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,{"id":53635,"text":"ofr4876 - 1948 - Reconnaissance study of ground water in the vicinity of Ruidoso, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr4876","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"48-76","title":"Reconnaissance study of ground water in the vicinity of Ruidoso, New Mexico","language":"ENGLISH","doi":"10.3133/ofr4876","usgsCitation":"Murrary, C., and Jones, R.S., 1948, Reconnaissance study of ground water in the vicinity of Ruidoso, New Mexico: U.S. Geological Survey Open-File Report 48-76, 22 p., https://doi.org/10.3133/ofr4876.","productDescription":"22 p.","costCenters":[],"links":[{"id":177068,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1948/0076/report-thumb.jpg"},{"id":87510,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1948/0076/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87511,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1948/0076/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636719","contributors":{"authors":[{"text":"Murrary, C.R.","contributorId":16906,"corporation":false,"usgs":true,"family":"Murrary","given":"C.R.","email":"","affiliations":[],"preferred":false,"id":247967,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jones, R. S.","contributorId":26288,"corporation":false,"usgs":true,"family":"Jones","given":"R.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":247968,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":945,"text":"wsp968B - 1948 - Floods of the Puyallup and Chehalis River Basins, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp968B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"968","chapter":"B","title":"Floods of the Puyallup and Chehalis River Basins, Washington","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp968B","usgsCitation":"Anderson, I.E., 1948, Floods of the Puyallup and Chehalis River Basins, Washington: U.S. Geological Survey Water Supply Paper 968, 61-124 p. :ill., maps (1 folded) ;23 cm., https://doi.org/10.3133/wsp968B.","productDescription":"61-124 p. :ill., maps (1 folded) ;23 cm.","costCenters":[],"links":[{"id":136943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0968b/report-thumb.jpg"},{"id":25445,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0968b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df861","contributors":{"authors":[{"text":"Anderson, Irving Elmer","contributorId":25544,"corporation":false,"usgs":true,"family":"Anderson","given":"Irving","email":"","middleInitial":"Elmer","affiliations":[],"preferred":false,"id":142899,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55608,"text":"ofr485 - 1948 - Uses of water in upper Bruneau River","interactions":[],"lastModifiedDate":"2012-02-02T00:11:55","indexId":"ofr485","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"48-5","title":"Uses of water in upper Bruneau River","language":"ENGLISH","doi":"10.3133/ofr485","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Uses of water in upper Bruneau River: U.S. Geological Survey Open-File Report 48-5, NA, https://doi.org/10.3133/ofr485.","productDescription":"NA","costCenters":[],"links":[{"id":174208,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1948/0005/report-thumb.jpg"},{"id":88060,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1948/0005/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88061,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1948/0005/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a16e4b07f02db603cd5","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":532370,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4136,"text":"cir32 - 1948 - Flood of September 1946 at San Antonio, Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:04:24","indexId":"cir32","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"32","title":"Flood of September 1946 at San Antonio, Texas","docAbstract":"<p>A flood occurred in the streams in and near San Antonio, Teat., during the early morning hours of September 27, 1946, as a result of heavy rains falling during the previous night. Much property damage occurred in San Antonio and below, and four lives were lost. . It is the purpose of the present report to describe this flood and its relation to the flood of September 10, 1921 the greatest of record since 1819.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir32","usgsCitation":"Breeding, S., 1948, Flood of September 1946 at San Antonio, Texas: U.S. Geological Survey Circular 32, 19 p., https://doi.org/10.3133/cir32.","productDescription":"19 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":31243,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0032/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eebd0","contributors":{"authors":[{"text":"Breeding, Seth D.","contributorId":89505,"corporation":false,"usgs":true,"family":"Breeding","given":"Seth D.","affiliations":[],"preferred":false,"id":148269,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3831,"text":"cir23 - 1948 - Reservoirs in the United States","interactions":[{"subject":{"id":3831,"text":"cir23 - 1948 - Reservoirs in the United States","indexId":"cir23","publicationYear":"1948","noYear":false,"title":"Reservoirs in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","indexId":"wsp1360A","publicationYear":"1956","noYear":false,"chapter":"A","title":"Reservoirs in the United States"},"id":1}],"supersededBy":{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","indexId":"wsp1360A","publicationYear":"1956","noYear":false,"title":"Reservoirs in the United States"},"lastModifiedDate":"2017-09-07T12:11:03","indexId":"cir23","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"23","title":"Reservoirs in the United States","docAbstract":"<p>Man has engaged in the control of flowing water since history began. Among his early recorded efforts were reservoirs for muncipal water-supplies constructed near ancient Jerusalem to store water which was brought there in masonry conduits. <u>1</u>/ &nbsp;Irrigation was practiced in Egypt as early as 2000 B. C. There the \"basin system\" was used from ancient times until the 19th century. The land was divided , into basins of approximately 40,000 acres, separated by earthen dikes. <u>2</u>/ &nbsp;Flood waters of the Nile generally inundated the basins through canals, many of which were built by the Pharaohs. Even then the economic consequences of a deficient annual flood were recognized. Lake Maeris, which according to Herodotus was an ancient storage reservoir, is said to have had an area of 30,000 acres. In India, the British found at the time of their occupancy of the Presidency of Madras about 50,000 reservoirs for irrigation, many believed to be of ancient construction. <u>3</u>/ During the period 115-130 A. D. reservoirs were built to improve the water-supply of Athens. Much has been written concerning the elaborate collection and distribution system built to supply Rome, and parts of it remain to this day as monuments to the engineering skill employed by the Romans in solving the problem of large-scale municipal water-supplies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir23","usgsCitation":"Harbeck, G.E., 1948, Reservoirs in the United States: U.S. Geological Survey Circular 23, 72 p., https://doi.org/10.3133/cir23.","productDescription":"72 p.","numberOfPages":"82","costCenters":[],"links":[{"id":30904,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1948/0023/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118132,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1948/0023/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c68a","contributors":{"authors":[{"text":"Harbeck, G. Earl Jr.","contributorId":18736,"corporation":false,"usgs":true,"family":"Harbeck","given":"G.","suffix":"Jr.