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,{"id":391,"text":"wsp522 - 1925 - Surface water supply of the United States, 1921, Part II, South Atlantic slope and eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp522","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"522","title":"Surface water supply of the United States, 1921, Part II, South Atlantic slope and eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp522","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1925, Surface water supply of the United States, 1921, Part II, South Atlantic slope and eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 522, iv, 72 p. ;23 cm., https://doi.org/10.3133/wsp522.","productDescription":"iv, 72 p. ;23 cm.","costCenters":[],"links":[{"id":137325,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0522/report-thumb.jpg"},{"id":24954,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0522/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697c21","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":527364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":384,"text":"wsp509 - 1925 - Surface water supply of the United States, 1919-1920, Part IX, Colorado River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:11","indexId":"wsp509","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"509","title":"Surface water supply of the United States, 1919-1920, Part IX, Colorado River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp509","usgsCitation":"Grover, N., Follansbee, R., Purton, A., and McGlashan, H., 1925, Surface water supply of the United States, 1919-1920, Part IX, Colorado River basin: U.S. Geological Survey Water Supply Paper 509, v, 269 p. ;23 cm., https://doi.org/10.3133/wsp509.","productDescription":"v, 269 p. ;23 cm.","costCenters":[],"links":[{"id":136392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0509/report-thumb.jpg"},{"id":24947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0509/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697c42","contributors":{"authors":[{"text":"Grover, Nathan C.","contributorId":11583,"corporation":false,"usgs":true,"family":"Grover","given":"Nathan C.","affiliations":[],"preferred":false,"id":142306,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Follansbee, Robert","contributorId":51713,"corporation":false,"usgs":true,"family":"Follansbee","given":"Robert","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":142308,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Purton, A.B.","contributorId":18338,"corporation":false,"usgs":true,"family":"Purton","given":"A.B.","email":"","affiliations":[],"preferred":false,"id":142307,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"McGlashan, H.D.","contributorId":81876,"corporation":false,"usgs":true,"family":"McGlashan","given":"H.D.","affiliations":[],"preferred":false,"id":142309,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":39360,"text":"pp132E - 1925 - An early Eocene florule from central Texas","interactions":[],"lastModifiedDate":"2013-09-19T09:32:22","indexId":"pp132E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"E","title":"An early Eocene florule from central Texas","docAbstract":"In 1916 I described a florule collected by Alexander Deussen and L. W. Stephenson at the town of Earle, in Bexar County, Tex. This florule was tentatively considered of Midway age by these geologists, and examination of the fossil plants tended to confirm this assignment, particularly because of their lack of\nharmony with the extensive Wilcox flora described in the volume cited above and because of their resemblance to the described floras from the Raton and Denver formations of Colorado and New Mexico.","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/pp132E","usgsCitation":"Berry, E.W., 1925, An early Eocene florule from central Texas: U.S. Geological Survey Professional Paper 132, 6 p., https://doi.org/10.3133/pp132E.","productDescription":"6 p.","startPage":"87","endPage":"92","numberOfPages":"7","costCenters":[],"links":[{"id":172966,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132e/report-thumb.jpg"},{"id":271211,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132e/report.pdf"}],"country":"United States","state":"Texas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -106.65,25.84 ], [ -106.65,36.5 ], [ -93.51,36.5 ], [ -93.51,25.84 ], [ -106.65,25.84 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684d93","contributors":{"authors":[{"text":"Berry, Edward Wilber","contributorId":36206,"corporation":false,"usgs":true,"family":"Berry","given":"Edward","email":"","middleInitial":"Wilber","affiliations":[],"preferred":false,"id":221355,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39362,"text":"pp132H - 1925 - The resuscitation of the term Bryn Mawr gravel","interactions":[],"lastModifiedDate":"2013-09-19T14:45:52","indexId":"pp132H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"H","title":"The resuscitation of the term Bryn Mawr gravel","docAbstract":"In the course of geologic and physiographic work in eastern Pennsylvania, it has seemed to the writer that the time was ripe for the restriction of the term Brandywine formation, now including presumably both Pliocene and Pleistocene gravels, and the reinstatement