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,{"id":70170554,"text":"70170554 - 1962 - Instructions for US P-61-A1 suspended-sediment sampler","interactions":[],"lastModifiedDate":"2018-03-05T12:28:54","indexId":"70170554","displayToPublicDate":"1962-01-01T13:45:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":66,"text":"Report","active":false,"publicationSubtype":{"id":1}},"title":"Instructions for US P-61-A1 suspended-sediment sampler","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Federal Interagency Sedimentation Project","publisherLocation":"Vickburg, MS","usgsCitation":"Colby, V., and Witzgman, F., 1962, Instructions for US P-61-A1 suspended-sediment sampler: Report, 9 p.","productDescription":"9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":320513,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"571f3fbee4b071321fe56a42","contributors":{"authors":[{"text":"Colby, V.C.","contributorId":168886,"corporation":false,"usgs":false,"family":"Colby","given":"V.C.","email":"","affiliations":[],"preferred":false,"id":627601,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Witzgman, F.W.","contributorId":168892,"corporation":false,"usgs":false,"family":"Witzgman","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":627602,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":37736,"text":"37736 - 1962 - Fur catch in the United States, 1961","interactions":[],"lastModifiedDate":"2014-07-22T13:26:02","indexId":"37736","displayToPublicDate":"1962-01-01T13:25:11","publicationYear":"1962","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":"444","title":"Fur catch in the United States, 1961","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Department of the Interior","publisherLocation":"Washington, D.C.","collaboration":"Complied in Bird and Mammal Laboratories, Branch of Wildlife Research.","usgsCitation":"U.S. Branch of Wildlife Research, 1962, Fur catch in the United States, 1961 (Updates Wildlife Leaflet BS-140 (1939).): Wildlife Leaflet 444, 3 p.","productDescription":"3 p.","numberOfPages":"3","temporalStart":"1961-01-01","temporalEnd":"1961-12-31","costCenters":[],"links":[{"id":290718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Updates Wildlife Leaflet BS-140 (1939).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffd085e4b0824b2d1763f6","contributors":{"authors":[{"text":"U.S. Branch of Wildlife Research","contributorId":127903,"corporation":true,"usgs":false,"organization":"U.S. Branch of Wildlife Research","id":529689,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207379,"text":"70207379 - 1962 - Metallogenetic provinces of Chile, S. A","interactions":[],"lastModifiedDate":"2019-12-19T08:03:37","indexId":"70207379","displayToPublicDate":"1962-01-01T13:13:11","publicationYear":"1962","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":"Metallogenetic provinces of Chile, S. A","docAbstract":"<p><span>The metalliferous deposits of Chile tend to be restricted to well denned metallogenetic provinces, each characterized by a dominant mineral or mineral assemblage. The most important ore deposits are those of copper, iron, silver, gold, and manganese. The primary minerals are few in number and most are simple sulfides and oxides; more complex sulfosalts are scarce. Secondary minerals in great variety are important constituents of the ores. Many of the ore deposits are situated along well defined structural lines, several hundred kilometers long, that parallel the structural grain of the Andes.The deposits, with few exceptions, are found in sedimentary or volcanic rocks that range in age from Jurassic to Late Cretaceous or in intrusive rocks of Late Jurassic to Late Cretaceous age. Most deposits are genetically related to intrusive bodies, which have an average composition within the range of granite-diorite.The metalliferous deposits can be classed as hydrothermal, sedimentary, contact-metasomatic and magmatic. Copper deposits are typically hydro-thermal, manganese deposits are sedimentary, and most of the iron ore deposits are contact-metasomatic. A unique group of iron ore deposits apparently formed by near-surface intrusion and surface flows of a magma consisting of iron oxides. Hydrothermal deposits, the most abundant and most important economically, were formed under conditions ranging from low to high temperature and pressure. © 1962 Society of Economic Geologists, Inc.</span></p>","language":"English","publisher":"Society of Economic Geologists ","doi":"10.2113/gsecongeo.57.1.91","issn":"03610128","usgsCitation":"Martinez-Ruiz, F., and Ericksen, G.E., 1962, Metallogenetic provinces of Chile, S. A: Economic Geology, v. 57, no. 1, p. 91-106, https://doi.org/10.2113/gsecongeo.57.1.91.","productDescription":"16 p. 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,{"id":70114641,"text":"70114641 - 1962 - Records of wells and ground-water quality in Burlington County, New Jersey","interactions":[],"lastModifiedDate":"2014-07-15T14:06:04","indexId":"70114641","displayToPublicDate":"1962-01-01T13:09:22","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"title":"Records of wells and ground-water quality in Burlington County, New Jersey","docAbstract":"<This basic-data report is limited to the presentation of selected drillers' logs and their geologic correlations, well data, and chemical analyses of water from wells in Burlington County, N. J.  The county lies within the Coastal Plain province; it is underlain by unconsolidated sediments of Quarternary, Tertiary, and Cretaceous age and at great depth by much older consolidated rocks.