The United States Geological Survey was established by Congress in 1879 to make a systematic study of the geology and natural resources of the United States. To provide the essential base maps for these studies, the Survey immediately began a program of topographic mapping. In 1882 a general plan was adopted for a standard series of general-purpose topographic maps covering the entire country. Today ... the primary job of the Topographic Division of the Geological Survey is to carry out topographic surveys, and to publish the results as quadrangles in the National Topographic Map Series.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70170888","usgsCitation":"U.S. Geological Survey, 1964, Topographic mapping: A challenging future, 35 p., https://doi.org/10.3133/70170888.","productDescription":"35 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":321043,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70170888.jpg"},{"id":321056,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70170888/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5731b4ede4b0dae0d5dbc370","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128037,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":628926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210484,"text":"70210484 - 1964 - Blood parasites","interactions":[],"lastModifiedDate":"2020-06-04T18:18:35.918821","indexId":"70210484","displayToPublicDate":"1965-06-17T13:16:33","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Blood parasites","docAbstract":"No abstract available.
","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Waterfowl tomorrow","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"U. S. Department of the Interior","usgsCitation":"Fallis, A.M., and Trainer, D.O., 1964, Blood parasites, chap. of Waterfowl tomorrow, p. 343-348.","productDescription":"6 p.","startPage":"343","endPage":"348","costCenters":[],"links":[{"id":375366,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Fallis, A. Murray","contributorId":225103,"corporation":false,"usgs":false,"family":"Fallis","given":"A.","email":"","middleInitial":"Murray","affiliations":[],"preferred":false,"id":790347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Trainer, Daniel O. Jr.","contributorId":225104,"corporation":false,"usgs":false,"family":"Trainer","given":"Daniel","suffix":"Jr.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":790348,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70106994,"text":"70106994 - 1964 - Surface water records of Indiana, 1964","interactions":[],"lastModifiedDate":"2014-06-02T06:05:17","indexId":"70106994","displayToPublicDate":"1965-01-01T13:50:14","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Indiana, 1964","docAbstract":"The surface-water records for the 1964 water year for gaging stations, partial-record stations, and miscellaneous sites within the State of Indiana are given in this report. For convenience there are also included records for a few pertinent gaging stations in bordering States. The records were collected and computed by the Water Resources Division of the U.S. Geological Survey, under the direction of Malcolm D. Hale, district engineer, Surface Water Branch.
\nThis report marks the beginning of a new method of presenting, annually, basic data on surface-water records by States. Through September 30, 1960, the records of discharge and stage of streams and contents and stage of lakes or reservoirs were published in an annual series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply of the United States.\" Since 1951 there have been 20 volumes in the series; each volume covered an area whose boundaries coincided with those of certain natural drainage areas. The records in Indiana were contained in Parts 3A, 4 and 5 of that series.
\nBeginning with the 1961 water year, streamflow records and related data will be released by the Geological Survey in annual reports on a State-boundary basis. Distribution of these basic-data reports will be limited and primarily for local needs. The records later will be published in Geological Survey water-supply papers at 5-year intervals. These 5-year water-supply papers will show daily discharge and will be compiled on the same geographical areas previously used for the annual series; however, some of the 14 parts of coterminous United States will be further subdivided.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/70106994","collaboration":"Prepared in cooperation with Indiana Flood Control and Water Resources Commission; State Department of Conservation, Division of Water Resources; State Highway Commission; State Board of Health; Corps of Engineers, U.S. Army","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1964, Surface water records of Indiana, 1964, vii, 208 p., https://doi.org/10.3133/70106994.","productDescription":"vii, 208 p.","numberOfPages":"218","temporalStart":"1963-10-01","temporalEnd":"1964-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287926,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287925,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106994/report.pdf"}],"country":"United States","state":"Indiana","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.0979,37.7717 ], [ -88.0979,41.7607 ], [ -84.7847,41.7607 ], [ -84.7847,37.7717 ], [ -88.0979,37.7717 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"537b2808e4b0929ba496abc7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":535654,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70222265,"text":"70222265 - 1964 - Gravel resources in the Patuxent Formation of Cretaceous age in the Beltsville quadrangle, Prince Georges and Montgomery Counties, Maryland","interactions":[],"lastModifiedDate":"2022-06-01T21:32:57.989239","indexId":"70222265","displayToPublicDate":"1964-12-31T15:31:30","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Gravel resources in the Patuxent Formation of Cretaceous age in the Beltsville quadrangle, Prince Georges and Montgomery Counties, Maryland","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70222265","usgsCitation":"Withington, C.F., 1964, Gravel resources in the Patuxent Formation of Cretaceous age in the Beltsville quadrangle, Prince Georges and Montgomery Counties, Maryland: Open-File Report, Report; 6 p.; 1 Plate: 23.84 x 30.01 inches, https://doi.org/10.3133/70222265.","productDescription":"Report; 6 p.; 1 Plate: 23.84 x 30.01 inches","costCenters":[],"links":[{"id":401629,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/unnumbered/70222265/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":401628,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70222265/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":387366,"rank":1,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8575.htm","linkFileType":{"id":5,"text":"html"}},{"id":396966,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/unnumbered/70222265/report-thumb.jpg"}],"country":"United States","state":"Maryland","county":"Montgomery County, Prince Georges County","otherGeospatial":"Beltsville quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -77,\n 39\n ],\n [\n -76.875,\n 39\n ],\n [\n -76.875,\n 39.125\n ],\n [\n -77,\n 39.125\n ],\n [\n -77,\n 39\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Withington, C. F.","contributorId":98394,"corporation":false,"usgs":true,"family":"Withington","given":"C.