{"pageNumber":"649","pageRowStart":"16200","pageSize":"25","recordCount":16437,"records":[{"id":55761,"text":"ofr5731 - 1957 - Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California","interactions":[],"lastModifiedDate":"2014-05-21T08:06:20","indexId":"ofr5731","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-31","title":"Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California","docAbstract":"<p>At the request of the United States Forest Service, the Ground Water Branch of the United Stated Geological Survey made a reconnaissance of the geologic features and water resources of the Dora Belle Campground in Sierra National Forest on the shore of Shaver Lake, Fresno County, California.</p>\n<br>\n<p>Basically, the water-supply problem at Dora Belle Campground is that the present supply obtained from a spring is not adequate to meet the present summer demand, and is of poor quality. Plans call for a considerable increase in camping facilities.. This, it is imperative that the present supply be augmented or, preferably, be replaced entirely. the Forest Service estimated the future peak demand to be about 25,00 gallons per day.</p>\n<br>\n<p>On October 28, 1957, the writer examined the are in the company of C. H. Fankboner, Assistant Forest Engineer, Sierra National Forest, and Ben Dix, Construction and Maintenance Foreman, Pine Ridge District. Field work, done on October 28th and 29th, consisted of a brief geologic reconnaissance to determine the rock types and geologic structure, and a hydrologic reconnaissance consisting of a partial inventory of water walls and springs in the vicinity of the campground. A spring box near the western edge of Bell Diamond Meadow was pumped out with a Forest Service pump truck to determine its rate of recovery and potential production.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Sacramento, CA","doi":"10.3133/ofr5731","collaboration":"Prepared at the request of the Department of Agriculture, Forest Service","usgsCitation":"Davis, G.H., 1957, Reconnaissance investigation of ground-water supply for Dora Belle Campground, Shaver Lake, California: U.S. Geological Survey Open-File Report 57-31, 17 p., https://doi.org/10.3133/ofr5731.","productDescription":"17 p.","numberOfPages":"22","costCenters":[],"links":[{"id":287371,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287370,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0031/report.pdf"}],"country":"United States","state":"California","otherGeospatial":"Shaver Lake","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -119.374409,37.035345 ], [ -119.374409,37.158277 ], [ -119.242267,37.158277 ], [ -119.242267,37.035345 ], [ -119.374409,37.035345 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6ce4b07f02db63eba4","contributors":{"authors":[{"text":"Davis, G. H.","contributorId":40963,"corporation":false,"usgs":true,"family":"Davis","given":"G.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":254206,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":56087,"text":"ofr5790 - 1957 - Hydrology and water law: what is their future common ground?","interactions":[],"lastModifiedDate":"2014-05-21T09:33:55","indexId":"ofr5790","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-90","title":"Hydrology and water law: what is their future common ground?","docAbstract":"<p>We live in an age of social and economic evolution--evolution so deep reaching and rapid it constitutes ad revolution in numerous fields of human concern. Long-standing concepts of what is appropriate and orderly face drastic modification if they are to survive. To this situation the principles of applied hydrology and the tenets of water law are no exceptions. Their common ground, incomplete in the past, becomes tenuous when projected into the future.</p>\n<br>\n<p>To hydrologists it is common knowledge that the Nation has some trouble spots tin water supply, occasioned by burgeoning population, by standards of living that seem luxurious to other peoples if not to us, and by tremendously dynamic industry whose voracious thirst for water seems insatiable. Seldom is the \"trouble\" a mere lack of water in a quantity sufficient to serve all real needs; rather, water usually is available only part of the time, at greater-than-customary cost, or under competition among several potential uses. We can expect only that such spots will increase in number and in geographic reach.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5790","usgsCitation":"Piper, A., and Thomas, H.E., 1957, Hydrology and water law: what is their future common ground?: U.S. Geological Survey Open-File Report 57-90, 33 p., https://doi.org/10.3133/ofr5790.","productDescription":"33 p.","numberOfPages":"34","costCenters":[],"links":[{"id":287407,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287406,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0090/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e871","contributors":{"authors":[{"text":"Piper, Arthur M.","contributorId":65060,"corporation":false,"usgs":true,"family":"Piper","given":"Arthur M.","affiliations":[],"preferred":false,"id":254748,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thomas, Harold E.","contributorId":36116,"corporation":false,"usgs":true,"family":"Thomas","given":"Harold","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":254747,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":55777,"text":"ofr5768 - 1957 - Reconnaissance of the water resources of the Lonesome Valley area, Yavapai County, Arizona","interactions":[],"lastModifiedDate":"2014-05-21T08:43:42","indexId":"ofr5768","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-68","title":"Reconnaissance of the water resources of the Lonesome Valley area, Yavapai County, Arizona","docAbstract":"<p>In accordance with a request from its cooperating agency, the Arizona State Land Department, the U.S. Geological Survey has made a brief reconnaissance of the water resources of the Lonesome Valley area, Yavapai County, Ariz., to determine the probable hydrologic effects of a proposed dam on Lynx Creek. The construction of this dam has been proposed by the Arizona Game and Fish Department, for recreational and fish-cultural purposes.</p>\n<br>\n<p>Data on the geology of the area were furnished by Mrs. Medora M. Krieger, geologist, Geologic Division, U.S. Geological Survey, and the map was prepared by Floyd R. Twenter, geologist, Ground Water Branch.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Phoenix, AZ","doi":"10.3133/ofr5768","collaboration":"Prepared in cooperation with the Arizona State Land Department","usgsCitation":"Metzger, D., 1957, Reconnaissance of the water resources of the Lonesome Valley area, Yavapai County, Arizona: U.S. Geological Survey Open-File Report 57-68, Report: 4 p.; 1 Plate: 7.37 x 7.81 inches, https://doi.org/10.3133/ofr5768.","productDescription":"Report: 4 p.; 1 Plate: 7.37 x 7.81 inches","numberOfPages":"5","costCenters":[],"links":[{"id":287393,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0068/report.pdf"},{"id":287394,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287392,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1957/0068/plate-1.pdf"}],"country":"United States","state":"Arizona","county":"Yavapai County","otherGeospatial":"Lonesome Valley","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.3342,33.8882 ], [ -113.3342,35.5311 ], [ -111.4613,35.5311 ], [ -111.4613,33.8882 ], [ -113.3342,33.8882 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636a3b","contributors":{"authors":[{"text":"Metzger, Donald G.","contributorId":44226,"corporation":false,"usgs":true,"family":"Metzger","given":"Donald G.","affiliations":[],"preferred":false,"id":254229,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":22821,"text":"ofr5730 - 1957 - Progress report of hydrology and sedimentation in Bixler Run, Corey Creek, and Elk Run watersheds, Pennsylvania","interactions":[],"lastModifiedDate":"2024-12-27T20:59:46.865069","indexId":"ofr5730","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-30","title":"Progress report of hydrology and sedimentation in Bixler Run, Corey Creek, and Elk Run watersheds, Pennsylvania","docAbstract":"<p>This report describes the results of an investigation in progress and presents some tentative findings from a study of hydrology and sedimentation of three small watersheds where soil conservation practices are being applied. The study was begun in April 1954, to determine precipitation, runoff, probable sources and yields of sediment, and channel changes in two small watersheds in Pennsylvania. This report covers the period April 1954, to September 30, 1955 with the exception of the aggradation-degradation range data which covers the period October 1954 to November 1956. The internal or time control method of calibration is being used for the Bixler Run watershed study, and an external control is being used in the Corey Creek study.