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70114641","collaboration":"Prepared in cooperation with the State of New Jersey","usgsCitation":"Rush, F.E., 1962, Records of wells and ground-water quality in Burlington County, New Jersey, iii, 104 p., https://doi.org/10.3133/70114641.","productDescription":"iii, 104 p.","numberOfPages":"111","costCenters":[],"links":[{"id":290162,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":290160,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70114641/report.pdf"}],"country":"United States","state":"New Jersey","county":"Burlington County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.059913,39.540837 ], [ -75.059913,40.184235 ], [ -74.38979,40.184235 ], [ -74.38979,39.540837 ], [ -75.059913,39.540837 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53ad40f9e4b0729c154181d4","contributors":{"authors":[{"text":"Rush, F. Eugene","contributorId":16821,"corporation":false,"usgs":true,"family":"Rush","given":"F.","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":495391,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70211240,"text":"70211240 - 1962 - Tectonic map of the United States, exclusive of Alaska and Hawaii","interactions":[],"lastModifiedDate":"2020-07-22T14:19:18.641872","indexId":"70211240","displayToPublicDate":"1962-01-01T11:29:57","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Tectonic map of the United States, exclusive of Alaska and Hawaii","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70211240","usgsCitation":"U.S. Geological Survey, and American Association of Petroleum Geologists, 1962, Tectonic map of the United States, exclusive of Alaska and Hawaii, HTML Document, https://doi.org/10.3133/70211240.","productDescription":"HTML 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,{"id":70202536,"text":"70202536 - 1962 - Report on the Geological Survey Library: its history, technical work, resources, management","interactions":[],"lastModifiedDate":"2019-03-18T10:25:39","indexId":"70202536","displayToPublicDate":"1962-01-01T11:25:13","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Report on the Geological Survey Library: its history, technical work, resources, management","docAbstract":"<p>One of the limitations under which any library operates is the image it creates as a storehouse, This aspect can obscure the purposes and activities which make one library differ from another. In an institutional library, like the Survey's, the library purposes are related to the changing life of the organization, and to the world of ideas and facts it mirrors.</p><p>What goes on inside the Survey Library is understandable only in part from the standard practices it shares with other libraries as we view them today. For the other part, deeply rooted in the history and traditions of the organization, the understanding arises from the history that has made it what it is. This report will first provide, therefore, an historical sketch of the Survey Library with particular reference to its development over three quarters of a century, to the philosophy of librarianship that has animated it, and to the future growth to which it is committed.</p><p>By design and history, the Survey Library is a special library, maintained primarily for the benefit of Survey workers. This report will review the main routines and characteristics of the \"special\" aspects of the library operations.</p><p>Personnel and funds of the library have increased many..fold during the past decade, roughly parallel to the growth of the Geological Survey.&nbsp;This expansion is in sharp contrast to a long span of lean years when the library piled up a backlog of tasks partly finished or not done at all because of limited funds and staff. This report will describe the resources in personnel, funds, equipment and space available in the past and now to the library, their sufficiency, and the outlook for future growth. It will be demonstrated that the library's need for resources will continue to expand for reasons that are partly independent of any future growth of Survey employment.</p><p>Finally, against the background of history, functions, resources and problems described the report will attempt to express some measure of effectiveness for the management of the library. A measure of effectiveness is simply an expression of the degree to which a system fulfills its objectives.</p><p>Throughout this study, the aim has been to develop a body of systematic information about the various activities of the library for uses and judgements that go beyond immediate concerns. No such examination of this important area of the Survey's activities has been undertaken in recent decades, and none whatever in a context of changes such as those of the past decade. Yet the period of most profound change seems to lie ahead, seeded by explorations in the field of information storage and retrieval and forced by the volume of information in the various branches of science.</p><p>Acknowledgment of the cooperation given by the Chief Librarian and members of the library staff during the preparation of this report is gratefully made. It is not an easy task for members of an organization to open up their operating field to the questions and judgments of a&nbsp;staff member outside that organization. The willingness to do so, in the face of queries which have often suggested the need of change, is itself favorable to change when it becomes due and when it is sought by management.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70202536","usgsCitation":"Irving, W., 1962, Report on the Geological Survey Library: its history, technical work, resources, management, iv, 140 p., https://doi.org/10.3133/70202536.","productDescription":"iv, 140 p.","costCenters":[],"links":[{"id":362125,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70202536/report-thumb.jpg"},{"id":362126,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70202536/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Irving, W.C.","contributorId":214246,"corporation":false,"usgs":true,"family":"Irving","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":759440,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70095376,"text":"70095376 - 1962 - Generalized structure contour maps of the New Jersey coastal plain","interactions":[],"lastModifiedDate":"2014-03-25T10:35:02","indexId":"70095376","displayToPublicDate":"1962-01-01T10:06:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":112,"text":"Geologic report (New Jersey)","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"4","title":"Generalized structure contour maps of the New Jersey coastal plain","docAbstract":"Twelve generalized structural contour maps were prepared from a study of 169 well\nlogs or sample logs of drill cuttings from the Coastal Plain of New Jersey, Delaware, and\nthe E astern Shore of Maryland. The configuration of the tops of the nonmarine Cretaceous\ndeposits (Patuxent , Patapsco, Raritan, and Magothy formations) and the Piney Point Formation\n(Eocene) show the known subsurface extent of these formations in both New Jersey\nand Delaware. The structural contour maps show the tops of the Merchantville Formation\nand Woodbury Clay, the Englishtown Formation, the Marshalltown Formation, the Wenonah\nFormation and Mount Laurel Sand, the Navesink Forma ti on, and the Red Bank\nSand which are a ll of Late Cretaceous age. The maps of the Hornerstown Sand, the Vincentown\nFormation, and the Manasquan Formation and Shark River Marl of early Tertiary\nage show the subsurface extent of these formations only in New Jersey. Also included is an\noutline map showing the locations of wells and seismic station s and a structural contour map\nshowing the configuration of the bedrock surface of the report area.