of the old term Bryn Mawr gravel for a portion of the divided Brandywine. A brief history of the nomenclature and usage involved will show the grounds for the choice of terms.","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/pp132H","usgsCitation":"Bascom, F., 1925, The resuscitation of the term Bryn Mawr gravel: U.S. Geological Survey Professional Paper 132, 3 p., https://doi.org/10.3133/pp132H.","productDescription":"3 p.","startPage":"117","endPage":"119","costCenters":[],"links":[{"id":173311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132h/report-thumb.jpg"},{"id":271213,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132h/report.pdf"}],"country":"United States","state":"Pennsylvania","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -80.5199,39.7198 ], [ -80.5199,42.2694 ], [ -74.6895,42.2694 ], [ -74.6895,39.7198 ], [ -80.5199,39.7198 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640ec1","contributors":{"authors":[{"text":"Bascom, Florence","contributorId":107668,"corporation":false,"usgs":true,"family":"Bascom","given":"Florence","email":"","affiliations":[],"preferred":false,"id":221357,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39363,"text":"pp132I - 1925 - Origin of the boghead coals","interactions":[],"lastModifiedDate":"2013-09-19T15:03:23","indexId":"pp132I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"I","title":"Origin of the boghead coals","docAbstract":"The bituminous rocks of sedimentary origin may be classified roughly under two main heads - coals and bituminous shales. In a strict sense no definite line can be drawn between these two groups, because coals may be insensibly grade into bituminous shales. Chemically the boghead coals are preeminently bituminous.","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/pp132I","usgsCitation":"Thiessen, R., 1925, Origin of the boghead coals: U.S. Geological Survey Professional Paper 132, 17 p., https://doi.org/10.3133/pp132I.","productDescription":"17 p.","startPage":"121","endPage":"137","costCenters":[],"links":[{"id":173312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132i/report-thumb.jpg"},{"id":271220,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132i/report.pdf"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a603","contributors":{"authors":[{"text":"Thiessen, Reinhardt","contributorId":31457,"corporation":false,"usgs":true,"family":"Thiessen","given":"Reinhardt","email":"","affiliations":[],"preferred":false,"id":221358,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36204,"text":"b778 - 1925 - Chemistry of deposition of native copper from ascending solutions","interactions":[],"lastModifiedDate":"2012-02-02T00:09:40","indexId":"b778","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":"778","title":"Chemistry of deposition of native copper from ascending solutions","language":"ENGLISH","publisher":"Govt. Print. Office,","doi":"10.3133/b778","usgsCitation":"Wells, R.C., 1925, Chemistry of deposition of native copper from ascending solutions: U.S. Geological Survey Bulletin 778, 71 p. ill. ;24 cm., https://doi.org/10.3133/b778.","productDescription":"71 p. ill. ;24 cm.","costCenters":[],"links":[{"id":93795,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/0778/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":166104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/0778/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dee4b07f02db5e2ed1","contributors":{"authors":[{"text":"Wells, Roger Clark","contributorId":89193,"corporation":false,"usgs":true,"family":"Wells","given":"Roger","email":"","middleInitial":"Clark","affiliations":[],"preferred":false,"id":215940,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39366,"text":"pp136 - 1925 - The flora of the Ripley formation","interactions":[],"lastModifiedDate":"2012-02-02T00:10:37","indexId":"pp136","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"136","title":"The flora of the Ripley formation","language":"ENGLISH","doi":"10.3133/pp136","usgsCitation":"Berry, E.W., 1925, The flora of the Ripley formation: U.S. Geological Survey Professional Paper 136, 94 p., https://doi.org/10.3133/pp136.","productDescription":"94 p.","costCenters":[],"links":[{"id":113500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0136/report.pdf","size":"20150","linkFileType":{"id":1,"text":"pdf"}},{"id":173404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0136/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a71e4b07f02db6421d8","contributors":{"authors":[{"text":"Berry, E. W.","contributorId":82754,"corporation":false,"usgs":true,"family":"Berry","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":221362,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39358,"text":"pp132C - 1925 - Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah","interactions":[],"lastModifiedDate":"2013-09-13T14:32:30","indexId":"pp132C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"C","title":"Notes on the geology of Green River Valley between Green River, Wyoming, and Green River, Utah","docAbstract":"During July, August, and part of September, 1922, I had the privilege of accompanying a party sent out jointly by the Utah Power & Light Co. and the United States Geological Survey to gather such data as were still needed to complete a study of the power resources of Green River between Green River, Wyo., and Green River, Utah. 