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The ores generally are cut by late veinlets which are of the same mineralogy as the groundmass ore, or which consist of fluorite, white mica, and euclase. The ores are fine grained, and many of the individual mineral grains, except fluorite, are less than 1 mm in size. The beryllium content of bulk samples of ore ranges from 0.11 to 0.54 percent (0.31 to 1.50 percent BeO). 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1963 - Geology of the Kirksey quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:35","indexId":"gq246","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":"246","title":"Geology of the Kirksey quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/gq246","usgsCitation":"Wilshire, H.G., 1963, Geology of the Kirksey quadrangle, Kentucky: U.S. Geological Survey Geologic Quadrangle 246, 1 map :col. ;on sheet 76 x 85 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/gq246.","productDescription":"1 map :col. ;on sheet 76 x 85 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":102251,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_700.htm","linkFileType":{"id":5,"text":"html"},"description":"700"},{"id":248307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0246/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253201,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0246/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acee4b07f02db67f79b","contributors":{"authors":[{"text":"Wilshire, Howard Gordon","contributorId":102479,"corporation":false,"usgs":true,"family":"Wilshire","given":"Howard","email":"","middleInitial":"Gordon","affiliations":[],"preferred":false,"id":266926,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35549,"text":"b1158B - 1963 - Bedrock geology of the Crompton quadrangle, Rhode Island","interactions":[],"lastModifiedDate":"2012-02-02T00:09:36","indexId":"b1158B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1158","chapter":"B","title":"Bedrock geology of the Crompton quadrangle, Rhode Island","language":"ENGLISH","publisher":"U. S. Govt. Print. Off.,","doi":"10.3133/b1158B","usgsCitation":"Quinn, A.W., 1963, Bedrock geology of the Crompton quadrangle, Rhode Island: U.S. Geological Survey Bulletin 1158, p. B1-B17 :map (fold. in pocket) ;24 cm., https://doi.org/10.3133/b1158B.","productDescription":"p. 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1963 - Aeromagnetic map of the Dragoon quadrangle, Cochise County, Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:55","indexId":"gp412","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":"412","title":"Aeromagnetic map of the Dragoon quadrangle, Cochise County, Arizona","language":"ENGLISH","doi":"10.3133/gp412","usgsCitation":"Dempsey, W., and Fackler, W., 1963, Aeromagnetic map of the Dragoon quadrangle, Cochise County, Arizona: U.S. Geological Survey Geophysical Investigations Map 412, 1 map., https://doi.org/10.3133/gp412.","productDescription":"1 map.","costCenters":[],"links":[{"id":186842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260652,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/gp/0412/plate-1.pdf"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -110.25,32 ], [ -110.25,32.25 ], [ -110,32.25 ], [ -110,32 ], [ -110.25,32 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a4e","contributors":{"authors":[{"text":"Dempsey, W.J.","contributorId":13988,"corporation":false,"usgs":true,"family":"Dempsey","given":"W.J.","affiliations":[],"preferred":false,"id":270794,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fackler, W.D.","contributorId":66787,"corporation":false,"usgs":true,"family":"Fackler","given":"W.D.","email":"","affiliations":[],"preferred":false,"id":270795,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":42239,"text":"ofr6383 - 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr63135","usgsCitation":"Weigle, J., 1963, Ground-water favorability map of the Nashua-Merrimack area, New Hampshire: U.S. Geological Survey Open-File Report 63-135, 1 Plate: 22.30 x 28.51 inches, https://doi.org/10.3133/ofr63135.","productDescription":"1 Plate: 22.30 x 28.51 inches","costCenters":[],"links":[{"id":135664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1963/0135/report-thumb.jpg"},{"id":372078,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1963/0135/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"4666","country":"United States","state":"New Hampshire","otherGeospatial":"Nashua-Merrimack area","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -71.73797607421874,\n 42.68243539838623\n ],\n [\n -71.25457763671874,\n 42.68243539838623\n ],\n [\n -71.25457763671874,\n 42.92224052343343\n ],\n [\n -71.73797607421874,\n 42.92224052343343\n ],\n [\n -71.73797607421874,\n 42.68243539838623\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66ce03","contributors":{"authors":[{"text":"Weigle, J.J.","contributorId":15172,"corporation":false,"usgs":true,"family":"Weigle","given":"J.J.","email":"","affiliations":[],"preferred":false,"id":227718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6219,"text":"pp422B - 1963 - Hydraulic geometry of a small tidal estuary","interactions":[],"lastModifiedDate":"2017-03-24T16:16:21","indexId":"pp422B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1963","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":"B","title":"Hydraulic geometry of a small tidal estuary","docAbstract":"A tidal channel in a marsh bordering the Potomac River near Alexandria, Va., was mapped, and current-meter measurements of discharge were made at various locations and at various stages in the tidal cycle. These measurements allowed analysis of the change of width, depth, and velocity with discharge at various cross sections and along the length of the channel.
There is also presented a theoretical development of some, of these same relations based on hydraulic principles and on the assumption of a uniform distribution of energy and a minimum rate of work in the system as a whole.
The change of width, depth, and velocity with discharge downstream developed from the field data checked closely with the theoretically derived values.
The estuarine channel differs from a terrestrial one in that discharge at any section in an estuary varies depending on how the flow shaped the entire length of the channel between the point in question and the main body of tidal water. The result is that a tidal channel changes more rapidly in width and less rapidly in depth as discharge changes downstream than does a terrestrial channel.
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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr634","usgsCitation":"Armstrong, F.C., 1963, The Bannock thrust zone, southeastern Idaho: U.S. Geological Survey Open-File Report 63-4, Report: vii, 88 p.; 7 Figures: 17.76 x 23.83 inches or smaller, https://doi.org/10.3133/ofr634.","productDescription":"Report: vii, 88 p.; 7 Figures: 17.76 x 23.83 inches or smaller","costCenters":[],"links":[{"id":490231,"rank":7,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0004/figure-6.pdf","text":"Figure 6","linkFileType":{"id":1,"text":"pdf"}},{"id":490230,"rank":6,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0004/figure-5.pdf","text":"Figure 5","linkFileType":{"id":1,"text":"pdf"}},{"id":490229,"rank":5,"type":{"id":29,"text":"Figure"},"url":"https://pubs.usgs.gov/of/1963/0004/figure-4.pdf","text":"Figure 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