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":837697,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207229,"text":"70207229 - 1964 - Late quaternary sea-level change and crustal rise at Boston, Massachusetts, with notes on the autocompaction of peat","interactions":[],"lastModifiedDate":"2019-12-12T13:54:19","indexId":"70207229","displayToPublicDate":"1964-12-31T13:44:18","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Late quaternary sea-level change and crustal rise at Boston, Massachusetts, with notes on the autocompaction of peat","docAbstract":"The compression of peat beneath its own weight (autocompaction) is discussed, and it is shown that because of this process radiocarbondated samples of salt-marsh peat or peaty sediment, other than very thin samples cut from the base of the deposit, cannot be correlated with sea level without construction of a sea-level change curve from other types of data. With rising sea level there is a maximum thickness of salt-marsh peat for any given productivity of marsh grass. Because of this limitation, most marshes older than about 5500 years B.P. have been drowned. An important effect of peat autocompaction is the intrusion of wood into older peat horizons and the juxtaposition of wood of different ages. Wood, therefore, should be avoided in the dating of peat profiles. The roots of salt-marsh plants generally descend a foot or more beneath the rhizomes, contaminating older horizons insofar as radiocarbon dating is concerned. This contamination tends to make dates from marsh samples err on the young side. Sixteen radiocarbon dates from the Boston area are used to construct a sea-level curve going back to 14,000 years B.P. Relative sea level was at +60 feet or higher 14,000 years B.P., dropping sharply to approximately -70 feet about 10,000 years B.P. From a low of -70 feet, sea level rose steadily to about -2 feet approximately 3000 years B.P. Since then sea level appears to have kept close to its present level, probably fluctuating about a foot during the course of the stillstand. A crustal movement curve, based on the relative sea-level curve for Boston and the eustatic curve, indicates that about 290 feet of crustal rise occurred between 14,000-6000 years B.P., with a maximum rate of uplift of about 0.2 foot per year at 12,750 years B.P., and that from 6000 to 3000 years B.P., crustal subsidence occurred at Boston. © 1964, The Geological Society of America, Inc.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1964)75[63:LQSCAC]2.0.CO;2","issn":"00167606","usgsCitation":"Kaye, C.A., and Barghoorn, E., 1964, Late quaternary sea-level change and crustal rise at Boston, Massachusetts, with notes on the autocompaction of peat: Geological Society of America Bulletin, v. 75, no. 2, p. 63-80, https://doi.org/10.1130/0016-7606(1964)75[63:LQSCAC]2.0.CO;2.","productDescription":"18 p. ","startPage":"63","endPage":"80","costCenters":[],"links":[{"id":370223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Massachusetts ","city":"Boston ","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.34521484375,\n 42.23665188032057\n ],\n [\n -70.740966796875,\n 42.23665188032057\n ],\n [\n -70.740966796875,\n 42.44778143462245\n ],\n [\n -71.34521484375,\n 42.44778143462245\n ],\n [\n -71.34521484375,\n 42.23665188032057\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"75","issue":"2","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kaye, C. A.","contributorId":6003,"corporation":false,"usgs":true,"family":"Kaye","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":777359,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Barghoorn, E.S.","contributorId":105052,"corporation":false,"usgs":true,"family":"Barghoorn","given":"E.S.","email":"","affiliations":[],"preferred":false,"id":777360,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70207227,"text":"70207227 - 1964 - Boulder train of silicified paleozoic wood, southeastern Massachusetts","interactions":[],"lastModifiedDate":"2019-12-12T13:32:32","indexId":"70207227","displayToPublicDate":"1964-12-31T13:25:44","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1786,"text":"Geological Society of America Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Boulder train of silicified paleozoic wood, southeastern Massachusetts","docAbstract":"Pebbles of silicified gymnospermous wood occur widely in the drift of southeastern Massachusetts. An investigation of the distribution of these pebbles shows the bedrock source of the wood to be tuffaceous beds that apparently overlie older granite in the Middleboro-Plympton area, Massachusetts, and are at the base of the Carboniferous rocks of the Narragansett Basin. A second center of distribution of the wood may lie offshore, north of Cape Cod. It is estimated that many thousands of large logs were broken up and carried away from the outcrop by Pleistocene ice sheets in the production of the boulder train. © 1964, The Geological Society of America, Inc.
","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1964)75[233:BTOSPW]2.0.CO;2","issn":"00167606","usgsCitation":"Kaye, C.A., 1964, Boulder train of silicified paleozoic wood, southeastern Massachusetts: Geological Society of America Bulletin, v. 75, no. 3, p. 233-236, https://doi.org/10.1130/0016-7606(1964)75[233:BTOSPW]2.0.CO;2.","productDescription":"4 p.","startPage":"233","endPage":"236","costCenters":[],"links":[{"id":370221,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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\"}}]}","volume":"75","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Kaye, C. A.","contributorId":6003,"corporation":false,"usgs":true,"family":"Kaye","given":"C.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":777353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70197740,"text":"70197740 - 1964 - Franciscan and related rocks, and their significance in the geology of western California","interactions":[],"lastModifiedDate":"2018-06-19T13:38:51","indexId":"70197740","displayToPublicDate":"1964-12-31T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5710,"text":"California Division of Mines and Geology Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"183","title":"Franciscan and related rocks, and their significance in the geology of western California","docAbstract":"No abstract available.