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. Jr.","contributorId":29787,"corporation":false,"usgs":true,"family":"Reeside","given":"J.B.","suffix":"Jr.","affiliations":[],"preferred":false,"id":221353,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":39359,"text":"pp132D - 1925 - The evolution and disintegration of matter","interactions":[],"lastModifiedDate":"2013-09-13T15:24:34","indexId":"pp132D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"D","title":"The evolution and disintegration of matter","docAbstract":"In any attempt to study the evolution of matter it is necessary to begin with its simplest known forms, the so-called chemical elements. 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":39357,"text":"pp132B - 1925 - A new fauna from the Colorado group of southern Montana","interactions":[],"lastModifiedDate":"2013-09-13T14:13:18","indexId":"pp132B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"B","title":"A new fauna from the Colorado group of southern Montana","docAbstract":"This paper describes a small but interesting fauna collected in 1921 by W. T. Thorn, Jr., Gail F. Moulton, T. W. Stanton, and K. C. Heald in the Crow Indian Reservation in southern Montana. The locality is in sec. 36, T. 6 S., R. 32 E., Big Horn County, and is 2 miles east of the Soap Creek oil field.","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/pp132B","usgsCitation":"Reeside, J.B., 1925, A new fauna from the Colorado group of southern Montana: U.S. Geological Survey Professional Paper 132, 6 p., https://doi.org/10.3133/pp132B.","productDescription":"6 p.","startPage":"25","endPage":"33","numberOfPages":"19","costCenters":[],"links":[{"id":172963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132b/report-thumb.jpg"},{"id":271208,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132b/report.pdf"}],"country":"United States","state":"Montana","otherGeospatial":"Big Horn County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108.6992,44.9939 ], [ -108.6992,46.0429 ], [ -106.2643,46.0429 ], [ -106.2643,44.9939 ], [ -108.6992,44.9939 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b20e4b07f02db6abf57","contributors":{"authors":[{"text":"Reeside, John B. Jr.","contributorId":98299,"corporation":false,"usgs":true,"family":"Reeside","given":"John","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":221352,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":36285,"text":"b769 - 1925 - The geologic time classification of the United States Geological Survey compared with other classifications, accompanied by the original definitions of era, period and epoch terms","interactions":[],"lastModifiedDate":"2022-08-22T21:20:03.236811","indexId":"b769","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":"769","title":"The geologic time classification of the United States Geological Survey compared with other classifications, accompanied by the original definitions of era, period and epoch terms","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b769","usgsCitation":"Wilmarth, M.G., 1925, The geologic time classification of the 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,{"id":39356,"text":"pp132A - 1925 - Rock formations in the Colorado Plateau of Southeastern Utah and Northern Arizona","interactions":[],"lastModifiedDate":"2013-09-13T13:16:03","indexId":"pp132A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"A","title":"Rock formations in the Colorado Plateau of Southeastern Utah and Northern Arizona","docAbstract":"The field work of which this report is a record was done in the summer and fall of 1921 by members of the United States Geological Survey. A project to build a large storage dam at Lees Ferry, on Colorado River in northern Arizona, called for a detailed topographic survey of the area covered by the project, for the purpose of determining the capacity of the reservoir. This work was undertaken by the United States Geological Survey in cooperation with the Southern California Edison Co. Three surveying parties were sent to the field, each accompanied by a geologist, whose specific duty was to study and report on the rock formations within the area to be flooded. One topographic party, under A. T. Fowler, which started at Lees Ferry and worked up stream in Arizona, was accompanied by Kirk Bryan. Another party, under K. W. Trimble, which started near Bluff and worked down the San Juan and thence down the Colorado, was accompanied by H. D. Miser. The third party, under W. R. Chenoweth, worked from Fremont River to the Waterpocket Fold and then returned to Green River, Utah, and traversed Cataract Canyon during the period of low water. C. R. Longwell was with this party until September, when his place was taken by Sidney Paige. Mr. Paige, in company with the Kolb brothers, E. C. La Rue, and Henry Ranch, left the Chenoweth party after Cataract Canyon had been surveyed and rowed down the Colorado to the mouth of the San Juan, where they were joined by Mr. Miser. Then they took a hurried trip by boat down the Colorado to Lees Ferry, making a few short stops and visiting the famous Rainbow Bridge. Thus the geology of the canyons of Colorado and San Juan rivers and of the lower parts of tributary canyons was examined continuously, and reconnaissance work was done in the country back from the rivers. At the same time a fourth party, under R. C. Moore, was mapping parts of Kane, Garfield, and Wayne counties, Utah, to determine whether oil might be found there. The present paper includes brief descriptions of the rocks of the regions traversed, detailed geologic sections, and columnar sections measured not only by the geologists who accompanied these parties but by other geologists who have worked in the same regions or in adjoining regions. The positions of the columnar sections measured and many of the other sections are shown on Figure 1.