{"pageNumber":"1970","pageRowStart":"49225","pageSize":"25","recordCount":68919,"records":[{"id":44490,"text":"wri844111 - 1986 - Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:26:08","indexId":"wri844111","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"84-4111","title":"Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota","docAbstract":"<p>The Red River-Winnipeg aquifer of Ordovician age occupies a depression in the Proterozoic crystalline bedrock of northwestern Minnesota. The Winnipeg Formation, which underlies the Red River Formation, consists of two units: A lower shaley mudstone and an upper medium-grained sandstone. The Red River Formation consists of a lower dolomitic, dark-gray limestone and upper, slightly less-dolomitic, limestone. A porous zone at the top of the upper limestone yields most of the water to wells in the Red River-Winnipeg aquifer.</p>\n<p>Ground water generally flows eastward through the aquifer from North Dakota and discharges upward to wells and to overlying deposits. Yields of wells open to the full thickness of the aquifer range from 100 t 250 gallons per minute. The water is unsuitable for most uses because of the high mineral content. Dissolved-solids concentrations range from about 3,000 milligrams per liter in the eastern part of the aquifer to about 60,000 milligrams per liter in the northwestern corner of Minnesota.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri844111","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Ruhl, J.F., and Adolphson, D.G., 1986, Hydrogeologic and water-quality characteristics of the Red River-Winnipeg aquifer northwestern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 84-4111, 2 Plates: 36.02 x 29.44 inches and 36.23 x 30.42 inches, https://doi.org/10.3133/wri844111.","productDescription":"2 Plates: 36.02 x 29.44 inches and 36.23 x 30.42 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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F.","contributorId":81866,"corporation":false,"usgs":true,"family":"Ruhl","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229867,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Adolphson, D. G.","contributorId":106081,"corporation":false,"usgs":true,"family":"Adolphson","given":"D.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":229868,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44484,"text":"wri854002 - 1986 - Hydrogeology of the Lake Miona area, northeast Sumter County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"wri854002","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4002","title":"Hydrogeology of the Lake Miona area, northeast Sumter County, Florida","docAbstract":"The Lake Miona area, in northeast Sumter County, is characterized by karstic depressions that contain lakes, ponds, and marshes that drain vertically to the upper Floridan aquifer. Lake Miona, Black Lake, and Cherry Lake are the prominent water features of the area. When the lake levels are lowest, the lakes are not connected, but at higher levels, they become connected and water flows eastward from Lake Miona through Black Lake to Cherry Lake. The chemical and biological conditions in the lakes are such that, although they support a large population of submerged aquatic plants, no problem with algae blooms was observed. (USGS)","language":"ENGLISH","doi":"10.3133/wri854002","usgsCitation":"Bradner, L.A., 1986, Hydrogeology of the Lake Miona area, northeast Sumter County, Florida: U.S. Geological Survey Water-Resources Investigations Report 85-4002, 1 map : col. ; 38 x 38 cm., on sheet 70 x 92 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri854002.","productDescription":"1 map : col. ; 38 x 38 cm., on sheet 70 x 92 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":134664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81844,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4002/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db6150fe","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229859,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44447,"text":"wri854144 - 1986 - Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida","interactions":[],"lastModifiedDate":"2022-01-04T20:10:19.899943","indexId":"wri854144","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4144","title":"Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854144","usgsCitation":"Thagard, M.E., and Seaber, P.R., 1986, Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida: U.S. Geological Survey Water-Resources Investigations Report 85-4144, 1 Plates: 39.28 × 22.21 inches, https://doi.org/10.3133/wri854144.","productDescription":"1 Plates: 39.28 × 22.21 inches","costCenters":[],"links":[{"id":173744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393874,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36307.htm"},{"id":81770,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4144/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Florida","otherGeospatial":"West Palm Beach 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82,\n              26\n            ],\n            [\n              -80,\n              26\n            ],\n            [\n              -80,\n              27\n            ],\n            [\n              -82,\n              27\n            ],\n            [\n              -82,\n              26\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bf1e","contributors":{"authors":[{"text":"Thagard, Martha E.","contributorId":68315,"corporation":false,"usgs":true,"family":"Thagard","given":"Martha","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44446,"text":"wri864062 - 1986 - Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas","interactions":[],"lastModifiedDate":"2016-08-10T15:04:47","indexId":"wri864062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4062","title":"Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas","docAbstract":"<p>The Edwards aquifer extends in a narrow belt from Bell County in the northeast to Kinney County in the southwest (index map) and provides water for at least nine counties in south-central Texas. Hydrologic boundaries divide the Edwards aquifer in the Austin area for which Barton Springs is the major discharge point. This part of the Edwards aquifer provides the