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No abstract available.

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In this atlas, mineralized ground water is viewed presently as a source of water in some areas, but in much of the country as a source for future development. Mineralized water underlies large areas of the country, and its importance will grow as present supplies of fresh water are appropriated and developed. The potential uses fall in two main categories: (1) direct use in industrial processes, such as cooling, or for irrigation, where a moderate mineral content may not be a disadvantage; and (2) use after demineralization or dilution to whatever degree may be required by the intended user. It is clearly more efficient to produce and process water of moderate mineralization at points of use, where available in adequate amounts, than it is to process ocean water and pump it many miles from the sea.

\n

The Geological Survey, as a part of its responsibility to describe the water resources of the United States, has surveyed the known occurrences of mineralized ground water in the conterminous United States. The results are shown on the maps (sheets 1 and 2).

\n

This atlas was prepared to meet needs for information on the distribution and availability of mineralized water as expressed by Government agencies, private industries, and consultants. The maps are one step in providing an inventory of mineralized water of the Nation and will serve as a planning guide for further investigations and for development. They are necessarily generalized in many places owing to the complexity of the occurrence of the mineralized water, lack of detailed information for parts of the nation, and the difficulties inherent in attempts to put three-dimensional information on maps.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db6969e0","contributors":{"authors":[{"text":"Feth, John Henry Frederick","contributorId":37310,"corporation":false,"usgs":true,"family":"Feth","given":"John","email":"","middleInitial":"Henry Frederick","affiliations":[],"preferred":false,"id":278189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68115,"text":"ha151 - 1965 - Floods in Fox Lake Quadrangle, Northeastern Illinois","interactions":[],"lastModifiedDate":"2012-02-10T00:11:26","indexId":"ha151","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"151","title":"Floods in Fox Lake Quadrangle, Northeastern Illinois","language":"ENGLISH","doi":"10.3133/ha151","usgsCitation":"Noehre, A.W., May, V.J., and Walter, G.L., 1965, Floods in Fox Lake Quadrangle, Northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 151, 1 col. map ;58 x 43 cm., on sheet 81 x 102 cm., https://doi.org/10.3133/ha151.","productDescription":"1 col. map ;58 x 43 cm., on sheet 81 x 102 cm.","costCenters":[],"links":[{"id":186659,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89391,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/151/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.25,42.3675 ], [ -88.25,42.5 ], [ -88.11749999999999,42.5 ], [ -88.11749999999999,42.3675 ], [ -88.25,42.3675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7145","contributors":{"authors":[{"text":"Noehre, Allen W.","contributorId":17659,"corporation":false,"usgs":true,"family":"Noehre","given":"Allen","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277667,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":277669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Walter, Gerald L.","contributorId":59880,"corporation":false,"usgs":true,"family":"Walter","given":"Gerald","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":277668,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68504,"text":"ha193 - 1965 - Ground-water resources of the northern Tularosa basin near Carizozo, Lincoln County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:31","indexId":"ha193","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"193","title":"Ground-water resources of the northern Tularosa basin near Carizozo, Lincoln County, New Mexico","language":"ENGLISH","doi":"10.3133/ha193","usgsCitation":"Cooper, J., 1965, Ground-water resources of the northern Tularosa basin near Carizozo, Lincoln County, New Mexico: U.S. Geological Survey Hydrologic Atlas 193, 1 map., https://doi.org/10.3133/ha193.","productDescription":"1 map.","costCenters":[],"links":[{"id":186064,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90079,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/193/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"25000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -10.901388888888889,33.75 ], [ -10.901388888888889,33.75 ], [ -10.901388888888889,33.75 ], [ -10.901388888888889,33.75 ], [ -10.901388888888889,33.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a96e4b07f02db65a812","contributors":{"authors":[{"text":"Cooper, James B.","contributorId":94367,"corporation":false,"usgs":true,"family":"Cooper","given":"James B.","affiliations":[],"preferred":false,"id":278344,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68239,"text":"ha156 - 1965 - Availability of ground water in the Fairdealing quadrangle, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha156","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"156","title":"Availability of ground water in the Fairdealing quadrangle, Kentucky","language":"ENGLISH","doi":"10.3133/ha156","usgsCitation":"Lambert, T.W., 1965, Availability of ground water in the Fairdealing quadrangle, Kentucky: U.S. Geological Survey Hydrologic Atlas 156, col. map ;92 x 120 cm., https://doi.org/10.3133/ha156.","productDescription":"col. map ;92 x 120 cm.","costCenters":[],"links":[{"id":189455,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89619,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/156/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.11749999999999,36.75 ], [ -88.11749999999999,36.8675 ], [ -88.11749999999999,36.8675 ], [ -88.11749999999999,36.75 ], [ -88.11749999999999,36.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65de11","contributors":{"authors":[{"text":"Lambert, T. William","contributorId":40574,"corporation":false,"usgs":true,"family":"Lambert","given":"T.