This report gives a summarized description of the public water supplies in 35 counties of central and north-central Texas, extending from the southern boundaries of Travis, Blanco, Gillespie, and Kerr Counties northward to the TexasOklahoma State line. It gives the available data as follows for each of the 145 communities: Population of the community; name of the official from whom the information was obtained; ownership of water works, whether private or municipal source of supply, whether ground water 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, if any; and 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; yields of the wells, and records of water levels, if available.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1069","usgsCitation":"Sundstrom, R.W., Broadhurst, W., and Dwyer, B., 1949, Public water supplies in central and north-central Texas: U.S. Geological Survey Water Supply Paper 1069, vii, 128 p., https://doi.org/10.3133/wsp1069.","productDescription":"vii, 128 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":29222,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1069/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138675,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1069/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4382","contributors":{"authors":[{"text":"Sundstrom, Raymond W.","contributorId":8080,"corporation":false,"usgs":true,"family":"Sundstrom","given":"Raymond","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":145761,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Broadhurst, W. L.","contributorId":55414,"corporation":false,"usgs":true,"family":"Broadhurst","given":"W. L.","affiliations":[],"preferred":false,"id":145763,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dwyer, B.C.","contributorId":53774,"corporation":false,"usgs":true,"family":"Dwyer","given":"B.C.","email":"","affiliations":[],"preferred":false,"id":145762,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":775,"text":"wsp1028 - 1949 - Water levels and artesian pressure in observation wells in the United States, 1945, Part 6, Southwestern States and Hawaii","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1028","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1028","title":"Water levels and artesian pressure in observation wells in the United States, 1945, Part 6, Southwestern States and Hawaii","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1028","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Water levels and artesian pressure in observation wells in the United States, 1945, Part 6, Southwestern States and Hawaii: U.S. Geological Survey Water Supply Paper 1028, vi, 301 p. ;23 cm., https://doi.org/10.3133/wsp1028.","productDescription":"vi, 301 p. ;23 cm.","costCenters":[],"links":[{"id":136049,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1028/report-thumb.jpg"},{"id":25342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1028/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db69608a","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":527707,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":604,"text":"wsp1091 - 1949 - Surface water supply of the United States, 1947, Part XI, Pacific slope basins in California","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1091","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1091","title":"Surface water supply of the United States, 1947, Part XI, Pacific slope basins in California","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1091","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1947, Part XI, Pacific slope basins in California: U.S. Geological Survey Water Supply Paper 1091, xi, 450 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1091.","productDescription":"xi, 450 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1091/report-thumb.jpg"},{"id":25167,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1091/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e33","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":527576,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2795,"text":"wsp1029 - 1949 - Ground water in the Jordan Valley, Utah","interactions":[],"lastModifiedDate":"2017-09-20T12:43:40","indexId":"wsp1029","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1029","title":"Ground water in the Jordan Valley, Utah","docAbstract":"The Jordan Valley is a small part of a larger area that during the glacial epoch was covered by an ancient lake known as Lake Bonneville. The Jordan River, the natural drainage path from Utah Lake, flows northward through the center of the valley and empties into Great Salt Lake. The Jordan Valley is a rockbottomed valley in which a great thickness of clay, silt, sand, and gravel has been laid down irregularly. The thickness of this material is not definitely known, but wells in the valley have penetrated as much as 2,000 feet without encountering bedrock. These sediments are chiefly stream and lake deposits. The material at the surface of the valley was deposited in an ancient lake which at its highest stage stood about 1,000 feet above the level of Great Salt Lake. The shore deposits laid down in this lake occur in the form of terraces or benches around the margin of this basin. The two most prominent benches are known as the Bonneville and Provo benches. The Bonneville bench was formed during the highest stage of the lake, and the Provo bench during a later stage about 400 feet lower.
