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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha124","usgsCitation":"MacCary, L., 1964, Availability of ground water in the Hazel quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 124, 1 Plate: 47.50 x 34.00 inches, https://doi.org/10.3133/ha124.","productDescription":"1 Plate: 47.50 x 34.00 inches","costCenters":[],"links":[{"id":186117,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89542,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/124/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":413584,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15481.htm","linkFileType":{"id":5,"text":"html"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Hazel quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.375,\n 36.5\n ],\n [\n -88.375,\n 36.625\n ],\n [\n -88.25,\n 36.625\n ],\n [\n -88.25,\n 36.5\n ],\n [\n -88.375,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d952","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":277827,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68480,"text":"ha112 - 1964 - Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","interactions":[],"lastModifiedDate":"2023-03-01T22:50:13.724412","indexId":"ha112","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","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":"112","title":"Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha112","usgsCitation":"Davis, R.W., 1964, Availability of ground water in the Lynn Grove quadrangle, Kentucky-Tennessee: U.S. Geological Survey Hydrologic Atlas 112, 1 Plate: 47.50 x 32.50 inches, https://doi.org/10.3133/ha112.","productDescription":"1 Plate: 47.50 x 32.50 inches","costCenters":[],"links":[{"id":188021,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":413586,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15468.htm","linkFileType":{"id":5,"text":"html"}},{"id":90033,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/112/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Kentucky, Tennessee","otherGeospatial":"Lynn Grove quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.5,\n 36.5\n ],\n [\n -88.5,\n 36.625\n ],\n [\n -88.375,\n 36.625\n ],\n [\n -88.375,\n 36.5\n ],\n [\n -88.5,\n 36.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d936","contributors":{"authors":[{"text":"Davis, R. W.","contributorId":93459,"corporation":false,"usgs":true,"family":"Davis","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":278301,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70190800,"text":"70190800 - 1964 - Selected hydrologic data, upper Sevier River basin, Utah","interactions":[],"lastModifiedDate":"2017-09-14T12:50:52","indexId":"70190800","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5497,"text":"Utah Basic-Data Report","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"8","title":"Selected hydrologic data, upper Sevier River basin, Utah","docAbstract":"This report is intended to serve two purposes: (1) to make available to the public basic ground-water data useful in planning and studying development of water resources, and (2) to supplement an interpretive report that will be published later.
Records were collected during 1961-63 by the U.S. Geological Survey in cooperation with the Utah State Engineer as a part of the investigation of ground-water conditions in the upper Sevier River basin, in parts of Garfield, Iron, Kane, Piute, and Sevier Counties, Utah. The interpretive material will be published in a companion report by Carl H. Carpenter, Gerald B. Robinson, Jr., and Louis J. Bjorklund.
This report is most useful in predicting conditions likely to be found in areas that are being considered as well sites. The person considering the new well can spot the proposed site on plate 1 and examine the records of nearby wells and springs as shown in the tables. From table 1 he can find information on wells, including depth, diameter, water level, yield, drawdown, use of water, temperature of water, and depth of perforations. Table 2 gives information on springs such as yield, use of water, temperature, and improvements. From tables 1 and 2 he can note the type of material that yields water in the vicinity. Table 3 shows the historic fluctuations and trends of water levels. Table 4 shows the type of material penetrated by wells. From table 5 he can note the chemical quality of water from wells and springs, and from table 6, the chemical quality of surface water. If the reader decides from his examination that conditions are favorable, he can place an application to drill a well with the State Engineer. If the State Engineer believes unappropriated water is available, the application may be approved after minimum statutory requirements have been satisfied.
The report is also useful when planning large-scale developments of water supply. This and other uses of the report will be helped by use of the interpretive report upon its release.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with the Utah State Engineer","usgsCitation":"Carpenter, C.H., Robinson, G.B., and Bjorklund, L.J., 1964, Selected hydrologic data, upper Sevier River basin, Utah: Utah Basic-Data Report 8, 29 p.","productDescription":"29 p.","numberOfPages":"37","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345770,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":345769,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.waterrights.utah.gov/cgi-bin/docview.exe?Folder=TP21-1-160&Title=Basic+Data+Report+8"}],"country":"United States","state":"Utah","county":"Garfield County, Iron County, Kane County, Piute County, Sevier County","otherGeospatial":"Sevier River basi","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"59bb953ae4b091459a578226","contributors":{"authors":[{"text":"Carpenter, Carl H.","contributorId":46074,"corporation":false,"usgs":true,"family":"Carpenter","given":"Carl","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":710428,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Robinson, Gerald B. Jr.","contributorId":91837,"corporation":false,"usgs":true,"family":"Robinson","given":"Gerald","suffix":"Jr.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":710429,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bjorklund, Louis Jay","contributorId":21138,"corporation":false,"usgs":true,"family":"Bjorklund","given":"Louis","email":"","middleInitial":"Jay","affiliations":[],"preferred":false,"id":710430,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":70185698,"text":"70185698 - 1964 - Water in the world","interactions":[],"lastModifiedDate":"2017-03-27T16:44:51","indexId":"70185698","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":5341,"text":"The UNESCO Courier","active":true,"publicationSubtype":{"id":10}},"title":"Water in the world","docAbstract":"The earth, Including Its oceans and atmosphere, ls a giant distillation system whose operation brings about the distribution of fresh water throughout the world, from the frozen wastes of polar regions to the burning equatorial deserts. Stated in the simplest terms, distillation, condensation and liquid flow are the elemental processes which, on a grand scale, distribute and circulate throughout the world the water which ls essential for all life.