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":147693,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57084,"text":"ofr4884 - 1948 - Ground water in the Anadarko area [Caddo County], Oklahoma","interactions":[],"lastModifiedDate":"2020-06-12T19:29:36.224537","indexId":"ofr4884","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"48-84","title":"Ground water in the Anadarko area [Caddo County], Oklahoma","docAbstract":"This report offers a preliminary interpretation of the geology and ground-water hydrology of the Anadarko area, Oklahoma. L.V. Davis prepared the accompanying map from aerial photographs and furnished much of the geologic information, and records of the State Mineral Survey (WPA) were used in the preparation of the section on the Rush Springs sandstone.\r\n(available as photostat copy only)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr4884","usgsCitation":"Schoff, S., 1948, Ground water in the Anadarko area [Caddo County], Oklahoma: U.S. Geological Survey Open-File Report 48-84, Report: 7 p.; 1 Plate: 8.93 x 6.17 inches, https://doi.org/10.3133/ofr4884.","productDescription":"Report: 7 p.; 1 Plate: 8.93 x 6.17 inches","costCenters":[],"links":[{"id":375575,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1948/0084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1948/0084/report-thumb.jpg"},{"id":375574,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1948/0084/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oklahoma","county":"Caddo County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.3181,35.5502],[-98.3187,35.5479],[-98.3193,35.5438],[-98.3193,35.5429],[-98.3142,35.5406],[-98.3119,35.5401],[-98.3085,35.541],[-98.3051,35.5437],[-98.305,35.3744],[-98.0985,35.3767],[-98.0906,34.8581],[-98.1937,34.8571],[-98.5091,34.8557],[-98.6206,34.8565],[-98.6177,35.0994],[-98.616,35.2038],[-98.6216,35.2038],[-98.6209,35.4639],[-98.6199,35.552],[-98.3181,35.5502]]]},\"properties\":{\"name\":\"Caddo\",\"state\":\"OK\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d93f","contributors":{"authors":[{"text":"Schoff, Stuart L.","contributorId":104467,"corporation":false,"usgs":true,"family":"Schoff","given":"Stuart L.","affiliations":[],"preferred":false,"id":256236,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":312,"text":"wsp1045 - 1948 - Surface water supply of Hawaii : July 1, 1944, to June 30, 1945","interactions":[],"lastModifiedDate":"2012-02-02T00:05:10","indexId":"wsp1045","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1045","title":"Surface water supply of Hawaii : July 1, 1944, to June 30, 1945","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1045","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of Hawaii : July 1, 1944, to June 30, 1945: U.S. Geological Survey Water Supply Paper 1045, iv, 130 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1045.","productDescription":"iv, 130 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":135996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1045/report-thumb.jpg"},{"id":24874,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697875","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":527300,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":593,"text":"wsp1061 - 1948 - Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1061","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1061","title":"Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1061","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part XI, Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1061, x, 431 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1061.","productDescription":"x, 431 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136310,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1061/report-thumb.jpg"},{"id":25156,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1061/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968ac","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":527565,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":592,"text":"wsp1060 - 1948 - Surface water supply of the United States, 1946, Part X, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1060","title":"Surface water supply of the United States, 1946, Part X, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1060","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part X, The Great Basin: U.S. Geological Survey Water Supply Paper 1060, vii, 198 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1060.","productDescription":"vii, 198 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136309,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1060/report-thumb.jpg"},{"id":25155,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968ab","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":527564,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":602,"text":"wsp1058 - 1948 - Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1058","title":"Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1058","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part VIII, Western Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1058, ix, 344 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1058.","productDescription":"ix, 344 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1058/report-thumb.jpg"},{"id":25165,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1058/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696981","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":527574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":595,"text":"wsp1064 - 1948 - Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1064","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1064","title":"Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1064","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1948, Surface water