{"pageNumber":"5876","pageRowStart":"146875","pageSize":"25","recordCount":165658,"records":[{"id":61614,"text":"gq607 - 1967 - Geologic map of the Fredonia quadrangle, western Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"gq607","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"607","title":"Geologic map of the Fredonia quadrangle, western Kentucky","language":"ENGLISH","doi":"10.3133/gq607","usgsCitation":"Rogers, W.B., and Hays, W.H., 1967, Geologic map of the Fredonia quadrangle, western Kentucky: U.S. Geological Survey Geologic Quadrangle 607, 1 map :col. ;76 x 83 cm., https://doi.org/10.3133/gq607.","productDescription":"1 map :col. ;76 x 83 cm.","costCenters":[],"links":[{"id":103334,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1920.htm","linkFileType":{"id":5,"text":"html"},"description":"1920"},{"id":247920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0607/report.pdf","size":"33","linkFileType":{"id":1,"text":"pdf"}},{"id":252345,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0607/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,37.1175 ], [ -88.11749999999999,37.25 ], [ -88,37.25 ], [ -88,37.1175 ], [ -88.11749999999999,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b03e4b07f02db698f2a","contributors":{"authors":[{"text":"Rogers, William B.","contributorId":31469,"corporation":false,"usgs":true,"family":"Rogers","given":"William","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":266141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hays, William Henry","contributorId":29424,"corporation":false,"usgs":true,"family":"Hays","given":"William","email":"","middleInitial":"Henry","affiliations":[],"preferred":false,"id":266140,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3075,"text":"wsp1881 - 1967 - Quality of surface waters of the United States, 1961, Parts 1 and 2: North Atlantic slope basins and South Atlantic slope and Eastern Gulf of Mexico basins","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp1881","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1881","title":"Quality of surface waters of the United States, 1961, Parts 1 and 2: North Atlantic slope basins and South Atlantic slope and Eastern Gulf of Mexico basins","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1881","usgsCitation":"Love, S.K., 1967, Quality of surface waters of the United States, 1961, Parts 1 and 2: North Atlantic slope basins and South Atlantic slope and Eastern Gulf of Mexico basins: U.S. Geological Survey Water Supply Paper 1881, xi, 412 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1881.","productDescription":"xi, 412 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139410,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1881/report-thumb.jpg"},{"id":29947,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1881/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651adb","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1687,"text":"wsp1817C - 1967 - Determination of phenoxy acid herbicides in water by electron-capture and microcoulometric gas chromatography","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp1817C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1817","chapter":"C","title":"Determination of phenoxy acid herbicides in water by electron-capture and microcoulometric gas chromatography","docAbstract":"A sensitive gas chromatographic method using microcoulometric titration and electron-capture detection for the analysis of 2,4-D, silvex, 2,4,5-T, and other phenoxy acid herbicides in water is described. The herbicides are extracted from unfiltered water samples (800-1,000 ml) by use of ethyl ether ; then the herbicides are concentrated and esterilied. To allow the analyst a choice, two esterilication procedures--using either boron trifluoride-methanol or diazomethane--are evaluated. \r\n\r\nMicrocoulometric gas chromatography is specific for the detection of halogenated compounds such as the phenoxy acid herbicides whereas it does not respond to nonhalogenated components. Microcoulometric gas chromatography requires care and patience. It is not convenient for rapid screening of l-liter samples that contain less than 1 microgram of the herbicide. Although electroncapture gas chromatography is less selective and more critically affected by interfering substances, it is, nevertheless, convenient and more sensitive than microcoulometric gas chromatography. \r\n\r\nTwo different liquid phases are used in the gas chromatographic columns--DC-200 silicone in one column and QF-1 silicone in the other. The performance of both columns is improved by the addition of Carbowax 20M. The Gas Chrom Q support is coated with the liquid phases by the 'frontal-analysis' technique. The practical lower limits for measurement of the phenoxy acid herbicides in water primarily depend upon the sample size, interferences present, anal instrumentation used. With l-liter samples of water, the practical lower limits of measurement are 10 ppt (parts per trillion) for 2,4-D and 2 ppt for silvex and 2,4,5-T when electron-capture detection is used, and approximately 20 ppt for each herbicide when analyzed by microcoulometric-titration gas chromatography. Recoveries of the herbicides immediately after addition to unfiltered water samples averaged 92 percent for 2,4-D, 90 percent for silvex, and 98 percent for 2,4,5-T. Studies on the stability of herbicides added to water samples showed that 2,4-D may be rapidly degraded, especially if the samples are obtained from areas which have been repeatedly sprayed with 2,4-D. When degradation was observed, added 2,4-D rapidly decomposed within 10 days. At concentrations of about 200 ppt, however, the degradation rate was diminished. In 20 days the concentration of 2,4-D was reduced to 160-180 ppt.