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,{"id":38929,"text":"pp462D - 1964 - Scour and fill in sand-bed streams","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"pp462D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"462","chapter":"D","title":"Scour and fill in sand-bed streams","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Sediment transport in alluvial channels, 1963-65","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp462D","usgsCitation":"Colby, B.R., 1964, Scour and fill in sand-bed streams: U.S. Geological Survey Professional Paper 462, p. D1-D32, https://doi.org/10.3133/pp462D.","productDescription":"p. D1-D32","costCenters":[],"links":[{"id":123283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0462d/report-thumb.jpg"},{"id":65972,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0462d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcdcf","contributors":{"authors":[{"text":"Colby, B. R.","contributorId":59776,"corporation":false,"usgs":true,"family":"Colby","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":220684,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62125,"text":"gq305 - 1964 - Geology of the Mont quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"gq305","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"305","title":"Geology of the Mont quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq305","usgsCitation":"Weis, P., and Theobald, P., 1964, Geology of the Mont quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 305, 1 map., https://doi.org/10.3133/gq305.","productDescription":"1 map.","costCenters":[],"links":[{"id":102316,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_765.htm","linkFileType":{"id":5,"text":"html"},"description":"765"},{"id":248319,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0305/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253213,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0305/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,36.8675 ], [ -88.11749999999999,37 ], [ -88,37 ], [ -88,36.8675 ], [ -88.11749999999999,36.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e9bc","contributors":{"authors":[{"text":"Weis, Paul L.","contributorId":102872,"corporation":false,"usgs":true,"family":"Weis","given":"Paul L.","affiliations":[],"preferred":false,"id":266953,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":266952,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":38964,"text":"pp418B - 1964 - Middle Bajocian ammonites from the Cook Inlet region, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp418B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"418","chapter":"B","title":"Middle Bajocian ammonites from the Cook Inlet region, Alaska","language":"ENGLISH","doi":"10.3133/pp418B","usgsCitation":"Imlay, R.W., 1964, Middle Bajocian ammonites from the Cook Inlet region, Alaska: U.S. Geological Survey Professional Paper 418, p. B1-B61, https://doi.org/10.3133/pp418B.","productDescription":"p. B1-B61","costCenters":[],"links":[{"id":111445,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.dggs.dnr.state.ak.us/pubs/id/3863","linkFileType":{"id":5,"text":"html"}},{"id":113302,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0418b/report.pdf","size":"19829","linkFileType":{"id":1,"text":"pdf"}},{"id":173226,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0418b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a03e4b07f02db5f82c9","contributors":{"authors":[{"text":"Imlay, R. W.","contributorId":23118,"corporation":false,"usgs":true,"family":"Imlay","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":220733,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38885,"text":"pp473B - 1964 - Field investigation of mine waters in the northern anthracite field, Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp473B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"473","chapter":"B","title":"Field investigation of mine waters in the northern anthracite field, Pennsylvania","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Mining hydrology","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"ENGLISH","doi":"10.3133/pp473B","usgsCitation":"Barnes, I., Stuart, W., and Fisher, D., 1964, Field investigation of mine waters in the northern anthracite field, Pennsylvania: U.S. Geological Survey Professional Paper 473, p. B1-B8, https://doi.org/10.3133/pp473B.","productDescription":"p. B1-B8","costCenters":[],"links":[{"id":121992,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0473b/report-thumb.jpg"},{"id":65886,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0473b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fce4b07f02db5f588a","contributors":{"authors":[{"text":"Barnes, Ivan","contributorId":56619,"corporation":false,"usgs":true,"family":"Barnes","given":"Ivan","email":"","affiliations":[],"preferred":false,"id":220603,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stuart, W.T.","contributorId":19217,"corporation":false,"usgs":true,"family":"Stuart","given":"W.T.","email":"","affiliations":[],"preferred":false,"id":220602,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fisher, D.W.","contributorId":77519,"corporation":false,"usgs":true,"family":"Fisher","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":220604,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":38869,"text":"pp496A - 1964 - Geology of Green River Formation and associated Eocene rocks in southwestern Wyoming and adjacent parts of Colorado and Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp496A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"496","chapter":"A","title":"Geology of Green River Formation and associated Eocene rocks in southwestern Wyoming and adjacent parts of Colorado and Utah","language":"ENGLISH","doi":"10.3133/pp496A","usgsCitation":"Bradley, W.H., 1964, Geology of Green River Formation and associated Eocene rocks in southwestern Wyoming and adjacent parts of Colorado and Utah: U.S. Geological Survey Professional Paper 