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1923-24","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp132A","usgsCitation":"Longwell, C., Miser, H., Moore, R., Bryan, K., and Paige, S., 1925, Rock formations in the Colorado Plateau of Southeastern Utah and Northern Arizona: U.S. Geological Survey Professional Paper 132, 23 p., https://doi.org/10.3133/pp132A.","productDescription":"23 p.","numberOfPages":"33","costCenters":[],"links":[{"id":124645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132a/report-thumb.jpg"},{"id":12446,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://www.nps.gov/history/history/online_books/geology/publications/pp/132-A/index.htm","linkFileType":{"id":5,"text":"html"}},{"id":271205,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132a/report.pdf"}],"country":"United States","state":"Arizona;Utah","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ], [ -0.016666666666666666,8.333333333333334E-4 ], [ -0.016666666666666666,8.333333333333334E-4 ], [ -0.01638888888888889,8.333333333333334E-4 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968c5","contributors":{"authors":[{"text":"Longwell, C.R.","contributorId":53439,"corporation":false,"usgs":true,"family":"Longwell","given":"C.R.","affiliations":[],"preferred":false,"id":221349,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miser, H.D.","contributorId":43329,"corporation":false,"usgs":true,"family":"Miser","given":"H.D.","affiliations":[],"preferred":false,"id":221348,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, R.C.","contributorId":77180,"corporation":false,"usgs":true,"family":"Moore","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":221350,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Bryan, Kirk","contributorId":37308,"corporation":false,"usgs":true,"family":"Bryan","given":"Kirk","email":"","affiliations":[],"preferred":false,"id":221347,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Paige, Sidney","contributorId":107752,"corporation":false,"usgs":true,"family":"Paige","given":"Sidney","email":"","affiliations":[],"preferred":false,"id":221351,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":39361,"text":"pp132G - 1925 - Discovery of a Balkan fresh-water fauna in the Idaho formation of Snake River Valley, Idaho","interactions":[],"lastModifiedDate":"2013-09-19T14:38:13","indexId":"pp132G","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"G","title":"Discovery of a Balkan fresh-water fauna in the Idaho formation of Snake River Valley, Idaho","docAbstract":"In 1866 Gabb described Melania taylori and Lithasia antiqua \"from a fresh-water deposit on Snake River, Idaho Territory, on the road from Fort Boise to the Owyhee mining country. Collected by A. Taylor.\" He states that a small bivalve, perhaps a Sphaerium, was associated with them.","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/pp132G","usgsCitation":"Dall, W., 1925, Discovery of a Balkan fresh-water fauna in the Idaho formation of Snake River Valley, Idaho: U.S. Geological Survey Professional Paper 132, 7 p., https://doi.org/10.3133/pp132G.","productDescription":"7 p.","startPage":"109","endPage":"115","numberOfPages":"9","costCenters":[],"links":[{"id":173310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132g/report-thumb.jpg"},{"id":271212,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132g/report.pdf"}],"country":"United States","state":"Idaho","otherGeospatial":"Snake River Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -95.63,38.86 ], [ -95.63,39.04 ], [ -95.26,39.04 ], [ -95.26,38.86 ], [ -95.63,38.86 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64ab03","contributors":{"authors":[{"text":"Dall, W.H.","contributorId":23600,"corporation":false,"usgs":true,"family":"Dall","given":"W.H.","affiliations":[],"preferred":false,"id":221356,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4648,"text":"wsp561 - 1925 - Surface water supply of the United States, 1923, Part I, North Atlantic slope basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"wsp561","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"561","title":"Surface water supply of the United States, 1923, Part I, North Atlantic slope basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp561","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1925, Surface water supply of the United States, 1923, Part I, North Atlantic slope basins: U.S. Geological Survey Water Supply Paper 561, vi, 294 p. ;23 cm., https://doi.org/10.3133/wsp561.","productDescription":"vi, 294 p. ;23 