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.
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.
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.
","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 p.","costCenters":[],"links":[{"id":139499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0169/report-thumb.jpg"},{"id":405415,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0169/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699d32","contributors":{"authors":[{"text":"Channel, L. K.","contributorId":35304,"corporation":false,"usgs":true,"family":"Channel","given":"L.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":153666,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7249,"text":"ofr81815 - 1981 - Hydrology of Area 7, Eastern Coal Province, Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr81815","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":"81-815","title":"Hydrology of Area 7, Eastern Coal Province, Ohio","docAbstract":"The U.S. Geological Survey established 24 study areas in Eastern Appalachian Coal Province to appraise the hydrology and water resources from Alabama to Pennsylvania. Chemical, physical, biological, and streamflow data were collected from 138 synoptic sites in Area 7, eastern Ohio. The data are evaluated and presented in this report. Area 7 lies within the drainage basins of Muskingum Rivers and Duck and Willis Creeks in eastern Ohio. Walhounding, Tuscarawas, and Little Muskingum, and Muskingum Rivers and Wills and Duck Creeks are the major streams draining the study area.\r\n\r\nIn Ohio, surface and subsurface coal mining has altered the environment. In areas where land has been reclaimed, the environmental stress expected to be temporary. Hydrologic problems related to coal mining are erosion and sedimentation which degrade water-quality. Based on available sediment data, suspended sediment concentration were highest in abandoned mine areas, followed by currently mined and reclaimed areas, and lowest in unmined areas.\r\n\r\nLow pH, high specific conductance, high concentrations of iron, sulfate and manganese, increased sediment yields, discoloration of streambeds, limited aquatic vegetation and animal life typify streams draining areas with abandoned mines. In abandoned mine areas, the specific conductance of water ranged from 800 to 2,300 micromhos; pH ranged from 2.8 to 5.8; dissolved-iron concentrations ranged from 1,000 to 85,000 micrograms per liter; dissolved-sulfate concentrations ranged from 14 to 1,200 milligrams per liter and dissolved-manganese concentration commonly exceeded 2,000 micrograms per liter. Red and yellow coloration on the streambeds were precipitates from the hydrolysis of iron, manganese, and sulfate minerals carried into the stream channel by increased sediment erosion from abandoned coal mines. Trace metal concentrations (arsenic, cadmium, chromium, cobalt, copper, lead, mercury, selenium, and zinc) were generally low. Degradation of fish habitat is illustrated by conceptual model of the aquatic biology related to water chemistry.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81815","usgsCitation":"Engelke, M.J., Roth, D., and and others, 1981, Hydrology of Area 7, Eastern Coal Province, Ohio: U.S. Geological Survey Open-File Report 81-815, v, 60 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81815.","productDescription":"v, 60 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94764,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0815/report.pdf","size":"21723","linkFileType":{"id":1,"text":"pdf"}},{"id":139916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0815/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e780","contributors":{"authors":[{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154898,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Roth, D.K.","contributorId":60275,"corporation":false,"usgs":true,"family":"Roth","given":"D.K.","email":"","affiliations":[],"preferred":false,"id":154897,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528824,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7245,"text":"ofr81343 - 1981 - Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia","interactions":[],"lastModifiedDate":"2012-02-02T00:05:49","indexId":"ofr81343","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":"81-343","title":"Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia","docAbstract":"Area 4 (one of the 24 hydrologic areas defining the Eastern Coal Province) is located at the northern end of the Eastern Coal Province in eastern Ohio, northern West Virginia, and western Pennsylvania. It is part of the upper Ohio River basin, which includes the Beaver, Mahoning, and Shenango Rivers. The area is underlain by rocks of the Pottsville, Allegheny, Conemaugh, Monongahela Groups (or Formations) and Dunkard Group. Area 4 has a temperate climate with an annual average rainfall of 38 to 42 inches, most of its area is covered by forest. The soils have a high erosion potential where the vegetation cover is removed. In response to Public Law 95-87, 132 sites were added to the existing surface-water data-collection network in area 4. At these added sites, collected data includes discharge, water quality, sediment, and biology. The data are available from computer storage through the National Water Data Exchange (NAWDEX) or the published annual Water Resources Data reports for Ohio, Pennsylvania, and West Virginia. Hydrologic problems related to mining are: (1) Erosion and increased sedimentation, and (2) degradation of water quality. Erosion and sedimentation are associated chiefly with surface mining. Sediment yields increase drastically when vegetation is removed from the highly erosive soils. Degradation of water quality can be caused by acid-mine drainage from underground and surface mining. More than half the acid-mine drainage effluent in area 4 comes from underground mines. The rest seeps from abandoned surface mines. Usually in reclaimed surface mines the overburden is replaced in such a short time after the coal is taken out that oxidation of acid-forming minerals, commonly pyrite or marcasite, is not complete or is neutralized by the buffering action of calcareous minerals in the soils. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81343","usgsCitation":"Roth, D.K., Engelke, M.J., and and others, 1981, Hydrology of area 4, Eastern Coal Province, Pennsylvania, Ohio, and West Virginia: U.S. Geological Survey Open-File Report 81-343, v, 62 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81343.","productDescription":"v, 62 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94761,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0343/report.pdf","size":"18771","linkFileType":{"id":1,"text":"pdf"}},{"id":139902,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0343/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602088","contributors":{"authors":[{"text":"Roth, Donald K.","contributorId":30977,"corporation":false,"usgs":true,"family":"Roth","given":"Donald","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154887,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Engelke, Morris J. Jr.","contributorId":100379,"corporation":false,"usgs":true,"family":"Engelke","given":"Morris","suffix":"Jr.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"and others","contributorId":127886,"corporation":true,"usgs":false,"organization":"and others","id":528823,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":7241,"text":"ofr81403 - 1981 - Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81403","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":"81-403","title":"Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81403","usgsCitation":"Zuehls, E., Ryan, G., Peart, D., and Fitzgerald, K.K., 1981, Hydrology of Area 35, Eastern region, Interior coal province, Illinois and Kentucky: U.S. Geological Survey Open-File Report 81-403, v, 82 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81403.","productDescription":"v, 82 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94759,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0403/report.pdf","size":"21275","linkFileType":{"id":1,"text":"pdf"}},{"id":139843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0403/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67e76b","contributors":{"authors":[{"text":"Zuehls, E.E.","contributorId":19942,"corporation":false,"usgs":true,"family":"Zuehls","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":154874,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, G.L.","contributorId":68727,"corporation":false,"usgs":true,"family":"Ryan","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":154877,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":154876,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154875,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7240,"text":"ofr81498 - 1981 - Hydrology of area 32, Eastern Region, Interior Coal Province, Indiana","interactions":[],"lastModifiedDate":"2016-06-03T17:18:08","indexId":"ofr81498","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":"81-498","title":"Hydrology of area 32, Eastern Region, Interior Coal Province, Indiana","docAbstract":"Hydrologic and water-quality information from the coal region in parts of 11 counties in southwestern Indiana are summarized. Pennsylvanian and Mississippian bedrock are overlain by drift and till from the Kansan, Illinoian, and Wisconsinan glaciers that covered two-thirds of the area. Most of the coal is mined from Pennsylvanian coal units. As of 1978, more than 1-billion short tons of coal had been mined from the 11 counties. More than 12-billion short tons remained in reserve. During 1978, 17.8-million short tons were mined. Coal mining disturbs less than 1% of the land in the study area. Sixty-two percent of the land use is agricultural, and 29% is forested. More coal is mined in the southern and western parts of the study area than elsewhere. Surface water in these parts had lower pH and alkalinity than water in the north and east parts. Specific conductance and concentrations of sulfate, iron, and manganese in surface water were higher in the south and west than elsewhere. (USGS)
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81498","usgsCitation":"Wangsness, D.J., Miller, R.L., Bailey, Z., and Crawford, C.G., 1981, Hydrology of area 32, Eastern Region, Interior Coal Province, Indiana: U.S. Geological Survey Open-File Report 81-498, v, 76 p., https://doi.org/10.3133/ofr81498.","productDescription":"v, 76 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":94758,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0498/report.pdf","size":"22065","linkFileType":{"id":1,"text":"pdf"}},{"id":139842,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0498/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602057","contributors":{"authors":[{"text":"Wangsness, David J.","contributorId":81475,"corporation":false,"usgs":true,"family":"Wangsness","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":154873,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Miller, R. L.","contributorId":54178,"corporation":false,"usgs":true,"family":"Miller","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":154871,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bailey, Z. C.","contributorId":54587,"corporation":false,"usgs":true,"family":"Bailey","given":"Z. C.","affiliations":[],"preferred":false,"id":154872,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crawford, Charles G. 0000-0003-1653-7841 cgcrawfo@usgs.gov","orcid":"https://orcid.org/0000-0003-1653-7841","contributorId":1064,"corporation":false,"usgs":true,"family":"Crawford","given":"Charles","email":"cgcrawfo@usgs.gov","middleInitial":"G.