municipal, industrial, domestic, and agricultural water supplies for about 30,000 people in the Austin area (southern Travis and northern Hays counties). Discharge from Barton Springs sustains streamflow at the mouth of Barton Creek and flows into Town Lake. Much of the land use within the outcrop area of the Edwards aquifer near Austin is rapidly changing from natural woodland and grassland to commercial and residential developments. Because urban development can result in a substantial degradation of the quality of water that recharges the aquifer, the extent of the recharge zone of the Edwards aquifer was delineated to provide information to the City of Austin for their use in formulating a plan for protecting and managing groundwater quality. The purpose of this report is to define and delineate the areal extent of the recharge zone of the Edwards aquifer in southern Travis and northern Hays Counties. The areal boundary of the recharge zone was determined by: (1) geologic mapping of the aquifer area; (2) interpretation of aerial photographs; (3) field verification of existing geologic maps; and (4) streamflow-loss studies.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864062","usgsCitation":"Slagle, D.L., Ardis, A.F., and Slade, R.M., 1986, Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas: U.S. Geological Survey Water-Resources Investigations Report 86-4062, 30.00 x 41.76 inches, https://doi.org/10.3133/wri864062.","productDescription":"30.00 x 41.76 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":173743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri864062.PNG"},{"id":81769,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4062/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a221","contributors":{"authors":[{"text":"Slagle, Diana L.","contributorId":103730,"corporation":false,"usgs":true,"family":"Slagle","given":"Diana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ardis, Ann F.","contributorId":96672,"corporation":false,"usgs":true,"family":"Ardis","given":"Ann","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slade, Raymond M. Jr.","contributorId":46487,"corporation":false,"usgs":true,"family":"Slade","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229779,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44445,"text":"wri864059 - 1986 - Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","interactions":[],"lastModifiedDate":"2019-08-20T09:41:43","indexId":"wri864059","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4059","title":"Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","docAbstract":"Generalized contours of the altitude of water levels in wells completed in the Catahoula aquifer in central Louisiana, are illustrated by this map. Most water level measurements used in compiling the map were made in 1980; however, in parts of the State where water levels from 1980 were unavailable and where evidence indicated little change in water level, some measurements from as early as 1961 and as late as 1982 were used. Groundwater levels in and near the outcrop areas fluctuate 2 ft or less yearly and no significant long-term declines have occurred. The slow downward trend in water level altitude since early 1976 may be caused by pumpage from the Catahoula aquifer by a rural water system approximately 3 miles away. Recharge to the Catahoula aquifer occurs by rainfall on the upland outcrop-subcrop areas. Saltwater occurs throughout the Catahoula aquifer downgradient from the outcrop area. The ' approximate limit of freshwater ' line on the map indicates the downgradient limit of water with a concentration of chloride &lt; 250 mg/L; the line was determined using water quality data and analysis of resistivity curves from geophysical well logs. Water from the Catahoula aquifer is used for municipal, industrial, and domestic purposes. Total pumpage from the aquifer in Louisiana was slightly over 1.1 million gallons/day in 1980. Local cones of depression result from pumpage just east of Anacoco in Vernon Parish and northwest of Jonesville in Catahoula Parish. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864059","usgsCitation":"Martin, A., and Whiteman, C.D., 1986, Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980: U.S. Geological Survey Water-Resources Investigations Report 86-4059, 1 Plate: 35.86 x 22.96 inches, https://doi.org/10.3133/wri864059.","productDescription":"1 Plate: 35.86 x 22.96 inches","costCenters":[],"links":[{"id":366594,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4059/report-thumb.jpg"}],"country":"United States","state":"Louisiana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aecc1","contributors":{"authors":[{"text":"Martin, Angel Jr.","contributorId":42571,"corporation":false,"usgs":true,"family":"Martin","given":"Angel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":229777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whiteman, Charles D. Jr.","contributorId":108081,"corporation":false,"usgs":true,"family":"Whiteman","given":"Charles","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44444,"text":"wri864058 - 1986 - Altitude of the freshwater-saltwater interface in a regionally extensive coastal plain aquifer of Mississippi, Alabama, and Georgia","interactions":[],"lastModifiedDate":"2017-01-27T08:54:34","indexId":"wri864058","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4058","title":"Altitude of the freshwater-saltwater interface in a regionally extensive coastal plain aquifer of Mississippi, Alabama, and Georgia","docAbstract":"Geophysical well logs from over 150 oil test and water wells in Mississippi, Alabama, and Georgia were examined and calculations of the dissolved solids concentration in ground water were made using the spontaneous potential deflection as a measure of ionic activity. The values derived from these calculations were used to prepare a map showing the altitude relative to sea level at which the concentration of dissolved solids in the groundwater reached 10,000 mg/L within a regionally extensive aquifer in Mississippi, Alabama, and Georgia. A dissolved solids concentration of 10,000 mg/L is used to delineate the interface between moderately saline and saline water; 10,000 mg/L dissolved solids was designated to delineate the freshwater-saltwater interface. For a finite difference computer flow model being used this interface represents the location where horizontal flow of freshwater is greatly diminished. 