supply of the United States, 1946, Part XIV, Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1064, viii, 255 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1064.","productDescription":"viii, 255 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136312,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1064/report-thumb.jpg"},{"id":25158,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1064/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696873","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":527567,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1355,"text":"wsp997 - 1948 - Floods in Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:05:13","indexId":"wsp997","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"997","title":"Floods in Colorado","docAbstract":"The first records of floods in Colorado antedated the settlement of the State by about 30 years. These were records of floods on the Arkansas and Republican Rivers in 1826. Other floods noted by traders, hunters and emigrants, some of whom were on their way to the Far West, occurred in 1844 on the Arkansas River, and by inference on the South Platte River. Other early floods were those on the Purgatoire, the Lower Arkansas, and the San Juan Rivers about 1859. The most serious flood since settlement began was that on the Arkansas River during June 1921, which caused the loss of about 100 lives and an estimated property loss of $19,000,000. Many floods of lesser magnitude have occurred, and some of these have caused loss of life and very considerable property damage. Topography is the chief factor in determining the location of storms and resulting floods. These occur most frequently on the eastern slope of the Front Range. In the mountains farther west precipitation is insufficient to cause floods except during periods of melting snow, in June. In the southwestern part of the State, where precipitation during periods of melting snow is insufficient to cause floods, the severest floods yet experienced resulted from heavy rains in September 1909 and October 1911. \r\n\r\nIn the eastern foothills region, usually below an altitude of about 7,500 feet and extending for a distance of about 50 miles east of the mountains, is a zone subject to rainfalls of great intensity known as cloudbursts. These cloudbursts are of short duration and are confined to very small areas. At times the intensity is so great as to make breathing difficult for those exposed to a storm. The areas of intense rainfall are so small that Weather Bureau precipitation stations have not been located in them. Local residents, being cloudburst conscious, frequently measure the rainfall in receptacles in their yards, and such records constitute the only source of information regarding the intensity. \r\n\r\nA flood resulting from a cloudburst rises so quickly that it is usually described as a 'wall of water.' It has a peak duration of only a few minutes, followed by a rapid subsidence. Nearly 90 cloudburst floods in Colorado are described in varying detail in this report. The earliest recorded cloudburst--called at that time a waterspout--occurred in Golden Gate Gulch, July 14, 1872. The 'wall of water' was described as a 'perpendicular breast of 10 or 12 feet.' A cloudburst flood on Kiowa Creek in May 1878 caused the loss of a standard-gage locomotive, and although search was made by means of long metallic rods, the locomotive was never recovered, as bedrock was about 50 feet below the creek bed. All available information relative to floods in Colorado, beginning with the flood of 1826 on the Arkansas River, is presented in this report, although for many of the earlier floods estimates of discharge are lacking. Floods throughout a large part of the State have occurred in 1844, June 1864, June 1884, May 1894, and June 1921. The highest floods of record were on the larger streams and occurred as follows: South Platte River, June 1921; Rio Grande, June 1927; Colorado River, June and July 1884; San Juan River, October 1911. \r\n\r\nThe greatest floods on the plains streams occurred during May and June 1935 and were caused by cloudbursts. Ranchers living in the vicinity noted rainfalls as high as 24 inches in a 13-hour period, measurements being made in a stock tank. The effect of settlement on channel capacities can be clearly traced. When settlement began, and with it the beginning of the livestock industry, the plains were thickly covered with a luxuriant growth of grasses. With the development of the livestock industry the grass cover was grazed so closely that it afforded little protection against erosion during the violent rains and resulting floods. The intensive grazing packed the soil so hard as to increase greatly the percentage of rainfall that entered the streams. This co","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp997","isbn":"pbk","usgsCitation":"Follansbee, R., and Sawyer, L.R., 1948, Floods in Colorado: U.S. Geological Survey Water Supply Paper 997, iv, 151 p. :ill., photos ;24 cm., https://doi.org/10.3133/wsp997.","productDescription":"iv, 151 p. :ill., photos ;24 cm.","costCenters":[],"links":[{"id":137557,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0997/report-thumb.jpg"},{"id":26437,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0997/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dfe4b07f02db5e329f","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":143619,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sawyer, Leon R.","contributorId":19932,"corporation":false,"usgs":true,"family":"Sawyer","given":"Leon","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143618,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":2775,"text":"wsp1047 - 1948 - Public water supplies in eastern Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:33:33","indexId":"wsp1047","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1948","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":"1047","title":"Public water supplies in eastern Texas","docAbstract":"<p>This report gives a summarized description of the public water supplies in 77 counties of eastern Texas, extending from the Louisiana boundary to a northsouth line approximately along the ninety-seventh meridian. It gives the available data as follows for each of 323 communities: The population of the community; the name of the official from whom the information was obtained; the ownership of the waterworks, whether private or municipal; the source of supply, whether ground or surface water; the amount of water consumed; the facilities for storage; the number of customers served; the character of the chemical and sanitary treatment of the water, if any; and the chemical analyses of the water. Where ground water is used the following is also given: Records of wells, including drillers' logs; character of the pumping equipment; yield of the wells and water level records where they are available.