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,{"id":2600,"text":"wsp1539V - 1963 - Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","interactions":[],"lastModifiedDate":"2023-11-01T21:34:49.498797","indexId":"wsp1539V","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1539","chapter":"V","title":"Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1539V","usgsCitation":"Robinove, C.J., Berry, D.W., and Connor, J.G., 1963, Availability of ground water in the Bear River valley, Wyoming, with a section on the chemical quality of the water: U.S. Geological Survey Water Supply Paper 1539, Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches, https://doi.org/10.3133/wsp1539V.","productDescription":"Report: iv, 44 p.; 2 Plates: 25.00 x 42.75 inches and 27.00 x 11.88 inches","costCenters":[],"links":[{"id":422319,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24743.htm","linkFileType":{"id":5,"text":"html"}},{"id":28882,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1539v/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28881,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":28880,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1539v/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138893,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1539v/report-thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"Bear River Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -110.8033,\n              42.221\n            ],\n            [\n              -111.048,\n              42.221\n            ],\n            [\n              -111.048,\n              41\n            ],\n            [\n              -110.8033,\n              41\n            ],\n            [\n              -110.8033,\n              42.221\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db66035d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":145473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berry, Delmar W.","contributorId":25107,"corporation":false,"usgs":true,"family":"Berry","given":"Delmar","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145472,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Connor, John G.","contributorId":34489,"corporation":false,"usgs":true,"family":"Connor","given":"John","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":887319,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70009999,"text":"70009999 - 1963 - Spectrophotometric determination of micro quantities of zinc in rocks","interactions":[],"lastModifiedDate":"2020-11-19T17:57:54.921349","indexId":"70009999","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1759,"text":"Geochimica et Cosmochimica Acta","active":true,"publicationSubtype":{"id":10}},"title":"Spectrophotometric determination of micro quantities of zinc in rocks","docAbstract":"<p>A chemical method is presented for the determination of microgram amounts of zinc in rocks. Zinc is absorbed on anion-exchange resin from 1.2 M hydrochloric acid and eluted with 0.01 M hydrochloric acid. A diethyldithiocarbamate separation removes traces of interfering elements from the eluate. The zinc-diethyldithiocarbamate complex is extracted into chloroform at pH 8.5 and reextracted from other elements in the chloroform solution with 0.16 M hydrochloric acid and finally determined spectrophotometrically as the zincon complex at 621 mμ.</p><p>The coefficient of variation of the method determined from replicate determinations of zinc on 75 selected samples of basalt, ranging in zinc content from 0.004 to 0.018 per cent, was found to be 6.3 per cent and essentially constant in the range of zinc content studied. This method of analysis has been used extensively for a study of zinc in basalts reported by Rader, Swadley, Huffman and Lipp (companion paper, 1963).</p>","language":"English","publisher":"Elsevier","doi":"10.1016/0016-7037(63)90023-1","usgsCitation":"Huffman, C., Lipp, H.H., and Rader, L., 1963, Spectrophotometric determination of micro quantities of zinc in rocks: Geochimica et Cosmochimica Acta, v. 27, no. 3, p. 209-215, https://doi.org/10.1016/0016-7037(63)90023-1.","productDescription":"7 p.","startPage":"209","endPage":"215","numberOfPages":"7","costCenters":[],"links":[{"id":218769,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"27","issue":"3","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505b95a8e4b08c986b31b03d","contributors":{"authors":[{"text":"Huffman, C. Jr.","contributorId":20064,"corporation":false,"usgs":true,"family":"Huffman","given":"C.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":357624,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lipp, H. H.","contributorId":47906,"corporation":false,"usgs":true,"family":"Lipp","given":"H.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":357625,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rader, L. F.","contributorId":9730,"corporation":false,"usgs":true,"family":"Rader","given":"L. F.","affiliations":[],"preferred":false,"id":357623,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70176112,"text":"70176112 - 1963 - Surface water records of Texas, 1962","interactions":[],"lastModifiedDate":"2017-06-07T17:30:06","indexId":"70176112","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":5196,"text":"Water Data Report","active":true,"publicationSubtype":{"id":6}},"title":"Surface water records of Texas, 1962","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/70176112","usgsCitation":"U.S. Geological Survey, 1963, Surface water records of Texas, 1962: Water Data Report, 414 p., https://doi.org/10.3133/70176112.","productDescription":"414 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science 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,{"id":81380,"text":"81380 - 1963 - Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81380","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"564","title":"Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"705/FH","usgsCitation":"Hoffman, G.L., 1963, Parasites of freshwater fish, I Fungi, Fungi (Saprolegnia and relatives) of fish and fish eggs: Fishery Leaflet 564, 6 p.","productDescription":"6 p.","startPage":"0","endPage":"6","numberOfPages":"6","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198183,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db689261","contributors":{"authors":[{"text":"Hoffman, G. L.","contributorId":70713,"corporation":false,"usgs":true,"family":"Hoffman","given":"G.