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":37947,"text":"Upper Midwest Water Science Center","active":true,"usgs":true}],"preferred":true,"id":154870,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7238,"text":"ofr81636 - 1981 - Hydrology of area 25, Eastern Region, Interior Coal Province, Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81636","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":"81-636","title":"Hydrology of area 25, Eastern Region, Interior Coal Province, Illinois","docAbstract":"The eastern region of the Interior Coal Province has been divided into 11 hydrologic study areas. Area 25, located in west-central Illinois, includes the Spoon River and small tributaries to the Illinois River. Pennsylvanian age rocks underlie most of the study area. Illinois, with the largest reserves of bituminous coal, is second only to Montana in total coal reserves. Loess soils cover most of the study area. Agriculture is the dominant land use. Surface water provides 97% of all the water used. Precipitation averages 34 to 35 inches. Water-quality data has been collected at over 31 sites. Analysis for specific conductance, pH, alkalinity, iron, manganese, sulfate and many trace elements and other water-quality constituents have been completed. These data are available from computer storage through the National Water Data Storage and Retrieval System (WATSTORE). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81636","usgsCitation":"Zuehls, E., Ryan, G., Peart, D., and Fitzgerald, K.K., 1981, Hydrology of area 25, Eastern Region, Interior Coal Province, Illinois: U.S. Geological Survey Open-File Report 81-636, v, 66 p. :col. ill., maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81636.","productDescription":"v, 66 p. :col. ill., maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94756,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0636/report.pdf","size":"19580","linkFileType":{"id":1,"text":"pdf"}},{"id":139838,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0636/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db602062","contributors":{"authors":[{"text":"Zuehls, E.E.","contributorId":19942,"corporation":false,"usgs":true,"family":"Zuehls","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":154864,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ryan, G.L.","contributorId":68727,"corporation":false,"usgs":true,"family":"Ryan","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":154867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Peart, D.B.","contributorId":45304,"corporation":false,"usgs":true,"family":"Peart","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":154866,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Fitzgerald, K. K.","contributorId":34501,"corporation":false,"usgs":true,"family":"Fitzgerald","given":"K.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":154865,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":7236,"text":"ofr81492 - 1981 - Hydrology of area 18, Eastern Coal Province, Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81492","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":"81-492","title":"Hydrology of area 18, Eastern Coal Province, Tennessee","docAbstract":"The Eastern Coal Province is divided into 24 hydrologic reporting areas. This report describes the hydrology of area 18 which is located in the Cumberland River basin in central Tennessee near the southern end of the Province. Hydrologic information and sources are presented as text, tables, maps, and other illustrations designed to be useful to mine owners, operators, and consulting engineers in implementing permit applications that comply with the environmental requirements of the ' Surface Mining Control and Reclamation Act of 1977. ' Area 18 encompasses parts of three physiographic regions; from east to west the Cumberland Plateau, Highland Rim, and Central Basin. The Plateau is underlain by sandstones and shales, with thin interbedded coal beds, of Pennsylvanian age. The Highland Rim and Central Basin are underlain by limestone and dolomite of Mississippian age. Field and laboratory analyses of chemical and physical water-quality parameters of streamflow samples show no widespread water quality problems. Some streams, however, in the heavily mined areas have concentrations of sulfate, iron, manganese, and sediment above natural levels, and pH values below natural levels. Mine seepage and direct mine drainage were not sampled. Ground water occurs in and moves through fractures in the sandstones and shales and solution openings in the limestones and dolomites. Depth to water is variable, ranging from about 5 to 70 feet below land-surface in the limestones and dolomites, and 15 to 40 feet in the coal-bearing rocks. The quality of ground water is generally good. Locally, in coal-bearing rocks, acidic water and high concentrations of manganese, chloride, and iron have been detected. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81492","usgsCitation":"May, V., 1981, Hydrology of area 18, Eastern Coal Province, Tennessee: U.S. Geological Survey Open-File Report 81-492, 78 p. :ill. (some col.), maps (some col.) ;29 cm., https://doi.org/10.3133/ofr81492.","productDescription":"78 p. :ill. (some col.), maps (some col.) ;29 cm.","costCenters":[],"links":[{"id":94754,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0492/report.pdf","size":"25049","linkFileType":{"id":1,"text":"pdf"}},{"id":139836,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0492/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db6045e5","contributors":{"authors":[{"text":"May, V.J.","contributorId":71539,"corporation":false,"usgs":true,"family":"May","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":154862,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7234,"text":"ofr81137 - 1981 - Hydrology of area 14, Eastern Coal Province, Kentucky","interactions":[],"lastModifiedDate":"2012-02-02T00:05:50","indexId":"ofr81137","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":"81-137","title":"Hydrology of area 14, Eastern Coal Province, Kentucky","docAbstract":"The general hydrology of Area 14, Eastern Coal Province, in Kentucky, is described. The area includes 4,423 square miles in the Kentucky, Licking, and Red River basins. Coal-bearing rocks of Pennsylvanian age underlie most