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,{"id":64133,"text":"gp391 - 1963 - Aeromagnetic map of the Quantico quadrangle, Prince William and Stafford Counties, Virginia","interactions":[],"lastModifiedDate":"2025-04-23T21:07:15.915263","indexId":"gp391","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"391","title":"Aeromagnetic map of the Quantico quadrangle, Prince William and Stafford Counties, Virginia","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gp391","usgsCitation":"Bromery, R.W., Galat, G., and Chandler, E.J., 1963, Aeromagnetic map of the Quantico quadrangle, Prince William and Stafford Counties, Virginia: U.S. Geological Survey Geophysical Investigations Map 391, 1 Plate: 23.54 x 27.79 inches, https://doi.org/10.3133/gp391.","productDescription":"1 Plate: 23.54 x 27.79 inches","costCenters":[],"links":[{"id":254101,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0391/report-thumb.jpg"},{"id":250601,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0391/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":250600,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0391/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":484943,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_3330.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Virginia","county":"Prince William County, Stafford County","otherGeospatial":"Quantico quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.375,\n              38.625\n            ],\n            [\n              -77.375,\n              38.5\n            ],\n            [\n              -77.25,\n              38.5\n            ],\n            [\n              -77.25,\n              38.625\n            ],\n            [\n              -77.375,\n              38.625\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af3e4b07f02db691a54","contributors":{"authors":[{"text":"Bromery, R. W.","contributorId":11676,"corporation":false,"usgs":true,"family":"Bromery","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":270016,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Galat, G.A.","contributorId":80757,"corporation":false,"usgs":true,"family":"Galat","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":270018,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Chandler, E. J.","contributorId":20834,"corporation":false,"usgs":true,"family":"Chandler","given":"E.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":270017,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":66255,"text":"i372 - 1963 - Geologic map of the Storm Hill quadrangle, Crook County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:11:19","indexId":"i372","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"372","subseriesTitle":"NONE","title":"Geologic map of the Storm Hill quadrangle, Crook County, Wyoming","language":"ENGLISH","doi":"10.3133/i372","usgsCitation":"Izett, G., 1963, Geologic map of the Storm Hill quadrangle, Crook County, Wyoming: U.S. Geological Survey IMAP 372, 1 map., https://doi.org/10.3133/i372.","productDescription":"1 map.","costCenters":[],"links":[{"id":102877,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1343.htm","linkFileType":{"id":5,"text":"html"},"description":"1343"},{"id":188673,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.75,44.6175 ], [ -104.75,44.75 ], [ -104.61749999999999,44.75 ], [ -104.61749999999999,44.6175 ], [ -104.75,44.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a76c","contributors":{"authors":[{"text":"Izett, G. A.","contributorId":21131,"corporation":false,"usgs":true,"family":"Izett","given":"G. A.","affiliations":[],"preferred":false,"id":274253,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":62482,"text":"gq212 - 1963 - Geologic map of the Mesa Gigante quadrangle, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:10:40","indexId":"gq212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"212","title":"Geologic map of the Mesa Gigante quadrangle, New Mexico","language":"ENGLISH","doi":"10.3133/gq212","usgsCitation":"Moench, R.H., and Puffett, W.P., 1963, Geologic map of the Mesa Gigante quadrangle, New Mexico: U.S. Geological Survey Geologic Quadrangle 212, 1 map :col. ;58 x 48 cm., https://doi.org/10.3133/gq212.","productDescription":"1 map :col. ;58 x 48 cm.","costCenters":[],"links":[{"id":102216,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_665.htm","linkFileType":{"id":5,"text":"html"},"description":"665"},{"id":248645,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0212/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":253872,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0212/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -107.25,35 ], [ -107.25,35.1175 ], [ -107.11749999999999,35.1175 ], [ -107.11749999999999,35 ], [ -107.25,35 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a43","contributors":{"authors":[{"text":"Moench, Robert Hadley","contributorId":28238,"corporation":false,"usgs":true,"family":"Moench","given":"Robert","email":"","middleInitial":"Hadley","affiliations":[],"preferred":false,"id":267434,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Puffett, Willard P.","contributorId":63382,"corporation":false,"usgs":true,"family":"Puffett","given":"Willard","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":267435,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":62492,"text":"gq264 - 1963 - Pre-Quaternary geology of the Browns Mills quadrangle, New Jersey","interactions":[],"lastModifiedDate":"2021-11-10T20:42:28.318506","indexId":"gq264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"264","title":"Pre-Quaternary geology of the Browns Mills quadrangle, New Jersey","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/gq264","usgsCitation":"Minard, J.P., and Owens, J.P., 1963, Pre-Quaternary geology of the Browns Mills quadrangle, New Jersey: U.S. Geological Survey Geologic Quadrangle 264, Report: 1 p.; Plate, https://doi.org/10.3133/gq264.","productDescription":"Report: 1 p.; Plate","costCenters":[],"links":[{"id":102270,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_719.htm","linkFileType":{"id":5,"text":"html"},"description":"719"},{"id":248655,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0264/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":253882,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0264/report-thumb.jpg"}],"scale":"24000","country":"United States","state":"New Jersey","otherGeospatial":"Browns Mills quadrangle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -74.625,39.875 ], [ -74.625,40 ], [ -74.5,40 ], [ -74.5,39.875 ], [ -74.625,39.875 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db681271","contributors":{"authors":[{"text":"Minard, James Patrick","contributorId":25640,"corporation":false,"usgs":true,"family":"Minard","given":"James","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":267450,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Owens, James Patrick","contributorId":105706,"corporation":false,"usgs":true,"family":"Owens","given":"James","email":"","middleInitial":"Patrick","affiliations":[],"preferred":false,"id":267451,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":66395,"text":"i404 - 1963 - Geologic map of the Grand Junction area, Colorado","interactions":[],"lastModifiedDate":"2014-01-30T10:56:24","indexId":"i404","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"404","subseriesTitle":"NONE","title":"Geologic