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1817C","usgsCitation":"Goerlitz, D., and Lamar, W.L., 1967, Determination of phenoxy acid herbicides in water by electron-capture and microcoulometric gas chromatography: U.S. Geological Survey Water Supply Paper 1817, 21 p. ;24 cm., https://doi.org/10.3133/wsp1817C.","productDescription":"21 p. ;24 cm.","costCenters":[],"links":[{"id":138120,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1817c/report-thumb.jpg"},{"id":26768,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1817c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6676a6","contributors":{"authors":[{"text":"Goerlitz, D.F.","contributorId":8445,"corporation":false,"usgs":true,"family":"Goerlitz","given":"D.F.","affiliations":[],"preferred":false,"id":143972,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lamar, William L.","contributorId":15592,"corporation":false,"usgs":true,"family":"Lamar","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":143973,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3077,"text":"wsp1885 - 1967 - Quality of surface waters of the United States, 1961, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:05:38","indexId":"wsp1885","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1885","title":"Quality of surface waters of the United States, 1961, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin","language":"ENGLISH","publisher":"U.S. Govt. Print. Off.,","doi":"10.3133/wsp1885","usgsCitation":"Love, S.K., 1967, Quality of surface waters of the United States, 1961, Parts 9-14, Colorado River basin to Pacific slope basins in Oregon and lower Columbia River basin: U.S. Geological Survey Water Supply Paper 1885, xviii, 677 p. :ill. ;23 cm., https://doi.org/10.3133/wsp1885.","productDescription":"xviii, 677 p. :ill. ;23 cm.","costCenters":[],"links":[{"id":139412,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1885/report-thumb.jpg"},{"id":29949,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1885/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8be4b07f02db651ac3","contributors":{"authors":[{"text":"Love, S. K.","contributorId":27419,"corporation":false,"usgs":true,"family":"Love","given":"S.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":146246,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61714,"text":"gq666 - 1967 - Geologic map of the Imlay quadrangle, Pershing County, Nevada","interactions":[],"lastModifiedDate":"2012-02-10T00:10:30","indexId":"gq666","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"666","title":"Geologic map of the Imlay quadrangle, Pershing County, Nevada","language":"ENGLISH","doi":"10.3133/gq666","usgsCitation":"Silberling, N.J., and Wallace, R.E., 1967, Geologic map of the Imlay quadrangle, Pershing County, Nevada: U.S. Geological Survey Geologic Quadrangle 666, 1 map., https://doi.org/10.3133/gq666.","productDescription":"1 map.","costCenters":[],"links":[{"id":103389,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1975.htm","linkFileType":{"id":5,"text":"html"},"description":"1975"},{"id":248012,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0666/report.pdf","size":"32","linkFileType":{"id":1,"text":"pdf"}},{"id":252589,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0666/report-thumb.jpg"}],"scale":"62500","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -118.25,40.5 ], [ -118.25,40.75 ], [ -118,40.75 ], [ -118,40.5 ], [ -118.25,40.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b00e4b07f02db697f28","contributors":{"authors":[{"text":"Silberling, Norman J.","contributorId":102438,"corporation":false,"usgs":true,"family":"Silberling","given":"Norman","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":266272,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wallace, R. E.","contributorId":6823,"corporation":false,"usgs":true,"family":"Wallace","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266271,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":3288,"text":"cir528 - 1967 - Reports and maps of the Geological Survey released only in the open files, 1966","interactions":[],"lastModifiedDate":"2012-02-02T00:05:28","indexId":"cir528","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"528","title":"Reports and maps of the Geological Survey released only in the open files, 1966","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir528","usgsCitation":"Weld, B., Griffin, M.S., and Brett, G.W., 1967, Reports and maps of the Geological Survey released only in the open files, 1966: U.S. Geological Survey Circular 528, 14 p. ;26 cm., https://doi.org/10.3133/cir528.","productDescription":"14 p. ;26 cm.","costCenters":[],"links":[{"id":126469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1967/0528/report-thumb.jpg"},{"id":30284,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1967/0528/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a58e4b07f02db62f3fc","contributors":{"authors":[{"text":"Weld, Betsy A.","contributorId":68714,"corporation":false,"usgs":true,"family":"Weld","given":"Betsy A.","affiliations":[],"preferred":false,"id":146596,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Griffin, Margaret S.","contributorId":101252,"corporation":false,"usgs":true,"family":"Griffin","given":"Margaret","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":146597,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brett, George W.","contributorId":58622,"corporation":false,"usgs":true,"family":"Brett","given":"George","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146595,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":42348,"text":"ofr67224 - 1967 - Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","interactions":[],"lastModifiedDate":"2025-07-24T19:44:54.186569","indexId":"ofr67224","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"67-224","title":"Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr67224","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1967, Aeromagnetic map of the Aurora, Powell Mountain, and Huntoon Valley quadrangles and part of the Trench Canyon quadrangle, Nevada-California: U.S. Geological Survey Open-File Report 67-224, 1 Plate: 29.67 x 42.79 inches, https://doi.org/10.3133/ofr67224.","productDescription":"1 Plate: 29.67 x 42.79 inches","costCenters":[],"links":[{"id":414489,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_8179.htm","linkFileType":{"id":5,"text":"html"}},{"id":80114,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1967/0224/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Aurora, Powell Mountain, Huntoon Valley, and Trench Canyon quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -119,\n 38.5\n ],\n [\n -119,\n 38\n ],\n [\n -118.5,\n 38\n ],\n [\n -118.5,\n 38.5\n ],\n [\n -119,\n 38.5\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697271","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":530914,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62023,"text":"mr51 - 1967 - Iron in the United States, exclusive of Alaska and Hawaii","interactions":[],"lastModifiedDate":"2025-05-13T15:04:13.648266","indexId":"mr51","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":324,"text":"Mineral Investigations Resource Map","code":"MR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"51","title":"Iron in the United States, exclusive of Alaska and Hawaii","docAbstract":"