of the area. Coal production in 1978 was about 38 million tons, 65% of which was from surface mining. The drainage from the mined areas contains large amounts of dissolved solids. Sulfate, manganese, and iron concentrations in most of the area streams exceed background levels, with the higher concentrations in streams draining the headwaters of the North and Middle Forks of the Kentucky River. The pH of most of the streams is near neutral acid-mine drainage being partially neutralized close to its source. Ground waters in the upper 300 feet of the aquifers are generally suitable for most purposes, although dissolved iron is generally high. Below 300 feet, the water is saline. Yields to wells range from 1 to 325 gallons per minute. A network of 66 surface quantity and quality of water stations was implemented in 1979 in response to the Surface Mining and Reclamation Act of 1977. An intensive study of the ground water resources of the area is also in progress. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr81137","usgsCitation":"Quinones, F., 1981, Hydrology of area 14, Eastern Coal Province, Kentucky: U.S. Geological Survey Open-File Report 81-137, v, 112 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr81137.","productDescription":"v, 112 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":94752,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0137/report.pdf","size":"25342","linkFileType":{"id":1,"text":"pdf"}},{"id":139830,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0137/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a14e4b07f02db602439","contributors":{"authors":[{"text":"Quinones, F.","contributorId":93037,"corporation":false,"usgs":true,"family":"Quinones","given":"F.","email":"","affiliations":[],"preferred":false,"id":154857,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":8876,"text":"ofr81482 - 1981 - Drainage areas of selected surface-water sites in Florida","interactions":[{"subject":{"id":23049,"text":"ofr80957 - 1980 - Drainage areas of selected surface-water sites in Florida","indexId":"ofr80957","publicationYear":"1980","noYear":false,"title":"Drainage areas of selected surface-water sites in Florida"},"predicate":"SUPERSEDED_BY","object":{"id":8876,"text":"ofr81482 - 1981 - Drainage areas of selected surface-water sites in Florida","indexId":"ofr81482","publicationYear":"1981","noYear":false,"title":"Drainage areas of selected surface-water sites in Florida"},"id":1}],"lastModifiedDate":"2022-08-11T14:01:32.365963","indexId":"ofr81482","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":"81-482","title":"Drainage areas of selected surface-water sites in Florida","docAbstract":"Drainage areas for about 1,600 surface-water sites on streams and lakes in Florida are contained in this report. The sites are generally either U.S. Geological Survey gaging stations or the mouths of gaged streams. Each site is identified by latitude and longitude, by the general stream type, and by the U.S. Geological Survey 7 1/2-minute topographic map on which it can be located. The gaging stations are further identified by a downstream order number, a county code, and a nearby city or town. In addition to drainage areas, the surface areas of lakes are shown for the elevation given on the topographic map. These data were retrieved from the Surface Water Index developed and maintained by the Hydrologic Surveillance Section of the Florida District Office, U.S. Geological Survey.
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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635efe","contributors":{"authors":[{"text":"Foose, Donald W.","contributorId":85144,"corporation":false,"usgs":true,"family":"Foose","given":"Donald","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":158472,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43688,"text":"ofr81494 - 1981 - Hydrologic description of Lake Jackson, Sebring, Florida","interactions":[],"lastModifiedDate":"2022-04-18T23:20:19.771099","indexId":"ofr81494","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":"81-494","title":"Hydrologic description of Lake Jackson, Sebring, Florida","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81494","usgsCitation":"Hammett, K., 1981, Hydrologic description of Lake Jackson, Sebring, Florida: U.S. Geological Survey Open-File Report 81-494, 1 Plate: 38.51 x 29.02 inches, https://doi.org/10.3133/ofr81494.","productDescription":"1 Plate: 38.51 x 29.02 inches","costCenters":[],"links":[{"id":399061,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0494/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":397145,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_12052.htm"},{"id":161801,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0494/report-thumb.jpg"}],"country":"United States","state":"Florida","city":"Sebring","otherGeospatial":"Lake Jackson","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -81.53778076171874,\n 27.358351545806766\n ],\n [\n -81.38397216796875,\n 27.358351545806766\n ],\n [\n -81.38397216796875,\n 27.577677346218785\n ],\n [\n -81.53778076171874,\n 27.577677346218785\n ],\n [\n -81.53778076171874,\n 27.358351545806766\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688d20","contributors":{"authors":[{"text":"Hammett, K.M.","contributorId":59006,"corporation":false,"usgs":true,"family":"Hammett","given":"K.M.","email":"","affiliations":[],"preferred":false,"id":228560,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":11724,"text":"ofr81491 - 1981 - Hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1979","interactions":[],"lastModifiedDate":"2022-08-10T17:31:30.042271","indexId":"ofr81491","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":"81-491","title":"Hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1979","docAbstract":"Hydrologic investigations of urban watersheds in Texas were begun by the U.S. Geological Survey in 1954. These studies are now in progress in Austin, Houston, and San Antonio. The study for the Fort Worth metropolitan area was completed at the end of the 1978 water year, and this report is the last annual report for the Dallas metropolitan area. Hydrologic data contained in this report and all previous reports of both the Dallas and Fort Worth metropolitan areas are being used to prepare an interpretive report entitled \"Techniques for estimating the magnitude and frequency of floods in the Dallas-Fort Worth, Texas, metropolitan areas,\" which will be released in 1981.