map of the Grand Junction area, Colorado","language":"ENGLISH","doi":"10.3133/i404","usgsCitation":"Lohman, S.W., 1963, Geologic map of the Grand Junction area, Colorado: U.S. Geological Survey IMAP 404, 1 map :col. ;on sheet 145 x 103 cm. folded to 29 x 21 cm. in envelope 30 x 24 cm., https://doi.org/10.3133/i404.","productDescription":"1 map :col. ;on sheet 145 x 103 cm. folded to 29 x 21 cm. in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102850,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1316.htm","linkFileType":{"id":5,"text":"html"},"description":"1316"},{"id":187645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0404/report-thumb.jpg"},{"id":281729,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0404/plate-1.pdf"}],"scale":"680","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.75,38.833333333333336 ], [ -108.75,39.166666666666664 ], [ -108.41666666666667,39.166666666666664 ], [ -108.41666666666667,38.833333333333336 ], [ -108.75,38.833333333333336 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db698641","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":274460,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":64244,"text":"gp318 - 1963 - Aeromagnetic map of the Ahmeek quadrangle, Keweenaw and Houghton Counties, Michigan","interactions":[],"lastModifiedDate":"2012-02-10T00:10:58","indexId":"gp318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":317,"text":"Geophysical Investigations Map","code":"GP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"318","title":"Aeromagnetic map of the Ahmeek quadrangle, Keweenaw and Houghton Counties, Michigan","language":"ENGLISH","doi":"10.3133/gp318","usgsCitation":"Balsley, J.R., Meuschke, J.L., and Blanchett, J., 1963, Aeromagnetic map of the Ahmeek quadrangle, Keweenaw and Houghton Counties, Michigan: U.S. Geological Survey Geophysical Investigations Map 318, 1 map., https://doi.org/10.3133/gp318.","productDescription":"1 map.","costCenters":[],"links":[{"id":250814,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gp/0318/report.pdf","size":"30","linkFileType":{"id":1,"text":"pdf"}},{"id":250815,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0318/plate-1.pdf","size":"1993","linkFileType":{"id":1,"text":"pdf"}},{"id":254283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gp/0318/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.5,47.25 ], [ -88.5,47.3675 ], [ -88.36749999999999,47.3675 ], [ -88.36749999999999,47.25 ], [ -88.5,47.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973ba","contributors":{"authors":[{"text":"Balsley, James R.","contributorId":10010,"corporation":false,"usgs":true,"family":"Balsley","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":270297,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meuschke, J. L.","contributorId":53349,"corporation":false,"usgs":true,"family":"Meuschke","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":270298,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blanchett, Jean","contributorId":91177,"corporation":false,"usgs":true,"family":"Blanchett","given":"Jean","email":"","affiliations":[],"preferred":false,"id":270299,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70112249,"text":"70112249 - 1963 - Photography and imagery: a clarification of terms","interactions":[],"lastModifiedDate":"2017-03-27T13:36:30","indexId":"70112249","displayToPublicDate":"1990-06-12T08:42:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3051,"text":"Photogrammetric Engineering","active":true,"publicationSubtype":{"id":10}},"title":"Photography and imagery: a clarification of terms","docAbstract":"<p>The increased use of pictorial displays of data in the fields of photogrammetry and photo interpretation has led to some confusion of terms, not so much b photogrammetrists as bu users and interpreters of pictorial data. The terms \"remote sensing\" and \"remote sensing of environment\" are being used as general terms to describe \"the measurement of some property of an object without having the measuring device physically in contact with the object\" (Parker, 1962).</p><p>Measurements of size and shape by photogrammetric and optical means are common examples of remote sensing and therefore require no elaboration. Other techniques of remote sensing of electromagnetic radiation in and beyond the limits of the visible spectrum require some explanation and differentiation from the techniques used in the visible spectrum.</p><p>The following definitions of \"photography\" and \"imagery\" are proposed to clarify these two terms in hope that this will lead to more precise understanding and explanation of the processes.</p>","language":"English","publisher":"American Society of Photogrammetry","publisherLocation":"Falls Church, VA","usgsCitation":"Robinove, C.J., 1963, Photography and imagery: a clarification of terms: Photogrammetric Engineering, v. 29, no. 5, p. 880-881.","productDescription":"2 p.","startPage":"880","endPage":"881","numberOfPages":"2","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":288415,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"5","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"539acc0de4b0e83db6d08fad","contributors":{"authors":[{"text":"Robinove, Charles J.","contributorId":16983,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":494573,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70187527,"text":"70187527 - 1963 - Downstream patterns of riverbed scour and fill","interactions":[],"lastModifiedDate":"2017-05-07T09:56:56","indexId":"70187527","displayToPublicDate":"1965-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Downstream patterns of riverbed scour and fill","docAbstract":"<p>Progress has been made in describing riverbed scour and fill at a given stream section. One needs only the data routinely collected at a stream-gaging station to observe scour and fill at that station. However, similar progress has not been made to determine whether or not the scour and fill observed at a given section extends over a relatively long reach of the channel. Gaging stations are generally located too far apart to draw any conclusions as to scour processes between stations. It remains necessary then to establish a sufficient number of cross sections along a channel to describe the downstream pattern of riverbed scour.