cm.","costCenters":[],"links":[{"id":139374,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0561/report-thumb.jpg"},{"id":31703,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0561/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697b89","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528339,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4647,"text":"wsp544 - 1925 - Surface water supply of the United States, 1922, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:37","indexId":"wsp544","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"544","title":"Surface water supply of the United States, 1922, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp544","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1925, Surface water supply of the United States, 1922, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 544, iv, 140 p. ;23 cm., https://doi.org/10.3133/wsp544.","productDescription":"iv, 140 p. ;23 cm.","costCenters":[],"links":[{"id":139373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0544/report-thumb.jpg"},{"id":31702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0544/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697bd7","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528338,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32857,"text":"pp132J - 1925 - Aniakchak Crater, Alaska Peninsula","interactions":[],"lastModifiedDate":"2013-10-31T14:18:42","indexId":"pp132J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"J","title":"Aniakchak Crater, Alaska Peninsula","docAbstract":"The discovery of a gigantic crater northwest of Aniakchak Bay (see fig. 11) closes what had been thought to be a wide gap in the extensive series of volcanoes occurring at irregular intervals for nearly 600 miles along the axial line of the Alaska Peninsula and the Aleutian Islands. In this belt there are more active and recently active volcanoes than in all the rest of North America. Exclusive of those on the west side of Cook Inlet, which, however, belong to the same group, this belt contains at least 42 active or well-preserved volcanoes and about half as many mountains suspected or reported to be volcanoes. The locations of some of these mountains and the hot springs on the Alaska Peninsula and the Aleutian Islands are shown on a map prepared by G. A. Waring. Attention has been called to these volcanoes for nearly two centuries, but a record of their activity since the discovery of Alaska is far from being complete, and an adequate description of them as a group has never been written. Owing to their recent activity or unusual scenic beauty, some of the best known of the group are Mounts Katmai, Bogoslof, and Shishaldin, but there are many other beautiful and interesting cones and craters.","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter Contributions to General Geology, 1923-24","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp132J","usgsCitation":"Smith, W., 1925, Aniakchak Crater, Alaska Peninsula: U.S. Geological Survey Professional Paper 132, p. 139-145, https://doi.org/10.3133/pp132J.","productDescription":"p. 139-145","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":126719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132j/report-thumb.jpg"},{"id":12441,"rank":100,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132j/report.pdf","linkFileType":{"id":5,"text":"html"}}],"geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -159,56 ], [ -159,57.5 ], [ -157,57.5 ], [ -157,56 ], [ -159,56 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bffa","contributors":{"authors":[{"text":"Smith, Walter R.","contributorId":38619,"corporation":false,"usgs":true,"family":"Smith","given":"Walter R.","affiliations":[],"preferred":false,"id":209294,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":32856,"text":"pp132F - 1925 - Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation","interactions":[{"subject":{"id":32856,"text":"pp132F - 1925 - Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation","indexId":"pp132F","publicationYear":"1925","noYear":false,"chapter":"F","title":"Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation"},"predicate":"IS_PART_OF","object":{"id":45709,"text":"pp132 - 1925 - Shorter contributions to general geology, 1923-1924","indexId":"pp132","publicationYear":"1925","noYear":false,"title":"Shorter contributions to general geology, 1923-1924"},"id":1}],"isPartOf":{"id":45709,"text":"pp132 - 1925 - Shorter contributions to general geology, 1923-1924","indexId":"pp132","publicationYear":"1925","noYear":false,"title":"Shorter contributions to general geology, 1923-1924"},"lastModifiedDate":"2025-01-24T19:23:18.084697","indexId":"pp132F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"132","chapter":"F","title":"Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Shorter contributions to general geology, 1923-1924 (Professional Paper 132)","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp132F","usgsCitation":"Sears, J.D., and Bradley, W.H., 1925, Relations of the Wasatch and Green River formations in northwestern Colorado and southern Wyoming, with notes on oil shale in the Green River formation: U.S. Geological Survey Professional Paper 132, 18 p., https://doi.org/10.3133/pp132F.","productDescription":"18 