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":295310,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81363,"text":"81363 - 1963 - Surface currents of Lake Michigan, 1931 and 1932","interactions":[],"lastModifiedDate":"2012-02-02T00:15:00","indexId":"81363","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":84,"text":"Special Scientific Report - Fisheries","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"413","title":"Surface currents of Lake Michigan, 1931 and 1932","docAbstract":"Seven hundred fourty-five bottles containing post cards for recording of information were released at stations in Lake Michigan; 283 were released June 17 to August 17, 1931, south of a line from Frankfort, Michigan, to Algoma, Wisconsin, and 462 during May 9 to August 25, 1932, both south and north of that line.  One hundred eighty-six bottles or 65.7 percent of those released in 1931, 331 bottles or 71.6 percent of 1932 releases, and 517 bottles or 69.4 percent of releases in the 2 years were recovered.  Recoveries of bottles from both years indicated that the surface currents were somewhat variable, but their general direction was from west to east and predominately northeast in 1931 and northeast and southeast in 1932.","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"Out-of-print","usgsCitation":"Van Oosten, J., 1963, Surface currents of Lake Michigan, 1931 and 1932: Special Scientific Report - Fisheries 413, 51 p.","productDescription":"51 p.","startPage":"0","endPage":"51","numberOfPages":"51","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":101760,"rank":9999,"type":{"id":10,"text":"Digital Object Identifier"},"url":"https://hdl.handle.net/2027/mdp.39015045826347?urlappend=%3Bseq=183"},{"id":199160,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697935","contributors":{"authors":[{"text":"Van Oosten, John","contributorId":23479,"corporation":false,"usgs":true,"family":"Van Oosten","given":"John","email":"","affiliations":[],"preferred":false,"id":295292,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":81383,"text":"81383 - 1963 - Sacramento River chinook disease (SRCD)","interactions":[],"lastModifiedDate":"2012-02-02T00:15:02","indexId":"81383","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":29,"text":"Fishery Leaflet","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"562","title":"Sacramento River chinook disease (SRCD)","language":"English","publisher":"U.S. Fish and Wildlife Service","collaboration":"759/FH","usgsCitation":"Parisot, T., 1963, Sacramento River chinook disease (SRCD): Fishery Leaflet 562, 2 p.","productDescription":"2 p.","startPage":"0","endPage":"2","numberOfPages":"2","costCenters":[{"id":365,"text":"Leetown Science Center","active":true,"usgs":true}],"links":[{"id":198186,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe056","contributors":{"authors":[{"text":"Parisot, T. J.","contributorId":43014,"corporation":false,"usgs":true,"family":"Parisot","given":"T. J.","affiliations":[],"preferred":false,"id":295313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32753,"text":"pp403C - 1963 - Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam","interactions":[],"lastModifiedDate":"2025-04-15T16:24:21.582891","indexId":"pp403C","displayToPublicDate":"1963-01-01T00:00:00","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":"403","chapter":"C","title":"Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geology and hydrology of Guam, Mariana Islands (Professional Paper 403)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp403C","usgsCitation":"Stark, J.T., and Tracey, J.I., 1963, Petrology of the volcanic rocks of Guam, with a section on trace elements in the volcanic rocks of Guam: U.S. Geological Survey Professional Paper 403, iv, 32 p., https://doi.org/10.3133/pp403C.","productDescription":"iv, 32 p.","costCenters":[],"links":[{"id":415898,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_44668.htm","linkFileType":{"id":5,"text":"html"}},{"id":119255,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0403c/report-thumb.jpg"},{"id":60687,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0403c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"otherGeospatial":"Guam","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              144.6075439453125,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.213208268446683\n            ],\n            [\n              145.0689697265625,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.7153719325982\n            ],\n            [\n              144.6075439453125,\n              13.213208268446683\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adfe4b07f02db687c6d","contributors":{"authors":[{"text":"Stark, J. T.","contributorId":62650,"corporation":false,"usgs":true,"family":"Stark","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":209101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tracey, J. I. Jr.","contributorId":17205,"corporation":false,"usgs":true,"family":"Tracey","given":"J.","suffix":"Jr.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":209100,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70010840,"text":"70010840 - 1963 - Unmineralized fossil bacteria","interactions":[],"lastModifiedDate":"2020-11-19T19:07:51.975759","indexId":"70010840","displayToPublicDate":"1963-01-01T00:00:00","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":"Unmineralized fossil bacteria","docAbstract":"<p><span>Unmineralized bacterial cells, mostly Micrococcus sp., but including also Streptococcus sp. and Actinomyces sp., were found in enormous numbers in lake beds of the Newark Canyon Formation of Early Cretaceous age, Eureka County, Nevada. The micrococci are black, and have an average diameter about 0.5 µ. Similar black micrococci (0.4 to 0.7 µ) were found in profusion in the bottom mud of Green Lake, New York. About 80 percent of this mud consists of minute idiomorphic calcite crystals and about 20 percent of these contain enormous numbers of the black micrococci. It is suggested that the Early Cretaceous bacterial cells owe their preservation to occlusion in calcite crystals that grew in a black, bacterial mud in a meromictic lake in which part of the Newark Canyon Formation accumulated.