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1047","usgsCitation":"Sundstrom, R.W., Hastings, W., and Broadhurst, W., 1948, Public water supplies in eastern Texas: U.S. Geological Survey Water Supply Paper 1047, xi, 285 p., https://doi.org/10.3133/wsp1047.","productDescription":"xi, 285 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":29223,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1047/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138676,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1047/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db65677e","contributors":{"authors":[{"text":"Sundstrom, Raymond W.","contributorId":8080,"corporation":false,"usgs":true,"family":"Sundstrom","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145764,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hastings, W.W.","contributorId":11203,"corporation":false,"usgs":true,"family":"Hastings","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":145765,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Broadhurst, W. L.","contributorId":55414,"corporation":false,"usgs":true,"family":"Broadhurst","given":"W. L.","affiliations":[],"preferred":false,"id":145766,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":70215757,"text":"70215757 - 1948 - Some solutional features of the limestone near Lexington, Kentucky","interactions":[],"lastModifiedDate":"2020-10-28T19:58:10.057194","indexId":"70215757","displayToPublicDate":"1948-10-28T14:34:17","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1472,"text":"Economic Geology","active":true,"publicationSubtype":{"id":10}},"title":"Some solutional features of the limestone near Lexington, Kentucky","docAbstract":"<p><span>Field work on the Ordovician limestones and shales of the Lexington area, Kentucky, has shown that no appreciable quantity of ground water is transmitted through interstitial openings in these rocks. Ground-water movement is restricted to joint planes and, to a lesser extent, bedding planes that have been enlarged by solution. Studies of these planes indicate that solution has been effective only to a limited depth below the land surface. The bottom of the solutional zone is an exaggerated replica of the land surface, showing a greater depth of the solutional zone below stream valleys. The greater depth is attributed to the greater accumulation of ground water, the dissolving agent, in those areas. Modifications of the ideal condition are effected by the less soluble beds and the configuration of the land surface.</span></p><p><span>The underground drainage systems of the area develop in a manner similar to rectilinear stream patterns, showing a definite alignment along the two joint sets of the area. Directional solution has taken place where one of these joint sets has been developed to the exclusion of the other.</span></p>","language":"English","publisher":"Society of Economic Geologist","doi":"10.2113/gsecongeo.43.1.39","usgsCitation":"Hamilton, D., 1948, Some solutional features of the limestone near Lexington, Kentucky: Economic Geology, v. 43, no. 1, p. 39-52, https://doi.org/10.2113/gsecongeo.43.1.39.","productDescription":"14 p.","startPage":"39","endPage":"52","costCenters":[],"links":[{"id":379896,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Kentucky","otherGeospatial":"Lexington","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -85.18798828125,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              37.54893261064111\n            ],\n            [\n              -83.75976562499999,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              38.47939467327645\n            ],\n            [\n              -85.18798828125,\n              37.54893261064111\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"43","issue":"1","noUsgsAuthors":false,"publicationDate":"1948-01-01","publicationStatus":"PW","contributors":{"authors":[{"text":"Hamilton, D.K.","contributorId":244110,"corporation":false,"usgs":false,"family":"Hamilton","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":803313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215752,"text":"70215752 - 1948 - Quality of water in the upper Colorado River basin","interactions":[],"lastModifiedDate":"2021-04-06T15:23:39.269743","indexId":"70215752","displayToPublicDate":"1948-10-28T12:21:45","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Quality of water in the upper Colorado River basin","docAbstract":"<p>In a drainage area as large as the Colorado River Basin there are naturally large differences in the quality of the surface waters. The chemical character of the water at six gaging stations on the Colorado River from near the headwaters to near the mouth is shown by the analyses in Table 1.</p><p>It will be seen that the concentration of dissolved solids increased from 64 ppm (0.09 tons per ac ft) in the headwaters to 699 ppm (0.95 tons per ac ft) near the mouth.</p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00375","usgsCitation":"Howard, C.S., 1948, Quality of water in the upper Colorado River basin: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 375-378, https://doi.org/10.1029/TR029i003p00375.","productDescription":"4 p.","startPage":"375","endPage":"378","costCenters":[],"links":[{"id":379878,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Upper Colorado River Basin","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-106.190554,40.997607],[-106.061181,40.996999],[-105.730421,40.996886],[-105.724804,40.99691],[-105.277138,40.998173],[-105.27686,40.998173],[-105.256527,40.998191],[-105.254779,40.99821],[-104.943371,40.998084],[-104.855273,40.998048],[-104.829504,40.99927],[-104.675999,41.000957],[-104.497149,41.001828],[-104.497058,41.001805],[-104.467672,41.001473],[-104.214692,41.001657],[-104.214191,41.001568],[-104.211473,41.001591],[-104.123586,41.001626],[-104.10459,41.001543],[-104.086068,41.001563],[-104.066961,41.001504],[-104.053249,41.001406],[-104.039238,41.001502],[-104.023383,41.001887],[-104.018223,41.001617],[-103.972642,41.001615],[-103.971373,41.001524],[-103.953525,41.001596],[-103.906324,41.001387],[-103.896207,41.00175],[-103.877967,41.001673],[-103.858449,41.001681],[-103.750498,41.002054],[-103.574522,41.001721],[-103.497447,41.001635],[-103.486697,41.001914],[-103.421975,41.002007],[-103.421925,41.001969],[-103.396991,41.002558],[-103.382492,41.002232],[-103.365314,41.001846],[-103.362979,41.001844],[-103.077804,41.002298],[-103.076536,41.002253],[-103.059538,41.002368],[-103.057998,41.002368],[-103.043444,41.002344],[-103.038704,41.002251],[-103.002026,41.002486],[-103.000102,41.0024],[-102.98269,41.002157],[-102.981483,41.002112],[-102.963669,41.002186],[-102.962522,41.002072