824b2d17708c","contributors":{"authors":[{"text":"Wildlife Research Laboratory","contributorId":128030,"corporation":true,"usgs":false,"organization":"Wildlife Research Laboratory","id":529728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37875,"text":"37875 - 1957 - Ground squirrels and their control","interactions":[],"lastModifiedDate":"2014-07-22T10:04:41","indexId":"37875","displayToPublicDate":"1957-05-01T10:04:12","publicationYear":"1957","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":"356","title":"Ground squirrels and their control","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Fish and Wildlife Service, 1957, Ground squirrels and their control: Wildlife Leaflet 356, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290666,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f3e4b0824b2d17708e","contributors":{"authors":[{"text":"U.S. Fish and Wildlife Service","contributorId":128143,"corporation":true,"usgs":false,"organization":"U.S. Fish and Wildlife Service","id":529753,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37798,"text":"37798 - 1957 - Refuge bird lists","interactions":[],"lastModifiedDate":"2014-07-24T09:09:33","indexId":"37798","displayToPublicDate":"1957-05-01T09:07:58","publicationYear":"1957","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":"384","title":"Refuge bird lists","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Sport Fisheries and Wildlife, 1957, Refuge bird lists: Wildlife Leaflet 384, 2 p.","productDescription":"2 p.","numberOfPages":"2","costCenters":[],"links":[{"id":290853,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f4e4b0824b2d177090","contributors":{"authors":[{"text":"U.S. Bureau of Sport Fisheries and Wildlife","contributorId":128149,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Sport Fisheries and Wildlife","id":529727,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37797,"text":"37797 - 1957 - Public use of National Wildlife Refuges, 1956","interactions":[],"lastModifiedDate":"2014-07-24T09:06:21","indexId":"37797","displayToPublicDate":"1957-05-01T09:05:49","publicationYear":"1957","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":"383","title":"Public use of National Wildlife Refuges, 1956","docAbstract":"No abstract available.","language":"English","publisher":"U.s. Department of the Interior","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Branch of Wildlife Refuges, 1957, Public use of National Wildlife Refuges, 1956 (Reissued from Wildlife Leaflet 375 (1956).): Wildlife Leaflet 383, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290852,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Reissued from Wildlife Leaflet 375 (1956).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd3f4e4b0824b2d177092","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Refuges","contributorId":127986,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Refuges","id":529726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":5220906,"text":"5220906 - 1957 - A summer whistling cock count of bobwhite quail as an index to wintering populations","interactions":[],"lastModifiedDate":"2025-01-31T17:04:37.584418","indexId":"5220906","displayToPublicDate":"1957-04-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2508,"text":"Journal of Wildlife Management","active":true,"publicationSubtype":{"id":10}},"title":"A summer whistling cock count of bobwhite quail as an index to wintering populations","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Wiley","doi":"10.2307/3797580","usgsCitation":"Rosene, W., 1957, A summer whistling cock count of bobwhite quail as an index to wintering populations: Journal of Wildlife Management, v. 21, no. 2, p. 153-158, https://doi.org/10.2307/3797580.","productDescription":"6 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