10 ,000 mg/L also is the lower limit for dissolved solids concentrations for water in target zones for injection wells. This 10,000 mg/L dissolved solids line is of value as a water quality indicator; although water containing 3,000 to 10,000 mg/L or more of dissolved solids is too saline for agricultural use (upper limit approximately 3,000 mg/L), it may be useful for some industrial purposes. Waters containing dissolved solids concentrations &gt; 10,000 mg/L have little potential for any use involving human activities. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864058","usgsCitation":"Strickland, D.J., and Mahon, G.L., 1986, Altitude of the freshwater-saltwater interface in a regionally extensive coastal plain aquifer of Mississippi, Alabama, and Georgia: U.S. Geological Survey Water-Resources Investigations Report 86-4058, 1 map : col. ; 36 x 63 cm., on sheet 61 x 91 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864058.","productDescription":"1 map : col. ; 36 x 63 cm., on sheet 61 x 91 cm., folded in envelope 31 x 23 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":173651,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81768,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4058/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Alabama, Georgia, 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,{"id":44443,"text":"wri864048 - 1986 - Ground-water availability in the Genesee River Basin, New York and Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"wri864048","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4048","title":"Ground-water availability in the Genesee River Basin, New York and Pennsylvania","docAbstract":"New York State 's need to develop a groundwater management strategy for the protection of its aquifers led, in 1985, to a cooperative program between the U.S. Geological Survey and the New York State Department of Environmental Conservation, through the Genesee/Finger Lakes Regional Planning Council, to publish basinwide groundwater availability maps. As a part of this program, several maps that had been compiled during the 1960s, were selected for publication through a grant between the State and several regional planning agencies. These maps depict the surficial geology and groundwater availability of the basin at 1:125,000 scale. Each map consists of two sheets; sheets 1 and 2 depict the groundwater availability and geology of the northern and southern parts of the basin, and sheets 3 and 4 depict well and test-hole locations within the northern and southern parts of the basin. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864048","usgsCitation":"Kammerer, J., and Hobba, W.A., 1986, Ground-water availability in the Genesee River Basin, New York and Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 86-4048, 2 maps on 4 sheets : col. ; sheets 76 x 97 cm. and 69 x 84 cm., folded in envelope 33 x 25 cm., https://doi.org/10.3133/wri864048.","productDescription":"2 maps on 4 sheets : col. ; sheets 76 x 97 cm. and 69 x 84 cm., folded in envelope 33 x 25 cm.","costCenters":[],"links":[{"id":173650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81764,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81765,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81766,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81767,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d387","contributors":{"authors":[{"text":"Kammerer, John C.","contributorId":53815,"corporation":false,"usgs":true,"family":"Kammerer","given":"John C.","affiliations":[],"preferred":false,"id":229774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hobba, William A. Jr.","contributorId":46076,"corporation":false,"usgs":true,"family":"Hobba","given":"William","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44442,"text":"wri864046 - 1986 - Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984","interactions":[],"lastModifiedDate":"2023-03-13T19:56:15.075174","indexId":"wri864046","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4046","title":"Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864046","usgsCitation":"Whiteman, K.J., 1986, Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4046, 4 Plates: 36.62 x 35.41 inches or smaller, https://doi.org/10.3133/wri864046.","productDescription":"4 Plates: 36.62 x 35.41 inches or smaller","costCenters":[],"links":[{"id":173649,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414040,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36510.htm","linkFileType":{"id":5,"text":"html"}},{"id":81763,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81762,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81761,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81760,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia Plateau","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.633,\n              48.112\n            ],\n            [\n              -121.633,\n              44.817\n            ],\n            [\n              -116.367,\n              44.817\n            ],\n            [\n              -116.367,\n              48.112\n            ],\n            [\n              -121.633,\n              48.112\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674be","contributors":{"authors":[{"text":"Whiteman, K. J.","contributorId":48147,"corporation":false,"usgs":true,"family":"Whiteman","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57230,"text":"wdrTN851 - 1986 - Water resources data, Tennessee, water year 1985","interactions":[],"lastModifiedDate":"2020-11-10T17:12:26.190696","indexId":"wdrTN851","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"TN-85-1","title":"Water resources data, Tennessee, water year 1985","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrTN851","usgsCitation":"Lowery, J., Counts, P., Edmiston, H., and Edwards, F., 1986, Water resources data, Tennessee, water year 1985: U.S. Geological Survey Water Data Report TN-85-1, xii, 411 p., https://doi.org/10.3133/wdrTN851.","productDescription":"xii, 411 