],[-102.960706,41.002059],[-102.959624,41.002095],[-102.94483,41.002303],[-102.943109,41.002051],[-102.925568,41.00228],[-102.924029,41.002142],[-102.906547,41.002276],[-102.904796,41.002207],[-102.887407,41.002178],[-102.885746,41.002131],[-102.867822,41.002183],[-102.865784,41.001988],[-102.849263,41.002301],[-102.846455,41.002256],[-102.830303,41.002351],[-102.82728,41.002143],[-102.773546,41.002414],[-102.766723,41.002275],[-102.754617,41.002361],[-102.739624,41.00223],[-102.653463,41.002332],[-102.621033,41.002597],[-102.578696,41.002291],[-102.575738,41.002268],[-102.575496,41.0022],[-102.566048,41.0022],[-102.556789,41.002219],[-102.487955,41.002445],[-102.470537,41.002382],[-102.469223,41.002424],[-102.379593,41.002301],[-102.364066,41.002174],[-102.292833,41.002207],[-102.292622,41.00223],[-102.292553,41.002207],[-102.291354,41.002207],[-102.2721,41.002245],[-102.267812,41.002383],[-102.231931,41.002327],[-102.2122,41.002462],[-102.209361,41.002442],[-102.19121,41.002326],[-102.124972,41.002338],[-102.070598,41.002423],[-102.051718,41.002377],[-102.051614,41.002377],[-102.051292,40.749591],[-102.051292,40.749586],[-102.051398,40.697542],[-102.051725,40.537839],[-102.051519,40.520094],[-102.051465,40.440008],[-102.05184,40.396396],[-102.051572,40.39308],[-102.051798,40.360069],[-102.051553,40.349214],[-102.051309,40.338381],[-102.051922,40.235344],[-102.051894,40.229193],[-102.051909,40.162674],[-102.052001,40.148359],[-102.051744,40.003078],[-102.051569,39.849805],[-102.051363,39.843471],[-102.051318,39.833311],[-102.051254,39.818992],[-102.050594,39.675594],[-102.050099,39.653812],[-102.050422,39.646048],[-102.049954,39.592331],[-102.049806,39.574058],[-102.049764,39.56818],[-102.049554,39.538932],[-102.049673,39.536691],[-102.049679,39.506183],[-102.049369,39.423333],[-102.04937,39.41821],[-102.049167,39.403597],[-102.04896,39.373712],[-102.048449,39.303138],[-102.04725,39.13702],[-102.047189,39.133147],[-102.047134,39.129701],[-102.046571,39.047038],[-102.045388,38.813392],[-102.045334,38.799463],[-102.045448,38.783453],[-102.045371,38.770064],[-102.045287,38.755528],[-102.045375,38.754339],[-102.045212,38.697567],[-102.045156,38.688555],[-102.045127,38.686725],[-102.04516,38.675221],[-102.045102,38.674946],[-102.045074,38.669617],[-102.045288,38.615249],[-102.045288,38.615168],[-102.045211,38.581609],[-102.045189,38.558732],[-102.045223,38.543797],[-102.045112,38.523784],[-102.045262,38.505532],[-102.045263,38.505395],[-102.045324,38.453647],[-102.044936,38.41968],[-102.044442,38.415802],[-102.044944,38.384419],[-102.044613,38.312324],[-102.044568,38.268819],[-102.044567,38.268749],[-102.04451,38.262412],[-102.044398,38.250015],[-102.044251,38.141778],[-102.044589,38.125013],[-102.044255,38.113011],[-102.044644,38.045532],[-102.043844,37.928102],[-102.043845,37.926135],[-102.043219,37.867929],[-102.043033,37.824146],[-102.042953,37.803535],[-102.042668,37.788758],[-102.042158,37.760164],[-102.04199,37.738541],[-102.041876,37.723875],[-102.041574,37.680436],[-102.041694,37.665681],[-102.041582,37.654495],[-102.041585,37.644282],[-102.041618,37.607868],[-102.041894,37.557977],[-102.041899,37.541186],[-102.042016,37.535261],[-102.041786,37.506066],[-102.041801,37.469488],[-102.041755,37.434855],[-102.041669,37.43474],[-102.041676,37.409898],[-102.041586,37.38919],[-102.041524,37.375018],[-102.042089,37.352819],[-102.041974,37.352613],[-102.041817,37.30949],[-102.041664,37.29765],[-102.041963,37.258164],[-102.042002,37.141744],[-102.042135,37.125021],[-102.042092,37.12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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. S.","contributorId":73180,"corporation":false,"usgs":true,"family":"Howard","given":"C.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":803306,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215751,"text":"70215751 - 1948 - Fluctuations in concentration of dissolved solids of some southwestern streams","interactions":[],"lastModifiedDate":"2020-10-28T17:15:15.508813","indexId":"70215751","displayToPublicDate":"1948-10-28T12:11:05","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Fluctuations in concentration of dissolved solids of some southwestern streams","docAbstract":"<p><span>The concentration of dissolved solids in waters of streams of the Southwestern United Stated fluctuates widely as the stream discharge changes. These fluctuations may be extensive in a period of a few days or even a few hours. Data in this paper show the extent of the day‐to‐day changes in specific conductance and discharge of the Rio Grande at San Acacia, New Mexico, during the spring run‐off period of 1945. Data also are presented to show rapid fluctuations in concentration for the Pecos River near Artesia, New Mexico, the Gila River near Bylas, Arizona, and the Rio Grande at San Acacia during typical summer months. Hourly changes in chloride and discharge are shown for a day of approximately normal flow for the Pecos River near Malaga, New Mexico, and for a 36‐hour period of extremely low flow for the Gila River near Fort Thomas, Arizona.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00080","usgsCitation":"Hem, J., 1948, Fluctuations in concentration of dissolved solids of some southwestern streams: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 80-84, https://doi.org/10.1029/TR029i001p00080.","productDescription":"5 p.","startPage":"80","endPage":"84","costCenters":[],"links":[{"id":379877,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Arizona, New Mexico","otherGeospatial":"Southwestern Streams","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -110.41259765625,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              32.7503226078097\n            ],\n            [\n              -108.30322265624999,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              34.488447837809304\n            ],\n            [\n              -110.41259765625,\n              32.7503226078097\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Hem, J.D.","contributorId":54576,"corporation":false,"usgs":true,"family":"Hem","given":"J.D.","affiliations":[],"preferred":false,"id":803305,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215693,"text":"70215693 - 1948 - Geology and ground-water resources of Iwo Jima ","interactions":[],"lastModifiedDate":"2020-10-27T20:28:58.557427","indexId":"70215693","displayToPublicDate":"1948-10-27T15:01:22","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1723,"text":"GSA Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Geology and ground-water resources of Iwo Jima ","docAbstract":"<p>Iwo Jima, in the western Pacific Ocean, consists of Motoyama, a broad volcanic cone, at the north, and Mt. Suribachi at the south, with an undulating isthmus between. Motoyama is largely light-gray-buff tuff. A thick andesitic lava flow under Suribachi, exposed in several places, is overlain by a thick deposit of cinder and scoria. The isthmus (called Tidorigahara by the Japanese) is underlain by more than 200 feet of loose black volcanic ash and fine cinder derived from Suribachi. Several small coral reefs are located about 340 and 110 feet above present sea level.