\nStructural contours on top of the Magothy Formation, or on the top of the Raritan Formation\nwhere the Magothy formation is absent, show the configuration of the nonmarine\ndeposits of Cretaceous age. Isopachs of the nonmarine deposits are derived by interpolation\nbetween contours on top of the bedrock and the top of either the Magothy Formation or the\nRaritan Formation where the Magothy is absent.\n\nThe Merchantville Formation and Woodbury Clay are difficult to separate in the subsurface,\nand therefore the contour a re drawn on top of the Woodbury Clay. In New Jersey,\nthe thickness of the combined Merchantville Form a ti on and Woodbury Clay ranges from\nab out 100 to 140 feet near the outcrop, but exceeds 250 feet in the subsurface along the\ncoast in Ocean County.\n\nThe top of the Englishtown Formation is easy to recognize because it generally consists\nof a micaceous white and yellow sand, although locally it is a silty clay . The formation\nthins toward the southwest from about 160 feet in central Ocean County to less than 20 feet\nin Salem County . It has not been recognized in Delaware.\n\nThe Marshalltown Formation varies from black clay to a glauconitic sand. It usually\nranges in thickness from 20 to 60 feet . It is very thin or absent in Delaware.\n\nThe Wenonah Formation and Mount Laurel and arc difficult to separate in New Jersey,\nand therefore are shown as a unit. The combined thickness range from 60 to 100) feet. In\nDelaware the two formations are easily separated.\n\nThe Navesink Formation is generally highly glauconitc and it is difficult to determine\nthe upper limit where overlain by the Hornerstown Sand which is also glauconitic. The contour\nmap on the top of the Navesink is based upon relatively little control.\n\nThe Red Bank Sand reaches a thickness of about 160 feet in Monmouth County. It thins\nsouthwestward and is absent in outcrop in the southern part of the Coastal Plain of New\nJersey. A probable equivalent of the Reel Bank has be recognized in Delaware. The Tinton\nSand Member is the topmost unit of the Red Bank and in Monmouth County.\n\nThe Hornerstown Sand is most glauconitic and is about 30 feet thick in outcrop. This\nis overlain by the Vincentown Formation which consists of two facies (1) calcareous sand\nfacies and (2) quartz sand facies. These a re overlain by the Manasquan Formation and\nShark River Marl which are here treated as a unit . In outcrop the combined thickness of the\nManasquan Formation and Shark River Marl is about 40 feet, but in the subsurface they\nthicken to about 200 feet. The Piney Point Formation of Jackson age occur in the subsurface\nin Cape May and Atlantic Counties, N.J. and in southern Delaware but is not\nexposed in these States.\nBrief notes are given on formation of later Tertiary and Pleistocene age , but no contour\nmaps were constructed.","language":"English","publisher":"New Jersey Deptartment of Conservation and Economic Development","publisherLocation":"Trenton, NJ","usgsCitation":"Richards, H.G., Olmsted, F.H., and Ruhle, J.L., 1962, Generalized structure contour maps of the New Jersey coastal plain: Geologic report (New Jersey) 4, iv, 38 p.","productDescription":"iv, 38 p.","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":283183,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70095376.jpg"},{"id":284834,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70095376/report.pdf"}],"country":"United States","state":"Delaware;New Jersey","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.9924,38.4977 ], [ -75.9924,40.1894 ], [ -73.9160,40.1894 ], [ -73.9160,38.4977 ], [ -75.9924,38.4977 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5355943ae4b0120853e8bf94","contributors":{"authors":[{"text":"Richards, Hoarce G.","contributorId":60124,"corporation":false,"usgs":true,"family":"Richards","given":"Hoarce","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":491182,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Olmsted, F. H.","contributorId":24765,"corporation":false,"usgs":true,"family":"Olmsted","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":491181,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ruhle, James L.","contributorId":22676,"corporation":false,"usgs":true,"family":"Ruhle","given":"James","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":491180,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":71774,"text":"tei821 - 1962 - Physical properties of evaporite minerals","interactions":[],"lastModifiedDate":"2014-06-11T08:48:06","indexId":"tei821","displayToPublicDate":"1962-01-01T09:37:00","publicationYear":"1962","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":"821","title":"Physical properties of evaporite minerals","docAbstract":"<p>The data in the following tables were abstracted from measurements of physical properties of evaporite minerals or of equivalent synthetic compounds. The compounds considered are the halide and sulfate salts which supposedly precipitated from evaporating ocean water and which form very extensive and thick \"rock salt\" beds. These beds are composed almost entirely of NaCl. In places where the beds are deeply buried and where fractures occur in the overlying rocks, the salt is plastically extruded upward as in a pipe to form the \"salt domes\".