</p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"Proceedings of the second federal interagency sedimentation conference (U.S. DOA Miscellaneous Publication 70)","largerWorkSubtype":{"id":12,"text":"Conference publication"},"conferenceTitle":"Federal Interagency Sedimentation Conference","conferenceDate":"January 28, 1963","conferenceLocation":"Jackson, MS","language":"English","publisher":"U.S. Department of Agriculture","usgsCitation":"Emmett, W.W., and Leopold, L.B., 1963, Downstream patterns of riverbed scour and fill, <i>in</i> Proceedings of the second federal interagency sedimentation conference (U.S. DOA Miscellaneous Publication 70), Jackson, MS, January 28, 1963, p. 399-409.","productDescription":"11 p.","startPage":"399","endPage":"409","costCenters":[],"links":[{"id":340877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":340876,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://acwi.gov/8thFISC-ordering-revised.html"}],"publicComments":"Paper no. 46","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5910322ce4b0e541a03a8584","contributors":{"authors":[{"text":"Emmett, William W.","contributorId":68715,"corporation":false,"usgs":true,"family":"Emmett","given":"William","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":694324,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":694325,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70106991,"text":"70106991 - 1963 - Surface water records of Indiana, 1963","interactions":[],"lastModifiedDate":"2014-06-02T06:01:42","indexId":"70106991","displayToPublicDate":"1964-01-01T13:43:33","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"title":"Surface water records of Indiana, 1963","docAbstract":"<p>The surface-water records for the 1963 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":"10.3133/70106991","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, 1963, Surface water records of Indiana, 1963, vii, 194 p., https://doi.org/10.3133/70106991.","productDescription":"vii, 194 p.","numberOfPages":"204","temporalStart":"1962-10-01","temporalEnd":"1963-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":287924,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287923,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70106991/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":"537b2808e4b0929ba496abc2","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":535653,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":37741,"text":"wl449 - 1963 - 1962 Public use of National Wildlife Refuges.","interactions":[],"lastModifiedDate":"2012-02-02T00:16:00","indexId":"wl449","displayToPublicDate":"1964-01-01T12:20:15","publicationYear":"1963","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":"449","title":"1962 Public use of National Wildlife Refuges.","language":"ENGLISH","publisher":"U.S. Fish and Wildife Service","usgsCitation":"Bureau Of Sport Fisheries And Wildlife, 1963, 1962 Public use of National Wildlife Refuges. (Revises Wildlife Leaflet 442 (1962).): Wildlife Leaflet 449, 6 p.","productDescription":"6 p.","costCenters":[],"links":[{"id":112351,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015007538955?urlappend=%3Bseq=3"},{"id":204199,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"edition":"Revises Wildlife Leaflet 442 (1962).","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd490fe4b0b290850eed91","contributors":{"authors":[{"text":"Bureau Of Sport Fisheries And Wildlife","contributorId":128243,"corporation":true,"usgs":false,"organization":"Bureau Of Sport Fisheries And Wildlife","id":529692,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207390,"text":"70207390 - 1963 - Cathedral Cliffs formation, the early acid Breccia unit of northwestern Wyoming","interactions":[],"lastModifiedDate":"2019-12-19T07:49:39","indexId":"70207390","displayToPublicDate":"1963-12-31T14:20:00","publicationYear":"1963","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":"Cathedral Cliffs formation, the early acid Breccia unit of northwestern Wyoming","docAbstract":"<p><span>The name Cathedral Cliffs Formation is proposed for the rocks in the Clarks Fork area of northwestern Wyoming that have long been known by the informal designation \"early acid breccia.\" In the Clarks Fork area the Cathedral Cliffs Formation is composed of tuffs, with lesser amounts of volcanic sedimentary rocks and breccias. Its thickness ranges from less than 100 feet to about 1500 feet but more commonly is 500-900 feet. The formation is tentatively considered to be late early Eocene or early middle Eocene. It is underlain by rocks ranging from Precambrian to early Eocene(?) and is overlain unconformably by the early basic breccia of middle Eocene age. Low-angle detachment faulting, which involved the Cathedral Cliffs Formation but not the overlying early basic breccia, has made recognition and correlation of the formation difficult. Blocks and masses of Madison Limestone of Mississippian age were emplaced locally on its upper surface by the Reef Creek detachment fault. The Cathedral Cliffs Formation and the Paleozoic carbonate rocks beneath it, as well as the Reef Creek fault masses on its surface, were then transported southeastward by the Heart Mountain detachment fault. As movement on the Heart Mountain detachment proceeded, the large fault mass broke up into smaller blocks, which separated as movement continued. Consequently the Cathedral Cliffs Formation was distributed in a pattern which gives the appearance of isolated occurrences and erosional remnants. The detached blocks of the Reef Creek fault on the upper surface of the Cathedral Cliffs also were scattered more widely than by their original movement on the Reef Creek fault. Soon after the fault-transported segments of the Cathedral Cliffs Formation ceased moving they were buried beneath the early basic breccia. The unconformity between the early acid breccia and the early basic breccia is thus substantiated in the Clarks Fork area; in the time interval represented, the Reef Creek and Heart Mountain fault masses were emplaced. The Cathedral Cliffs Formation is correlated with the early acid breccia in northern Yellowstone National Park and the upper part of the Reese Formation as mapped by Calvert west of Gardiner, Montana. The volcanic-source area probably is not in the central Yellowstone Park region, but somewhere to the north. © 1963, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[9:CCFTEA]2.0.CO;2","issn":"00167606","usgsCitation":"Pierce, W.G., 1963, Cathedral Cliffs formation, the early acid Breccia unit of northwestern Wyoming: Geological Society of America Bulletin, v. 74, no. 1, p. 9-22, https://doi.org/10.1130/0016-7606(1963)74[9:CCFTEA]2.0.CO;2.","productDescription":"14 p. 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States","state":"Wyoming","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-110.048476,40.997555],[-110.121639,40.997101],[-110.125709,40.99655],[-110.237848,40.995427],[-110.250709,40.996089],[-110.375714,40.994947],[-110.500718,40.994746],[-110.539819,40.996346],[-110.715026,40.996347],[-110.750727,40.996847],[-111.046723,40.997959],[-111.046551,41.251716],[-111.0466,41.360692],[-111.046264,41.377731],[-111.045789,41.565571],[-111.045818,41.579845],[-111.046689,42.001567],[-111.047109,42.142497],[-111.047107,42.148971],[-111.047058,42.182672],[-111.047097,42.194773],[-111.047074,42.280787],[-111.04708,42.34942],[-111.046801,42.504946],[-111.046719,42.513118],[-111.046017,42.582723],[-111.043564,42.722624],[-111.044135,42.874924],[-111.043959,42.96445],[-111.043957,42.969482],[-111.043924,42.975063],[-111.044129,43.018702],[-111.044156,43.020052],[-111.044206,43.022614],[-111.044034,43.024581],[-111.044034,43.024844],[-111.044033,43.026411],[-111.044094,43.02927],[-111.043997,43.041415],[-111.044058,43.04464],[-111.044063,43.046302],[-111.044086,43.054819],[-111.044117,43.060309],[-111.04415,43.066172],[-111.044162,43.068222],[-111.044143,43.072364],[-111.044235,43.177121],[-111.044266,43.177236],[-111.044232,43.18444],[-111.044168,43.189244],[-111.044229,43.195579],[-111.044617,43.31572],[-111.045205,43.501136],[-111.045706,43.659112],[-111.04588,43.681033],[-111.046118,43.684902],[-111.046051,43.685812],[-111.04611,43.687848],[-111.046421,43.722059