{"pageNumber":"554","pageRowStart":"13825","pageSize":"25","recordCount":16498,"records":[{"id":9991,"text":"ofr801298 - 1981 - Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977","interactions":[],"lastModifiedDate":"2024-06-04T21:30:23.997764","indexId":"ofr801298","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-1298","title":"Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977","docAbstract":"<p>Hydrologic and chemical data were collected during base-flow conditions on three streams in southeastern Montana from October 26 to November 5, 1977, to characterize groundwater discharge. Maximum measured flow of Otter Creek, an interrupted stream, was 1.2 cubic feet per second. The water chemistry was dominated by sodium, magnesium, and sulfate ions, with a maximum dissolved-solids concentration of 3,540 milligrams per liter. Chemistry of groundwater inflow is dominated by sodium, magnesium, and sulfate. A discharge of 156 cubic feet per second from the Tongue River Reservoir into the Tongue River complicated interpretation of groundwater discharge to the reach downstream from the reservoir. Many reaches of gain and loss were observed along the Tongue River; the flow near the mouth was 233 cubic feet per second. Minor changes in quality of the base flow indicate groundwater discharges dominated by sodium, sulfate, and bicarbonate plus carbonate. Dissolved-solids concentration increased from 506 milligrams per liter near the dam to 630 milligrams per liter near the mouth. Maximum measured flow of Rosebud Creek was 19.0 cubic feet per second. Water quality in the upper reaches was dominated by magnesium, calcium , and bicarbonate, with dissolved-solids concentrations ranging from 560 to 703 milligrams per liter. Sodium, sulfate, and dissolved solids increase downstream.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr801298","usgsCitation":"Lee, R.W., Slagle, S.E., and Stimson, J.R., 1981, Magnitude and chemical quality of base flow of Otter Creek, Tongue River, and Rosebud Creek, southeastern Montana, October 26-November 5, 1977: U.S. Geological Survey Open-File Report 80-1298, Report: iv, 29 p.; 1 Plate: 19.02 x 18.56 inches, https://doi.org/10.3133/ofr801298.","productDescription":"Report: iv, 29 p.; 1 Plate: 19.02 x 18.56 inches","costCenters":[],"links":[{"id":429509,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11517.htm","linkFileType":{"id":5,"text":"html"}},{"id":37801,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/1298/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37802,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/1298/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142534,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/1298/report-thumb.jpg"}],"country":"United States","state":"Montana","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107.25,\n              46.5\n            ],\n            [\n              -107.25,\n              45\n            ],\n            [\n              -105.5,\n              45\n            ],\n            [\n              -105.5,\n              46.5\n            ],\n            [\n              -107.25,\n              46.5\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db6494e7","contributors":{"authors":[{"text":"Lee, Roger W.","contributorId":105273,"corporation":false,"usgs":true,"family":"Lee","given":"Roger","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160631,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Slagle, Steven E.","contributorId":35284,"corporation":false,"usgs":true,"family":"Slagle","given":"Steven","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160629,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stimson, James R.","contributorId":77152,"corporation":false,"usgs":true,"family":"Stimson","given":"James","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":160630,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":10621,"text":"ofr811072 - 1981 - Results of exploratory drilling at Point MacKenzie, Alaska, 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:06:21","indexId":"ofr811072","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1072","title":"Results of exploratory drilling at Point MacKenzie, Alaska, 1981","docAbstract":"The Matanuska-Susitna Borough anticipates industrial development near Point MacKenzie, Alaska. Because little hydrologic information is available for the area, the Borough contracted for the drilling of two test wells. It was found that: Both wells penetrated unconsolidated stratified clay, silt, sand, and gravel; each well penetrated a shallow unconfined and deeper confined aquifers; the water levels in the wells rise and fall with the tide; the chemical analyses indicate that the water quality meets the Alaska Drinking Water Standards, except for slightly high levels of manganese and pH; and the potential for saltwater intrusion should be evaluated as part of future studies. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811072","usgsCitation":"Patrick, L., 1981, Results of exploratory drilling at Point MacKenzie, Alaska, 1981: U.S. Geological Survey Open-File Report 81-1072, ii, 11 p. ill. ;28 cm., https://doi.org/10.3133/ofr811072.","productDescription":"ii, 11 p. ill. ;28 cm.","costCenters":[],"links":[{"id":142488,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1072/report-thumb.jpg"},{"id":38453,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ae4b07f02db6248c1","contributors":{"authors":[{"text":"Patrick, Leslie","contributorId":36136,"corporation":false,"usgs":true,"family":"Patrick","given":"Leslie","email":"","affiliations":[],"preferred":false,"id":161695,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44656,"text":"wri8054 - 1981 - Appraisal of Hydrologic Information Needed in Anticipation of Lignite Mining in Lauderdale County, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:11:03","indexId":"wri8054","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-54","title":"Appraisal of Hydrologic Information Needed in Anticipation of Lignite Mining in Lauderdale County, Tennessee","docAbstract":"Lignite in western Tennessee occurs as lenses or beds at various stratigraphic horizons in the Coastal Plain sediments of Late Cretaceous and Tertiary age. The occurrence of this lignite has been known for many decades, but not until the energy crisis was it considered an important energy resource. In recent years, several energy companies have conducted extensive exploration programs in western Tennessee, and tremendous reserves of lignite have been found.\r\n\r\nFrom available information, Lauderdale County was selected as one of the counties where strip-mining of lignite will most likely occur. Lignite in this county occurs in the Jackson and Cockfield Formations, undivided, of Tertiary age. The hydrology of the county is known only from regional studies and the collection of some site-specific data. Therefore, in anticipation of the future mining of lignite, a plan is needed for obtaining hydrologic and geologic information to adequately define the hydrologic system before mining begins and to monitor the effects of strip-mining once it is begun.\r\n\r\nFor this planning effort, available hydrologic, geologic, land use, and associated data were located and compiled; a summary description of the surface and shallow subsurface hydrologic system was prepared: the need for additional baseline hydrologic information was outlined; and plans to monitor the effects of strip-mining were proposed. This planning approach, although limited to a county area, has transferability to other Coastal Plain areas under consideration for strip-mining of lignite.","language":"ENGLISH","doi":"10.3133/wri8054","usgsCitation":"Parks, W.S., 1981, Appraisal of Hydrologic Information Needed in Anticipation of Lignite Mining in Lauderdale County, Tennessee: U.S. Geological Survey Water-Resources Investigations Report 80-54, vi, 67 p. : ill., maps ; 28 cm., https://doi.org/10.3133/wri8054.","productDescription":"vi, 67 p. : ill., maps ; 28 cm.","costCenters":[],"links":[{"id":3761,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri80-0054","linkFileType":{"id":5,"text":"html"}},{"id":124476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_80_54.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac6e4b07f02db67a3c0","contributors":{"authors":[{"text":"Parks, William Scott","contributorId":52148,"corporation":false,"usgs":true,"family":"Parks","given":"William","email":"","middleInitial":"Scott","affiliations":[],"preferred":false,"id":230207,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8759,"text":"ofr811125 - 1981 - Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","interactions":[],"lastModifiedDate":"2022-08-31T19:15:57.552529","indexId":"ofr811125","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1125","title":"Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective","docAbstract":"<p>The channels of the Platte River and its major tributaries, the South Platte and North Platte Rivers in Colorado, Wyoming, and Nebraska, have undergone major changes in hydrologic regime and morphology since 1860. These changes are attributed here to agricultural, municipal, and industrial water use.</p><p>Although water-resource development varied temporally throughout the basin, the history of development along the Platte River and tributaries followed four stages: (1) Construction of small, crude ditches to irrigate flood plains; (2) construction of larger canals to irrigate bench lands; (3) construction of reservoirs to store snowmelt runoff; and (4) accelerated development of ground-water resources. Despite differences in rates of development, diversion and storage of water for irrigation, municipal, and industrial use have changed streamflow patterns throughout the basin. At some stations, significant changes in flood peaks, annual mean discharges, and shapes of flow-duration curves have been recorded.