</p>\n<br>\n<p>\nMost of the tables are for NaCl, both the natural (halite) and the synthetic salt, polycrystalline and single crystals. These measurements have been collected for use 1) in studies on storage of radioactive wastes in salt domes or beds, 2) in calculations concerned with nuclear tests in salt domes and beds, and 3) in studies of phenomena in salt of geologic interest.</p>\n<br>\n<p>\nRather than an exhaustive compilation of physical property measurements, there tables represent a summary of data from accessible sources. As limitations of time have presented making a more systematic and comprehensive selection, the data given may seem arbitrarily chosen. Some of the data listed are old, and newer, more accurate data are undoubtedly available.</p>\n<br>\n<p>Halite (an synthetic NaCl) has been very thoroughly studied because of its relatively simple and highly symmetrical crystal structure, its easy availability naturally or synthetically, both in single crystals and polycrystalline, its useful and scientifically interesting properties, and its role as a compound of almost purely ionic bonding. The measurements of NaCl in the tables, however, represent only a small part of the total number of observations; discrimination was necessary to keep the size of the tabulations manageable. The physical properties of the evaporite minerals other than halite and sylvite have received only desultory attention of experiementalists, and appear in only a few tables.</p>\n<br>\n<p>The effects of temperature, hydrostatic pressure, stress difference, and other mechanical, eletrical, and optical conditions on the physical properties have probably been observed more completely on NaCl than on any other solid substance, which makes it a unique and important substance. Several new and important phenomena have been observed first on it. The mechanical properties of NaCl, for example, depend very strongly on the condition and the composition of the gas or liquid in contact with the sample surface; the data are sparse as yet and are not reported here.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/tei821","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission","usgsCitation":"Robertson, E.C., 1962, Physical properties of evaporite minerals: U.S. Geological Survey Trace Elements Investigations 821, 90 p., https://doi.org/10.3133/tei821.","productDescription":"90 p.","numberOfPages":"90","costCenters":[],"links":[{"id":288266,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":288265,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/tei/0821/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5385b3fbe4b09e18fc023a7b","contributors":{"authors":[{"text":"Robertson, Eugene C.","contributorId":71139,"corporation":false,"usgs":true,"family":"Robertson","given":"Eugene","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":284738,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70220665,"text":"70220665 - 1962 - Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","interactions":[],"lastModifiedDate":"2021-05-24T13:58:30.40077","indexId":"70220665","displayToPublicDate":"1962-01-01T08:53:59","publicationYear":"1962","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":"Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah","docAbstract":"<p><span>Uranium-vanadium&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the Salt Wash Member of the Morrison Formation&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Montezuma</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Canyon</span><span>, San Juan County,&nbsp;</span><span class=\"ScopusTermHighlight\">Utah</span><span>, exhibit zoning that is interpreted as a result of metal transport by&nbsp;</span><span class=\"ScopusTermHighlight\">diffusion</span><span>. The concentric zones consist of a brown nonmineralized core, an olive-gray mineralized shell, and a gray nonmineralized outer zone. The brown zone is iron-stained, porous sandstone commonly containing abundant carbonaceous material. The curved mineralized layer completely encloses the brown zone, and is composed of oxidized uranium-vanadium minerals that impregnate sandstone. The gray zone is light-gray sandstone tightly cemented with calcite and commonly freckled with limonitic specks.Formation of the&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;most likely took place during Late Cretaceous or early Tertiary time when the ore-bearing sandstones were deeply buried and saturated with connate waters. The concentration of organic material&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the brown zone suggests that this zone was once saturated with a reducing solution containing soluble organic compounds like alcohols and aldehydes derived from the organic material. The gray zone, on the other hand, was probably saturated with an oxidizing solution containing uranium and vanadium. Where these two solutions were&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;contact, oxidation-reduction reactions took place that caused the precipitation of low-valent uranium and vanadium minerals.The ellipsoidal shape of the ore layer and the lack of any exit or entrance for flowing solutions indicates that the dissolved metals moved through the gray zone by&nbsp;</span><span class=\"ScopusTermHighlight\">diffusion</span><span>&nbsp;and were precipitated at the periphery of the reducing zone. Recent weathering and oxidation have altered the primary low-valent minerals to high-valent forms without noticeable leaching of the ore metals.&nbsp;</span></p>","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.57.2.226","usgsCitation":"Huff, L., and Lesure, F., 1962, Diffusion features of uranium-vanadium deposits in Montezuma Canyon, Utah: Economic Geology, v. 57, no. 2, p. 226-237, https://doi.org/10.2113/gsecongeo.57.2.226.","productDescription":"12 p.","startPage":"226","endPage":"237","costCenters":[],"links":[{"id":385897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Montezuma Canyon","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.654541015625,\n              37.02886944696474\n            ],\n            [\n              -109.061279296875,\n              37.02886944696474\n            ],\n            [\n              -109.061279296875,\n              38.53957267203905\n            ],\n            [\n              -109.654541015625,\n              38.53957267203905\n            ],\n            [\n              -109.654541015625,\n              37.02886944696474\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"57","issue":"2","noUsgsAuthors":false,"publicationDate":"1962-03-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Huff, L.C.","contributorId":32919,"corporation":false,"usgs":true,"family":"Huff","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":816355,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lesure, F. G.","contributorId":7694,"corporation":false,"usgs":true,"family":"Lesure","given":"F. G.