Ground water occurs in the valley as (1) shallow ground water overlying the confining layer creating the artesian basin, (2) local perched water bodies, and (3) an artesian basin or reservoir including the recharge area. It occurs chiefly in the pore spaces of the sand and gravel of the stream and lake deposits. The most permeable water-bearing material occurs near the foot of the Wasatch Mountains in the area occupied by the Provo and Bonneville benches. At some distance from the mountains beds of finer material dense silt and clay alternate with more permeable beds of sand and gravel, giving rise to artesian conditions. On the Provo and Bonneville benches the water levels lie at considerable distances below the surface; but in the lower areas along the Jordan River and west of Salt Lake City as far as the lake, artesian conditions exist and many flowing wells have been drilled.
The principal sources of ground water in the Jordan Valley are the water that seeps into the ground from the streams entering the valley, the water that penetrates directly from the ram and snow that fall upon the bench lands on the east side of the valley, and the water that percolates downward from irrigation canals and from irrigated lands, chiefly derived from Utah Lake. In addition some deep-seated thermal water rises along the Wasatch fault.
Field determinations of the chloride content of the ground water show that nearly all the waters from the main part of the area of artesian flow, extending from Salt Lake City to Murray have a chloride content of less than 100 parts per million, and most of them have less than 50 parts per million. The distribution of waters of different chloride content indicates that the water of the main part of the area of artesian flow is derived chiefly from supplies that contain only small amounts of chloride namely, seepage from the streams that head in the Wasatch Mountains and rain and snow that fall upon the Provo and Bonneville benches and penetrate downward through the permeable materials that underlie these benches
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1029","collaboration":"Prepared in cooperation with Salt Lake City","usgsCitation":"Taylor, G., and Leggette, R., 1949, Ground water in the Jordan Valley, Utah: U.S. Geological Survey Water Supply Paper 1029, report: vi, 357 p.; 10 Plates: 13.00 X 17.50 inches or smaller, https://doi.org/10.3133/wsp1029.","productDescription":"report: vi, 357 p.; 10 Plates: 13.00 X 17.50 inches or smaller","numberOfPages":"370","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29287,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-05.pdf","text":"Plate 5","size":"637 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Jordan Valley showing average altitude of the ground-water surface during November 1931 and location of observation wells"},{"id":29284,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-01.pdf","text":"Plate 1","size":"801 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Index map of Utah showing areas covered by ground-water investigations"},{"id":29285,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-02.pdf","text":"Plate 2","size":"827 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Jordan Valley, Salt Lake County, Utah, showing the position of the Bonneville and Provo benches, area of artesian flow, 1931-33, and and location of wells drilled by Salt Lake City Corporation during 1934"},{"id":29286,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-04.pdf","text":"Plate 4","size":"999 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of Jordan Valley showing chloride content of the ground water"},{"id":138612,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1029/report-thumb.jpg"},{"id":247249,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-11.pdf","text":"Plate 11","size":"530 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrograph of well (D-2-1) 16 bbd 9, September 5-14, 1933"},{"id":247250,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-12.pdf","text":"Plate 12","size":"385 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrograph of well (D-2-1) 16 baa 8, September 3-15, 1933"},{"id":247251,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-13.pdf","text":"Plate 13","size":"405 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of well (D-2-1) 8 ada 3, September 3-16, well (D-2-1) ccd 1, September 11-13, and well (D-2-1) 16 bab 10, October 2-7 1933"},{"id":29288,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-08.pdf","text":"Plate 8","size":"1.24 MB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing location of wells operated and observed during the interference tests"},{"id":29289,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-09.pdf","text":"Plate 9","size":"731 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of observation wells, with barometric pressure and record of time of pumping from artesian wells by Salt Lake City during Interference Test 1"},{"id":29290,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1029/plate-10.pdf","text":"Plate 10","size":"548 KB","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrographs of observation wells, with barometric pressure and record of time of pumping from artesian wells by Salt Lake City during Interference Test 2"},{"id":29291,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1029/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Salt Lake County","otherGeospatial":"Jordan Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b1360","contributors":{"authors":[{"text":"Taylor, G.H.","contributorId":85158,"corporation":false,"usgs":true,"family":"Taylor","given":"G.H.","email":"","affiliations":[],"preferred":false,"id":145804,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leggette, R.M.","contributorId":87525,"corporation":false,"usgs":true,"family":"Leggette","given":"R.M.","email":"","affiliations":[],"preferred":false,"id":145805,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":776,"text":"wsp1071 - 1949 - Water levels and artesian pressure in observation wells in the United States, 1946, Part 1, Northeastern States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1071","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1071","title":"Water levels and artesian pressure in observation wells in the United States, 1946, Part 1, Northeastern States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1071","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Water levels and artesian pressure in observation wells in the United States, 1946, Part 1, Northeastern States: U.S. Geological Survey Water Supply Paper 1071, vii, 460 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1071.","productDescription":"vii, 460 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1071/report-thumb.jpg"},{"id":25343,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1071/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa05a","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":527708,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":603,"text":"wsp1090 - 1949 - Surface water supply of the United States, 1947, Part X, The Great Basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1090","title":"Surface water supply of the United States, 1947, Part X, The Great Basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1090","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1947, Part X, The Great Basin: U.S. Geological Survey Water Supply Paper 1090, vii, 196 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1090.","productDescription":"vii, 196 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136346,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1090/report-thumb.jpg"},{"id":25166,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696e19","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":527575,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":594,"text":"wsp1062 - 1949 - Surface water supply of the United States, 1946, Part XII, Pacific slope basins in Washington and upper Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1062","title":"Surface water supply of the United States, 1946, Part XII, Pacific slope basins in Washington and upper Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1062","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1946, Part XII, Pacific slope basins in Washington and upper Columbia River basin: U.S. Geological Survey Water Supply Paper 1062, ix, 314 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1062.","productDescription":"ix, 314 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1062/report-thumb.jpg"},{"id":25157,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968bb","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":527566,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":779,"text":"wsp1075 - 1949 - Water levels and artesian pressure in observation wells in the United States, 1946, Part 5, Northwestern States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1075","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1075","title":"Water levels and artesian pressure in observation wells in the United States, 1946, Part 5, Northwestern States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1075","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Water levels and artesian pressure in observation wells in the United States, 1946, Part 5, Northwestern States: U.S. Geological Survey Water Supply Paper 1075, 192 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1075.","productDescription":"192 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1075/report-thumb.jpg"},{"id":25346,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa100","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":527711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":778,"text":"wsp1074 - 1949 - Water levels and artesian pressure in observation wells in the United States, 1946, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp1074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1074","title":"Water levels and artesian pressure in observation wells in the United States, 1946, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1074","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Water levels and artesian pressure in observation wells in the United States, 1946, Part 4, South-Central States: U.S. Geological Survey Water Supply Paper 1074, vi, 215 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1074.","productDescription":"vi, 215 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":136052,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1074/report-thumb.jpg"},{"id":25345,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa033","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":527710,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":599,"text":"wsp1055 - 1949 - Surface water supply of the United States, 1946, Part V, Hudson Bay and upper Mississippi River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:08","indexId":"wsp1055","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1055","title":"Surface water supply of the United States, 1946, Part V, Hudson Bay and upper Mississippi River basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1055","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1946, Part V, Hudson Bay and upper Mississippi River basins: U.S. Geological Survey Water Supply Paper 1055, xii, 471 p. ;23 cm., https://doi.org/10.3133/wsp1055.","productDescription":"xii, 471 p. ;23 cm.","costCenters":[],"links":[{"id":136342,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1055/report-thumb.jpg"},{"id":25162,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1055/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968ca","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":527571,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3409,"text":"cir63 - 1949 - The chromograph, a new analytical tool for laboratory and field use","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"cir63","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"63","title":"The chromograph, a new analytical tool for laboratory and field use","docAbstract":"Water supplies in the Greater Atlanta Region, Georgia, are obtained mainly from surface-water sources, but there is concern that these sources may be unable to meet rising demands. This study indicates that large quantities of good-quality ground water are obtainable from selected sites in the crystalline rocks of the area. Hydrogeologic investigations of 1,051 wells that produce 20 to nearly 500 gallons per minute revealed that large supplies can be developed where favorable structural, stratigraphic, and topographic features result in localized increases in bedrock permeability. These features are described in detail and methods are presented for using them in selecting sites for locating high-producing wells. Most of the site-selection methods are applicable to the north half of the report area, which has rectangular and trellis drainage systems, but their use is restricted in the south half where a dendritic drainage system predominates. Borehole geophysical logs and core drilling revealed that some of the highest production wells derive water from 1- to 8-inch wide horizontal fractures. These fractures occur in a variety of topographic settings and are believed to be stress-relief fractures. (USGS)","language":"ENGLISH","publisher":"[U.S. Geological Survey],","doi":"10.3133/cir63","usgsCitation":"Stevens, R.E., and Lakin, H.W., 1949, The chromograph, a new analytical tool for laboratory and field use: U.S. Geological Survey Circular 63, 11 p. :illus. ;27 cm., https://doi.org/10.3133/cir63.","productDescription":"11 p. :illus. ;27 cm.","costCenters":[],"links":[{"id":123892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0063/report-thumb.jpg"},{"id":30427,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669493","contributors":{"authors":[{"text":"Stevens, Rollin Elbert","contributorId":43745,"corporation":false,"usgs":true,"family":"Stevens","given":"Rollin","email":"","middleInitial":"Elbert","affiliations":[],"preferred":false,"id":146844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lakin, Hubert William","contributorId":54578,"corporation":false,"usgs":true,"family":"Lakin","given":"Hubert","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":146845,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3741,"text":"cir52 - 1949 - Annual runoff in the United States","interactions":[],"lastModifiedDate":"2017-02-21T15:37:28","indexId":"cir52","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"52","title":"Annual runoff in the United States","docAbstract":"The water that drains from the land into creeks and rivers is called runoff. Supplying many of our basic human needs for water, runoff occurs chiefly as a residual of rainfall after Nature’s take – that is, after the persistent demands of evaporation from land and transpiration from vegetation have been supplied.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/cir52","usgsCitation":"Langbein, W.B., 1949, Annual runoff in the United States: U.S. Geological Survey Circular 52, Report: 14 p.; Plate 1: 23.50 x 16.25 inches, https://doi.org/10.3133/cir52.","productDescription":"Report: 14 p.; Plate 1: 23.50 x 16.25 inches","numberOfPages":"16","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":30802,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0052/plate-1.pdf","text":"Plate 1","size":"2.57 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":30803,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0052/report.pdf","text":"Report","size":"580 KB","linkFileType":{"id":1,"text":"pdf"}},{"id":118290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0052/report-thumb.jpg"}],"country":"United States","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67b8d9","contributors":{"authors":[{"text":"Langbein, Walter Basil","contributorId":40581,"corporation":false,"usgs":true,"family":"Langbein","given":"Walter","email":"","middleInitial":"Basil","affiliations":[],"preferred":false,"id":147515,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4578,"text":"wsp1087 - 1949 - Surface water supply of the United States, 1947, Part VII, Lower Mississippi River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"wsp1087","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1087","title":"Surface water supply of the United States, 1947, Part VII, Lower Mississippi River basin","language":"ENGLISH","publisher":"U.S. Govt. 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Off.,","doi":"10.3133/wsp1087","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1947, Part VII, Lower Mississippi River basin: U.S. Geological Survey Water Supply Paper 1087, ix, 419 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1087.","productDescription":"ix, 419 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139910,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1087/report-thumb.jpg"},{"id":31635,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1087/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db696845","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":528273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":4577,"text":"wsp1063 - 1949 - Surface water supply of the United States, 1946, Part XIII, Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:48","indexId":"wsp1063","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"1063","title":"Surface water supply of the United States, 1946, Part XIII, Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp1063","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1949, Surface