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F.D.","contributorId":74060,"corporation":false,"usgs":true,"family":"Edwards","given":"F.D.","email":"","affiliations":[],"preferred":false,"id":256408,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":44441,"text":"wri864041 - 1986 - Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York","interactions":[],"lastModifiedDate":"2022-04-06T18:25:17.387303","indexId":"wri864041","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4041","title":"Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York","docAbstract":"<p>New York State 's need to develop a groundwater management program for protection of its aquifers led in 1985 to a cooperative program between the U.S. Geological Survey and the New York State Department of Environmental Conservation (through regional planning agencies) to publish data from previous studies. The two maps presented are from original compilations done in a 1967 study. Sheet 1 depicts the surficial geology as mapped in 1967; sheet 2 shows the groundwater availability (well yield) throughout the basin. These maps are presented at 1:250 ,000 scale for compatibility with published maps of adjacent river basins.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864041","usgsCitation":"Frimpter, M.H., 1986, Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4041, 2 Plates: 30.19 × 20.31 inches and 30.82 × 20.40 inches, https://doi.org/10.3133/wri864041.","productDescription":"2 Plates: 30.19 × 20.31 inches and 30.82 × 20.40 inches","costCenters":[],"links":[{"id":173474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81759,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81758,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398249,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36505.htm"}],"scale":"250000","country":"United States","state":"New York","otherGeospatial":"Allegheny River basin, Lake Erie basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.749,\n              42\n            ],\n            [\n              -78,\n              42\n            ],\n            [\n              -78,\n              42.557\n            ],\n            [\n              -79.749,\n              42.557\n            ],\n            [\n              -79.749,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c46","contributors":{"authors":[{"text":"Frimpter, Michael H.","contributorId":8074,"corporation":false,"usgs":true,"family":"Frimpter","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44440,"text":"wri864040 - 1986 - Ground-water availability in the Black River Basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864040","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4040","title":"Ground-water availability in the Black River Basin, New York","docAbstract":"There are three maps in this set, which were prepared in 1966-68 as part of a study on the water resources of the Black River basin in cooperation with the New York State Department of Environmental Conservation. The data presented on the maps show well locations, well yield from bedrock aquifers, and well yield from unconsolidated aquifers. The well location map shows locations of all wells represented in the initial report. The well yields given on the bedrock aquifer map were recorrelated with the most recent New York State geologic maps; the well yields shown on the unconsolidated aquifer map are correlated with a surficial geology map of the area. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864040","usgsCitation":"Waller, R.M., 1986, Ground-water availability in the Black River Basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4040, 3 maps ; 65 x 100 cm., on sheets 76 x 104 cm., folded in envelope 33 x 26 cm., https://doi.org/10.3133/wri864040.","productDescription":"3 maps ; 65 x 100 cm., on sheets 76 x 104 cm., folded in envelope 33 x 26 cm.","costCenters":[],"links":[{"id":173473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81755,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81756,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81757,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d37f","contributors":{"authors":[{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":229770,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44439,"text":"wri864033 - 1986 - Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota","interactions":[],"lastModifiedDate":"2022-02-18T22:25:36.58533","indexId":"wri864033","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4033","title":"Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota","docAbstract":"<p>Five aquifers in crystalline rocks of Archean and Proterozoic age in Minnesota include in descending order the North Shore Volcanic, Sioux Quartzite, Proterozoic metasedimentary, Biwabik Iron formation and undifferentiated Precambrian aquifers. The North Shore Volcanic aquifer generally yields &lt; 15 gal/min to wells from interflow sediments and fractures in the basaltic lava flows along the northern shore of Lake Superior and along the upper St. Croix River. Dissolved solids concentrations range from 91 to 74,300 mg/L, and the water is of several chemical types. The Sioux Quartzite aquifer yields from 1 to 450 gal/min to wells open to joints and fractures and loose sand zones in the predominantly pink orthoquartzite in southwestern Minnesota. Dissolved solids concentrations range from 237 mg/L in water from wells in outcrop areas to 2,300 mg/L from wells where the Sioux Quartzite aquifer underlies Cretaceous rocks or thick Des Moines drift. The water generally is a calcium sulfate type. The Proterozoic metasedimentary aquifer generally yields &lt; 20 gal/min to wells in weathered regolith and fractures in thin-bedded gray to black argillite in north-central Minnesota. Dissolved solids concentrations generally range from 126 to 340 mg/L, and the water is a calcium magnesium bicarbonate type. The Biwabik Iron formation aquifer yields 1,000 gal/min to wells in leached zones in the ferruginous chert and interbedded hematite and magnitite iron ore in north-central Minnesota. Dissolved solids range from 157 to 388 mg/L in water that is a calcium magnesium bicarbonate type. The undifferentiated Precambrian aquifer generally yields &lt; 25 gal/min to wells from fractures and the weathered regolith developed on a variety of crystalline-rock types. Wells have been developed in parts of the aquifer throughout the State except in the southeast where it is too deeply buried. Dissolved solids concentrations average &lt; 400 mg/L in central and northeastern Minnesota, but average about 700 mg/L in the northwest and 900 mg/L in the south west. The water is a calcium magnesium bicarbonate type in central and northeastern Minnesota and a variety of mixed water types in northwestern and Southwestern Minnesota.