</p><p>Changes in streamflow patterns are manifested by changes in appearance of channels of the Platte River. Prior to water development in the 19th century, the Platte was a wide (-2 kilometers), shallow (1.8 to 2.4 meters) river characterized by bankfull spring flows and low summer flows. Although timber generally was scarce in the valley, the Platte channels contained hundreds of small, timbered islands. Since development, the channels have changed radically. Comparing surveyor's maps (General Land Office), drawn during the 1860's, with six sets of aerial photographs, taken between 1938 and 1979, for six 5-kilometer reaches of the river shows that the channels have narrowed considerably above the confluence with the Loup River. The width of the channels in 1979 ranged from 8 to 50 percent of the channel width in 1860. Below the confluence with the Loup River, the width of the river in 1979 was about 92 percent of the channel width in 1860. Above the confluence with the Loup River, width reduction has occurred by progressive encroachment of vegetation and consequent vertical and horizontal accretion on sand bars in the channel. Vegetative encroachment on sand bars has occurred because (1) the present hydrologic regime provides more favorable conditions for germination and growth on sand bars, and (2) since development of the basin, flood peaks are no longer capable of scouring vegetation from the sand bars. Overbank flows evidently have become more common, probably because channel narrowing and vegetative encroachment have increased the hydraulic roughness of the channels. Moreover, the magnitude of low flows has increased and the days of no flows has decreased giving the channels a more perennial character.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811125","usgsCitation":"Eschner, T., Hadley, R.F., and Crowley, K., 1981, Hydrologic and morphologic changes in channels of the Platte River basin: A historical perspective: U.S. Geological Survey Open-File Report 81-1125, v, 57 p., https://doi.org/10.3133/ofr811125.","productDescription":"v, 57 p.","costCenters":[],"links":[{"id":406027,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1125/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1125/report-thumb.jpg"}],"country":"United States","state":"Colorado, Nebraska, Wyoming","otherGeospatial":"Platte River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              39.57182223734374\n            ],\n            [\n              -95.9326171875,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              43.99281450048989\n            ],\n            [\n              -108.67675781249999,\n              39.57182223734374\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6117ba","contributors":{"authors":[{"text":"Eschner, T.R.","contributorId":45700,"corporation":false,"usgs":true,"family":"Eschner","given":"T.R.","email":"","affiliations":[],"preferred":false,"id":158281,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":158280,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Crowley, K.D.","contributorId":86769,"corporation":false,"usgs":true,"family":"Crowley","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":158282,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","interactions":[{"subject":{"id":7233,"text":"ofr79988 - 1979 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"ofr79988","publicationYear":"1979","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"predicate":"SUPERSEDED_BY","object":{"id":3127,"text":"wsp2068 - 1981 - Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","indexId":"wsp2068","publicationYear":"1981","noYear":false,"title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},"id":1}],"lastModifiedDate":"2023-03-14T20:06:08.759442","indexId":"wsp2068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2068","title":"Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah","docAbstract":"<p>Data obtained during a hydrologic reconnaissance in 1975-77 in the Wasatch Plateau-Book Cliffs coal-fields area of Utah were correlated with existing long-term data. Maps were prepared showing average precipitation, average streamflow, stream temperature, ground- and surface-water quality, sediment yield, and geology. Recommendations were made for additional study and suggested approaches for continued monitoring in the coalfields areas.</p><p>moDuring the 1931-75 water years, the minimum discharges for the five major streams that head in the area ranged from about 12,000 to 26,000 acre-feet per year, and the maximum discharges ranged from about 59,000 to 315,000 acre-feet per year. Correlations indicate that 3 years of low-flow records at stream sites in the Wasatch Plateau would allow the development of relationships with long-term sites that can be used to estimate future low-flow records within a standard error of about 20 percent.</p><p>Most water-quality degradation in streams occurs along the flanks of the Wasatch Plateau and Book Cliffs. In the uplands, dissolved-solids concentrations generally ranged from less than 100 to about 250 milligrams per liter, and in the lowlands, the concentrations ranged from about 250 to more than 6,000 milligrams per liter.</p><p>Most springs in the Wasatch Plateau and Book Cliffs discharge from the Star Point Sandstone or younger formations, and the water generally contains less than about 1,000 milligrams per liter of dissolved solids. The discharges of 65 springs ranged from about 0.2 to 200 gallons per minute. The Blackhawk Formation, which is the principal coal-bearing formation, produces water in many of the mines. The dissolved-solids concentration in water discharging from springs and mines in the Blackhawk ranged from about 60 to 800 milligrams per liter.</p><p>In the lowland areas, the Ferron Sandstone Member of the Maneos Shale appears to have the most potential for subsurface development of water of suitable chemical quality for human consumption. Three wells in the Ferron yielded water with dissolved-solids concentrations ranging from about 650 to 1,230 milligrams per liter.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2068","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management and the U.S. Environmental Protection Agency","usgsCitation":"Waddell, K.M., Contratto, P., Sumsion, C.T., and Butler, J.R., 1981, Hydrologic reconnaissance of the Wasatch Plateau-Book Cliffs coal-fields area, Utah: U.S. Geological Survey Water Supply Paper 2068, Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches, https://doi.org/10.3133/wsp2068.","productDescription":"Report: v, 45 p.; 9 Plates: 40.00 in x 30.19 inches or smaller; Table: 12.50 in. x 13.45 inches","numberOfPages":"61","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":414125,"rank":13,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25489.htm","linkFileType":{"id":5,"text":"html"}},{"id":30038,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":247290,"rank":11,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Hydrgraphs for selected wells, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247284,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-3.pdf","text":"Plate 3","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average discharges of streams, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247283,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing average annual precipitation, 1931-75, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247282,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing general geology of the Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":139323,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2068/report-thumb.jpg"},{"id":247289,"rank":10,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-8.pdf","text":"Plate 8","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Fence diagram showing stratigraphic units and concentrations of dissolved solids, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247288,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-7.pdf","text":"Plate 7","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in ground water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247287,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-6.pdf","text":"Plate 6","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated sediment yields, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247286,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-5.pdf","text":"Plate 5","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing concentrations of dissolved solids in surface water, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247285,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2068/plate-4.pdf","text":"Plate 4","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing estimated range of stream temperature, Wasatch Plateau-Book Cliffs coal-fields area, Utah"},{"id":247291,"rank":12,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/wsp/2068/plate-table_2.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Published stream-gaging records and ranges of annual discharge, 1931-75 water years"}],"country":"United States","state":"Utah","otherGeospatial":"Wasatch Plateau-Book Cliffs coal-fields area","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -111.54,\n              40.045\n            ],\n            [\n              -111.54,\n              38.687\n            ],\n            [\n              -109.059,\n              38.687\n            ],\n            [\n              -109.059,\n              40.045\n            ],\n            [\n              -111.54,\n              40.045\n            ]\n          ]\n       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Kay","contributorId":15598,"corporation":false,"usgs":true,"family":"Contratto","given":"P. Kay","affiliations":[],"preferred":false,"id":146300,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Sumsion, C. T.","contributorId":23129,"corporation":false,"usgs":true,"family":"Sumsion","given":"C.