496, p. A1-A86, https://doi.org/10.3133/pp496A.","productDescription":"p. A1-A86","costCenters":[],"links":[{"id":113289,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0496a/plate-2.pdf","size":"3891","linkFileType":{"id":1,"text":"pdf"}},{"id":113287,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0496a/report.pdf","size":"15524","linkFileType":{"id":1,"text":"pdf"}},{"id":113288,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0496a/plate-1.pdf","size":"11280","linkFileType":{"id":1,"text":"pdf"}},{"id":113290,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0496a/plate-3.pdf","size":"1501","linkFileType":{"id":1,"text":"pdf"}},{"id":173724,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0496a/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683f87","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":220579,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32765,"text":"pp422D - 1964 - Channel patterns and terraces of the Loup Rivers in Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:09:11","indexId":"pp422D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"422","chapter":"D","title":"Channel patterns and terraces of the Loup Rivers in Nebraska","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp422D","usgsCitation":"Brice, J.C., 1964, Channel patterns and terraces of the Loup Rivers in Nebraska: U.S. Geological Survey Professional Paper 422, iv, 41 p. *MISSING PAGES*, https://doi.org/10.3133/pp422D.","productDescription":"iv, 41 p. *MISSING PAGES*","costCenters":[],"links":[{"id":95929,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0422d/report.pdf","size":"6106","linkFileType":{"id":1,"text":"pdf"}},{"id":119271,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0422d/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e4e4b07f02db5e627d","contributors":{"authors":[{"text":"Brice, James Coble","contributorId":49004,"corporation":false,"usgs":true,"family":"Brice","given":"James","email":"","middleInitial":"Coble","affiliations":[],"preferred":false,"id":209120,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70112250,"text":"70112250 - 1964 - Geographic data from space","interactions":[],"lastModifiedDate":"2017-03-27T13:37:15","indexId":"70112250","displayToPublicDate":"1990-06-12T09:04:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3191,"text":"Professional Geographer","active":true,"publicationSubtype":{"id":10}},"title":"Geographic data from space","docAbstract":"Space science has been called “the collection of scientific problems to which space vehicles can make some specific contributions not achievable by ground-based experiments.” Geography, the most spatial of the sciences, has now been marked as one of these “space sciences.” The National Aeronautics and Space Administration (NASA) is sponsoring an investigation to identify the Potential geographic benefits from the nation’s space program. This is part of NASA’s long-range inquiry to determine the kinds of scientific activities which might profitably be carried out on future space missions. Among such future activities which are now being planned by NASA are a series of manned earth orbital missions, many of which would be devoted to research. Experiments in physics, astronomy, geophysics, meteorology, and biology are being discussed for these long-range missions. The question which is being put to geographers is, essentially, what would it mean to geographic research to have an observation satellite (or many such satellites) orbiting the earth, gathering data about earth-surface features and environments?","language":"English","publisher":"Association of American Geographers","publisherLocation":"Hamilton, NY","doi":"10.1111/j.0033-0124.1964.001_w.x","usgsCitation":"Alexander, R.H., 1964, Geographic data from space: Professional Geographer, v. 16, no. 6, p. 1-5, https://doi.org/10.1111/j.0033-0124.1964.001_w.x.","productDescription":"5 p.","startPage":"1","endPage":"5","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288421,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":288420,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://dx.doi.org/10.1111/j.0033-0124.1964.001_w.x"}],"volume":"16","issue":"6","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acbfee4b0e83db6d08f38","contributors":{"authors":[{"text":"Alexander, Robert H.","contributorId":53807,"corporation":false,"usgs":true,"family":"Alexander","given":"Robert","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":494574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70170888,"text":"70170888 - 1964 - Topographic mapping: A challenging future","interactions":[],"lastModifiedDate":"2016-05-09T15:47:29","indexId":"70170888","displayToPublicDate":"1970-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Topographic mapping: A challenging future","docAbstract":"<p>The United States Geological Survey was established by Congress&nbsp;in 1879 to make a systematic study of the geology and natural&nbsp;resources of the United States. To provide the essential base maps&nbsp;for these studies, the Survey immediately began a program of&nbsp;topographic mapping. In 1882 a general plan was adopted for&nbsp;a standard series of general-purpose topographic maps covering&nbsp;the entire country. Today ... the primary job of the Topographic&nbsp;Division of the Geological Survey is to carry out&nbsp;topographic surveys, and to publish the results as quadrangles in&nbsp;the National Topographic Map Series.</p>","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":"<p>No abstract available.</p>","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. <i>of</i> 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":"<p>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.</p>\n<br/>\n<p>This 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.</p>\n<br/>\n<p>Beginning 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.</p>","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":"<p>No abstract available.</p>","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":"<p><span>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.</span></p>","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":"<p><span>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.</span></p>","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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,{"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. <i>of</i> 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":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":"<p>No abstract available.