No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87128","usgsCitation":"Jacobson, R., 1987, Pedological studies at Grays Landing terrace, Fayette County, Pennsylvania: U.S. Geological Survey Open-File Report 87-128, 44 p., https://doi.org/10.3133/ofr87128.","productDescription":"44 p.","costCenters":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"links":[{"id":406487,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_18921.htm","linkFileType":{"id":5,"text":"html"}},{"id":42968,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0128/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":144506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0128/report-thumb.jpg"}],"country":"United States","state":"Pennsylvania","county":"Fayette County","otherGeospatial":"Grays Landing terrace","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -79.958,\n 39.792\n ],\n [\n -79.875,\n 39.792\n ],\n [\n -79.875,\n 39.875\n ],\n [\n -79.958,\n 39.875\n ],\n [\n -79.958,\n 39.792\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688957","contributors":{"authors":[{"text":"Jacobson, R. B. 0000-0002-8368-2064","orcid":"https://orcid.org/0000-0002-8368-2064","contributorId":92614,"corporation":false,"usgs":true,"family":"Jacobson","given":"R. B.","affiliations":[{"id":192,"text":"Columbia Environmental Research Center","active":true,"usgs":true}],"preferred":true,"id":169228,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":14250,"text":"ofr87226 - 1987 - Review of the Water Resources Information System of Argentina","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr87226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-226","title":"Review of the Water Resources Information System of Argentina","docAbstract":"A representative of the U.S. Geological Survey traveled to Buenos Aires, Argentina, in November 1986, to discuss water information systems and data bank implementation in the Argentine Government Center for Water Resources Information. Software has been written by Center personnel for a minicomputer to be used to manage inventory (index) data and water quality data. Additional hardware and software have been ordered to upgrade the existing computer. Four microcomputers, statistical and data base management software, and network hardware and software for linking the computers have also been ordered. The Center plans to develop a nationwide distributed data base for Argentina that will include the major regional offices as nodes. Needs for continued development of the water resources information system for Argentina were reviewed. Identified needs include: (1) conducting a requirements analysis to define the content of the data base and insure that all user requirements are met, (2) preparing a plan for the development, implementation, and operation of the data base, and (3) developing a conceptual design to inform all development personnel and users of the basic functionality planned for the system. A quality assurance and configuration management program to provide oversight to the development process was also discussed. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87226","usgsCitation":"Hutchison, N., 1987, Review of the Water Resources Information System of Argentina: U.S. Geological Survey Open-File Report 87-226, 24 p. v. in various pagings :ill. ;28 cm., https://doi.org/10.3133/ofr87226.","productDescription":"24 p. v. in various pagings :ill. ;28 cm.","costCenters":[],"links":[{"id":144683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0226/report-thumb.jpg"},{"id":42936,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0226/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d5e4b07f02db5ddbe0","contributors":{"authors":[{"text":"Hutchison, N.E.","contributorId":20749,"corporation":false,"usgs":true,"family":"Hutchison","given":"N.E.","email":"","affiliations":[],"preferred":false,"id":169151,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":12330,"text":"ofr87105 - 1987 - Surface water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; project description","interactions":[],"lastModifiedDate":"2012-02-02T00:06:27","indexId":"ofr87105","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-105","title":"Surface water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; project description","docAbstract":"In 1986 the U.S. Geological Survey began a National Water-Quality Assessment Program to: (1) provide nationally consistent descriptions of the current status of water quality for a large, diverse, and geographically distributed part of the Nation 's surface water resources; (2) where possible, define trends in water quality; and (3) identify and describe the relation between water quality and natural and land use factors. This report describes the pilot study of the lower Kansas River basin, which is one of four surface water pilot studies that will be used to test, and modify as necessary, assessment concepts and approaches in preparation for future full implementation of the national program. Water quality issues in the lower Kansas River basin are dominated by possible nonpoint sources of contamination from agricultural land, with issues including: (1) large sediment discharge in the streams and sediment deposition in the reservoirs caused by intensive cultivation of row crops and subsequent erosion; (2) occurrence of pesticides in streams and reservoirs that could impair the suitability of water for aquatic life and has the potential for impairing the water 's suitability for public supply; (3) bacterial contamination caused by runoff from pastureland and feedlot operations and municipal wastewater discharges; and (4) nutrient enrichment of reservoirs. Data from fixed stations will be used to determine frequency distributions of constituent concentrations and mass balances of constituents between stations. Subbasin or river reach studies will provide a better understanding of the origin, movement, and fate of potential contaminants. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87105","usgsCitation":"Stamer, J., Jordan, P.R., Engberg, R., and Dugan, J.T., 1987, Surface water-quality assessment of the lower Kansas River basin, Kansas and Nebraska; project description: U.S. Geological Survey Open-File Report 87-105, iv, 36 p. :maps ;28 cm., https://doi.org/10.3133/ofr87105.","productDescription":"iv, 36 p. :maps ;28 cm.","costCenters":[],"links":[{"id":144048,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0105/report-thumb.jpg"},{"id":40560,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0105/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db691473","contributors":{"authors":[{"text":"Stamer, J. K.","contributorId":47753,"corporation":false,"usgs":true,"family":"Stamer","given":"J. K.","affiliations":[],"preferred":false,"id":165912,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Jordan, P. R.","contributorId":7282,"corporation":false,"usgs":true,"family":"Jordan","given":"P.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":165911,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Engberg, R. A.","contributorId":104876,"corporation":false,"usgs":true,"family":"Engberg","given":"R. A.","affiliations":[],"preferred":false,"id":165914,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Dugan, J. T.","contributorId":67890,"corporation":false,"usgs":true,"family":"Dugan","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":165913,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":12120,"text":"ofr85153 - 1987 - Hydrology of area 59, northern Great Plains and Rocky Mountain coal provinces, Colorado and Wyoming","interactions":[],"lastModifiedDate":"2017-09-20T16:55:01","indexId":"ofr85153","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"85-153","title":"Hydrology of area 59, northern Great Plains and Rocky Mountain coal provinces, Colorado and Wyoming","docAbstract":"Hydrologic information and analysis aid in decisions to lease federally owned coal and to prepare necessary Environmental Assessments and Impact Study reports. This need has become even more critical with the enactment of Public Law 95-87, the \"Surface Mining Control and Reclamation Act of 1977.\" This act requires an appropriate regulatory agency to issue permits, based on the review of permit-application data to assess hydrologic impacts. This report, which partially fulfills this requirement, is one in a series of nationwide coal province reports that present information thematically, through the use of a brief text and accompanying maps, graphs, charts, or other illustrations for single hydrologic topics. The report broadly characterizes the hydrology of Area 59 in north-central Colorado and southeastern Wyoming.
