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The purpose of this report is to present the facts regarding available water supply and all known dam sites on Colorado River between Cataract Canyon, Utah, and Parker, Ariz., and to show the relative value of these dam sites. To determine the relative value of the dam sites, a comprehensive plan of development for Colorado River below the mouth of Green River is presented that will provide for the maximum practicable utilization of the potential power, maximum preservation of water for irrigation, effective elimination of the flood menace, and adequate solution of the silt problem. This plan, which is preliminary and is offered by the writer to show the basis for his conclusions relative to flood control, irrigation, power development, and silt storage, contemplates the construction of 13 dams making available 3,383 feet of head for the development of power and a maximum of 42,000,000 acre-feet of storage capacity for the control of floods, equalization of flow, and storage of silt.

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No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp539","usgsCitation":"Pardee, J.T., 1925, Geology and ground-water resources of Townsend Valley, Montana: U.S. Geological Survey Water Supply Paper 539, iv, 61 p., https://doi.org/10.3133/wsp539.","productDescription":"iv, 61 p.","costCenters":[],"links":[{"id":139060,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0539/report-thumb.jpg"},{"id":28478,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696a34","contributors":{"authors":[{"text":"Pardee, Joseph Thomas","contributorId":86319,"corporation":false,"usgs":true,"family":"Pardee","given":"Joseph","email":"","middleInitial":"Thomas","affiliations":[],"preferred":false,"id":145188,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1073,"text":"wsp537 - 1925 - A study of coastal ground water, with special reference to Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:05:18","indexId":"wsp537","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":"537","title":"A study of coastal ground water, with special reference to Connecticut","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp537","usgsCitation":"Brown, J.S., 1925, A study of coastal ground water, with special reference to Connecticut: U.S. Geological Survey Water Supply Paper 537, viii, 101 p. :illus., VII pl. (incl. fold. col. map), tables, diagrs. ;23 cm., https://doi.org/10.3133/wsp537.","productDescription":"viii, 101 p. :illus., VII pl. (incl. fold. col. map), tables, diagrs. ;23 cm.","costCenters":[],"links":[{"id":138037,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0537/report-thumb.jpg"},{"id":25758,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0537/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0537/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a620a","contributors":{"authors":[{"text":"Brown, John Stafford","contributorId":81882,"corporation":false,"usgs":true,"family":"Brown","given":"John","email":"","middleInitial":"Stafford","affiliations":[],"preferred":false,"id":143133,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":1086,"text":"wsp499 - 1925 - The Papago country, Arizona: A geographic, geologic, and hydrologic reconnaissance, with a guide to desert watering places","interactions":[],"lastModifiedDate":"2022-12-29T20:29:54.824264","indexId":"wsp499","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":"499","title":"The Papago country, Arizona: A geographic, geologic, and hydrologic reconnaissance, with a guide to desert watering places","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp499","usgsCitation":"Bryan, K., 1925, The Papago country, Arizona: A geographic, geologic, and hydrologic reconnaissance, with a guide to desert watering places: U.S. Geological Survey Water Supply Paper 499, Report: xviii, 436 p.; 4 Plates: 18.80 x 39.75 inches or smaller, https://doi.org/10.3133/wsp499.","productDescription":"Report: xviii, 436 p.; 4 Plates: 18.80 x 39.75 inches or smaller","costCenters":[],"links":[{"id":411187,"rank":7,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24579.htm","linkFileType":{"id":5,"text":"html"}},{"id":25806,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0499/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25805,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0499/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25804,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0499/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25803,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0499/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25802,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0499/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137124,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0499/report-thumb.jpg"}],"country":"United States","state":"Arizona","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -110.906,\n 31.336\n ],\n [\n -110.906,\n 33.467\n ],\n [\n -114.8294,\n 33.467\n ],\n [\n -114.8294,\n 31.336\n ],\n [\n -110.906,\n 31.336\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67aeac","contributors":{"authors":[{"text":"Bryan, Kirk","contributorId":37308,"corporation":false,"usgs":true,"family":"Bryan","given":"Kirk","email":"","affiliations":[],"preferred":false,"id":143155,"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. 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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":25061,"text":"wsp520C - 1925 - Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in Contributions to the hydrology of the United States, 1923-1924","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 Contributions to the hydrology of the United States, 1923-1924","docAbstract":"

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.

\n
\n

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.

\n
\n

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.