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":277896,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":57734,"text":"ofr65184 - 1965 - Ground-water levels in observation wells in Oklahoma, 1963-64","interactions":[],"lastModifiedDate":"2012-02-02T00:12:13","indexId":"ofr65184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-184","title":"Ground-water levels in observation wells in Oklahoma, 1963-64","docAbstract":"The investigation of the ground-water resources of Oklahoma by the U.S. Geological Survey in cooperation with the Oklahoma Water Resources Board includes a continuing program to collect records of water levels in selected observation wells on a systematic basis. These water-level records: (1) provide an index to available ground-water supplies; (2) facilitate the prediction of trends in water levels that will indicate likely changes in storage; (3) aid in the prediction of the base flow of streams; (4) provide information for use in basic research; (5) provide long-time continuous records of fluctuations of water levels in representative wells; and (6) serve as a framework to which other types of hydrologic data my be related.\r\nPrior to 1956, measurements of water levels in observation wells in Oklahoma were included in water-supply papers published annually by the U.S. Geological Survey. Beginning with the 1956 calendar year, however, Geological Survey water-level reports will contain only records of a selected network of observation wells, and will be published at 5-year intervals. The first of this series, for the 1956-59 period was published in 1962.\r\n\r\nThis report has been prepared primarily to present water-level records of wells not included in the Federal network. However, for the sake of completeness it includes water-level records of Federal wells that either have been or will be published in water-supply papers since 1955. This report, which contains water-level records for the 2-year period (1963-64), is the third of a series presenting water-level records for all permanent observations wells in Oklahoma. The first report, published in 1963, contains water-level records for the 5-year period of (1956-60). The second report, published in 1964, contains water-level records for the 2-year period (1961-62.)\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr65184","usgsCitation":"Wood, P., 1965, Ground-water levels in observation wells in Oklahoma, 1963-64: U.S. Geological Survey Open-File Report 65-184, 82 p., https://doi.org/10.3133/ofr65184.","productDescription":"82 p.","costCenters":[],"links":[{"id":184448,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db66757e","contributors":{"authors":[{"text":"Wood, P.R.","contributorId":102068,"corporation":false,"usgs":true,"family":"Wood","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":257664,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":52506,"text":"ofr65155 - 1965 - Ground-water data of selected test holes and wells along the Arkansas river in Muskogee County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr65155","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-155","title":"Ground-water data of selected test holes and wells along the Arkansas river in Muskogee County, Oklahoma","docAbstract":"The data in this report were collected during the period 1958-64 by the U.S. Geological Survey in cooperation with the U.S. Army, Corps of Engineers, as part of a comprehensive study of the ground-water resources of the alluvium along the Arkansas and Verdigris Rivers between Moffett and Catoosa, Oklahoma (fig. 1). The purpose of this report is to make the hydrologic data obtained during the study of ground water in the alluvium along the Arkansas River in Muskogee County readily available to the public. The data in this report should be useful in predicting geologic and hydrologic conditions when drilling new wells. Table 1 gives information on the sizes, depths, yields, and other characteristics of wells in the area. The table also provides a key to the additional information for each well site given in tables 2 through 6. Table 2 gives logs for the materials penetrated at test holes and wells in the report area; table 3 gives depths to water measured in wells; table 4 includes chemical analyses of water from wells; table 5 gives laboratory determinations of particle-size distribution of earth samples collected from test holes and wells; and table 6 gives coefficients of permeability and other hydrologic properties of earth samples from the selected test holes. Similar data for Sequoyah County, LeFlore-Haskell Counties, and Wagoner-Rogers Counties are available in other open-file reports.\r\nAn interpretive report, 'Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas,' by Harry H. Tanaka and Jerrald R. Hollowell will be published as U.S. Geological Survey Water-Supply Paper 1809-T.","language":"ENGLISH","doi":"10.3133/ofr65155","usgsCitation":"Tanaka, H., Hart, D., and Knott, R., 1965, Ground-water data of selected test holes and wells along the Arkansas river in Muskogee County, Oklahoma: U.S. Geological Survey Open-File Report 65-155, 287 p., https://doi.org/10.3133/ofr65155.","productDescription":"287 p.","costCenters":[],"links":[{"id":176972,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf0f","contributors":{"authors":[{"text":"Tanaka, H.H.","contributorId":30610,"corporation":false,"usgs":true,"family":"Tanaka","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":245459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D.L. Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":245460,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":245461,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":52505,"text":"ofr65153 - 1965 - Preliminary report on investigation of salt springs and seeps in a portion of the Permian Basin in Texas","interactions":[],"lastModifiedDate":"2016-08-23T16:49:47","indexId":"ofr65153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-153","title":"Preliminary report on investigation of salt springs and seeps in a portion of the Permian Basin in Texas","docAbstract":"