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864033","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Anderson, H.W., 1986, Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 86-4033, 3 Plates: 42.08 x 30.11 inches or smaller, https://doi.org/10.3133/wri864033.","productDescription":"3 Plates: 42.08 x 30.11 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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W. Jr.","contributorId":11187,"corporation":false,"usgs":true,"family":"Anderson","given":"H.","suffix":"Jr.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229769,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44438,"text":"wri864014 - 1986 - Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864014","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4014","title":"Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984","docAbstract":"The Mississippi River Valley alluvial aquifer, is a major source of water for most of eastern Arkansas. Agriculture is largely dependent on the aquifer as approximately 3.3 billion gallon per day are withdrawn for that purpose. Much smaller withdrawals also occur for industrial, public supply, and domestic use. The purpose of the report is to illustrate, using the spring and fall potentiometric surface maps, the water levels in the alluvial aquifer under pre-pumping and post-pumping conditions, respectively, and to illustrate, using the depth-to-water and saturated thickness maps, the effect of heavy pumpage in the alluvial aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864014","usgsCitation":"Plafcan, M., and Edds, J., 1986, Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4014, 4 maps on 1 sheet : col. ; 78 x 46 cm. and smaller, sheet 98 x 107 cm., https://doi.org/10.3133/wri864014.","productDescription":"4 maps on 1 sheet : col. ; 78 x 46 cm. and smaller, sheet 98 x 107 cm.","costCenters":[],"links":[{"id":173366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81751,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa12f","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":229767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44437,"text":"wri864010 - 1986 - Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4010","title":"Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","docAbstract":"An investigation was conduced to define the configuration and hydrology of the rock surface upon which the sand aquifers and confining beds of the Southeastern Coastal Plain aquifer system were deposited. The base of the Southeastern Coastal Plain aquifer system consists of crystalline rocks, saprolite, Paleozoic rocks, Triassic sedimentary rocks (some of which are intruded by basalt), and Jurassic sedimentary rocks. The permeability of these rocks is extremely low and little exchange of water occurs upward to the overlying Cretaceous aquifers. Porosity values are in the range of 10% or less in some of the rocks, indicating little water is stored in them. The transmissivity values are extremely low, indicating very slow movement of water in these rocks. The small volume of water moving at a very slow rate has a long residence time and is usually mineralized to a greater degree than water in the more permeable overlying sediments. (Peters-PTT)","language":"ENGLISH","doi":"10.3133/wri864010","usgsCitation":"Wait, R.L., and Davis, M.E., 1986, Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system: U.S. Geological Survey Water-Resources Investigations Report 86-4010, 1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864010.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4010/report-thumb.jpg"},{"id":81750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3499","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Marvin E.","contributorId":36553,"corporation":false,"usgs":true,"family":"Davis","given":"Marvin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28536,"text":"wri864072 - 1986 - Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri864072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4072","title":"Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","docAbstract":"Data collected at 97 of the 176 gaging stations operated in Illinois during 1983 were used to describe rainfall-runoff processes, to monitor and forecast floods, and to monitor and regulate lake levels, discharge from reservoirs, or discharge of navigable streams. Stream-gaging stations on the Illinois River at Havana, East Branch Du Page River, and interior streams of the Mississippi River floodplain; peak-flow stations on small watersheds; and stage-only stations upstream from unsafe high-hazard dams should be considered for inclusion in future stream-gaging programs. The accuracy of regression models for peak-flow and 1-day mean flood-volume characteristics would not be considerably improved if the density of gaging stations and length of record at those gaging stations are increased. Model error masks tradeoffs between accuracy, density, and record length. The large number of streamflow records presently available is sufficient for fairly accurately determining most streamflow characteristics. The accuracy of streamflow records reported for stream gaging stations and peak-flow stations varies widely. The accuracy of streamflow records for 12 stream-gaging stations and 11 peak-flow stations is substantially less than the accuracy of records for the other 143 gaging stations considered. Based on an evaluation of relative worth, 26 gaging stations are candidates for some type of action if budgetary limitations so demand. A candidate stream-gaging stations could be operated during only part of a year, converted to a peak-flow station, or discontinued. Candidate peak-flow stations should be discontinued. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri864072","usgsCitation":"Mades, D., and Oberg, K.A., 1986, Evaluation of the U.S. Geological Survey's gaging-station network in Illinois: U.S. Geological Survey Water-Resources Investigations Report 86-4072, vii, 88 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864072.","productDescription":"vii, 88 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4072/report-thumb.jpg"},{"id":57349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4c2","contributors":{"authors":[{"text":"Mades, D. M.","contributorId":40230,"corporation":false,"usgs":true,"family":"Mades","given":"D. M.","affiliations":[],"preferred":false,"id":199981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, K. A.","contributorId":67553,"corporation":false,"usgs":true,"family":"Oberg","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43864,"text":"ofr8618 - 1986 - Land use and land cover and associated maps for Tulsa, Oklahoma; Arkansas; Missouri; Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:02","indexId":"ofr8618","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-18","title":"Land use and land cover and associated maps for Tulsa, Oklahoma; Arkansas; Missouri; Kansas","language":"ENGLISH","doi":"10.3133/ofr8618","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Tulsa, Oklahoma; Arkansas; Missouri; Kansas: U.S. Geological Survey Open-File Report 86-18, maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm., https://doi.org/10.3133/ofr8618.","productDescription":"maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm.","costCenters":[],"links":[{"id":168127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec26","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531413,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14144,"text":"ofr86496 - 1986 - Analyses of flood-flow frequency for selected gaging stations in South Dakota through September 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:06:44","indexId":"ofr86496","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-496","title":"Analyses of flood-flow frequency for selected gaging stations in South Dakota through September 1985","docAbstract":"Analyses of flood-flow frequency were made for 80 active continuous-record gaging stations and 105 discontinued crest-stage partial-record stations in South Dakota with 10 or more years of record. The analyses were developed using the log-Pearson Type III procedure recommended by the U.S. Water Resources Council (Interagency Advisory Committee on Water Data, 1981.) (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86496","usgsCitation":"Hoffman, E., Freese, M., and Winter, D., 1986, Analyses of flood-flow frequency for selected gaging stations in South Dakota through September 1985: U.S. Geological Survey Open-File Report 86-496, xii, 137 p. :maps ;28 cm., https://doi.org/10.3133/ofr86496.","productDescription":"xii, 137 p. :maps ;28 cm.","costCenters":[],"links":[{"id":145276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0496/report-thumb.jpg"},{"id":42793,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0496/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680dca","contributors":{"authors":[{"text":"Hoffman, E.B.","contributorId":47379,"corporation":false,"usgs":true,"family":"Hoffman","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":168997,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Freese, M.E.","contributorId":12492,"corporation":false,"usgs":true,"family":"Freese","given":"M.E.","email":"","affiliations":[],"preferred":false,"id":168995,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Winter, D.R.","contributorId":27064,"corporation":false,"usgs":true,"family":"Winter","given":"D.R.","email":"","affiliations":[],"preferred":false,"id":168996,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43876,"text":"ofr83110 - 1986 - Land use and land cover and associated maps for Vya, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:11:02","indexId":"ofr83110","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"83-110","title":"Land use and land cover and associated maps for Vya, Nevada","language":"ENGLISH","doi":"10.3133/ofr83110","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Vya, Nevada: U.S. Geological Survey Open-File Report 83-110, maps :photocopy ;45 x 67 cm., https://doi.org/10.3133/ofr83110.","productDescription":"maps :photocopy ;45 x 67 cm.","costCenters":[],"links":[{"id":168236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6ae6fe","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531424,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":1185,"text":"wsp2289 - 1986 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","interactions":[{"subject":{"id":13161,"text":"ofr84621 - 1985 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","indexId":"ofr84621","publicationYear":"1985","noYear":false,"title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming"},"predicate":"SUPERSEDED_BY","object":{"id":1185,"text":"wsp2289 - 1986 - Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","indexId":"wsp2289","publicationYear":"1986","noYear":false,"title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:16","indexId":"wsp2289","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"2289","title":"Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming","docAbstract":"The major Paleozoic artesian aquifers, the aquifers most favorable for continued development, in the Ten Sleep area of the Bighorn Basin of Wyoming are the Tensleep Sandstone, the Madison Limestone and Bighorn Dolomite (Madison-Bighorn aquifer), and the Flathead Sandstone. The minor aquifers include the Goose Egg and Park City Formations (considered in the Ten Sleep area to be the lateral equivalent of the Phosphoria Formation) and the Amsden Formation. Most wells completed in the major and minor aquifers flow at the land surface. Wellhead pressures generally are less than 50 pounds per square inch for the Tensleep Sandstone, 150-250 pounds per square inch for the Madison-Bighorn aquifer, and more than 400 pounds per square inch for the Flathead Sandstone. Flowing wells completed in the Madison-Bighorn aquifer and the Flathead Sandstone yield more than 1,000 gallons per minute. The initial test of one well completed in the Madison-Bighorn aquifer indicated a flow rate of 14,000 