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In an alternate procedure, 18 elements are precipitated quantitatively with complexing reagents 8-hydroxyquinoline, tannic acid, and thioanlide. This method is faster than the thioacetamide method, but at the sacrifice of some elements. A Fortran IV computer program for processing densitometric data is given in the section 'Computer Program.'","language":"English","publisher":"U.S. Govt. Print. 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In addition, with a current meter installed on a special bracket to allow measurements to 0.5 foot above streambed, data were obtained at two to four verticals in four gaging-station cross sections. \r\n\r\nThe mean velocity determined for the 66-minute period of record was 3.30 fps (feet per second). The graphic record of velocity was analyzed on a minute-by-minute basis. It was noted that the shape of the vertical velocity curves (plot of horizontal flow velocities measured in a vertical) changed from one minute to the next, but the change seemed to be random. Velocities obtained at different depths in the, profile fluctuated significantly, with the 1-minute velocities obtained at 0.05 depth (5 percent of total depths measured from the surface at indicated vertical) showing the smallest range--0.66 fps--and those at 0.55 depth the largest range--l.22 fps. \r\n\r\nThe standard deviation, expressed in feet per second, of the velocity at each point in the vertical tended to increase with depth--from 0.16 fps at 0.05 depth to a maximum of 0.24 fps at 0.75 depth. The standard deviation, expressed as a percentage of the mean velocity, ranged from about 4 percent near the surface to 11 percent at 0.95 depth. In spite of the fluctuation in mean velocity that occurred during the 66 minutes and observation period of 4 minutes yields a mean velocity that differs from the 66-minute mean by less than one-half of a percent. \r\n\r\nDetermining the mean velocity by averaging the 10-point observations of the 66minute run proved to be as accurate as by plotting the vertical velocity curvy (from the averaged 10 points) and then integrating the depth-velocity profile. In comparing the velocity obtained by integrating the depth-velocity profile with the 10-point mean velocity for other field data, collected beyond that obtained during the 66-minute run, the difference ranged from -1.3 to +1.7 percent and averaged -0.2 percent. Extension of the curve below the 0.95 depth by use of a power function proved to be fairly accurate (when compared with actual measurements within this reach made with the special current-meter bracket). However, the extension did not improve significantly the accuracy of the integrated-curve mean velocity. \r\n\r\nBoth the one- and two-point methods were found to agree with the 10-point velocity. In computing mean river velocity, values determined by the two-point method ranged from -1.4 to +1.6 percent when compared with the base integrated-curve mean river velocity. The one-point method yielded results that ranged from -1.9 to +4.4 percent and averaged 40.1 percent. \r\n\r\nIn determining river flow by use of the midsection and mean-section methods, the mean-section method uniformly yields lower flows for the same dart.. The range in difference is from -0.2 percent to -1.6 percent, with an average difference of -0.6 percent.","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.; [for sale by the Supt. of Docs.],","doi":"10.3133/wsp1869F","usgsCitation":"Savini, J., and Bodhaine, G., 1971, Analysis of current-meter data at Columbia River gaging stations, Washington and Oregon: U.S. Geological Survey Water Supply Paper 1869, iv, 59 p. :illus., map. ;24 cm., https://doi.org/10.3133/wsp1869F.","productDescription":"iv, 59 p. :illus., map. ;24 cm.","costCenters":[],"links":[{"id":138601,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1869f/report-thumb.jpg"},{"id":28960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1869f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db6805cc","contributors":{"authors":[{"text":"Savini, John","contributorId":67491,"corporation":false,"usgs":true,"family":"Savini","given":"John","email":"","affiliations":[],"preferred":false,"id":145546,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bodhaine, G. L.","contributorId":26671,"corporation":false,"usgs":true,"family":"Bodhaine","given":"G. L.","affiliations":[],"preferred":false,"id":145545,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":4693,"text":"twri02E1 - 1971 - Application of borehole geophysics to water-resources investigations","interactions":[],"lastModifiedDate":"2012-02-02T00:05:31","indexId":"twri02E1","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":336,"text":"Techniques of Water-Resources Investigations","code":"TWRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"02-E1","title":"Application of borehole geophysics to water-resources investigations","docAbstract":"This manual is intended