","language":"English","publisher":"California Division of Mines and Geology","usgsCitation":"Bailey, E.H., Irwin, W., and Jones, D.L., 1964, Franciscan and related rocks, and their significance in the geology of western California: California Division of Mines and Geology Bulletin 183, 177 p.","productDescription":"177 p.","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bailey, E. H.","contributorId":44509,"corporation":false,"usgs":true,"family":"Bailey","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":738347,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":738349,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70197739,"text":"70197739 - 1964 - Franciscan and related rocks, and their significance in the geology of western California","interactions":[],"lastModifiedDate":"2018-06-19T13:35:55","indexId":"70197739","displayToPublicDate":"1964-12-31T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Franciscan and related rocks, and their significance in the geology of western California","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Central portion of Great Valley of California, San Juan Bautista to Yosemite Valley: Annual Field Trip 1963, Guidebook","language":"English","publisher":"Geological Society of Sacramento","publisherLocation":"Sacramento, CA","usgsCitation":"Bailey, E.H., Irwin, W., and Jones, D.L., 1964, Franciscan and related rocks, and their significance in the geology of western California, chap. of Central portion of Great Valley of California, San Juan Bautista to Yosemite Valley: Annual Field Trip 1963, Guidebook, p. 39-46.","productDescription":"8 p.","startPage":"39","endPage":"46","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":355165,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Bailey, E. H.","contributorId":44509,"corporation":false,"usgs":true,"family":"Bailey","given":"E.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":738344,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Irwin, W. P.","contributorId":82347,"corporation":false,"usgs":true,"family":"Irwin","given":"W. P.","affiliations":[],"preferred":false,"id":738345,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Jones, D. L.","contributorId":65045,"corporation":false,"usgs":true,"family":"Jones","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":738346,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70010814,"text":"70010814 - 1964 - Paleozoic mollusk: Hyolithes","interactions":[],"lastModifiedDate":"2026-02-11T16:29:51.738158","indexId":"70010814","displayToPublicDate":"1964-12-25T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Paleozoic mollusk: Hyolithes","docAbstract":"An unusually well-preserved Ordovician fossil from Czechoslovakia shows that the enigmatic paired structures once thought to be outgrowths of the operculum of Hyolithes are really independent structures lying between the operculum and the aperture of the shell. The find seems to provide conclusive proof of the morphologic uniqueness of hyolithids.
","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.146.3652.1674","issn":"00368075","usgsCitation":"Marek, L., and Yochelson, E.L., 1964, Paleozoic mollusk: Hyolithes: Science, v. 146, no. 3652, p. 1674-1675, https://doi.org/10.1126/science.146.3652.1674.","productDescription":"2 p.","startPage":"1674","endPage":"1675","costCenters":[],"links":[{"id":218741,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Czech Republic","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 12.07683656894153,\n 51.37803979080644\n ],\n [\n 12.07683656894153,\n 48.516807647547694\n ],\n [\n 18.940933354965523,\n 48.516807647547694\n ],\n [\n 18.940933354965523,\n 51.37803979080644\n ],\n [\n 12.07683656894153,\n 51.37803979080644\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"146","issue":"3652","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a746ee4b0c8380cd7763a","contributors":{"authors":[{"text":"Marek, L.","contributorId":11752,"corporation":false,"usgs":true,"family":"Marek","given":"L.","email":"","affiliations":[],"preferred":false,"id":359709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yochelson, E. L.","contributorId":50948,"corporation":false,"usgs":true,"family":"Yochelson","given":"E.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221137,"text":"70221137 - 1964 - Some aspects of the eolian saltation load","interactions":[],"lastModifiedDate":"2021-06-02T19:10:33.003359","indexId":"70221137","displayToPublicDate":"1964-12-01T14:03:21","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3369,"text":"Sedimentology","active":true,"publicationSubtype":{"id":10}},"title":"Some aspects of the eolian saltation load","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1365-3091.1964.tb00642.x","usgsCitation":"Williams, G., 1964, Some aspects of the eolian saltation load: Sedimentology, v. 3, no. 4, p. 257-287, https://doi.org/10.1111/j.1365-3091.1964.tb00642.x.","productDescription":"31 p.","startPage":"257","endPage":"287","costCenters":[],"links":[{"id":386152,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"3","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-06-14","publicationStatus":"PW","contributors":{"authors":[{"text":"Williams, G.","contributorId":147724,"corporation":false,"usgs":false,"family":"Williams","given":"G.","affiliations":[],"preferred":false,"id":816829,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70210549,"text":"70210549 - 1964 - Exploration for mineral deposits in White County, Georgia","interactions":[],"lastModifiedDate":"2022-05-27T19:38:58.388931","indexId":"70210549","displayToPublicDate":"1964-12-01T14:01:18","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Exploration for mineral deposits in White County, Georgia","docAbstract":"White County is in the Northeast Georgia Highland. It comprises 243 square miles and has abouit 7,000 Inhabitants. The county seat is Cleveland.
Although the scene of considerable mining activity in the past, White County now has few operating mines: a small production of clay1 for the manufacture of miscellaneous potter near Cleveland, and three sand-gravel operations2 at Helen.
