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,{"id":30102,"text":"wri904084 - 1991 - Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah","interactions":[],"lastModifiedDate":"2017-09-13T16:14:50","indexId":"wri904084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4084","title":"Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah","docAbstract":"<p>Bydrologic data were collected for the proposed Quitchupah and Pines coal-lease tracts in Sevier and Bnery Counties, Utah, in order to describe the hydrology and potential effects of mining on the hydrologic system. The Quitchupah and Pines coal-lease tracts are near the Southern Utah Fuel Company coal mine in an area of the central Wasatch Plateau that is characterized by a relatively flat plateau deeply dissected by steep-sided canyons.</p><p>Surface water in the Quitchupah and Pines study area drains to two perennial streams, Muddy Creek to the north and Quitchupah Creek to the south. Peak streamflow is usually in May and June in response to snowmelt runoff; however, thunderstorms can cause short-term high flows in late summer and fall. The specific conductance of surface water in and near the study area measured during the 1987 water year ranged from 440 (iS/cm to 860 (iS/cm. Suspended-sediment concentrations ranged from 17 to 10,900 mg/L in the Quitchupah Creek drainage and 34 to 312 mg/L in the Muddy Creek drainage.</p><p>Stable-isotope studies indicate that recharge to aquifers in the study area is by seepage of snowmelt into rock outcrops. Discharge from the aquifers is at springs, seeps, mines, and zones of seepage in streambeds. The chemical quality of ground water is related to the mineralogy of the formations with which the water has contact. Water from the upper part of the Cast legate Sandstone has the smallest concentration of dissolved solids, 61 mg/L, and water from the North Horn Formation has the largest concentration, 1,080 mg/L.</p><p>Observed effects of underground coal mining at the nearby active mine are considered indicative of the changes that can be expected in the Quitchupah and Pines coal-lease tracts. Subsidence above the mined area could cause dewatering of the Blackhawk Formation and the Star Point Sandstone, changes in the natural drainage patterns, and alteration of both surface- and ground-water quality. Additional studies are needed to gain a better understanding of the hydrologic effects of underground mining in the Quitchupah and Pines coal-lease tracts.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, Utah","doi":"10.3133/wri904084","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Thiros, S.A., and Cordy, G., 1991, Hydrology and potential effects of mining in the Quitchupah and Pines coal-lease tracts, central Utah: U.S. Geological Survey Water-Resources Investigations Report 90-4084, Report: vii, 63 p.; Plate: 26.82 x 24.37 inches, https://doi.org/10.3133/wri904084.","productDescription":"Report: vii, 63 p.; Plate: 26.82 x 24.37 inches","numberOfPages":"72","costCenters":[],"links":[{"id":58920,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4084/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119617,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4084/report-thumb.jpg"},{"id":58919,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1990/4084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.4208,\n              39.03333\n            ],\n            [\n              -111.2583,\n              39.03333\n            ],\n            [\n               -111.2583,\n              38.95\n            ],\n            [\n              -111.3208,\n              38.95\n            ],\n            [\n              -111.3208,\n              38.88333\n            ],\n            [\n              -111.425,\n              38.88333\n            ],\n            [\n              -111.425,\n              38.93333\n            ],\n            [\n              -111.4589,\n               38.93333\n            ],\n            [\n              -111.4589,\n              38.9875\n            ],\n            [\n              -111.4208,\n              38.9875\n            ],\n            [\n              -111.4208,\n              39.03333\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60517d","contributors":{"authors":[{"text":"Thiros, Susan A. 0000-0002-8544-553X sthiros@usgs.gov","orcid":"https://orcid.org/0000-0002-8544-553X","contributorId":965,"corporation":false,"usgs":true,"family":"Thiros","given":"Susan","email":"sthiros@usgs.gov","middleInitial":"A.","affiliations":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"preferred":true,"id":202681,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cordy, G. 