to be a guide for hydrologists using borehole geophysics in ground-water studies. The emphasis is on the application and interpretation of geophysical well logs, and not on the operation of a logger. It describes in detail those logging techniques that have been utilized within the Water Resources Division of the U.S. Geological Survey, and those used in petroleum investigations that have potential application to hydrologic problems. Most of the logs described can be made by commercial logging service companies, and many can be made with small water-well loggers. The general principles of each technique and the rules of log interpretation are the same, regardless of differences in instrumentation. Geophysical well logs can be interpreted to determine the lithology, geometry, resistivity, formation factor, bulk density, porosity, permeability, moisture content, and specific yield of water-bearing rocks, and to define the source, movement, and chemical and physical characteristics of ground water. Numerous examples of logs are used to illustrate applications and interpretation in various ground-water environments. The interrelations between various types of logs are emphasized, and the following aspects are described for each of the important logging techniques: Principles and applications, instrumentation, calibration and standardization, radius of investigation, and extraneous effects.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/twri02E1","issn":"0565-596X","usgsCitation":"Keys, W., and MacCary, L., 1971, Application of borehole geophysics to water-resources investigations: U.S. Geological Survey Techniques of Water-Resources Investigations 02-E1, ix, 126 p. :ill. ;26 cm. Reprinted in 1973, 1981, 1983, 1986, 1990., https://doi.org/10.3133/twri02E1.","productDescription":"ix, 126 p. :ill. ;26 cm. Reprinted in 1973, 1981, 1983, 1986, 1990.","costCenters":[],"links":[{"id":139178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":253,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/twri/twri2-e1/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67aa48","contributors":{"authors":[{"text":"Keys, W.S.","contributorId":75126,"corporation":false,"usgs":true,"family":"Keys","given":"W.S.","email":"","affiliations":[],"preferred":false,"id":149631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":149630,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61889,"text":"gq924 - 1971 - Geologic map of the Mills Junction quadrangle, Tooele County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq924","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"924","title":"Geologic map of the Mills Junction quadrangle, Tooele County, Utah","language":"ENGLISH","doi":"10.3133/gq924","usgsCitation":"Tooker, E.W., and Roberts, R.J., 1971, Geologic map of the Mills Junction quadrangle, Tooele County, Utah: U.S. Geological Survey Geologic Quadrangle 924, 1 map., https://doi.org/10.3133/gq924.","productDescription":"1 map.","costCenters":[],"links":[{"id":103638,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2224.htm","linkFileType":{"id":5,"text":"html"},"description":"2224"},{"id":248178,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0924/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252921,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0924/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.36749999999999,40.6175 ], [ -112.36749999999999,40.75 ], [ -112.25,40.75 ], [ -112.25,40.6175 ], [ -112.36749999999999,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969b5","contributors":{"authors":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":266515,"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":266516,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":36009,"text":"b1318 - 1971 - Geochemistry and geology of deep drill holes at Iron Canyon, Lander County, Nevada","interactions":[],"lastModifiedDate":"2022-12-30T20:42:27.07783","indexId":"b1318","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"1318","title":"Geochemistry and geology of deep drill holes at Iron Canyon, Lander County, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1318","usgsCitation":"Theodore, T., Roberts, R.J., and Zablocki, C.J., 1971, Geochemistry and geology of deep drill holes at Iron Canyon, Lander County, Nevada: U.S. Geological Survey Bulletin 1318, Report: iv, 32 p.; 4 Plates: 27.00 x 36.00 inches, https://doi.org/10.3133/b1318.","productDescription":"Report: iv, 32 p.; 4 Plates: 27.00 x 36.00 inches","costCenters":[],"links":[{"id":411249,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_21421.htm","linkFileType":{"id":5,"text":"html"}},{"id":63956,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1318/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63955,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1318/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":163616,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1318/report-thumb.jpg"},{"id":63954,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1318/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63957,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/bul/1318/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":63958,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1318/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Iron