The Permian Basin (fig. 1) comprises a large area in the southern midcontinent region and includes major portions of Texas, New Mexico, Oklahoma, and Kansas. Within this basin brine springs and seeps discharge more than 20,000 tons per day of sodium chloride (common table salt). This brine contaminates many streams greatly impairing the utility of their waters. The water in some streams is of such poor quality it cannot be used for municipal and industrial purposes and for irrigation. Nor is the problem limited to the Permian Basin. The contaminated streams leaving the Permian Basin bring salty water to downstream areas of Arkansas and Louisiana, as well as to other parts of Texas, New Mexico, Oklahoma, and Kansas. In no comparable area of the interior United States are natural sources of salt water so widespread or deleterious to the fresh water supply of so large a segment of the nation's population and industry.

The Brazos River traverses the eastern part of the Permian Basin, and is potentially one of the principal sources of water in Texas. It carries an average daily load of 1,650 tons of sodium chloride (common table salt) into Possum Kingdom Reservoir, about 110 miles west of Dallas. More than 85 percent of this salt is contributed by the Salt Fork Brazos River, and more than one-half originates from Springs and seeps in Croton and Salt Croton Creeks, tributaries to the Salt Fork Brazos River. The undesirably high chloride content of the water impounded in Possum Kingdom Reservoir limits the utility of this water, although it is used for irrigation and by some industries.

Understanding of the origin and hydrology of the natural brine is fundamental to consideration of engineering measures to control the flow of salt water to streams, or to general plans to alleviate the situation in any way that includes altering the brine-discharge system.

Previous investigations of natural brine features have been directed toward describing the local details of individual problem areas. Thus the occurrence of brine features has been described strictly in terms of the local environment. The origin and discharge of brine have been ascribed invariably to local sources and to local hydraulic controls. The case for local origin of the brine has been stated by Ward and Leonard (1961). According to their hypothesis brines evolve in the circulation of ground water in local hydraulic systems which feature the following conditions: (a) halite deposits or halite-bearing rocks at relatively shallow depth; (b) ground water that circulates to the halite-bearing zones; and (c) a local topographically low area where the water can emerge as a mineral spring.