The iron-ore deposits in the United States (exclusive of Alaska and Hawaii) are shown on the accompanying map; many iron-bearing deposits that are of lesser or only potential value are also shown. Because these deposits range widely in extent, two general categories of symbols are used, each of which is subdivided as explained below. The first category is for deposits of such restricted extent that they can be represented by a \"spot\": the second is for deposits which, although not necessarily extremely large in terms of volume or tonnage, are either continuous (or essentially so) or clustered in reasonably well-defined districts of numerous small occurrences.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mr51","usgsCitation":"Carr, M.S., Guild, P.W., and Wright, W., 1967, Iron in the United States, exclusive of Alaska and Hawaii: U.S. Geological Survey Mineral Investigations Resource Map 51, Report: 20 p.; 1 Plate: 64.10 x 41.00 inches, https://doi.org/10.3133/mr51.","productDescription":"Report: 20 p.; 1 Plate: 64.10 x 41.00 inches","costCenters":[],"links":[{"id":485810,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/mr/51/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":485634,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1783.htm","linkFileType":{"id":5,"text":"html"}},{"id":179789,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mr/51/report-thumb.jpg"},{"id":260471,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mr/51/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"3168000","country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -127.25,24.25 ], [ -127.25,49.25 ], [ -66.5,49.25 ], [ -66.5,24.25 ], [ -127.25,24.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667339","contributors":{"authors":[{"text":"Carr, Martha S.","contributorId":8169,"corporation":false,"usgs":true,"family":"Carr","given":"Martha","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":266733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Guild, Philip White","contributorId":94285,"corporation":false,"usgs":true,"family":"Guild","given":"Philip","email":"","middleInitial":"White","affiliations":[],"preferred":false,"id":266734,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wright, W.B.","contributorId":101296,"corporation":false,"usgs":true,"family":"Wright","given":"W.B.","affiliations":[],"preferred":false,"id":266735,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":1715,"text":"wsp1608H - 1967 - Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","interactions":[],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp1608H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","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":"1608","chapter":"H","title":"Ground-water hydrology of the Punjab region of West Pakistan, with emphasis on problems caused by canal irrigation","docAbstract":"Rising water tables and the salinization of land as the result of canal irrigation threaten the agricultural economy of the Punjab. Since 1954 the Water and Soils Investigation Division of the West Pakistan Water and Power Development Authority has inventoried the water and soils resources of the Punjab and investigated the relations between irrigation activities, the natural hydrologic factors, and the incidence of waterlogging and subsurface-drainage problems. This report summarizes the findings of the investigation, which was carried out under a cooperative agreement between the Government of Pakistan and the U.S. Agency for International Development, and its predecessor, the U.S. International Cooperation Administration. \r\n\r\nLeakage from the canal systems, some of which have been in operation for more than 100 years, is the principal cause of rising water levels and constitutes the major component of ground-water recharge in the Punjab. Geologic studies have shown that virtually the entire Punjab is underlain to depths of 1,000 feet or more by unconsolidated alluvium, which is saturated to within a few feet of land surface. The alluvium varies in texture from medium sand to silty clay, but sandy sediments predominate. Large capacity wells, yielding 4 cfs or more, can be developed almost everywhere. Ground water occurring within a depth of 500 feet below the surface averages less than 1,000 ppm of dissolved solids throughout approximately two-thirds of the Punjab. It is estimated that the volume of usable ground water in storage in this part of the alluvial aquifer is on the order of 2 billion acre-feet. In the other one-third of the Punjab, total dissolved solids range from 1,000 to about 20,000 ppm. In about one-half of this area (one-sixth of the area of the Punjab) some ground water can be utilized by diluting with surface water from canals. \r\n\r\nThe ground-water reservoir underlying the Punjab is an unexploited resource of enormous economic value. It is recognized that the scientific management of this ground-water reservoir is the key to permanent irrigation agriculture in the Punjab. The