],[-111.046435,43.726545],[-111.04634,43.726957],[-111.046715,43.815832],[-111.046515,43.908376],[-111.046917,43.974978],[-111.047064,43.983467],[-111.047349,43.999921],[-111.049077,44.020072],[-111.048751,44.060403],[-111.048751,44.060838],[-111.048633,44.062903],[-111.048452,44.114831],[-111.049119,44.124923],[-111.049695,44.353626],[-111.049148,44.374925],[-111.049216,44.435811],[-111.049194,44.438058],[-111.048974,44.474072],[-111.055208,44.624927],[-111.055333,44.666263],[-111.055511,44.725343],[-111.056416,44.749928],[-111.056888,44.866658],[-111.055629,44.933578],[-111.056207,44.935901],[-111.055199,45.001321],[-111.044275,45.001345],[-110.785008,45.002952],[-110.761554,44.999934],[-110.750767,44.997948],[-110.705272,44.992324],[-110.552433,44.992237],[-110.547165,44.992459],[-110.48807,44.992361],[-110.402927,44.99381],[-110.362698,45.000593],[-110.342131,44.999053],[-110.324441,44.999156],[-110.28677,44.99685],[-110.199503,44.996188],[-110.110103,45.003905],[-110.026347,45.003665],[-110.025544,45.003602],[-109.99505,45.003174],[-109.875735,45.003275],[-109.798687,45.002188],[-109.75073,45.001605],[-109.663673,45.002536],[-109.574321,45.002631],[-109.386432,45.004887],[-109.375713,45.00461],[-109.269294,45.005283],[-109.263431,45.005345],[-109.103445,45.005904],[-109.08301,44.99961],[-109.062262,44.999623],[-108.621313,45.000408],[-108.578484,45.000484],[-108.565921,45.000578],[-108.500679,44.999691],[-108.271201,45.000251],[-108.249345,44.999458],[-108.238139,45.000206],[-108.218479,45.000541],[-108.14939,45.001062],[-108.000663,45.001223],[-107.997353,45.001565],[-107.911743,45.001292],[-107.750654,45.000778],[-107.608854,45.00086],[-107.607824,45.000929],[-107.49205,45.00148],[-107.351441,45.001407],[-107.13418,45.000109],[-107.125633,44.999388],[-107.105685,44.998734],[-107.084939,44.996599],[-107.074996,44.997004],[-107.050801,44.996424],[-106.892875,44.995947],[-106.888773,44.995885],[-106.263586,44.993788],[-106.024814,44.993688],[-105.928184,44.993647],[-105.914258,44.999986],[-105.913382,45.000941],[-105.848065,45.000396],[-105.076607,45.000347],[-105.038405,45.000345],[-105.025266,45.00029],[-105.019284,45.000329],[-105.01824,45.000437],[-104.765063,44.999183],[-104.759855,44.999066],[-104.72637,44.999518],[-104.665171,44.998618],[-104.663882,44.998869],[-104.470422,44.998453],[-104.470117,44.998453],[-104.250145,44.99822],[-104.057698,44.997431],[-104.055914,44.874986],[-104.056496,44.867034],[-104.055963,44.768236],[-104.055963,44.767962],[-104.055934,44.72372],[-104.05587,44.723422],[-104.055777,44.700466],[-104.055938,44.693881],[-104.05581,44.691343],[-104.055877,44.571016],[-104.055892,44.543341],[-104.055927,44.51773],[-104.055389,44.249983],[-104.054487,44.180381],[-104.054562,44.141081],[-104.05495,43.93809],[-104.055077,43.936535],[-104.055488,43.853477],[-104.055488,43.853476],[-104.055138,43.750421],[-104.055133,43.747105],[-104.054902,43.583852],[-104.054885,43.583512],[-104.05484,43.579368],[-104.055032,43.558603],[-104.054787,43.503328],[-104.054786,43.503072],[-104.054779,43.477815],[-104.054766,43.428914],[-104.054614,43.390949],[-104.054403,43.325914],[-104.054218,43.30437],[-104.053884,43.297047],[-104.053876,43.289801],[-104.053127,43.000585],[-104.052863,42.754569],[-104.052809,42.749966],[-104.052583,42.650062],[-104.052741,42.633982],[-104.052586,42.630917],[-104.052773,42.611766],[-104.052775,42.61159],[-104.052775,42.610813],[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 \"}}]}","volume":"74","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Pierce, W. G.","contributorId":11267,"corporation":false,"usgs":true,"family":"Pierce","given":"W.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":777888,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70207263,"text":"70207263 - 1963 - Geologic history of the teays valley in West Virginia","interactions":[],"lastModifiedDate":"2019-12-16T06:49:01","indexId":"70207263","displayToPublicDate":"1963-12-31T08:23:40","publicationYear":"1963","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":"Geologic history of the teays valley in West Virginia","docAbstract":"<p><span>The segment of the abandoned pre-Pleistocene Teays Valley between Scary and Huntington, W. Va. stands 130-240 feet above the Ohio and Kanawha rivers, and its bedrock floor slopes westward at about 0.6 foot per mile. The bedrock floor is overlain by highly weathered gravel in which a soil profile developed; only resistant siliceous materials remain. As much as 100 feet of locally derived sediments overlies the basal gravel. Sand was deposited at each end of the valley but in the east-central part it grades laterally into a laminated silty clay that was deposited during a period of ponding, probably in Kansan time. These deposits are deeply eroded. Probably during Illinoian time, ponding at a lower level resulted in deposition of a younger silty clay in the western part of the valley. This silty clay is weathered to a depth of about 14 feet. During a brief ponding in Wisconsin time, a widely scattered veneer of ice-rafted unweathered pebbles of igneous and metamorphic rocks was deposited. This veneer represents the youngest Pleistocene deposits in the valley and it occurs as much as 110 feet above the present Ohio River. Depositional, weathering, erosional, and topographic evidence argues that the Teays Valley in West Virginia was abandoned in late Tertiary or early Pleistocene time by normal stream-capture processes and that prolonged weathering followed. © 1963, The Geological Society of America, Inc.</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[251:GHOTTV]2.0.CO;2","issn":"00167606","usgsCitation":"Rhodehamel, E., and Carlston, C., 1963, Geologic history of the teays valley in West Virginia: Geological Society of America Bulletin, v. 74, no. 3, p. 251-274, https://doi.org/10.1130/0016-7606(1963)74[251:GHOTTV]2.0.CO;2.","productDescription":"24 p.","startPage":"251","endPage":"274","costCenters":[],"links":[{"id":370269,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"West Virginia 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Virginia\",\"nation\":\"USA  \"}}]}","volume":"74","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Rhodehamel, E. C.","contributorId":91517,"corporation":false,"usgs":true,"family":"Rhodehamel","given":"E. C.","affiliations":[],"preferred":false,"id":777490,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carlston, C.W.","contributorId":26062,"corporation":false,"usgs":true,"family":"Carlston","given":"C.W.","affiliations":[],"preferred":false,"id":777491,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010631,"text":"70010631 - 1963 - Uranyl ion coordination","interactions":[],"lastModifiedDate":"2026-02-19T16:55:12.605558","indexId":"70010631","displayToPublicDate":"1963-12-27T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Uranyl ion coordination","docAbstract":"<p><span>A review of the known crystal structures containing the uranyl ion shows that plane-pentagon coordination is equally as prevalent as plane0square or plane-hexagon. It is suggested that puckered-hexagon configurations of OH</span><sup>-</sup><span>&nbsp;or H</span><sub>2</sub><span>O about the uranyl group will tend to revert to plane-pentagon coordination. The concept of pentagonal coordination is invoked for possible explanations of the complex crystallography of the natural uranyl hydroxides and the unusual behavior of polynuclear ions in hydrolyzed uranyl solutions.