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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b751","usgsCitation":"Heald, K.C., and Thom, W.T., 1925, Contributions to economic geology (short papers and preliminary reports), 1923-1924: Part II. - Mineral fuels: U.S. Geological Survey Bulletin 751, 326 p., https://doi.org/10.3133/b751.","productDescription":"326 p.","costCenters":[],"links":[{"id":92883,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0751/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166299,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0751/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a40","contributors":{"authors":[{"text":"Heald, K. C.","contributorId":80239,"corporation":false,"usgs":true,"family":"Heald","given":"K.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":213333,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thom, W. T. Jr.","contributorId":63452,"corporation":false,"usgs":true,"family":"Thom","given":"W.","suffix":"Jr.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":213332,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":35663,"text":"b774 - 1925 - The copper deposits near Salmon, Idaho","interactions":[],"lastModifiedDate":"2012-02-02T00:09:43","indexId":"b774","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"774","title":"The copper deposits near Salmon, Idaho","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/b774","usgsCitation":"Ross, C.P., 1925, The copper deposits near Salmon, Idaho: U.S. Geological Survey Bulletin 774, 44 p. illus., v pl. (part fold., incl. maps, plan) ;23 cm., https://doi.org/10.3133/b774.","productDescription":"44 p. illus., v pl. (part fold., incl. maps, plan) ;23 cm.","costCenters":[],"links":[{"id":93435,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0774/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":167734,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0774/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69684a","contributors":{"authors":[{"text":"Ross, Clyde Polhemus","contributorId":71954,"corporation":false,"usgs":true,"family":"Ross","given":"Clyde","email":"","middleInitial":"Polhemus","affiliations":[],"preferred":false,"id":215023,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52783,"text":"b766J - 1925 - Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 118 degrees to 119 degrees longitude","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"b766J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"766","chapter":"J","title":"Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 118 degrees to 119 degrees longitude","language":"ENGLISH","publisher":"Govt. 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During a great part of the nineteenth century many philosophical chemists held a vague belief that these elements were not distinct entities but manifestations of one primal substance-the protyle, as it is sometimes called. Other chemists, more conservative, looked askance at all such speculations and held fast to what they regarded as established facts. To them an element was something distinct from other kinds of matter, a substance which could neither be decomposed nor transmuted into anything else. This belief, however, was based entirely upon negative evidence-the inadequacy of our existing resources to produce such sweeping changes. Many important facts were ignored, and especially the fact that the elements are connected by very intimate relations, such as are best shown in the periodic law of Mendeleef, who, from gaps in his table of atomic weights, predicted the existence of three unknown metals, which have since been discovered. For these metals, scandium, gallium, and germanium, he foretold not only their atomic weights but also their most characteristic physical properties and the sort of compounds that each one would form. His prophecies have been verified in every essential particular. One obvious conclusion was soon drawn from Mendeleef's \"law,\" although he was too cautious to admit it, namely, that the chemical elements must have had some community of origin. The philosophical speculations as to their nature were fully justified.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1923-24","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","doi":"10.3133/pp132D","usgsCitation":"Clarke, F.W., 1925, The evolution and disintegration of matter: U.S. Geological Survey Professional Paper 132, 37 p., https://doi.org/10.3133/pp132D.","productDescription":"37 p.","startPage":"51","endPage":"86","costCenters":[],"links":[{"id":172965,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132d/report-thumb.jpg"},{"id":271210,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132d/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65dc90","contributors":{"authors":[{"text":"Clarke, Frank Wigglesworth","contributorId":88798,"corporation":false,"usgs":true,"family":"Clarke","given":"Frank","email":"","middleInitial":"Wigglesworth","affiliations":[],"preferred":false,"id":221354,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52782,"text":"b766I - 1925 - Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 117 degrees to 118 degrees longitude","interactions":[],"lastModifiedDate":"2012-02-02T00:11:46","indexId":"b766I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"766","chapter":"I","title":"Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 117 degrees to 118 degrees longitude","language":"ENGLISH","publisher":"Govt. 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The limitation in a particular instance may be the quantity of water available, the quality determined by the mineral matter in solution or in suspension or by organic pollution, or the temperature of the water. Generally it is a combination of two or more of these factors.
Many publications of the Geological Survey give data in regard to the quantity of surface water and ground water obtainable at different points. Other publications of this Survey and of other organizations give data on the quality of waters available for industrial use. The temperature of these waters is discussed in the present report.