West Pakistan Water .and Power Development Authority has prepared a long-range program for reclaiming the irrigated lands of the Punjab. The essential feature of this program is a proposed network of tubewells (drilled wells) located with an .average density of about one per square mile. Groundwater withdrawals will serve the dual purpose of helping to supply irrigation requirements and of providing subsurface drainage. Despite the feasibility and inherent advantages of tubewell reclamation methods, it is inevitable that just as the superposition of the canal system on the native environment caused undesirable side effects, large-scale ground-water withdrawals again will disturb the hydrologic regimen. The distribtution of withdrawals and maintenance of a favorable salt balance are two distinct, but related aspects of the ground-water budget that present potential hazards that must be considered in the design and management of the tubewell projects. The availability of ground water for irrigation diminishes from northeast to southwest, or downgradient along the doab (an area lying between two rivers) and is negligible in the centers of the lower parts of the doabs, where the ground water is too highly mineralized for use. Ground-water supplies must be developed in areas where they are available and it might become necessary, under a program of maximum exploitation of ground-water resources, to transfer supplies from outside sources to points of use in the lower parts of the doabs. \r\n\r\nSeveral factors inherent in the tubewell system will tend to depreciate the quality of ground water with time. Among these are the addition of salts leached from the soils, increased concentration of salts due .to repeated cycles of recirculation, and the possible lateral and upward encroachment of saline water in response to pumping. 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No abstract available. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp551","usgsCitation":"Varnes, D., Scott, G.R., Cardwell, W.D., and Jenkins, E.D., 1967, General and engineering geology of the United States Air Force Academy site, Colorado, with a section on ground water: U.S. Geological Survey Professional Paper 551, Report: v, 93 p.; 8 Plates: 33.00 x 38.50 inches or smaller, https://doi.org/10.3133/pp551.","productDescription":"Report: v, 93 p.; 8 Plates: 33.00 x 38.50 inches or smaller","costCenters":[],"links":[{"id":33903,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"}},{"id":411442,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4599.htm","linkFileType":{"id":5,"text":"html"}},{"id":33904,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"}},{"id":33905,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"}},{"id":33906,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"}},{"id":33907,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/0551/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}},{"id":33900,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"}},{"id":33901,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"}},{"id":33902,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"}},{"id":117737,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/0551/report-thumb.jpg"},{"id":33899,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/0551/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Colorado","otherGeospatial":"United States Air Force Academy","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -104.95651245117188,\n 38.88729161549412\n ],\n [\n -104.65507507324219,\n 38.88729161549412\n ],\n [\n -104.65507507324219,\n 39.07784203269269\n ],\n [\n -104.95651245117188,\n 39.07784203269269\n ],\n [\n -104.95651245117188,\n 38.88729161549412\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b27e4b07f02db6b1012","contributors":{"authors":[{"text":"Varnes, David J.","contributorId":86322,"corporation":false,"usgs":true,"family":"Varnes","given":"David J.","affiliations":[],"preferred":false,"id":152788,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Scott, Glenn R.","contributorId":102046,"corporation":false,"usgs":true,"family":"Scott","given":"Glenn","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":152789,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cardwell, W. D. E.","contributorId":69120,"corporation":false,"usgs":true,"family":"Cardwell","given":"W.","email":"","middleInitial":"D. E.","affiliations":[],"preferred":false,"id":152787,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jenkins, E. D.","contributorId":9250,"corporation":false,"usgs":true,"family":"Jenkins","given":"E.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":152786,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":34087,"text":"b1238 - 1967 - Volcanic hazards at Mount Rainier, Washington","interactions":[],"lastModifiedDate":"2014-06-06T11:02:23","indexId":"b1238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1238","title":"Volcanic hazards at Mount Rainier, Washington","docAbstract":"