Canyon","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -117.1170,\n 40.537\n ],\n [\n -117.1170,\n 40.557\n ],\n [\n -117.088,\n 40.557\n ],\n [\n -117.088,\n 40.537\n ],\n [\n -117.1170,\n 40.537\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6ab76f","contributors":{"authors":[{"text":"Theodore, Ted G.","contributorId":57840,"corporation":false,"usgs":true,"family":"Theodore","given":"Ted G.","affiliations":[],"preferred":false,"id":215610,"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":215611,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Zablocki, Charles J.","contributorId":48961,"corporation":false,"usgs":true,"family":"Zablocki","given":"Charles","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":215609,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":66207,"text":"i668 - 1971 - Geologic map of the Marshall Quadrangle, western Alaska","interactions":[],"lastModifiedDate":"2012-02-10T00:11:14","indexId":"i668","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"668","subseriesTitle":"NONE","title":"Geologic map of the Marshall Quadrangle, western Alaska","language":"ENGLISH","doi":"10.3133/i668","usgsCitation":"Hoare, J., and Condon, W.H., 1971, Geologic map of the Marshall Quadrangle, western Alaska: U.S. Geological Survey IMAP 668, 1 map., https://doi.org/10.3133/i668.","productDescription":"1 map.","costCenters":[],"links":[{"id":106904,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9445.htm","linkFileType":{"id":5,"text":"html"},"description":"9445"},{"id":188730,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -165,61 ], [ -165,62 ], [ -162,62 ], [ -162,61 ], [ -165,61 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696c54","contributors":{"authors":[{"text":"Hoare, J. M.","contributorId":52143,"corporation":false,"usgs":true,"family":"Hoare","given":"J. M.","affiliations":[],"preferred":false,"id":274170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Condon, W. H.","contributorId":28611,"corporation":false,"usgs":true,"family":"Condon","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":274169,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66618,"text":"i677 - 1971 - Bathymetry and geology— East cape of the island of Hawaii","interactions":[],"lastModifiedDate":"2021-11-17T22:20:33.201818","indexId":"i677","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"677","title":"Bathymetry and geology— East cape of the island of Hawaii","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i677","usgsCitation":"Moore, J., 1971, Bathymetry and geology— East cape of the island of Hawaii: U.S. Geological Survey IMAP 677, 1 Plate: 30.00 × 41.85 inches, https://doi.org/10.3133/i677.","productDescription":"1 Plate: 30.00 × 41.85 inches","costCenters":[],"links":[{"id":391832,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_9454.htm"},{"id":260867,"rank":900,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0677/plate-1.pdf"},{"id":189504,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"62500","country":"United States","state":"Hawaii","otherGeospatial":"Island of Hawaii","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -154.875,\n 19.397\n ],\n [\n -154.5,\n 19.397\n ],\n [\n -154.5,\n 19.739\n ],\n [\n -154.875,\n 19.739\n ],\n [\n -154.875,\n 19.397\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ee4b07f02db640201","contributors":{"authors":[{"text":"Moore, J.G.","contributorId":67496,"corporation":false,"usgs":true,"family":"Moore","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":274801,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61887,"text":"gq922 - 1971 - Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"922","title":"Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah","language":"ENGLISH","doi":"10.3133/gq922","usgsCitation":"Tooker, E.W., and Roberts, R.J., 1971, Geologic map of the Garfield quadrangle, Salt Lake and Tooele Counties, Utah: U.S. Geological Survey Geologic Quadrangle 922, 1 map., https://doi.org/10.3133/gq922.","productDescription":"1 map.","costCenters":[],"links":[{"id":103636,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2222.htm","linkFileType":{"id":5,"text":"html"},"description":"2222"},{"id":248176,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0922/report.pdf","size":"34","linkFileType":{"id":1,"text":"pdf"}},{"id":252919,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0922/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,40.6175 ], [ -112.25,40.75 ], [ -112.11749999999999,40.75 ], [ -112.11749999999999,40.6175 ], [ -112.25,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b02e4b07f02db698d5f","contributors":{"authors":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":266511,"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":266512,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":43073,"text":"ofr71334 - 1971 - Preliminary geologic map of the Tenabo area, Shoshone Range, Lander County, Nevada","interactions":[{"subject":{"id":43073,"text":"ofr71334 - 1971 - Preliminary geologic map of the Tenabo area, Shoshone Range, Lander County, Nevada","indexId":"ofr71334","publicationYear":"1971","noYear":false,"title":"Preliminary geologic map of the Tenabo area, Shoshone Range, Lander County, Nevada"},"predicate":"SUPERSEDED_BY","object":{"id":61260,"text":"mf647 - 1974 - Geologic map of the Gold Acres--Tenabo area Shoshone Range, Lander County, Nevada","indexId":"mf647","publicationYear":"1974","noYear":false,"title":"Geologic map of the Gold Acres--Tenabo area Shoshone Range, Lander County, Nevada"},"id":1}],"supersededBy":{"id":61260,"text":"mf647 - 1974 - Geologic map of the Gold Acres--Tenabo area Shoshone Range, Lander County, Nevada","indexId":"mf647","publicationYear":"1974","noYear":false,"title":"Geologic map of the Gold Acres--Tenabo area Shoshone Range, Lander County, Nevada"},"lastModifiedDate":"2022-04-15T17:42:26.902319","indexId":"ofr71334","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"71-334","title":"Preliminary geologic map of the Tenabo area, Shoshone Range, Lander County, Nevada","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr71334","usgsCitation":"Wrucke, C., and Armbrustmacher, T., 1971, Preliminary geologic map of the Tenabo area, Shoshone Range, Lander County, Nevada: U.S. Geological Survey Open-File Report 71-334, 1 Plate: 35.93 x 23.80 inches, https://doi.org/10.3133/ofr71334.","productDescription":"1 Plate: 35.93 x 23.80 inches","costCenters":[],"links":[{"id":398843,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0334/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":135450,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0334/report-thumb.jpg"}],"country":"United States","state":"Nevada","county":"Lander County","otherGeospatial":"Shoshone Range","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.78333333333333,40.21666666666667 ], [ -116.78333333333333,40.36666666666667 ], [ -116.66666666666667,40.36666666666667 ], [ -116.66666666666667,40.21666666666667 ], [ -116.78333333333333,40.21666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67ab0a","contributors":{"authors":[{"text":"Wrucke, C. T.","contributorId":8067,"corporation":false,"usgs":true,"family":"Wrucke","given":"C. T.","affiliations":[],"preferred":false,"id":227682,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Armbrustmacher, T.J.","contributorId":92642,"corporation":false,"usgs":true,"family":"Armbrustmacher","given":"T.J.","affiliations":[],"preferred":false,"id":227683,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61888,"text":"gq923 - 1971 - Geologic map of the Magna quadrangle, Salt Lake County, Utah","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"gq923","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"923","title":"Geologic map of the Magna quadrangle, Salt Lake County, Utah","language":"ENGLISH","doi":"10.3133/gq923","usgsCitation":"Tooker, E.W., and Roberts, R.J., 1971, Geologic map of the Magna quadrangle, Salt Lake County, Utah: U.S. Geological Survey Geologic Quadrangle 923, 1 map., https://doi.org/10.3133/gq923.","productDescription":"1 map.","costCenters":[],"links":[{"id":103637,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2223.htm","linkFileType":{"id":5,"text":"html"},"description":"2223"},{"id":248177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0923/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252920,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0923/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.11749999999999,40.6175 ], [ -112.11749999999999,40.75 ], [ -112,40.75 ], [ -112,40.6175 ], [ -112.11749999999999,40.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696ced","contributors":{"authors":[{"text":"Tooker, Edwin Wilson","contributorId":33295,"corporation":false,"usgs":true,"family":"Tooker","given":"Edwin","email":"","middleInitial":"Wilson","affiliations":[],"preferred":false,"id":266513,"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":266514,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":66848,"text":"i627 - 1971 - Geologic map of the Lansberg P region of the Moon Lunar Orbiter Site III P-9, Oceanus Procellarum including Apollo landing site 7 (Apollo 12)","interactions":[],"lastModifiedDate":"2023-04-26T14:00:03.373278","indexId":"i627","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"627","subseriesTitle":"MOON","title":"Geologic map of the Lansberg P region of the Moon Lunar Orbiter Site III P-9, Oceanus Procellarum including Apollo landing site 7 (Apollo 12)","docAbstract":"The Lansberg P region lies within a lowland area between Mare Cognitum and the main part of Oceanus Procellarum, about 135 km due south of the crater Reinhold. The Apollo 12 landing site is in the west-central part of the region and has been mapped in detail by Cannon (1969). Although the entire region is covered by cratered and rayed mare materials, the mare is almost entirely surrounded by the terrae and is probably relatively thin. Superposed on the mare are two rays from the crater Copernicus, many individual craters, and crater clusters.