</p><p>Iwo Jima first came into existence, probably early in Pleistocene time, with the building above sea level of the tuff cone of Motoyama. Quite late in the active life of Motoyama, volcanic activity on the southwestern flank resulted in the formation of Suribachi. This activity may have started with the welling up of the andesitic lava which underlies Suribachi. Following the major eruption of Suribachi, relative sea level changed, and the sea stood about 360 feet higher than at present. The broad cone of Motoyama was beveled; the relative sea level then dropped 240 feet, with minor halts to about 120 feet above present level. As the island rose, Suribachi burst forth in its last stage of explosive activity. Wave erosion cut deeply into the andesite flow of Suribachi, and a prominent bench level was formed 120 feet above present sea level.</p><p>The Japanese on the island were often faced with serious water shortages. Americans drilled wells and obtained moderately large supplies of usable water. The temperature of the water ranges from 105° to 179° F., and the water is somewhat mineralized. The most favorable area for ground-water development is the isthmus.</p>","language":"English","publisher":"Geological Society of America","doi":"10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2","usgsCitation":"Swenson, F.A., 1948, Geology and ground-water resources of Iwo Jima : GSA Bulletin, v. 59, no. 10, p. 995-1008, https://doi.org/10.1130/0016-7606(1948)59[995:GAGROI]2.0.CO;2.","productDescription":"14 p.","startPage":"995","endPage":"1008","costCenters":[],"links":[{"id":379832,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"Japan","otherGeospatial":"Iwo Jima","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              141.251220703125,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.693814995267424\n            ],\n            [\n              141.4057159423828,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.85092688067188\n            ],\n            [\n              141.251220703125,\n              24.693814995267424\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","volume":"59","issue":"10","noUsgsAuthors":false,"publicationStatus":"PW","contributors":{"authors":[{"text":"Swenson, F. A.","contributorId":71622,"corporation":false,"usgs":true,"family":"Swenson","given":"F.","email":"","middleInitial":"A.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":803152,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215685,"text":"70215685 - 1948 - Report of Committee on Ground Water, 1945–1946","interactions":[],"lastModifiedDate":"2021-03-17T14:36:25.886627","indexId":"70215685","displayToPublicDate":"1948-10-27T13:19:47","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Report of Committee on Ground Water, 1945–1946","docAbstract":"<p><span>The principal activity of the Committee during the year was the arranging and presentation of a symposium on methods of estimating ground‐water supplies. The response was gratifying and resulted in the presentation of 11 interesting papers at the 1946 meeting. The report of the Subcommittee on Permeability by C. E. Jacob, Chairman, is given as Appendix A. At a meeting of the Executive Committee of the Section of Hydrology in June 1946, this Subcommittee of the Committee on Ground Water was changed to the Committee on Permeability of the Section of Hydrology, with Jacob continuing as Chairman. This will give the new Committee much greater latitude in dealing with a subject which is of concern to several of the Research Committees.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i001p00117","usgsCitation":"Lohman, S.W., 1948, Report of Committee on Ground Water, 1945–1946: Eos, Transactions, American Geophysical Union, v. 29, no. 1, p. 117-123, https://doi.org/10.1029/TR029i001p00117.","productDescription":"7 p.","startPage":"117","endPage":"123","costCenters":[],"links":[{"id":379876,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Lohman, S. W.","contributorId":45318,"corporation":false,"usgs":true,"family":"Lohman","given":"S.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":803144,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215684,"text":"70215684 - 1948 - Development of limestone reservoirs in Comal County, Texas","interactions":[],"lastModifiedDate":"2020-10-28T12:00:02.648533","indexId":"70215684","displayToPublicDate":"1948-10-27T13:13:15","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Development of limestone reservoirs in Comal County, Texas","docAbstract":"<p><span>The Edwards limestone, and to a lesser extent the Comanche Peak limestone and the lower part of the Glen Rose limestone below, all of Lower Cretaceous age, form one of the most extensive ground‐water reservoirs in Texas. As a result of normal faulting, these formations are connected by underground channels to form a hydrologic unit which is partly artesian and partly unconfined. Observations in Comal County show that the development of the reservoir by solution is closely related to the geologic history, in which complex faulting and the disconformity between the Edwards and Georgetown limestones are important factors. Various phases of development are shown in different fault blocks, depending upon length of exposure at the surface. The Edwards limestone, which contains the main channels of underground drainage, is almost uniformly permeable from top to bottom, whereas the older, but more recently exposed lower part of the Glen Rose limestone is generally relatively impermeable except where exposed by mature streams.