Minerals are one of White County's three basic resources, and the one whose development has been most neglected. This special study has been undertaken to expand mineral production, increase employment and create new economic opportunities in White County and adjacent areas.
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Vernon J.","contributorId":288097,"corporation":false,"usgs":false,"family":"Hurst","given":"Vernon","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":837388,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37779,"text":"37779 - 1964 - Manufacturers of chemical animal repellents","interactions":[],"lastModifiedDate":"2014-07-23T13:52:16","indexId":"37779","displayToPublicDate":"1964-12-01T13:51:46","publicationYear":"1964","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":"464","title":"Manufacturers of chemical animal repellents","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, 1964, Manufacturers of chemical animal repellents: Wildlife Leaflet 464, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290825,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcef1e4b0824b2d175da4","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":529715,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":37778,"text":"37778 - 1964 - Recreational policy on National Wildlife Refuges","interactions":[],"lastModifiedDate":"2014-07-23T13:50:09","indexId":"37778","displayToPublicDate":"1964-12-01T13:49:22","publicationYear":"1964","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":"463","title":"Recreational policy 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, 1964, Recreational policy on National Wildlife Refuges: Wildlife Leaflet 463, 4 p.","productDescription":"4 p.","numberOfPages":"4","costCenters":[],"links":[{"id":290823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57ffcef2e4b0824b2d175da6","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":529714,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221182,"text":"70221182 - 1964 - Low-amplitude aeromagnetic anomalies in Southeastern Missouri","interactions":[],"lastModifiedDate":"2021-06-04T17:29:34.833281","indexId":"70221182","displayToPublicDate":"1964-12-01T12:25:39","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1808,"text":"Geophysics","active":true,"publicationSubtype":{"id":10}},"title":"Low-amplitude aeromagnetic anomalies in Southeastern Missouri","docAbstract":"This study shows that aeromagnetic anomalies of less than 200 gammas are associated with topographic relief of exposed Precambrian granitic and volcanic rocks of the St. François Mountains. Anomalies resulting from hills coarsely crystalline granite are as high as 100 gammas in amplitude, whereas anomalies over comparable hills of fine-grained rocks, such as granophyre or devitrified volcanic rock, are as much as 200 gammas. Anomalies caused by normal faulting or shearing of igneous rocks have amplitudes of less than 100 gammas; they are observed best in profile. These anomalies are superposed on larger magnetic features related to pendants of volcanic rock in the roof of a granite batholith and are distinguished from large lateral variations in magnetic intensity by their low amplitude and small areal extent. Analyses of the compound anomalies yielded the subsurface configuration of isolated roof pendants of resistant extrusive rock in some areas. As many of these pendants have negligible remanent magnetization, induction theory was used in the analyses. Application of these results to the lead-mining areas shows that aeromagnetic patterns of low amplitude can guide mineral exploration in the region flanking the Ozark uplift, where isolated, buried hills of Precambrian igneous rocks controlled the development of some lead-bearing sedimentary structures in the overlying Cambrian carbonate strata.
","language":"English","publisher":"Society of Exploration Geophysicists","doi":"10.1190/1.1439390","usgsCitation":"Allingham, J., 1964, Low-amplitude aeromagnetic anomalies in Southeastern Missouri: Geophysics, v. 29, no. 4, p. 537-552, https://doi.org/10.1190/1.1439390.","productDescription":"16 p.","startPage":"537","endPage":"552","costCenters":[],"links":[{"id":386223,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Missouri","otherGeospatial":"southeast Missouri","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -90.17578124999999,\n 36.491973470593685\n ],\n [\n -90.120849609375,\n 36.19109202182454\n ],\n [\n -90.384521484375,\n 36.01356058518153\n ],\n [\n -89.659423828125,\n 35.97800618085566\n ],\n [\n -89.044189453125,\n 36.94111143010769\n ],\n [\n -89.835205078125,\n 37.96152331396614\n ],\n [\n -90.428466796875,\n 38.34165619279595\n ],\n [\n -92.032470703125,\n 38.24680876017446\n ],\n [\n -92.16430664062499,\n 36.491973470593685\n ],\n [\n -90.17578124999999,\n 36.491973470593685\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Allingham, J.W.","contributorId":85573,"corporation":false,"usgs":true,"family":"Allingham","given":"J.W.","affiliations":[],"preferred":false,"id":816989,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221122,"text":"70221122 - 1964 - Principal features and origin of podiform chro-mite deposits, and some observations on the Guleman-Soridag District, Turkey","interactions":[],"lastModifiedDate":"2021-06-02T16:58:37.925498","indexId":"70221122","displayToPublicDate":"1964-12-01T11:53:52","publicationYear":"1964","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":"Principal features and origin of podiform chro-mite deposits, and some observations on the Guleman-Soridag District, Turkey","docAbstract":"Podiform chromite deposits occur in alpine