An alternate hypothesis (Greenman and Stevens, 1963) is that the salt springs originate as outcrops of a regional body of brine and that the primary factors determining their distribution are regional hydrologic controls, such as physiography, geology, and climate. The precise location of springs, the nature and amount of discharge, as well as their salinity, depend on secondary hydrologic factors, such as local geologic conditions, local topography that governs the movement of the overlying fresh water, and the hydrologic environment in the vicinity of the springs, which determines the amount of mixing of the brine and the fresh water at each locality. In general, the brine is a water body separate and distinct from the overlying fresh water. The salinity of individual springs is determined by the amount of mixing of the brine with the fresh water not by solution of salt-bearing materials in local hydraulic systems. The geographic zone in which all of the brine springs and seeps occur is determined by regional topographic and perhaps climatic conditions. If the regional hypothesis is true, remedial measures must take into account a set of hydraulic and hydrologic circumstances that is fundamentally different from that postulated previously.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr65153","usgsCitation":"Stevens, P.R., and Hardt, W.F., 1965, Preliminary report on investigation of salt springs and seeps in a portion of the Permian Basin in Texas: U.S. Geological Survey Open-File Report 65-153, Document: 19 p.; 5 Plates: 25.85 x 12.59 inches or smaller, https://doi.org/10.3133/ofr65153.","productDescription":"Document: 19 p.; 5 Plates: 25.85 x 12.59 inches or smaller","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":178218,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1965/0153/report-thumb.jpg"},{"id":86930,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0153/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86931,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0153/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86932,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0153/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86933,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0153/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86934,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1965/0153/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":86935,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1965/0153/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa9e4b07f02db6680cf","contributors":{"authors":[{"text":"Stevens, P. R.","contributorId":90289,"corporation":false,"usgs":true,"family":"Stevens","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":245458,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hardt, W. F.","contributorId":12455,"corporation":false,"usgs":true,"family":"Hardt","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":245457,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68301,"text":"ha192 - 1965 - Water resources of the Three Rivers area, Otero and Lincoln Counties, New Mexico","interactions":[],"lastModifiedDate":"2012-02-10T00:11:30","indexId":"ha192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"192","title":"Water resources of the Three Rivers area, Otero and Lincoln Counties, New Mexico","language":"ENGLISH","doi":"10.3133/ha192","usgsCitation":"Hood, J.W., and Herrick, E.H., 1965, Water resources of the Three Rivers area, Otero and Lincoln Counties, New Mexico: U.S. Geological Survey Hydrologic Atlas 192, 1 map., https://doi.org/10.3133/ha192.","productDescription":"1 map.","costCenters":[],"links":[{"id":186686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":89737,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/192/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"26720","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ 0,36.36666666666667 ], [ 0,36.36666666666667 ], [ 36.36666666666667,36.36666666666667 ], [ 36.36666666666667,36.36666666666667 ], [ 0,36.36666666666667 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0329","contributors":{"authors":[{"text":"Hood, J. W.","contributorId":87908,"corporation":false,"usgs":true,"family":"Hood","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":277992,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Herrick, Eugene H.","contributorId":80360,"corporation":false,"usgs":true,"family":"Herrick","given":"Eugene","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":277991,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68609,"text":"ha202 - 1965 - Floods in West Chicago quadrangle, northeastern Illinois","interactions":[],"lastModifiedDate":"2023-01-13T22:01:08.911464","indexId":"ha202","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"202","title":"Floods in West Chicago quadrangle, northeastern Illinois","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha202","usgsCitation":"Allen, H., and May, V.J., 1965, Floods in West Chicago quadrangle, northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 202, 1 Plate: 43.68 x 31.50 inches, https://doi.org/10.3133/ha202.","productDescription":"1 Plate: 43.68 x 31.50 inches","costCenters":[],"links":[{"id":188460,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":411931,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15567.htm","linkFileType":{"id":5,"text":"html"}},{"id":90270,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/202/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinois","otherGeospatial":"West Chicago quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.25,\n 41.875\n ],\n [\n -88.25,\n 42\n ],\n [\n -88.125,\n 42\n ],\n [\n -88.125,\n 41.875\n ],\n [\n -88.25,\n 41.875\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e48fc","contributors":{"authors":[{"text":"Allen, Howard E.","contributorId":17274,"corporation":false,"usgs":true,"family":"Allen","given":"Howard E.","affiliations":[],"preferred":false,"id":278565,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"May, V. Jeff","contributorId":80358,"corporation":false,"usgs":true,"family":"May","given":"V.","email":"","middleInitial":"Jeff","affiliations":[],"preferred":false,"id":278566,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":52542,"text":"ofr6645 - 1965 - The operation and maintenance of a crest-stage gaging station","interactions":[],"lastModifiedDate":"2016-11-10T16:20:28","indexId":"ofr6645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"66-45","title":"The operation and maintenance of a crest-stage gaging station","docAbstract":"