</span></p>","language":"English","publisher":"AAAS","doi":"10.1126/science.141.3584.919","usgsCitation":"Bradley, W.H., 1963, Unmineralized fossil bacteria: Science, v. 141, no. 3584, p. 919-921, https://doi.org/10.1126/science.141.3584.919.","productDescription":"3 p.","startPage":"919","endPage":"921","numberOfPages":"3","costCenters":[],"links":[{"id":219011,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"141","issue":"3584","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505bbcd7e4b08c986b328e32","contributors":{"authors":[{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359766,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010783,"text":"70010783 - 1963 - Heat capacity from 12 to 305°K and entropy of talc and tremolite","interactions":[],"lastModifiedDate":"2020-11-19T18:57:32.705083","indexId":"70010783","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2423,"text":"Journal of Physical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Heat capacity from 12 to 305°K and entropy of talc and tremolite","docAbstract":"<p>The heat capacities of talc, Mg<sub>3</sub>Si<sub>4</sub>O<sub>10</sub>(OH)<sub>2</sub>, and tremolite, Ca<sub>2</sub>Mg<sub>6</sub>Si<sub>8</sub>O<sub>22</sub>(OH)<sub>2</sub>, have been measured between 12 and 305°K. Smoothed values of heat capacity, entropy, enthalpy, and free energy are tabulated. At 298.15° K. the values of the thermodynamic functions are: talc, C<sub>p</sub>°= 76.89 <span>±</span>&nbsp;0.23 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, S° = 62.33<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.19 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, H° - H<sub>0</sub>° = 11,206&nbsp;<span>±</span>&nbsp;34 cal. mole<sup>-1</sup>; tremolite, Cp° = 156.7<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.6 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, S° = 131.2<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>0.5 cal. deg.<sup>-1</sup> mole<sup>-1</sup>, H° - H<sub>0</sub>° = 23,335<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>90 cal. mole<sup>-1</sup>. From the equilibrium data of Bowen and Tuttle and the entropy of talc, the heat of formation of talc from MgO, SiO<sub>2</sub>, and H<sub>2</sub>O (liq.) is calculated to be <span>Δ</span>H°f<sub>298</sub> = -43.6<span class=\"nowrap\"><span>&nbsp;</span></span><span>±</span><span>&nbsp;</span>1 kcal.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/j100805a003","usgsCitation":"Robie, R.A., and Stout, J.W., 1963, Heat capacity from 12 to 305°K and entropy of talc and tremolite: Journal of Physical Chemistry, v. 67, no. 11, p. 2252-2256, https://doi.org/10.1021/j100805a003.","productDescription":"5 p.","startPage":"2252","endPage":"2256","numberOfPages":"5","costCenters":[],"links":[{"id":219712,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"67","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a2ff3e4b0c8380cd5d241","contributors":{"authors":[{"text":"Robie, R. A.","contributorId":71237,"corporation":false,"usgs":true,"family":"Robie","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":359638,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stout, J. W.","contributorId":53943,"corporation":false,"usgs":true,"family":"Stout","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":359637,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1000140,"text":"1000140 - 1963 - Age and growth of the whitefish in Lake Superior","interactions":[],"lastModifiedDate":"2013-02-04T11:54:57","indexId":"1000140","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1663,"text":"Fishery Bulletin","printIssn":"0090-0656","active":true,"publicationSubtype":{"id":10}},"title":"Age and growth of the whitefish in Lake Superior","docAbstract":"The average annual commercial production of whitefish in the U.S. waters of Lake Superior dropped from 2,194,000 pounds in 1879-1908 to 504,000 pounds in 1911-59.  The modern production, though far below the earlier, has accounted for more than 10 percent of the total value of the fishery in all but one of the last 20 years. Data are given on growth rate, age and year-class composition, size distribution, and length-weight relation of 1,800 fish collected in 1957-59 at Bayfield, Wis., and Marquette, Whitefish Point, and Dollar Settlement, Mich.  Studies of the body-scale relation, sex ratio, and age and size at maturity were limited to fish collected at Bayfield. The age composition and mean age varied widely by port and year of capture. Oldest fish were those of the 1957 Bayfield samples which were dominated by age group VII and averaged 5.5 years old. The youngest were from Whitefish Point in 1959; age-group III was dominant, and the mean age was 3.2 years. The evidence on the strength of year classes was not clear-cut, but it was obvious that fluctuations in stocks of different areas were largely independent. The percentage of legal-size fish (17 inches or longer) in age groups ranged widely; only 8.6 percent of the V group were legal in the 1957 Bayfield collections, whereas 100 percent of fish of the same age were legal in the 1957-59 collections from Whitefish Point. The weight of whitefish in the combined samples increased as the 3.2408 power of the length. The growth rate from the fastest to the slowest growing stocks ranked as follows: Whitefish Point; Dollar Settlement and Marquette (fish from the two ports reversed ranks after 3 years); Bayfield. The major differences in growth in length among the various stocks occurred during the first years of life. Beyond the fifth year the annual increments were nearly the same in all stocks. The whitefish from Whitefish Point, Dollar Settlement, and Marquette are among the fastest growing in the Great Lakes. The differences among the Lake Superior stocks in age and year-class composition, and in growth rate offer convincing evidence that populations of different areas are entirely independent. The sexes were almost equally represented (51.5 percent males) in the combined Bayfield samples, but males were scarce in age groups older than VIII. Whitefish from Bayfield shorter than 14.5 inches were immature and those larger than 17.4 inches were mature. The youngest mature fish belonged to age-group V,and all older than the VII group were mature.