No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp869","usgsCitation":"Youngquist, C.V., Langbein, W.B., Smith, W.E., and Showalter, A.K., 1941, Flood of August 1935 in the Muskingum River Basin, Ohio, with sections on the associated meteorology and hydrology: U.S. Geological Survey Water Supply Paper 869, vi, 118 p., https://doi.org/10.3133/wsp869.","productDescription":"vi, 118 p.","costCenters":[],"links":[{"id":393777,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24676.htm"},{"id":29862,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0869/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0869/report-thumb.jpg"}],"country":"United States","state":"Ohio","otherGeospatial":"Muskingum River Basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -82.779,\n 39.377\n ],\n [\n -80.9070,\n 39.377\n ],\n [\n -80.9070,\n 41.158\n ],\n [\n -82.779,\n 41.158\n ],\n [\n -82.779,\n 39.377\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eef0a","contributors":{"authors":[{"text":"Youngquist, C. V.","contributorId":28230,"corporation":false,"usgs":true,"family":"Youngquist","given":"C.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":146178,"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":146179,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Waldo E.","contributorId":15188,"corporation":false,"usgs":true,"family":"Smith","given":"Waldo","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146176,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Showalter, A. K.","contributorId":15600,"corporation":false,"usgs":true,"family":"Showalter","given":"A.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":4620,"text":"wsp894 - 1941 - Surface water supply of the United States, 1940, Part IV, St. Lawrence River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:40","indexId":"wsp894","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"894","title":"Surface water supply of the United States, 1940, Part IV, St. Lawrence River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp894","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Surface water supply of the United States, 1940, Part IV, St. Lawrence River basin: U.S. Geological Survey Water Supply Paper 894, v, 213 p. ;23 cm., https://doi.org/10.3133/wsp894.","productDescription":"v, 213 p. ;23 cm.","costCenters":[],"links":[{"id":139220,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0894/report-thumb.jpg"},{"id":31677,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0894/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973cb","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":528313,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":3182,"text":"wsp866A - 1941 - Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana","interactions":[],"lastModifiedDate":"2024-02-01T23:11:46.67183","indexId":"wsp866A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"866","chapter":"A","title":"Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp866A","usgsCitation":"Erdmann, C.E., 1941, Geology of dam sites on the upper tributaries of the Columbia river in Idaho and Montana: Part 1. Katka, Tunnel no. 8 and Kootenai Falls dam sites, Kootenai River Idaho and Montana: U.S. Geological Survey Water Supply Paper 866, v, 36 p., https://doi.org/10.3133/wsp866A.","productDescription":"v, 36 p.","costCenters":[],"links":[{"id":30140,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0866a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139031,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0866a/report-thumb.jpg"},{"id":394778,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24664.htm","text":"Katka Dam site","linkFileType":{"id":5,"text":"html"}},{"id":425262,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24665.htm","text":"Kootenai Falls Dam site","linkFileType":{"id":5,"text":"html"}},{"id":425263,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24666.htm","text":"Tunnel No. 8 Dam site","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Idaho","otherGeospatial":"Kootenai River","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -116.129,\n 48.869\n ],\n [\n -116.129,\n 48.596\n ],\n [\n -115.72,\n 48.596\n ],\n [\n -115.72,\n 48.869\n ],\n [\n -116.129,\n 48.869\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad5e4b07f02db68397d","contributors":{"authors":[{"text":"Erdmann, C. E.","contributorId":87122,"corporation":false,"usgs":true,"family":"Erdmann","given":"C.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146386,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2466,"text":"wsp885 - 1941 - Surface water supply of Hawaii, July 1, 1938, to June 30, 1939","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"wsp885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"885","title":"Surface water supply of Hawaii, July 1, 1938, to June 30, 1939","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp885","usgsCitation":"Paulsen, C., and Carson, M.H., 1941, Surface water supply of Hawaii, July 1, 1938, to June 30, 1939: U.S. Geological Survey Water Supply Paper 885, v, 142 p. :ill. ;24 cm., https://doi.org/10.3133/wsp885.","productDescription":"v, 142 p. :ill. ;24 cm.","costCenters":[],"links":[{"id":138729,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0885/report-thumb.jpg"},{"id":28542,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0885/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697806","contributors":{"authors":[{"text":"Paulsen, Carl