</p><p>Precipitation on Bixler Run watershed was 47.33 inches for the 1955 water year. Total runoff was 14.08 inches and the suspended sediment yield was 1,143.3 tons or 76 tons per square mile of drainage area. Precipitation on Corey Creek watershed for the same period totaled 35.81 inches. The total runoff was 8.37 inches and the suspended-sediment yield was 713.0 tons or 58.2 tons per square mile of drainage area. The precipitation on Elk Run, external control watershed for the Corey Creek study was 34.54 inches. The runoff was 10.10 inches and the suspended sediment yield was 709.9 tons or 69.5 tons per square mile.</p><p>Results from the study of channel changes by means of sediment aggradation-degradation ranges showed fill in all three watersheds. Bixler Run showed an average channel fill of 1.3 square feet per stream cross section. Corey Creek and Elk Run watersheds showed average fills of 2.9 and 4.1 square feet per cross section respectively. Most of the sediments comprising this fill were in the particle size range of gravel and coarser material.</p><p>The water in all three watersheds was low in dissolved solids during the period of investigation, varying from 72 to 127 ppm in Bixler Run, from 58 to 130 ppm in Corey Creek, and from 58 to 117 ppm in Elk Run. These waters are essentially of the secondary alkaline type with calcium and magnesium bicarbonate being the main dissolved constituents.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/ofr5730","issn":"0094-9140","usgsCitation":"Culbertson, J., 1957, Progress report of hydrology and sedimentation in Bixler Run, Corey Creek, and Elk Run watersheds, Pennsylvania: U.S. Geological Survey Open-File Report 57-30, iii, 44 p., https://doi.org/10.3133/ofr5730.","productDescription":"iii, 44 p.","numberOfPages":"49","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":155477,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr5730.PNG"},{"id":330297,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0030/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":465502,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52766.htm","text":"Corey Creek and Elk Run watersheds","linkFileType":{"id":5,"text":"html"}},{"id":465503,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_52770.htm","text":"Bixier Run watershed","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Bixler Run Watershed, Corey Creek Watershed, Elk Run Watershed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.0833,\n              41.8553\n            ],\n            [\n              -77.0833,\n              41.7561\n            ],\n            [\n              -76.9639,\n              41.7561\n            ],\n            [\n              -76.9639,\n              41.8553\n            ],\n            [\n              -77.0833,\n              41.8553\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    },\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -77.4972,\n              40.4214\n            ],\n            [\n              -77.4972,\n              40.3633\n            ],\n            [\n              -77.3833,\n              40.3633\n            ],\n            [\n              -77.3833,\n              40.4214\n            ],\n            [\n              -77.4972,\n              40.4214\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65df78","contributors":{"authors":[{"text":"Culbertson, J.K.","contributorId":11649,"corporation":false,"usgs":true,"family":"Culbertson","given":"J.K.","email":"","affiliations":[],"preferred":false,"id":188937,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55773,"text":"ofr5758 - 1957 - Geology and ground-water hydrology of the Oahe unit, James River division, South Dakota: Appendixes A, B, C, and E","interactions":[{"subject":{"id":55773,"text":"ofr5758 - 1957 - Geology and ground-water hydrology of the Oahe unit, James River division, South Dakota: Appendixes A, B, C, and E","indexId":"ofr5758","publicationYear":"1957","noYear":false,"title":"Geology and ground-water hydrology of the Oahe unit, James River division, South Dakota: Appendixes A, B, C, and E"},"predicate":"SUPERSEDED_BY","object":{"id":2054,"text":"wsp1425 - 1957 - Ground water in the Crow Creek-Sand Lake area, Brown and Marshall Counties, South Dakota","indexId":"wsp1425","publicationYear":"1957","noYear":false,"title":"Ground water in the Crow Creek-Sand Lake area, Brown and Marshall Counties, South Dakota"},"id":1}],"supersededBy":{"id":2054,"text":"wsp1425 - 1957 - Ground water in the Crow Creek-Sand Lake area, Brown and Marshall Counties, South Dakota","indexId":"wsp1425","publicationYear":"1957","noYear":false,"title":"Ground water in the Crow Creek-Sand Lake area, Brown and Marshall Counties, South Dakota"},"lastModifiedDate":"2013-08-29T10:09:33","indexId":"ofr5758","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-58","title":"Geology and ground-water hydrology of the Oahe unit, James River division, South Dakota: Appendixes A, B, C, and E","language":"ENGLISH","doi":"10.3133/ofr5758","usgsCitation":"Jones, J., and and others, 1957, Geology and ground-water hydrology of the Oahe unit, James River division, South Dakota: Appendixes A, B, C, and E: U.S. Geological Survey Open-File Report 57-58, 718 p.; 3 pls., https://doi.org/10.3133/ofr5758.","productDescription":"718 p.; 3 pls.","costCenters":[],"links":[{"id":181732,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67ac92","contributors":{"authors":[{"text":"Jones, J.R.","contributorId":15967,"corporation":false,"usgs":true,"family":"Jones","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":254224,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":532395,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":53638,"text":"ofr57123 - 1957 - A reconnaissance report on the geology and hydrology of the western part of the province of Fezzan, United Kingdom of Libya","interactions":[],"lastModifiedDate":"2012-02-02T00:11:42","indexId":"ofr57123","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-123","title":"A reconnaissance report on the geology and hydrology of the western part of the province of Fezzan, United Kingdom of Libya","language":"ENGLISH","doi":"10.3133/ofr57123","usgsCitation":"Whitcomb, H.A., 1957, A reconnaissance report on the geology and hydrology of the western part of the province of Fezzan, United Kingdom of Libya: U.S. Geological Survey Open-File Report 57-123, vi, 102 p. : ill. ; 28 cm., https://doi.org/10.3133/ofr57123.","productDescription":"vi, 102 p. : ill. ; 28 cm.","costCenters":[],"links":[{"id":177071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1957/0123/report-thumb.jpg"},{"id":87519,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1957/0123/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":87520,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0123/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a856c","contributors":{"authors":[{"text":"Whitcomb, Harold A.","contributorId":102868,"corporation":false,"usgs":true,"family":"Whitcomb","given":"Harold","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":247971,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14401,"text":"ofr5760 - 1957 - Records available to September 30, 1956, on use of water in the Delaware Basin Project area","interactions":[],"lastModifiedDate":"2014-05-21T08:30:12","indexId":"ofr5760","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-60","title":"Records available to September 30, 1956, on use of water in the Delaware Basin Project area","docAbstract":"<p>The purpose of this report is to summarize data on the use of water in the Delaware Basin Project area (fig. 2) and to list the principal data sources that are available in published form. The tables and bibliography will assist Geological Survey personnel  assigned to the Delaware Basin Project in evaluating the scope and deficiencies of previous studies of the basin. Information is also given on the use of water by public supplies in the New York-New Jersey region comprising the New York City Metropolitan Area and in the remaining north-central and south-eastern parts of New Jersey. These regions may depend increasingly on water from the Delaware River basin for part of their public supplies.