water supply of the United States, 1946, Part XIII, Snake River basin: U.S. Geological Survey Water Supply Paper 1063, viii, 262 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1063.","productDescription":"viii, 262 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":139909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1063/report-thumb.jpg"},{"id":31634,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1063/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6968c0","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":528272,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3718,"text":"cir54 - 1949 - Geology and ground-water hydrology of the Angostura irrigation project, South Dakota, with a section on the mineral quality of the waters","interactions":[],"lastModifiedDate":"2016-04-04T13:27:41","indexId":"cir54","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"54","title":"Geology and ground-water hydrology of the Angostura irrigation project, South Dakota, with a section on the mineral quality of the waters","docAbstract":"The lands to be irrigated from water stored in the Angostura Reservoir are situated on the lover of two terraces along the southeast side of the Cheyenne River in northeastern Fall River County and on the terrace known as Harrison Plat in southeastern Custer County, S. Dak. The terrace deposits are composed of relatively permeable sands and gravels that rest on a shale bedrock platform. The terrace surfaces are mantled in part by slope wash derived from higher shale slopes and by wind-blown sand. Ground water occurs under water-table conditions in the river alluvium and in terraces above the river. Although the zone of saturation in the terrace deposits is 6enerally thin, it is essentially continuous in the area southeast of the river, and the water issues as springs in the terrace faces along the inner valley of the river and along the valleys of tributary streams cuttin6 back into the terraces. A zone of saturation is present only in part of the Harrison Plat area, and it extends to the terrace face only along Cottonwood Creek. Wells in the unconsolidated mantle rock supply water for domestic and stock purposes, but yields are small. Abundant supplies of artesian water are available at depths ranging up to 3,000 feet but are not now utilized except at the extreme western end of the area where the bedrock aquifer is close below the surface. The effect of applying irrigation water on the terrace lands will depend on the character of the underlying material and on the measures taken to forestall waterlogging and other undesirable effects. Terrace areas that are mantled by slope wash will be especially susceptible to waterlogging, as will valley-bottom areas mantled by colluvium that are adjacent to irrigated terracea. Periodic measurements of water levels in observation wells will give warning of potential waterlogging in time to permit taking preventive measures. Analyses of samples of both ground water and surface water indicate a high mineral content. In general, samples from the Cheyenne River are higher in total dissolved solids and lower in percent sodium than the ground water.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir54","usgsCitation":"Littleton, R.T., and Swenson, H.A., 1949, Geology and ground-water hydrology of the Angostura irrigation project, South Dakota, with a section on the mineral quality of the waters: U.S. Geological Survey Circular 54, Report: v, 96 p.; 2 Plates: 25.96 x 1.52 inches and 26.39 x 11.83 inches, https://doi.org/10.3133/cir54.","productDescription":"Report: v, 96 p.; 2 Plates: 25.96 x 1.52 inches and 26.39 x 11.83 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":30776,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0054/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30777,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0054/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":30778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0054/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124472,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0054/report-thumb.jpg"}],"country":"United States","state":"South Dakota","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -103.4307861328125,\n 43.34315755514772\n ],\n [\n -103.4307861328125,\n 43.536104967254566\n ],\n [\n -103.04008483886717,\n 43.536104967254566\n ],\n [\n -103.04008483886717,\n 43.34315755514772\n ],\n [\n -103.4307861328125,\n 43.34315755514772\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db6841fe","contributors":{"authors":[{"text":"Littleton, Robert T.","contributorId":34496,"corporation":false,"usgs":true,"family":"Littleton","given":"Robert","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":147477,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147478,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3312,"text":"cir20 - 1949 - Progress report on the geology and ground-water hydrology of the lower Platte River Valley, Nebraska, with a section on the chemical quality of the ground water","interactions":[],"lastModifiedDate":"2017-03-09T12:56:23","indexId":"cir20","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1949","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":"20","title":"Progress report on the geology and ground-water hydrology of the lower Platte River Valley, Nebraska, with a section on the chemical quality of the ground water","docAbstract":"The occurrence of abundant ground-water supplies in the lower Platte River Valley has made possible the present agricultural and industrial economy of the area. Likewise, the future development of the area is dependent on the wise use of this important resource. The current investigation, on which this report is based, is a necessary step in the planning for the greatest ultimate utilization of the water resources in the lower Platte River Valley.