G.","contributorId":106865,"corporation":false,"usgs":true,"family":"Paulsen","given":"Carl G.","affiliations":[],"preferred":false,"id":145240,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carson, Max H.","contributorId":21132,"corporation":false,"usgs":true,"family":"Carson","given":"Max","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":145239,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1608,"text":"wsp903 - 1941 - Surface water supply of the United States, 1940 : Part 13 Snake River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:14","indexId":"wsp903","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"903","title":"Surface water supply of the United States, 1940 : Part 13 Snake River basin","language":"ENGLISH","publisher":"Govt. Print. Off.,","doi":"10.3133/wsp903","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Surface water supply of the United States, 1940 : Part 13 Snake River basin: U.S. Geological Survey Water Supply Paper 903, vi, 246 p. :ill. ;23 cm., https://doi.org/10.3133/wsp903.","productDescription":"vi, 246 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":137137,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0903/report-thumb.jpg"},{"id":26673,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0903/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6973dd","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":527971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2960,"text":"wsp848 - 1941 - Ground water in Keith County, Nebraska","interactions":[],"lastModifiedDate":"2026-04-30T16:57:06.702842","indexId":"wsp848","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"848","title":"Ground water in Keith County, Nebraska","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. G.P.O.","doi":"10.3133/wsp848","usgsCitation":"Wenzel, L., Waite, H.A., Halmos, E.E., and Johnson, G.E., 1941, Ground water in Keith County, Nebraska: U.S. Geological Survey Water Supply Paper 848, Report: iv, 68 p.; 3 Plates: 25.50 × 17.50 inches, https://doi.org/10.3133/wsp848.","productDescription":"Report: iv, 68 p.; 3 Plates: 25.50 × 17.50 inches","costCenters":[],"links":[{"id":29671,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0848/plate-3.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":29670,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0848/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":29669,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/0848/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}},{"id":29672,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0848/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139291,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0848/report-thumb.jpg"},{"id":109959,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24661.htm","linkFileType":{"id":5,"text":"html"},"description":"24661"}],"country":"United States","state":"Nebraska","county":"Keith County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-101.2702,41.3959],[-101.2688,41.0488],[-101.2487,41.0476],[-101.248,41.005],[-101.3618,41.0035],[-102.0504,41.0037],[-102.0505,41.0477],[-102.0542,41.0481],[-102.0556,41.2214],[-102.0551,41.3939],[-101.9853,41.3955],[-101.4055,41.3954],[-101.2702,41.3959]]]},\"properties\":{\"name\":\"Keith\",\"state\":\"NE\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66daf5","contributors":{"authors":[{"text":"Wenzel, Leland K.","contributorId":46077,"corporation":false,"usgs":true,"family":"Wenzel","given":"Leland K.","affiliations":[],"preferred":false,"id":146047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Waite, Herbert A.","contributorId":40973,"corporation":false,"usgs":true,"family":"Waite","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":146046,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Halmos, E. E.","contributorId":79870,"corporation":false,"usgs":true,"family":"Halmos","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":146048,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Johnson, G. E.","contributorId":103261,"corporation":false,"usgs":true,"family":"Johnson","given":"G.","email":"","middleInitial":"E.","affiliations":[],"preferred":true,"id":146049,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":796,"text":"wsp910 - 1941 - Water levels and artesian pressures in observation wells in the United States in 1940, Part 5, Northwestern States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp910","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"910","title":"Water levels and artesian pressures in observation wells in the United States in 1940, Part 5, Northwestern States","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp910","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1941, Water levels and artesian pressures in observation wells in the United States in 1940, Part 5, Northwestern States: U.S. Geological Survey Water Supply Paper 910, 184 p. ;24 cm., https://doi.org/10.3133/wsp910.","productDescription":"184 p. ;24 cm.","costCenters":[],"links":[{"id":25363,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0910/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":136173,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0910/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5f9f13","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":527725,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2497,"text":"wsp868B - 1941 - Investigations of methods and equipment