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,{"id":30280,"text":"wri894157 - 1991 - Use of Landsat imagery to estimate ground-water pumpage for irrigation on the Columbia Plateau in eastern Washington, 1985","interactions":[],"lastModifiedDate":"2022-10-26T16:33:22.328642","indexId":"wri894157","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4157","title":"Use of Landsat imagery to estimate ground-water pumpage for irrigation on the Columbia Plateau in eastern Washington, 1985","docAbstract":"<p>A method for estimating ground-water pumpage for irrigation was developed for the Columbia Plateau in eastern Washington. The method combines water-application rates estimated from pumpage data with acreage of irrigated crops that was mapped by using Landsat imagery. The study area consisted of Grant, Lincoln, Adams, and Franklin Counties, an area of approximately 8,900 square miles, and accounts for approximately three-fourths of the ground-water pumpage in the Columbia Plateau in eastern Washington. </p><p>Data from two passes of Landsat's multispectral scanner were analyzed by using a spectral band ratioing procedure to map irrigated crops for the study area. Data from one pass of Landsat's thematic mapper, covering approximately two-thirds of the study area, also were analyzed for determining irrigated crops in the area resulting in a 6-percent improvement in accuracy over the multispectral scanner analysis. </p><p>A total of 576 annual water-application rates associated with particular crops, for the 1982 through 1985 seasons, were calculated. A regression equation was developed for estimating annual water-application rates as a function of crop type, annual precipitation, irrigation system type, and available water capacity of the soil. Crops were grouped into three water-use categories: (1) small grains, primarily wheat and barley; (2) high water-use crops consisting of corn, alfalfa, and potatoes; and (3) miscellaneous vegetable and row crops. Annual water-application rates, expressed as a depth of water, then were multiplied by irrigated area determined by Landsat to estimate a volume of water pumped for irrigation for 1985-620,000 acre-feet. An assessment of accuracy for estimating pumpage for 28 of the sites showed that total predicted pumpage was within 4 percent of the total observed pumpage.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894157","usgsCitation":"Van Metre, P., and Seevers, P., 1991, Use of Landsat imagery to estimate ground-water pumpage for irrigation on the Columbia Plateau in eastern Washington, 1985: U.S. Geological Survey Water-Resources Investigations Report 89-4157, iv, 38 p., https://doi.org/10.3133/wri894157.","productDescription":"iv, 38 p.","costCenters":[{"id":222,"text":"Earth Resources Observation and Science (EROS) Center","active":true,"usgs":true}],"links":[{"id":408757,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_47245.htm","linkFileType":{"id":5,"text":"html"}},{"id":59069,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4157/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4157/report-thumb.jpg"}],"country":"United States","state":"Washington","otherGeospatial":"Columbia Plateau","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -120,\n              48\n            ],\n            [\n              -120,\n              46.2167\n            ],\n            [\n              -117.8333,\n              46.2167\n            ],\n            [\n              -117.8333,\n              48\n            ],\n            [\n              -120,\n              48\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db60517c","contributors":{"authors":[{"text":"Van Metre, P. C.","contributorId":92999,"corporation":false,"usgs":true,"family":"Van Metre","given":"P. C.","affiliations":[],"preferred":false,"id":202978,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seevers, Paul","contributorId":30258,"corporation":false,"usgs":true,"family":"Seevers","given":"Paul","email":"","affiliations":[],"preferred":false,"id":202977,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30427,"text":"wri904079 - 1991 - Regional ground-water flow in upper and middle Paleozoic rocks in southeastern Utah and adjacent parts of Arizona, Colorado, and New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri904079","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4079","title":"Regional ground-water flow in upper and middle Paleozoic rocks in southeastern Utah and adjacent parts of Arizona, Colorado, and New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904079","usgsCitation":"Weiss, E., 1991, Regional ground-water flow in upper and middle Paleozoic rocks in southeastern Utah and adjacent parts of Arizona, Colorado, and New Mexico: U.S. Geological Survey Water-Resources Investigations Report 90-4079, v, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904079.","productDescription":"v, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159816,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4079/report-thumb.jpg"},{"id":59201,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4079/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c4fd","contributors":{"authors":[{"text":"Weiss, Emanuel","contributorId":74383,"corporation":false,"usgs":true,"family":"Weiss","given":"Emanuel","affiliations":[],"preferred":false,"id":203231,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29215,"text":"wri904121 - 1991 - Estimates of hydraulic conductivity from aquifer-test analyses and specific-capacity data, Gulf Coast Regional Aquifer Systems, south-central United States","interactions":[],"lastModifiedDate":"2018-01-30T19:21:58","indexId":"wri904121","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4121","title":"Estimates of hydraulic conductivity from aquifer-test analyses and specific-capacity data, Gulf Coast Regional Aquifer