The report area, located within the South Platte River basin, covers a 16,000-square-mile area of diverse geology, topography, and climate. This diversity results in contrasting hydrologic characteristics.
The South Platte River, the major stream in the area, and most of its tributaries originate in granitic mountains and flow into and through the sedimentary rocks of the Great Plains. Altitudes range from less than 5,000 feet to more than 14,000 feet above sea level. Precipitation in the mountains may exceed 40 inches annually, much of it during the winter, and produces deep snowpacks. Snowmelt during the spring and summer produces most streamflow. Transmountain diversion of water from the streams on the western slope of the mountains also adds to the streamflow. Precipitation in the plains is as little as 10 inches annually. Streams that originate in the plains are ephemeral.
Streamflow quality is best in the mountains, where dissolved-solids concentrations are generally small. Concentrations increase in the plains as streams flow through sedimentary basins, and as urbanization and irrigation increase. The quality of some mountain streams is affected by drainage from previous metalmining areas, as indicated by greater trace-element concentrations and smaller pH values. However, the large trace-element concentrations decrease rapidly downstream from the metal-mining areas. Because the climate is semiarid in most of the area, the soils are not adequately leached; therefore, flows in ephemeral streams usually have larger concentrations of dissolved solids than flows in perennial streams.
Ground water is available throughout the area; yields range from less than 0.1 gallons per minute in the fractured granite aquifer in the mountains to more than 2,000 gallons per minute in the alluvial aquifer of the South Platte River valley. Major bedrock aquifers in order of decreasing age are the Laramie-Fox Hills, Arapahoe, Denver, and Dawson; these aquifers are used for municipal, domestic, and livestock supplies. Alluvial aquifers supply the high-yield irrigation wells.
The best quality ground water is found at the center of the major bedrock aquifers, where dissolved-solids concentrations are less than 200 milligrams per liter. The poorest-quality water is usually found near the edges of these aquifers. Water in the coal-bearing Laramie and Denver Formations is locally affected by coal deposits, causing dissolved-solids concentrations to be relatively large.
Only one coal mine is now operating in Area 59, the Coors Energy Company surface coal mine, which produced 100,000 short tons of subbituminous coal from the Upper Cretaceous Laramie Formation in 1982. Past coal-mining operations removed more than 130 million tons of coal and lignite from Area 59,99 percent of which came from underground mines. The largest coal production was in Weld and Boulder Counties, Colorado.
Hydrologic problems related to surface mining are erosion, sedimentation, decline in water levels, disruption of aquifers, and degradation of water quality. Because the semiarid mine areas have very little runoff, and the major streams have large buffer and dilution capacities, the effects of mining on surface water is minimal. However, effects on ground water may be much more severe and long-lasting.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr85153","usgsCitation":"Gaggiani, N.G., Britton, L.J., Minges, D.R., Kilpatrick, F.A., Parker, R.S., and Kircher, J.E., 1987, Hydrology of area 59, northern Great Plains and Rocky Mountain coal provinces, Colorado and Wyoming: U.S. Geological Survey Open-File Report 85-153, vi, 124 p., https://doi.org/10.3133/ofr85153.","productDescription":"vi, 124 p.","costCenters":[{"id":5050,"text":"WY-MT Water Science Center","active":true,"usgs":true}],"links":[{"id":95064,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0153/report.pdf","text":"Report","size":"45.67 MB","linkFileType":{"id":1,"text":"pdf"},"description":"Report"},{"id":146286,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0153/report-thumb.jpg"}],"country":"United States","state":"Colorado, Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.3,\n 38.4\n ],\n [\n -106.3,\n 41.6\n ],\n [\n -104.07,\n 41.6\n ],\n [\n -104.07,\n 38.4\n ],\n [\n -106.3,\n 38.4\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fbe","contributors":{"authors":[{"text":"Gaggiani, Neville G. gaggiani@usgs.gov","contributorId":3280,"corporation":false,"usgs":true,"family":"Gaggiani","given":"Neville","email":"gaggiani@usgs.gov","middleInitial":"G.","affiliations":[],"preferred":true,"id":165146,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Britton, Linda J.","contributorId":72780,"corporation":false,"usgs":true,"family":"Britton","given":"Linda","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":165149,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Minges, Donald R.","contributorId":99564,"corporation":false,"usgs":true,"family":"Minges","given":"Donald","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":165150,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kilpatrick, F. A.","contributorId":22319,"corporation":false,"usgs":true,"family":"Kilpatrick","given":"F.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165147,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Parker, Randolph S.","contributorId":58638,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":165148,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Kircher, James E. jkircher@usgs.gov","contributorId":248,"corporation":false,"usgs":true,"family":"Kircher","given":"James","email":"jkircher@usgs.gov","middleInitial":"E.","affiliations":[],"preferred":true,"id":165145,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":12010,"text":"ofr87212 - 1987 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","interactions":[{"subject":{"id":12010,"text":"ofr87212 - 1987 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","indexId":"ofr87212","publicationYear":"1987","noYear":false,"title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds"},"predicate":"SUPERSEDED_BY","object":{"id":3162,"text":"wsp2368A - 1990 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","indexId":"wsp2368A","publicationYear":"1990","noYear":false,"chapter":"A","title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds"},"id":1}],"supersededBy":{"id":3162,"text":"wsp2368A - 1990 - Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","indexId":"wsp2368A","publicationYear":"1990","noYear":false,"title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds"},"lastModifiedDate":"2020-10-08T18:48:16.718535","indexId":"ofr87212","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-212","title":"Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds","docAbstract":"Information on the geology, geomorphology, soils, climate, hydrology, water use, land use, population, and coal mining history of Clay, Owen, Sullivan, and Vigo Counties in Indiana is summarized. Site-specific information is given on the morphology , geology, soils, land use, coal mining history, and hydrologic instrumentation of the six watersheds which are each less than 3 sq mi in area. The Wabash, White, and Eel Rivers are the major drainages in west-central Indiana. Average annual precipitation is about 39.5 in/yr and average annual runoff is about 13 in/yr. The most productive aquifers are confined or unconfined outwash aquifers located along the major rivers. Bedrock aquifers are regionally insignificant but are the sole source of groundwater for areas that lack outwash, alluvium, or sand and gravel lenses in till. Indiana has more than 17 billion short tons of recoverable coal reserves; about 11% can be mined by surface methods. Almost half of Indiana's surface reserves are in Clay, Owen, Sullivan, and Vigo Counties. More than 50,000 acres in west-central Indiana have been disturbed by surface coal mining from 1941 through 1980. Big Slough and Hooker Creek are streams that drain unmined, agricultural watersheds. Row-crop corn and soybeans are the principal crops. Soils are moderately well drained silt loams, and the watersheds well developed dendritic drainage systems. Unnamed tributaries drain mined and reclaimed watersheds. Ridges of mine spoil have been graded to a gently rolling topography. Soils are well drained and consist of 6 to 12 inches of silt-loam topsoil that was stockpiled and then replaced over shale and sandstone fragments of the graded mine spoil. Grasses and legumes form the vegetative cover in each watershed. Pond Creek and an unnamed tributary to Big Branch are streams that drain mined and unreclaimed watersheds. Soils are very well drained shaly silty loams that have formed on steeply sloping banks. Both watersheds contain numerous impoundments of water and have enclosed areas that do not contribute surface runoff to streamflow. The ridges of mine spoil are covered with pine trees, but much of the soil surface is devoid of vegetation. (Lantz-PTT)