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00503","usgsCitation":"George, W., 1948, Development of limestone reservoirs in Comal County, Texas: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 503-510, https://doi.org/10.1029/TR029i004p00503.","productDescription":"8 p.","startPage":"503","endPage":"510","costCenters":[],"links":[{"id":379823,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Texas","county":"Comal County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-98.2986,30.0395],[-98.1102,29.9036],[-98.0389,29.8493],[-97.9996,29.7537],[-98.0895,29.6857],[-98.2045,29.6363],[-98.3124,29.5973],[-98.3149,29.6014],[-98.3191,29.6033],[-98.3279,29.6053],[-98.3295,29.6058],[-98.3305,29.6086],[-98.3341,29.6109],[-98.3383,29.6128],[-98.3419,29.6147],[-98.3445,29.6175],[-98.3439,29.623],[-98.3432,29.6303],[-98.3452,29.6345],[-98.3478,29.6381],[-98.3498,29.6423],[-98.3492,29.645],[-98.3475,29.6496],[-98.3464,29.6523],[-98.3479,29.6551],[-98.3516,29.657],[-98.3589,29.6589],[-98.361,29.6603],[-98.3625,29.6631],[-98.364,29.6645],[-98.3677,29.6659],[-98.3724,29.6656],[-98.3772,29.6638],[-98.3793,29.6643],[-98.3803,29.6657],[-98.3833,29.6721],[-98.3842,29.6786],[-98.3826,29.6822],[-98.3794,29.6849],[-98.3783,29.689],[-98.3787,29.6913],[-98.3813,29.6945],[-98.3828,29.6973],[-98.3828,29.7001],[-98.3806,29.7028],[-98.3779,29.7046],[-98.3722,29.705],[-98.3601,29.7048],[-98.3543,29.7047],[-98.3511,29.7051],[-98.3458,29.7101],[-98.3425,29.715],[-98.3419,29.7192],[-98.3424,29.7228],[-98.3449,29.7265],[-98.3527,29.7308],[-98.3559,29.7317],[-98.3606,29.7318],[-98.3638,29.7282],[-98.3676,29.7237],[-98.3734,29.7215],[-98.376,29.7215],[-98.377,29.7261],[-98.3779,29.7316],[-98.3795,29.7348],[-98.3889,29.7345],[-98.3941,29.736],[-98.3978,29.737],[-98.3988,29.7397],[-98.4014,29.7439],[-98.4045,29.7467],[-98.4081,29.7476],[-98.4134,29.7468],[-98.4182,29.7446],[-98.4203,29.7419],[-98.4219,29.7391],[-98.4226,29.7341],[-98.4216,29.73],[-98.4216,29.729],[-98.4253,29.7277],[-98.4279,29.7278],[-98.4296,29.726],[-98.4301,29.7241],[-98.4291,29.7218],[-98.4291,29.7195],[-98.4318,29.7182],[-98.4371,29.7178],[-98.4402,29.7188],[-98.4428,29.7188],[-98.4449,29.7202],[-98.4459,29.723],[-98.4458,29.7276],[-98.4452,29.7326],[-98.4462,29.734],[-98.4499,29.7345],[-98.4546,29.7327],[-98.4588,29.7337],[-98.463,29.7361],[-98.4661,29.7379],[-98.4719,29.7376],[-98.4772,29.7353],[-98.4851,29.735],[-98.5008,29.738],[-98.5086,29.7413],[-98.5122,29.7436],[-98.5143,29.7446],[-98.5196,29.7455],[-98.5238,29.7456],[-98.5254,29.7447],[-98.529,29.7452],[-98.5332,29.7485],[-98.5357,29.7526],[-98.5399,29.7541],[-98.5441,29.7527],[-98.5473,29.7528],[-98.5499,29.7547],[-98.5493,29.756],[-98.5488,29.7565],[-98.5488,29.7592],[-98.5498,29.7602],[-98.5524,29.7606],[-98.5535,29.7602],[-98.5545,29.7588],[-98.5562,29.7566],[-98.5572,29.7557],[-98.5604,29.7534],[-98.5662,29.7526],[-98.5741,29.7504],[-98.5783,29.7495],[-98.5805,29.7473],[-98.5816,29.7445],[-98.5837,29.7432],[-98.5874,29.7446],[-98.59,29.7469],[-98.5936,29.7488],[-98.5983,29.7489],[-98.6015,29.7494],[-98.6051,29.7499],[-98.6052,29.748],[-98.6047,29.7457],[-98.6026,29.7448],[-98.6016,29.7425],[-98.6048,29.7407],[-98.61,29.7399],[-98.6137,29.7395],[-98.6174,29.7409],[-98.6216,29.7423],[-98.6231,29.7428],[-98.6257,29.7437],[-98.6321,29.7429],[-98.6384,29.7416],[-98.6431,29.7403],[-98.6458,29.7403],[-98.6468,29.7426],[-98.6478,29.7477],[-98.4138,29.9442],[-98.2986,30.0395]]]},\"properties\":{\"name\":\"Comal\",\"state\":\"TX\"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"George, W.O.","contributorId":41886,"corporation":false,"usgs":true,"family":"George","given":"W.O.","email":"","affiliations":[],"preferred":false,"id":803143,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215683,"text":"70215683 - 1948 - Hydrology of limestone terrane in Schoharie County, New York","interactions":[],"lastModifiedDate":"2021-04-07T13:48:14.233831","indexId":"70215683","displayToPublicDate":"1948-10-27T13:02:34","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Hydrology of limestone terrane in Schoharie County, New York","docAbstract":"<p><span>During the summer of 1946 the writer studied the ground‐water resources of Schoharie County, New York, as a part of the program of ground‐water investigation being carried on in cooperation between the United States Geological Survey and the New York State Water Power and Control Commission. Because the outcrop belt of Devonian and Upper Silurian carbonate rocks is wider in Schoharie County than in other parts of the State, the effects of solution on these formations is better displayed here than elsewhere. The conditions described below probably apply on a smaller scale to the areas to the west, where the upper formations are cut out by an unconformity, and to the east in the Helderberg area, where similar effects have been described by Goldring [see “References” at end of paper, 1935]. However, it is probable that solution in the limestones in the Hudson Valley is not comparable because of the folded condition of the rocks.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00251","usgsCitation":"Berdan, J.M., 1948, Hydrology of limestone terrane in Schoharie County, New York: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 251-253, https://doi.org/10.1029/TR029i002p00251.","productDescription":"3 p.","startPage":"251","endPage":"253","costCenters":[],"links":[{"id":379822,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"New York","county":"Schoharie County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-74.264,42.7981],[-74.2622,42.7963],[-74.2579,42.7949],[-74.2548,42.793],[-74.2529,42.7898],[-74.2511,42.7857],[-74.2506,42.7825],[-74.2525,42.7798],[-74.2545,42.7707],[-74.2572,42.7621],[-74.261,42.7585],[-74.266,42.7572],[-74.2729,42.7573],[-74.2848,42.7569],[-74.2941,42.7566],[-74.2998,42.7552],[-74.3035,42.7535],[-74.3042,42.7521],[-74.3067,42.7485],[-74.2779,42.7196],[-74.2711,42.7195],[-74.2687,42.714],[-74.2424,42.7174],[-74.2393,42.7178],[-74.2026,42.7107],[-74.1838,42.7123],[-74.1773,42.73],[-74.1619,42.7166],[-74.168,42.6912],[-74.1684,42.674],[-74.1697,42.6672],[-74.1718,42.6595],[-74.1757,42.6499],[-74.1833,42.64],[-74.1878,42.6342],[-74.1903,42.6324],[-74.1949,42.6201],[-74.1963,42.6165],[-74.2197,42.5927],[-74.2198,42.5899],[-74.2218,42.5845],[-74.2237,42.5813],[-74.23,42.5764],[-74.2338,42.5737],[-74.2357,42.5705],[-74.2392,42.5488],[-74.2321,42.5323],[-74.2298,42.521],[-74.2263,42.5046],[-74.227,42.5014],[-74.2354,42.4837],[-74.2425,42.4688],[-74.2457,42.4648],[-74.2509,42.4516],[-74.2652,42.4177],[-74.2636,42.4063],[-74.253,42.4071],[-74.246,42.3839],[-74.246,42.3816],[-74.2472,42.3807],[-74.2497,42.3807],[-74.2547,42.3812],[-74.2591,42.3795],[-74.2666,42.3732],[-74.2748,42.3673],[-74.2804,42.3647],[-74.2861,42.3629],[-74.2954,42.363],[-74.2997,42.363],[-74.306,42.3599],[-74.3078,42.359],[-74.3141,42.3595],[-74.3227,42.3605],[-74.3314,42.3601],[-74.3389,42.3602],[-74.3426,42.3584],[-74.3469,42.3594],[-74.3513,42.3617],[-74.358,42.3676],[-74.3617,42.3699],[-74.3685,42.3704],[-74.3778,42.3701],[-74.389,42.3697],[-74.3977,42.3675],[-74.4432,42.3547],[-74.6168,42.4219],[-74.7145,42.5175],[-74.671,42.5654],[-74.652,42.5926],[-74.6317,42.6242],[-74.6382,42.6511],[-74.6501,42.6935],[-74.6621,42.7322],[-74.6681,42.7513],[-74.668,42.764],[-74.6645,42.7917],[-74.6504,42.828],[-74.5619,42.8092],[-74.4562,42.7716],[-74.3311,42.7828],[-74.2893,42.7838],[-74.264,42.7981]]]},\"properties\":{\"name\":\"Schoharie\",\"state\":\"NY\"}}]}","volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Berdan, Jean Milton","contributorId":86758,"corporation":false,"usgs":true,"family":"Berdan","given":"Jean","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":803142,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215681,"text":"70215681 - 1948 - Runoff from rain and snow","interactions":[],"lastModifiedDate":"2021-04-02T14:46:48.221141","indexId":"70215681","displayToPublicDate":"1948-10-27T12:31:09","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Runoff from rain and snow","docAbstract":"<p><span>The basic principles of the idealized hydrologic cycle are reviewed with emphasis on storage and movement of water in the soil. A distinction is made between ground‐water runoff and overland runoff in terms of storage and lag, expressed as accumulated deviations from uniform flow over a period of several years. These functions are presented for the period 1920 through 1945 for three rivers in central Oregon: John Day, Deschutes, and Metolius, which exemplify minimum, moderate, and maximum effects, respectively, of storage and lag. The Metolius River is shown to have extremely small fluctuations in discharge from year to year, ascribed to a great portion of its flow being derived from ground‐water runoff; and its response to fluctuations in annual precipitation lags behind that of the John Day River by about five years. Specific techniques and measures for improving seasonal water supply forecasts are suggested.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i004p00511","usgsCitation":"Piper, A.M., 1948, Runoff from rain and snow: Eos, Transactions, American Geophysical Union, v. 29, no. 4, p. 511-524, https://doi.org/10.1029/TR029i004p00511.","productDescription":"14 p.","startPage":"511","endPage":"524","costCenters":[],"links":[{"id":379816,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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 \"}}]}","volume":"29","issue":"4","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Piper, A. M.","contributorId":102865,"corporation":false,"usgs":true,"family":"Piper","given":"A.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":803140,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70215680,"text":"70215680 - 1948 - Trends in runoff in the Pacific Northwest","interactions":[],"lastModifiedDate":"2021-03-19T22:32:03.584067","indexId":"70215680","displayToPublicDate":"1948-10-27T12:12:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Trends in runoff in the Pacific Northwest","docAbstract":"<p><span>The diminution in runoff in the Pacific Northwest, particularly the Columbia River Basin, during the past 50 years, and its hydrologic significance are discussed in this paper. An analysis of the rainfall‐runoff relations for the Basin is made in order to explain the different influence of short‐ and long‐term precipitation factors on the diminution of runoff. The indicated effects of long‐term precipitation may reflect the influence of ground‐water storage.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00387","usgsCitation":"McDonald, C.C., and Langbein, W.B., 1948, Trends in runoff in the Pacific Northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 387-397, https://doi.org/10.1029/TR029i003p00387.","productDescription":"11 p.","startPage":"387","endPage":"397","costCenters":[],"links":[{"id":379814,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Pacific 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"McDonald, C. C.","contributorId":69204,"corporation":false,"usgs":true,"family":"McDonald","given":"C.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":803138,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Langbein, W. B.","contributorId":102053,"corporation":false,"usgs":true,"family":"Langbein","given":"W.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":803139,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70215679,"text":"70215679 - 1948 - Quality of water in the northwest","interactions":[],"lastModifiedDate":"2021-03-16T20:54:25.168523","indexId":"70215679","displayToPublicDate":"1948-10-27T11:52:33","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Quality of water in the northwest","docAbstract":"<h3 class=\"article-section__header main main\">Abstract</h3><div class=\"article-section__content en main\"><p>The quality of natural waters, as judged by the dissolved mineral content, is quite varied throughout the Northwest. The concentrations of dissolved solids range from less than 50 ppm for many of the surface waters in Washington and Oregon, to several thousand ppm in the alkaline lakes of these states. On the whole, the quality of the natural waters is good but in some areas the waters have become unsatisfactory for many purposes, including irrigation, through contamination with wastes from industrial processes, which may include drainage from irrigated lands.</p></div>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i003p00379","usgsCitation":"Howard, C.S., 1948, Quality of water in the northwest: Eos, Transactions, American Geophysical Union, v. 29, no. 3, p. 379-383, https://doi.org/10.1029/TR029i003p00379.","productDescription":"5 p.","startPage":"379","endPage":"383","costCenters":[],"links":[{"id":379801,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"The 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 \"}}]}","volume":"29","issue":"3","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Howard, C. 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,{"id":70215677,"text":"70215677 - 1948 - Effect of water temperature on flow of a natural stream","interactions":[],"lastModifiedDate":"2020-10-27T16:42:53.600045","indexId":"70215677","displayToPublicDate":"1948-10-27T11:34:00","publicationYear":"1948","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Effect of water temperature on flow of a natural stream","docAbstract":"<p><span>Approximately three per cent of the variation in streamflow of the Kootenai River near Copeland, Idaho, has been found to be associated with variation in water temperature. This has been determined by correlation analysis of residuals in streamflow that were not accounted for by either gage height or slope.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR029i002p00240","usgsCitation":"Eisenlohr, W.S., 1948, Effect of water temperature on flow of a natural stream: Eos, Transactions, American Geophysical Union, v. 29, no. 2, p. 240-242, https://doi.org/10.1029/TR029i002p00240.","productDescription":"3 p.","startPage":"240","endPage":"242","costCenters":[],"links":[{"id":379798,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"2","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Eisenlohr, William Stewart Jr.","contributorId":115220,"corporation":false,"usgs":false,"family":"Eisenlohr","given":"William","suffix":"Jr.","email":"","middleInitial":"Stewart","affiliations":[],"preferred":false,"id":803113,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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