","language":"English","doi":"10.3133/i627","usgsCitation":"Pohn, H., 1971, Geologic map of the Lansberg P region of the Moon Lunar Orbiter Site III P-9, Oceanus Procellarum including Apollo landing site 7 (Apollo 12): U.S. Geological Survey IMAP 627, 1 map, https://doi.org/10.3133/i627.","productDescription":"1 map","costCenters":[],"links":[{"id":188753,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":260870,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0627/plate-1.pdf"}],"scale":"100000","otherGeospatial":"Moon, Oceanus Procellarum","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696f29","contributors":{"authors":[{"text":"Pohn, H. A.","contributorId":6912,"corporation":false,"usgs":true,"family":"Pohn","given":"H. A.","affiliations":[],"preferred":false,"id":275178,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":6007,"text":"pp704 - 1971 - Ostracode biostratigraphy of the Yorktown Formation (upper Miocene and lower Pliocene) of Virginia and North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:05:54","indexId":"pp704","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"704","title":"Ostracode biostratigraphy of the Yorktown Formation (upper Miocene and lower Pliocene) of Virginia and North Carolina","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/pp704","usgsCitation":"Hazel, J.E., 1971, Ostracode biostratigraphy of the Yorktown Formation (upper Miocene and lower Pliocene) of Virginia and North Carolina: U.S. Geological Survey Professional Paper 704, 13 p., https://doi.org/10.3133/pp704.","productDescription":"13 p.","costCenters":[],"links":[{"id":121763,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0704/report-thumb.jpg"},{"id":32949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0704/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a4d1","contributors":{"authors":[{"text":"Hazel, Joseph E. Jr.","contributorId":15609,"corporation":false,"usgs":true,"family":"Hazel","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":true,"id":151955,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":15295,"text":"ofr71222 - 1971 - Selected fluvial monazite deposits in the southeastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr71222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"71-222","title":"Selected fluvial monazite deposits in the southeastern United States","docAbstract":"Farther southwest in Georgia, around Griffin and Zebullon, along streams tributary to the Flint River in the monazite belt the flood plains are generally small and discontinuous, and only about 1 percent of the sediment is gravel. The area between Griffin, Zebullon, and the Flint River is underlain by biotite schist and biotite gneiss into which biotite granite has been intruded. Only along one stream, Flat Creek, which drains monazite-bearing granite near Zetella, Ga., are the tenors in monazite even moderately high, but a combination of thick, clayey overburden and discontinuous flood plains make the stream unsuitable for placer mining. Elsewhere in the Flint River area the heavy-mineral concentrates contain less than 1 percent monazite. \r\n\r\nThe southwesternmost area in which reconnaissance of the monazite belt was conducted includes a groups of southwest-flowing tributaries to the Chattahoochee River north of Pine Mountain and near La Grange, Ga. A combination of three characteristics of the alluvium make the area unfavorable for mining: (1) the upper half of the sedimentary sequence is clay and silt, (2) there is scant gravel, and (3) much of the sand is fine grained. Monazite is associated with the Snelson Granite, schists, and gneisses north of the Towaliga fault, but even in this area the tenor of most riffle sediments is only 0.1 to 0.5 pound of monazite per cubic yard, and the average tenor of the alluvium is about 0.2 pound per cubic Yard. Rocks south of the Towaliga fault contain scant monazite. The monazite-bearing area in the drainage basin of the Chattahoochee River has no monazite placers.\r\n\r\nEvidence from the areas on the Flint and Chattahoochee Rivers shows that streams in western Georgia are a much poorer source of monazite than streams farther to the northeast in Georgia, South Carolina, and North Carolina. Also, the northeastern part of the belt in the drainage basins of the Yadkin and Dan Rivers is a poorer source for monazite than the area between the Savannah and Catawba Rivers, S.C.