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":146302,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Butler, John R.","contributorId":36540,"corporation":false,"usgs":true,"family":"Butler","given":"John","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146303,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8740,"text":"ofr81678 - 1981 - Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana","interactions":[],"lastModifiedDate":"2018-02-16T16:22:55","indexId":"ofr81678","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-678","title":"Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana","docAbstract":"The purpose of the investigation is to provide a means to assess the impacts on surface-water hydrology due to changes in land use resulting from surface mining of coal in the Fort Union Coal Region, North Dakota and Montana. The objectives of the study are to: (1) Determine premining hydrologic conditions in small representative drainage basins and provide historical data with which to compare the magnitude of changes resulting from mining, and (2) develop the capability of making reasonably accurate projections of hydrologic effects resulting from the various land-use changes caused by surface mining. Data collection has been underway since October 1976 for the West Branch Antelope Creek study area in western North Dakota and since March 1978 for the Hay Creek study area in eastern Montana. Data collected during the premining period are being analyzed using statistical methods for the evaluation of the premining conditions. A digitial model with the capability of making hydrologic projections is being developed. Most of the model components have been tested during 1979 and 1980. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81678","usgsCitation":"Emerson, D.G., 1981, Progress report on the effects of surface mining on the surface-water hydrology of selected basins in the Fort Union coal region, North Dakota and Montana: U.S. Geological Survey Open-File Report 81-678, v, 33 p., https://doi.org/10.3133/ofr81678.","productDescription":"v, 33 p.","costCenters":[{"id":478,"text":"North Dakota Water Science Center","active":true,"usgs":true},{"id":34685,"text":"Dakota Water Science Center","active":true,"usgs":true}],"links":[{"id":142709,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0678/report-thumb.jpg"},{"id":36317,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0678/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a82e4b07f02db64af90","contributors":{"authors":[{"text":"Emerson, Douglas G.","contributorId":40579,"corporation":false,"usgs":true,"family":"Emerson","given":"Douglas","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":158244,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38159,"text":"ofr81423 - 1981 - Hydrology of Area 33, eastern region, Interior Coal Province, Indiana and Kentucky","interactions":[],"lastModifiedDate":"2021-09-03T11:54:45.501973","indexId":"ofr81423","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-423","title":"Hydrology of Area 33, eastern region, Interior Coal Province, Indiana and Kentucky","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81423","usgsCitation":"Wangsness, D.J., 1981, Hydrology of Area 33, eastern region, Interior Coal Province, Indiana and Kentucky: U.S. Geological Survey Open-File Report 81-423, v, 149 p., https://doi.org/10.3133/ofr81423.","productDescription":"v, 149 p.","costCenters":[],"links":[{"id":97383,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0423/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":165692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0423/report-thumb.jpg"},{"id":388818,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12032.htm"}],"country":"United States","state":"Indiana, Kentucky","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.7060,\n              37.3230\n            ],\n            [\n              -86.3230,\n              37.3230\n            ],\n            [\n              -86.3230,\n              38.3640\n            ],\n            [\n              -87.7060,\n              38.3640\n            ],\n            [\n              -87.7060,\n              37.3230\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602059","contributors":{"authors":[{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":219239,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6955,"text":"ofr82169 - 1981 - Activities in Idaho; status of projects, fiscal year 1981","interactions":[],"lastModifiedDate":"2022-08-23T13:41:15.264711","indexId":"ofr82169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"82-169","title":"Activities in Idaho; status of projects, fiscal year 1981","docAbstract":"<p>Twenty-three projects were conducted by the Water Resources Division of the U.S. Geological Survey in Idaho during fiscal year 1981. These projects were made in cooperation with 6 State and local and 11 Federal agencies. State and local cooperative funding amounted to $720,670; Federal funding amounted to $2,437,628.</p><p>Eighty-three persons were employed--40 full time and 43 other than full time. In addition, the Water Resources Division maintains a project office at the Idaho National Engineering Laboratory. Work there is done in cooperation with the U.S. Department of Energy, the sole funding source.</p><p>Projects other than continuing programs for collection of hydrologic data included flood-characteristics and flood-mapping studies, geothermal-resource investigations, ground-water quality assessments, basin- and region-wide water-resource investigations, river quality-of-water monitoring studies, volcanic-ash related studies, and ground-water-trends and stream-gaging program evaluations.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82169","usgsCitation":"Channel, L.K., 1981, Activities in Idaho; status of projects, fiscal year 1981: U.S. Geological Survey Open-File Report 82-169, i, 42 p., https://doi.org/10.3133/ofr82169.","productDescription":"i, 42 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,{"id":7505,"text":"ofr81401 - 1981 - Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr81401","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-401","title":"Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis","docAbstract":"Increasing demand for water to meet needs for energy, industry, irrigation, domestic, and municipal uses has resulted in a study of the geology and hydrology of rocks of Mesozoic and Cenozoic age. This report presents the results of a literature search for the part of the study area in Montana. It consists of an annotated listing of pertinent published reports, a partial subject and area index of the reports, and a correlation chart of geologic and aquifer units listed in the annotations. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81401","usgsCitation":"Levings, J.F., Levings, G.W., Feltis, R., Hotchkiss, W.R., and Lee, R.W., 1981, Selective annotated bibliography of geology and ground-water resources for the Montana part of the Northern Great Plains regional aquifer-system analysis: U.S. Geological Survey Open-File Report 81-401, iii, 93 p., 1 over-size sheet ;26 cm., https://doi.org/10.3133/ofr81401.","productDescription":"iii, 93 p., 1 over-size sheet ;26 cm.","costCenters":[],"links":[{"id":142181,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0401/report-thumb.jpg"},{"id":34959,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0401/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34960,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0401/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a00e4b07f02db5f7d3b","contributors":{"authors":[{"text":"Levings, Julianne F.","contributorId":29818,"corporation":false,"usgs":true,"family":"Levings","given":"Julianne","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":155922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Levings, G. W.","contributorId":12485,"corporation":false,"usgs":true,"family":"Levings","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155921,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Feltis, R.D.","contributorId":93467,"corporation":false,"usgs":true,"family":"Feltis","given":"R.D.","affiliations":[],"preferred":false,"id":155925,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Hotchkiss, W. R.","contributorId":61820,"corporation":false,"usgs":true,"family":"Hotchkiss","given":"W.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":155923,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Lee, R. W.","contributorId":86757,"corporation":false,"usgs":true,"family":"Lee","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":155924,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":9173,"text":"ofr811112 - 1981 - Preliminary data from Arbuckle test wells, Miami, Douglas, Saline, and Labette counties, Kansas","interactions":[],"lastModifiedDate":"2016-02-22T09:26:45","indexId":"ofr811112","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1112","title":"Preliminary data from Arbuckle test wells, Miami, Douglas, Saline, and Labette counties, Kansas","docAbstract":"<p>Preliminary data are presented for test wells in Kansas that were completed in Cambrian and Ordovician rocks of the Arbuckle Group in late 1979 and early 1980. Included in the report are hole history, electrical logs, geology (sample descriptions and cores), hydrologic testing, and geochemistry. These wells were drilled as part of a cooperative investigation between the U.S. Geological Survey and the Kansas Geological Survey, the Kansas Department of Health and Environment, and the U.S. Army Corps of Engineers to determine the regional hydrology of the Arbuckle Group and to investigate the hydraulic characteristics of the formation at site-specific areas.</p>\n<p>The test wells were drilled in Miami (site 1), Douglas (site 2), Saline (site 3), and Labette (site4) Counties, Kansas. Depths of the wells ranged from 1,816 feet in Labette County to 3,665 feet in Saline County. All wells have surface casing installed to depths well below the base of freshwater. The wells were cased from land surface to near the top of the Arbuckle Group; the remainder of the hole was left open so that additional hydrologic tests could be made.</p>\n<p>Cores of rocks in the Arbuckle Group were collected at sites 2, 3, and 4. Results ofcore analyses are presented for vertical and horizontal permeability to air, porosity , fluid saturation, accoustic velocity, resistivity indices, and formation factor. Gamma-ray logs of the core were run for correlation with electrical logs. A series of electrical logs was run at each site, consisting of dual-induction laterolog, sonic, and compensated neutron-formation density logs for correlating geologic and hydrologic data. Flow logs and temperature logs also were run at some sites.