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81491","collaboration":"Prepared in cooperation with the cities of Dallas, Garland and Mesquite; the Dallas County Department of Public Works; and the Texas Department of Water Resources","usgsCitation":"Wood, C., Butler, H., and Benton, J., 1981, Hydrologic data for urban studies in the Dallas, Texas, metropolitan area, 1979: U.S. Geological Survey Open-File Report 81-491, 147 p., https://doi.org/10.3133/ofr81491.","productDescription":"147 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":405082,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0491/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":143787,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0491/report-thumb.jpg"}],"country":"United States","state":"Texas","city":"Dallas","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -97.8662109375,\n 32.10118973232094\n ],\n [\n -95.80078125,\n 32.10118973232094\n ],\n [\n -95.80078125,\n 33.394759218577995\n ],\n [\n -97.8662109375,\n 33.394759218577995\n ],\n [\n -97.8662109375,\n 32.10118973232094\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ce4b07f02db607c66","contributors":{"authors":[{"text":"Wood, C.M.","contributorId":106454,"corporation":false,"usgs":true,"family":"Wood","given":"C.M.","email":"","affiliations":[],"preferred":false,"id":163625,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Butler, H.S.","contributorId":28602,"corporation":false,"usgs":true,"family":"Butler","given":"H.S.","email":"","affiliations":[],"preferred":false,"id":163624,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Benton, J.D.","contributorId":25152,"corporation":false,"usgs":true,"family":"Benton","given":"J.D.","email":"","affiliations":[],"preferred":false,"id":163623,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":43691,"text":"ofr81908 - 1981 - Hydrologic maps of Ogallala Aquifer, west-central Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:10","indexId":"ofr81908","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":"81-908","title":"Hydrologic maps of Ogallala Aquifer, west-central Kansas","language":"ENGLISH","doi":"10.3133/ofr81908","usgsCitation":"Dunlap, L.E., and Spinazola, J.M., 1981, Hydrologic maps of Ogallala Aquifer, west-central Kansas: U.S. Geological Survey Open-File Report 81-908, 4 maps ;61 x 126 cm., https://doi.org/10.3133/ofr81908.","productDescription":"4 maps ;61 x 126 cm.","costCenters":[],"links":[{"id":161804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20211,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20212,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20213,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":20214,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1981/0908/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606797","contributors":{"authors":[{"text":"Dunlap, Lloyd E.","contributorId":92261,"corporation":false,"usgs":true,"family":"Dunlap","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":228564,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Spinazola, Joseph M.","contributorId":102044,"corporation":false,"usgs":true,"family":"Spinazola","given":"Joseph","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":228565,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":11142,"text":"ofr811014 - 1981 - Potential hydrologic effects of developing coal and other geo-energy resources of Oregon; a review","interactions":[],"lastModifiedDate":"2012-02-02T00:06:19","indexId":"ofr811014","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":"81-1014","title":"Potential hydrologic effects of developing coal and other geo-energy resources of Oregon; a review","docAbstract":"Southwestern Oregon has several hundred million tons of good-quality minable coal. Because of the dip of the coal beds, the only economical method of mining would be by underground methods. In addition, minor occurrences of low-quality coal have been noted at more than 20 sites in both western and northeastern Oregon. About 2 million acres are now under lease for petroleum and gas exploration across the State. Natural gas was discovered in northwestern Oregon in 1979, and current production is about 17 million cubic feet per day from five wells. Thirteen Known Geothermal Resource Areas in several parts of the State cover 432,000 acres, and more than 420,000 acres are under lease for geothermal exploration. No hydrologic impacts have been noted from exploration and production of coal or other geoenergy resources in Oregon. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr811014","usgsCitation":"Sidle, W., 1981, Potential hydrologic effects of developing coal and other geo-energy resources of Oregon; a review: U.S. Geological Survey Open-File Report 81-1014, v, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr811014.","productDescription":"v, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":142469,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/1014/report-thumb.jpg"},{"id":38911,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/1014/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692264","contributors":{"authors":[{"text":"Sidle, W.C.","contributorId":93911,"corporation":false,"usgs":true,"family":"Sidle","given":"W.C.","email":"","affiliations":[],"preferred":false,"id":162612,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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":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":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":"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.