</p>","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":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":"<p><span>An unusually well-preserved Ordovician fossil from Czechoslovakia shows that the enigmatic paired structures once thought to be outgrowths of the operculum of&nbsp;</span><i>Hyolithes</i><span>&nbsp;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.</span></p>","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":"<p>No abstract available.&nbsp;</p>","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":"<p>White County is in the Northeast Georgia Highland. It comprises 243 square miles and has abouit 7,000 Inhabitants. The county seat is Cleveland.</p><p>Although the scene of considerable mining activity in the past, White County now has few operating mines: a small production of clay<sup>1</sup> for the manufacture of miscellaneous potter near Cleveland, and three sand-gravel operations<sup>2</sup> at Helen.</p><p>Minerals are one of White County's three basic resources, and the one whose development has been most neglected. 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,{"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":"<p><span>This study shows that&nbsp;</span>aeromagnetic<span>&nbsp;</span>anomalies<span>&nbsp;of less than 200 gammas are associated with topographic relief of exposed Precambrian granitic and volcanic rocks of the St. François Mountains.&nbsp;</span>Anomalies<span>&nbsp;resulting from hills coarsely crystalline granite are as high as 100 gammas&nbsp;</span>in<span>&nbsp;</span>amplitude<span>, whereas&nbsp;</span>anomalies<span>&nbsp;over comparable hills of fine-grained rocks, such as granophyre or devitrified volcanic rock, are as much as 200 gammas.&nbsp;</span>Anomalies<span>&nbsp;caused by normal faulting or shearing of igneous rocks have amplitudes of less than 100 gammas; they are observed best&nbsp;</span>in<span>&nbsp;profile. These&nbsp;</span>anomalies<span>&nbsp;are superposed on larger magnetic features related to pendants of volcanic rock&nbsp;</span>in<span>&nbsp;the roof of a granite batholith and are distinguished from large lateral variations&nbsp;</span>in<span>&nbsp;magnetic intensity by their&nbsp;</span>low<span>&nbsp;</span>amplitude<span>&nbsp;and small areal extent. Analyses of the compound&nbsp;</span>anomalies<span>&nbsp;yielded the subsurface configuration of isolated roof pendants of resistant extrusive rock&nbsp;</span>in<span>&nbsp;some areas. As many of these pendants have negligible remanent magnetization, induction theory was used&nbsp;</span>in<span>&nbsp;the analyses. Application of these results to the lead-mining areas shows that&nbsp;</span>aeromagnetic<span>&nbsp;patterns of&nbsp;</span>low<span>&nbsp;</span>amplitude<span>&nbsp;can guide mineral exploration&nbsp;</span>in<span>&nbsp;the region flanking the Ozark uplift, where isolated, buried hills of Precambrian igneous rocks controlled the development of some lead-bearing sedimentary structures&nbsp;</span>in<span>&nbsp;the overlying Cambrian carbonate strata.&nbsp;</span></p>","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":"<p><span class=\"ScopusTermHighlight\">Podiform</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">chromite</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;occur in alpine peridotite and mafic complexes and fundamentally are tabular, pencil-shaped, or irregular in form. The&nbsp;</span><span class=\"ScopusTermHighlight\">chromite</span><span>&nbsp;characteristically is anhedral and commonly shows effects of granulation and magmatic corrosion. Flow-layering, foliation, and lineation are parallel in most&nbsp;</span><span class=\"ScopusTermHighlight\">chromite</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;and peridotite host rocks, and normally pass through major rock units, including&nbsp;</span><span class=\"ScopusTermHighlight\">chromite</span><span>; locally, foliation and lineation may cross layering. Most&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;are oriented with their longer dimensions essentially parallel to layering or foliation in the host peridotite, but some are crosswise. In all&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>, 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&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;and stratiform&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;are analogous to those between metamorphic and sedimentary rocks. Though relict structures formed by crystal settling are preserved in some massive ore, most&nbsp;</span><span class=\"ScopusTermHighlight\">features</span><span>&nbsp;in&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;are due to extensive flowage during re-emplacement, under magmatic conditions. As the rules governing sedimentary rocks apply in exploration of stratiform&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>, so metamorphic principles apply to&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>. Evidence is presented to show that the&nbsp;</span><span class=\"ScopusTermHighlight\">chromite</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;in the Gule-man-Soridag&nbsp;</span><span class=\"ScopusTermHighlight\">district</span><span>,&nbsp;</span><span class=\"ScopusTermHighlight\">Turkey</span><span>, are&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;; and that the Golalan ore body is closely related to nearby gabbroic rocks of normal alpine type. The Soridag&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>&nbsp;are regarded as originally&nbsp;</span><span class=\"ScopusTermHighlight\">podiform</span><span>&nbsp;rather than as fault segments of stratiform&nbsp;</span><span class=\"ScopusTermHighlight\">deposits</span><span>.</span></p>","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":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":"<i>Pasteurella</i> sp. from an epizootic of white perch (<i>Roccus americanus</i>) in Chesapeake Bay tidewater areas","title":"Pasteurella sp. from an epizootic of white perch (Roccus americanus) in Chesapeake Bay tidewater areas","docAbstract":"<p>No abstract available.</p>","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":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":"<p>No abstract available.&nbsp;</p>","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}]}}
]}