The area covered by this study is the floor of the lower Platte River Valley between North Platte and Fremont and embraces about 2,500 square miles. The entire valley floor is underlain by unconsolidated Pleistocene sediments which consist of clay, silt, sand and gravel and range in thickness from less than 20 feet to nearly 200 feet. Westward from Cozad these sediments were deposited in a valley entrenched in bedrock, but east of Cozad they are continuous with similar deposits which underlie the adjacent uplands. Bedrock formations of Tertiary age are in contact with the basal Pleistocene sediments from the west end of the area to about Central City. From Central City eastward, formations of Cretaceous age immediately underlie the Pleistocene deposits.
The Pleistocene sediments and underlying pervious formations are water saturated below depths which range from less than 1 foot to about 90 feet below the surface. In general, the configuration of the water table is similar to the topography of the land surface, but the relief on the water table is considerably less by comparison. Movement of ground water is either toward the river or parallel to it. Based on present information, movement of ground water out of the valley is not indicated but additional water-level control is needed south of the valley between Grand Island and Columbus to determine the possibility of ground-water loss in this stretch of the valley.
Periodic observations of water-table fluctuations have constituted an important phase of ground-water studies in the lower Platte River Valley. Examination of water-level data collected by the Geological Survey in cooperation with the Conservation and Survey Division of the University of Nebraska indicates that water levels throughout most of the valley between Gothenburg and Grand Island declined during the 9-year period, December 1930 to December 1939. The maximum net declines observed during this period were a little greater than 4 feet. During the period December 1939 to December 1946, water levels recovered throughout much of the same area; in local areas on the south side of the Platte River between North Platte and Overton water levels rose in excess of 10 feet as a result of seepage losses tram canals and irrigated lands. However, north of Wood River in western Hall County water levels continued to decline to the extent that in at least 3 observation wells water levels in December 1946 were more than 5 feet lower than in December 1930.
Water levels were measured monthly in 1946 and bimonthly in 1947 in observation wells located throughout the area covered by this report. During this period water levels fluctuated through a range of about 3 feet, the lowest levels being reached in September 1946 and the highest levels being reached in July 1947. Average fluctuations between successive measurements were a little less than 0.4 foot. The amount of ground-water discharge in the summer months of 1947 was approximately double that of the previous summer. However, replenishment to groundwater storage during the fall of 1946 and the spring of 1947 was sufficiently great that the amount of water in storage in the valley as a whole at the end of the 2-year period was essentially equal to the amount in storage at the beginning of the period. At the end of 1947 the Dawson and Buffalo County areas showed gains to storage whereas the remainder of the valley suffered vary slight losses during the same 2 years.
The quantity of ground water that a water-bearing material will yield is dependent upon the hydrologic properties of the material. Two hydrologic properties of greatest importance are permeability and specific yield. During the course of the present investigation 5 pumping tests were conducted to determine the coefficients of permeability and storage of the Pleistocene deposits. The values of the former range from 955 to 4,925 and the latter tram 0.007. to 0.236 attar 24 hours of pumping.