used in stream gaging, Part 2, Intakes for gage wells","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp868B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"868","chapter":"B","title":"Investigations of methods and equipment used in stream gaging, Part 2, Intakes for gage wells","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp868B","usgsCitation":"Pierce, C.H., 1941, Investigations of methods and equipment used in stream gaging, Part 2, Intakes for gage wells: U.S. Geological Survey Water Supply Paper 868, iv, p.37-75, 4 p. of plates :ill. ;23 cm., https://doi.org/10.3133/wsp868B.","productDescription":"iv, p.37-75, 4 p. of plates :ill. ;23 cm.","costCenters":[],"links":[{"id":138768,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0868b/report-thumb.jpg"},{"id":28616,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0868b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db69859e","contributors":{"authors":[{"text":"Pierce, Charles Henry","contributorId":89876,"corporation":false,"usgs":true,"family":"Pierce","given":"Charles","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":145291,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2976,"text":"wsp849C - 1941 - Geology and ground-water resources of the Balmorhea area, western Texas","interactions":[],"lastModifiedDate":"2016-08-19T14:48:55","indexId":"wsp849C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"849","chapter":"C","title":"Geology and ground-water resources of the Balmorhea area, western Texas","docAbstract":"Balmorhea is the center of a thriving farming community, the lands of which are irrigated with water derived chiefly from large springs but partly from the storm flow of Toyah Creek. The storm flow of the creek and a part of the winter flow of the springs is stored in a reservoir near Balmorhea and used later to supplement the flow of the springs. The present investigation was made to determine the geologic and hydrologic relations of the springs, whether additional water can be obtained from wells, and what effect the withdrawal of large amounts of water from wells would have upon the discharge of the springs. Balmorhea is situated near the foot of the Davis and Barrilla Mountains and along the southwestern margin of the Toyah Basin. The mountains and adjacent basin are drained by Toyah and Limpia Creeks. The group of springs around Balmorhea occur in the floor of the valley of Toyah Creek. They have been divided into artesian springs--Phantom Lake, Giffin and San Solomon Springs; and gravity springs--Toyah Creek, Saragosa, East Sandia and West Sandia Springs. The combined discharge of the springs during dry years is about 23,000 gallons a minute, of which amount the artesian springs supply more than 90 percent. The underground reservoir which supplies the artesian springs is the fractured and cavernous Lower Cretaceous limestone. This limestone, about 500 feet thick, is underlain by impermeable rocks, probably of Permian age, and is overlain by impermeable Upper Cretaceous strata that have a maximum thickness of about 500 feet. These are in turn overlain in the mountains by Tertiary lava and on the plains by gravel and other surficial deposits. The Lower Cretaceous limestone is at the surface or covered by a thin layer of gravel in a belt that lies athwart the stream channels and extends from Gomez Peak southeastward along the foothills of the Davis Mountains. In this belt all the streams suffer heavy seepage losses. From this belt the limestone dips gently northeastward to the axis of a northwestward-trending syncline and then rises to the surface in the vicinity of Phantom Lake, where a part of the water is discharged. About 1,000 feet northeast of this lake is a northwestward-trending fault of small displacement, on the northeast side of which the limestone is downthrown, northeastward from this fault the limestone rises gently and appears at the surface about a mile to the northeast, where it is again downfaulted, but the throw is not sufficient to affect the movement of the water. For several miles to the north the water-bearing Lower Cretaceous limestone is covered by 400 to 500 feet of impermeable Upper Cretaceous strata. It is believed that the Lower Cretaceous rocks are again near the surface and covered by only a thin mantle of gravel and other surficial deposits at San Solomon and Giffin Springs and that just northeast of the springs a fault crosses the valley along which the impermeable Upper Cretaceous rocks are faulted into a position opposite the Lower Cretaceous rocks, thus obstructing further northward movement of the water in the Lower Cretaceous limestone and forcing it to issue as large springs. Between this fault and Brogada the Lower Cretaceous rocks are believed to lie at a depth of about 500 feet and are overlain by Upper Cretaceous strata and a blanket of gravel and other surficial deposits, which are the source of the water of Toyah Creek, Sandia, and Saragosa Springs. Northeast of Brogada the Lower Cretaceous lies at a greater depth, and the mantle of gravel is much thicker. Wells put down to the limestone in the vicinity of San Solomon and Giffin Springs would decrease the flow of the springs. The effect of wells in limestone between the fault near these springs and the Brogado Hills on the flow of the springs would depend on the completeness with which the fault cuts off northward movement of ground water in the limestone. If the movement of water across the fault has been prev