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":816356,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70227016,"text":"70227016 - 1962 - Diatremes and uranium deposits in the Hopi Buttes, Arizona","interactions":[],"lastModifiedDate":"2021-12-27T15:01:01.710863","indexId":"70227016","displayToPublicDate":"1962-01-01T08:45:58","publicationYear":"1962","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Diatremes and uranium deposits in the Hopi Buttes, Arizona","docAbstract":"<p>The Hopi Buttes diatremes erupted in a shallow lake that was filled in as volcanic activity progressed in Pliocene time. At the end of the period of volcanism the landscape included low lava domes capping some of the diatremes, a few flows, and numerous craters of the maar type, surrounded by rims of volcanic debris with gentle exterior slopes that merged with the surrounding plain. Erosion, probably chiefly during early and middle Pleistocene, has exposed the diatremes in varying stages of denudation.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Petrologic studies: A volume in honor of A. F. Buddington","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Geological Society of America","doi":"10.1130/Petrologic.1962.327","usgsCitation":"Shoemaker, E.M., Roach, C.H., and Byers, F., 1962, Diatremes and uranium deposits in the Hopi Buttes, Arizona, chap. <i>of</i> Petrologic studies: A volume in honor of A. F. Buddington, p. 327-355, https://doi.org/10.1130/Petrologic.1962.327.","productDescription":"29 p.","startPage":"327","endPage":"355","costCenters":[],"links":[{"id":393421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona","otherGeospatial":"Hopi Buttes","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.621337890625,\n              35.40808023595146\n            ],\n            [\n              -110.62545776367186,\n              35.226550551891116\n            ],\n            [\n              -110.36178588867188,\n              35.12664799144554\n            ],\n            [\n              -110.25741577148438,\n              35.107551518679074\n            ],\n            [\n              -110.09811401367188,\n              35.14349410278418\n            ],\n            [\n              -109.8577880859375,\n              35.34425514918409\n            ],\n            [\n              -109.86740112304688,\n              35.571331599581654\n            ],\n            [\n              -110.06240844726562,\n              35.83896829930447\n            ],\n            [\n              -110.32196044921874,\n              35.83451505415075\n            ],\n            [\n              -110.621337890625,\n              35.40808023595146\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"editors":[{"text":"Engel, A.E.J.","contributorId":241621,"corporation":false,"usgs":false,"family":"Engel","given":"A.E.J.","affiliations":[],"preferred":false,"id":829225,"contributorType":{"id":2,"text":"Editors"},"rank":1},{"text":"James, Harold L.","contributorId":88204,"corporation":false,"usgs":true,"family":"James","given":"Harold L.","affiliations":[],"preferred":false,"id":829226,"contributorType":{"id":2,"text":"Editors"},"rank":2},{"text":"Leonard, B. F.","contributorId":117454,"corporation":false,"usgs":true,"family":"Leonard","given":"B.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":829227,"contributorType":{"id":2,"text":"Editors"},"rank":3}],"authors":[{"text":"Shoemaker, Eugene Merle","contributorId":20342,"corporation":false,"usgs":true,"family":"Shoemaker","given":"Eugene","email":"","middleInitial":"Merle","affiliations":[],"preferred":false,"id":829222,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roach, C. H.","contributorId":12117,"corporation":false,"usgs":true,"family":"Roach","given":"C.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":829223,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Byers, F. M. Jr.","contributorId":270390,"corporation":false,"usgs":false,"family":"Byers","given":"F. M.","suffix":"Jr.","affiliations":[],"preferred":false,"id":829224,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70220651,"text":"70220651 - 1962 - Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","interactions":[],"lastModifiedDate":"2021-05-24T11:47:18.288311","indexId":"70220651","displayToPublicDate":"1962-01-01T06:43:05","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2420,"text":"Journal of Petrology","active":true,"publicationSubtype":{"id":10}},"title":"Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid","docAbstract":"<p><span>Geological and experimental evidence indicate that the three-phase field, plagioclase-alkalifeldspar-liquid, may terminate in several different ways. The possible&nbsp;</span><span class=\"ScopusTermHighlight\">terminations</span><span>&nbsp;have been developed from Schreinemakers' rules governing the disappearance of three-phase fields. In igncous rocks, these different&nbsp;</span><span class=\"ScopusTermHighlight\">terminations</span><span>&nbsp;may arise from variations in the relative amounts of additional components in magmas, or from changes of total pressure, or from structural changes that effect the extent of solid solution in feldspar.The three-phase&nbsp;</span><span class=\"ScopusTermHighlight\">region</span><span>&nbsp;originates from the intersection of the solidus and the feldspar solvus. The available evidence regarding this intersection is reviewed, as is the evidence for the existence and form of the boundary curve on the feldspar liquidus. The data are used to project a series of isobaric polythermal and isobaric isothermal diagrams for each