-N.C. \r\n\r\nMonazite-bearing crystalline rocks in the western belt contain about 0.06 pound of monazite per cubic yard. Residual soil derived from the crystalline rocks contains about 0.3 to 0.4 pound of monazite per cubic yard, and colluvial sediments formed by sheet-wash from saprolite, residual soil, and, rarely, old stream deposits, have an average of 3.1 pounds of monazite to the cubic yard. The data on the tenors of residual and colluvial deposits are far less comprehensive than those an the quantity of monazite in the crystalline rocks, but the tenors are probably of the correct order of magnitude. Neither the crystalline rocks nor the residual soils are ores of monazite. Because the colluvial deposits are thin and have patch distribution they could not be mined independently, but some colluvium could be stripped from the adjoining hills in conjunction with the mining of alluvial deposits in the valleys. \r\n\r\nIt is most unlikely that alluvial monazite placers have formed in the trunk streams leading southeastward out of the monazite belt. Churn drilling on the Broad and North Tyger Rivers, South Carolina, at the east edge of the belt has shown that the bulk of the alluvium is fine-grained sediment that contains 0.2 to 0.4 pound of monazite per cubic yard--tenors that represent no considerable enrichment over those in the crystalline rocks and residual soils. The probable persistence of predominantly fine-grained alluvium downstream to the Coastal Plain and the certain dilution of monazite-bearing concentrates by the inflow of monazite-free suites of heavy minerals between the belt and the fall line suggest that the trunk streams east of the belt are the least favorable sources for alluvial monazite in the Piedmont?","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr71222","usgsCitation":"Overstreet, W.C., White, A.M., Theobald, P., and Caldwell, D.W., 1971, Selected fluvial monazite deposits in the southeastern United States: U.S. Geological Survey Open-File Report 71-222, iv, 108 leaves :4 folded maps ;27 cm., https://doi.org/10.3133/ofr71222.","productDescription":"iv, 108 leaves :4 folded maps ;27 cm.","costCenters":[],"links":[{"id":146455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1971/0222/report-thumb.jpg"},{"id":44219,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44220,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0222/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44221,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0222/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44222,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1971/0222/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":44223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1971/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa31c","contributors":{"authors":[{"text":"Overstreet, William C.","contributorId":73586,"corporation":false,"usgs":true,"family":"Overstreet","given":"William","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":170908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, A. M.","contributorId":86778,"corporation":false,"usgs":true,"family":"White","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":170909,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Theobald, P. K.","contributorId":45293,"corporation":false,"usgs":true,"family":"Theobald","given":"P. K.","affiliations":[],"preferred":false,"id":170907,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Caldwell, D. W.","contributorId":27461,"corporation":false,"usgs":true,"family":"Caldwell","given":"D.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":170906,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":63392,"text":"gq879 - 1971 - Geologic maps of parts of the Naugatuck and Delbarton quadrangles, eastern Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:12:52","indexId":"gq879","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1971","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":"879","title":"Geologic maps of parts of the Naugatuck and Delbarton quadrangles, eastern Kentucky","language":"ENGLISH","doi":"10.3133/gq879","usgsCitation":"Alvord, D.C., 1971, Geologic maps of parts of the Naugatuck and Delbarton quadrangles, eastern Kentucky: U.S. Geological Survey Geologic Quadrangle 879, 1 map., https://doi.org/10.3133/gq879.","productDescription":"1 map.","costCenters":[],"links":[{"id":103595,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2181.htm","linkFileType":{"id":5,"text":"html"},"description":"2181"},{"id":249487,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0879/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252969,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0879/report-thumb.jpg"}],"scale":"24000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6885dc","contributors":{"authors":[{"text":"Alvord, Donald Clayton","contributorId":49356,"corporation":false,"usgs":true,"family":"Alvord","given":"Donald","email":"","middleInitial":"Clayton","affiliations":[],"preferred":false,"id":268773,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}