gallons per minute. Transmissivities range from 500 to 1,900 feet squared per day for the Madison-Bighorn aquifer and from about 90 to 325 feet squared per day for the Tensleep and Flathead Sandstones. \r\n\r\nSignificant secondary permeability from fracturing in the Paleozoic aquifers allows local upward interformational movement of water, and this affects the altitude of the potentiometric surfaces of the Tensleep Sandstone and the Madison-Bighorn aquifer. Water moves upward from the Tensleep and other formations, through the Goose Egg Formation, to discharge at the land surface as springs. Much of the spring flow is diverted for irrigation or is used for rearing fish. \r\n\r\nDecreases from original well pressures were not apparent in wells completed in the Tensleep Sandstone or in the Madison-Bighorn aquifer in the study area except for a few wells in or near the town of Ten Sleep. Most wells completed in the Flathead Sandstone, which also are open to the Madison-Bighorn aquifer, show a decrease of pressure from the time of completion to 1978. The decrease of pressure is partly the result of water moving from the Flathead Sandstone into the Madison-Bighorn aquifer, which has a lower potentiometric surface than does the Flathead Sandstone, even during the time the wells are not in operation. Pressure in some small-capacity wells completed in the Goose Egg Formation also has decreased near Ten Sleep. Most of the wells, particularly the irrigation wells, show a progressive decrease in pressure during the irrigation season but recover during periods of nonuse. Measurements of the pressure were made principally in 1953, 1962, 1970, and 1975-78. \r\n\r\nWell water from the Paleozoic aquifers generally contains minimal concentrations of dissolved solids and individual constituents but excessive hardness. Dissolved-solids concentrations of water are less than 300 milligrams per liter in the Tensleep Sandstone and the Madison-Bighorn aquifer, less than 200 milligrams per liter in the Flathead Sandstone, and as much as 450 milligrams per liter in the Goose Egg Formation. Bicarbonate is the major constituent, followed by calcium and magnesium. Relatively large concentrations of sulfate, as much as 490 milligrams per liter, were found, mainly in water from the Goose Egg Formation. The water has low sodium (alkali) and medium salinity; therefore, the water is satisfactory for irrigation and most other uses, if excessive hardness is not a detrimental factor. \r\n\r\nWellhead temperatures range from 11 ? to 27.5 ? Celsius (51 ? to 81.5 ? Fahrenheit) within a range in depth of approximately 250 to 4,000 feet. This gives a geothermal gradient of about 0.44 ? Celsius per 100 feet (0.79 ? Fahrenheit per 100 feet).","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2289","usgsCitation":"Cooley, M.E., 1986, Artesian pressures and water quality in Paleozoic aquifers in the Ten Sleep area of the Bighorn Basin, north-central Wyoming: U.S. Geological Survey Water Supply Paper 2289, iv, 54 p. :ill., maps ;28 cm.; 5 plates in pocket, https://doi.org/10.3133/wsp2289.","productDescription":"iv, 54 p. :ill., maps ;28 cm.; 5 plates in pocket","costCenters":[],"links":[{"id":138030,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2289/report-thumb.jpg"},{"id":26042,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26043,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26044,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26045,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26046,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2289/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":26047,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2289/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48c9e4b07f02db542320","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":143318,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14307,"text":"ofr86133 - 1986 - Water-resources activities of the U.S. Geological Survey in Minnesota, fiscal year 1985","interactions":[],"lastModifiedDate":"2018-03-12T12:14:58","indexId":"ofr86133","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-133","title":"Water-resources activities of the U.S. Geological Survey in Minnesota, fiscal year 1985","docAbstract":"<p>Water-resources activities in the Minnesota District included 26 projects in 1985. The report describes the projects which were funded by 9 local and 6 State agencies, by the U.S. Geological Survey, and by 10 other Federal agencies.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/ofr86133","usgsCitation":"1986, Water-resources activities of the U.S. Geological Survey in Minnesota, fiscal year 1985: U.S. Geological Survey Open-File Report 86-133, vi, 83 p., https://doi.org/10.3133/ofr86133.","productDescription":"vi, 83 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":42974,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0133/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0133/report-thumb.jpg"}],"country":"United 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,{"id":48961,"text":"ofr86400K - 1986 - New information resources of the U.S. Geological Survey Library System, December 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:10:06","indexId":"ofr86400K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-400","chapter":"K","title":"New information resources of the U.S. Geological Survey Library System, December 1986","language":"ENGLISH","doi":"10.3133/ofr86400K","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, New information resources of the U.S. Geological Survey Library System, December 1986: U.S. Geological Survey Open-File Report 86-400, 18 p. ; 28 cm., https://doi.org/10.3133/ofr86400K.","productDescription":"18 p. ; 28 cm.","costCenters":[],"links":[{"id":162221,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0400k/report-thumb.jpg"},{"id":85853,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0400k/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697700","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531853,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48959,"text":"ofr86400I - 1986 - New information resources of the U.S. Geological Survey Library System, October 