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Fishery Bulletin","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Dryer, W.R., 1963, Age and growth of the whitefish in Lake Superior: Fishery Bulletin, v. 63, no. 1, p. 77-95.","productDescription":"19 p.","startPage":"77","endPage":"95","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128720,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":266925,"type":{"id":11,"text":"Document"},"url":"https://fishbull.noaa.gov/63-1/dryer.pdf"}],"volume":"63","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db6896d5","contributors":{"authors":[{"text":"Dryer, William R.","contributorId":71921,"corporation":false,"usgs":true,"family":"Dryer","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":308130,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1000251,"text":"1000251 - 1963 - Some phases of the life history of the trout-perch","interactions":[],"lastModifiedDate":"2023-12-19T14:14:40.560809","indexId":"1000251","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1465,"text":"Ecology","active":true,"publicationSubtype":{"id":10}},"title":"Some phases of the life history of the trout-perch","docAbstract":"The trout-perch, Percopsis omiscomaycus (Walbaum), is one of the more abundant forage fishes in the larger lakes of midwestern United States and central Canada where walleye, Stizostedion v. vitreum (Mitchill), yellow perch, Perca flavescens (Mitchill), and coregonids predominate.  It has been suggested that it may have considerable effect on perch and walleye populations of these lakes.  The present study describes growth, food habits, population structure, year-class strengths, and reproductive capacity of the trout-perch in relation to its population dynamics in lower Red Lake, Minnesota.","language":"English","publisher":"Ecological Society of America","doi":"10.2307/1933183","usgsCitation":"Magnuson, J.L., and Smith, L., 1963, Some phases of the life history of the trout-perch: Ecology, v. 44, no. 1, p. 83-95, https://doi.org/10.2307/1933183.","productDescription":"13 p.","startPage":"83","endPage":"95","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":128952,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"44","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e8e4b07f02db5e8fbe","contributors":{"authors":[{"text":"Magnuson, John L.","contributorId":80608,"corporation":false,"usgs":true,"family":"Magnuson","given":"John","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":308294,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, Lloyd L.","contributorId":34859,"corporation":false,"usgs":true,"family":"Smith","given":"Lloyd L.","affiliations":[],"preferred":false,"id":308293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1017033,"text":"1017033 - 1963 - A study of the food habits of some Lake Erie fish","interactions":[],"lastModifiedDate":"2012-02-02T00:04:36","indexId":"1017033","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1133,"text":"Bulletin of the Ohio Biological Survey","active":true,"publicationSubtype":{"id":10}},"title":"A study of the food habits of some Lake Erie fish","docAbstract":"A study of the food habits by means of stomach analyses of eight species of Lake Erie fishes was begun June 16, 1958.  The species studied were smelt, yellow perch, troutperch, spottail shiner, sheepshead, yellow walleye (hereafter termed walleye), gizzard shad, and alewife.  In a similar manner, stomach analyses were made of the white bass and channel catfish.  Both projects were parts of a cooperative study of the life histories of Lake Erie fish.\rA total of 14,118 fish stomachs were examined; the analyses of their contents are reported here.","largerWorkType":{"id":2,"text":"Article"},"largerWorkTitle":"Bulletin of the Ohio Biological Survey","largerWorkSubtype":{"id":10,"text":"Journal Article"},"language":"English","collaboration":"Out-of-print","usgsCitation":"Price, J.W., 1963, A study of the food habits of some Lake Erie fish: Bulletin of the Ohio Biological Survey, v. 2, no. 1.","productDescription":"89 p.","startPage":"89","numberOfPages":"89","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":133001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"2","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a6131","contributors":{"authors":[{"text":"Price, John W.","contributorId":10006,"corporation":false,"usgs":true,"family":"Price","given":"John","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":324550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4091,"text":"cir478 - 1963 - Floods in Wyoming, magnitude and frequency","interactions":[],"lastModifiedDate":"2023-04-27T19:49:17.622715","indexId":"cir478","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"478","title":"Floods in Wyoming, magnitude and frequency","docAbstract":"<p>This report contains the results of four separate flood-frequency analyses designated A, B, C, and D. Analysis A is for the portion of Wyoming east of the Continental Divide. Analysis B applies to the portion of Wyoming in Part 9, as designated in streamflow reports entitled \"Surface Water Supply of the United Stated\" published by the U.S. Geological Survey, and was extracted fro.m an unpublished study by W. P. Somers in 1959. Analysis C applies to Part 10 and was extracted from Circutar 457 (Berwick, 1962). Analysis D applies to Part 13 and was extracted from a report by C. A. Thomas, H. C. Broom, and J. E. Cummans (1963).</p><p>Methods described in this report can be used to estimate the magnitude of a flood of any selected recurrence interval between 1.1 and 50 years for any unregulated stream in Wyoming, gaged or ungaged, within the scope of the data. Flood-frequency relations are not defined for a large part of the North Platte River basin in south-central Wyoming because of insufficient data. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir478","collaboration":"Prepared in cooperation with Wyoming State Highway Department","usgsCitation":"Carter, J.R., and Green, A.R., 1963, Floods in Wyoming, magnitude and frequency: U.S. Geological Survey Circular 478, Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches, https://doi.org/10.3133/cir478.","productDescription":"Report: iv, 27 p.; 2 Plates: 9.36 x 12.59 and 9.18 x 12.67 inches","numberOfPages":"32","costCenters":[],"links":[{"id":416456,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_23527.htm","linkFileType":{"id":5,"text":"html"}},{"id":31192,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/0478/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":271068,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-1.pdf"},{"id":271069,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/0478/plate-2.pdf"},{"id":124473,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/0478/report-thumb.jpg"}],"country":"United States","state":"Wyoming","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -111.0569,40.9947 ], [ -111.0569,45.0059 ], [ -104.0522,45.0059 ], [ -104.0522,40.9947 ], [ -111.0569,40.9947 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699af5","contributors":{"authors":[{"text":"Carter, J. R.","contributorId":23128,"corporation":false,"usgs":true,"family":"Carter","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":148173,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Green, A. Rice","contributorId":31731,"corporation":false,"usgs":true,"family":"Green","given":"A.","email":"","middleInitial":"Rice","affiliations":[],"preferred":false,"id":148174,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185692,"text":"70185692 - 1963 - Association and determinacy in geomorphology","interactions":[],"lastModifiedDate":"2017-03-27T16:04:40","indexId":"70185692","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":5,"text":"Book chapter"},"publicationSubtype":{"id":24,"text":"Book Chapter"},"title":"Association and determinacy in geomorphology","docAbstract":"<p>You find a rock. It looks like an ordinary piece of flint, broken and rough. On a part of it is a patina whose soft grey color contrasts with the shiny brownish surfaces of conchoidal fracture. You could have found this rock in nearly any kind of an environment almost anyplace in the world. There is nothing distinctive about it.</p><p>You hand this same piece of rock to a colleague and ask what he can make of it. He considers it soberly before he says, “You know, that could be an artifact.” There springs to mind then a picture of a primitive man, squatting barefoot before a fire warming his hands. The firelight casts his shadow against the cliff below which he crouches. </p><p>The difference between the reaction before and after the passing thought that this might indeed be the tool of ancient man is the difference between mild disinterest and a kaleidoscope of mental pictures. This difference reflects differences in the associations of thoughts. </p><p>The present essay is concerned with how associations are used in geologic reasoning, and then with certain philosophic considerations which seem to be influencing the methodology and direction of geomorphology. </p>","largerWorkType":{"id":4,"text":"Book"},"largerWorkTitle":"The fabric of geology","largerWorkSubtype":{"id":15,"text":"Monograph"},"language":"English","publisher":"Addison-Wesley Publishing Company, inc","usgsCitation":"Leopold, L.B., and Langbein, W.B., 1963, Association and determinacy in geomorphology, chap. <i>of</i> The fabric of geology, p. 184-192.","productDescription":"9 p.","startPage":"184","endPage":"192","costCenters":[],"links":[{"id":338419,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda887","contributors":{"editors":[{"text":"Albritton, Claude C. Jr.","contributorId":87129,"corporation":false,"usgs":true,"family":"Albritton","given":"Claude","suffix":"Jr.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":686416,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686414,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":686415,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185608,"text":"70185608 - 1963 - Government responsibility for land and water: Guardian or developer? ","interactions":[],"lastModifiedDate":"2017-03-24T14:05:55","indexId":"70185608","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Government responsibility for land and water: Guardian or developer? ","docAbstract":"<p>Ideas and concepts become obsolete just as do specific techniques. Obsolescence is the inevitable companion of progress; in fact, it is a sign of progress, provided that the obsolescence is recognized. </p>","conferenceTitle":"Land and water use with special reference to the mountain and plains region: A Symposium of the American Association for the Advancement of Science","language":"English","publisher":"American Association for the Advancement of Science","publisherLocation":"Washington, D.C.","usgsCitation":"Leopold, L.B., and Nace, R.L., 1963, Government responsibility for land and water: Guardian or developer? , Land and water use with special reference to the mountain and plains region: A Symposium of the American Association for the Advancement of Science, p. 349-357.","productDescription":"9 p.","startPage":"349","endPage":"357","costCenters":[],"links":[{"id":338308,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63044e4b05ec79913113b","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686104,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nace, Raymond L.","contributorId":93460,"corporation":false,"usgs":true,"family":"Nace","given":"Raymond","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":686105,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70185607,"text":"70185607 - 1963 - Some climatic indicators in the period A.D. 1200-1400 in New Mexico","interactions":[],"lastModifiedDate":"2017-03-24T13:26:28","indexId":"70185607","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Some climatic indicators in the period A.D. 1200-1400 in New Mexico","docAbstract":"<p>Three centuries before Columbus landed in America, the alluvial valleys of the south-western United States teemed with activity. The indigenous peoples had been building for 300 years a culture centred around community life based on flood-water farming and on hunting. A large number of pueblos had developed on sites earlier occupied by pit-house people. Community organization had brought advances in the ceramic and decorative arts, and changes in these artistic activities were sufficiently rapid that accurate chronologies have become available through the work of archaeologists during the twentieth century. </p><p>These chronologies were at first unrelated to absolute dates, but the excavations of the 1920s at Chaco Canyon (New Mexico) provided the materials through which absolute dates could be established. This was accomplished by matching the changes in tree-ring width backward in time from living trees through successively older samples. Trees overlapping in age provided, by unique successions of distinctive tree-ring widths, a calendar by which individual logs could be dated. Beams found in the excavations at Chaco Canyon gave the first material by which the cultural developments culminating about A.D. 1300 could be dated.