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3600.1651.a","issn":"00368075","usgsCitation":"Evans, H.T., 1963, Uranyl ion coordination: Science, v. 141, no. 3576, p. 154-158, https://doi.org/10.1126/science.142.3600.1651.a.","productDescription":"5 p.","startPage":"154","endPage":"158","costCenters":[],"links":[{"id":219251,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3576","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbe08e4b08c986b329399","contributors":{"authors":[{"text":"Evans, H. T. Jr.","contributorId":41859,"corporation":false,"usgs":true,"family":"Evans","given":"H.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":359301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010790,"text":"70010790 - 1963 - Tellurium content of marine manganese oxides and other manganese oxides","interactions":[],"lastModifiedDate":"2026-02-13T16:33:48.830135","indexId":"70010790","displayToPublicDate":"1963-12-20T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tellurium content of marine manganese oxides and other manganese oxides","docAbstract":"Tellurium in amounts ranging from 5 to 125 parts per million was present in all of 12 samples of manganese oxide nodules from the floor of the Pacific and Indian oceans. These samples represent the first recognized points of high tellurium concentration in a sedimentary cycle. The analyses may lend support to the theory that the minor-element content of seafloor manganese nodules is derived from volcanic emanations.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3599.1568","issn":"00368075","usgsCitation":"Lakin, H.W., Thompson, C.E., and Davidson, D., 1963, Tellurium content of marine manganese oxides and other manganese oxides: Science, v. 142, no. 3599, p. 1568-1569, https://doi.org/10.1126/science.142.3599.1568.","productDescription":"2 p.","startPage":"1568","endPage":"1569","costCenters":[],"links":[{"id":218666,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3599","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba4b3e4b08c986b320503","contributors":{"authors":[{"text":"Lakin, H. W.","contributorId":11594,"corporation":false,"usgs":true,"family":"Lakin","given":"H.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359651,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, C. E.","contributorId":44171,"corporation":false,"usgs":true,"family":"Thompson","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359652,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Davidson, D.F.","contributorId":68293,"corporation":false,"usgs":true,"family":"Davidson","given":"D.F.","email":"","affiliations":[],"preferred":false,"id":359653,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010803,"text":"70010803 - 1963 - Phosphate glass electrode with good selectivity for alkaline-earth cations","interactions":[],"lastModifiedDate":"2026-02-13T16:38:06.037492","indexId":"70010803","displayToPublicDate":"1963-12-06T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Phosphate glass electrode with good selectivity for alkaline-earth cations","docAbstract":"<p><span>A phosphate glass has been found to have a significant electrode specificity toward alkaline-earth ions. The order of selectivity is 2H</span><sup>+</sup><span>&nbsp;&gt; Ba</span><sup>++</sup><span>&nbsp;&gt; Sr</span><sup>++</sup><span>&nbsp;&gt; Ca</span><sup>++</sup><span>&nbsp;&gt; 2K</span><sup>+</sup><span>&nbsp;&gt; 2Na</span><sup>+</sup><span>&nbsp;&gt; Mg</span><sup>++</sup><span>. Exchange properties are discussed in relation to possible structure. Its use to determine activity of Ca</span><sup>++</sup><span>&nbsp;in natural systems containing Mg</span><sup>++</sup><span>&nbsp;is suggested.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3597.1292","issn":"00368075","usgsCitation":"Truesdell, A., and Pommer, A., 1963, Phosphate glass electrode with good selectivity for alkaline-earth cations: Science, v. 142, no. 3597, p. 1292-1294, https://doi.org/10.1126/science.142.3597.1292.","productDescription":"3 p.","startPage":"1292","endPage":"1294","costCenters":[],"links":[{"id":218669,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3597","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a789ee4b0c8380cd78739","contributors":{"authors":[{"text":"Truesdell, A.H.","contributorId":52566,"corporation":false,"usgs":false,"family":"Truesdell","given":"A.H.","email":"","affiliations":[{"id":6672,"text":"former: USGS Southwest Biological Science Center, Colorado Plateau Research Station, Flagstaff, AZ. Current address:  TN-SCORE, Univ of Tennessee, Knoxville, TN, e-mail: jennen@gmail.com","active":true,"usgs":false}],"preferred":false,"id":359684,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pommer, A. M.","contributorId":20795,"corporation":false,"usgs":false,"family":"Pommer","given":"A. M.","affiliations":[],"preferred":false,"id":359683,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221080,"text":"70221080 - 1963 - Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","interactions":[],"lastModifiedDate":"2021-06-01T18:12:38.075721","indexId":"70221080","displayToPublicDate":"1963-12-01T13:08:36","publicationYear":"1963","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":"Correlations and problems in belt series stratigraphy, Northern idaho and western Montana","docAbstract":"<p><span>A continuous strip of geologic maps has recently been completed along the&nbsp;</span><span class=\"ScopusTermHighlight\">Idaho</span><span>-</span><span class=\"ScopusTermHighlight\">Montana</span><span>&nbsp;state line between Clark Fork,&nbsp;</span><span class=\"ScopusTermHighlight\">Idaho</span><span>, and Superior,&nbsp;</span><span class=\"ScopusTermHighlight\">Montana</span><span>. New stratigraphic and petrographic information provides the basis for stratigraphic&nbsp;</span><span class=\"ScopusTermHighlight\">correlations</span><span>&nbsp;and for the interpretation of facies changes&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;this part of the basin of deposition of the Precambrian&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">Series</span><span>. Identification of facies changes is aided by the recognition of siltite (low-grade metamorphosed siltstone) as a valid rock type,&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;addition to quartzite and argillite, to classify most of these rocks and to establish mappable units. The older&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;rocks (Prichard through Wallace Formations) were deposited&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;a trough whose axis trended northwestward, perhaps approximately through Libby,&nbsp;</span><span class=\"ScopusTermHighlight\">Montana</span><span>. Subtle facies changes suggest an ancient shore line southwest of the Coeur d'Alene district,&nbsp;</span><span class=\"ScopusTermHighlight\">Idaho</span><span>, perhaps near the present exposed edge of the&nbsp;</span><span class=\"ScopusTermHighlight\">Idaho</span><span>&nbsp;batholith. The younger&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;formations of the Missoula Group, however, thicken markedly southeastward toward Superior. Thus, the