The purpose of this report is to present the facts regarding the available water supply of the Green River Basin and other data that will be helpful in planning to put this water to beneficial use. For some parts of the basin a mass of information is available; for other parts the data are less complete. An attempt is made in this report to present an analysis of all this information, supplemented by personal field studies, in such a way as to indicate the economic factors involved in utilizing the waters of the basin, and also to give facts from which the relative value of the irrigation and power projects may be readily deduced.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp618","usgsCitation":"Woolley, R.R., 1930, The Green River and its utilization: U.S. Geological Survey Water Supply Paper 618, Report: xv, 456 p.; Plate: 38.00 x 53.00 inches, https://doi.org/10.3133/wsp618.","productDescription":"Report: xv, 456 p.; Plate: 38.00 x 53.00 inches","numberOfPages":"529","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29838,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0618/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29837,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0618/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139563,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0618/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Green River","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c43e","contributors":{"authors":[{"text":"Woolley, Ralf Rumel","contributorId":46511,"corporation":false,"usgs":true,"family":"Woolley","given":"Ralf","email":"","middleInitial":"Rumel","affiliations":[],"preferred":false,"id":146152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25075,"text":"wsp636C - 1930 - The New England flood of November 1927","interactions":[{"subject":{"id":25075,"text":"wsp636C - 1930 - The New England flood of November 1927","indexId":"wsp636C","publicationYear":"1930","noYear":false,"chapter":"C","title":"The New England flood of November 1927"},"predicate":"IS_PART_OF","object":{"id":1449,"text":"wsp636 - 1930 - Contributions to the hydrology of the United States, 1929","indexId":"wsp636","publicationYear":"1930","noYear":false,"title":"Contributions to the hydrology of the United States, 1929"},"id":1}],"isPartOf":{"id":1449,"text":"wsp636 - 1930 - Contributions to the hydrology of the United States, 1929","indexId":"wsp636","publicationYear":"1930","noYear":false,"title":"Contributions to the hydrology of the United States, 1929"},"lastModifiedDate":"2023-06-12T18:41:29.317533","indexId":"wsp636C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1930","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":"636","chapter":"C","title":"The New England flood of November 1927","docAbstract":"No abstract available.
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","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp636D","usgsCitation":"McGlashan, H., 1930, Surface water supply of the San Joaquin River Basin, California, 1895-1927: U.S. Geological Survey Water Supply Paper 636, 68 p., https://doi.org/10.3133/wsp636D.","productDescription":"68 p.","startPage":"101","endPage":"168","numberOfPages":"68","costCenters":[{"id":154,"text":"California Water Science Center","active":true,"usgs":true},{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":264569,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0636d/report-thumb.jpg"},{"id":264568,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0636d/report.pdf","size":"7006","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"California","otherGeospatial":"San Joaquin River Basin","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4affe4b07f02db697c8e","contributors":{"authors":[{"text":"McGlashan, H.D.","contributorId":81876,"corporation":false,"usgs":true,"family":"McGlashan","given":"H.D.","affiliations":[],"preferred":false,"id":193170,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25074,"text":"wsp636B - 1930 - Suspended matter in the Colorado River in 1925-1928","interactions":[{"subject":{"id":25074,"text":"wsp636B - 1930 - Suspended matter in the Colorado River in 1925-1928","indexId":"wsp636B","publicationYear":"1930","noYear":false,"chapter":"B","title":"Suspended matter in the Colorado River in 1925-1928"},"predicate":"IS_PART_OF","object":{"id":1449,"text":"wsp636 - 1930 - Contributions to the hydrology of the United States, 1929","indexId":"wsp636","publicationYear":"1930","noYear":false,"title":"Contributions to the hydrology of the United States, 1929"},"id":1}],"isPartOf":{"id":1449,"text":"wsp636 - 1930 - Contributions to the hydrology of the United States, 1929","indexId":"wsp636","publicationYear":"1930","noYear":false,"title":"Contributions to the hydrology of the United States, 1929"},"lastModifiedDate":"2018-12-17T09:19:24","indexId":"wsp636B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1930","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":"636","chapter":"B","title":"Suspended matter in the Colorado River in 1925-1928","docAbstract":"Determinations of the quantity of solid material carried by the Colorado River are necessary for the proper consideration of plans for the development of the resources of the river. Much of the material carried by the river will be deposited in the proposed reservoirs and eventually will occupy a large part of the capacity of the reservoirs, so that their effectiveness for flood control or river regulation will be greatly decreased. A capacity of 6,000,000 acre-feet is reserved for silt storage in plans for a reservoir in Boulder Canyon that is to have a maximum capacity of about 25,000,000 to 30,000,000 acre-feet. It has been estimated that such a silt-storage capacity will not be entirely used for nearly 100 years.1 However, the discharge of sediment including the sediment from the Gila was reported to be more than 1,000,000 acre-feet for the four years 1909-19122 and a similar quantity for the four years 1912-1916.3