p.","costCenters":[],"links":[{"id":388465,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4144.htm","linkFileType":{"id":5,"text":"html"}},{"id":122214,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0132f/report-thumb.jpg"},{"id":408816,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_93365.htm","linkFileType":{"id":5,"text":"html"}},{"id":60797,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0132f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado, Wyominng","otherGeospatial":"Wasatch and Green River Formations","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.6469,\n              40.4594\n            ],\n            [\n              -107.50,\n              40.4594\n            ],\n            [\n              -107.50,\n              41.3306\n            ],\n            [\n              -109.6469,\n              41.3306\n            ],\n            [\n              -109.6469,\n              40.4594\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69693f","contributors":{"authors":[{"text":"Sears, J. D.","contributorId":60604,"corporation":false,"usgs":true,"family":"Sears","given":"J.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":209292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradley, W. H.","contributorId":102452,"corporation":false,"usgs":true,"family":"Bradley","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":209293,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":32862,"text":"pp140E - 1925 - Correlation of the Eocene formations in Mississippi and Alabama","interactions":[],"lastModifiedDate":"2013-11-06T08:32:13","indexId":"pp140E","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"140","chapter":"E","title":"Correlation of the Eocene formations in Mississippi and Alabama","docAbstract":"During Eocene time the site of the boundary between the States of Mississippi and Alabama fell within the transition zone between the Mississippi embayment and the open Gulf of Mexico.  That different types of deposition proceeded simultaneously within these two regions may be inferred from the different facies which deposits of the same age exhibit on opposite sides of the State line.  In general, much clay and carbonaceous material were laid down in Mississippi, while shell marl, laminated sand, and limestone were being formed in Alabama.  The purpose of this paper is to point out the equivalences of formations of different facies in the two States.  The formations of different facies in the two States.  The correlation adopted in shown in the following table, all the formation names in which have been previously used, except Kosciusko sandstone, a new name proposed for a member of the Lisbon formation.","language":"English","doi":"10.3133/pp140E","usgsCitation":"Cooke, W., 1925, Correlation of the Eocene formations in Mississippi and Alabama: U.S. Geological Survey Professional Paper 140, 4 p., https://doi.org/10.3133/pp140E.","productDescription":"4 p.","startPage":"133","endPage":"136","costCenters":[],"links":[{"id":164351,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0140e/report-thumb.jpg"},{"id":271251,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0140e/report.pdf"}],"country":"United States","state":"Alabama;Mississippi","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.65,30.17 ], [ -91.65,35.0 ], [ -84.98,35.0 ], [ -84.98,30.17 ], [ -91.65,30.17 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad7e4b07f02db684570","contributors":{"authors":[{"text":"Cooke, Wythe","contributorId":34582,"corporation":false,"usgs":true,"family":"Cooke","given":"Wythe","email":"","affiliations":[],"preferred":false,"id":209302,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25061,"text":"wsp520C - 1925 - Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in <i>Contributions to the hydrology of the United States, 1923-1924</i>","interactions":[],"lastModifiedDate":"2013-12-13T12:10:37","indexId":"wsp520C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"C","title":"Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in <i>Contributions to the hydrology of the United States, 1923-1924</i>","docAbstract":"<p>Thousands of people are familiar with that part of Snake River where it flows for more than 300 miles in a general westward course across the plains of southern Idaho, but few have traversed the river where it flows northward and for 200 miles forms the boundary between Idaho and Oregon and for 30 miles the boundary between Idaho and Washington. Below the mining town of Homestead, Oreg., which is the end of a branch line of the Oregon Short Line Railroad, Snake River finds its way through the mountain ranges that seem to block its way to Columbia River in a canyon which, though not so well known, so majestic, nor so kaleidoscopic in color, is in some respects worthy of comparison with the Grand Canyon of the Colorado, for at some places it is deeper and narrower than the Grand Canyon at El Tovar. The Snake, unlike the Colorado, can be reached at many points through the valleys of tributary streams, and the early prospectors no doubt thoroughly explored all parts of the canyon. To traverse the river between Homestead, Oreg., and Lewiston, Idaho, is, however, a difficult undertaking and there are only a few records of boat journeys through the entire stretch.