The purpose of this manual is to familiarize field personnel with the procedures involved in operating crest-stage gaging stations. Crest-stage gages are used to determine the elevation of a peak stage occurring at a specific location in a stream.

\n

A crest-stage gage consists of a length of 14-inch diameter pipe installed in a vertical position in the stream channel (figure 1). The pipe is vented and equipped with an intake system that allows water to enter and leave the pipe as the stream rises and recedes. An equal length of aluminum \"T\" channel (staff) is inserted in the pipe and made to rest on a positive stop called a datum pin. When granulated cork is placed in the gage, the cork will float on the rising stage, then adhere to the staff after the stage recedes. The peak stage is then determined by removing the staff and measuring the distance between the cork line and the lower end of the staff.

\n

The primary purpose of a crest-stage gaging station is to collect hydrologic data for flood-frequency analyses. Collection of data for such analyses involves operating a network of stations for a period of years until sufficient peak flow data are obtained to accurately define flood-frequency curves. Because carelessness in collecting data at the gage site might result in the loss of an entire year's flood event, the importance of proper operation and maintenance of these gages can not be overemphasized.

\n

Peak discharges are related to the basin characteristics and major changes in these characteristics must be evaluated. For€st fires, timber harvest, or a new road location that alters the natural drainage of the basin, may effect the intensity and timing of the runoff of the basin.