</p><p>As a result of the time sequence provided by the tree-ring calendar, the dates within which different pottery types were developed could be accurately established. The dates of pottery types have been checked at a sufficiently large number of sites throughout the south-western United States that absolute dating of a large number of distinctive patterns can be considered unassailable. </p><p>The sequence of tree-ring widths gives some climatic indications of great interest both to archaeologists and to climatologists. A relatively large number of logs spanning the period from A.D. 1200 to 1300 and, in particular, the years between 1276 and 1299, indicate that this period was generally characterized by smaller&nbsp;tree-ring widths than in the centuries immediately before and after. As a first approximation, the hundred years of narrow tree-ring widths were interpreted as a time of relative aridity, and have been referred to as the “Pueblo Drought”.&nbsp;</p><p>More recent studies of tree-ring widths using sophisticated statistical techniques have thrown some doubts on any direct correlation of tree-ring widths with rainfall. Such doubts have been put forward before by Glock (1955) whose studies have been aimed at separating the various effects of seasonal occurrence of precipitation, the amount falling in various seasons, and other climatic factors in their relative influence on tree-ring widths. At present, then, tree-ring widths may be considered more satisfactory for reading chronology than for reading climate. </p><p>It is this concern about direct correlation of tree-ring width with climate that led to initiation of the present study. This work is a preliminary attempt to obtain independent evidence from pollen concerning the probable nature of the vegetation and thus the climate in a period known to be characterized by narrow tree rings. </p>","conferenceTitle":"Arid Zone Research - XX: Changes of Climate","conferenceDate":"Rome, Italy","conferenceLocation":"October 2-7, 1961","language":"English","publisher":"UNESCO","publisherLocation":"Paris, France","usgsCitation":"Leopold, L.B., Leopold, E.B., and Wendorf, F., 1963, Some climatic indicators in the period A.D. 1200-1400 in New Mexico, Arid Zone Research - XX: Changes of Climate, October 2-7, 1961, Rome, Italy, p. 265-270.","productDescription":"6 p.","startPage":"265","endPage":"270","costCenters":[],"links":[{"id":338307,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338306,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.unesco.org/ulis/cgi-bin/ulis.pl?catno=69895&set=0058D562F8_3_182&gp=1&lin=1&ll=1"}],"country":"United States","state":"New Mexico","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63044e4b05ec79913113d","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686101,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Estella B.","contributorId":30979,"corporation":false,"usgs":true,"family":"Leopold","given":"Estella","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":686102,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wendorf, F.","contributorId":103801,"corporation":false,"usgs":true,"family":"Wendorf","given":"F.","email":"","affiliations":[],"preferred":false,"id":686103,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70190982,"text":"70190982 - 1963 - Quality of water, Upper Colorado River Basin: Progress report","interactions":[],"lastModifiedDate":"2017-09-19T16:08:07","indexId":"70190982","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":9,"text":"Other Report"},"title":"Quality of water, Upper Colorado River Basin: Progress report","docAbstract":"<p>No abstract available.</p>","language":"English","publisherLocation":"Washington, D.C.","usgsCitation":"U.S. Bureau of Reclamation, 1963, Quality of water, Upper Colorado River Basin: Progress report, iv, 66 p.","productDescription":"iv, 66 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345897,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"Upper Colorado River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb7e4b091459a61b759","contributors":{"authors":[{"text":"U.S. Bureau of Reclamation","contributorId":128054,"corporation":true,"usgs":false,"organization":"U.S. Bureau of Reclamation","id":710813,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70190981,"text":"70190981 - 1963 - Chemical analyses of surface waters in Utah, October 1959 to September 1962","interactions":[],"lastModifiedDate":"2017-09-19T16:04:30","indexId":"70190981","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":375,"text":"Open-File Report","active":false,"publicationSubtype":{"id":6}},"title":"Chemical analyses of surface waters in Utah, October 1959 to September 1962","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/70190981","usgsCitation":"U.S. Geological Survey, 1963, Chemical analyses of surface waters in Utah, October 1959 to September 1962: Open-File Report, 51 p., https://doi.org/10.3133/70190981.","productDescription":"51 p.","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Utah","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59c22cb7e4b091459a61b75c","contributors":{"authors":[{"text":"U.S. Geological Survey","contributorId":128240,"corporation":true,"usgs":false,"organization":"U.S. Geological Survey","id":710812,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70185600,"text":"70185600 - 1963 - Simple measurements of morphological changes in river channels and hillslopes","interactions":[],"lastModifiedDate":"2017-03-24T13:19:41","indexId":"70185600","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":24,"text":"Conference Paper"},"publicationSubtype":{"id":19,"text":"Conference Paper"},"title":"Simple measurements of morphological changes in river channels and hillslopes","docAbstract":"<p>One of the principal types of observational evidence on climatic changes in the recent geologic past is in river position and elevation. It is well known that river channels, particularly those flowing through alluvium or on relatively soft bedrock, tend to develop flood plains by lateral migration of the channel. Abandoned flood plains at elevations distinctly above the present river channel are the origin of river terraces, widespread through the world but particularly noticeable in arid regions. Climatic change is one of the causes of the abandonment of flood plains and the consequent formation of river terraces. Therefore, the identification and stratigraphy of river terraces is one of the methods by which climatic changes in the recent geologic past can be studied.