Mount Rainier is a large stratovolcano of andesitic rock in the Cascade Range of western Washington. Although the volcano as it now stands was almost completely formed before the last major glaciation, geologic formations record a variety of events that have occurred at the volcano in postglacial time. Repetition of some of these events today without warning would result in property damage and loss of life on a catastrophic scale. It is appropriate, therefore, to examine the extent, frequency, and apparent origin of these phenomena and to attempt to predict the effects on man of similar events in the future.

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The present report was prompted by a contrast that we noted during a study of surficial geologic deposits in Mount Rainier National Park, between the present tranquil landscape adjacent to the volcano and the violent events that shaped parts of that same landscape in the recent past.

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\n

Natural catastrophes that have geologic causes - such as eruptions, landslides, earthquakes, and floods - all too often are disastrous primarily because man has not understood and made allowance for the geologic environment he occupies. Assessment of the potential hazards of a volcanic environment is especially difficult, for prediction of the time and kind of volcanic activity is still an imperfect art, even at active volcanoes whose behavior has been closely observed for many years. Qualified predictions, however, can be used to plan ways in which hazards to life and property can be minimized.

\n
\n

The prediction of eruptions is handicapped because volcanism results from conditions far beneath the surface of the earth, where the causative factors cannot be seen and, for the most part, cannot be measured. Consequently, long-range predictions at Mount Rainier can be based only on the past behavior of the volcano, as revealed by study of the deposits that resulted from previous eruptions. Predictions of this sort, of course, cannot be specific as to time and locale of future events, and clearly are valid only if the past behavior is, as we believe, a reliable guide.

\n
\n

The purpose of this report is to infer the events recorded by certain postglacial deposits at Mount Rainier and to suggest what bearing similar events in the future might have on land use within and near the park. In addition, table 2 (page 22) gives possible warning signs of an impending eruption. We want to increase man's understanding of a possibly hazardous geologic environment around Mount Rainier volcano, yet we do not wish to imply for certain that the hazards described are either immediate or inevitable. However, we do believe that hazards exist, that some caution is warranted, and that some major hazards can be avoided by judicious planning.

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\n

Most of the events with which we are concerned are sporadic phenomena that have resulted directly or indirectly from volcanic eruptions. Although no eruptions (other than steam emission) of the volcano in historic time are unequivocally known (Hopson and others, 1962), pyroclastic (air-laid) deposits of pumice and rock debris attest to repeated, widely spaced eruptions during the 10,000 years or so of postglacial time. In addition, the constituents of some debris flows indicate an origin during eruptions of molten rock; other debris flows, because of their large size and constituents, are believed to have been caused by steam explosions. Some debris flows, however, are not related to volcanism at all.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/b1238","usgsCitation":"Crandell, D.R., and Mullineaux, D.R., 1967, Volcanic hazards at Mount Rainier, Washington: U.S. Geological Survey Bulletin 1238, v, 26 p., https://doi.org/10.3133/b1238.","productDescription":"v, 26 p.","numberOfPages":"36","onlineOnly":"Y","costCenters":[{"id":617,"text":"Volcano Science Center","active":true,"usgs":true}],"links":[{"id":288142,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/b1238.jpg"},{"id":12497,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/bul/1238/","linkFileType":{"id":5,"text":"html"}},{"id":61999,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1238/pdf/B1238.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Washington","otherGeospatial":"Mount Rainier","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -122.5,46.5 ], [ -122.5,47.5 ], [ -121.5,47.5 ], [ -121.5,46.5 ], [ -122.5,46.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fda34","contributors":{"authors":[{"text":"Crandell, Dwight Raymond","contributorId":6440,"corporation":false,"usgs":true,"family":"Crandell","given":"Dwight","email":"","middleInitial":"Raymond","affiliations":[],"preferred":false,"id":212437,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mullineaux, Donal Ray","contributorId":31759,"corporation":false,"usgs":true,"family":"Mullineaux","given":"Donal","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":212438,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":67235,"text":"i495 - 1967 - (LAC-93) Geologic map of the Mare Humorum region of the moon","interactions":[],"lastModifiedDate":"2023-03-29T17:10:31.229509","indexId":"i495","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"495","subseriesTitle":"NONE","title":"(LAC-93) Geologic map of the Mare Humorum region of the moon","docAbstract":"

The principal feature of the Mare Humorum region is the Humorum basin, a circular mare basin approximately 200 km (kilometer) in diameter. The basin formed early in the history of the moon and was later flooded by mare material. Impact cratering with attendant erosion and aggradation and episodic volcanism and faulting have occurred in the region. The inferred history of the Humorum basin is similar to that of the Imbrium basin (Shoemaker and Hackman, 1962; Titley, 1964), but the more subdued topography and the larger density of craters on the rim of the Humorum basin suggest that it is older than the Imbrium basin. 