peridotite and mafic complexes and fundamentally are tabular, pencil-shaped, or irregular in form. The chromite characteristically is anhedral and commonly shows effects of granulation and magmatic corrosion. Flow-layering, foliation, and lineation are parallel in most chromite deposits and peridotite host rocks, and normally pass through major rock units, including chromite; locally, foliation and lineation may cross layering. Most podiform deposits are oriented with their longer dimensions essentially parallel to layering or foliation in the host peridotite, but some are crosswise. In all podiform deposits, whether parallel or crosswise, internal flow structures are, to use Hans Cloos' terminology, harmonious with those in the country rock, except where disturbed by postmagmatic faulting. The relations between podiform and stratiform deposits are analogous to those between metamorphic and sedimentary rocks. Though relict structures formed by crystal settling are preserved in some massive ore, most features in podiform deposits are due to extensive flowage during re-emplacement, under magmatic conditions. As the rules governing sedimentary rocks apply in exploration of stratiform deposits, so metamorphic principles apply to podiform deposits. Evidence is presented to show that the chromite deposits in the Gule-man-Soridag district, Turkey, are podiform ; and that the Golalan ore body is closely related to nearby gabbroic rocks of normal alpine type. The Soridag deposits are regarded as originally podiform rather than as fault segments of stratiform deposits.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.8.1497","usgsCitation":"Thayer, T.P., 1964, Principal features and origin of podiform chro-mite deposits, and some observations on the Guleman-Soridag District, Turkey: Economic Geology, v. 59, no. 8, p. 1497-1524, https://doi.org/10.2113/gsecongeo.59.8.1497.","productDescription":"28 p.","startPage":"1497","endPage":"1524","costCenters":[],"links":[{"id":386137,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Turkey","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 29.28955078125,\n 41.29431726315258\n ],\n [\n 25.51025390625,\n 40.245991504199026\n ],\n [\n 25.7958984375,\n 38.09998264736481\n ],\n [\n 27.75146484375,\n 35.47856499535729\n ],\n [\n 33.59619140624999,\n 35.90684930677121\n ],\n [\n 36.01318359374999,\n 36.527294814546245\n ],\n [\n 39.70458984374999,\n 37.92686760148135\n ],\n [\n 39.90234375,\n 40.97989806962013\n ],\n [\n 35.04638671874999,\n 42.17968819665961\n ],\n [\n 29.28955078125,\n 41.29431726315258\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"59","issue":"8","noUsgsAuthors":false,"publicationDate":"1964-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Thayer, T. P.","contributorId":64629,"corporation":false,"usgs":true,"family":"Thayer","given":"T.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":816807,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1014245,"text":"1014245 - 1964 - Nocardial infection in hatchery-reared fingerling rainbow trout (Salmo gairdneri)","interactions":[],"lastModifiedDate":"2025-03-03T16:28:52.112923","indexId":"1014245","displayToPublicDate":"1964-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2192,"text":"Journal of Bacteriology","active":true,"publicationSubtype":{"id":10}},"title":"Nocardial infection in hatchery-reared fingerling rainbow trout (Salmo gairdneri)","docAbstract":"No abstract available.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/jb.88.6.1809-1810.1964","usgsCitation":"Snieszko, S.F., Bullock, G.L., Dunbar, C.E., and Pettijohn, L., 1964, Nocardial infection in hatchery-reared fingerling rainbow trout (Salmo gairdneri): Journal of Bacteriology, v. 88, no. 6, p. 1809-1810, https://doi.org/10.1128/jb.88.6.1809-1810.1964.","productDescription":"2 p.","startPage":"1809","endPage":"1810","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":487148,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/jb.88.6.1809-1810.1964","text":"Publisher Index Page"},{"id":132183,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia","city":"Elkins","otherGeospatial":"Bowden Spring National Fish Hatchery","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -79.87320492091962,\n 38.94947621200663\n ],\n [\n -79.87320492091962,\n 38.91034985281962\n ],\n [\n -79.8155881317989,\n 38.91034985281962\n ],\n [\n -79.8155881317989,\n 38.94947621200663\n ],\n [\n -79.87320492091962,\n 38.94947621200663\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"88","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db6971ab","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320036,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320038,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dunbar, C. E.","contributorId":96623,"corporation":false,"usgs":true,"family":"Dunbar","given":"C.","middleInitial":"E.","affiliations":[],"preferred":false,"id":320039,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Pettijohn, L.L.","contributorId":32878,"corporation":false,"usgs":true,"family":"Pettijohn","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":320037,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1014246,"text":"1014246 - 1964 - Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay Tidewater areas","interactions":[],"lastModifiedDate":"2025-03-03T16:37:29.33012","indexId":"1014246","displayToPublicDate":"1964-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2192,"text":"Journal of Bacteriology","active":true,"publicationSubtype":{"id":10}},"title":"Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay Tidewater areas","docAbstract":"No abstract available.