</p>\n<br>\n<p>The Geological Survey has the responsibility for appraising and describing the water resources of the Nation as a guide to use, development, control, and conservation of these resources. Cooperative Federal-State water-resources investigations in the Delaware Basin States have been carried on the the Geological Survey for more than 50 years. In July 1956 the Survey began the \"Delaware Basin Project,\" a hydrologic study of the Delaware River basin in order to: 1) Determine present status and trends in water availability, quality, and use, 2) assess and improve the adequacy of the Survey's basic water data program in the basin, 3) interpret and evaluate the water-resources data in terms of past and possible future water-use and land-use practices, and 4) disseminate promptly the results of this investigation for the benefit of all interested agencies and the general public. The Geological Survey is working closely with the U.S. Corps of Engineers and other cooperating Federal and State agencies in providing water data which will contribute to the present coordinated investigation aimed at developing a plan for long-range water development in the Delaware River basin.</p>\n<br>\n<p>Estimates of quantities of water used are given for water withdrawn from streams and aquifers during calendar year 1955, as compiled or estimated from publications and manuscripts prepared between 1950 and 1956. All quantities are given in millions of gallons per day (mgd). The source of the water used, ground or surface, and the type of use to which is was put -- public supply, industrial supply, irrigation, or rural use -- is given. Use of water for hydroelectric power was not compiled for this report. Most tables in this report do not subdivide withdrawals into fresh and saline water; however, most supplies are fresh, except some of those withdrawn directly from the Delaware River downstream from Philadelphia, Pa. All quantities are expressed as an average rate for a full year and are lower, therefore, than rates resulting from the increased demand for water during the summer for air conditioning and supplemental irrigation.</p>\n<br>\n<p>The primary emphasis of this study was to get an over-all picture of water use throughout large parts of the basin. Therefore, publications relating to a dingle city or county, other than New York City, seldom were used; revisions and refinement based on such sources of information are best made by the field personnel most familiar with locally filed publications and published data. </p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington D.C.","doi":"10.3133/ofr5760","usgsCitation":"Kammerer, J., 1957, Records available to September 30, 1956, on use of water in the Delaware Basin Project area: U.S. Geological Survey Open-File Report 57-60, ii, 33 p., https://doi.org/10.3133/ofr5760.","productDescription":"ii, 33 p.","numberOfPages":"37","costCenters":[],"links":[{"id":287385,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":287384,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1957/0060/report.pdf"}],"country":"United States","state":"Delaware","otherGeospatial":"Delaware Basin","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -76.0,39.0 ], [ -76.0,42.0 ], [ -75.0,42.0 ], [ -75.0,39.0 ], [ -76.0,39.0 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db63579e","contributors":{"authors":[{"text":"Kammerer, John C.","contributorId":53815,"corporation":false,"usgs":true,"family":"Kammerer","given":"John C.","affiliations":[],"preferred":false,"id":169392,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":47192,"text":"ofr5726 - 1957 - Four maps and 38 graphs showing hydrologic and quality-of-water features east of Roswell, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:04:54","indexId":"ofr5726","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1957","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":"57-26","title":"Four maps and 38 graphs showing hydrologic and quality-of-water features east of Roswell, New Mexico","language":"ENGLISH","doi":"10.3133/ofr5726","usgsCitation":"onover, C.S., 1957, Four maps and 38 graphs showing hydrologic and quality-of-water features east of Roswell, New Mexico: U.S. Geological Survey Open-File Report 57-26, 4 maps., https://doi.org/10.3133/ofr5726.","productDescription":"4 maps.","costCenters":[],"links":[{"id":135237,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a9101","contributors":{"authors":[{"text":"onover, Clyde Stuart","contributorId":90278,"corporation":false,"usgs":true,"family":"onover","given":"Clyde","email":"","middleInitial":"Stuart","affiliations":[],"preferred":false,"id":234798,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":70174078,"text":"70174078 - 1957 - Drainage areas of Iowa streams","interactions":[],"lastModifiedDate":"2025-07-23T17:34:34.200527","indexId":"70174078","displayToPublicDate":"1960-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":2,"text":"State or Local Government Series"},"seriesTitle":{"id":5105,"text":"Iowa Highway Research Board Bulletin","active":true,"publicationSubtype":{"id":2}},"seriesNumber":"7","title":"Drainage areas of Iowa streams","docAbstract":"<p>The drainage area of a stream at a specified location ordinarily may be defined as that area, measured in a horizontal plane, which is enclosed by a topographic divide such that direct surface runoff from precipitation would drain by gravity into the river basin above the specified point.</p>\n<p>One of the most important factors in the hydrologic computation for the design of structures on or over watercourses is the drainage area upstream from the point under consideration. Other hydrologic studies such as low-flow, flood-frequency analyses, rainfall-runoff correlations, stream density, and area-distance make use of this factor as a basic premise for computation.</p>\n<p>In order that the drainage-area information of the interior streams of Iowa be of uniform accuracy and available to all users of these data, this report has been compiled, and the drainage areas of all streams in excess of 5 square mies are listed. For the larger streams, drainage areas have been determined at numerous intermediate points. As a result of this report much basic background material has been compiled that will he useful in future hydrologic studies of drainage basin characteristics.</p>\n<p>This publication is limited to the presentation of the drainage-area data for the interior streams of the State. The methods of application of these data to the study of streamflow characteristics, and the design of related structures are properly the function of the design engineer and are not discussed herein.