Systems, south-central United States","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904121","usgsCitation":"Prudic, D.E., 1991, Estimates of hydraulic conductivity from aquifer-test analyses and specific-capacity data, Gulf Coast Regional Aquifer Systems, south-central United States: U.S. Geological Survey Water-Resources Investigations Report 90-4121, v, 38 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904121.","productDescription":"v, 38 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":58071,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4121/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4121/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcada","contributors":{"authors":[{"text":"Prudic, David E. deprudic@usgs.gov","contributorId":3430,"corporation":false,"usgs":true,"family":"Prudic","given":"David","email":"deprudic@usgs.gov","middleInitial":"E.","affiliations":[{"id":465,"text":"Nevada Water Science Center","active":true,"usgs":true}],"preferred":true,"id":201159,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29083,"text":"wri884016 - 1991 - Water quality of lakes and streams in Voyageurs National Park, northern Minnesota, 1977-84","interactions":[],"lastModifiedDate":"2022-09-27T18:38:46.93796","indexId":"wri884016","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"88-4016","title":"Water quality of lakes and streams in Voyageurs National Park, northern Minnesota, 1977-84","docAbstract":"<p>Water-quality investigations in six interconnected lakes that comprise most of the surface area of Voyageurs National Park in northern Minnesota revealed substantial differences in water-quality. Three large lakes; Sand Point, Namakan, and Rainy, near the eastern and northern boundaries of the Park; are oligotrophic to mesotrophic, having low dissolved solids and alkalinity, and dimictic circulation. In contrast, Kabetogama Lake, Black Bay, and Sullivan Bay, near the western and southern boundaries of the Park, were eutrophic, having higher dissolved solids and alkalinity, and polymictic circulation. Chemical characteristics of the three lakes along the eastern and northern boundary were similar to those of the Namakan River--a major source of inflow that drains an extensive area of exposed bedrock and thin noncalcareous drift east of the Park. The lake and embayments along the western and southern boundary receive inflow from two streams that drain an area west and south of the Park that is overlain by calcareous drift. Samples from one of these streams contained dissolved-solids concentrations about five times, and total alkalinity concentrations about eight times concentrations measured in the Namakan River. The nutrient-enriched lakes and embayments had high algal productivity that produced blooms of blue-green algae in some years. Annual patterns in the levels of trophic-state indicators revealed that the shallow, polymictic lakes experienced seasonal increases in totalphosphorus concentrations in their euphotic zones that did not occur in the deeper, dimictic lakes; this indicates a link between the frequent recirculation of these lakes and internal cycling of phosphorus. Secchi-disk transparency was limited by organic color in Sand Point, Namakan, and Rainy Lakes, and resuspended bottom material reduced transparency in Black Bay. Waters in the large lakes and embayments met nearly all U.S. Environmental Protection Agency criteria for protection of freshwater aquatic life, recreation, and drinking water. Some sites exceeded criteria because of oil and grease, phenols, sulfide, and ammonia. Reconnaissance sampling of 19 small lakes in remote areas of the Park indicated that most of them are sharply stratified and had very low dissolved solids and alkalinity concentrations (4.0-29 milligrams per liter total alkalinity). Thirteen of the lakes could be classified as moderately sensitive to acid precipitation, and two could be classified extremely sensitive. About half of the interior lakes had low nutrient concentrations (10-30 micrograms per liter total phosphorus) and low algal productivity (0.1- 2.0 micrograms per liter chlorophyll a). Five of the lakes had a marked reduction in trophic state from spring to summer. The Namakan River is the largest source of inflow to the Park and was found to have better quality than its receiving waters based on dissolved solids and nutrient concentrations, algal productivity, and transparency. The Ash River was found to deliver water that generally was poorer in quality than its receiving waters.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri884016","collaboration":"Prepared in cooperation with the National Park Service","usgsCitation":"Payne, G.A., 1991, Water quality of lakes and streams in Voyageurs National Park, northern Minnesota, 1977-84: U.S. Geological Survey Water-Resources Investigations Report 88-4016, vi, 95 p., https://doi.org/10.3133/wri884016.","productDescription":"vi, 95 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":407460,"rank":3,"type":{"id":36,"text":"NGMDB Index 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A.","contributorId":62190,"corporation":false,"usgs":true,"family":"Payne","given":"G.