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/i495","collaboration":"prepared in cooperation with the National Aeronautics and Space Administration and the USAF Aeronautical Chart and Information Center","usgsCitation":"Titley, S., 1967, (LAC-93) Geologic map of the Mare Humorum region of the moon: U.S. Geological Survey IMAP 495, Report; 1 map, https://doi.org/10.3133/i495.","productDescription":"Report; 1 map","costCenters":[],"links":[{"id":439091,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P1APLDWF","text":"USGS data release","linkHelpText":"Interactive Map: IMAP 495 - (LAC-93) Geologic map of the Mare Humorum region of the moon"},{"id":439090,"rank":4,"type":{"id":30,"text":"Data Release"},"url":"https://doi.org/10.5066/P9Z042ET","text":"USGS data release","linkHelpText":"(LAC-93) Geologic map of the Mare Humorum region of the moon"},{"id":189990,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/0495/report-thumb.jpg"},{"id":115209,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/0495/plate-1.pdf","size":"8729","linkFileType":{"id":1,"text":"pdf"}},{"id":115208,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/0495/report.pdf","size":"47","linkFileType":{"id":1,"text":"pdf"}}],"scale":"1000000","otherGeospatial":"Mare Humorum, Moon","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4905e4b0b290850eed0f","contributors":{"authors":[{"text":"Titley, S.R.","contributorId":60602,"corporation":false,"usgs":true,"family":"Titley","given":"S.R.","affiliations":[],"preferred":false,"id":275828,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68020,"text":"ha238 - 1967 - Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","interactions":[{"subject":{"id":23192,"text":"ofr6336 - 1963 - Floods on White Rock Creek above White Rock Lake at Dallas, Texas","indexId":"ofr6336","publicationYear":"1963","noYear":false,"title":"Floods on White Rock Creek above White Rock Lake at Dallas, Texas"},"predicate":"SUPERSEDED_BY","object":{"id":68020,"text":"ha238 - 1967 - Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","indexId":"ha238","publicationYear":"1967","noYear":false,"title":"Floods on White Rock Creek at Dallas, Texas in 1962 and 1964"},"id":1}],"lastModifiedDate":"2017-06-14T14:10:01","indexId":"ha238","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"238","title":"Floods on White Rock Creek at Dallas, Texas in 1962 and 1964","docAbstract":"

This atlas presents data pertaining to the regimen of flooding along White Rock Creek and its tributaries, Spanky Branch, Floyd Branch, and Cottonwood Creek at Dallas, Texas. The map and flood data were prepared to aid those concerned with, and responsible for, the safe and yet extensive use of the floodplain along White Rock Creek and its tributaries. The flood map is shown in two parts—A, north half, and B, south half.

\n

The map shows areas inundated by the flood of September 21, 1964, along White Rock Creek and Spanky Branch and by the flood of October 8, 1962, along Cottonwood Creek and Floyd Branch.

\n

The flood of September 21, 1964, is known to be the greatest since at least 1886 on White Rock Creek upstream from the Texas and Pacific Railroad (mile 6.6). Downstream from the Texas and Pacific Railroad, White Rock Creek has been subject to inundation from backwater from the Trinity River. The greatest known flood on Trinity River occurred May 25, 1908. Because of extensive flood-control works built since 1908 in the upper Trinity River basin, the degree of flooding resulting from a storm of the magnitude of the 1908 catastrophe probably would be substantially different today. No backwater from Trinity River occurred during the flood of September 21, 1964.

\n

The greatest flood since at least 1892 on Cottonwood Creek and Floyd Branch occurred June 14, 1949. The storm of October 8, 1962, caused flood heights at Forest Lane to be comparable to those of June 14, 1949, on Cottonwood Creek and about 1 foot lower on Floyd Branch. The greatest flood since at least 1917 on Spanky Branch was that of September 21, 1964. Greater floods than those delineated are possible.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha238","collaboration":"Prepared in cooperation with the City of Dallas","usgsCitation":"Ruggles, F.H., and Gilbert, C.R., 1967, Floods on White Rock Creek at Dallas, Texas in 1962 and 1964: U.S. Geological Survey Hydrologic Atlas 238, 36.5 x 51.0 inches, https://doi.org/10.3133/ha238.","productDescription":"36.5 x 51.0 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":326594,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ha238.JPG"},{"id":89268,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/238/plate-1.pdf","text":"Plate 1","size":"8.21 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Plate 1"}],"scale":"24000","country":"United States","state":"Texas","city":"Dallas","otherGeospatial":"White Rock Creek","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -96.83333333333333,32.700833333333335 ], [ -96.83333333333333,33 ], [ -96.70083333333334,33 ], [ -96.70083333333334,32.700833333333335 ], [ -96.83333333333333,32.700833333333335 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d8e4b07f02db5df796","contributors":{"authors":[{"text":"Ruggles, F. H.","contributorId":105805,"corporation":false,"usgs":true,"family":"Ruggles","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277516,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gilbert, Carter R.","contributorId":7667,"corporation":false,"usgs":true,"family":"Gilbert","given":"Carter","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":277515,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":62547,"text":"gq620 - 1967 - Geologic map of the Bordeaux quadrangle, Platte County, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:39","indexId":"gq620","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"620","title":"Geologic map of the Bordeaux quadrangle, Platte County, Wyoming","language":"ENGLISH","doi":"10.3133/gq620","usgsCitation":"McGrew, L.W., 1967, Geologic map of the Bordeaux quadrangle, Platte County, Wyoming: U.S. Geological Survey Geologic Quadrangle 620, 1 map., https://doi.org/10.3133/gq620.","productDescription":"1 map.","costCenters":[],"links":[{"id":103344,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1930.htm","linkFileType":{"id":5,"text":"html"},"description":"1930"},{"id":248707,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0620/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":254017,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0620/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -104.86749999999999,41.8675 ], [ -104.86749999999999,42 ], [ -104.75,42 ], [ -104.75,41.8675 ], [ -104.86749999999999,41.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0be4b07f02db69da78","contributors":{"authors":[{"text":"McGrew, Laura W.","contributorId":102893,"corporation":false,"usgs":true,"family":"McGrew","given":"Laura","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":267527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":67909,"text":"ha241 - 1967 - Water resources of the Roseau River Watershed, Northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-04-02T12:08:38","indexId":"ha241","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"241","title":"Water resources of the Roseau River Watershed, Northwestern Minnesota","docAbstract":"