possible&nbsp;</span><span class=\"ScopusTermHighlight\">termination</span><span>. Subsequent discussions relate the theoretical arguments to the natural evidence, suggest the more probable geological environments of some of the&nbsp;</span><span class=\"ScopusTermHighlight\">terminations</span><span>, and indicate characteristic features of each&nbsp;</span><span class=\"ScopusTermHighlight\">termination</span><span>.It may be possible to identify the type of&nbsp;</span><span class=\"ScopusTermHighlight\">termination</span><span>&nbsp;involved in the crystallization of some rocks. The necessary data are the amounts and compositions of both kinds of coexisting feldspars and of the feldspar components of the coexisting liquid at one or more stages of the crystallization process. Volcanic rocks are most suitable for such studies.The&nbsp;</span><span class=\"ScopusTermHighlight\">terminations</span><span>&nbsp;explain many of the compositional relationships possible between feldspar crystals and silicate melt under geological and experimental conditions. These compositional relationships are fundamental to understanding the crystallization of igneous rocks and the formation of melts by partial fusion. Other geological applications include a simple explanation for some resorbed feldspars, the separation, correlation, and comparison of porphyritic rock units, interpretation of compositional changes of successive zones of zoned feldspars, and mantling of one feldspar by another. With all types of&nbsp;</span><span class=\"ScopusTermHighlight\">termination</span><span>, extensive fractionation yields a liquid rich in Or and Ab that may crystallize to alkali feldspar or feldspars.&nbsp;</span></p>","language":"English","publisher":"Oxford University Press","doi":"10.1093/petrology/3.3.280","usgsCitation":"Stewart, D.B., and Roseboom, E.H., 1962, Lower temperature terminations of the three-phase region plagioclase-alkali feldspar-liquid: Journal of Petrology, v. 3, no. 3, p. 280-315, https://doi.org/10.1093/petrology/3.3.280.","productDescription":"36 p.","startPage":"280","endPage":"315","costCenters":[],"links":[{"id":385877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Stewart, D. B.","contributorId":41809,"corporation":false,"usgs":true,"family":"Stewart","given":"D.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":816300,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roseboom, E. H. Jr.","contributorId":40730,"corporation":false,"usgs":true,"family":"Roseboom","given":"E.","suffix":"Jr.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":816301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2002571,"text":"2002571 - 1962 - Whirling disease of trouts caused by Myxosoma cerebralis in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:15:01","indexId":"2002571","displayToPublicDate":"1962-01-01T01:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"427","title":"Whirling disease of trouts caused by Myxosoma cerebralis in the United States","docAbstract":"No abstract available at this time","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Special Scientific Report-Fisheries ","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"114/FH","usgsCitation":"Hoffman, G.L., Dunbar, C.E., and Bradford, A., 1962, Whirling disease of trouts caused by Myxosoma cerebralis in the United States: Special Scientific Report - Fisheries 427.","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":197749,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101761,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826016?urlappend=%3Bseq=13"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4938","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":326620,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":326622,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bradford, A.","contributorId":72486,"corporation":false,"usgs":true,"family":"Bradford","given":"A.","email":"","affiliations":[],"preferred":false,"id":326621,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":81353,"text":"81353 - 1962 - Use of mobile bioassay equipment in the chemical control of sea lamprey","interactions":[],"lastModifiedDate":"2023-04-04T15:41:19.291438","indexId":"81353","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"418","title":"Use of mobile bioassay equipment in the chemical control of sea lamprey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Howell, J.H., and Marquette, W.M., 1962, Use of mobile bioassay equipment in the chemical control of sea lamprey: Special Scientific Report - Fisheries 418, iv, 9 p.","productDescription":"iv, 9 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198475,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":101763,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://spo.nmfs.noaa.gov/content/use-mobile-bioassay-equipment-chemical-control-sea-lamprey","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6858a4","contributors":{"authors":[{"text":"Howell, John H.","contributorId":39720,"corporation":false,"usgs":true,"family":"Howell","given":"John","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":295278,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Marquette, William M.","contributorId":14920,"corporation":false,"usgs":true,"family":"Marquette","given":"William","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":295277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":81391,"text":"81391 - 1962 - Freshwater fish diseases caused by bacteria belonging to the genera Aeromonas and Pseudomonas: Revised","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"81391","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"459","title":"Freshwater fish diseases caused by bacteria belonging to the genera Aeromonas and Pseudomonas: Revised","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"768/FH","usgsCitation":"Snieszko, S.F., 1962, Freshwater fish diseases caused by bacteria belonging to the genera Aeromonas and Pseudomonas: Revised: Fishery Leaflet 459, 7 p.","productDescription":"7 p.","startPage":"0","endPage":"7","numberOfPages":"7","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198975,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b19e4b07f02db6a7f8a","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":295322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81382,"text":"81382 - 1962 - Whirling disease of trout","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81382","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"508","title":"Whirling disease of trout","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"664/FH","usgsCitation":"Hoffman, G.L., 1962, Whirling disease of trout: Fishery Leaflet 508, 3 p.","productDescription":"3 p.","startPage":"0","endPage":"3","numberOfPages":"3","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198185,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db543dcc","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70175632,"text":"70175632 - 1962 - Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas","interactions":[],"lastModifiedDate":"2016-08-17T13:58:13","indexId":"70175632","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5177,"text":"Edwards Underground Water District Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"1","title":"Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"Edwards Underground Water District","usgsCitation":"Garza, S., 1962, Chemical analysis of water from observation wells in the Edwards and associated limestones, San Antonio area, Texas: Edwards Underground Water District Bulletin 1, 56 p.","productDescription":"56 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326718,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57b58ac0e4b03bcb0104bb6e","contributors":{"authors":[{"text":"Garza, Sergio","contributorId":88713,"corporation":false,"usgs":true,"family":"Garza","given":"Sergio","email":"","affiliations":[],"preferred":false,"id":645896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2015,"text":"wsp1539N - 1962 - Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:52:29.473357","indexId":"wsp1539N","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"1539","chapter":"N","title":"Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539N","usgsCitation":"Keech, C.F., and Rosene, P.G., 1962, Ground-water resources of Hamilton County, Nebraska, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: v, 64 p.; 2 Plates: 14.76 x 23.80 inches and 27.00 x 38.440 inches, https://doi.org/10.3133/wsp1539N.","productDescription":"Report: v, 64 p.; 2 Plates: 14.76 x 23.80 inches and 27.00 x 38.440 inches","costCenters":[],"links":[{"id":109981,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24736.htm","linkFileType":{"id":5,"text":"html"},"description":"24736"},{"id":27481,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539n/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27480,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539n/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":27479,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539n/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137583,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539n/report-thumb.jpg"}],"country":"United States","state":"Nebraska","county":"Hamilton County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-97.8283,41.1733],[-97.8276,41.0467],[-97.8245,40.6985],[-97.9385,40.6981],[-98.278,40.6987],[-98.2829,40.6992],[-98.2829,40.8725],[-98.2443,40.9044],[-98.2187,40.9308],[-98.192,40.9444],[-98.1707,40.9588],[-98.1318,40.9964],[-98.1109,41.0068],[-98.1082,41.0031],[-98.1,41.0075],[-98.0856,41.0114],[-98.0647,41.0307],[-98.0384,41.0469],[-98.0404,41.0486],[-98.0189,41.066],[-97.9781,41.0895],[-97.9745,41.0851],[-97.9638,41.0866],[-97.9366,41.095],[-97.9299,41.0992],[-97.9309,41.1007],[-97.9116,41.1047],[-97.8916,41.1118],[-97.8633,41.134],[-97.8367,41.1618],[-97.8283,41.1733]]]},\"properties\":{\"name\":\"Hamilton\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d71c","contributors":{"authors":[{"text":"Keech, Charles Franklin","contributorId":44123,"corporation":false,"usgs":true,"family":"Keech","given":"Charles","email":"","middleInitial":"Franklin","affiliations":[],"preferred":false,"id":144533,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rosene, P. G.","contributorId":22192,"corporation":false,"usgs":true,"family":"Rosene","given":"P.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144532,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010519,"text":"70010519 - 1962 - Bedrock geology of the Thiel Mountains, Antarctica","interactions":[],"lastModifiedDate":"2017-05-10T15:52:48","indexId":"70010519","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Bedrock geology of the Thiel Mountains, Antarctica","docAbstract":"<p><span>Cordierite-bearing, hyper-sthene-quartz monzonite porphyry, the most widespread rock unit, is intruded by biotite granite and porphyritic biotite granite. Sedimentary and metasedimentary rocks, mainly quartzites and argillites, have been metamorphosed locally to hornfels and have been involved in high-angle faulting. Shear zones are common in the plutonic rocks.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.137.3532.751","issn":"00368075","usgsCitation":"Ford, A.B., and Aaron, J., 1962, Bedrock geology of the Thiel Mountains, Antarctica: Science, v. 137, no. 3532, p. 751-752, https://doi.org/10.1126/science.137.3532.751.","productDescription":"2 p.","startPage":"751","endPage":"752","costCenters":[],"links":[{"id":219537,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"otherGeospatial":"Antarctica, Thiel Mountains","volume":"137","issue":"3532","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059f08de4b0c8380cd4a7ab","contributors":{"authors":[{"text":"Ford, A. B.","contributorId":44924,"corporation":false,"usgs":false,"family":"Ford","given":"A.