</p>\n<p>Formation data from drill-stem tests are presented for use in calculating transmissivity, hydraulic conductivity, and hydraulic head. Complete analyses of water samples from wells at sites 2, 3, and 4, and a partial analysis at site 1, are presented to indicate water quality in the aquifers.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811112","usgsCitation":"Gogel, T., 1981, Preliminary data from Arbuckle test wells, Miami, Douglas, Saline, and Labette counties, Kansas: U.S. Geological Survey Open-File Report 81-1112, 155 p., https://doi.org/10.3133/ofr811112.","productDescription":"155 p.","numberOfPages":"156","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":141650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/ofr811112.jpg"},{"id":318185,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1112/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Kansas","county":"Douglas County, Labette County, Miami County, Saline County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"MultiPolygon\",\"coordinates\":[[[[-95.188,39.0437],[-95.1875,38.9635],[-95.1762,38.9659],[-95.1737,38.9681],[-95.1712,38.9721],[-95.1642,38.9814],[-95.152,38.9766],[-95.1474,38.9737],[-95.141,38.9713],[-95.1305,38.9683],[-95.1133,38.9687],[-95.1076,38.964],[-95.1083,38.9604],[-95.1025,38.9589],[-95.1001,38.9588],[-95.0872,38.9571],[-95.0794,38.9596],[-95.079,38.9678],[-95.0861,38.9807],[-95.0788,38.9836],[-95.0693,38.9847],[-95.064,38.985],[-95.061,38.985],[-95.0593,38.9836],[-95.0558,38.9816],[-95.0572,38.7395],[-95.5006,38.7383],[-95.5016,38.8703],[-95.502,38.9039],[-95.5021,38.9175],[-95.504,39.0586],[-95.4831,39.0608],[-95.4639,39.0676],[-95.4483,39.0699],[-95.4353,39.07],[-95.4137,39.0627],[-95.4025,39.0592],[-95.3832,39.0538],[-95.3757,39.0504],[-95.3717,39.0467],[-95.3654,39.0415],[-95.3578,39.0377],[-95.3479,39.0338],[-95.3367,39.0331],[-95.3195,39.034],[-95.3043,39.0414],[-95.2965,39.043],[-95.2908,39.0401],[-95.2885,39.0378],[-95.2858,39.0322],[-95.2831,39.0381],[-95.2831,39.0394],[-95.2864,39.0445],[-95.242,39.0438],[-95.188,39.0437]]],[[[-95.087,37.3843],[-95.073,37.3843],[-95.0739,37.3417],[-95.0723,36.9994],[-95.0723,36.9987],[-95.4003,37.0005],[-95.4067,37.0005],[-95.5236,37.0009],[-95.521,37.3844],[-95.087,37.3843]]],[[[-94.6102,38.7376],[-94.6123,38.4758],[-94.6124,38.4673],[-94.6134,38.3892],[-95.066,38.3905],[-95.0658,38.6948],[-95.0558,38.695],[-95.0572,38.7395],[-94.6102,38.7376]]],[[[-97.9281,38.9592],[-97.705,38.9584],[-97.3736,38.9595],[-97.372,38.61],[-97.9261,38.6102],[-97.9282,38.8713],[-97.9281,38.9592]]]]},\"properties\":{\"name\":\"Douglas\",\"state\":\"KS\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3716","contributors":{"authors":[{"text":"Gogel, Tony","contributorId":37745,"corporation":false,"usgs":true,"family":"Gogel","given":"Tony","email":"","affiliations":[],"preferred":false,"id":159221,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10640,"text":"ofr81922 - 1981 - Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","interactions":[],"lastModifiedDate":"2022-11-16T19:38:09.654274","indexId":"ofr81922","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-922","title":"Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978","docAbstract":"<p>Hydrologic investigations of urban drainage basins in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. Studies were completed in the Fort Worth metropolitan area at the end of the 1977 water year, and in the Dallas metropolitan area at the end of the 1979 water year.</p><p>The Geological Survey, in cooperation with the Texas Department of Water Resources, expanded the existing streamflow network in the San Antonio metropolitan area in May 1968 to begin urban hydrology studies in this area. In September 1968, the program was further expanded to include the collection of water-quality data.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81922","collaboration":"Prepared in cooperation with the Texas Department of Water Resources","usgsCitation":"Perez, R., 1981, Hydrologic data for urban studies in the San Antonio, Texas, metropolitan area, 1978: U.S. Geological Survey Open-File Report 81-922, 91 p., https://doi.org/10.3133/ofr81922.","productDescription":"91 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":409400,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0922/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144071,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0922/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"San Antonio","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.123373210819224\n            ],\n            [\n              -98.19580078125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.699982298744377\n            ],\n            [\n              -98.8165283203125,\n              29.123373210819224\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db6079f2","contributors":{"authors":[{"text":"Perez, Roberto","contributorId":97114,"corporation":false,"usgs":true,"family":"Perez","given":"Roberto","email":"","affiliations":[],"preferred":false,"id":161726,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","interactions":[{"subject":{"id":10125,"text":"ofr81220 - 1981 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","indexId":"ofr81220","publicationYear":"1981","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska"},"predicate":"SUPERSEDED_BY","object":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"chapter":"E","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"id":1}],"supersededBy":{"id":45714,"text":"pp1273E - 1983 - Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming","indexId":"pp1273E","publicationYear":"1983","noYear":false,"title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, and Wyoming"},"lastModifiedDate":"2022-08-09T15:28:15.441093","indexId":"ofr81220","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-220","title":"Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska","docAbstract":"<p>The need for large quantities of energy has created interest in the Fort Union coal region of the Northern Great Plains. Extensive development of this coal, which may include onsite steam-power generation, gasification, liquefaction, and slurry-pipeline transport of the coal from this region, would place a heavy demand on the region's limited streamflow. Paleozoic rocks that underlie the Fort Union coal region and aquifers in these rocks, including the Red River Formation and the Madison Limestone, might supply, at least on a temporary basis, a significant part of the water required for coal development. The area of study covers approximately 200,000 square miles, and includes eastern Montana, western North Dakota and South Dakota, northeastern Wyoming, and northwestern Nebraska. This report, one of a series in the Madison Limestone study, uses hydrologic and geologic data to outline potentially favorable areas for well construction - that is, areas in which there is a good probability that large-yield wells (more than 500 gallons per minute) can be completed in the Red River Formation and in the Madison Limestone. Potentially favorable areas in terms of aquifer characteristics, for both the Red River Formation and the Madison Limestone, are given a numerical evaluation from 1 to 3 based on the number of the following criteria that are met: (1) the presence of more than 100 feet of relatively porous rock, (2) the presence of more than 100 feet of dolomite, and (3) the presence of known geologic structures which could affect yield. Areas rated 3 are those in which all three criteria are satisfied; areas rated 2 are those in which two criteria are satisfied; and areas rated 1 are those in which only one criterion is satisfied. The criteria selected for this analysis were chosen because they can be recognized and mapped over the entire study area. Local features such as minor structures, solution zones, and rock facies of small extent were not included in this regional evaluation. In addition, water quality was considered in a general way in defining the favorable areas, by excluding areas in which the electrical resistivity of formation water, as calculated from geophysical well logs, was less than 1 ohm-meter. The numerical scales of the Red River Formation and Madison Limestone are summed to show potentially favorable areas for the combined aquifers. Certain additional factors which may be important to a prospective water user were not included in the numerical ranking - these include depths to the two aquifers, calcite saturation, water temperature, total dissolved solids, and piezometric head in relation to land surface. For a complete evaluation, potential users should consider these factors plus local structures, facies, and solution zones in conjunction with the numerical rankings reflecting aquifer characteristics. To facilitate consideration of piezometric head, maps are included in this report showing areas in which the piezometric head falls in certain ranges with respect to land surface.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81220","usgsCitation":"MacCary, L., Cushing, E.M., and Brown, D.L., 1981, Potentially favorable areas for large-yield wells in the Red River Formation and Madison Limestone in parts of Montana, North Dakota, South Dakota, Wyoming, and Nebraska: U.S. Geological Survey Open-File Report 81-220, Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches, https://doi.org/10.3133/ofr81220.","productDescription":"Report: vi, 29 p.; 1 Plate: 17.86 x 21.76 inches","costCenters":[],"links":[{"id":405012,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0220/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405011,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0220/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":145531,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0220/report-thumb.jpg"}],"country":"United States","state":"Montana, Nebraska, North Dakota, South Dakota, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -115.13671875,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              40.111688665595956\n            ],\n            [\n              -96.328125,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              49.03786794532644\n            ],\n            [\n              -115.13671875,\n              40.111688665595956\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86be","contributors":{"authors":[{"text":"MacCary, L.M.","contributorId":13200,"corporation":false,"usgs":true,"family":"MacCary","given":"L.M.","email":"","affiliations":[],"preferred":false,"id":160852,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cushing, E. M.","contributorId":94273,"corporation":false,"usgs":true,"family":"Cushing","given":"E.