</p><p>There are, of course, morphologic changes in river channels of a more subtle nature. Even when a channel is progressively degrading-a trend which will eventually result in the formation of a river terracethere are no obvious criteria by which the current changes in a river channel can be positively identified. For this reason simple techniques, which will aid in the direct observation of current changes in a channel’s position, can be helpful in identifying the nature of changes in progress. </p><p>It is the purpose of this paper to describe some relatively simple techniques which have been found to be useful in observing morphological changes on slopes and in channels. The methods have been tested primarily in arid climates but to some extent they can also be useful even where vegetation is prominent. </p>","conferenceTitle":"Arid Zone Research - XX: Changes of Climate","conferenceDate":"October 2-7, 1961","conferenceLocation":"Rome, Italy","language":"English","publisher":"UNESCO","publisherLocation":"Paris, France","usgsCitation":"Miller, J., and Leopold, L.B., 1963, Simple measurements of morphological changes in river channels and hillslopes, Arid Zone Research - XX: Changes of Climate, Rome, Italy, October 2-7, 1961, p. 421-427.","productDescription":"7 p.","startPage":"421","endPage":"427","costCenters":[],"links":[{"id":338305,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338304,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.unesco.org/ulis/cgi-bin/ulis.pl?catno=69895&set=0058D562F8_3_182&gp=1&lin=1&ll=1"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58d63044e4b05ec79913113f","contributors":{"authors":[{"text":"Miller, J.P.","contributorId":62269,"corporation":false,"usgs":true,"family":"Miller","given":"J.P.","email":"","affiliations":[],"preferred":false,"id":686096,"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":686097,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2000007,"text":"2000007 - 1963 - Limnological survey of Lake Erie 1959 and 1960","interactions":[],"lastModifiedDate":"2012-02-02T00:14:59","indexId":"2000007","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":3,"text":"Organization Series"},"seriesTitle":{"id":222,"text":"Technical Report","active":false,"publicationSubtype":{"id":3}},"seriesNumber":"6","title":"Limnological survey of Lake Erie 1959 and 1960","docAbstract":"Federal, provincial, state, and university organizations participated in cooperative limnological surveys of Lake Erie in September 1959 and August 1960 to determine the extent and severity of the low dissolved-oxygen content of the hypolimnetic waters.  Observations were restricted to the central basin in 1959, but were lake-wide in 1960.  Approximately 70 percent of the bottom waters of the central basin had a serious oxygen deficiency during both years.  Data were obtained also on the distribution of temperature, transparency, specific conductance, pH, and phenolphthalein and total alkalinity.  The distributions of the chemical values are discussed in terms of their relationships to each other, and to thermal stratification, river outflow, lake morphometry, and lake currents.","language":"English","publisher":"Great Lakes Fishery Commission","collaboration":"Out-of-print","usgsCitation":"Beeton, A.M., 1963, Limnological survey of Lake Erie 1959 and 1960: Technical Report 6, 32 p.","productDescription":"32 p.","startPage":"0","endPage":"32","numberOfPages":"32","costCenters":[{"id":324,"text":"Great Lakes Science Center","active":true,"usgs":true}],"links":[{"id":198577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":92067,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://www.glfc.org/pubs/TechReports/Tr06.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1de4b07f02db6a9d92","contributors":{"authors":[{"text":"Beeton, Alfred M.","contributorId":94247,"corporation":false,"usgs":true,"family":"Beeton","given":"Alfred","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":324916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010715,"text":"70010715 - 1963 - Antiferromagnetism of UO2⋅2H2O","interactions":[],"lastModifiedDate":"2025-01-28T16:27:45.518806","indexId":"70010715","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2207,"text":"Journal of Chemical Physics","active":true,"publicationSubtype":{"id":10}},"displayTitle":"Antiferromagnetism of UO<sub>2</sub>⋅2H<sub>2</sub>O","title":"Antiferromagnetism of UO2⋅2H2O","docAbstract":"<p><span>Magnetic susceptibility measurements have been made on UO</span><sub>2</sub><span>·</span><i>x</i><span>H</span><sub>2</sub><span>O for&nbsp;</span><i>x</i><span>=1.78 to&nbsp;</span><i>x</i><span>=2.13, and from 77° to 375°K. As the value of&nbsp;</span><i>x</i><span>&nbsp;decreased the susceptibility increased. Both these data and structural arguments imply that the formula of this compound is U(OH)</span><sub>4</sub><span>&nbsp;rather than the dihydrate form. Based on this concept the data have been corrected for diamagnetism and also small amounts of UO</span><sub>2</sub><span>&nbsp;and H</span><sub>2</sub><span>O which were present. The molar susceptibility of U</span><sup>4+</sup><span>&nbsp;in U(OH)</span><sub>4</sub><span>&nbsp;is nearly an order of magnitude less than in other uranium compounds, and it is suggested that this is probably due to superexchange between adjacent uranium atoms through intervening oxygen atoms.