The drainage area of the Roseau River consists of 2,060 square miles above its confluence with the Red River of the North. About 1,150 square miles lie in the United States and 910 square miles in Canada. This report deals only with that portion within the United States, except for a detailed analysis of low flow characteristics of tributary streams.

\n

Most of the area is within Roseau County, but small portions are in Marshall, Beltrami, Lake of the Woods, and Kittson Counties. Most of the watershed has little relief, and lies entirely within the plain of former Glacial Lake Agassiz. However, the flat topography of this lake washed till plain is broken by beach ridges in its southwestern part and Beltrami Island, a topographic high underlain by sand, in tis southeastern part.

\n

Population within the watershed is about 8000. The town of Roseau, the largest community, has a population of 2146 (1960).

\n

The watershed has an agricultural economy. Spring wheat, oats, and bluegrass seed are the three most important crops in the area, but many other small grains, legumes, and grasses are also grown. Dairy farming and sheep raising are the most important types of livestock production and for many farms stock is the major sources of income.

\n

Large areas of the watershed are peat lands, covered with shrubs, marsh grasslands, and spruce, tamarack, and cedar trees. Forest vegetation in the remainder of the area is largely aspen, but oak is common on the beach ridges and jack pine is common on Beltrami Island.

\n

Outdoor recreation in the area is primarily hunting of deer, small game, and waterfowl.

\n

This report is a general appraisal of the water resources in the Roseau River watershed unit. Detailed studies of water movement through the ground-water reservoir are needed for more exact determination of the amount of water immediately available and the specific effects of water-management practices.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/ha241","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation Division of Waters","usgsCitation":"Winter, T.C., Maclay, R., and Pike, G., 1967, Water resources of the Roseau River Watershed, Northwestern Minnesota: U.S. Geological Survey Hydrologic Atlas 241, 6 Plates: 35.5 x 39.0 inches or smaller, https://doi.org/10.3133/ha241.","productDescription":"6 Plates: 35.5 x 39.0 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":189360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89100,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89099,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89101,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89102,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89103,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":89104,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/241/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Minnesota","otherGeospatial":"Roseau River watershed","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.75,\n 49\n ],\n [\n -96.75,\n 48.75\n ],\n [\n -96.07,\n 48.75\n ],\n [\n -96.07,\n 48.45\n ],\n [\n -95,\n 48.45\n ],\n [\n -95,\n 48.625\n ],\n [\n -95.375,\n 48.625\n ],\n [\n -95.375,\n 49\n ],\n [\n -96.75,\n 49\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0360","contributors":{"authors":[{"text":"Winter, Thomas C.","contributorId":84736,"corporation":false,"usgs":true,"family":"Winter","given":"Thomas","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":277301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Maclay, R.W.","contributorId":72804,"corporation":false,"usgs":true,"family":"Maclay","given":"R.W.","affiliations":[],"preferred":false,"id":277299,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Pike, G.M.","contributorId":80359,"corporation":false,"usgs":true,"family":"Pike","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":277300,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":67979,"text":"ha266 - 1967 - Availability of water in eastern Saunders County, Nebraska","interactions":[],"lastModifiedDate":"2017-11-13T09:32:42","indexId":"ha266","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":318,"text":"Hydrologic Atlas","code":"HA","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"266","title":"Availability of water in eastern Saunders County, Nebraska","docAbstract":"

The sand and gravel deposits of Quaternary age constitute the most important ground-water reservoir and are the source of nearly all the water pumped from wells in the area. An estimated 3.5 million acre-feet for good quality water is stored in these deposits and an additional 1.5 million acre-feet is stored in the underlying Dakota Sandstone. Even larger quantities are stored at greater depths in the Paleozoic dolomites and sandstones, but the water is of poorer quality. 