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":160854,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Brown, David L.","contributorId":55425,"corporation":false,"usgs":true,"family":"Brown","given":"David","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":160853,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":31045,"text":"ofr81149 - 1981 - Preliminary data from a series of artificial recharge experiments at Stanton, Texas","interactions":[],"lastModifiedDate":"2016-08-23T15:45:59","indexId":"ofr81149","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-149","title":"Preliminary data from a series of artificial recharge experiments at Stanton, Texas","docAbstract":"<p>A series of artificial recharge experiments was conducted by the U.S. Geological Survey at an experimental site located in Stanton, Texas. Five tests were performed from March 1977 through December 1978 to: (1) Evaluate the hydraulic properties of the aquifer; (2) test sampling and monitoring equipment; (3) compare tracers for future use in hydrologic investigations; and (4) determine the radial and vertical distribution of hydraulic properties at the site. Suites of inorganic, and both volatile and nonvolatile organic tracers were used in the tests, and comparative data were obtained from sampling points at several radial distances and depths from the injection well. Hydraulic data from aquifer tests and geologic data from core material also were obtained during the investigation.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr81149","usgsCitation":"Bassett, R., Weeks, E., Ceazan, M., Perkins, S., Signor, D., Redinger, D., Malcolm, R., Aiken, G., Thurman, E., Avery, P., Wood, W., Thompson, G., and Stiles, G., 1981, Preliminary data from a series of artificial recharge experiments at Stanton, Texas: U.S. Geological Survey Open-File Report 81-149, ix, 235 p., https://doi.org/10.3133/ofr81149.","productDescription":"ix, 235 p.","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":164100,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0149/report-thumb.jpg"},{"id":59601,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0149/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","city":"Stanton","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b06e4b07f02db69a244","contributors":{"authors":[{"text":"Bassett, R.L.","contributorId":13233,"corporation":false,"usgs":true,"family":"Bassett","given":"R.L.","email":"","affiliations":[],"preferred":false,"id":204666,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Weeks, E.P.","contributorId":38514,"corporation":false,"usgs":true,"family":"Weeks","given":"E.P.","email":"","affiliations":[],"preferred":false,"id":204669,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ceazan, M.L.","contributorId":80015,"corporation":false,"usgs":true,"family":"Ceazan","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":204673,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Perkins, S.G.","contributorId":93483,"corporation":false,"usgs":true,"family":"Perkins","given":"S.G.","email":"","affiliations":[],"preferred":false,"id":204675,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Signor, D. C.","contributorId":95100,"corporation":false,"usgs":true,"family":"Signor","given":"D. C.","affiliations":[],"preferred":false,"id":204676,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Redinger, D.L.","contributorId":103139,"corporation":false,"usgs":true,"family":"Redinger","given":"D.L.","email":"","affiliations":[],"preferred":false,"id":204678,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Malcolm, Ronald L.","contributorId":46075,"corporation":false,"usgs":true,"family":"Malcolm","given":"Ronald L.","affiliations":[],"preferred":false,"id":204670,"contributorType":{"id":1,"text":"Authors"},"rank":7},{"text":"Aiken, G. R. 0000-0001-8454-0984","orcid":"https://orcid.org/0000-0001-8454-0984","contributorId":14452,"corporation":false,"usgs":true,"family":"Aiken","given":"G. R.","affiliations":[],"preferred":false,"id":204667,"contributorType":{"id":1,"text":"Authors"},"rank":8},{"text":"Thurman, E.M.","contributorId":102864,"corporation":false,"usgs":true,"family":"Thurman","given":"E.M.","affiliations":[],"preferred":false,"id":204677,"contributorType":{"id":1,"text":"Authors"},"rank":9},{"text":"Avery, P.A.","contributorId":52450,"corporation":false,"usgs":true,"family":"Avery","given":"P.A.","email":"","affiliations":[],"preferred":false,"id":204671,"contributorType":{"id":1,"text":"Authors"},"rank":10},{"text":"Wood, W.W.","contributorId":21974,"corporation":false,"usgs":true,"family":"Wood","given":"W.W.","email":"","affiliations":[],"preferred":false,"id":204668,"contributorType":{"id":1,"text":"Authors"},"rank":11},{"text":"Thompson, G.M.","contributorId":57246,"corporation":false,"usgs":true,"family":"Thompson","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":204672,"contributorType":{"id":1,"text":"Authors"},"rank":12},{"text":"Stiles, G.K.","contributorId":91629,"corporation":false,"usgs":true,"family":"Stiles","given":"G.K.","email":"","affiliations":[],"preferred":false,"id":204674,"contributorType":{"id":1,"text":"Authors"},"rank":13}]}}
,{"id":9353,"text":"ofr81135 - 1981 - Hydrology of area 22, Eastern Coal Province, Alabama","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr81135","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-135","title":"Hydrology of area 22, Eastern Coal Province, Alabama","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81135","usgsCitation":"Harkins, J.R., and and others, 1981, Hydrology of area 22, Eastern Coal Province, Alabama: U.S. Geological Survey Open-File Report 81-135, v, 72 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81135.","productDescription":"v, 72 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0135/report.pdf","size":"18190","linkFileType":{"id":1,"text":"pdf"}},{"id":144149,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0135/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602bca","contributors":{"authors":[{"text":"Harkins, Joe R.","contributorId":28982,"corporation":false,"usgs":true,"family":"Harkins","given":"Joe","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":159532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528901,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8619,"text":"ofr81542 - 1981 - The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr81542","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-542","title":"The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments","docAbstract":"A requirement of Public Law 95-87, the Surface Mining Control and Reclamation Act of 1977, is the understanding of the hydrology in actual and proposed surface-mined areas. Surface-water data for small specific-sites and for larger areas such as adjacent and general areas are needed also to satisfy the hydrologic requirements of the Act. The Act specifies that surface-water modeling techniques may be used to generate the data and information. The purpose of this report is to describe how this can be achieved for smaller watersheds. This report also characterizes 12 ' state-of-the-art ' strip-mining assessment models that are to be tested with data from two data-intensive studies involving small watersheds in Tennessee and Indiana. Watershed models are best applied to small watersheds with specific-site data. Extending the use of modeling techniques to larger watersheds remains relatively untested, and to date the upper limits for application have not been established. The U.S. Geological Survey is currently collecting regional hydrologic data in the major coal provinces of the United States and this data will be used to help satisfy the ' general-area ' data requirements of the Act. This program is reviewed and described in this report. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81542","usgsCitation":"Doyle, W., 1981, The U.S. Geological Survey Coal Hydrology Program and the potential of hydrologic models for impact assessments: U.S. Geological Survey Open-File Report 81-542, v, 61 p. :maps ;28 cm., https://doi.org/10.3133/ofr81542.","productDescription":"v, 61 p. :maps ;28 cm.","costCenters":[],"links":[{"id":141105,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0542/report-thumb.jpg"},{"id":36209,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0542/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667575","contributors":{"authors":[{"text":"Doyle, W. Harry","contributorId":32900,"corporation":false,"usgs":true,"family":"Doyle","given":"W. Harry","affiliations":[],"preferred":false,"id":158038,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7422,"text":"ofr811187 - 1981 - Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","interactions":[],"lastModifiedDate":"2012-02-02T00:06:04","indexId":"ofr811187","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1187","title":"Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma","docAbstract":"Bedrock in the Blocker area of southeastern Oklahoma consists principally of shale, siltstone, and sandstone of the Boggy and Savanna Formations of Pennsylvanian age. These rocks have been folded to form the Panther Mountain syncline on the south and the Kinta anticline on the north. Alluvium along streams is less than 15 feet thick and consists mainly of sandy silt. Water in bedrock is under artesian