\n

Rigid datum controls must be maintained at the gage site throughout the period of record. Physical changes of the site resulting from flood flows or manmade alterations must be evaluated. If a drainage structure such as a culvert is part of the site features, free-flow conditions must be maintained or obstructions carefully documented.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Portland, OR","doi":"10.3133/ofr6645","usgsCitation":"Friday, J., 1965, The operation and maintenance of a crest-stage gaging station: U.S. Geological Survey Open-File Report 66-45, vi, 20 p., https://doi.org/10.3133/ofr6645.","productDescription":"vi, 20 p.","numberOfPages":"28","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":173959,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr6645.jpg"},{"id":324122,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1966/0045/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64935b","contributors":{"authors":[{"text":"Friday, John","contributorId":19160,"corporation":false,"usgs":true,"family":"Friday","given":"John","email":"","affiliations":[],"preferred":false,"id":245520,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68526,"text":"ha126 - 1965 - Flood of 1962 near Baton Rouge, Louisiana","interactions":[],"lastModifiedDate":"2016-07-28T07:37:00","indexId":"ha126","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"126","title":"Flood of 1962 near Baton Rouge, Louisiana","language":"ENGLISH","doi":"10.3133/ha126","usgsCitation":"Camp, J.D., 1965, Flood of 1962 near Baton Rouge, Louisiana: U.S. Geological Survey Hydrologic Atlas 126, 1 map., https://doi.org/10.3133/ha126.","productDescription":"1 map.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":185708,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/ha/126/report-thumb.jpg"},{"id":90126,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/126/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -91.20083333333334,30.5 ], [ -91.20083333333334,30.6175 ], [ -91.06666666666666,30.6175 ], [ -91.06666666666666,30.5 ], [ -91.20083333333334,30.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5ef03b","contributors":{"authors":[{"text":"Camp, Joseph D.","contributorId":47869,"corporation":false,"usgs":true,"family":"Camp","given":"Joseph","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":278400,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68481,"text":"ha164 - 1965 - Availability of ground water in the Mayfield quadrangle, Jackson Purchase region, Kentucky","interactions":[],"lastModifiedDate":"2012-02-10T00:11:25","indexId":"ha164","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"164","title":"Availability of ground water in the Mayfield quadrangle, Jackson Purchase region, Kentucky","language":"ENGLISH","doi":"10.3133/ha164","usgsCitation":"Davis, R.W., 1965, Availability of ground water in the Mayfield quadrangle, Jackson Purchase region, Kentucky: U.S. Geological Survey Hydrologic Atlas 164, 1 map., https://doi.org/10.3133/ha164.","productDescription":"1 map.","costCenters":[],"links":[{"id":188022,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90034,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/164/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -88.75,36.6175 ], [ -88.75,36.75 ], [ -88.61749999999999,36.75 ], [ -88.61749999999999,36.6175 ], [ -88.75,36.6175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d6c5","contributors":{"authors":[{"text":"Davis, R. 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J.","contributorId":8440,"corporation":false,"usgs":true,"family":"Coskery","given":"O.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":278481,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":68183,"text":"ha203 - 1965 - Floods in Streamwood quadrangle, northeastern Illinois","interactions":[],"lastModifiedDate":"2022-08-01T19:37:38.022269","indexId":"ha203","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"203","title":"Floods in Streamwood quadrangle, northeastern Illinois","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ha203","usgsCitation":"May, V.J., and Allen, H., 1965, Floods in Streamwood quadrangle, northeastern Illinois: U.S. Geological Survey Hydrologic Atlas 203, 1 Plate: 48.74 × 31.50 inches, https://doi.org/10.3133/ha203.","productDescription":"1 Plate: 48.74 × 31.50 inches","costCenters":[],"links":[{"id":186467,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404594,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_15568.htm","linkFileType":{"id":5,"text":"html"}},{"id":89493,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/203/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","country":"United States","state":"Illinois","otherGeospatial":"Streamwood quadrangle","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.25,\n 42\n ],\n [\n -88.125,\n 42\n ],\n [\n -88.125,\n 42.125\n ],\n [\n -88.25,\n 42.125\n ],\n [\n -88.25,\n 42\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4e7f","contributors":{"authors":[{"text":"May, V. 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The purpose of this report is to make the hydrologic data obtained during the study of ground water in the alluvium along the Arkansas River in Le Flore and Haskell Counties readily available to the public. The data in this report should be useful in predicting geologic and hydrologic conditions when drilling new wells. Table 1 gives information on the sizes, depths, yields, and other characteristics of wells in the area. The table also provides a key to the additional information for each well site given in tables 2 through 6. Table 2 gives logs for the materials penetrated at test holes and wells in the report area; table 3 gives depths to water measured in wells; table 4 includes chemical analyses of water from wells; table 5 gives laboratory determinations of particle-size distribution of earth samples collected from test holes and wells; and table 6 gives coefficients of permeability and other hydrologic properties of earth samples from the selected test holes. Similar data for Sequoyah County, Muskogee County, and Wagoner-Rogers Counties are available in other open-file reports.