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87212","usgsCitation":"Martin, J., Crawford, C.G., Duwelius, R., and Renn, D., 1987, Description of the physical environment and coal-mining history of west-central Indiana, with emphasis on six small watersheds: U.S. Geological Survey Open-File Report 87-212, vi, 62 p., https://doi.org/10.3133/ofr87212.","productDescription":"vi, 62 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":144639,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0212/report-thumb.jpg"},{"id":379248,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0212/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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All ongoing water-resources projects in North Dakota in fiscal year 1986 are listed. Information on each project includes objectives, approach, progress in 1985, plans for 1986, completed and planned report products, and the name of the project chief.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87530","usgsCitation":"1987, Water-resources activities of the U.S. Geological Survey in North Dakota, fiscal year 1986: U.S. Geological Survey Open-File Report 87-530, viii, 100 p., https://doi.org/10.3133/ofr87530.","productDescription":"viii, 100 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":145857,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0530/report-thumb.jpg"},{"id":40606,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0530/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db543e0e","contributors":{"compilers":[{"text":"Martin, Cathy R.","contributorId":87951,"corporation":false,"usgs":true,"family":"Martin","given":"Cathy R.","affiliations":[],"preferred":false,"id":730813,"contributorType":{"id":3,"text":"Compilers"},"rank":1}]}} ,{"id":16270,"text":"ofr87152 - 1987 - Preliminary geologic maps, cross sections, and explanation pamphlet for the Ophir and Mercur 7 1/2-minute quadrangles, Utah","interactions":[],"lastModifiedDate":"2022-12-02T19:49:37.473744","indexId":"ofr87152","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-152","title":"Preliminary geologic maps, cross sections, and explanation pamphlet for the Ophir and Mercur 7 1/2-minute quadrangles, Utah","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87152","usgsCitation":"Tooker, E.W., 1987, Preliminary geologic maps, cross sections, and explanation pamphlet for the Ophir and Mercur 7 1/2-minute quadrangles, Utah: U.S. Geological Survey Open-File Report 87-152, Report: 18 p.; 3 Plates: 16.85 × 31.65 inches or smaller, https://doi.org/10.3133/ofr87152.","productDescription":"Report: 18 p.; 3 Plates: 16.85 × 31.65 inches or smaller","costCenters":[],"links":[{"id":45188,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0152/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45187,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0152/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":108724,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17147.htm","linkFileType":{"id":5,"text":"html"},"description":"17147"},{"id":45186,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0152/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45185,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0152/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":150385,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0152/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Ophir and Mercur 71/2-minute quadrangles","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -112.375,\n 40.375\n ],\n [\n -112.375,\n 40.25\n ],\n [\n -112.125,\n 40.25\n ],\n [\n -112.125,\n 40.375\n ],\n [\n -112.375,\n 40.375\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db673e6d","contributors":{"authors":[{"text":"Tooker, E. W.","contributorId":102071,"corporation":false,"usgs":true,"family":"Tooker","given":"E.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":172527,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":40983,"text":"ofr86482 - 1987 - Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona","interactions":[{"subject":{"id":40983,"text":"ofr86482 - 1987 - Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona","indexId":"ofr86482","publicationYear":"1987","noYear":false,"title":"Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona"},"predicate":"SUPERSEDED_BY","object":{"id":68596,"text":"ha713 - 1988 - Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona","indexId":"ha713","publicationYear":"1988","noYear":false,"title":"Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona"},"id":1}],"supersededBy":{"id":68596,"text":"ha713 - 1988 - Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona","indexId":"ha713","publicationYear":"1988","noYear":false,"title":"Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona"},"lastModifiedDate":"2012-02-02T00:10:33","indexId":"ofr86482","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-482","title":"Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona","docAbstract":"In 1979 the U.S. Geological Survey, in cooperation with the city of Tucson, began an investigation of aquifer compaction and its effects in the Tucson basin, including the potential hazards of aquifer compaction and subsequent damage to engineered structures, roads, water supply systems, gaslines, and sewage systems. Groundwater is the main source of water for irrigation, public supply, and industry. Pumping has exceeded recharge for several decades, and declines in groundwater levels have occurred in parts of the basin. In places, water level declines have resulted in small amounts of aquifer compaction and land subsidence. Further water level declines in parts of the Tucson basin may result in large amounts of aquifer compaction and land subsidence. Differential land subsidence may, in places, be accompanied by the formation of earth fissures. Aquifer compaction, land subsidence, and earth fissures can damage or affect the functional capability of manmade features. Specifically, aquifer compaction may damage wells, fissures may damage engineered structures, and differential land subsidence may affect structures such as sewers and water-supply systems that are dependent on gravity for their operation. (USGS)","language":"ENGLISH","doi":"10.3133/ofr86482","usgsCitation":"Anderson, S.R., 1987, Potential for aquifer compaction, land subsidence, and earth fissures in the Tucson basin, Pima County, Arizona: U.S. Geological Survey Open-File Report 86-482, 5 maps on 3 sheets ;38 x 29 cm., sheets 102 x 132 cm. and smaller., https://doi.org/10.3133/ofr86482.","productDescription":"5 maps on 3 sheets ;38 x 29 cm., sheets 102 x 132 cm. and smaller.","costCenters":[],"links":[{"id":172371,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a86e4","contributors":{"authors":[{"text":"Anderson, S. R.","contributorId":93518,"corporation":false,"usgs":true,"family":"Anderson","given":"S.