conditions. Well depths range from 11 to 213 feet and average 75 feet. In 86% of the wells measured, the water level was less than 30 feet below the land surface. Because the rocks have minimal permeability, well yields probably are less than 5 gallons per minute. Ground water is commonly a mixed cation bicarbonate type with dissolved solids ranging from about 300 to 2,000 milligrams per liter. No relationship between water chemistry and well depth or geographic distribution is apparent. Streams in the area are ephemeral and there are extended periods of no flow. Blue Creek was dry 30% of the time during 1976-80 and had flows of less than 0.1 cubic foot per second for at least 80 consecutive days. Stream water is generally a mixed cation sulfate type. The maximum dissolved-solids concentration determined in stream water was 3670 milligrams per liter. Maximum suspended sediment discharge, in tons per day, was about 235 for Blue Creek, 40 for Blue Creek tributary, and 630 for Mathuldy Creek. Silt-clay particles (diameters less than 0.062 millimeter) are the dominant sediment size. Surface mining for coal undoubtedly will have some effect on the environment. The most likely deleterious effects are increased sediment loads in streams and increased mineralization of stream waters. However, these effects should be of only limited extent and duration if appropriate mining and reclamation practices are followed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811187","usgsCitation":"Marcher, M.V., Bergman, D.L., Stoner, J., and Blumer, S.P., 1981, Preliminary appraisal of the hydrology of the Blocker area, Pittsburg County, Oklahoma: U.S. Geological Survey Open-File Report 81-1187, iv, 52 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811187.","productDescription":"iv, 52 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140449,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1187/report-thumb.jpg"},{"id":34831,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34832,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34833,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1187/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":34834,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1187/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67ca5b","contributors":{"authors":[{"text":"Marcher, Melvin V.","contributorId":11590,"corporation":false,"usgs":true,"family":"Marcher","given":"Melvin","email":"","middleInitial":"V.","affiliations":[],"preferred":false,"id":155545,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bergman, D. L.","contributorId":93038,"corporation":false,"usgs":true,"family":"Bergman","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":155548,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stoner, J.D.","contributorId":58261,"corporation":false,"usgs":true,"family":"Stoner","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":155547,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Blumer, S. P.","contributorId":23938,"corporation":false,"usgs":true,"family":"Blumer","given":"S.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":155546,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":3021,"text":"wsp2177 - 1981 - Hydrologic effects of stress-relief fracturing in an Appalachian Valley","interactions":[],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"wsp2177","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"2177","title":"Hydrologic effects of stress-relief fracturing in an Appalachian Valley","docAbstract":"A hydrologic study at Twin Falls State Park, Wyoming County, West Virginia, was made to determine how fracture systems affect the occurrence and movement of ground water in a typical valley of the Appalachian Plateaus Physiographic Province. Twin Falls was selected because it is generally unaffected by factors that would complicate an analysis of the data. The study area was the Black Fork Valley at Twin Falls. The valley is about 3 miles long and 400 to 600 feet wide and is cut into massive sandstone units interbedded with thin coal and shale beds. The study was made to determine how aquifer characteristics were related to fracture systems in this valley, so that the relation could be applied to studies of other valleys. \r\n\r\nTwo sites were selected for test drilling, pumping tests, and geophysical studies. One site is in the upper part of the valley, and the second is near the lower central part. At both sites, ground water occurs mainly in horizontal bedding-plane fractures under the valley floor and in nearly vertical and horizontal slump fractures along the valley wall. The aquifer is under confined conditions under the valley floor and unconfined conditions along the valley wall. The fractures pinch out under the valley walls, which form impermeable barriers. Tests of wells near the valley center indicated a change in storage coefficient as the cone of depression caused by pumping reached the confined-unconfined boundaries; the tests also indicated barrier-image effects when the cone reached the impermeable boundaries. Drawdown from pumping near the center of the valley affected water levels at both sites, indicating a hydraulic connection from the upper to the lower end of the valley. Stream gain-and-loss studies show that ground water discharges to the stream from horizontal fractures beneath Black Fork Falls, near the mouth of Black Fork. The fracture systems that constitute most of the transmissive part of the aquifer at Twin Falls are like those described as being formed from stress relief. As stress-relief fractures have been described in other valleys of the Appalachian Plateaus, the same aquifer conditions may exist in those valleys.","language":"ENGLISH","publisher":"G.P.O.,","doi":"10.3133/wsp2177","usgsCitation":"Wyrick, G.G., and Borchers, J.W., 1981, Hydrologic effects of stress-relief fracturing in an Appalachian Valley: U.S. Geological Survey Water Supply Paper 2177, vii, 51 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wsp2177.","productDescription":"vii, 51 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":139462,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2177/report-thumb.jpg"},{"id":29851,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2177/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db606ff8","contributors":{"authors":[{"text":"Wyrick, Granville G.","contributorId":67493,"corporation":false,"usgs":true,"family":"Wyrick","given":"Granville","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":146160,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Borchers, James W.","contributorId":25931,"corporation":false,"usgs":true,"family":"Borchers","given":"James","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":146159,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":8544,"text":"ofr811185 - 1981 - Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","interactions":[],"lastModifiedDate":"2022-09-02T17:15:45.287223","indexId":"ofr811185","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-1185","title":"Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport","docAbstract":"<p>The lower Merrimack River basin study area drains approximately 180 square miles along the New Hampshire border in northeastern Massachusetts. This area includes parts of the Merrimack River basin within Massachusetts east of the Beaver Brook and Concord River basins, except for the Shawsheen River basin. Even though the Blackwater River basin within Massachusetts isn't part of the lower Merrimack River basin, it has been included in this report. Principal tributaries to the Merrimack River, which discharges to the Atlantic Ocean at Newburyport, Massachusetts, are: Bare Meadow, Bartlett, Cobbler Creek, Fish, Richardson, and Trull Brooks, Artichoke, East Meadow, Indian, Little, Powwow, and Spicket Rivers, and Johnson Creek.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr811185","collaboration":"Prepared in cooperation with the Commonwealth of Massachusetts, Water Resources Commission","usgsCitation":"Delaney, D.F., and Gay, F.B., 1981, Hydrologic data of the lower Merrimack River basin, Massachusetts, from Concord River, Lowell, to Plum Island, Newburyport: U.S. Geological Survey Open-File Report 81-1185, Report: iii, 34 p.; 1 Plate: 44.98 x 34.31 inches, https://doi.org/10.3133/ofr811185.","productDescription":"Report: iii, 34 p.; 1 Plate: 44.98 x 34.31 inches","costCenters":[],"links":[{"id":406153,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/1185/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":406152,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1185/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141699,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1185/report-thumb.jpg"}],"country":"United States","state":"Massachusetts","otherGeospatial":"Merrimack River basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -71.30401611328125,\n              42.64204079304426\n            ],\n            [\n              -70.80001831054688,\n              42.64204079304426\n            ],\n            [\n              -70.80001831054688,\n              42.85180609584705\n            ],\n            [\n              -71.30401611328125,\n              42.85180609584705\n            ],\n            [\n              -71.30401611328125,\n              42.64204079304426\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607348","contributors":{"authors":[{"text":"Delaney, David F.","contributorId":41797,"corporation":false,"usgs":false,"family":"Delaney","given":"David","email":"","middleInitial":"F.","affiliations":[{"id":27261,"text":"U.S. Army Construction Engineering Research Laboratory, Champaig","active":true,"usgs":false}],"preferred":false,"id":157911,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gay, Frederick B.","contributorId":102052,"corporation":false,"usgs":true,"family":"Gay","given":"Frederick","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":157912,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9126,"text":"ofr81682 - 1981 - Hydrologic data for urban storm runoff from nine sites in the Denver metropolitan area, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:12","indexId":"ofr81682","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-682","title":"Hydrologic data for urban storm runoff from nine sites in the Denver metropolitan area, Colorado","docAbstract":"Urban storm-runoff data were collected April through September 1980, from nine urbanrunoff sites in the Denver metropolitan area, and are presented in this report. The sites consist of two single-family residential areas, two multi-family residential areas, one commercial area (shopping center), one mixed commercial and multi-family residential area, one native area (open space), and two detention ponds. Precipitation, rainfall-runoff, water-quality (common constituents, nutrients, coliform bacteria, solids, and trace elements) and basin-area data are necessary to use the U.S. Geological Survey 's Distributed Routing Rainfall-Runoff Model, Version II. The urban storm-runoff data may be used to characterize runoff pollution loading for various land-use types in Denver and other semi-arid regions. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81682","usgsCitation":"Gibbs, J.W., 1981, Hydrologic data for urban storm runoff from nine sites in the Denver metropolitan area, Colorado: U.S. Geological Survey Open-File Report 81-682, viii, 150 p. ill., maps ;28 cm., https://doi.org/10.3133/ofr81682.","productDescription":"viii, 150 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":142021,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0682/report-thumb.jpg"},{"id":36747,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36748,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36749,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36750,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36751,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36752,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36753,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0682/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36754,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0682/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db6081e2","contributors":{"authors":[{"text":"Gibbs, Johnnie W.","contributorId":14410,"corporation":false,"usgs":true,"family":"Gibbs","given":"Johnnie","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":159145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":7312,"text":"ofr8174 - 1981 - Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr8174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-74","title":"Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8174","usgsCitation":"Shown, L., Frickel, D., Hadley, R.F., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine: The Tsosie Swale basin, San Juan County, New Mexico: U.S. Geological Survey Open-File Report 81-74, vi, 63 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8174.","productDescription":"vi, 63 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140619,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0074/report-thumb.jpg"},{"id":34702,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fcb","contributors":{"authors":[{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":155176,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Frickel, D. G.","contributorId":11213,"corporation":false,"usgs":true,"family":"Frickel","given":"D. G.","affiliations":[],"preferred":false,"id":155174,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":155175,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":155177,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8526,"text":"ofr80159 - 1981 - Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-03-30T16:12:06","indexId":"ofr80159","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"80-159","title":"Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma","docAbstract":"<p>The U.S. Geological Survey has collected data on Oklahoma's groundwater resources since 1934. The data in this report were collected as part of a study in cooperation with the Oklahoma Water Resources Board to evaluate the geohydrology of the alluvium and terrace aquifer of the Beaver-North Canadian River 4] in northwestern Oklahoma. The data include records of approximately 900 wells, test-holes, and springs, results of chemical analyses of water from 30 wells tapping the aquifer, monthly water-level measurements for selected wells, and low-flow discharge measurements of the Beaver-North Canadian River and its tributaries (plate 1). All of the data were collected in the field during the period 1977-79. Information prior to this period is not included in this report but is contained in reports by Wood and Stacy (1965) and Morton (in press).</p><p>The stratigraphic nomenclature is that of the Oklahoma Geological Survey and does.not necessarily agree with that of the U.S. Geological Survey.</p><p>Acknowledgement is extended to the residents of the study area for their cooperation in obtaining the data in this report.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr80159","usgsCitation":"Davis, R.E., Christenson, S.C., and Blumer, S.P., 1981, Hydrologic data for the alluvium and terrace aquifer of the Beaver-North Canadian River from the Panhandle to Canton Reservoir, northwestern Oklahoma: U.S. Geological Survey Open-File Report 80-159, Report: iii, 77 p.; Plate: 28.92 x 21.39 inches, https://doi.org/10.3133/ofr80159.","productDescription":"Report: iii, 77 p.; Plate: 28.92 x 21.39 inches","costCenters":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"links":[{"id":142798,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Oklahoma","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -100,\n              36\n            ],\n            [\n              -98.5,\n              36\n            ],\n            [\n              -98.5,\n              37\n            ],\n            [\n              -100,\n              37\n            ],\n            [\n              -100,\n              36\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c62d","contributors":{"authors":[{"text":"Davis, Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157872,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157873,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blumer, Stephen P. spblumer@usgs.gov","contributorId":2419,"corporation":false,"usgs":true,"family":"Blumer","given":"Stephen","email":"spblumer@usgs.gov","middleInitial":"P.","affiliations":[],"preferred":true,"id":157871,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":8525,"text":"ofr81483 - 1981 - Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","interactions":[],"lastModifiedDate":"2018-11-05T11:39:46","indexId":"ofr81483","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-483","title":"Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma","docAbstract":"<p>A quantitative description of the hydrologic system in alluvium and terrace deposits along the Beaver-North Canadian River in northwestern Oklahoma is needed as an aid for planning and management of the aquifer. A two-dimensional finite-difference model was used to describe the aquifer and to predict the effects of future ground-water withdrawals.</p><p>The aquifer principally consists of three geologic units: Alluvium with an average thickness of 30 feet, low terrace deposits with an average thickness of 50 feet, and high terrace deposits with an average thickness of 70 feet. A thin cover of dune sand overlies much of the area and provides an excellent catchment for recharge, but is generally unsaturated.</p><p>Hydraulic conductivity of the aquifer ranges from 0 to 160 feet per day and averages 59 feet per day. Specific yield is estimated to be 0.29. Recharge to the aquifer is approximately 1 inch annually. Under present conditions (1978), most discharge is the result of ground-water flow to the Beaver-North Canadian River at a rate of 36 cubic feet per second and to pumpage for public-supply, industrial, and irrigation use at a rate of 28 cubic feet per second. In 1978, the aquifer had an average saturated thickness of 31 feet and contained 4.07 million acre-feet of water.</p><p>The model was used to predict future head response in the aquifer to various pumping stresses. For any one area, the pumping stress was applied until the saturated thickness for that area was less than 5 feet, at which time the pumping ceased.</p><p>The results of the modeled projections show that if the aquifer is stressed from 1978 to 1993 at the 1977 pumpage rates and well distribution, the average saturated thickness will decrease 1.0 foot and the volume of water in storage will be 3.94 million acre-feet, or 97 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 0.7 foot and the volume of water in storage will be 3.84 million acre-feet, or 94 percent of the 1978 volume.</p><p>If all areas of the aquifer having a 1978 saturated thickness of 5 feet or more are stressed from 1978 to 1993 at a rate of approximately<br>1.4 acre-feet per acre per year, the average saturated thickness will decrease by 20.9 feet and the volume of water in storage will be 1.28 million acre-feet, or 31 percent of the 1978 volume. If the aquifer is stressed at this same rate until 2020, the average saturated thickness will decrease an additional 2.2 feet and the volume of water in storage will be 980,000 acre-feet, or 24 percent of the 1978 volume.</p><p>The water in the aquifer is generally of the calcium bicarbonate type and is suitable for most uses. Most of the 30 water samples analyzed contained less than 500 milligrams of dissolved solids per liter.