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Aaron, J.M.","contributorId":73998,"corporation":false,"usgs":true,"family":"Aaron","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":359102,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1015410,"text":"1015410 - 1962 - [Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher","interactions":[],"lastModifiedDate":"2023-12-06T01:28:30.437862","indexId":"1015410","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1337,"text":"Copeia","active":true,"publicationSubtype":{"id":10}},"title":"[Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher","docAbstract":"Review of: Taschenbuch der Fischkrankheiten, fu?r Fischereibiologen, Tiera?rzte, Fischzu?chter und Aquarianer. Erwin Amlacher. Jena, Fischer, 1961. xi, 286 p. illus.","language":"English","publisher":"American Society of Ichthyologists and Herpetologists (ASIH)","doi":"10.2307/1441217","usgsCitation":"Snieszko, S.F., 1962, [Book review] Taschenbuch der Fischkrankheiten fuur Fischereibiologen Tierarzte Fischzuchter und Aquarianer (Pocketbook of fish diseases for fishery biologists, veterinarians, fish culturists, and aquarium fanciers), by Erwin Amlacher: Copeia, v. 3, p. 670-671, https://doi.org/10.2307/1441217.","productDescription":"2 p.","startPage":"670","endPage":"671","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":132460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684c97","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":322981,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010573,"text":"70010573 - 1962 - Concentration method for the spectrochemical determination of seventeen minor elements in natural water","interactions":[],"lastModifiedDate":"2020-11-19T17:30:23.631193","indexId":"70010573","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","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":"Concentration method for the spectrochemical determination of seventeen minor elements in natural water","docAbstract":"<p>A method for the quantitative spectrochemical determination of microgram amounts of 17 minor elements in water is given. The chelating reagents 8-quinolinol, tannic acid, and thionalide are utilized to concentrate traces (1 to 500 <span>μ</span>g.) of aluminum, cobalt, chromium, copper, iron, gallium, germanium, manganese, nickel, titanium, vanadium, bismuth, lead, molybdenum, cadmium, zinc, and beryllium. Indium is added as a buffer, and palladium is used as an internal standard. The ashed oxides of these 17 metals are subsequently subjected to direct current arcing conditions during spectrum analysis. The method can be used to analyze waters with dissolved solids ranging from less than 100 to more than 100,000 p.p.m. There is no limiting concentration range for the determination of the heavy metals since any volume of sample can be used that will contain a heavy metal concentration within the analytical range of the method. Both the chemical and spectrographic procedures are described, and precision and accuracy data are given.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60187a021","usgsCitation":"Silvey, W., and Brennan, R., 1962, Concentration method for the spectrochemical determination of seventeen minor elements in natural water: Analytical Chemistry, v. 34, no. 7, p. 784-786, https://doi.org/10.1021/ac60187a021.","productDescription":"3 p.","startPage":"784","endPage":"786","numberOfPages":"3","costCenters":[],"links":[{"id":219021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"34","issue":"7","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"5059f97ee4b0c8380cd4d62b","contributors":{"authors":[{"text":"Silvey, W. D.","contributorId":102914,"corporation":false,"usgs":true,"family":"Silvey","given":"W. D.","affiliations":[],"preferred":false,"id":359203,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Brennan, R.","contributorId":62572,"corporation":false,"usgs":true,"family":"Brennan","given":"R.","email":"","affiliations":[],"preferred":false,"id":359202,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70171159,"text":"70171159 - 1962 - Microorganic constituents of water of the Great Lakes","interactions":[],"lastModifiedDate":"2017-11-14T10:16:23","indexId":"70171159","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Microorganic constituents of water of the Great Lakes","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 5th Conference on Great Lakes Reserach","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"8th Conference on Great Lakes Research","conferenceDate":"April 9-10, 1962","conferenceLocation":"Toronto, Canada","language":"English","publisher":"University of Michigan","usgsCitation":"Kempe, L.L., Daniels, S.L., and Beeton, A.M., 1962, Microorganic constituents of water of the Great Lakes, <i>in</i> Proceedings of the 5th Conference on Great Lakes Reserach, Toronto, Canada, April 9-10, 1962, p. 172-173.","productDescription":"2 p.","startPage":"172","endPage":"173","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321597,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d65d1e4b07e28b66847a1","contributors":{"authors":[{"text":"Kempe, Lloyd L.","contributorId":55117,"corporation":false,"usgs":true,"family":"Kempe","given":"Lloyd","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Daniels, Stacy L.","contributorId":105821,"corporation":false,"usgs":true,"family":"Daniels","given":"Stacy","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":630139,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630140,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70171161,"text":"70171161 - 1962 - Light penetration in the Great Lakes","interactions":[],"lastModifiedDate":"2016-05-24T10:43:55","indexId":"70171161","displayToPublicDate":"1962-01-01T00:00:00","publicationYear":"1962","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Light penetration in the Great Lakes","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":24,"text":"Conference Paper"},"largerWorkTitle":"Proceedings of the 5th Conference on Great Lakes Research","largerWorkSubtype":{"id":19,"text":"Conference Paper"},"conferenceTitle":"5th Conference on Great Lakes Research","conferenceDate":"April 9-10, 1962","conferenceLocation":"Toronto, Canada","language":"English","publisher":"University of Michigan","usgsCitation":"Beeton, A.M., 1962, Light penetration in the Great Lakes, <i>in</i> Proceedings of the 5th Conference on Great Lakes Research, Toronto, Canada, April 9-10, 1962, p. 68-76.","productDescription":"9 p.","startPage":"68","endPage":"76","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":321601,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"574d65a6e4b07e28b66845ef","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":630142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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