</p>","language":"English","publisher":"Iowa Highway Research Board","usgsCitation":"Larimer, O., 1957, Drainage areas of Iowa streams: Iowa Highway Research Board Bulletin 7, 404 p.","productDescription":"404 p.","numberOfPages":"404","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science Center","active":true,"usgs":true}],"links":[{"id":324436,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/unnumbered/70174078/DAIowaStreams1957.pdf","size":"20.1 MB","linkFileType":{"id":1,"text":"pdf"}},{"id":324437,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United 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,{"id":70010722,"text":"70010722 - 1957 - Modified determination of radium in water","interactions":[],"lastModifiedDate":"2023-03-20T16:48:23.586049","indexId":"70010722","displayToPublicDate":"1957-01-01T00:00:00","publicationYear":"1957","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":761,"text":"Analytical Chemistry","active":true,"publicationSubtype":{"id":10}},"title":"Modified determination of radium in water","docAbstract":"<p>The proposed method embodies a barium sulfate carrier precipitation, filtration through molecular filter membranes, and collection of activity after prescribed aging period. The method is sufficiently accurate and precise to indicate the potability of water and for use in general studies of radium in chemical hydrology. Amounts of radium as low as 0.1 <i><span>μ</span><span>μ</span></i>c. can be detected by using 1 -hour counting times. Radium-226 is used as the standard and the results indicate about 100 to 110 % of the activity of the alpha-emitting radium isotopes as radium-223, radium-224, and radium-226.</p>","language":"English","publisher":"ACS Publications","doi":"10.1021/ac60131a003","usgsCitation":"Barker, F.B., and Thatcher, L.L., 1957, Modified determination of radium in water: Analytical Chemistry, v. 29, no. 11, p. 1573-1575, https://doi.org/10.1021/ac60131a003.","productDescription":"3 p.","startPage":"1573","endPage":"1575","numberOfPages":"3","costCenters":[],"links":[{"id":219556,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"29","issue":"11","noUsgsAuthors":false,"publicationDate":"2002-05-01","publicationStatus":"PW","scienceBaseUri":"505a5cc8e4b0c8380cd6ff3d","contributors":{"authors":[{"text":"Barker, F. B.","contributorId":88709,"corporation":false,"usgs":true,"family":"Barker","given":"F.","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":359491,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thatcher, L. L.","contributorId":23271,"corporation":false,"usgs":true,"family":"Thatcher","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":359490,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70175988,"text":"70175988 - 1956 - Progress report on the ground-water hydrology of the Equus-beds area, Kansas","interactions":[],"lastModifiedDate":"2016-08-23T11:21:30","indexId":"70175988","displayToPublicDate":"2015-12-07T00:00:00","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2579,"text":"Kansas Geological Survey Bulletin","active":true,"publicationSubtype":{"id":10}},"title":"Progress report on the ground-water hydrology of the Equus-beds area, Kansas","language":"English","publisher":"University of Kansas","publisherLocation":"Lawrence, KS","usgsCitation":"Stramel, G., 1956, Progress report on the ground-water hydrology of the Equus-beds area, Kansas: Kansas Geological Survey Bulletin, v. 119, no. 1, 59 p. .","productDescription":"59 p. ","costCenters":[{"id":353,"text":"Kansas Water Science Center","active":false,"usgs":true}],"links":[{"id":327637,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"},{"id":327636,"rank":1,"type":{"id":15,"text":"Index Page"},"url":"https://www.kgs.ku.edu/General/geologyBulls.html"}],"volume":"119","issue":"1","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"57bd73ede4b03fd6b7df2d72","contributors":{"authors":[{"text":"Stramel, G.J.","contributorId":47768,"corporation":false,"usgs":true,"family":"Stramel","given":"G.J.","affiliations":[],"preferred":false,"id":646760,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14337,"text":"ofr5662 - 1956 - Preliminary report on waterpower possibilities of Bradley Lake, Alaska, with a chapter on tentative geologic conclusions on Bradley Lake power site","interactions":[],"lastModifiedDate":"2024-01-03T20:29:29.941739","indexId":"ofr5662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-62","title":"Preliminary report on waterpower possibilities of Bradley Lake, Alaska, with a chapter on tentative geologic conclusions on Bradley Lake power site","docAbstract":"<p>The purpose of this report is to give a preliminary estimate of the power possibilities of Bradley Lake, Alaska, and to describe outstanding hydrologic, geologic and topographic features that might determine the character of development. Bradley Lake lies in the Kenai Mountains near the southwestern end of the Kenai Peninsula. It is at an altitude of 1,090 feet, at a point about 25 miles northeast of the town of Homer, and about 3 miles southward from the head of Kachemak Bay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr5662","usgsCitation":"Johnson, F., and Soward, K.S., 1956, Preliminary report on waterpower possibilities of Bradley Lake, Alaska, with a chapter on tentative geologic conclusions on Bradley Lake power site: U.S. Geological Survey Open-File Report 56-62, Report: 85 p.; 3 Plates: 27.52 x 21.40 inches or smaller, https://doi.org/10.3133/ofr5662.","productDescription":"Report: 85 p.; 3 Plates: 27.52 x 21.40 inches or smaller","costCenters":[],"links":[{"id":424092,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0062/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":148271,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1956/0062/report-thumb.jpg"},{"id":424091,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0062/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424090,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1956/0062/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":424089,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1956/0062/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alaska","otherGeospatial":"Bradley Lake","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -149.19967142964998,\n              61.55478240758791\n            ],\n            [\n              -149.19967142964998,\n              61.55099595914939\n            ],\n            [\n              -149.18414234890037,\n              61.55099595914939\n            ],\n            [\n              -149.18414234890037,\n              61.55478240758791\n            ],\n            [\n              -149.19967142964998,\n              61.55478240758791\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aade4b07f02db66b4f6","contributors":{"authors":[{"text":"Johnson, Fred A.","contributorId":93863,"corporation":false,"usgs":true,"family":"Johnson","given":"Fred A.","affiliations":[],"preferred":false,"id":169284,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Soward, Kenneth S.","contributorId":39351,"corporation":false,"usgs":true,"family":"Soward","given":"Kenneth","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":169283,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":51905,"text":"ofr5640 - 1956 - Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955","interactions":[{"subject":{"id":51905,"text":"ofr5640 - 1956 - Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955","indexId":"ofr5640","publicationYear":"1956","noYear":false,"title":"Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955"},"predicate":"SUPERSEDED_BY","object":{"id":1297,"text":"wsp1586A - 1961 - Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","indexId":"wsp1586A","publicationYear":"1961","noYear":false,"chapter":"A","title":"Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55"},"id":1}],"supersededBy":{"id":1297,"text":"wsp1586A - 1961 - Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55","indexId":"wsp1586A","publicationYear":"1961","noYear":false,"title":"Water quality and hydrology in the Fort Belvoir area, Virginia, 1954-55"},"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr5640","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-40","title":"Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955","language":"ENGLISH","doi":"10.3133/ofr5640","usgsCitation":"Durfor, C., 1956, Investigation of water-quality hydrology in the Ft. Belvoir, Virginia area, 1954-1955: U.S. Geological Survey