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:10:03","indexId":"ofr86400I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-400","chapter":"I","title":"New information resources of the U.S. Geological Survey Library System, October 1986","language":"ENGLISH","doi":"10.3133/ofr86400I","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, New information resources of the U.S. Geological Survey Library System, October 1986: U.S. Geological Survey Open-File Report 86-400, 216 p.; 28 cm., https://doi.org/10.3133/ofr86400I.","productDescription":"216 p.; 28 cm.","costCenters":[],"links":[{"id":162279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0400i/report-thumb.jpg"},{"id":85851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0400i/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db697654","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531851,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48958,"text":"ofr86400H - 1986 - New information resources of the U.S. Geological Survey Library System, September 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:10:07","indexId":"ofr86400H","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-400","chapter":"H","title":"New information resources of the U.S. Geological Survey Library System, September 1986","language":"ENGLISH","doi":"10.3133/ofr86400H","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, New information resources of the U.S. Geological Survey Library System, September 1986: U.S. Geological Survey Open-File Report 86-400, 191 p. ; 28 cm., https://doi.org/10.3133/ofr86400H.","productDescription":"191 p. ; 28 cm.","costCenters":[],"links":[{"id":162591,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0400h/report-thumb.jpg"},{"id":85850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0400h/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db69763e","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531850,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":48955,"text":"ofr86400B - 1986 - New information resources of the U.S. Geological Survey Library System, February-March 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:10:07","indexId":"ofr86400B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"86-400","chapter":"B","title":"New information resources of the U.S. Geological Survey Library System, February-March 1986","language":"ENGLISH","doi":"10.3133/ofr86400B","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, New information resources of the U.S. Geological Survey Library System, February-March 1986: U.S. Geological Survey Open-File Report 86-400, 75 p. ; 28 cm., https://doi.org/10.3133/ofr86400B.","productDescription":"75 p. ; 28 cm.","costCenters":[],"links":[{"id":162588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0400b/report-thumb.jpg"},{"id":85847,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0400b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afee4b07f02db6976d9","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":531847,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26784,"text":"wri864098 - 1986 - Hydrogeology of confined-drift aquifers near the Pomme de Terre and Chippewa rivers, western Minnesota","interactions":[],"lastModifiedDate":"2018-03-12T10:27:01","indexId":"wri864098","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4098","title":"Hydrogeology of confined-drift aquifers near the Pomme de Terre and Chippewa rivers, western Minnesota","docAbstract":"<p>Confined-drift aquifers in a 1,380-square-mile area of western Minnesota range in thickness from less than 10 feet to 114 feet. Transmissivities range from less than 1,000 square feet per day to over 16,000 square feet per day and theoretical well yields range from less than 100 gallons per minute to more than 1,800 gallons per minute.</p>\n<p>Regional ground water flow in the confined-drift aquifers is toward the Minnesota River and locally toward smaller streams, lakes, wetlands, and wells. Water levels near high-capacity pumping wells generally fluctuate 5 to 10 feet annually, compared to annual fluctuations of 2 to 3 feet in the surficial aquifers.</p>\n<p>Water from confined-drift aquifers generally is suitable for most uses. The water is hard to very hard and contains locally elevated concentrations of some chemical constituents. Dissolved-solids concentrations ranged from about 400 to 1,800 milligrams per liter.</p>\n<p>A ground-water-flow model indicated that increased pumping from two of the confined aquifers simulated, the Appleton and Benson-middle aquifers, would not adversely affect water levels. The addition of 30 hypothetical wells in the Benson-middle aquifer, pumping a total of approximately 792 million gallons per year, resulted in regional water-level declines of as much as 1.4 and 2.7 feet in the surficial and Benson-middle aquifers, respectively. The addition of 28 hypothetical wells in the Appleton aquifer, pumping a total of approximately 756 million gallons per year, lowered water levels as much as 5 feet in the surficial and Appleton aquifers. Simulations of reduced recharge and increased pumping, which could represent a 3-year drought, probably would lower water levels 2 to 6 feet regionally in the surficial and confined aquifers and as much as 11 feet near aquifer boundaries. Ground-water discharge to the Pomme de Terre and Chippewa Rivers in the southern part of the study area probably would be reduced by approximately 15.2 and 7.4 cubic feet per second, respectively, as a result of the simulated drought. Mean discharge of the Pomme de Terre and Chippewa Rivers is 104 and 267 cubic feet per second, respectively.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri864098","collaboration":"Prepared in cooperation with the Minnesota Department of Natural Resources and the Pomme de Terre and Chippewa Ground-water Study Steering Committee","usgsCitation":"Delin, G., 1986, Hydrogeology of confined-drift aquifers near the Pomme de Terre and Chippewa rivers, western Minnesota: U.S. Geological Survey Water-Resources Investigations Report 86-4098, Document: vi, 90 p.; 6 Plates: 42.39 x 37.23 inches or smaller, https://doi.org/10.3133/wri864098.","productDescription":"Document: vi, 90 p.; 6 Plates: 42.39 x 37.23 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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