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81483","usgsCitation":"Davis, R.E., and Christenson, S.C., 1981, Geohydrology and numerical simulation of the alluvium and terrace aquifer along the Beaver-North Canadian River from the Panhandle to Canton Lake, northwestern Oklahoma: U.S. Geological Survey Open-File Report 81-483, Report: vi, 42 p.; 15 Plates, https://doi.org/10.3133/ofr81483.","productDescription":"Report: vi, 42 p.; 15 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Robert E.","contributorId":10403,"corporation":false,"usgs":true,"family":"Davis","given":"Robert","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":157870,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Christenson, Scott C. schris@usgs.gov","contributorId":980,"corporation":false,"usgs":true,"family":"Christenson","given":"Scott","email":"schris@usgs.gov","middleInitial":"C.","affiliations":[{"id":516,"text":"Oklahoma Water Science Center","active":true,"usgs":true}],"preferred":true,"id":157869,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":7311,"text":"ofr8175 - 1981 - Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:06:03","indexId":"ofr8175","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-75","title":"Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8175","usgsCitation":"Frickel, D.G., Shown, L., Hadley, R.F., and Miller, R., 1981, Methodology for hydrologic evaluation of a potential surface mine, Red Rim Site, Carbon and Sweetwater counties, Wyoming: U.S. Geological Survey Open-File Report 81-75, vi, 65 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr8175.","productDescription":"vi, 65 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":140618,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0075/report-thumb.jpg"},{"id":34701,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0075/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629fbe","contributors":{"authors":[{"text":"Frickel, Donald G.","contributorId":23524,"corporation":false,"usgs":true,"family":"Frickel","given":"Donald","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":155170,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Shown, L. M.","contributorId":43757,"corporation":false,"usgs":true,"family":"Shown","given":"L. M.","affiliations":[],"preferred":false,"id":155172,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hadley, R. F.","contributorId":27028,"corporation":false,"usgs":true,"family":"Hadley","given":"R.","middleInitial":"F.","affiliations":[],"preferred":false,"id":155171,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Miller, R.F.","contributorId":83882,"corporation":false,"usgs":true,"family":"Miller","given":"R.F.","email":"","affiliations":[],"preferred":false,"id":155173,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":10911,"text":"ofr8178 - 1981 - Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979","interactions":[],"lastModifiedDate":"2014-06-11T08:26:00","indexId":"ofr8178","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-78","title":"Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979","docAbstract":"This report summarizes the hydrologic setting and the water-resources investigations in the Southwest Florida Water management District performed by the U.S. Geological Survey, Water Resources Division, for fiscal year 1979. Hydrologic conditions in southwest Florida are described and illustrated by hydrographs of selected surface-water, ground-water, and lake-stage data-collection sites. In addition, summaries of water-use data and data on the regional observation monitor-well program are provided. The investigations are pay of the Federal program of appraising the nation's water resources.l The cooperative program for fiscal year 1979 included 37 investigations. Abstracts of 15 reports released during 1979 are included.","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Tallahassee, FL","doi":"10.3133/ofr8178","collaboration":"Prepared in cooperation with the Southwest Florida Management District","usgsCitation":"Rollins, H., 1981, Summary of U.S. Geological Survey investigations and hydrologic conditions in southwest Florida for 1979: U.S. Geological Survey Open-File Report 81-78, vi, 93 p., https://doi.org/10.3133/ofr8178.","productDescription":"vi, 93 p.","numberOfPages":"101","costCenters":[],"links":[{"id":288251,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0078/report.pdf"},{"id":288252,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"Florida","county":"Charlotte County;Citrus County;De Soto County;Hardee County;Hernando County;Highlands County;Hillsborough County;Lake County;Levy County;Manatee County;Marion County;Pasco County;Pinellas County;Polk County;Sarasota County;Sumter County","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -83.1657,26.3087 ], [ -83.1657,29.5913 ], [ -80.8541,29.5913 ], [ -80.8541,26.3087 ], [ -83.1657,26.3087 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b04e4b07f02db699413","contributors":{"authors":[{"text":"Rollins, H.C.","contributorId":102885,"corporation":false,"usgs":true,"family":"Rollins","given":"H.C.","email":"","affiliations":[],"preferred":false,"id":162195,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8504,"text":"ofr81539 - 1981 - Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","interactions":[],"lastModifiedDate":"2022-08-15T18:16:56.208692","indexId":"ofr81539","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","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":"81-539","title":"Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah","docAbstract":"<p>The hydrology of coal-resource areas in the upper drainages of Huntington and Cottonwood Creeks in central Utah was studied in order to better define the hydrologic system, to identify the hydrologic effects of underground coal mining, and to devise methods to detect the effects.</p><p>Discharge records from gaging stations in this mountainous area indicated that there are large differences in the annual discharge of streams per unit area of drainage. These differences are attributed to differences in precipitation, differences in evaporation and sublimation of the snowpack, and to subsurface movement of water out of some basins. Surface waters sampled during 1977-79 were of good chemical quality; dissolved-solids concentrations rarely exceeded 500 milligrams per liter.</p><p>The Star Point Sandstone and the lower coal-bearing part of the Blackhawk Formation, both of Cretaceous age, are saturated in some areas, and the aquifer yields water to underground coal mines. Most of the larger discharging springs in the study area issue from the Star Point-Blackhawk aquifer where faulted. Ground water also occurs in several water-bearing zones above the Star Point-Blackhawk aquifer. It is not known whether the water in these overlying units is part of a continuous zone of saturation or whether unsaturated zones occur between units and some water is perched.</p><p>Dissolved-solids concentrations in water from about 140 springs ranged from 50 to 750 milligrams per liter. The chemical characteristics of water from the water-bearing zones of different formations usually were very similar.</p><p>Dewatering of underground coal mines was the largest manmade discharge from the Star Point-Blackhawk aquifer in the study area during 1979. The dewatering of mines has decreased the amount of water in storage in the aquifer, but water-level data were not available to define the extent of the depletion. Other possible impacts due to mine dewatering include the diminution of spring flows and increases in ground-water recharge, both of which are more likely to occur where rocks have been fractured due to subsidence above mines. Also, the flows of streams that receive water discharged from mines probably have increased accordingly. The discharge of mine water into streams causes some degradation in surface-water quality, but the quality of ground water is probably not adversely affected by mining.</p><p>Some environmental changes associated with underground mining are difficult to detect without data collected over a long period. With respect to the ground-water system, the year-to-year similarity of spring-discharge recession curves may provide a method to detect some of these changes. Changes in the benthic-invertebrate population may help detect pollution of surface waters.</p><p>Comprehensive studies of the ground-water system are needed in conjunction with hydrologic monitoring in order to fully assess the hydrologic impacts of the underground coal mining.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81539","collaboration":"Prepared in cooperation with the Utah Department of Natural Resources and Energy, Division of Oil, Gas, and Mining","usgsCitation":"Danielson, T.W., ReMillard, M.D., and Fuller, R.H., 1981, Hydrology of the coal-resource areas in the upper drainages of Huntington and Cottonwood creeks, central Utah: U.S. Geological Survey Open-File Report 81-539, Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches, https://doi.org/10.3133/ofr81539.","productDescription":"Report: vi, 85 p.; 2 Plates: 24.71 x 37.66 inches and 24.58 x 37.93 inches","costCenters":[],"links":[{"id":405144,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405143,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0539/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":405142,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0539/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143564,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0539/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"central Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -111.39175415039062,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.13645165015621\n            ],\n            [\n              -111.13014221191406,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.35022841846271\n            ],\n            [\n              -111.39175415039062,\n              39.13645165015621\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fc78b","contributors":{"authors":[{"text":"Danielson, T. W.","contributorId":48590,"corporation":false,"usgs":true,"family":"Danielson","given":"T.","middleInitial":"W.","affiliations":[],"preferred":false,"id":157825,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"ReMillard, Michael D.","contributorId":95748,"corporation":false,"usgs":true,"family":"ReMillard","given":"Michael","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":157827,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Fuller, Richard H.","contributorId":66236,"corporation":false,"usgs":true,"family":"Fuller","given":"Richard","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":157826,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
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