Open-File Report 56-40, 115 p., https://doi.org/10.3133/ofr5640.","productDescription":"115 p.","costCenters":[],"links":[{"id":177001,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47b3e4b07f02db49ed08","contributors":{"authors":[{"text":"Durfor, C.N.","contributorId":10094,"corporation":false,"usgs":true,"family":"Durfor","given":"C.N.","affiliations":[],"preferred":false,"id":244458,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68202,"text":"ha8 - 1956 - Availability of ground water for domestic use in Jefferson County, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:28","indexId":"ha8","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"8","title":"Availability of ground water for domestic use in Jefferson County, Kentucky","language":"ENGLISH","doi":"10.3133/ha8","usgsCitation":"MacCary, L., 1956, Availability of ground water for domestic use in Jefferson County, Kentucky: U.S. Geological Survey Hydrologic Atlas 8, 1 map ;43 x 49 cm., https://doi.org/10.3133/ha8.","productDescription":"1 map ;43 x 49 cm.","costCenters":[],"links":[{"id":252272,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/008/report-thumb.jpg"},{"id":251448,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/008/report.pdf","size":"2188","linkFileType":{"id":1,"text":"pdf"}}],"scale":"9750","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85.91666666666667,38 ], [ -85.91666666666667,38.36666666666667 ], [ -82.41666666666667,38.36666666666667 ], [ -82.41666666666667,38 ], [ -85.91666666666667,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671cf","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":277833,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2999,"text":"wsp1365 - 1956 - Saline-water resources of Texas","interactions":[],"lastModifiedDate":"2016-08-22T10:43:42","indexId":"wsp1365","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1365","title":"Saline-water resources of Texas","docAbstract":"<p>Large quantities of saline water are available in the world, both on the surface and underground; however, these waters have not been studied extensively as sources of potable water.</p>\n<p>Saline water is defined herein as water containing more than 1,000 parts per million of dissolved solids, or, with certain mineralized irrigation waters whose exact dissolved solids content is not known, water containing more than 60 percent sodium.</p>\n<p>Saline ground water occurs as connate water or other saline water that entered an aquifer in the geologic past and has not been flushed from the aquifer; as the result of solution of soluble materials in aquifers by percolating ground water; as a result of salt-water encroachment into aquifers which are in hydrologic connection with saline waters; or as the result of concentration by evaporation, especially in the vicinity of playa lakes.</p>\n<p>Surface water may become saline as a result of seepage of highly mineralized ground water; solution of salts from rocks over which the streams flow; intrusion of sea water in tidal reaches of a stream; and discharge of saline wastes from industrial operations.</p>\n<p>Most of the aquifers in Texas contain saline water in some parts, and a few are capable of producing large quantities of saline water. Of the early Paleozoic formations, the Hickory sandstone member of the Riley formation of Cambrian age and the Ellenburger group of Ordovician age are potential sources of small to moderate supplies of saline water in parts of central and west-central Texas.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1365","usgsCitation":"Winslow, A.G., and Kister, L.R., 1956, Saline-water resources of Texas: U.S. Geological Survey Water Supply Paper 1365, Report: v, 105 p.; 9 Plates, https://doi.org/10.3133/wsp1365.","productDescription":"Report: v, 105 p.; 9 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":29780,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29781,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29782,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29783,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29784,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29785,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29786,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29787,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29788,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1365/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":29789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1365/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":139400,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1365/report-thumb.jpg"},{"id":109938,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24346.htm","linkFileType":{"id":5,"text":"html"},"description":"24346"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc05f","contributors":{"authors":[{"text":"Winslow, Allen George","contributorId":44522,"corporation":false,"usgs":true,"family":"Winslow","given":"Allen","email":"","middleInitial":"George","affiliations":[],"preferred":false,"id":146123,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kister, Lester Ray","contributorId":107670,"corporation":false,"usgs":true,"family":"Kister","given":"Lester","email":"","middleInitial":"Ray","affiliations":[],"preferred":false,"id":146124,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1997,"text":"wsp1364 - 1956 - Water resources of southwestern Louisiana","interactions":[{"subject":{"id":51647,"text":"ofr5477 - 1954 - An analysis of water-level contour maps of southwestern Louisana, 1952 and 1953","indexId":"ofr5477","publicationYear":"1954","noYear":false,"title":"An analysis of water-level contour maps of southwestern Louisana, 1952 and 1953"},"predicate":"SUPERSEDED_BY","object":{"id":1997,"text":"wsp1364 - 1956 - Water resources of southwestern Louisiana","indexId":"wsp1364","publicationYear":"1956","noYear":false,"title":"Water resources of southwestern Louisiana"},"id":1}],"lastModifiedDate":"2013-11-27T13:39:09","indexId":"wsp1364","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1364","title":"Water resources of southwestern Louisiana","docAbstract":"In southwestern Louisiana large quantities of fresh water are available for agricultural, \nmunicipal, domestic, and industrial purposes. However, local and regional problems resulting \nfrom salt-water encroachment in the streams and persistent declines of the groundwater \nlevels in certain areas during . drought periods have caused some concern regarding \nthe future water supply of the region. · In order to appraise the situation, to provide hydrologic \ninformation basic to development of the area, and to provide a basis for sound plans \nfor alleviating recurrent dry-year losses, a study of the ground-water resources of the area \nwas begun in 1938 through cooperation with the Louisiana Geological Survey, Department \nof Conservation. An intensive investigation comprising ground-water, surface-water, and \nquality-of-water studies was authorized in 1948 in cooperation with the Louisiana Department \nof Public Works, and was completely under' way before the 1949 irrigation season. \nThe studies were carried through the irrigation season of 1951.","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1364","collaboration":"Prepared in cooperation with the Louisiana Department of Public Works and the Louisiana Geological Survey, Department of Conservation","usgsCitation":"Jones, P.H., Hendricks, E.L., Irelan, B., and and others, 1956, Water resources of southwestern Louisiana: U.S. Geological Survey Water Supply Paper 1364, Report: xiii, 460 p.; 38 Plates, https://doi.org/10.3133/wsp1364.","productDescription":"Report: xiii, 460 p.; 38 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,{"id":2483,"text":"wsp1363 - 1956 - Hydrology of Indiana lakes","interactions":[],"lastModifiedDate":"2016-06-21T13:27:34","indexId":"wsp1363","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1363","title":"Hydrology of Indiana lakes","docAbstract":"<p>Indiana's lakes are a valuable resource for both recreational use and their industrial potential. Some lakes are used for water supply.