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.
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.
","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":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":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":"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.
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.
","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":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":"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.
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.
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.
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.
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.
","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 ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a18e4b07f02db605450","contributors":{"authors":[{"text":"Waddell, Kidd M.","contributorId":20720,"corporation":false,"usgs":true,"family":"Waddell","given":"Kidd","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":146301,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Contratto, P. 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":6396,"text":"pp1044I - 1981 - The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study","interactions":[],"lastModifiedDate":"2021-12-23T22:37:05.37152","indexId":"pp1044I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1981","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1044","chapter":"I","title":"The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study","docAbstract":"No abstract available.
","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Geohydrology of geothermal systems","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1044I","usgsCitation":"Sammel, E.A., and Craig, R.W., 1981, The geothermal hydrology of Warner Valley, Oregon: A reconnaissance study: U.S. Geological Survey Professional Paper 1044, Report: 147 p.; 1 Plate: 28.50 × 40.00 inches, https://doi.org/10.3133/pp1044I.","productDescription":"Report: 147 p.; 1 Plate: 28.50 × 40.00 inches","costCenters":[],"links":[{"id":33769,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1044i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33770,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1044i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121573,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1044i/report-thumb.jpg"},{"id":393395,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4698.htm"}],"country":"United States","state":"Oregon","otherGeospatial":"Warner Valley","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.125,\n 42.5167\n ],\n [\n -119.6250,\n 42.5167\n ],\n [\n -119.6250,\n 42\n ],\n [\n -120.125,\n 42\n ],\n [\n -120.125,\n 42.5167\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ae4b07f02db65d59d","contributors":{"authors":[{"text":"Sammel, Edward A.","contributorId":78320,"corporation":false,"usgs":true,"family":"Sammel","given":"Edward","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":152647,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Craig, Robert W.","contributorId":37729,"corporation":false,"usgs":true,"family":"Craig","given":"Robert","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":152646,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"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":27826,"text":"wri8153 - 1981 - Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana","interactions":[],"lastModifiedDate":"2020-11-04T18:05:32.65912","indexId":"wri8153","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":"81-53","title":"Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana","docAbstract":"A 3-year study in northwest Elkhart County, Indiana, was done to (1) de-fine the general flow and quality of water in the outwash aquifer system, (2) determine if a well field proposed for a site at the Elkhart Municipal Airport would draw leachate from the Himco landfill, and (3) define the areal extent of the ground water affected by the landfill and an east-side industrial-park area.
The outwash aquifers are mainly composed of sand and gravel and are separated by a silt and clay bed. The saturated thickness of these deposits averages 175 feet and ranges from 85 to 500 feet. Where present, the silt and clay bed confines the underlying aquifer. The confining bed is absent in the area underlying the landfill and part of the airport. Average hydraulic conductivities of the sand, and the sand and gravel, are 80 and 400 feet per day, respectively. Regional ground-water flow is toward the St. Joseph River.
A quasi-three-dimensional ground-water flow model, calibrated to match measured water levels and river seepages, was used to simulate proposed pumpings in the airport area. Drawdowns for simulated pumpings of 7.5-, 10-, and 20-million gallons per day were small percentages of the saturated thick-nesses of the unconfined aquifer underlying the airport area. Model-simulated streamflow reductions in Christiana Creek for these pumpings were 9, 12, and 23 percent of base flow, respectively. The model-simulated, steady-state water-level maps for the 7.5- and 10-million-gallons-per-day pumping experiments indicated that these pumpings would not draw water from the land-fill area to the pumping center at the airport. The simulated map for the 20-million-gallons-per-day pumping indicated that only a small part of the flow into the pumping center could come from the landfill area.
The general quality of ground water in the study area, defined by analyses of 68 water samples from 35 observation wells, included slightly basic pH (7-8), average hardness greater than 200 milligrams per liter as calcium carbonate, average alkalinity greater than 150 milligrams per liter as calcium carbonate, and, in more than 90 percent of the analyses, a calcium bicarbonate water type.