</p>\n<br/>\n<p>It has long been known that this portion of Snake River contains large potential water powers, but until recently no detailed surveys or examinations covering the entire stretch of the river had been made to determine their location or extent. A railroad has been proposed between Homestead and Lewiston which would provide a direct connection between the railroad systems of northern and southern Idaho.</p>\n<br/>\n<p>One function of the Geological Survey is to determine the possible interface between transportation routes on land and potential water-power development, and the information set forth in this paper has a bearing on that problem.</p>","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/wsp520C","collaboration":"This report is Chapter C in <i>Contributions to the hydrology of the United States, 1923-1924</i>. For more information, see <a href=\"http://pubs.er.usgs.gov/publication/wsp520\" target=\"_blank\">Water Supply Paper 520</a>.","usgsCitation":"Hoyt, W.G., 1925, Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in <i>Contributions to the hydrology of the United States, 1923-1924</i>: U.S. Geological Survey Water Supply Paper 520, iv, 25 p., https://doi.org/10.3133/wsp520C.","productDescription":"iv, 25 p.","startPage":"27","endPage":"51","numberOfPages":"29","costCenters":[],"links":[{"id":156696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520c/report-thumb.jpg"},{"id":279499,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520c/report.pdf"}],"country":"United States","state":"Idaho;Oregon","city":"Huntington;Lewiston","otherGeospatial":"Snake River","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -117.2829,44.2994 ], [ -117.2829,46.4442 ], [ -116.4274,46.4442 ], [ -116.4274,44.2994 ], [ -117.2829,44.2994 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681d29","contributors":{"authors":[{"text":"Hoyt, William Glenn","contributorId":14382,"corporation":false,"usgs":true,"family":"Hoyt","given":"William","email":"","middleInitial":"Glenn","affiliations":[],"preferred":false,"id":193148,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25059,"text":"wsp520A - 1925 - Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>","interactions":[],"lastModifiedDate":"2013-12-13T12:45:32","indexId":"wsp520A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"A","title":"Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>","docAbstract":"<p>Records of run-off in the Rocky Mountain States since the nineties and for a few stations since the eighties afford a means of studying the variation in the annual run-off in this region. The data presented in this report show that the variation in annual run-off differs in different areas in the Rocky Mountain region, owing to the differences in the sources of the precipitation in these areas. Except in the drainage basins of streams in northern Montana the year of lowest run-off shown by the records was 1902, when the run-ff at one station was only 36 per cent of the mean run-ff for the periods covered by the several records available. The percentage variation of run-ff for streams in different parts of Colorado is less for any one year than that for streams in the mountain region as a whole, and for streams in the same major drainage basin the annual variation is markedly similar. The influence of topography upon variation in annual run-ff for streams in Colorado is marked, the streams that rise in the central mountain region having a smaller range in variation than the streams that rise on the eastern or western edges of the central mountain mass. The streams that rise on the plains just east of the mountains have a greater variation than those of any of the mountain groups.</p>\n<br/>\n<p>The ratio of any 10-year mean to the mean for the entire period covered by the records ranges from 72 to 133 per cent. For the South Platte, Arkansas, and Rio Grande the run-off during the nineties was below the normal, but since about 1903 it has been above normal. For the Cache la Poudre low-water periods occurred during the eighties and from 1905 to 1922, but during the nineties the run-off was above the normal.</p>","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/wsp520A","collaboration":"This report is Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>. For more information, see <a href=\"http://pubs.er.usgs.gov/publication/wsp520\" target=\"_blank\">Water Supply Paper 520</a>.","usgsCitation":"Follansbee, R., 1925, Variation in annual run-off in the Rocky Mountain region: Chapter A in <i>Contributions to the hydrology of the United States, 1923-1924</i>: U.S. Geological Survey Water Supply Paper 520, iv, 14 p., https://doi.org/10.3133/wsp520A.","productDescription":"iv, 14 p.","startPage":"1","endPage":"14","numberOfPages":"20","costCenters":[],"links":[{"id":156694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520a/report-thumb.jpg"},{"id":279500,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520a/report.pdf"}],"country":"United States","state":"Colorado;Montana;Wyoming","otherGeospatial":"Arkansas River Basin;Big Horn River Basin;Colorado River Basin;Green River Basin;Rocky Mountains","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.05,36.98 ], [ -116.05,49.0 ], [ -102.02,49.0 ], [ -102.02,36.98 ], [ -116.05,36.98 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602b56","contributors":{"authors":[{"text":"Follansbee, Robert","contributorId":51713,"corporation":false,"usgs":true,"family":"Follansbee","given":"Robert","email":"","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":193146,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25060,"text":"wsp520B - 1925 - Additional ground-water supplies for the city of Enid, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wsp520B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"520","chapter":"B","title":"Additional ground-water supplies for the city of Enid, Oklahoma","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp520B","usgsCitation":"Renick, B., 1925, Additional ground-water supplies for the city of Enid, Oklahoma: U.S. Geological Survey Water Supply Paper 520, p. 15-26; iv, 129 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp520B.","productDescription":"p. 15-26; iv, 129 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":156695,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520b/report-thumb.jpg"},{"id":54073,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699b2b","contributors":{"authors":[{"text":"Renick, B. C.","contributorId":99587,"corporation":false,"usgs":true,"family":"Renick","given":"B. C.","affiliations":[],"preferred":false,"id":193147,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25068,"text":"wsp560C - 1925 - Index of analyses of natural waters in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:08:20","indexId":"wsp560C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"560","chapter":"C","title":"Index of analyses of natural waters in the United States","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp560C","usgsCitation":"Collins, W.D., and Howard, C.S., 1925, Index of analyses of natural waters in the United States: U.S. Geological Survey Water Supply Paper 560, p. 53-85; iii, 134 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp560C.","productDescription":"p. 53-85; iii, 134 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":157242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0560c/report-thumb.jpg"},{"id":54075,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0560c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fae4b07f02db5f432c","contributors":{"authors":[{"text":"Collins, W. D.","contributorId":37713,"corporation":false,"usgs":true,"family":"Collins","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":193158,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":193159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":25067,"text":"wsp560B - 1925 - Chemical character of ground waters of the northern Great Plains","interactions":[],"lastModifiedDate":"2013-01-08T14:22:50","indexId":"wsp560B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"560","chapter":"B","title":"Chemical character of ground waters of the northern Great Plains","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp560B","usgsCitation":"Riffenburg, H., 1925, Chemical character of ground waters of the northern Great Plains: U.S. Geological Survey Water Supply Paper 560, p. 31-52; iii, 134 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp560B.","productDescription":"p. 31-52; iii, 134 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":157225,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0560B/report-thumb.jpg"},{"id":265413,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0560B/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e479a","contributors":{"authors":[{"text":"Riffenburg, H.B.","contributorId":32197,"corporation":false,"usgs":true,"family":"Riffenburg","given":"H.B.","affiliations":[],"preferred":false,"id":193157,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":25066,"text":"wsp560A - 1925 - Water power and irrigation in the Madison River basin, Montana","interactions":[],"lastModifiedDate":"2013-01-08T14:21:56","indexId":"wsp560A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1925","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":"560","chapter":"A","title":"Water power and irrigation in the Madison River basin, Montana","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp560A","usgsCitation":"Deeds, J., and White, W.N., 1925, Water power and irrigation in the Madison River basin, Montana: U.S. Geological Survey Water Supply Paper 560, p. 1-30; iii, 134 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp560A.","productDescription":"p. 1-30; iii, 134 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":157224,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0560A/report-thumb.jpg"},{"id":265412,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0560A/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696837","contributors":{"authors":[{"text":"Deeds, J.F.","contributorId":14854,"corporation":false,"usgs":true,"family":"Deeds","given":"J.F.","email":"","affiliations":[],"preferred":false,"id":193155,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"White, W. N.","contributorId":69954,"corporation":false,"usgs":true,"family":"White","given":"W.","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":193156,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
]}