</p>\n<p>The natural lakes are glacial in origin and are most concentrated in northeastern Indiana. Many of the lakes were drained by the early settlers. The natural processes of sedimentation ad accumulation of organic deposits tend also to reduce the number and size of lakes. The trend toward fewer lakes has been reversed in recent years by the construction of artificial lakes; the number of lakes has increased from a little over 500 in 1800 to 1,000 at the present time.</p>\n<p>The recreational value of the lakes and the desirability of maintaining constant lake level led to legislation relative to the establishment of legal lake levels and to a program of lake-level observations, supplemented by the collection of hydrologic data affecting lake levels.</p>\n<p>Observations of both surface temperature and temperature profile were made by investigates as early as 1875. The earlier data and data collected since 1946 have been analyzed to show the fluctuation of temperature with season, depth of water, size of lake, and other influencing factors. Surface temperature, which may vary several degrees within a 24-hour period, fluctuate with air temperature and reach highs of about 85&deg;F in August. The bottom temperature of lakes more than 100 feet deep seldom rise above 45&deg;F. Subsurface water temperatures below ice cover reach a uniform value of about 39&deg;F except that just below the ice which remains closely 32&deg;F. During summer, temperature stratification is established as the lake warms. Shallow lakes reach temperature extremes about 5&deg;F above and below those of deep lakes. Size of the contributing drainage area, surface area of the lake, and flow through the lake have little effect on water temperatures below a depth of about 20 feet. Little aquatic life exists below depths of 30 feet from mid April to mid September owing to a lack of oxygen in the water. Large amounts of cool water, 50 to 10 degrees cooler than groundwater which averages 50&deg;F to 55&deg;F in northern Indiana, are available in the lower portions of the deep lakes.&nbsp;</p>\n<p>Evapotranspiration accounts for the disposal of about 70 percent of the precipitation in Indiana. During a year's time evaporation from the lake surface about equals the precipitation falling on the lake. During dry periods evaporation from a lake may exceed the inflow from small drainage areas and cause a lowering of lake levels. For the period April through October, evaporation as measure in a class A land pan of the U. S. Weather Bureau has averaged 44 inches at Evansville, 34 inches at Indianapolis, and 31 inches at Valpariso. A coefficient of about 0.7 is usually applied to yearly evaporation data from Class A land pans to obtain equivalent evaporation from lake surfaces.</p>\n<p>Ice cover on the lakes extends from about December 15 to March 15 and reaches thickness of 24 to 30 inches during colder winters. Ice can be damaging to the lakeside installations by thrust action of by the wind action on ice cakes.</p>\n<p>The stabilization of lake levels often requires the construction of outlet control structures. A detailed study of past lake-level elevations and other hydologic date is necessary to establish a level that can be maintained and to determine the means necessary for maintaining the established level. Detailed lake-level records for 28 lakes are included in the report, and records for over 100 other lakes data are available in the U.S. Geological Survey Office, Indianapolis, Ind. Evaporation data from the four Class A evaporation station of the U. S. Weather Bureau have been compiled in this report. A table showing the established legal lake level and related data is included.</p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1363","usgsCitation":"Perrey, J.I., and Corbett, D.M., 1956, Hydrology of Indiana lakes: U.S. Geological Survey Water Supply Paper 1363, xi, 347 p. :ill. ;24 cm., https://doi.org/10.3133/wsp1363.","productDescription":"xi, 347 p. :ill. ;24 cm.","startPage":"1","endPage":"347","numberOfPages":"360","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":138767,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1363/report-thumb.jpg"},{"id":28577,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1363/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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,{"id":2148,"text":"wsp1360C - 1956 - Geology and occurrence of ground water in the Townsend Valley, Montana","interactions":[],"lastModifiedDate":"2024-11-27T15:34:11.366693","indexId":"wsp1360C","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1360","chapter":"C","title":"Geology and occurrence of ground water in the Townsend Valley, Montana","docAbstract":"<p>No abstract available.</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1955","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp1360C","usgsCitation":"Lorenz, H.W., McMurtrey, R.G., and Swenson, H.A., 1956, Geology and occurrence of ground water in the Townsend Valley, Montana: U.S. Geological Survey Water Supply Paper 1360, Report: iv, 121 p.; 2 Plates: 22.00 × 34.07 inches and 19.50 × 33.85 inches, https://doi.org/10.3133/wsp1360C.","productDescription":"Report: iv, 121 p.; 2 Plates: 22.00 × 34.07 inches and 19.50 × 33.85 inches","costCenters":[],"links":[{"id":247116,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360c/plate-20.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247115,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360c/plate-19.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":137819,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360c/report-thumb.jpg"},{"id":394259,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_24338.htm"},{"id":27758,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360c/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana","otherGeospatial":"Townsend Valley","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.759,\n              46.0410\n            ],\n            [\n              -111.2790,\n              46.0410\n            ],\n            [\n              -111.2790,\n              46.7470\n            ],\n            [\n              -111.759,\n              46.7470\n            ],\n            [\n              -111.759,\n              46.0410\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad8e4b07f02db68480f","contributors":{"authors":[{"text":"Lorenz, Howard W.","contributorId":47345,"corporation":false,"usgs":true,"family":"Lorenz","given":"Howard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":144741,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"McMurtrey, R. G.","contributorId":36913,"corporation":false,"usgs":true,"family":"McMurtrey","given":"R.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":144740,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Swenson, Herbert A.","contributorId":93461,"corporation":false,"usgs":true,"family":"Swenson","given":"Herbert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":144742,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","interactions":[{"subject":{"id":3831,"text":"cir23 - 1948 - Reservoirs in the United States","indexId":"cir23","publicationYear":"1948","noYear":false,"title":"Reservoirs in the United States"},"predicate":"SUPERSEDED_BY","object":{"id":2815,"text":"wsp1360A - 1956 - Reservoirs in the United States","indexId":"wsp1360A","publicationYear":"1956","noYear":false,"chapter":"A","title":"Reservoirs in the United States"},"id":1}],"lastModifiedDate":"2024-11-27T14:54:57.46166","indexId":"wsp1360A","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1360","chapter":"A","title":"Reservoirs in the United States","docAbstract":"<p>Reservoir storage facilities in the United States play an important part in the national economy. Storage facilities have enabled the country to utilize to a much fuller extent one of the most valuable natural resources: water. During recent years the construction of reservoirs has continued at a high rate. This report shows the status of these facilities