","language":"English","publisher":"U.S. Government Printing Office","doi":"10.3133/wsp849C","isbn":"pbk","usgsCitation":"White, W.N., Gale, H.S., and Nye, S.S., 1941, Geology and ground-water resources of the Balmorhea area, western Texas: U.S. Geological Survey Water Supply Paper 849, 69 p., https://doi.org/10.3133/wsp849C.","productDescription":"69 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138908,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0849c/report-thumb.jpg"},{"id":29732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0849c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db6857ca","contributors":{"authors":[{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":146080,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gale, H. S.","contributorId":102040,"corporation":false,"usgs":true,"family":"Gale","given":"H.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146081,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Nye, S. Spencer","contributorId":26570,"corporation":false,"usgs":true,"family":"Nye","given":"S.","email":"","middleInitial":"Spencer","affiliations":[],"preferred":false,"id":146079,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":753,"text":"wsp909 - 1941 - Water levels and artesian pressure in observation wells in the United States, 1940, Part 4, South-Central States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:09","indexId":"wsp909","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"909","title":"Water levels and artesian pressure in observation wells in the United States, 1940, Part 4, South-Central States","language":"ENGLISH","publisher":"U.S. Govt. Print. 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The area is underlain by a series of sands, clays, and shales of Eocene age that dip, in general, southward at an angle a little greater than that of the land surface, which also slopes southward, thus creating favorable artesian conditions. The formations cropping out in the area from north to south are the Wilcox group undifferentiated, the Carrizo sand, the Mont Selman formation, consisting of the Reklaw member, the Queen City sand member, and the Weches greensand member, the Sparta sand, the Cook Mountain and Yegua formations, and the Jackson group undifferentiated. Small supplies of potable water may be obtained from shallow wells in the outcrop areas of most of these formations. Only three of the formations appear to be likely to yield large supplies of water to wells, and in these the water is under sufficient artesian pressure in most places to cause wells to flow. The Yegua formation yields large amounts of water to some wells in the vicinity of Lufkin. However, the water is moderately mineralized and is not acceptable for municipal use except after dilution with surface water and treatment to reduce mineralization. Moreover, most of the wells in this formation yield only small quantities of water, which is highly mineralized. The Sparta sand appears to be likely to yield large supplies of water to wells throughout the northern part of Angelina County. The water, however, is moderately to highly mineralized and cannot be used for purposes that require water of good quality. The Carrizo sand promises to yield large quantities of water low in mineralization in northern Angelina County and southern Nacogdoches County. Computations indicate that the present southward flow through the formation is about 2,750,000 gallons a day, but pumping from wells and thus increasing the hydraulic gradient would greatly increase the flow. Considerable amounts of water will also be released from storage in the formation after pumping begins.
","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp849A","usgsCitation":"White, W.N., Sayre, A., and Heuser, J., 1941, Geology and ground-water resources of the Lufkin area, Texas: U.S. Geological Survey Water Supply Paper 849, iv, 58 p., https://doi.org/10.3133/wsp849A.","productDescription":"iv, 58 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":138909,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/0849a/report-thumb.jpg"},{"id":29733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/0849a/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b01e4b07f02db6984a1","contributors":{"authors":[{"text":"White, Walter N.","contributorId":99124,"corporation":false,"usgs":true,"family":"White","given":"Walter","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":146084,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sayre, A.N.","contributorId":84339,"corporation":false,"usgs":true,"family":"Sayre","given":"A.N.","email":"","affiliations":[],"preferred":false,"id":146083,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Heuser, J.F.","contributorId":54183,"corporation":false,"usgs":true,"family":"Heuser","given":"J.F.","affiliations":[],"preferred":false,"id":146082,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":534,"text":"wsp902 - 1941 - Surface water supply of the United States, 1940 : Part 12, North Pacific drainage basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:07","indexId":"wsp902","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1941","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":"902","title":"Surface water supply of the United States, 1940 : Part 12, North Pacific drainage basins","language":"ENGLISH","publisher":"U.S. Govt. 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