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1930 - Petrography of the Pioche district, Lincoln County, Nevada","indexId":"pp158D","publicationYear":"1930","noYear":false,"chapter":"D","title":"Petrography of the Pioche district, Lincoln County, Nevada"},"predicate":"IS_PART_OF","object":{"id":45708,"text":"pp158 - 1930 - Shorter contributions to general geology, 1929","indexId":"pp158","publicationYear":"1930","noYear":false,"title":"Shorter contributions to general geology, 1929"},"id":7},{"subject":{"id":39352,"text":"pp158F - 1930 - Contact metamorphism of the rocks in the Pend Oreille district, northern Idaho","indexId":"pp158F","publicationYear":"1930","noYear":false,"chapter":"F","title":"Contact metamorphism of the rocks in the Pend Oreille district, northern Idaho"},"predicate":"IS_PART_OF","object":{"id":45708,"text":"pp158 - 1930 - Shorter contributions to general geology, 1929","indexId":"pp158","publicationYear":"1930","noYear":false,"title":"Shorter contributions to general geology, 1929"},"id":8},{"subject":{"id":39353,"text":"pp158H - 1930 - The flora of the Frontier formation","indexId":"pp158H","publicationYear":"1930","noYear":false,"chapter":"H","title":"The flora of the Frontier formation"},"predicate":"IS_PART_OF","object":{"id":45708,"text":"pp158 - 1930 - Shorter contributions to general geology, 1929","indexId":"pp158","publicationYear":"1930","noYear":false,"title":"Shorter contributions to general geology, 1929"},"id":9}],"lastModifiedDate":"2023-07-24T15:03:23.639857","indexId":"pp158","displayToPublicDate":"1930-01-02T00:00:00","publicationYear":"1930","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":"158","title":"Shorter contributions to general geology, 1929","docAbstract":"Thin beds that consist almost wholly of euhedral analcite crystals occur at five or more horizons in the upper half of the Green River formation of Utah and Colorado, a series of Eocene lake beds that contain large deposits of oil shale. Most of these beds contain also minute crystals of apophyllite. The analcite crystals in some beds are cemented only by chalcedony, but in other beds that have less analcite the matrix is tuffaceous and consists of chalcedony in which are embedded splinters of feldspar, hornblende, and quartz, laths of biotite, and euhedral crystals of sanidine, apatite, and zircon. Analcite occurs plentifully also, disseminated in many of the oil-shale beds, and locally makes up as much as 16 per cent of weight of the rock. In these beds the analcite is accompanied by apophyllite, euhedral crystals of sanidine and orthoclase, angular fragments of quartz, and a little volcanic glass. The rocks associated with the beds of analcite and analcite-bearing oil shale contain salt-crystal cavities, that strongly suggest the former presence of glauberite and anhydrite.
Both clastic and hydrothermal hypotheses for the origin of the zeolites are considered and dismissed in the paper. The field and microscopic evidence presented leads to the conclusion that all the analcite and apophyllite formed in place on the lake bottom as a result of interactions between salts dissolved in the lake water and the dissolution products of volcanic ash that fell into the lake.
Meerschaum, or fibrous sepiolite, occurs in several thin beds near the top of the Green River formation in Duchesne County, Utah. It is mixed with structureless organic matter like that in the oil shale and apparently formed in place on the lake bottom.
Chemical analyses of the analcite rock and of the sepiolite are given.
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1929 - Shorter contributions to general geology, 1928","interactions":[{"subject":{"id":32799,"text":"pp154C - 1929 - Salinity of the water of Chesapeake Bay","indexId":"pp154C","publicationYear":"1929","noYear":false,"chapter":"C","title":"Salinity of the water of Chesapeake Bay"},"predicate":"IS_PART_OF","object":{"id":45718,"text":"pp154 - 1929 - Shorter contributions to general geology, 1928","indexId":"pp154","publicationYear":"1929","noYear":false,"title":"Shorter contributions to general geology, 1928"},"id":1},{"subject":{"id":32818,"text":"pp154A - 1929 - Moraines and shore lines of the Lake Superior Basin","indexId":"pp154A","publicationYear":"1929","noYear":false,"chapter":"A","title":"Moraines and shore lines of the Lake Superior Basin"},"predicate":"IS_PART_OF","object":{"id":45718,"text":"pp154 - 1929 - Shorter contributions to general geology, 1928","indexId":"pp154","publicationYear":"1929","noYear":false,"title":"Shorter contributions to general geology, 1928"},"id":2},{"subject":{"id":39338,"text":"pp154D - 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