on January 1, 1954, and describes briefly some of the reasons for growth of reservoir facilities in the United States. </p><p>Descriptive data are given for reservoirs having a capacity of 5, 000 acre-feet or more and for natural lakes having a usable capacity of 5,000 acre-feet or more. Included are reservoirs and lakes completed as of January 1, 1954, and reservoirs under construction on that date. The total number of such reservoirs and lakes is 1, 300. </p><p>A descriptive list of reservoirs in the United States was first published by the United States Geological Survey in March 1948. That report, Geological Survey Circular 23, entitled Reservoirs in the United States, included reservoirs completed as of January 1, 1947. Since January 1, 1947, reservoirs representing a total usable capacity of 115,000,000 acre-feet, or an increase of 71 percent, have been constructed or are under construction. Data about these new reservoirs are presented herein, and the data shown for reservoirs constructed before 1947 have been corrected on the basis of the latest available survey to determine reservoir capacity. </p><p>The total usable capacity of reservoirs and lakes included in this compilation amounts to 278, 120, 000 acre-feet, and the corresponding surface area totals 11, 046, 000 acres. </p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Contributions to the hydrology of the United States, 1955 (Water Supply Paper 1360)","largerWorkSubtype":{"id":1,"text":"Federal Government Series"},"language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp1360A","usgsCitation":"Thomas, N., and Harbeck, G.E., 1956, Reservoirs in the United States: U.S. Geological Survey Water Supply Paper 1360, Report: v, 99 p.; 9 Plates (in 10 Sheets): 50.19 x 33.95 inches or smaller, https://doi.org/10.3133/wsp1360A.","productDescription":"Report: v, 99 p.; 9 Plates (in 10 Sheets): 50.19 x 33.95 inches or smaller","numberOfPages":"106","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":29364,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1360a/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138823,"rank":2,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1360a/report-thumb.jpg"},{"id":276482,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1360a/plate-01.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map of United States showing drainage areas and index numbers"}],"country":"United States","publicComments":"Subtitle: <i>Revising and superseding Geological Survey Circular 23, Reservoirs in the United States, by G. Earl Harbeck, Jr.: March 1948</i>","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a55e4b07f02db62c697","contributors":{"authors":[{"text":"Thomas, N.O.","contributorId":99962,"corporation":false,"usgs":true,"family":"Thomas","given":"N.O.","email":"","affiliations":[],"preferred":false,"id":145844,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harbeck, G. Earl Jr.","contributorId":18736,"corporation":false,"usgs":true,"family":"Harbeck","given":"G.","suffix":"Jr.","email":"","middleInitial":"Earl","affiliations":[],"preferred":false,"id":145843,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":1161,"text":"wsp1373 - 1956 - Sedimentation and chemical quality of surface waters in the Wind River basin, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:05:12","indexId":"wsp1373","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"1373","title":"Sedimentation and chemical quality of surface waters in the Wind River basin, Wyoming","docAbstract":"This report gives results of an investigation by the U. S. Geological Survey of chemical quality of surface waters and sedimentation in the Wind River Basin, Wyo. The sedimentation study was begun in 1946 to determine the quantity of sediment that is transported by the streams in the basin; the probable sources of the sediment; the effect of large irrigation projects on sediment yield, particularly along Fivemile Creek; and the probable specific weight of the sediment when initially deposited in a reservoir. The study of the chemical quality of the water was begun in 1945 to obtain information on the sources, nature, and amounts of dissolved material that is transported by streams and on the suitability of the waters for different uses. Phases of geology and hydrology pertinent to the sedimentation and chemical quality were studied. Results of the investigation through September 30, 1952, and some special studies that were made during the 1953 and 1954 water years are reported. \r\n\r\nThe rocks in the Wind River Basin are granite, schist, and gneiss of Precambrian age and a thick series of sedimentary strata that range in age from Cambrian to Recent. Rocks of Precambrian and Paleozoic age are confined to the mountains, rocks of Mesozoic age crop out along the flank of the Wind River and Owl Creek Mountains and in denuded anticlines in the floor of the basin, and rocks of Tertiary age cover the greater part of the floor of the basin. Deposits of debris from glaciers are in the mountains, and remnants of gravel-capped terraces of Pleistocene age are on the floor of the basin. The lateral extent and depth of alluvial deposits of Recent age along all the streams are highly variable. \r\n\r\nThe climate of the floor of the basin is arid. The foothills probably receive a greater amount of intense rainfall than the areas at lower altitudes. Most precipitation in the Wind River Mountains falls as snow. The foothill sections, in general, are transitional zones between the cold, humid climate of the high mountains and the warmer, drier climate of the basin floor. \r\n\r\nAverage annual runoff in the basin is about 3.6 inches on the basis of adjusted streamflow records for the Bighorn River near Thermopolis. Runoff from the mountains is high and is mostly from melting of snow and from spring and early summer rains. It does not vary greatly from year to year because annual water losses are small in comparison to annual precipitation. In the areas on the floor of the basin, where runoff is low, the runoff is mostly the result of storms in late spring and early summer. The annual water losses nearly equal the annual precipitation; therefore, runoff is extremely variable, in terms of percentage changes, from year to year and from point to point during any 1 year.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp1373","usgsCitation":"Colby, B.R., Hembree, C., and Rainwater, F.H., 1956, Sedimentation and chemical quality of surface waters in the Wind River basin, Wyoming: U.S. Geological Survey Water Supply Paper 1373, x, 336 p. :ill., maps (12 folded in pocket) ;24 cm., https://doi.org/10.3133/wsp1373.","productDescription":"x, 336 p. :ill., maps (12 folded in pocket) ;24 cm.","costCenters":[],"links":[{"id":137362,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/1373/report-thumb.jpg"},{"id":25976,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25977,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25978,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25979,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25980,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25981,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25982,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25983,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25984,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25985,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25986,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25987,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/1373/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":25988,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/1373/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4883e4b07f02db5181b2","contributors":{"authors":[{"text":"Colby, B. R.","contributorId":59776,"corporation":false,"usgs":true,"family":"Colby","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":143280,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hembree, C. H.","contributorId":106866,"corporation":false,"usgs":true,"family":"Hembree","given":"C. H.","affiliations":[],"preferred":false,"id":143281,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rainwater, F. H.","contributorId":41402,"corporation":false,"usgs":true,"family":"Rainwater","given":"F.