Eight volatile organic compounds were detected in water from 8 of 19 wells sampled in the industrial-park area. The health-effects advisory limit for chronic exposure to trichloroethylene was exceeded in samples from six of these wells. Areally, the results did not define a plume or a source of the volatile organic compounds.
Concentrations of dissolved solids, bicarbonate, bromide, chloride, sulfate, ammonia, calcium, magnesium, manganese, potassium, sodium, and dis-solved organic carbon in the leachate were at least five times their back-ground concentrations. Concentrations of bromide and dissolved solids were the best indicators of leachate. Bromide concentrations plotted areally indicated that the landfill was the source of the leachate, the leachate plume extended between 3,100 and 5,600 feet downgradient from the landfill, and the plume had not spread laterally much farther than the original width of the landfill. Bromide and dissolved-solids concentrations plotted in cross section indicated that the leachate plume was sinking as it spread downgradient in the shallow unconfined aquifer and the leachate was present in deep wells under and immediately downgradient from the landfill. All chemical constituents were attenuated within approximately 1 mile downgradient from the landfill.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8153","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources and the Elkhart Water Works","usgsCitation":"Imbrigiotta, T., and Martin, A., 1981, Hydrologic and chemical evaluation of the ground-water resources of northwest Elkhart County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-53, ix, 140 p., https://doi.org/10.3133/wri8153.","productDescription":"ix, 140 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380154,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0053/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158684,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0053/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Elkhart County","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7874,41.7615],[-85.7591,41.7613],[-85.6606,41.7608],[-85.6589,41.699],[-85.6575,41.6122],[-85.6554,41.5251],[-85.6542,41.4733],[-85.6552,41.4384],[-85.7704,41.4377],[-85.8874,41.4379],[-86.0008,41.4375],[-86.059,41.4367],[-86.0594,41.4644],[-86.0593,41.474],[-86.0593,41.479],[-86.0592,41.4935],[-86.0598,41.4999],[-86.0624,41.7619],[-85.932,41.7623],[-85.7874,41.7615]]]},\"properties\":{\"name\":\"Elkhart\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db6118d0","contributors":{"authors":[{"text":"Imbrigiotta, Thomas E. 0000-0003-1716-4768 timbrig@usgs.gov","orcid":"https://orcid.org/0000-0003-1716-4768","contributorId":2466,"corporation":false,"usgs":true,"family":"Imbrigiotta","given":"Thomas E.","email":"timbrig@usgs.gov","affiliations":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"preferred":false,"id":198744,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, Angel Jr.","contributorId":42571,"corporation":false,"usgs":true,"family":"Martin","given":"Angel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":198745,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28255,"text":"wri8135 - 1981 - Ground-water resources of the White River basin, Madison County, Indiana","interactions":[],"lastModifiedDate":"2020-11-04T18:03:15.372006","indexId":"wri8135","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":"81-35","title":"Ground-water resources of the White River basin, Madison County, Indiana","docAbstract":"The ground-water resources of the White River basin in and near Madison County, Indiana, were investigated by mapping the aquifers, estimating their hydraulic properties, determining the distribution of potentiometric head in the aquifers, and estimating some of the components of the ground-water budget from data collected in the field. This information was used to construct and calibrate a five-layer, digital ground-water flow model. The model, constructed and calibrated to ground-water-level and seepage data collected during the study, simulates conditions for the autumn of 1976. The model was used to provide estimates of ground-water potential in terms of yield, drawdown, and depletion in streamflow.
Glacial drift covers nearly the entire study area and ranges in thickness from 0 to approximately 300 feet. Beneath the drift lie Ordovician to Devonian limestone, dolomite, and shale. A bedrock valley trends west-northwest through the center of the study area. Relief of the bedrock surface is approximately 325 feet.
Four confined sand and gravel aquifers interbedded in the glacial drift, a bedrock aquifer, and an unconfined outwash aquifer are the three most important aquifer systems in the study area. The nearly horizontal, areally discontinuous, confined sand and gravel aquifers have an average thickness of about 15 feet and an average hydraulic conductivity estimated to be 433 feet per day. The bedrock aquifer underlying the entire study area has a thick-ness estimated to be 150 feet and an average transmissivity estimated in previous studies in the basin to be 1,340 square feet per day. The unconfined outwash aquifer, although thin and narrow, is an important aquifer because of its proximity to sources of induced recharge.