</span></p>","language":"English","publisher":"American Institute of Physics","doi":"10.1063/1.1734516","issn":"00219606","usgsCitation":"Pankey, T., Senftle, F.E., and Cuttitta, F., 1963, Antiferromagnetism of UO2⋅2H2O: Journal of Chemical Physics, v. 39, no. 7, p. 1702-1706, https://doi.org/10.1063/1.1734516.","productDescription":"5 p.","startPage":"1702","endPage":"1706","numberOfPages":"5","costCenters":[],"links":[{"id":219484,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"39","issue":"7","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059ec63e4b0c8380cd4924b","contributors":{"authors":[{"text":"Pankey, T.","contributorId":58773,"corporation":false,"usgs":true,"family":"Pankey","given":"T.","affiliations":[],"preferred":false,"id":359480,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Senftle, F. E.","contributorId":47788,"corporation":false,"usgs":true,"family":"Senftle","given":"F.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359479,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cuttitta, F.","contributorId":33837,"corporation":false,"usgs":true,"family":"Cuttitta","given":"F.","affiliations":[],"preferred":false,"id":359478,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70010839,"text":"70010839 - 1963 - Tertiary lake deposits in western coterminous United States","interactions":[],"lastModifiedDate":"2026-02-25T14:39:34.885888","indexId":"70010839","displayToPublicDate":"1963-01-01T00:00:00","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":"Tertiary lake deposits in western coterminous United States","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.139.3550.107","issn":"00368075","usgsCitation":"Feth, J.H., 1963, Tertiary lake deposits in western coterminous United States: Science, v. 139, no. 3550, p. 107-110.","productDescription":"4 p.","startPage":"107","endPage":"110","costCenters":[],"links":[{"id":219010,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","otherGeospatial":"western coterminous United States","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -125.96491923714473,\n              48.85986140208797\n            ],\n            [\n              -125.96491923714473,\n              31.6162602251043\n            ],\n            [\n              -101.27376596663822,\n              31.6162602251043\n            ],\n            [\n              -101.27376596663822,\n              48.85986140208797\n            ],\n            [\n              -125.96491923714473,\n              48.85986140208797\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","volume":"139","issue":"3550","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505ba579e4b08c986b320a8e","contributors":{"authors":[{"text":"Feth, J. H.","contributorId":50495,"corporation":false,"usgs":true,"family":"Feth","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359765,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010714,"text":"70010714 - 1963 - Study of multicomponent mixtures in solution with a vertical-axis transmission-type filter-fluorometer","interactions":[],"lastModifiedDate":"2023-03-20T16:04:33.571393","indexId":"70010714","displayToPublicDate":"1963-01-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Study of multicomponent mixtures in solution with a vertical-axis transmission-type filter-fluorometer","docAbstract":"Fluorescence intensity, sensitivity, and the effect of diverse ions are discussed in relation to chemical equilibrium and the general equation for fluorescence. High sensitivity is the common denominator in eliminating or reducing all types of interference and the general equation is the key for quickly selecting conditions that give maximum sensitivity. With a transmission-type fluorometer, experimental fluorescence intensities adhere to the general equation over a very wide range of light absorption. If the instrument has a vertical axis, solution depth can be adjusted so that the data fall on that portion of the theoretical curve which is essentially a straight line. When the fluorescence wavelength selected for measurement is not absorbed by the solution, the general equation reduces to a much simpler expression, and then, under proper circumstances, fluorescence values can be used for calculations as confidently and as easily as absorbance values.","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60196a004","usgsCitation":"Fletcher, M.H., 1963, Study of multicomponent mixtures in solution with a vertical-axis transmission-type filter-fluorometer: Analytical Chemistry, v. 35, no. 3, p. 278-288, https://doi.org/10.1021/ac60196a004.","productDescription":"11 p.","startPage":"278","endPage":"288","numberOfPages":"11","costCenters":[],"links":[{"id":219483,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"35","issue":"3","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505b9cd7e4b08c986b31d4df","contributors":{"authors":[{"text":"Fletcher, M. H.","contributorId":53438,"corporation":false,"usgs":true,"family":"Fletcher","given":"M.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":359477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70010841,"text":"70010841 - 1963 - Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis","interactions":[],"lastModifiedDate":"2020-11-19T19:09:57.574769","indexId":"70010841","displayToPublicDate":"1963-01-01T00:00:00","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":"Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis","docAbstract":"<p>Experiments at 700°C and 800 bars total pressure demonstrate positive deviations from ideality for mixtures of hydrogen and H<sub>2</sub>O gases. The deviations are greater than predicted with Stockmayer's method. The composition of the mixture and the fugacity of hydrogen are controlled by diffusing hydrogen through metallic membranes. The results give the fugacities of both H<sub>2</sub>O and oxygen.</p>","language":"English","publisher":"AAAS","doi":"10.1126/science.139.3560.1220","usgsCitation":"Shaw, H.R., 1963, Hydrogen-water vapor mixtures: Control of hydrothermal atmospheres by hydrogen osmosis: Science, v. 139, no. 3560, p. 1220-1222, https://doi.org/10.1126/science.139.3560.1220.","productDescription":"3 p.","startPage":"1220","endPage":"1222","numberOfPages":"3","costCenters":[],"links":[{"id":219012,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"139","issue":"3560","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a3352e4b0c8380cd5eeea","contributors":{"authors":[{"text":"Shaw, H. R.","contributorId":23952,"corporation":false,"usgs":true,"family":"Shaw","given":"H.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":359767,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
]}