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":143279,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":51935,"text":"ofr56116 - 1956 - Hydrology vs. water allocation in the eastern United States","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr56116","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-116","title":"Hydrology vs. water allocation in the eastern United States","language":"ENGLISH","doi":"10.3133/ofr56116","usgsCitation":"Thomas, H.E., 1956, Hydrology vs. water allocation in the eastern United States: U.S. Geological Survey Open-File Report 56-116, 26 p., https://doi.org/10.3133/ofr56116.","productDescription":"26 p.","costCenters":[],"links":[{"id":177098,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc752","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":244500,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":23112,"text":"ofr5672 - 1956 - A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","interactions":[{"subject":{"id":23112,"text":"ofr5672 - 1956 - A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"ofr5672","publicationYear":"1956","noYear":false,"title":"A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"predicate":"SUPERSEDED_BY","object":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"chapter":"O","title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"id":1}],"supersededBy":{"id":2058,"text":"wsp1475O - 1963 - Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","indexId":"wsp1475O","publicationYear":"1963","noYear":false,"title":"Hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California"},"lastModifiedDate":"2012-02-02T00:08:08","indexId":"ofr5672","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-72","title":"A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California","language":"ENGLISH","publisher":"U.S. Geological Survey, Ground Water Branch,","doi":"10.3133/ofr5672","issn":"0094-9140","usgsCitation":"Kunkel, F., 1956, A brief hydrologic and geologic reconnaissance of Pinto Basin, Joshua Tree National Monument, Riverside County, California: U.S. Geological Survey Open-File Report 56-72, 35 p. (some folded) :ill., map ;27 cm., https://doi.org/10.3133/ofr5672.","productDescription":"35 p. (some folded) :ill., map ;27 cm.","costCenters":[],"links":[{"id":156657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd497ae4b0b290850ef379","contributors":{"authors":[{"text":"Kunkel, Fred","contributorId":47766,"corporation":false,"usgs":true,"family":"Kunkel","given":"Fred","email":"","affiliations":[],"preferred":false,"id":189457,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":51936,"text":"ofr56117 - 1956 - Some hydrologic principles to be considered in ground-water legislation","interactions":[],"lastModifiedDate":"2012-02-02T00:11:34","indexId":"ofr56117","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"56-117","title":"Some hydrologic principles to be considered in ground-water legislation","language":"ENGLISH","doi":"10.3133/ofr56117","usgsCitation":"Thomas, H.E., 1956, Some hydrologic principles to be considered in ground-water legislation: U.S. Geological Survey Open-File Report 56-117, 9 p., https://doi.org/10.3133/ofr56117.","productDescription":"9 p.","costCenters":[],"links":[{"id":177156,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad9e4b07f02db684e9e","contributors":{"authors":[{"text":"Thomas, H. E.","contributorId":12829,"corporation":false,"usgs":true,"family":"Thomas","given":"H.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":244501,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":68673,"text":"ha6 - 1956 - Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water","interactions":[],"lastModifiedDate":"2012-02-02T00:13:43","indexId":"ha6","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1956","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":"6","title":"Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water","language":"ENGLISH","doi":"10.3133/ha6","usgsCitation":"Bradley, E., and Rainwater, F.H., 1956, Reconnaissance of the geology and ground-water resources of southern Sioux County, Nebraska with a section on chemical quality of ground water: U.S. Geological Survey Hydrologic Atlas 6, 2 maps on 2 sheets ;32 x 38 cm. each., https://doi.org/10.3133/ha6.","productDescription":"2 maps on 2 sheets ;32 x 38 cm. each.","costCenters":[],"links":[{"id":251466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/ha/006/report.pdf","size":"2116","linkFileType":{"id":1,"text":"pdf"}},{"id":252445,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/006/report-thumb.jpg"}],"scale":"250000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a62e4b07f02db636d40","contributors":{"authors":[{"text":"Bradley, Edward","contributorId":67071,"corporation":false,"usgs":true,"family":"Bradley","given":"Edward","email":"","affiliations":[],"preferred":false,"id":278699,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rainwater, Francis Hays","contributorId":43045,"corporation":false,"usgs":true,"family":"Rainwater","given":"Francis","email":"","middleInitial":"Hays","affiliations":[],"preferred":false,"id":278698,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":70216343,"text":"70216343 - 1956 - Discussion of “Some factors affecting rates of sedimentation in the Columbia River basin”","interactions":[],"lastModifiedDate":"2020-11-12T18:23:37.858896","indexId":"70216343","displayToPublicDate":"1956-11-12T11:55:30","publicationYear":"1956","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":1578,"text":"Eos, Transactions, American Geophysical Union","onlineIssn":"2324-9250","printIssn":"0096-394","active":true,"publicationSubtype":{"id":10}},"title":"Discussion of “Some factors affecting rates of sedimentation in the Columbia River basin”","docAbstract":"<p>h<span>ydrologists are generally aware of the number and complexity of the variables that are encountered in all aspects of hydrology, and the great difficulty of analyzing these factors quantitatively because of inadequacy of basic data. Because of limitations in funds, time, or scientific manpower, it is likely that the basic data will generally be less than the hydrologist's hopes. In this predicament, many students have sought methods whereby it might be possible to determine the approximate effects of various factors, on the basis of meager available information. The authors, by using statistical methods of analysis, have pointed out one way that may well be rewarding in studies of other aspects of hydrology where little basic information is available.</span></p>","language":"English","publisher":"American Geophysical Union","doi":"10.1029/TR037i001p00110","usgsCitation":"Thomas, H., Flaxman, E., and Hobba, R., 1956, Discussion of “Some factors affecting rates of sedimentation in the Columbia River basin”: Eos, Transactions, American Geophysical Union, v. 37, no. 1, p. 110-112, https://doi.org/10.1029/TR037i001p00110.","productDescription":"3 p.","startPage":"110","endPage":"112","costCenters":[],"links":[{"id":380467,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"37","issue":"1","noUsgsAuthors":false,"publicationDate":"2014-08-18","publicationStatus":"PW","contributors":{"authors":[{"text":"Thomas, H.E.","contributorId":243568,"corporation":false,"usgs":false,"family":"Thomas","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":804763,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Flaxman, E.M.","contributorId":244849,"corporation":false,"usgs":false,"family":"Flaxman","given":"E.M.","email":"","affiliations":[],"preferred":false,"id":804764,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hobba, R.L.","contributorId":244850,"corporation":false,"usgs":false,"family":"Hobba","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":804765,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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