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224283,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":61251,"text":"mf1957 - 1987 - Geologic map of the northwest part of the San Francisco Volcanic Field, north-central Arizona","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"mf1957","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1957","title":"Geologic map of the northwest part of the San Francisco Volcanic Field, north-central Arizona","language":"ENGLISH","doi":"10.3133/mf1957","usgsCitation":"Wolfe, E., Newhall, C.G., and Ulrich, G., 1987, Geologic map of the northwest part of the San Francisco Volcanic Field, north-central Arizona: U.S. Geological Survey Miscellaneous Field Studies Map 1957, 2 maps ;79 x 94 cm., on sheets 139 x 99 cm. and 124 x 101 cm. folded in envelope 30 x 24 cm., https://doi.org/10.3133/mf1957.","productDescription":"2 maps ;79 x 94 cm., on sheets 139 x 99 cm. and 124 x 101 cm. folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":105135,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_5527.htm","linkFileType":{"id":5,"text":"html"},"description":"5527"},{"id":186943,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -112.25,35.5 ], [ -112.25,35.833333333333336 ], [ -111.75,35.833333333333336 ], [ -111.75,35.5 ], [ -112.25,35.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688995","contributors":{"authors":[{"text":"Wolfe, E.W.","contributorId":57470,"corporation":false,"usgs":true,"family":"Wolfe","given":"E.W.","email":"","affiliations":[],"preferred":false,"id":265258,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Newhall, C. G.","contributorId":93056,"corporation":false,"usgs":true,"family":"Newhall","given":"C.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":265260,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ulrich, G. E.","contributorId":88737,"corporation":false,"usgs":true,"family":"Ulrich","given":"G. 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Geological Survey. These 'Hydrologic Unit Maps' are four-color maps that present information on drainage, culture, hydrography, and hydrologic boundaries and codes of (1) the 21 major water-resources regions and the 222 subregions designated by the U.S . Water Resources Council, (2) the 352 accounting units of the U.S. Geological Survey's National Water Data Network, and (3) the 2,149 cataloging units of the U.S . Geological Survey's 'Catalog of information on Water Data:' The maps are plotted on the Geological Survey State base-map series at a scale of 1 :500,000 and, except for Alaska, depict hydrologic unit boundaries for all drainage basins greater than 700 square miles (1,813 square kilometers). A complete list of all the hydrologic units, along with their drainage areas, their names, and the names of the States or outlying areas in which they reside, is contained in the report.\r\n\r\nThese maps and associated codes provide a standardized base for use by water-resources organizations in locating, storing, retrieving, and exchanging hydrologic data, in indexing and inventorying hydrologic data and information, in cataloging water-data acquisition activities, and in a variety of other applications. Because the maps have undergone extensive review by all principal Federal, regional, and State water-resource agencies, they are widely accepted for use in planning and describing water-use and related land-use activities, and in geographically organizing hydrologic data . Examples of these uses are given in the report . The hydrologic unit codes shown on the maps have been approved as a Federal Information Processing Standard for use by the Federal establishment.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2294","usgsCitation":"Seaber, P.R., Kapinos, F., and Knapp, G.L., 1987, Hydrologic unit maps: U.S. Geological Survey Water Supply Paper 2294, iii, 63 p. :ill. (some col.), maps (some col.) ;28 cm.; 1 plate in pocket, https://doi.org/10.3133/wsp2294.","productDescription":"iii, 63 p. :ill. (some col.), maps (some col.) ;28 cm.; 1 plate in pocket","costCenters":[],"links":[{"id":138259,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":35,"rank":2,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.usgs.gov/wsp/wsp2294/index.html","linkFileType":{"id":5,"text":"html"}},{"id":258460,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wsp/2294/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4814e4b07f02db4dab42","contributors":{"authors":[{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":145590,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kapinos, F. Paul","contributorId":42581,"corporation":false,"usgs":true,"family":"Kapinos","given":"F. Paul","affiliations":[],"preferred":false,"id":145589,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Knapp, George L.","contributorId":93466,"corporation":false,"usgs":true,"family":"Knapp","given":"George","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":145591,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25694,"text":"wri864357 - 1987 - Overview of water resources in Owens Valley, California","interactions":[],"lastModifiedDate":"2012-02-02T00:08:18","indexId":"wri864357","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4357","title":"Overview of water resources in Owens Valley, California","docAbstract":"In 1982-84, a water resources appraisal of Owens Valley was made by using available hydrologic information. Results of the appraisal provided an overview of water resources in Owens Valley; a better understanding of the groundwater system; and a framework for additional studies. Owens Valley is in east-central California and is the major source of water supply for the city of Los Angeles, located 233 mi to the south. Since 1913, with the completion of the first aqueduct, surface water has been diverted from the Owens River to Los Angeles. In 1970, a second Aqueduct was completed. Groundwater pumping was increased to supplement the water needed for the increasing population in Los Angeles. Most of the outflow of water from Owens Valley is from exports via the aqueduct system and by evapotranspiration loss; principal sources of water are runoff, inflow from Pleasant Valley Reservoir, and precipitation. Streamflow from the Sierra Nevada is a source of tremendous quantities of water to the valley. Pumping from more than 90 pump-equipped wells averaged about 98,000 acre-ft/yr from 1971 to 1983, but it was generally < 10,000 acre-ft/yr from 1932 to 1970, except during dry years. Groundwater pumping is primarily from deep wells adjacent to the volcanic rocks near Big Pine. Wells completed in the volcanic rocks yield large quantities of groundwater. Water level fluctuations in deep wells indicate a direct correlation with groundwater pumpage. Fluctuations in shallow wells are affected not only by pumping, but also by evapotranspiration and precipitation. The cause-and-effect relation of water level fluctuations in deep and shallow wells is not well understood and is partly the subject of a 5-yr study currently being conducted by Inyo County, the city of Los Angeles, and the U.S. Geological Survey, which emphasizes: (1) vegetation, (2) plant survivability, and (3) groundwater. It is hoped that this study will better define the quantity and availability of groundwater in the valley, as well as determine the effects of groundwater withdrawals on native vegetation. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864357","usgsCitation":"Rogers, L., 1987, Overview of water resources in Owens Valley, California: U.S. Geological Survey Water-Resources Investigations Report 86-4357, iv, 38 p. :col. ill., col. maps ;28 cm., https://doi.org/10.3133/wri864357.","productDescription":"iv, 38 p. :col. ill., col. maps ;28 cm.","costCenters":[],"links":[{"id":123688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4357/report-thumb.jpg"},{"id":54459,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4357/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae4e4b07f02db68a187","contributors":{"authors":[{"text":"Rogers, L.S.","contributorId":18027,"corporation":false,"usgs":true,"family":"Rogers","given":"L.S.","email":"","affiliations":[],"preferred":false,"id":194690,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25714,"text":"wri874216 - 1987 - Potentiometric surface of the Magothy Aquifer in southern Maryland during the Fall of 1986","interactions":[],"lastModifiedDate":"2012-02-02T00:08:15","indexId":"wri874216","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4216","title":"Potentiometric surface of the Magothy Aquifer in southern Maryland during the Fall of 1986","docAbstract":"The potentiometric map is highlighted with indications concerning: (1) outcrop areas of the Magothy aquifer; (2) the potentiometric contour of the aquifer; (3) observation and/or supply wells yielding < 10,000 gallons/day (gpd); and (4) other supply wells with yields > 10,000 gpd. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874216","usgsCitation":"Mack, F.K., Andreasen, D.C., Curtin, S.E., and Wheeler, J.C., 1987, Potentiometric surface of the Magothy Aquifer in southern Maryland during the Fall of 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4216, 1 map ;28 x 22 cm., https://doi.org/10.3133/wri874216.","productDescription":"1 map ;28 x 22 cm.","costCenters":[],"links":[{"id":118881,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4216/report-thumb.jpg"},{"id":54473,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4216/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47d6e4b07f02db4b3555","contributors":{"authors":[{"text":"Mack, F. K.","contributorId":93471,"corporation":false,"usgs":true,"family":"Mack","given":"F.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":194771,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Andreasen, D. C.","contributorId":32565,"corporation":false,"usgs":true,"family":"Andreasen","given":"D.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194769,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Curtin, S. E.","contributorId":17235,"corporation":false,"usgs":true,"family":"Curtin","given":"S.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":194768,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Wheeler, J. C.","contributorId":66225,"corporation":false,"usgs":true,"family":"Wheeler","given":"J.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":194770,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25128,"text":"cir930F - 1987 - International strategic minerals inventory summary report; cobalt","interactions":[],"lastModifiedDate":"2012-02-02T00:08:16","indexId":"cir930F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"930","chapter":"F","title":"International strategic minerals inventory summary report; cobalt","docAbstract":"Major world resources of cobalt are described in this summary report of information in the International Strategic Minerals Inventory {ISMI}. ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, and the United States of America. This report, designed to be of benefit to policy analysts, contains two parts. Part I presents an overview of the resources and potential supply of cobalt on the basis of inventory information. Part II contains tables of some of the geologic information and mineral-resource and production data that were collected by ISMI participants.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930F","usgsCitation":"Crockett, R., Chapman, G., and Forrest, M., 1987, International strategic minerals inventory summary report; cobalt: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 54 p., https://doi.org/10.3133/cir930F.","productDescription":"v. :ill. ;26 cm.; 54 p.","costCenters":[],"links":[{"id":122561,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1987/0930f/report-thumb.jpg"},{"id":54108,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1987/0930f/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0773","contributors":{"authors":[{"text":"Crockett, R.N.","contributorId":6890,"corporation":false,"usgs":true,"family":"Crockett","given":"R.N.","email":"","affiliations":[],"preferred":false,"id":193262,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Chapman, G.R.","contributorId":98357,"corporation":false,"usgs":true,"family":"Chapman","given":"G.R.","email":"","affiliations":[],"preferred":false,"id":193264,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Forrest, M.D.","contributorId":39016,"corporation":false,"usgs":true,"family":"Forrest","given":"M.D.","email":"","affiliations":[],"preferred":false,"id":193263,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":25418,"text":"wri874044 - 1987 - Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83","interactions":[],"lastModifiedDate":"2012-02-02T00:08:09","indexId":"wri874044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4044","title":"Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83","docAbstract":"The relation between pumpage and change in storage was evaluated for most of a three-county area in southwestern Nebraska from 1975 through 1983. Initial comparison of the 1975-83 pumpage with change in storage in the study area indicated that the 1 ,042,300 acre-ft of change in storage was only about 30% of the 3,425,000 acre-ft of pumpage. An evaluation of the data used to calculate pumpage and change in storage indicated that there was a relatively large potential for error in estimates of specific yield. As a result, minimum and maximum values of specific yield were estimated and used to recalculate change in storage. Estimates also were derived for the minimum and maximum amounts of recharge that could occur as a result of cultivation practices. The minimum and maximum estimates for specific yield and for recharge from cultivation practices were used to compute a range of values for the potential amount of additional recharge that occurred as a result of irrigation. The minimum and maximum amounts of recharge that could be caused by irrigation in the study area were 953,200 acre-ft (28% of pumpage) and 2,611,200 acre-ft (76% of pumpage), respectively. These values indicate that a substantial percentage of the water pumped from the aquifer is resupplied to storage in the aquifer as a result of a combination of irrigation return flow and enhanced recharge from precipitation that results from cultivation and irrigation practices. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874044","usgsCitation":"Heimes, F., Ferrigno, C., Gutentag, E., Lucky, R., Stephens, D., and Weeks, J., 1987, Comparison of irrigation pumpage with change in ground-water storage in the High Plains aquifer in Chase, Dundy, and Perkins counties, Nebraska, 1975-83: U.S. Geological Survey Water-Resources Investigations Report 87-4044, iv, 34 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874044.","productDescription":"iv, 34 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123377,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4044/report-thumb.jpg"},{"id":54138,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae383","contributors":{"authors":[{"text":"Heimes, F.J.","contributorId":60654,"corporation":false,"usgs":true,"family":"Heimes","given":"F.J.","affiliations":[],"preferred":false,"id":193606,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ferrigno, C.F.","contributorId":27092,"corporation":false,"usgs":true,"family":"Ferrigno","given":"C.F.","email":"","affiliations":[],"preferred":false,"id":193604,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Gutentag, E. D.","contributorId":70015,"corporation":false,"usgs":true,"family":"Gutentag","given":"E. D.","affiliations":[],"preferred":false,"id":193608,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Lucky, R.R.","contributorId":89171,"corporation":false,"usgs":true,"family":"Lucky","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":193609,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stephens, D.M.","contributorId":42970,"corporation":false,"usgs":true,"family":"Stephens","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":193605,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Weeks, J.B.","contributorId":61426,"corporation":false,"usgs":true,"family":"Weeks","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":193607,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":25743,"text":"wri864325 - 1987 - A Reconnaissance study to relate land use and ground-water quality in the Gulf Coastal Plain of Louisiana and Mississippi","interactions":[],"lastModifiedDate":"2012-02-02T00:08:14","indexId":"wri864325","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4325","title":"A Reconnaissance study to relate land use and ground-water quality in the Gulf Coastal Plain of Louisiana and Mississippi","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864325","usgsCitation":"Strickland, D., Fendick, R., Bednar, G., and Everett, D., 1987, A Reconnaissance study to relate land use and ground-water quality in the Gulf Coastal Plain of Louisiana and Mississippi: U.S. Geological Survey Water-Resources Investigations Report 86-4325, iv, 20 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864325.","productDescription":"iv, 20 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":118892,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4325/report-thumb.jpg"},{"id":54504,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4325/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4966e4b0b290850ef20d","contributors":{"authors":[{"text":"Strickland, D.J.","contributorId":49400,"corporation":false,"usgs":true,"family":"Strickland","given":"D.J.","email":"","affiliations":[],"preferred":false,"id":194886,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fendick, R.B. Jr.","contributorId":69602,"corporation":false,"usgs":true,"family":"Fendick","given":"R.B.