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200922,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29708,"text":"wri914105 - 1991 - Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri914105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4105","title":"Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914105","usgsCitation":"Sholar, C., and Wood, P., 1991, Evaluation of the drought susceptibility of water supplies used in the Kentucky River Basin in 1988: U.S. Geological Survey Water-Resources Investigations Report 91-4105, v, 34 p. :ill. ;28 cm., https://doi.org/10.3133/wri914105.","productDescription":"v, 34 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119481,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4105/report-thumb.jpg"},{"id":58526,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afde4b07f02db696eed","contributors":{"authors":[{"text":"Sholar, C.J.","contributorId":44186,"corporation":false,"usgs":true,"family":"Sholar","given":"C.J.","affiliations":[],"preferred":false,"id":201984,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wood, P.A.","contributorId":106540,"corporation":false,"usgs":true,"family":"Wood","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":201985,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28655,"text":"wri894057 - 1991 - Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon","interactions":[],"lastModifiedDate":"2017-02-07T08:23:34","indexId":"wri894057","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4057","title":"Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri894057","usgsCitation":"McFarland, W.D., and Ryals, G., 1991, Adequacy of available hydrogeologic data for evaluation of declining ground-water levels in the Fort Rock Basin, south-central Oregon: U.S. Geological Survey Water-Resources Investigations Report 89-4057, vii, 47 p. :ill., maps (1 col.) ;28 cm., https://doi.org/10.3133/wri894057.","productDescription":"vii, 47 p. :ill., maps (1 col.) ;28 cm.","costCenters":[{"id":518,"text":"Oregon Water Science Center","active":true,"usgs":true}],"links":[{"id":126839,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4057/report-thumb.jpg"},{"id":57497,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4057/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57498,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4057/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699665","contributors":{"authors":[{"text":"McFarland, W. D.","contributorId":57099,"corporation":false,"usgs":true,"family":"McFarland","given":"W.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":200180,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryals, G.N.","contributorId":47374,"corporation":false,"usgs":true,"family":"Ryals","given":"G.N.","email":"","affiliations":[],"preferred":false,"id":200179,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28715,"text":"wri904139 - 1991 - Surficial geology of the Cane Creek basin, Lauderdale County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri904139","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4139","title":"Surficial geology of the Cane Creek basin, Lauderdale County, Tennessee","docAbstract":"The surficial geology of the Cane Creek basin, in Lauderdale County, West Tennessee, was studied from 1985-88. Peoria Loess is the parent material from which soils in the Cane Creek drainage basin were derived. In general, a brown silt grades into a gray silt from 5 to I7 feet below ground surface. This color change probably represents depth to water table prior to the channelization of Cane Creek. Only at river mile 11.9 does rock outcrop near the main channel.\r\n\r\nLower reaches of major tributaries have surficial geology similar to the main channel. In upper reaches of Hyde Creek and Fain Spring Creek, the sequence from the St&ace is sand and gravels, red-brown sandstone, sand and clay layers, and then, an orange sand layer. \r\n\r\nCoarse-grained deposits are found most often along the northern boundary of the basin and only occasionally in areas to the west and south of the main channel. Depth to sand or gravel ranges from about 0 to 158 feet in the uplands, and generally deeper than 40 feet near the main channel.","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904139","usgsCitation":"Miller, J., 1991, Surficial geology of the Cane Creek basin, Lauderdale County, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 90-4139, iii, 12 p. :maps ;28 cm., https://doi.org/10.3133/wri904139.","productDescription":"iii, 12 p. :maps ;28 cm.","costCenters":[],"links":[{"id":159476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":2284,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri904139/","linkFileType":{"id":5,"text":"html"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db6889de","contributors":{"authors":[{"text":"Miller, J.H.","contributorId":67554,"corporation":false,"usgs":true,"family":"Miller","given":"J.H.","email":"","affiliations":[],"preferred":false,"id":200276,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":28688,"text":"wri894140 - 1991 - Availability of water from stratified-drift aquifers in the Farmington River valley, Simsbury, Connecticut","interactions":[],"lastModifiedDate":"2012-02-02T00:08:46","indexId":"wri894140","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4140","title":"Availability