","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 Contributions to the hydrology of the United States, 1923-1924. For more information, see Water Supply Paper 520.","usgsCitation":"Hoyt, W.G., 1925, Power resources of Snake River between Huntington, Oregon and Lewiston, Idaho: Chapter C in Contributions to the hydrology of the United States, 1923-1924: 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":25062,"text":"wsp520D - 1925 - Base exchange in ground water by silicates as illustrated in Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wsp520D","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":"D","title":"Base exchange in ground water by silicates as illustrated in Montana","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp520D","usgsCitation":"Renick, B., 1925, Base exchange in ground water by silicates as illustrated in Montana: U.S. Geological Survey Water Supply Paper 520, p. 53-72; iv, 129 p. :ill., maps ;23 cm., https://doi.org/10.3133/wsp520D.","productDescription":"p. 53-72; iv, 129 p. :ill., maps ;23 cm.","costCenters":[],"links":[{"id":156697,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520d/report-thumb.jpg"},{"id":54074,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6492bc","contributors":{"authors":[{"text":"Renick, B. C.","contributorId":99587,"corporation":false,"usgs":true,"family":"Renick","given":"B. C.","affiliations":[],"preferred":false,"id":193149,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25063,"text":"wsp520E - 1925 - The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","interactions":[{"subject":{"id":25063,"text":"wsp520E - 1925 - The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","indexId":"wsp520E","publicationYear":"1925","noYear":false,"chapter":"E","title":"The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle"},"predicate":"IS_PART_OF","object":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"id":1}],"isPartOf":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"lastModifiedDate":"2021-08-30T21:13:52.498817","indexId":"wsp520E","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":"E","title":"The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle","docAbstract":"

The Dakota sandstone and the overlying dense plastic shales form the most remarkable artesian basin in the United States with respect to its great extent, the long distances through which its water has percolated from the outcrops of the sandstone in the western mountains to the areas of artesian flow, and especially the tremendous pressure under which the water in the sandstone was originally by thick and continuous cover of impermeable shales. In 1882 a well was drilled to the Dakota sandstone at Aberdeen, S. Dak., by the Chicago, Milwaukee & St. Paul Railway Co. This well was reported by Nettleton1 to have been \"the first bore put down which reached the artesian basin of the Dakotas.\" In 1896 Darton2 estimated that about 400 artesian wells had been drilled to the Dakota sandstone, presumably in South Dakota and adjacent parts of the artesian basin in North Dakota which he investigated.3 The strongest of these wells had pressures ranging from 100 to more than 200 pounds to the square inch and flows ranging from 1,000 to more than 4,000 gallons a minute.

\n
\n

The present brief paper is based chiefly on the data that have been obtained in the successive surveys in regard to about 230 artesian wells in or near the Edgeley quadrangle. A table of these well data is on file in the United States Geological Survey and is to be published in the detailed report on the geology and hydrology of the Edgeley and La Moure quadrangles that has been prepared by Mr. Hard. The well data obtained by Mr. Hard have already been published in a report prepared by him in his capacity as State flood-control engineer.

","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/wsp520E","usgsCitation":"Meinzer, O.E., and Hard, H.A., 1925, The artesian water supply of the Dakota sandstone in North Dakota, with special reference to the Edgeley quadrangle: U.S. Geological Survey Water Supply Paper 520, iv, 23 p., https://doi.org/10.3133/wsp520E.","productDescription":"iv, 23 p.","startPage":"73","endPage":"95","numberOfPages":"31","costCenters":[],"links":[{"id":388207,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24584.htm"},{"id":156698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0520e/report-thumb.jpg"},{"id":279498,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0520e/report.pdf"}],"country":"United States","state":"North Dakota","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -99.0,46.0 ], [ -99.0,46.5 ], [ -98.5,46.5 ], [ -98.5,46.0 ], [ -99.0,46.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db6697cb","contributors":{"authors":[{"text":"Meinzer, Oscar E.","contributorId":83436,"corporation":false,"usgs":true,"family":"Meinzer","given":"Oscar","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":193150,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hard, Herbert A.","contributorId":88205,"corporation":false,"usgs":true,"family":"Hard","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":193151,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25064,"text":"wsp520F - 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","interactions":[{"subject":{"id":25064,"text":"wsp520F - 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","indexId":"wsp520F","publicationYear":"1925","noYear":false,"chapter":"F","title":"Temperature of water available for industrial use in the United States: Chapter F in Contributions to the hydrology of the United States, 1923-1924"},"predicate":"IS_PART_OF","object":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"id":1}],"isPartOf":{"id":1737,"text":"wsp520 - 1925 - Contributions to the hydrology of the United States, 1923-1924","indexId":"wsp520","publicationYear":"1925","noYear":false,"title":"Contributions to the hydrology of the United States, 1923-1924"},"lastModifiedDate":"2017-09-11T19:06:02","indexId":"wsp520F","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":"F","title":"Temperature of water available for industrial use in the United States: Chapter F in Contributions to the hydrology of the United States, 1923-1924","docAbstract":"

The importance of water supply as a limiting factor in industrial development is becoming more evident each year. 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.

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