\r\nAn interpretive report, 'Hydrology of the alluvium of the Arkansas River, Muskogee, Oklahoma, to Fort Smith, Arkansas,' by Harry H. Tanaka and Jerrald R. Hollowell will be published as U.S. Geological Survey Water-Supply Paper 1809-T.","language":"ENGLISH","doi":"10.3133/ofr65158","usgsCitation":"Tanaka, H., Hart, D., and Knott, R., 1965, Ground-water data of selected test holes and wells along the Arkansas River in LeFlore and Haskell Counties, Oklahoma: U.S. Geological Survey Open-File Report 65-158, 236 p., https://doi.org/10.3133/ofr65158.","productDescription":"236 p.","costCenters":[],"links":[{"id":177059,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf5c","contributors":{"authors":[{"text":"Tanaka, H.H.","contributorId":30610,"corporation":false,"usgs":true,"family":"Tanaka","given":"H.H.","email":"","affiliations":[],"preferred":false,"id":245468,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hart, D.L. Jr.","contributorId":49403,"corporation":false,"usgs":true,"family":"Hart","given":"D.L.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":245469,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knott, R.K.","contributorId":102484,"corporation":false,"usgs":true,"family":"Knott","given":"R.K.","email":"","affiliations":[],"preferred":false,"id":245470,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":52517,"text":"ofr65176 - 1965 - Records of ground-water levels and effects of pumping in the Ardmore well-field area, Carter County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:11:41","indexId":"ofr65176","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"65-176","title":"Records of ground-water levels and effects of pumping in the Ardmore well-field area, Carter County, Oklahoma","docAbstract":"The purpose of this report is to outline the results of work done by the U.S. Geological Survey in the Ardmore well-field area, near Newport, Carter County. The work, completed in two periods between April 1964 and June 1965, was done as part of the ground-water program carried out by the Geological Survey in cooperation with the Oklahoma Water Resources Board.\r\nThe study in the report area included: (1) a physical inventory of wells in the vicinity of the Ardmore well field (fig. 1); (2) information on depths, perforated intervals, ground-water levels, and water use (table 1); (3) records of water-level fluctuations in deep and shallow wells (table 2) to determine if there is a hydraulic connection between the deep zones tapped by Ardmore's wells and the shallow and intermediate zones tapped by domestic and stock wells in the surrounding area; and (4) general information on the geologic and hydrologic features that may be of use in evaluating the ground-water potential of the Wichita Formation, the principal aquifer in the area.\r\n\r\n(available as photostat copy only)","language":"ENGLISH","doi":"10.3133/ofr65176","usgsCitation":"Wood, P., 1965, Records of ground-water levels and effects of pumping in the Ardmore well-field area, Carter County, Oklahoma: U.S. Geological Survey Open-File Report 65-176, 23 p., https://doi.org/10.3133/ofr65176.","productDescription":"23 p.","costCenters":[],"links":[{"id":177739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635746","contributors":{"authors":[{"text":"Wood, P.R.","contributorId":102068,"corporation":false,"usgs":true,"family":"Wood","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":245481,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":68557,"text":"ha134 - 1965 - Water-table, surface-drainage, and engineering soils map of the Little Creek quadrangle, Delaware","interactions":[],"lastModifiedDate":"2012-02-10T00:11:11","indexId":"ha134","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"134","title":"Water-table, surface-drainage, and engineering soils map of the Little Creek quadrangle, Delaware","language":"ENGLISH","doi":"10.3133/ha134","usgsCitation":"Boggess, D.H., and Adams, J.K., 1965, Water-table, surface-drainage, and engineering soils map of the Little Creek quadrangle, Delaware: U.S. Geological Survey Hydrologic Atlas 134, 1 map :col. ;on sheet 76 x 96 cm., https://doi.org/10.3133/ha134.","productDescription":"1 map :col. ;on sheet 76 x 96 cm.","costCenters":[],"links":[{"id":188890,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":90185,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/ha/134/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -75.5,39.1175 ], [ -75.5,39.25 ], [ -75.36749999999999,39.25 ], [ -75.36749999999999,39.1175 ], [ -75.5,39.1175 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7ee4b07f02db6485a6","contributors":{"authors":[{"text":"Boggess, Durward H.","contributorId":28650,"corporation":false,"usgs":true,"family":"Boggess","given":"Durward","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":278459,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adams, John K.","contributorId":17700,"corporation":false,"usgs":true,"family":"Adams","given":"John","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":278458,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":68192,"text":"ha201 - 1965 - Water resources of the Middle River Watershed, Northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T10:02:46","indexId":"ha201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1965","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":"201","title":"Water resources of the Middle River Watershed, Northwestern Minnesota","docAbstract":"

No abstract available.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ha201","collaboration":"Prepared in cooperation with the Minnesota Department of Conservation, Division of Waters","usgsCitation":"Maclay, R., Winter, T.C., and Pike, G., 1965, Water resources of the Middle River Watershed, Northwestern Minnesota: U.S. Geological Survey Hydrologic Atlas 201, 3 Plates: 47.73 x 39.50 inches or smaller, https://doi.org/10.3133/ha201.","productDescription":"3 Plates: 47.73 x 39.50 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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