","language":"English","publisher":"American Society for Microbiology","doi":"10.1128/jb.88.6.1814-1815.1964","usgsCitation":"Snieszko, S.F., Bullock, G.L., Hollis, E., and Boone, J., 1964, Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay Tidewater areas: Journal of Bacteriology, v. 88, no. 6, p. 1814-1815, https://doi.org/10.1128/jb.88.6.1814-1815.1964.","productDescription":"2 p.","startPage":"1814","endPage":"1815","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":486836,"rank":2,"type":{"id":40,"text":"Open Access Publisher Index Page"},"url":"https://doi.org/10.1128/jb.88.6.1814-1815.1964","text":"Publisher Index Page"},{"id":132184,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.er.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Delaware, Maryland, North Carolina, Virginia","otherGeospatial":"Chesapeake Bay Tidewater","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -76.5867302611951,\n 39.54788307905062\n ],\n [\n -76.5867302611951,\n 36.4297380147877\n ],\n [\n -75.3104606628179,\n 36.4297380147877\n ],\n [\n -75.3104606628179,\n 39.54788307905062\n ],\n [\n -76.5867302611951,\n 39.54788307905062\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"88","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d79","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":320040,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":320041,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hollis, E.","contributorId":97463,"corporation":false,"usgs":true,"family":"Hollis","given":"E.","email":"","affiliations":[],"preferred":false,"id":320042,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boone, J.G.","contributorId":103229,"corporation":false,"usgs":true,"family":"Boone","given":"J.G.","affiliations":[],"preferred":false,"id":320043,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":1014136,"text":"1014136 - 1964 - Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay tidewater areas","interactions":[],"lastModifiedDate":"2023-08-24T17:00:00.542963","indexId":"1014136","displayToPublicDate":"1964-12-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2192,"text":"Journal of Bacteriology","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay tidewater areas","title":"Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay tidewater areas","docAbstract":"No abstract available.
","language":"English","publisher":"ASM Journals","doi":"10.1128/jb.88.6.1814-1815.1964","usgsCitation":"Snieszko, S.F., Bullock, G.L., Hollis, E., and Boone, J., 1964, Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay tidewater areas: Journal of Bacteriology, v. 88, no. 6, p. 1814-1815, https://doi.org/10.1128/jb.88.6.1814-1815.1964.","productDescription":"2 p.","startPage":"1814","endPage":"1815","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":480365,"rank":2,"type":{"id":41,"text":"Open Access External Repository Page"},"url":"https://doi.org/10.1128/jb.88.6.1814-1815.1964","text":"External Repository"},{"id":131853,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"88","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bb0","contributors":{"authors":[{"text":"Snieszko, S. F.","contributorId":13169,"corporation":false,"usgs":true,"family":"Snieszko","given":"S.","middleInitial":"F.","affiliations":[],"preferred":false,"id":319850,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bullock, G. L.","contributorId":69498,"corporation":false,"usgs":true,"family":"Bullock","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":881124,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hollis, Edgar","contributorId":328731,"corporation":false,"usgs":false,"family":"Hollis","given":"Edgar","email":"","affiliations":[],"preferred":false,"id":881125,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Boone, J.G.","contributorId":103229,"corporation":false,"usgs":true,"family":"Boone","given":"J.G.","affiliations":[],"preferred":false,"id":881126,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70010470,"text":"70010470 - 1964 - Spalled, aerodynamically modified moldavite from Slavice, Moravia, Czechoslovakia","interactions":[],"lastModifiedDate":"2026-02-11T16:46:58.218961","indexId":"70010470","displayToPublicDate":"1964-11-06T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Spalled, aerodynamically modified moldavite from Slavice, Moravia, Czechoslovakia","docAbstract":"A Czechoslovakian tektite or moldavite shows clear, indirect evidence of aerodynamic ablation. This large tektite has the shape of a teardrop, with a strongly convex, deeply corroded, but clearly identifiable front and a planoconvex, relatively smooth, posterior surface. In spite of much erosion and corrosion, demarcation of the posterior and the anterior part of the specimen (the keel) is clearly preserved locally. This specimen provides the first tangible evidence that moldavites entered the atmosphere cold, probably at a velocity exceeding 5 kilometers per second; the result was selective heating of the anterior face and perhaps ablation during the second melting. This provides evidence of the extraterrestial origin of moldavites.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.146.3645.790","issn":"00368075","usgsCitation":"Chao, E.C., 1964, Spalled, aerodynamically modified moldavite from Slavice, Moravia, Czechoslovakia: Science, v. 146, no. 3645, p. 790-791, https://doi.org/10.1126/science.146.3645.790.","productDescription":"2 p.","startPage":"790","endPage":"791","costCenters":[],"links":[{"id":219075,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Czech Republic","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n 12.07683656894153,\n 51.37803979080644\n ],\n [\n 12.07683656894153,\n 48.516807647547694\n ],\n [\n 18.940933354965523,\n 48.516807647547694\n ],\n [\n 18.940933354965523,\n 51.37803979080644\n ],\n [\n 12.07683656894153,\n 51.37803979080644\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"146","issue":"3645","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b940ee4b08c986b31a834","contributors":{"authors":[{"text":"Chao, E. C. T.","contributorId":96713,"corporation":false,"usgs":true,"family":"Chao","given":"E.","email":"","middleInitial":"C. T.","affiliations":[],"preferred":false,"id":358993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70221124,"text":"70221124 - 1964 - Paleo-channels at the Guayacan copper mine, Cabildo District, Aconcagua Province, Chile","interactions":[],"lastModifiedDate":"2021-06-02T17:40:54.122219","indexId":"70221124","displayToPublicDate":"1964-11-04T12:35:41","publicationYear":"1964","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":"Paleo-channels at the Guayacan copper mine, Cabildo District, Aconcagua Province, Chile","docAbstract":"An uneven erosion surface separates calcareous sedimentary rocks above and vesicular andesite porphyry below at the Guayacan mine of central Chile. Channel-like depressions filled with sedimentary rock flank elongate, stratiform bodies of disseminated copper ore which impregnate the vesicular crests of andesite lava flows. The \"channels\" lie parallel to and mark the margins of tongues of lava. Erosional features such as scour surfaces, conglomerate and crossbedding mark some of the channels. Other channels show no evidence of erosion, suggesting that some, at least, represent depressions or spaces that were not filled during extrusion of the lava. The flows strike east. Their crests are vesicular and impregnated with copper sulfide minerals, mainly bornite, to depths as much as 3 m below the contact. Bornite fills vesicles and fractures, impregnates the andesite ground mass, and replaces andesine phenocrysts, mainly along cleavage planes. Chalcopyrite is mixed with bornite in the upper, more vesicular part of the flows and occurs with fine-grained pyrite as disseminations and replacing fossils in the base of the overlying sedimentary rock. The channel axes also strike roughly east and, in most places, are underlain by barren ground. These mappable features, when recognized, are valuable in determining the size, shape, and orientation of adjacent ore bodies and, thereby, assist in the evaluation, exploration and mining of these stratiform copper deposits.