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":194888,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bednar, G.A.","contributorId":94668,"corporation":false,"usgs":true,"family":"Bednar","given":"G.A.","email":"","affiliations":[],"preferred":false,"id":194889,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Everett, D.E.","contributorId":53420,"corporation":false,"usgs":true,"family":"Everett","given":"D.E.","email":"","affiliations":[],"preferred":false,"id":194887,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","interactions":[{"subject":{"id":11777,"text":"ofr8350 - 1984 - Quality of ground water in Idaho","indexId":"ofr8350","publicationYear":"1984","noYear":false,"title":"Quality of ground water in Idaho"},"predicate":"SUPERSEDED_BY","object":{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","indexId":"wsp2272","publicationYear":"1987","noYear":false,"title":"Quality of ground water in Idaho"},"id":1},{"subject":{"id":15414,"text":"ofr8550 - 1985 - Nearshore marine geologic investigations, Point Barrow to Skull Cliff, Northeast Chukchi Sea","indexId":"ofr8550","publicationYear":"1985","noYear":false,"title":"Nearshore marine geologic investigations, Point Barrow to Skull Cliff, Northeast Chukchi Sea"},"predicate":"SUPERSEDED_BY","object":{"id":3025,"text":"wsp2272 - 1987 - Quality of ground water in Idaho","indexId":"wsp2272","publicationYear":"1987","noYear":false,"title":"Quality of ground water in Idaho"},"id":2}],"lastModifiedDate":"2012-02-02T00:05:45","indexId":"wsp2272","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"2272","title":"Quality of ground water in Idaho","docAbstract":"The major aquifers in Idaho are categorized under two rock types, sedimentary and volcanic, and are grouped into six hydrologic basins. Areas with adequate, minimally adequate, or deficient data available for groundwater-quality evaluations are described. \r\n\r\nWide variations in chemical concentrations in the water occur within individual aquifers, as well as among the aquifers. The existing data base is not sufficient to describe fully the ground-water quality throughout the State; however, it does indicate that the water is generally suitable for most uses. In some aquifers, concentrations of fluoride, cadmium, and iron in the water exceed the U.S. Environmental Protection Agency's drinking-water standards. Dissolved solids, chloride, and sulfate may cause problems in some local areas. Water-quality data are sparse in many areas, and only general statements can be made regarding the areal distribution of chemical constituents. Few data are available to describe temporal variations of water quality in the aquifers. \r\n\r\nPrimary concerns related to special problem areas in Idaho include (1) protection of water quality in the Rathdrum Prairie aquifer, (2) potential degradation of water quality in the Boise-Nampa area, (3) effects of widespread use of drain wells overlying the eastern Snake River Plain basalt aquifer, and (4) disposal of low-level radioactive wastes at the Idaho National Engineering Laboratory. \r\n\r\nShortcomings in the ground-water-quality data base are categorized as (1) multiaquifer sample inadequacy, (2) constituent coverage limitations, (3) baseline-data deficiencies, and (4) data-base nonuniformity.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2272","usgsCitation":"Yee, J., and Souza, W.R., 1987, Quality of ground water in Idaho: U.S. Geological Survey Water Supply Paper 2272, iv, 53 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2272.","productDescription":"iv, 53 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":139471,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2272/report-thumb.jpg"},{"id":29856,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2272/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a73e4b07f02db643973","contributors":{"authors":[{"text":"Yee, Johnson J.","contributorId":13612,"corporation":false,"usgs":true,"family":"Yee","given":"Johnson J.","affiliations":[],"preferred":false,"id":146165,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Souza, William R.","contributorId":90295,"corporation":false,"usgs":true,"family":"Souza","given":"William","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":146166,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":25587,"text":"wri874090 - 1987 - Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:08:29","indexId":"wri874090","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4090","title":"Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985","docAbstract":"Hydrologic and geochemical monitoring, to detect changes caused by magmatic and tectonic processes in the Long Valley caldera has continued through 1985. The monitoring included the collection of the following types of data: chemical and isotopic composition of water and gases from springs, wells, and steam vents; temperatures in wells, springs, and steam vents; flow rates of springs and streams; water levels in wells; and barometric pressure and precipitation at several sites. In addition, reservoir temperatures for the geothermal system were estimated from computations based on chemical geothermometers applied to fluid samples from wells and springs. Estimates of thermal water discharged from springs were made on the basis of boron and chloride fluxes in surface waters for selected sites in the Casa Diablo area and along the Mammoth-Hot Creek drainage. These data are presented in tables and graphs. The Long Valley area was relatively quiescent throughout 1985 in terms of geodetic changes and seismic activity. As a consequence , the hydrologic system varied mainly in response to seasonal influences of temperature, atmospheric pressure, and precipitation. However, spring flows near Casa Diablo were influenced by pumping at the geothermal production well field nearby. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874090","usgsCitation":"Farrar, C.D., Sorey, M., Rojstaczer, S., Janik, C.J., Winnett, T.L., and Clark, M.D., 1987, Hydrologic and geochemical monitoring in Long Valley Caldera, Mono County, California, 1985: U.S. Geological Survey Water-Resources Investigations Report 87-4090, vi, 71 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874090.","productDescription":"vi, 71 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124293,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4090/report-thumb.jpg"},{"id":54329,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4090/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db61184e","contributors":{"authors":[{"text":"Farrar, C. D.","contributorId":71978,"corporation":false,"usgs":true,"family":"Farrar","given":"C.