of water from stratified-drift aquifers in the Farmington River valley, Simsbury, Connecticut","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri894140","usgsCitation":"Melvin, R., and Bingham, J., 1991, Availability of water from stratified-drift aquifers in the Farmington River valley, Simsbury, Connecticut: U.S. Geological Survey Water-Resources Investigations Report 89-4140, v, 77 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri894140.","productDescription":"v, 77 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121739,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4140/report-thumb.jpg"},{"id":57528,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4140/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57529,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1989/4140/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":57530,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4140/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d72e","contributors":{"authors":[{"text":"Melvin, R.L.","contributorId":50497,"corporation":false,"usgs":true,"family":"Melvin","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":200236,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bingham, J.W.","contributorId":35295,"corporation":false,"usgs":true,"family":"Bingham","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":200235,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29706,"text":"wri914147 - 1991 - Flood of June 14-15, 1990, in Belmont, Jefferson, and Harrison counties, Ohio, with emphasis on Pipe and Wegee Creek basins near Shadyside","interactions":[],"lastModifiedDate":"2012-02-02T00:08:54","indexId":"wri914147","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4147","title":"Flood of June 14-15, 1990, in Belmont, Jefferson, and Harrison counties, Ohio, with emphasis on Pipe and Wegee Creek basins near Shadyside","docAbstract":"A series of violent thunderstorms caused severe floods and consequent damage in the central part of Ohio during June 14-15, 1990. The eastern part of the State, particularly Belmont, Harrison, and Jefferson Counties, sustained the most damage. In the Pipe and Wegee Creek basins near Shadyside, Belmont County, at least 24 people died and property damage exceeded $10 million.\r\n\r\nAn indirect measurement of discharge on Pipe Creek made near the mouth, indicates a peak discharge of 15,000 ft? /s (cubic feet per second) for the drainage area of 11.3 mi? (square miles) and a unit discharge of 1,330 (ft? /s)/mi? (cubic feet per second per square mile). The recurrence interval for this peak discharge is greater than 100 years. An indirect measurement of discharge of Wegee Creek, made 3 miles upstream from the mouth, indicates a peak discharge of 2,200 (ft? /s) /mi? . The recurrence interval for this peak discharge also is greater than 100 years. Longitudal water-surface profiles showed depths ranging from 7 ft. to 22 ft.\r\n\r\nThe severity of flooding was highly variable. For example, the recurrence interval of the peak discharge at one U.S. Geological Survey streamflow-gaging station was only 2 years, whereas the recurrence interval for the peak discharge was greater than 100 years at another gaging station about 22 miles away.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914147","usgsCitation":"Shindel, H., 1991, Flood of June 14-15, 1990, in Belmont, Jefferson, and Harrison counties, Ohio, with emphasis on Pipe and Wegee Creek basins near Shadyside: U.S. Geological Survey Water-Resources Investigations Report 91-4147, vi, 33 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914147.","productDescription":"vi, 33 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":126784,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4147/report-thumb.jpg"},{"id":58524,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab2e4b07f02db66eb95","contributors":{"authors":[{"text":"Shindel, H.L.","contributorId":17652,"corporation":false,"usgs":true,"family":"Shindel","given":"H.L.","affiliations":[],"preferred":false,"id":201982,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29117,"text":"wri884192 - 1991 - Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:53","indexId":"wri884192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"88-4192","title":"Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri884192","usgsCitation":"Peterson, D.A., 1991, Streamflow recharge to the Madison Limestone and the Casper Formation in the Glenrock area, east-central Wyoming: U.S. Geological Survey Water-Resources Investigations Report 88-4192, iv, 18 p. :ill. ;28 cm., https://doi.org/10.3133/wri884192.","productDescription":"iv, 18 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":159525,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1988/4192/report-thumb.jpg"},{"id":57987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1988/4192/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b15e4b07f02db6a4d57","contributors":{"authors":[{"text":"Peterson, D. A.","contributorId":6453,"corporation":false,"usgs":true,"family":"Peterson","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200972,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30063,"text":"wri904184 - 1991 - Ground-water quality in the Nemaha Natural Resources