Water in liquid form absorbs heat energy, chiefly from the sun, and the absorbed energy changes the water from liquid to gaseous form. Transported in the atmosphere, the vapour later meets cooler conditions and condenses as precipitation, some of which replenishes the water in land areas.
Because water is continually being transformed from liquid to vapour and back to liquid again, the whole sequence of events ends where It began. That ls, the condensed moisture in the form of precipitation runs Into or off the surface of the earth, and a part of It collects in rivers which flow to the ocean. The events together form what is called the hydrological cycle.
","largerWorkTitle":"Water and Life","language":"English","publisher":"UNESCO","usgsCitation":"Leopold, L.B., 1964, Water in the world: The UNESCO Courier, v. 17, p. 11-13.","startPage":"11","endPage":"13","costCenters":[],"links":[{"id":338428,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":338427,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.unesco.org/new/en/unesco-courier/archives/","text":"Journal Archives","linkHelpText":"Article is findable using the search function"}],"volume":"17","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"58da2540e4b0543bf7fda87f","contributors":{"authors":[{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":686428,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70010816,"text":"70010816 - 1964 - Ground water in North America","interactions":[],"lastModifiedDate":"2017-03-27T12:47:37","indexId":"70010816","displayToPublicDate":"1964-01-01T00:00:00","publicationYear":"1964","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3338,"text":"Science","active":true,"publicationSubtype":{"id":10}},"title":"Ground water in North America","docAbstract":"The fast-growing demands on this natural resource expose a need to resolve many hydrologic unknowns.","language":"English","publisher":"American Association for the Advancement of Science","doi":"10.1126/science.143.3610.1001","issn":"00368075","usgsCitation":"Thomas, H.E., and Leopold, L.B., 1964, Ground water in North America: Science, v. 143, no. 3610, p. 1001-1006, https://doi.org/10.1126/science.143.3610.1001.","productDescription":"6 p.","startPage":"1001","endPage":"1006","costCenters":[],"links":[{"id":218743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"North America","volume":"143","issue":"3610","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a2ad0e4b0c8380cd5b4a7","contributors":{"authors":[{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":359714,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leopold, Luna Bergere","contributorId":93884,"corporation":false,"usgs":true,"family":"Leopold","given":"Luna","email":"","middleInitial":"Bergere","affiliations":[],"preferred":false,"id":359715,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70179734,"text":"70179734 - 1963 - Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","interactions":[],"lastModifiedDate":"2017-09-06T17:19:25","indexId":"70179734","displayToPublicDate":"2016-12-01T00:00:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5485,"text":"Utah Geological and Mineralogical Survey Water-Resources Bulletin","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"3-I","title":"Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data","docAbstract":"This report presents the data collected for a study of the dissolved-mineral load contributed by surficial sources to Great Salt Lake, Utah. The study was conducted by the U.S. Geological Survey in cooperation with the University of Utah during the period from July 1959 through June 1962, and is part of an overall investigation of the Great Salt Lake basin by the University. Financial support for the study was provided by the U.S. Geological Survey and by the University of Utah Research Fund and Uniform School Fund. Some of the data presented in this report were obtained as part of cooperative programs between the Geological Survey and other agencies.