Pumpage for irrigation since 1956 is estimated to have ranged from about 2,500 acre-feet (1962) to about 6,000 acre-feet (1957). The town of Wahoo annually pumps about 460 acre-feet, and other towns pump an estimated total of 180 acre-feet. In 1963 the City of Lincoln pumped 27,000 acre-feet from its well field alongside the Platte River in the southeast corner of the area; since then pumpage has increased and probably is likely to continue to do so. Pumping at Lincoln city well field induces recharge from Platte River.

The quantity of ground water pumped to date is very small compared to the amount of water stored in the rocks. Furthermore, most of the ground water withdrawn has been replaced by infiltrating precipitation and by influent seepage from the Platte River. The large quantity of ground water in storage in addition to the flow of the Platte River indicates that the water resources of the area, if managed properly, can be developed much more extensively without appreciably depleting the supply.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha266","collaboration":"Prepared in cooperation with the Conservation and Survey Division of the University of Nebraska","usgsCitation":"Souders, V.L., 1967, Availability of water in eastern Saunders County, Nebraska: U.S. Geological Survey Hydrologic Atlas 266, Plate: 51.95 x 34.79 inches, https://doi.org/10.3133/ha266.","productDescription":"Plate: 51.95 x 34.79 inches","costCenters":[],"links":[{"id":89215,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/266/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":186138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/266/report-thumb.jpg"}],"scale":"125000","country":"United States","state":"Nebraska","county":"Saunders County","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -96.95297241210938,\n 41.01202954845378\n ],\n [\n -96.30889892578125,\n 41.01202954845378\n ],\n [\n -96.30889892578125,\n 41.447873389865194\n ],\n [\n -96.95297241210938,\n 41.447873389865194\n ],\n [\n -96.95297241210938,\n 41.01202954845378\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d5cc","contributors":{"authors":[{"text":"Souders, Vernon L.","contributorId":95145,"corporation":false,"usgs":true,"family":"Souders","given":"Vernon","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277441,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":62495,"text":"gq693 - 1967 - Geologic map of the Center quadrangle, south-central Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:00","indexId":"gq693","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"693","title":"Geologic map of the Center quadrangle, south-central Kentucky","language":"ENGLISH","doi":"10.3133/gq693","usgsCitation":"Miller, R., and Moore, S.L., 1967, Geologic map of the Center quadrangle, south-central Kentucky: U.S. Geological Survey Geologic Quadrangle 693, 1 map., https://doi.org/10.3133/gq693.","productDescription":"1 map.","costCenters":[],"links":[{"id":103415,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_2001.htm","linkFileType":{"id":5,"text":"html"},"description":"2001"},{"id":248658,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0693/report.pdf","size":"35","linkFileType":{"id":1,"text":"pdf"}},{"id":253885,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0693/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.75,37.1175 ], [ -85.75,37.25 ], [ -85.61749999999999,37.25 ], [ -85.61749999999999,37.1175 ], [ -85.75,37.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ae4b07f02db69d180","contributors":{"authors":[{"text":"Miller, R.C.","contributorId":47871,"corporation":false,"usgs":true,"family":"Miller","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":267454,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Moore, Samuel L.","contributorId":88727,"corporation":false,"usgs":true,"family":"Moore","given":"Samuel","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":267455,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":63032,"text":"gq629 - 1967 - Geologic map of the Coiltown quadrangle, Hopkins County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:10:47","indexId":"gq629","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1967","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":316,"text":"Geologic Quadrangle","code":"GQ","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"629","title":"Geologic map of the Coiltown quadrangle, Hopkins County, Kentucky","language":"ENGLISH","doi":"10.3133/gq629","usgsCitation":"Franklin, G.J., 1967, Geologic map of the Coiltown quadrangle, Hopkins County, Kentucky: U.S. Geological Survey Geologic Quadrangle 629, 1 map :col. ;79 x 97 cm., https://doi.org/10.3133/gq629.","productDescription":"1 map :col. ;79 x 97 cm.","costCenters":[],"links":[{"id":103353,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_1939.htm","linkFileType":{"id":5,"text":"html"},"description":"1939"},{"id":249164,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/gq/0629/report.pdf","size":"37","linkFileType":{"id":1,"text":"pdf"}},{"id":252165,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/gq/0629/report-thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -87.75,37.25 ], [ -87.75,37.3675 ], [ -87.61749999999999,37.3675 ], [ -87.61749999999999,37.25 ], [ -87.75,37.25 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b09e4b07f02db69c8ec","contributors":{"authors":[{"text":"Franklin, George J.","contributorId":23218,"corporation":false,"usgs":true,"family":"Franklin","given":"George","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":268223,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}