District, southeastern Nebraska, 1989","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri904184","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4184","title":"Ground-water quality in the Nemaha Natural Resources District, southeastern Nebraska, 1989","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports [distributor],","doi":"10.3133/wri904184","usgsCitation":"Tanner, D.Q., and Steele, G.V., 1991, Ground-water quality in the Nemaha Natural Resources District, southeastern Nebraska, 1989: U.S. Geological Survey Water-Resources Investigations Report 90-4184, iv, 52 p. :ill. ;28 cm., https://doi.org/10.3133/wri904184.","productDescription":"iv, 52 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":119678,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4184/report-thumb.jpg"},{"id":58876,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4184/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db667209","contributors":{"authors":[{"text":"Tanner, D. Q.","contributorId":73224,"corporation":false,"usgs":true,"family":"Tanner","given":"D.","email":"","middleInitial":"Q.","affiliations":[],"preferred":false,"id":202613,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steele, G. V.","contributorId":62543,"corporation":false,"usgs":true,"family":"Steele","given":"G.","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":202612,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28906,"text":"wri914054 - 1991 - Suspended-sediment budgets for four drainage basins tributary to Lake Tahoe, California and Nevada, 1984-87","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri914054","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4054","title":"Suspended-sediment budgets for four drainage basins tributary to Lake Tahoe, California and Nevada, 1984-87","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-file Reports Section [distributor],","doi":"10.3133/wri914054","usgsCitation":"Nolan, K., and Hill, B.R., 1991, Suspended-sediment budgets for four drainage basins tributary to Lake Tahoe, California and Nevada, 1984-87: U.S. Geological Survey Water-Resources Investigations Report 91-4054, v, 40 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914054.","productDescription":"v, 40 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159148,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4054/report-thumb.jpg"},{"id":57778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4054/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687fb2","contributors":{"authors":[{"text":"Nolan, K.M.","contributorId":36151,"corporation":false,"usgs":true,"family":"Nolan","given":"K.M.","affiliations":[],"preferred":false,"id":200597,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hill, B. R.","contributorId":72833,"corporation":false,"usgs":true,"family":"Hill","given":"B.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":200598,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30061,"text":"wri894209 - 1991 - Water resources of the island of Kahoolawe, Hawaii: Preliminary findings","interactions":[],"lastModifiedDate":"2022-12-23T19:37:03.734673","indexId":"wri894209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"89-4209","title":"Water resources of the island of Kahoolawe, Hawaii: Preliminary findings","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri894209","usgsCitation":"Takasaki, K., 1991, Water resources of the island of Kahoolawe, Hawaii: Preliminary findings: U.S. Geological Survey Water-Resources Investigations Report 89-4209, iii, 17 p., https://doi.org/10.3133/wri894209.","productDescription":"iii, 17 p.","costCenters":[],"links":[{"id":411010,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_49234.htm","linkFileType":{"id":5,"text":"html"}},{"id":122218,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1989/4209/report-thumb.jpg"},{"id":58874,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1989/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Hawaii","otherGeospatial":"Kahoolawe Island","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -156.73507690429688,\n              20.486200430098492\n            ],\n            [\n              -156.49887084960938,\n              20.486200430098492\n            ],\n            [\n              -156.49887084960938,\n              20.632784250388028\n            ],\n            [\n              -156.73507690429688,\n              20.632784250388028\n            ],\n            [\n              -156.73507690429688,\n              20.486200430098492\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f0236","contributors":{"authors":[{"text":"Takasaki, K. J.","contributorId":44523,"corporation":false,"usgs":true,"family":"Takasaki","given":"K. J.","affiliations":[],"preferred":false,"id":202609,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30191,"text":"wri904172 - 1991 - A preliminary forecast of the advance of Hubbard Glacier and its influence on Russell Fiord, Alaska","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri904172","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4172","title":"A preliminary forecast of the advance of Hubbard Glacier and its influence on Russell Fiord, Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri904172","usgsCitation":"Trabant, D., Krimmel, R.M., and