","language":"English","publisher":"Utah Geological and Minerological Society","publisherLocation":"Salt Lake City, UT","collaboration":"Prepared in cooperation with The College of Mines and Mineral Industries, University of Utah, Salt Lake City, Utah","usgsCitation":"Hahl, D.C., and Mitchell, C., 1963, Dissolved-mineral inflow to Great Salt Lake and chemical characteristics of the salt lake brine. Part I: Selected hydrologic data: Utah Geological and Mineralogical Survey Water-Resources Bulletin 3-I, 39 p.","productDescription":"39 p.","numberOfPages":"51","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":345533,"rank":3,"type":{"id":22,"text":"Related Work"},"url":"https://pubs.usgs.gov/publication/70179736","text":"Part II: Technical report"},{"id":345532,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://ugspub.nr.utah.gov/publications/water_resources_bulletins/WRB-3part1.pdf"},{"id":333225,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Great Salt Lake","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -113.2305908203125,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 41.795888098191426\n ],\n [\n -111.81884765624999,\n 40.59727063442024\n ],\n [\n -113.2305908203125,\n 40.59727063442024\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5879f5ade4b0847d353f44d6","contributors":{"authors":[{"text":"Hahl, D. C.","contributorId":57436,"corporation":false,"usgs":true,"family":"Hahl","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":658473,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mitchell, C.G.","contributorId":177183,"corporation":false,"usgs":true,"family":"Mitchell","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":658474,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":71791,"text":"tei840 - 1963 - A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","interactions":[],"lastModifiedDate":"2014-07-16T14:13:44","indexId":"tei840","displayToPublicDate":"2013-07-16T14:10:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":337,"text":"Trace Elements Investigations","code":"TEI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"840","title":"A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water","docAbstract":"No abstract available.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/tei840","collaboration":"Prepared on behalf of the U.S. Atomic Energy Commission.","usgsCitation":"Winograd, I.J., 1963, A summary of the ground-water hydrology of the area between the Las Vegas Valley and the Amargosa Desert, Nevada, with special reference to the effects of possible new withdrawals of ground water: U.S. Geological Survey Trace Elements Investigations 840, Report: 79 p.; 1 Map, https://doi.org/10.3133/tei840.","productDescription":"Report: 79 p.; 1 Map","costCenters":[],"links":[{"id":290305,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Nevada","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -116.4011,36.2803 ], [ -116.4011,36.6184 ], [ -115.2713,36.6184 ], [ -115.2713,36.2803 ], [ -116.4011,36.2803 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53c79ee2e4b0194841642416","contributors":{"authors":[{"text":"Winograd, Isaac Judah","contributorId":9233,"corporation":false,"usgs":true,"family":"Winograd","given":"Isaac","email":"","middleInitial":"Judah","affiliations":[],"preferred":false,"id":284759,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","interactions":[{"subject":{"id":52309,"text":"ofr6316 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"ofr6316","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":70047480,"text":"70047480 - 1963 - Hydrology of Brooklyn Lake near Keystone Heights, Florida","indexId":"70047480","publicationYear":"1963","noYear":false,"title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida"},"id":1}],"lastModifiedDate":"2017-09-13T17:55:27","indexId":"70047480","displayToPublicDate":"2013-01-01T13:24:00","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5489,"text":"Florida Geological Survey Report of Investigations","active":false,"publicationSubtype":{"id":2}},"seriesNumber":"33","title":"Hydrology of Brooklyn Lake near Keystone Heights, Florida","docAbstract":"Brooklyn Lake receded about 20 feet during 1954-58 and reached its lowest stage of record (97.2 feet) in February 1958; this was the lowest stage in the memory of longtime residents. This unusually large recession was a result of deficient rainfall during more than a 3-year period, January 1954 to May 1957. However, by October 1959, after 2 1/2 years of above normal rainfall, the lake had recovered and water was flowing through the surface outlet.","language":"English","publisher":"Florida Geological Survey","publisherLocation":"Tallahassee, FL","collaboration":"Prepared by the United States Geological Survey in cooperation with the Florida Geological Survey","usgsCitation":"Clark, W.E., Musgrove, R.H., Menke, C.G., and Cagle, J.W., 1963, Hydrology of Brooklyn Lake near Keystone Heights, Florida: Florida Geological Survey Report of Investigations 33, viii, 43 p.","productDescription":"viii, 43 p.","costCenters":[],"links":[{"id":276166,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/70047480.PNG"},{"id":276162,"type":{"id":11,"text":"Document"},"url":"https://ufdc.ufl.edu/UF00001220/00001/pdf?search=report+%3dinvestigations"}],"country":"United States","state":"Florida","otherGeospatial":"Brooklyn Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.16,29.71 ], [ -82.16,29.86 ], [ -81.95,29.86 ], [ -81.95,29.71 ], [ -82.16,29.71 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5203a37be4b02bdb1bc63fc4","contributors":{"authors":[{"text":"Clark, William E.","contributorId":105365,"corporation":false,"usgs":true,"family":"Clark","given":"William","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":482149,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Musgrove, Rufus H.","contributorId":20245,"corporation":false,"usgs":true,"family":"Musgrove","given":"Rufus","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":482146,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Menke, Clarence G.","contributorId":25450,"corporation":false,"usgs":true,"family":"Menke","given":"Clarence","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":482147,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cagle, Joseph W. Jr.","contributorId":78640,"corporation":false,"usgs":true,"family":"Cagle","given":"Joseph","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":482148,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":70039573,"text":"70039573 - 1963 - Use of hydrologic models in the analysis of flood runoff","interactions":[],"lastModifiedDate":"2012-08-14T01:01:44","indexId":"70039573","displayToPublicDate":"2012-01-01T16:11:06","publicationYear":"1963","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":6,"text":"USGS Unnumbered Series"},"seriesTitle":{"id":371,"text":"Monograph","active":false,"publicationSubtype":{"id":6}},"title":"Use of hydrologic models in the analysis of flood runoff","docAbstract":"The analog technique is applied to the analysis of flood runoff. A quasi-linear analog model has been developed for simulating the runoff-producing characteristics of a drainage system. Where storage is linear a unique relationship correlating the inflow and outflow peaks is derived. The technique for synthesizing flood-frequency distribution is also discussed. 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