Data in regard to ground water have been obtained from Geological Survey water-supply papers, from the publications indicated in footnotes, and from an unpublished compilation of temperature records prepared by C. E. Van Orstrand, of the Geological Survey, in connection with studies of deep earth temperature. Data on temperature of surface water have been obtained mainly from officials of waterworks, as noted in the accompanying table. Data on air temperature have been obtained from reports of the United States Weather Bureau. The maps showing temperature of ground water and surface water (Pls. VIII and IX) are taken directly from Weather Bureau charts of temperature distribution.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1923-1924 (Water Supply Paper 520)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp520F","collaboration":"This report is Chapter F in Contributions to the hydrology of the United States, 1923-1924. For more information, see Water Supply Paper 520.","usgsCitation":"Collins, W.D., 1925, Temperature of water available for industrial use in the United States: Chapter F in Contributions to the hydrology of the United States, 1923-1924: U.S. Geological Survey Water Supply Paper 520, iv, 8 p., https://doi.org/10.3133/wsp520F.","productDescription":"iv, 8 p.","startPage":"97","endPage":"104","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":157222,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520f/report-thumb.jpg"},{"id":279497,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520f/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685812","contributors":{"authors":[{"text":"Collins, W. D.","contributorId":37713,"corporation":false,"usgs":true,"family":"Collins","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":193152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52776,"text":"b766C - 1925 - Spirit leveling in California, 1896-1923: 32 degrees to 33 degrees latitude, 115 degrees to 116 degrees longitude","interactions":[],"lastModifiedDate":"2012-02-02T00:11:39","indexId":"b766C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"766","chapter":"C","title":"Spirit leveling in California, 1896-1923: 32 degrees to 33 degrees latitude, 115 degrees to 116 degrees longitude","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/b766C","usgsCitation":"Birdseye, C., 1925, Spirit leveling in California, 1896-1923: 32 degrees to 33 degrees latitude, 115 degrees to 116 degrees longitude: U.S. Geological Survey Bulletin 766, 7-10 p. :fold. map ;23 cm., https://doi.org/10.3133/b766C.","productDescription":"7-10 p. :fold. map ;23 cm.","costCenters":[],"links":[{"id":100221,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0766c/report.pdf","size":"201","linkFileType":{"id":1,"text":"pdf"}},{"id":178296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0766c/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4d4b","contributors":{"authors":[{"text":"Birdseye, Claude Hale","contributorId":68793,"corporation":false,"usgs":true,"family":"Birdseye","given":"Claude Hale","affiliations":[],"preferred":false,"id":246011,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52781,"text":"b766H - 1925 - Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 116 degrees to 117 degrees longitude","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"b766H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"766","chapter":"H","title":"Spirit leveling in California, 1896-1923: 33 degrees to 34 degrees latitude, 116 degrees to 117 degrees longitude","language":"ENGLISH","publisher":"Govt. 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The chief deficiency to be supplied was a continuous topographic map of the valley in sufficient detail to permit calculation of the storage capacity of any reservoir site that might be used, the stream gradient, and similar features. Maps on a satisfactory scale of a number of isolated \nstretches of the river had already been made by public or private agencies, and it was necessary to verify them and connect them on a uniform datum. Inasmuch as it was deemed unlikely that a dam higher than 300 feet would be constructed anywhere on the part of the river to be examined, a plane 300 feet above the water surface was made the upper limit of mapping. Over such parts of the valley as had been mapped already the progress of the party was naturally very rapid, and even where no mapping had previously been done, the 300-foot limit set upon the work and the usual narrowness of the valley combined to reduce the extent of the area to be mapped, so that the speed maintained was relatively high. Under this condition of rapid movement it was seldom possible to make more than the most cursory examination of the rocks, though occasionally circumstances permitted more or less detailed observation. The notes here recorded are therefore mostly of a rather generalized character, but as they pertain in part to localities that are difficult of access and not often visited by geologists, and that are at the same time classic in the history of American geology, I venture to to record them for whatever value they may \nhave to other geologists.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1923-24","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","doi":"10.3133/pp132C","usgsCitation":"Reeside, J., 1925, Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah: U.S. Geological Survey Professional Paper 132, 16 p., https://doi.org/10.3133/pp132C.","productDescription":"16 p.","startPage":"35","endPage":"50","costCenters":[],"links":[{"id":172964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132c/report-thumb.jpg"},{"id":271209,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132c/report.pdf"}],"country":"United States","state":"Utah;Wyoming","otherGeospatial":"Green River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.13,37.75 ], [ -112.13,42.57 ], [ -109.43,42.57 ], [ -109.43,37.75 ], [ -112.13,37.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969b2","contributors":{"authors":[{"text":"Reeside, J.B. 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