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.7.1283","usgsCitation":"Carter, W.D., and Nelson, T.A., 1964, Paleo-channels at the Guayacan copper mine, Cabildo District, Aconcagua Province, Chile: Economic Geology, v. 59, no. 7, p. 1283-1292, https://doi.org/10.2113/gsecongeo.59.7.1283.","productDescription":"10 p.","startPage":"1283","endPage":"1292","costCenters":[],"links":[{"id":386140,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Chile","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -70.400390625,\n -27.371767300523032\n ],\n [\n -68.73046875,\n -27.371767300523032\n ],\n [\n -68.73046875,\n -22.67484735118852\n ],\n [\n -70.400390625,\n -22.67484735118852\n ],\n [\n -70.400390625,\n -27.371767300523032\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"59","issue":"7","noUsgsAuthors":false,"publicationDate":"1964-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Carter, W. D.","contributorId":75633,"corporation":false,"usgs":true,"family":"Carter","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":816809,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nelson, T. Aliste","contributorId":259203,"corporation":false,"usgs":false,"family":"Nelson","given":"T.","email":"","middleInitial":"Aliste","affiliations":[],"preferred":false,"id":816810,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70221134,"text":"70221134 - 1964 - Electronprobe analysis of \"cosmic\" particles","interactions":[],"lastModifiedDate":"2021-06-02T18:57:58.39092","indexId":"70221134","displayToPublicDate":"1964-11-01T13:54:17","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":801,"text":"Annals of the New York Academy of Sciences","active":true,"publicationSubtype":{"id":10}},"title":"Electronprobe analysis of \"cosmic\" particles","docAbstract":"No abstract available.
","language":"English","publisher":"Wiley","doi":"10.1111/j.1749-6632.1965.tb47439.x","usgsCitation":"Larson, R., Dwornik, E., and Adler, I., 1964, Electronprobe analysis of \"cosmic\" particles: Annals of the New York Academy of Sciences, v. 119, no. 1, p. 282-286, https://doi.org/10.1111/j.1749-6632.1965.tb47439.x.","productDescription":"5 p.","startPage":"282","endPage":"286","costCenters":[],"links":[{"id":386148,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"119","issue":"1","noUsgsAuthors":false,"publicationDate":"2006-12-16","publicationStatus":"PW","contributors":{"authors":[{"text":"Larson, R.","contributorId":30438,"corporation":false,"usgs":true,"family":"Larson","given":"R.","affiliations":[],"preferred":false,"id":816822,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dwornik, E.J.","contributorId":99128,"corporation":false,"usgs":true,"family":"Dwornik","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":816823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Adler, I.","contributorId":13371,"corporation":false,"usgs":true,"family":"Adler","given":"I.","email":"","affiliations":[],"preferred":false,"id":816824,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70221123,"text":"70221123 - 1964 - Supergene iron ores of minas Gerais, Brazil","interactions":[],"lastModifiedDate":"2021-06-02T17:31:15.936558","indexId":"70221123","displayToPublicDate":"1964-11-01T12:26:13","publicationYear":"1964","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":"Supergene iron ores of minas Gerais, Brazil","docAbstract":"The iron ores of Minas Gerais, Brazil, fall into two categories: (1) hypogene hematite ore averaging 66 percent or more Fe, and (2) lower-grade supergene ores. Most ore now extracted is high-grade hypogene ore; lower-grade supergene ores will be of much future value. All supergene ores formed by weathering of itabirite, a metamorphosed oxide-facies iron formation averaging about 38 percent Fe and 44 percent Si02. The Caue Itabirite crops out for about 540 linear kilometers in central Minas Gerais. Supergene ores fall into three intergradational categories: (1) enriched itabirite, averaging 49 percent Fe, easily con-centratable, with reserves about 25,000 million tons; (2) intermediate grade ores, averaging perhaps 63 percent Fe, with indicated and inferred reserves more than 600 million tons; and (3) canga, averaging between 57 and 62 percent Fe, with reserves in the hundreds of millions of tons. Disaggregation of hard and brittle itabirite by solution primarily of quartz and secondarily of other soluble constituents causes residual enrichment in iron with minor hydration of hematite. As weathering continues, most of the quartz is removed and more of the hematite is hydrated, producing intermediate grade ore. Secondary enrichment by limonite is important. The final weathering product is canga. In canga, almost all the iron is hydrated, and the rock is still further impoverished in Si02 and residually enriched in A1203 and P. Canga also forms by cementation of iron-rich detritus by limonite. Four factors control the supergene ore-forming process: (1) physiography, for ores occur on ridges and plateaus; (2) climate, for seasonal rainfall is apparently needed for the formation of extensive canga blankets; (3) grain size of the original itabirite, for quartz with a grain size much greater than 0.1 millimeter is not readily soluble; and (4) composition of the iron formation. The chemically inert and physically resistant canga blanket is essential to supergene ore formation because soft weathering products would otherwise be removed as fast as formed. Thus, canga gives time for the formation of other ore types. Iron fixed as cementing limonite in canga and as enriching limonite in intermediate grade ore was derived by leaching and hydration of hematite from itabirite. It probably moved in the ferrous state and was precipitated as insoluble hydrous ferric oxide primarily by oxygenation of the solutions, to a lesser extent by their evaporation at or near the surface, and to a still smaller degree by pH changes. The data show that the high-grade hematite ore, 66 percent Fe or higher, cannot have formed directly by supergene action. Geochemical processes resulting in supergene concentration of iron also concentrated alumina and phosphorus. The high-grade ore contains about the same low percentages of these materials as unweathered itabirite.