Post, A., 1991, A preliminary forecast of the advance of Hubbard Glacier and its influence on Russell Fiord, Alaska: U.S. Geological Survey Water-Resources Investigations Report 90-4172, v, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri904172.","productDescription":"v, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121459,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4172/report-thumb.jpg"},{"id":58987,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4172/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1fe4b07f02db6aab68","contributors":{"authors":[{"text":"Trabant, D.C.","contributorId":42209,"corporation":false,"usgs":true,"family":"Trabant","given":"D.C.","email":"","affiliations":[],"preferred":false,"id":202833,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Krimmel, R. M.","contributorId":81093,"corporation":false,"usgs":true,"family":"Krimmel","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":202834,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Post, Austin","contributorId":90709,"corporation":false,"usgs":true,"family":"Post","given":"Austin","affiliations":[],"preferred":false,"id":202835,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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Carolina\",\"nation\":\"USA  \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648747","contributors":{"authors":[{"text":"Patterson, G. G.","contributorId":40242,"corporation":false,"usgs":true,"family":"Patterson","given":"G.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":200889,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, B.A.","contributorId":28283,"corporation":false,"usgs":true,"family":"Davis","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":200888,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":28924,"text":"wri914080 - 1991 - Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri914080","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"91-4080","title":"Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River","language":"ENGLISH","publisher":"U.S. Geological Survey ;\r\nBooks and Open-File Reports Section [distributor],","doi":"10.3133/wri914080","usgsCitation":"Oblinger, C.J., Sheets, R.A., and Bair, E., 1991, Hydrology and water quality near the South Well Field, southern Franklin County, Ohio, with emphasis on the simulation of ground-water flow and transport of Scioto River: U.S. Geological Survey Water-Resources Investigations Report 91-4080, vii, 78 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri914080.","productDescription":"vii, 78 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":121718,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1991/4080/report-thumb.jpg"},{"id":57797,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1991/4080/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e87e","contributors":{"authors":[{"text":"Oblinger, C. J.","contributorId":21554,"corporation":false,"usgs":true,"family":"Oblinger","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":200626,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sheets, R. A.","contributorId":43381,"corporation":false,"usgs":true,"family":"Sheets","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200627,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bair, E. Scott","contributorId":73231,"corporation":false,"usgs":true,"family":"Bair","given":"E. Scott","affiliations":[],"preferred":false,"id":200628,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29456,"text":"wri904163 - 1991 - Water resources of the Red Lake Indian Reservation, northwestern Minnesota","interactions":[],"lastModifiedDate":"2018-03-19T11:20:34","indexId":"wri904163","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1991","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":"90-4163","title":"Water resources of the Red Lake Indian Reservation, northwestern Minnesota","docAbstract":"<p>This report presents the results of a study by the U.S. Geological Survey, done in cooperation with the Red Lake Indian Reservation Tribal Council, to evaluate the water resources of the contiguous Red Lake Indian Reservation. Water resources of the contiguous Red Lake Indian Reservation meet the present (1989) needs for potable supply and other household uses. In addition, they provide ecological, recreational, and aesthetic benefits.</p>\n<p>Mean annual precipitation in the study area is 22.7 inches. Approximately 90 percent of this precipitation returns to the atmosphere by evapotranspiration; the remainder becomes runoff. Some of the precipitation that contributes to evapotranspiration and runoff initially infiltrates the land surface and recharges the ground-water reservoir. The net recharge to ground water generally ranges from roughly 0.5 to 1.35 inches per year. Assuming negligible long-term changes in the amount of ground water in storage, the recharge to and discharge from the ground-water reservoir balance each other over time.</p>\n<p>Glacial-drift aquifers are the source of ground water in the Red Lake Indian Reservation. The most significant sources of ground-water supply are confined glacial-drift aquifers, which are discontinuous lenses of sand and gravel 50 to 150 feet below land surface. Estimated yields of wells completed in these aquifers range from approximately 20 to 240 gallons per minute.