younger&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;rocks were deposited&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;a trough whose main axis was about at right angles to that of the older trough and perhaps was near Missoula,&nbsp;</span><span class=\"ScopusTermHighlight\">Montana</span><span>. Deposition&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the Clark Fork area was scant and often interrupted&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;Missoula time. The young major cross-warp&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the old&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;geosyncline undoubtedly has contributed complexities to&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;</span><span class=\"ScopusTermHighlight\">correlation</span><span>&nbsp;farther north. Detailed petrographic studies indicate that the&nbsp;</span><span class=\"ScopusTermHighlight\">Belt</span><span>&nbsp;rocks from the Pend Oreille area,&nbsp;</span><span class=\"ScopusTermHighlight\">Idaho</span><span>, are remarkably uniform&nbsp;</span><span class=\"ScopusTermHighlight\">in</span><span>&nbsp;the mineralogic composition of similar rock types throughout 40,000 feet of strata. Further mineralogic studies are required to determine whether this uniformity is local or widespread.&nbsp;</span></p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2","usgsCitation":"Harrison, J.E., and Campbell, A., 1963, Correlations and problems in belt series stratigraphy, Northern idaho and western Montana: Geological Society of America Bulletin, v. 74, no. 12, p. 1413-1427, https://doi.org/10.1130/0016-7606(1963)74[1413:CAPIBS]2.0.CO;2.","productDescription":"15 p.","startPage":"1413","endPage":"1427","costCenters":[],"links":[{"id":386055,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Idaho, Montana","otherGeospatial":"northern Idaho, western Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.96044921875,\n              46.34692761055676\n            ],\n            [\n              -110.6982421875,\n              46.34692761055676\n            ],\n            [\n              -110.6982421875,\n              48.951366470947725\n            ],\n            [\n              -116.96044921875,\n              48.951366470947725\n            ],\n            [\n              -116.96044921875,\n              46.34692761055676\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"74","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Harrison, J. E.","contributorId":54532,"corporation":false,"usgs":true,"family":"Harrison","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":816709,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Campbell, A.B.","contributorId":22764,"corporation":false,"usgs":true,"family":"Campbell","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":816710,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221061,"text":"70221061 - 1963 - Relation between the crystal content and the chemical composition of welded tuffs","interactions":[],"lastModifiedDate":"2021-06-01T16:13:00.701383","indexId":"70221061","displayToPublicDate":"1963-12-01T11:09:37","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Relation between the crystal content and the chemical composition of welded tuffs","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02597280","usgsCitation":"Peterson, D.W., and Roberts, R.J., 1963, Relation between the crystal content and the chemical composition of welded tuffs: Bulletin Volcanologique, v. 26, p. 113-123, https://doi.org/10.1007/BF02597280.","productDescription":"11 p.","startPage":"113","endPage":"123","costCenters":[],"links":[{"id":386032,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"26","noUsgsAuthors":false,"publicationDate":"1963-12-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Peterson, Donald W.","contributorId":11209,"corporation":false,"usgs":true,"family":"Peterson","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":816672,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roberts, Ralph Jackson","contributorId":63010,"corporation":false,"usgs":true,"family":"Roberts","given":"Ralph","email":"","middleInitial":"Jackson","affiliations":[],"preferred":false,"id":816673,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70221112,"text":"70221112 - 1963 - Ash-flow problems — a synthesis based on field and laboratory studies","interactions":[],"lastModifiedDate":"2021-06-02T13:49:13.171003","indexId":"70221112","displayToPublicDate":"1963-12-01T08:46:21","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1093,"text":"Bulletin Volcanologique","active":true,"publicationSubtype":{"id":10}},"title":"Ash-flow problems — a synthesis based on field and laboratory studies","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"Springer","doi":"10.1007/BF02596543","usgsCitation":"Smith, R.L., 1963, Ash-flow problems — a synthesis based on field and laboratory studies: Bulletin Volcanologique, v. 25, p. 109-110, https://doi.org/10.1007/BF02596543.","productDescription":"2 p.","startPage":"109","endPage":"110","costCenters":[],"links":[{"id":386121,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"25","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Smith, Robert L.","contributorId":90803,"corporation":false,"usgs":true,"family":"Smith","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":816790,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010786,"text":"70010786 - 1963 - Paleontologic investigations at Big Bone Lick State Park, Kentucky: A preliminary report","interactions":[],"lastModifiedDate":"2026-02-13T16:58:28.760941","indexId":"70010786","displayToPublicDate":"1963-11-29T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Paleontologic investigations at Big Bone Lick State Park, Kentucky: A preliminary report","docAbstract":"<p><span>The Big Bone Lick area in Kentucky, the first widely known collecting locality for vertebrate fossils in North America, is being investigated for further faunal and geologic evidence. Mammal bones, ranging in age from Wisconsin (Tazewell?) to Recent, were recovered in 1962 from four different faunal zones in two terrace fills.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.142.3596.1167","issn":"00368075","usgsCitation":"Schultz, C., Tanner, L., Whitmore, F., Ray, L., and Crawford, E., 1963, Paleontologic investigations at Big Bone Lick State Park, Kentucky: A preliminary report: Science, v. 142, no. 3596, p. 1167-1169, https://doi.org/10.1126/science.142.3596.1167.","productDescription":"3 p.","startPage":"1167","endPage":"1169","costCenters":[],"links":[{"id":500093,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Kentucky","otherGeospatial":"Big Bone Lake State Park","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.7646713256836,\n              38.87419582538936\n            ],\n            [\n              -84.73274230957031,\n              38.87419582538936\n            ],\n            [\n              -84.73274230957031,\n              38.89343778664929\n            ],\n            [\n              -84.7646713256836,\n              38.89343778664929\n            ],\n            [\n              -84.7646713256836,\n              