Water-level fluctuations in observation wells in the basin indicate that the ground-water system is in dynamic equilibrium. Ground-water seepage to streams at 90-percent flow duration on October 1, 1976, was estimated to be between 15.9 and 74.4 cubic feet per second. Ground-water pumpage for 1976 was estimated to be 19.7 million gallons per day (30.5 cubic feet per second). The water budget, as simulated in the model, indicates that the rate of inflow to the ground-water system in the modeled area is 92.4 cubic feet per second. Of this, 78 percent is from effective areal recharge of precipitation, and 22 percent is from ground-water flow across the boundaries into the study area. Thirty-three percent of the ground-water outflow is pumpage, 59 percent is seepage to streams, and the remaining 8 percent is ground-water flow across the boundaries out of the study area.
Model simulations of eight pumping plans provide a general assessment of the water-yielding potential of the three major aquifer systems and indicate that as much as 2.5 million gallons per day can be obtained from well fields about half a square mile in area. Model results also indicate that, for as much as 2.5-million gallons per day pumping, flow in the large streams will not be significantly affected, whereas flow in the small streams may be significantly affected. In addition, simulations indicate that adding more wells to the well field northwest of Anderson, Ind., would probably be no more advantageous than increasing the pumpage in the existing wells. How-ever, well interference, well hydraulics, and pumping-level constraints were not considered in the investigation of alternative methods of expanding the well field. In developing the ground-water system in the area, use of many small, scattered well fields that produce less than about 3 million gallons per day may be more favorable hydrologically than a few, heavily pumped well fields.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8135","collaboration":"Prepared in cooperation with the Indiana Department of Natural Resources","usgsCitation":"Lapham, W.W., 1981, Ground-water resources of the White River basin, Madison County, Indiana: U.S. Geological Survey Water-Resources Investigations Report 81-35, vii, 112 p., https://doi.org/10.3133/wri8135.","productDescription":"vii, 112 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":380151,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0035/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159567,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0035/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Madison","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.5784,40.3794],[-85.5763,40.0769],[-85.5774,39.9459],[-85.8624,39.9436],[-85.863,40.139],[-85.8617,40.2201],[-85.8621,40.3784],[-85.5784,40.3794]]]},\"properties\":{\"name\":\"Madison\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db64931a","contributors":{"authors":[{"text":"Lapham, Wayne W.","contributorId":74734,"corporation":false,"usgs":true,"family":"Lapham","given":"Wayne","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":199477,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":7077,"text":"ofr81239 - 1981 - Data file: the 1976 Atlantic Margin Coring (AMCOR) Project of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2014-08-27T10:43:00","indexId":"ofr81239","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":"81-239","title":"Data file: the 1976 Atlantic Margin Coring (AMCOR) Project of the U.S. Geological Survey","docAbstract":"In 1976, the U.S. Geological Survey conducted the Atlantic Margin Coring Project (AMCOR) to obtain information on stratigraphy, hydrology and water chemistry, mineral resources other than petroleum hydrocarbons, and geotechnical engineering properties at sites widely distributed along the Continental Shelf and Slope of the Eastern United States (Hathaway and others, 1976, 1979). This program's primary purpose was to investigate a broad variety of sediment properties, many of which had not been previously studied in this region. Previous studies of sediments recovered by core drilling in this region were usually limited to one or two aspects of the sediment properties (Hathaway and others, 1979, table 2).
\nThe AMCOR program was limited by two factors: water depth and penetration depth. Because the ship selected for the program, the Glomar Conception, lacked dynamic positioning capability, its anchoring capacity determined the maximum water depth in which drilling could take place. Although it was equipped to anchor in water 450 m deep and did so successfully at one site, we attmepted no drilling in water depths greater than 300 m. Strong Gulf Stream currents at the one attempted deep (443 m) site frustrated attempts to \"spud in\" to begin the hole.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr81239","usgsCitation":"Poppe, L., 1981, Data file: the 1976 Atlantic Margin Coring (AMCOR) Project of the U.S. Geological Survey: U.S. Geological Survey Open-File Report 81-239, 96 p., https://doi.org/10.3133/ofr81239.","productDescription":"96 p.","numberOfPages":"97","costCenters":[{"id":186,"text":"Coastal and Marine Geology Program","active":true,"usgs":true}],"links":[{"id":140178,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1981/0239/report-thumb.jpg"},{"id":34403,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1981/0239/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -82.02,24.97 ], [ -82.02,43.0 ], [ -65.13,43.0 ], [ -65.13,24.97 ], [ -82.02,24.97 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c958","contributors":{"editors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":503962,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Poppe, Lawrence J. lpoppe@usgs.gov","contributorId":2149,"corporation":false,"usgs":true,"family":"Poppe","given":"Lawrence J.","email":"lpoppe@usgs.gov","affiliations":[{"id":678,"text":"Woods Hole Coastal and Marine Science Center","active":true,"usgs":true}],"preferred":false,"id":154195,"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}]}} ]}