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194309,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Sorey, M.L.","contributorId":73185,"corporation":false,"usgs":true,"family":"Sorey","given":"M.L.","affiliations":[],"preferred":false,"id":194310,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Rojstaczer, S.A.","contributorId":54620,"corporation":false,"usgs":true,"family":"Rojstaczer","given":"S.A.","email":"","affiliations":[],"preferred":false,"id":194308,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Janik, C. J.","contributorId":10795,"corporation":false,"usgs":true,"family":"Janik","given":"C.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":194305,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Winnett, T. L.","contributorId":27095,"corporation":false,"usgs":true,"family":"Winnett","given":"T.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194307,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Clark, M. D.","contributorId":25202,"corporation":false,"usgs":true,"family":"Clark","given":"M.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":194306,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ,{"id":26274,"text":"wri874068 - 1987 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 1","interactions":[],"lastModifiedDate":"2022-02-01T19:25:51.13635","indexId":"wri874068","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-4068","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 1","docAbstract":"This report delineates and describes the geohydrology and susceptibility of the major aquifers to contamination in Area 1 - Colbert, Franklin, Lauderdale, Lawrence, Limeston, Madison, and Morgan Counties. Most of the area is underlain by a Mississippian carbonate sequence that includes two major aquifers, the Tuscumbia-Fort Payne aquifer and the Bangor aquifer. A third major aquifer, the Tuscaloosa aquifer of Cretaceous age, occurs in the southwest part of the area. The Mississippi carbonate aquifers are the Tuscumbia-Fort Payne aquifer which includes most Tuscumbia Limestone and the Fort Payne Chert, and a small area of the Monteagle Limestone, and the Bangor aquifer which includes the Bangor Limestone and Hartselle Sandstone. Both of these aquifers possess highly-variable secondary porosity and permeability related to fractures that have been enlarged, sometimes to cavernous proportions, due to solution processes. The Tuscaloosa aquifer consists of the Tuscaloosa Group, an unconsolidated clastic deposit that has relatively uniform primary porosity and permeability. Significant quantities of groundwater are available from each of the aquifers. Water levels at nearly 2 ,000 wells indicate that, for each aquifer, general groundwater movement is from topographically high to low areas. Each of the aquifers is recharged throughout its outcrop in the study area and is susceptible to contamination within the outcrop. Generalized topographic settings such as closed-contour depressions are identified as areas that are highly susceptible to contamination. Specific features such as sinkholes also are identified as extremely susceptible to contamination.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri874068","usgsCitation":"Bossong, C., and Harris, W.F., 1987, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 1: U.S. Geological Survey Water-Resources Investigations Report 87-4068, Report: v, 34 p.; 1 Plate: 19.00 × 16.39 inches, https://doi.org/10.3133/wri874068.","productDescription":"Report: v, 34 p.; 1 Plate: 19.00 × 16.39 inches","costCenters":[],"links":[{"id":395231,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46744.htm"},{"id":55084,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4068/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55083,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4068/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126666,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4068/report-thumb.jpg"}],"country":"United States","state":"Alabama","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.2267,\n 34.0444\n ],\n [\n -86.2833,\n 34.0444\n ],\n [\n -86.2833,\n 35\n ],\n [\n -88.2267,\n 35\n ],\n [\n -88.2267,\n 34.0444\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8c18","contributors":{"authors":[{"text":"Bossong, C. R.","contributorId":39762,"corporation":false,"usgs":true,"family":"Bossong","given":"C. R.","affiliations":[],"preferred":false,"id":196098,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harris, W. F.","contributorId":66303,"corporation":false,"usgs":true,"family":"Harris","given":"W.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":196099,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":15304,"text":"ofr87171 - 1987 - A simple ternary/quaternary plotting program for microcomputers","interactions":[],"lastModifiedDate":"2012-02-02T00:06:47","indexId":"ofr87171","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-171","title":"A simple ternary/quaternary plotting program for microcomputers","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87171","usgsCitation":"O’Connor, J.T., 1987, A simple ternary/quaternary plotting program for microcomputers: U.S. Geological Survey Open-File Report 87-171, 33 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87171.","productDescription":"33 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":146392,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0171/report-thumb.jpg"},{"id":44227,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b17e4b07f02db6a64ef","contributors":{"authors":[{"text":"O’Connor, J. T.","contributorId":92266,"corporation":false,"usgs":true,"family":"O’Connor","given":"J.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":170924,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":2265,"text":"wsp2303 - 1987 - Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information; with a section on theory and application of generalized least squares","interactions":[{"subject":{"id":14939,"text":"ofr85680 - 1985 - Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information","indexId":"ofr85680","publicationYear":"1985","noYear":false,"title":"Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information"},"predicate":"SUPERSEDED_BY","object":{"id":2265,"text":"wsp2303 - 1987 - Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information; with a section on theory and application of generalized least squares","indexId":"wsp2303","publicationYear":"1987","noYear":false,"title":"Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information; with a section on theory and application of generalized least squares"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:20","indexId":"wsp2303","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"2303","title":"Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information; with a section on theory and application of generalized least squares","docAbstract":"This report documents the results of an analysis of the surface-water data network in Kansas for its effectiveness in providing regional streamflow information. The network was analyzed using generalized least squares regression. The correlation and time-sampling error of the streamflow characteristic are considered in the generalized least squares method. Unregulated medium-, low-, and high-flow characteristics were selected to be representative of the regional information that can be obtained from streamflow-gaging-station records for use in evaluating the effectiveness of continuing the present network stations, discontinuing some stations, and (or) adding new stations. The analysis used streamflow records for all currently operated stations that were not affected by regulation and for discontinued stations for which unregulated flow characteristics, as well as physical and climatic characteristics, were available. The State was divided into three network areas, western, northeastern, and southeastern Kansas, and analysis was made for the three streamflow characteristics in each area, using three planning horizons. \r\n\r\nThe analysis showed that the maximum reduction of sampling mean-square error for each cost level could be obtained by adding new stations and discontinuing some current network stations. Large reductions in sampling mean-square error for low-flow information could be achieved in all three network areas, the reduction in western Kansas being the most dramatic. The addition of new stations would be most beneficial for mean-flow information in western Kansas. The reduction of sampling mean-square error for high-flow information would benefit most from the addition of new stations in western Kansas. Southeastern Kansas showed the smallest error reduction in high-flow information. A comparison among all three network areas indicated that funding resources could be most effectively used by discontinuing more stations in northeastern and southeastern Kansas and establishing more new stations in western Kansas.