The mineral character of the ground water has been determined from analyses of samples, of which 15 represented municipal supplies and 3 were irrigation waters. Ground waters analyzed for this report contained variable amounts of dissolved solids ranging from 240 to 1,060 parts per million, with hardness values above limits considered desirable tor public supplies. The increased concentration of dissolved solids for ground waters in the western part of the valley as a result of return flow conditions, is noted. Ground waters in the valley are discussed as to suitability for municipal and irrigation uses, and analyses of samples do not reveal any serious condition that would adversely affect the use of these waters for the purposes intended. As irrigation increases, periodic chemical analyses of ground waters in this area will be required to evaluate the effects of the re-use of drainage waters and to provide information for salinity control.
Ground-water supplies are drawn upon extensively for irrigation purposes, for municipal supplies, and for rural, domestic and stock supplies. Nearly 4,000 irrigation wells are known to exist in the area, the greatest concentrations of these being in Dawson, Buffalo, and Hall Counties.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/cir20","usgsCitation":"Waite, H.A., and Swenson, H.A., 1949, Progress report on the geology and ground-water hydrology of the lower Platte River Valley, Nebraska, with a section on the chemical quality of the ground water: U.S. Geological Survey Circular 20, Report: v, 211 p.; 4 plates: 43.75 x 22.00 inches or less , https://doi.org/10.3133/cir20.","productDescription":"Report: v, 211 p.; 4 plates: 43.75 x 22.00 inches or less ","costCenters":[],"links":[{"id":121311,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1949/0020/report-thumb.jpg"},{"id":30314,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0020/plate-2.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 2"},{"id":30313,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0020/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"},{"id":30315,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0020/plate-3.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 3"},{"id":30316,"rank":301,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1949/0020/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":337200,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/circ/1949/0020/plate-9.pdf","text":"Plate 9","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Nebraska","otherGeospatial":"Lower Platte River Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.27319335937499,\n 41.47566020027821\n ],\n [\n -96.35009765625,\n 41.6154423246811\n ],\n [\n -96.800537109375,\n 41.66470503009207\n ],\n [\n -97.0751953125,\n 41.63186741069748\n ],\n [\n -97.44873046875,\n 41.549700145132725\n ],\n [\n -97.822265625,\n 41.50857729743935\n ],\n [\n -98.250732421875,\n 41.45919537950706\n ],\n [\n -98.50341796875,\n 41.236511201246216\n ],\n [\n -98.82202148437499,\n 41.08763212467916\n ],\n [\n -99.0966796875,\n 41.07935114946899\n ],\n [\n -99.55810546875,\n 41.07935114946899\n ],\n [\n -100.65673828125,\n 41.244772343082076\n ],\n [\n -101.162109375,\n 41.244772343082076\n ],\n [\n -101.458740234375,\n 41.19518982948959\n ],\n [\n -101.458740234375,\n 41.054501963290505\n ],\n [\n -101.14013671875,\n 40.93841495689795\n ],\n [\n -100.887451171875,\n 40.863679665481676\n ],\n [\n -100.283203125,\n 40.730608477796636\n ],\n [\n -99.931640625,\n 40.622291783092706\n ],\n [\n -99.459228515625,\n 40.463666324587685\n ],\n [\n -98.87695312499999,\n 40.50544628405211\n ],\n [\n -98.20678710937499,\n 40.772221877329024\n ],\n [\n -97.822265625,\n 40.9964840143779\n ],\n [\n -97.48168945312499,\n 41.20345619205131\n ],\n [\n -97.152099609375,\n 41.261291493919884\n ],\n [\n -96.78955078125,\n 41.178653972331674\n ],\n [\n -96.427001953125,\n 41.269549502842565\n ],\n [\n -96.27319335937499,\n 41.47566020027821\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de1e","contributors":{"authors":[{"text":"Waite, Herbert A.","contributorId":40973,"corporation":false,"usgs":true,"family":"Waite","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146642,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146643,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3906,"text":"cir44 - 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