","language":"English","publisher":"Society of Economic Geologists","doi":"10.2113/gsecongeo.59.7.1203","usgsCitation":"Dorr, J.V., 1964, Supergene iron ores of minas Gerais, Brazil: Economic Geology, v. 59, no. 7, p. 1203-1240, https://doi.org/10.2113/gsecongeo.59.7.1203.","productDescription":"38 p.","startPage":"1203","endPage":"1240","costCenters":[],"links":[{"id":386139,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Brazil","state":"Minas Gerais","city":"Gerais","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -46.724853515625,\n -20.3961232724676\n ],\n [\n -45.494384765625,\n -20.3961232724676\n ],\n [\n -45.494384765625,\n -18.656654486540006\n ],\n [\n -46.724853515625,\n -18.656654486540006\n ],\n [\n -46.724853515625,\n -20.3961232724676\n ]\n ]\n ]\n }\n }\n ]\n}","volume":"59","issue":"7","noUsgsAuthors":false,"publicationDate":"1964-11-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Dorr, J. V.N. II","contributorId":68807,"corporation":false,"usgs":true,"family":"Dorr","given":"J.","suffix":"II","middleInitial":"V.N.","affiliations":[],"preferred":false,"id":816808,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70207358,"text":"70207358 - 1964 - Hidden Recharge","interactions":[],"lastModifiedDate":"2019-12-18T10:56:54","indexId":"70207358","displayToPublicDate":"1964-10-31T10:53:38","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1861,"text":"Ground Water","active":true,"publicationSubtype":{"id":10}},"title":"Hidden Recharge","docAbstract":"“Hidden recharge” is defined as subsurface percolation of water from basin‐margin mountains directly into aquifers of the valley basins. It is an important, and sometimes neglected, item in hydrologic equations. Locally, geologic conditions permit inter‐basin circulation of ground water. The concept that ground‐water basins necessarily terminate at the contact between alluvium and hardrock is not tenable. Copyright © 1964, Wiley Blackwell. All rights reserved
","language":"English","publisher":"Wiley Blackwell","doi":"10.1111/j.1745-6584.1964.tb01780.x","issn":" 0017467X","usgsCitation":"Feth, J.H., 1964, Hidden Recharge: Ground Water, v. 2, no. 4, p. 14-17 , https://doi.org/10.1111/j.1745-6584.1964.tb01780.x.","productDescription":"4 p. ","startPage":"14","endPage":"17 ","costCenters":[],"links":[{"id":370399,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"4","noUsgsAuthors":false,"publicationDate":"2006-07-06","publicationStatus":"PW","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":777803,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010683,"text":"70010683 - 1964 - Origin of high-alumina basalt, andesite, and dacite magmas","interactions":[],"lastModifiedDate":"2026-02-11T16:52:44.688651","indexId":"70010683","displayToPublicDate":"1964-10-30T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Origin of high-alumina basalt, andesite, and dacite magmas","docAbstract":"The typical volcanic rocks of most island arcs and eugeosynclines, and of some continental environments, are basalt, andesite, and dacite, of high alumina content. The high-alumina basalt differs from tholeiitic basalt primarily in having a greater content of the components of calcic plagioclase. Laboratory data indicate that in the upper mantle, below the level at which the basaltic component of mantle rock is transformed by pressure to eclogite or pyroxenite, the entire basaltic portion probably is melted within a narrow temperature range, but that above the level of that transformation plagioclase is melted selectively before pyroxene over a wide temperature range. The broad spectrum of high-alumina magmas may represent widely varying degrees of partial melting above the transformation level, whereas narrow-spectrum tholeiite magma may represent more complete melting beneath it.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.146.3644.635","issn":"00368075","usgsCitation":"Hamilton, W., 1964, Origin of high-alumina basalt, andesite, and dacite magmas: Science, v. 146, no. 3644, p. 635-637, https://doi.org/10.1126/science.146.3644.635.","productDescription":"3 p.","startPage":"635","endPage":"637","costCenters":[],"links":[{"id":219403,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"146","issue":"3644","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a70d9e4b0c8380cd762ba","contributors":{"authors":[{"text":"Hamilton, W.","contributorId":46683,"corporation":false,"usgs":true,"family":"Hamilton","given":"W.","email":"","affiliations":[],"preferred":false,"id":359421,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}