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2303","usgsCitation":"Medina, K., and Tasker, G.D., 1987, Analysis of surface-water data network in Kansas for effectiveness in providing regional streamflow information; with a section on theory and application of generalized least squares: U.S. Geological Survey Water Supply Paper 2303, iv, 28 p. :ill., map ;28 cm., https://doi.org/10.3133/wsp2303.","productDescription":"iv, 28 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":137588,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2303/report-thumb.jpg"},{"id":28055,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2303/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acfe4b07f02db68015f","contributors":{"authors":[{"text":"Medina, K.D.","contributorId":46925,"corporation":false,"usgs":true,"family":"Medina","given":"K.D.","email":"","affiliations":[],"preferred":false,"id":144919,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Tasker, Gary D.","contributorId":95035,"corporation":false,"usgs":true,"family":"Tasker","given":"Gary","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":144920,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":16275,"text":"ofr87272B - 1987 - Gneiss-hosted kyanite gold and gneiss-hosted epithermal gold; a supplement to U.S. Geological Survey bulletin 1693","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr87272B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"87-272","chapter":"B","title":"Gneiss-hosted kyanite gold and gneiss-hosted epithermal gold; a supplement to U.S. Geological Survey bulletin 1693","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87272B","usgsCitation":"Tosdal, R., and Smith, D.B., 1987, Gneiss-hosted kyanite gold and gneiss-hosted epithermal gold; a supplement to U.S. Geological Survey bulletin 1693: U.S. Geological Survey Open-File Report 87-272, 8 p. ;28 cm., https://doi.org/10.3133/ofr87272B.","productDescription":"8 p. ;28 cm.","costCenters":[],"links":[{"id":150474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0272b/report-thumb.jpg"},{"id":45195,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0272b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674279","contributors":{"authors":[{"text":"Tosdal, R. M.","contributorId":54982,"corporation":false,"usgs":true,"family":"Tosdal","given":"R. M.","affiliations":[],"preferred":false,"id":172535,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smith, D. B. davidsmith@usgs.gov","contributorId":12840,"corporation":false,"usgs":true,"family":"Smith","given":"D.","email":"davidsmith@usgs.gov","middleInitial":"B.","affiliations":[],"preferred":false,"id":172534,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57543,"text":"wdrAR861 - 1987 - Water resources data for Arkansas, water year 1986","interactions":[],"lastModifiedDate":"2014-04-09T15:24:46","indexId":"wdrAR861","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"AR-86-1","title":"Water resources data for Arkansas, water year 1986","docAbstract":"Water resources data for the 1986 water year for Arkansas consist of records of gage height,\ndischarge, and water quality of streams; water quality of lakes; and water levels and water quality\nof wells. This report contains discharge records for 48 gaging stations; water quality for 154\nstations, 73 partial-record stations, 5 observation wells, and 1 precipitation station, and\nwater levels for 96 observation wells. Also included are data for 85 crest-stage partial record\nstations. Additional water data were collected at various sites, not part of the systematic\ndata-collection program, and are published as miscellaneous measurements. These data represent\nthat part of the National Water Data System operated by the U.S. Geological Survey and cooperating\nState and Federal agencies in Arkansas.
\nRecords of discharge or gage height of streams, and contents or elevation of lakes were first\npublished in a series of U.S. Geological Survey water-supply papers entitled \"Surface Water Supply\nof the United States.\" Through September 30, 1960, these water-supply papers were in an annual\nseries and for 1961-65 and 1966-70 were in a 5 -year series. Records of chemical quality, water\ntemperatures, and suspended sediment were published from 1941 to 1970 in an annual series of water-supply\npapers entitled \"Quality of Surface Waters of the United States.\" Records of ground-water\nlevels were published from 1935 to 1974 in a series of water-supply papers entitled \"Ground Water\nLevels in the United States.\" Water-supply papers may be consulted in the libraries of the principal\ncities in the United States or may be purchased from Branch of Distribution, U.S. Geological\nSurvey, 1200 South Eads Street, Arlington, VA 22202.
\nFor water years 1961 through 1974, streamflow data were released by the Geological Survey in\nannual reports on a State-boundary basis. Water-quality records for water years 1964 through\n1974 were similarly released, either in separate reports or in conjuction with streamflow records.\nBeginning with the 1975 water year, water data for streamflow, water quality, and ground water are\npublished as an official Survey report on a State-boundary basis. These official Survey reports\ncarry an identification number consisting of the two-letter State abbreviation, the last two\ndigits of the water year, and the volume number. For example, this report is identified as \"U.S.\nGeological Survey Water Data Report AR-86-1.\"
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrAR861","collaboration":"Prepared in cooperation with the Arkansas Department of Pollution Control and Ecology; Arkansas Geological Commission; Arkansas Soil and Water Conservation Commission; Arkansas State Highway and Transportation Department and with other State and Federal agencies","usgsCitation":"Lamb, T., Porter, J., Lambert, B., and Edds, J., 1987, Water resources data for Arkansas, water year 1986: U.S. Geological Survey Water Data Report AR-86-1, viii, 533 p., https://doi.org/10.3133/wdrAR861.","productDescription":"viii, 533 p.","numberOfPages":"546","temporalStart":"1985-10-01","temporalEnd":"1986-09-30","costCenters":[{"id":629,"text":"Water Resources Division","active":false,"usgs":true}],"links":[{"id":182169,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wdrAR861.jpg"},{"id":286067,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1986/ar-86-1/report.pdf"}],"country":"United States","state":"Arkansas","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94.6179,33.0041 ], [ -94.6179,36.4997 ], [ -89.6468,36.4997 ], [ -89.6468,33.0041 ], [ -94.6179,33.0041 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd173","contributors":{"authors":[{"text":"Lamb, T.E.","contributorId":58272,"corporation":false,"usgs":true,"family":"Lamb","given":"T.E.","email":"","affiliations":[],"preferred":false,"id":257292,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Porter, J.E.","contributorId":51779,"corporation":false,"usgs":true,"family":"Porter","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":257291,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lambert, B.F.","contributorId":30292,"corporation":false,"usgs":true,"family":"Lambert","given":"B.F.","email":"","affiliations":[],"preferred":false,"id":257290,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Edds, J.","contributorId":27549,"corporation":false,"usgs":true,"family":"Edds","given":"J.","email":"","affiliations":[],"preferred":false,"id":257289,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ]}