38.87419582538936\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"142","issue":"3596","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a7432e4b0c8380cd774d8","contributors":{"authors":[{"text":"Schultz, C.B.","contributorId":66838,"corporation":false,"usgs":true,"family":"Schultz","given":"C.B.","email":"","affiliations":[],"preferred":false,"id":359644,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tanner, L.G.","contributorId":100524,"corporation":false,"usgs":true,"family":"Tanner","given":"L.G.","email":"","affiliations":[],"preferred":false,"id":359646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitmore, F.C. Jr.","contributorId":16895,"corporation":false,"usgs":true,"family":"Whitmore","given":"F.C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359642,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ray, L.L.","contributorId":73741,"corporation":false,"usgs":true,"family":"Ray","given":"L.L.","email":"","affiliations":[],"preferred":false,"id":359645,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Crawford, E.C.","contributorId":37057,"corporation":false,"usgs":true,"family":"Crawford","given":"E.C.","email":"","affiliations":[],"preferred":false,"id":359643,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":70010836,"text":"70010836 - 1963 - Tritium distribution in ground water around large underground fusion explosions","interactions":[],"lastModifiedDate":"2026-02-13T16:54:23.910977","indexId":"70010836","displayToPublicDate":"1963-11-29T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Tritium distribution in ground water around large underground fusion explosions","docAbstract":"Tritium will be released in significant amounts from large underground nuclear fusion explosions in the Plowshare Program. The tritium could become highly concentrated in nearby ground waters, and could be of equal or more importance as a possible contaminant than other long-lived fission-product and induced radionuclides. Behavior of tritiated water in particular hydrologic and geologic environments, as illustrated by hypothetical explosions in dolomite and tuff, must be carefully evaluated to predict under what conditions high groundwater concentrations of tritium might occur.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3596.1163","issn":"00368075","usgsCitation":"Stead, F., 1963, Tritium distribution in ground water around large underground fusion explosions: Science, v. 142, no. 3596, p. 1163-1165, https://doi.org/10.1126/science.142.3596.1163.","productDescription":"3 p.","startPage":"1163","endPage":"1165","costCenters":[],"links":[{"id":218957,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3596","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bb86ce4b08c986b327852","contributors":{"authors":[{"text":"Stead, F.W.","contributorId":42653,"corporation":false,"usgs":true,"family":"Stead","given":"F.W.","email":"","affiliations":[],"preferred":false,"id":359759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70171205,"text":"70171205 - 1963 - Insecticides: effects on cutthroat trout of repeated exposure to DDT","interactions":[],"lastModifiedDate":"2016-05-25T15:22:28","indexId":"70171205","displayToPublicDate":"1963-11-15T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Insecticides: effects on cutthroat trout of repeated exposure to DDT","docAbstract":"<p><span>Cutthroat trout were periodically exposed to p, pp-DDT, in acetone solution or in the food. Excessive mortality occurred only in lots treated with high concentrations of DDT, probably as a result of decreased resistance to nonspecific stressors. Surviving fish in these lots were significantly larger than those in the control lot, or in the lots treated with low concentrations of DDT. The number and volume of eggs produced was not reduced by DDT, but mortality among sac fry appeared to be highest in the lots treated with high concentrations. The data suggest that the sublethal concentrations of DDT ordinarily encountered in the environment are unlikely to damage a fishery.</span></p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3594.958","usgsCitation":"Allison, D., Kallman, B.J., Cope, O.B., and Van Valin, C.C., 1963, Insecticides: effects on cutthroat trout of repeated exposure to DDT: Science, v. 142, no. 3594, p. 958-961, https://doi.org/10.1126/science.142.3594.958.","productDescription":"4 p.","startPage":"958","endPage":"961","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":321667,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"142","issue":"3594","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5746ccbde4b07e28b662dce8","contributors":{"authors":[{"text":"Allison, Don","contributorId":169608,"corporation":false,"usgs":true,"family":"Allison","given":"Don","email":"","affiliations":[],"preferred":false,"id":630264,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kallman, Burton J.","contributorId":169580,"corporation":false,"usgs":false,"family":"Kallman","given":"Burton","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":630265,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cope, Oliver B.","contributorId":13290,"corporation":false,"usgs":true,"family":"Cope","given":"Oliver","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":630266,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Van Valin, Charles C.","contributorId":169609,"corporation":false,"usgs":false,"family":"Van Valin","given":"Charles","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":630267,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":70221118,"text":"70221118 - 1963 - Early pennsylvanian currents in the southern Appalachian Mountains","interactions":[],"lastModifiedDate":"2021-06-04T12:02:11.312222","indexId":"70221118","displayToPublicDate":"1963-11-01T11:00:12","publicationYear":"1963","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":"Early pennsylvanian currents in the southern Appalachian Mountains","docAbstract":"<p>Measurement of more than 1200 cross-beds in lower Pennsylvanian sandstones of the southern Appalachian Mountains reveals a broad pattern of sediment transport to the southwest and west. Most of the sand appears to have been derived from the east and to have moved south-westward parallel to the axis of the Appalachian geosyncline. The pattern has a similar alignment to that in the Illinois basin, but it is at right angles to earlier Paleozoic dispersal directions in the Appalachian geosyncline. Little or no sand has been contributed from the Cincinnati arch.</p><p>The cross-beds are in sheetlike sandstone formations; the sandstone is conglomeratic, contains plant impressions, and is composed of lenticular, channeling, quartzose sedimentation units. The variation in thickness and lateral persistence of sedimentation units is also reflected in a moderate variability of mean cross-bedding directions between adjacent formations, and even within the same formation. Cross-bedding variability between adjacent units is thought to be due to regional changes in the position and orientation of channel-way systems from deposition of one sandstone formation to the next. Changes of cross-bedding azimuths within the same formation may result from channel curvature of local meanderlike deposits or from channel migration as the sands coalesced into a blanket deposit.