</p>\n<p>Lower and Upper Red Lakes, which extend over one fourth of the study area, are the largest surface-water bodies. The study area also includes streams and many smaller lakes. Most of the streams drain into Lower and Upper Red Lakes, and the lakes discharge into the Red Lake River. Spring snowmelt generally causes peak flows in the streams. Low-flow conditions commonly occur during midsummer to early fall and winter.</p>\n<p>The quality of ground water is suitable for drinking and other household uses, and the quality of the surface water generally meets U.S. Environmental Protection Agency criteria necessary for the maintenance of aquatic life. The major ions in both ground and surface water are calcium, magnesium, and bicarbonate. Lower and Upper Red Lakes are eutrophic to mesotrophic on the basis of their summer Secchi disk-transparency readings, which ranged from 2.6 to 8.2 feet. The concentration of total organic carbon in samples from Lower and Upper Red Lakes and four streams were below or, in the case of one stream, about equal to 30 milligrams per liter, which is indicative of water little affected by human activities. The sample with the highest organic carbon content was collected from a stream that drained peatlands, which were probably sources of organic matter in the runoff. The concentration of nitrite plus nitrate in samples collected from Lower and Upper Red Lakes in late summer was below 0.01 milligrams per liter, which is characteristic of water uncontaminated by animal wastes. Total phosphorus in these samples ranged from 0.01 to 0.02 milligrams per liter. Most of this phosphorus was in the particulate organic fraction because of the abundance of phytoplankton.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri904163","collaboration":"Prepared in cooperation with the Red Lake Indian Reservation Tribal Council","usgsCitation":"Ruhl, J.F., 1991, Water resources of the Red Lake Indian Reservation, northwestern Minnesota: U.S. Geological Survey Water-Resources Investigations Report 90-4163, vi, 49 p., https://doi.org/10.3133/wri904163.","productDescription":"vi, 49 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":58301,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1990/4163/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123219,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1990/4163/report-thumb.jpg"}],"country":"United States","state":"Minnesota","otherGeospatial":"Red Lake Indian Reservation","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -94.72824096679688,\n              48.20911695037711\n            ],\n            [\n              -94.71176147460938,\n              47.87214396888731\n            ],\n            [\n              -94.80789184570312,\n              47.87030156386572\n            ],\n            [\n              -94.80514526367188,\n              47.80393135603966\n            ],\n            [\n              -95.38604736328125,\n              47.80393135603966\n            ],\n            [\n              -95.40115356445312,\n              47.821453962500016\n            ],\n            [\n              -95.40939331054688,\n              47.8260641920274\n            ],\n            [\n              -95.42724609375,\n              47.82975208084834\n            ],\n            [\n              -95.4327392578125,\n              47.843579330145474\n            ],\n            [\n              -95.44097900390625,\n              47.84910919811478\n            ],\n            [\n              -95.45883178710938,\n              47.8527954492302\n            ],\n            [\n              -95.46844482421875,\n              47.855559965615484\n            ],\n            [\n              -95.47119140625,\n              47.871222774564146\n            ],\n            [\n              -95.48080444335938,\n              47.88043398091892\n            ],\n            [\n              -95.49316406249999,\n              47.88780176702122\n            ],\n            [\n              -95.50140380859374,\n              47.897930761804936\n            ],\n            [\n              -95.50140380859374,\n              47.908978314728685\n            ],\n            [\n              -95.52886962890625,\n              47.91542163178686\n            ],\n            [\n              -95.55221557617188,\n              47.91634204016118\n            ],\n            [\n              -95.5645751953125,\n              47.924624978768314\n            ],\n            [\n              -95.57830810546875,\n              47.9264654516972\n            ],\n            [\n              -95.57968139648438,\n              48.1789071002632\n            ],\n            [\n              -94.86282348632812,\n              48.182569848918504\n            ],\n            [\n              -94.79827880859375,\n              48.19721822655714\n            ],\n            [\n              -94.77218627929688,\n              48.203625575146994\n            ],\n            [\n              -94.72824096679688,\n              48.20911695037711\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f4e4b07f02db5f03d7","contributors":{"authors":[{"text":"Ruhl, J. 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