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1963)74[1439:EPCITS]2.0.CO;2","usgsCitation":"Schlee, J., 1963, Early pennsylvanian currents in the southern Appalachian Mountains: Geological Society of America Bulletin, v. 74, no. 12, p. 1439-1451, https://doi.org/10.1130/0016-7606(1963)74[1439:EPCITS]2.0.CO;2.","productDescription":"13 p.","startPage":"1439","endPage":"1451","costCenters":[],"links":[{"id":386190,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United  States","state":"Kentucky, Tennessee, Alabama, Georgia","otherGeospatial":"southern Appalachian Mountains","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.23291015625,\n              37.85750715625203\n            ],\n            [\n              -84.52880859375,\n              36.155617833818525\n            ],\n            [\n              -86.63818359375,\n              34.470335121217474\n            ],\n            [\n              -85.93505859374999,\n              33.815666308702774\n            ],\n            [\n              -84.17724609375,\n              34.903952965590065\n            ],\n            [\n              -80.52978515625,\n              36.27970720524017\n            ],\n            [\n              -81.23291015625,\n              37.85750715625203\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"74","issue":"12","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Schlee, J.","contributorId":45821,"corporation":false,"usgs":true,"family":"Schlee","given":"J.","affiliations":[],"preferred":false,"id":816939,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010838,"text":"70010838 - 1963 - Lead isotope variation with growth zoning in a galena crystal","interactions":[],"lastModifiedDate":"2026-02-19T16:01:25.872624","indexId":"70010838","displayToPublicDate":"1963-11-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Lead isotope variation with growth zoning in a galena crystal","docAbstract":"A large crystal of lead sulfide from Picher, Oklahoma, has significant differences in isotopic composition of lead in successive growth zones. Lead isotope ratios in the parent ore-fluid evidently changed with time during crystal growth. The growth history of this crystal, interpreted quantitatively, points to a tentative hypothesis of genesis of Mississippi Valley deposits of lead and zinc.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3592.574","issn":"00368075","usgsCitation":"Cannon, R., Pierce, A., and Delevaux, M., 1963, Lead isotope variation with growth zoning in a galena crystal: Science, v. 142, no. 3592, p. 574-576, https://doi.org/10.1126/science.142.3592.574.","productDescription":"3 p.","startPage":"574","endPage":"576","costCenters":[],"links":[{"id":218959,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oklahoma","city":"Picher","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -94.84474868584753,\n              36.99843933084928\n            ],\n            [\n              -94.84474868584753,\n              36.96871916843759\n            ],\n            [\n              -94.81377116646598,\n              36.96871916843759\n            ],\n            [\n              -94.81377116646598,\n              36.99843933084928\n            ],\n            [\n              -94.84474868584753,\n              36.99843933084928\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"142","issue":"3592","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a45c3e4b0c8380cd674ae","contributors":{"authors":[{"text":"Cannon, R.S. Jr.","contributorId":21622,"corporation":false,"usgs":true,"family":"Cannon","given":"R.S.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":359762,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, A.P.","contributorId":65833,"corporation":false,"usgs":true,"family":"Pierce","given":"A.P.","email":"","affiliations":[],"preferred":false,"id":359764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Delevaux, M.H.","contributorId":27853,"corporation":false,"usgs":true,"family":"Delevaux","given":"M.H.","email":"","affiliations":[],"preferred":false,"id":359763,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010447,"text":"70010447 - 1963 - Geomagnetic polarity epochs: Sierra Nevada II","interactions":[],"lastModifiedDate":"2026-02-19T16:14:27.361196","indexId":"70010447","displayToPublicDate":"1963-10-18T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Geomagnetic polarity epochs: Sierra Nevada II","docAbstract":"Ten new determinations on volcanic extrusions in the Sierra Nevada with potassium-argon ages of 3.1 million years or less indicate that the remanent magnetizations fall into two groups, a normal group in which the remanent magnetization is directed downward and to the north, and a reversed group magnetized up and to the south. Thermomagnetic experiments and mineralogic studies fail to provide an explanation of the opposing polarities in terms of mineralogic control, but rather suggest that the remanent magnetization reflects reversals of the main dipole field of the earth. All available radiometric ages are consistent with this field-reversal hypothesis and indicate that the present normal polarity epoch (N1) as well as the previous reversed epoch (R1) are 0.9 to 1.0 million years long, whereas the previous normal epoch (N2) was at least 25 percent longer.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.142.3590.382.b","issn":"00368075","usgsCitation":"Cox, A., Doell, R., and Dalrymple, G.B., 1963, Geomagnetic polarity epochs: Sierra Nevada II: Science, v. 142, no. 3590, p. 382-385, https://doi.org/10.1126/science.142.3590.382.b.","productDescription":"4 p.","startPage":"382","endPage":"385","costCenters":[],"links":[{"id":218726,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"California","otherGeospatial":"Sierra Nevada","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.5715952711419,\n              40.20991803398752\n            ],\n            [\n              -120.69651221728778,\n              37.971128897135316\n            ],\n            [\n              -119.45149706565401,\n              36.85808445584945\n            ],\n            [\n              -118.62149761871053,\n              35.54268894308095\n            ],\n            [\n              -117.72006781438974,\n              35.60080332324304\n            ],\n            [\n              -118.37604239661712,\n              37.3345088315523\n            ],\n            [\n              -120.06037076984778,\n              39.01118184089944\n            ],\n            [\n              -120.59713673430964,\n              40.34758079778908\n            ],\n            [\n              -121.5715952711419,\n              40.20991803398752\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"142","issue":"3590","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a275ee4b0c8380cd59800","contributors":{"authors":[{"text":"Cox, A.","contributorId":89266,"corporation":false,"usgs":true,"family":"Cox","given":"A.","email":"","affiliations":[],"preferred":false,"id":358947,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Doell, Richard R.","contributorId":66683,"corporation":false,"usgs":true,"family":"Doell","given":"Richard R.","affiliations":[],"preferred":false,"id":358946,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dalrymple, G. Brent","contributorId":55146,"corporation":false,"usgs":true,"family":"Dalrymple","given":"G.","email":"","middleInitial":"Brent","affiliations":[],"preferred":false,"id":358945,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}