{"pageNumber":"1920","pageRowStart":"47975","pageSize":"25","recordCount":68924,"records":[{"id":28857,"text":"wri864335 - 1987 - Magnitude and frequency of floods in Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri864335","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":"86-4335","title":"Magnitude and frequency of floods in Arkansas","docAbstract":"The magnitude and frequency of peak discharges on streams in Arkansas, were estimated through the use of comprehensive regression analyses, in which physical characteristics of streams were related to flood characteristics at gaging stations. Equations derived from the regression analyses provide estimates of peak discharges with selected recurrence intervals from 2 to 100 yrs on streams that have drainage areas < 3,000 sq mi. The regression analyses indicate that size of drainage area, slope of the main channel, length of the main channel, elevation of the basin, and mean annual precipitation were the most significant basin and climatic characteristics that affect the magnitude and frequency of floods. A technique is presented for estimating a stage-discharge relation at ungaged sites based on a cross section determined from topographic maps. This cross-section and stage-discharge relation is then used to determine the hydraulic radius for the discharges at each recurrence interval. Techniques are presented for estimating the magnitude and frequency of peak discharges using the hydraulic radius with other physical characteristics of the basin. The techniques that use the hydraulic radius give standard errors of estimate from 5% to 16% lower than techniques that do not use hydraulic radius. Data from 200 gaging stations with drainage areas less than 3,000 sq mi and with at least 10 yrs of record were used in the analyses. Large rivers such as the Red, Arkansas, White, Black, St. Francis, Mississippi, and Ouachita Rivers have flood flow characteristics that differ from those of smaller tributary streams and were, therefore, treated individually. Regional regression equations are not applicable to the large rivers; the magnitude and frequency of floods along these rivers are based on station data. A method is described for estimating the magnitude and frequency of peak discharges on streams for urban areas in Arkansas. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri864335","usgsCitation":"Neely, B., 1987, Magnitude and frequency of floods in Arkansas: U.S. Geological Survey Water-Resources Investigations Report 86-4335, v, 51 p. :maps ;28 cm., https://doi.org/10.3133/wri864335.","productDescription":"v, 51 p. :maps ;28 cm.","costCenters":[],"links":[{"id":124291,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4335/report-thumb.jpg"},{"id":57728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4335/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649544","contributors":{"authors":[{"text":"Neely, B.L.","contributorId":90344,"corporation":false,"usgs":true,"family":"Neely","given":"B.L.","affiliations":[],"preferred":false,"id":200514,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14239,"text":"ofr87728 - 1987 - Louisiana ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:06:38","indexId":"ofr87728","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":"87-728","title":"Louisiana ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87728","usgsCitation":"Huff, G.F., Fendick, R., Stuart, C., and Cramer, G., 1987, Louisiana ground-water quality: U.S. Geological Survey Open-File Report 87-728, iv, 7 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87728.","productDescription":"iv, 7 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":144373,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0728/report-thumb.jpg"},{"id":42918,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0728/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db644727","contributors":{"authors":[{"text":"Huff, G. F.","contributorId":11229,"corporation":false,"usgs":true,"family":"Huff","given":"G.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":169131,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fendick, R.B.","contributorId":19556,"corporation":false,"usgs":true,"family":"Fendick","given":"R.B.","affiliations":[],"preferred":false,"id":169132,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Stuart, C.G.","contributorId":58644,"corporation":false,"usgs":true,"family":"Stuart","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":169134,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Cramer, George","contributorId":37752,"corporation":false,"usgs":true,"family":"Cramer","given":"George","email":"","affiliations":[],"preferred":false,"id":169133,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":26779,"text":"wri874113 - 1987 - Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 6","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri874113","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":"87-4113","title":"Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 6","docAbstract":"This report delineates and describes the geohyrology and susceptibility of the major aquifers to contamination in Area 6, Greene, Marengo, Pickens, Sumter, and Tuscaloosa Counties in west-central Alabama. The major aquifers in the study area are the Nanafalia, Eutaw, Gordo, and Coker aquifers of Tertiary and Cretaceous age. The recharge areas for one or more of these aquifers are in each of the five counties. East aquifer is a source of public water supply in one or more of the five counties. All recharge areas for the major aquifers are susceptible to contamination from the surface. However, large parts of the recharge areas are in rural settings that are used for timberlands, farms, and pastures, and are several miles from pumping centers; therefore, these areas are not highly susceptible to contamination. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874113","usgsCitation":"DeJarnette, S., and Crownover, J., 1987, Geohydrology and susceptibility of major aquifers to surface contamination in Alabama; area 6: U.S. Geological Survey Water-Resources Investigations Report 87-4113, v, 27 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/wri874113.","productDescription":"v, 27 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":110242,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_46779.htm","linkFileType":{"id":5,"text":"html"},"description":"46779"},{"id":122843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4113/report-thumb.jpg"},{"id":55663,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4113/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55664,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4113/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bd3","contributors":{"authors":[{"text":"DeJarnette, S.S.","contributorId":6896,"corporation":false,"usgs":true,"family":"DeJarnette","given":"S.S.","affiliations":[],"preferred":false,"id":196989,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Crownover, J.E.","contributorId":79114,"corporation":false,"usgs":true,"family":"Crownover","given":"J.E.","email":"","affiliations":[],"preferred":false,"id":196990,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":41938,"text":"ofr87336 - 1987 - Aeromagnetic map of the Goshute area, northeastern Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"ofr87336","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":"87-336","title":"Aeromagnetic map of the Goshute area, northeastern Nevada","language":"ENGLISH","doi":"10.3133/ofr87336","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Aeromagnetic map of the Goshute area, northeastern Nevada: U.S. Geological Survey Open-File Report 87-336, 1 map :photocopy ;140 x 73 cm., on sheet 150 x 77 cm., https://doi.org/10.3133/ofr87336.","productDescription":"1 map :photocopy ;140 x 73 cm., on sheet 150 x 77 cm.","costCenters":[],"links":[{"id":172748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":21241,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0336/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af8e4b07f02db694084","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":530718,"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":28847,"text":"wri874021 - 1987 - Ground-water resources of Flagler County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:08:44","indexId":"wri874021","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":"87-4021","title":"Ground-water resources of Flagler County, Florida","docAbstract":"Groundwater is the only significant source of potable water in Flagler County. Usable water occurs in the Upper Floridan aquifer, the intermediate population is expected to place stresses on the water resources of the county. Although rainfall averages almost 50 in/yr, most of the water leaves as evapotranspiration and streamflow. Less than 1 in/yr recharge may be occurring to the Upper Floridan aquifer, the highest yielding aquifer. The Upper Floridan aquifer consists of the Avon Park Formation, the Ocala Limestone, and the basal dolomitic limestone of the Hawthorne. Use of the Upper Floridan aquifer for public water supply is limited in most of the county because it contains marginally potable or brackish water. It is used extensively for agricultural irrigation. The intermediate aquifer system consists of thin, discontinues lenses of sand, shell, and limestone between clays overlying the Floridan aquifer system. The intermediate aquifer system is an important part of the public water supply of the county because of the good quality of the water. The intermediate aquifer system has variable yields because of the discontinuous lenses. The surficial aquifer system is composed of sand and shell with varying fractions of finer materials. Well yields are small in the west and central parts of Flagler County, but the surficial aquifer system is an adequate source of domestic supply on the barrier island. A zone of freshwater in the surficial aquifer system is very important in the Hammock area, being the local source of most domestic supply in the area. Changes in hydrologic conditions from the 1950 's include a long-term decline in water levels in the Upper Floridan aquifer coincident with lower-than-average rainfall and a greater seasonal fluctuation of water levels. Chloride concentrations of water in the Upper Floridan aquifer do not appear to have changed significantly, presently ranging from 7 to 3,700 mg/L. Development will place stress on the aquifers and may result in upconing of brackish water in pumping centers and in lateral saltwater intrusion in coastal areas. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874021","usgsCitation":"Navoy, A., and Bradner, L.A., 1987, Ground-water resources of Flagler County, Florida: U.S. Geological Survey Water-Resources Investigations Report 87-4021, v, 45 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874021.","productDescription":"v, 45 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":123701,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4021/report-thumb.jpg"},{"id":57720,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63d2c8","contributors":{"authors":[{"text":"Navoy, A. S.","contributorId":51771,"corporation":false,"usgs":true,"family":"Navoy","given":"A. S.","affiliations":[],"preferred":false,"id":200501,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":200500,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":12115,"text":"ofr84734 - 1987 - Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:06:35","indexId":"ofr84734","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":"84-734","title":"Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana","docAbstract":"This report is one of a series designed to characterize the hydrology of drainage basins within coal provinces, nationwide. Area 51 (in the Rocky Mountain Coal Province) includes all or part of the Shoshone, Bighorn, Greybull, Wind, and Popo Agie River drainage basins - a total of 11,800 sq mi. Area 51 contains more than 18 million tons of strippable bituminous coal and extensive deposits of subbituminous coal, in the arid and semiarid basins. The report represents a summary of results of water resources investigations of the U.S. Geological Survey, some of which were conducted in cooperation with State and other Federal agencies. More than 30 individual topics are discussed in brief texts that are accompanied by maps, graphs, photographs , and illustrations. Primary topics in the reports are physiography, resources and economy, surface-water quantity and quality, and groundwater. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84734","usgsCitation":"Peterson, D.A., Mora, K.L., Lowry, M.E., Rankl, J.G., Wilson, J.F., Lowham, H., and Ringen, B.H., 1987, Hydrology of area 51, northern Great Plains and Rocky Mountain coal provinces, Wyoming and Montana (WRI/OFR): U.S. Geological Survey Open-File Report 84-734, v, 73 p. :ill. (some col.), maps (some col.) ;28 cm., https://doi.org/10.3133/ofr84734.","productDescription":"v, 73 p. :ill. (some col.), maps (some col.) ;28 cm.","costCenters":[],"links":[{"id":144783,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0734/report-thumb.jpg"},{"id":40143,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0734/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"edition":"WRI/OFR","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601fa8","contributors":{"authors":[{"text":"Peterson, David A. davep@usgs.gov","contributorId":1742,"corporation":false,"usgs":true,"family":"Peterson","given":"David","email":"davep@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":165124,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mora, K. L.","contributorId":55008,"corporation":false,"usgs":true,"family":"Mora","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":165128,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lowry, Marlin E.","contributorId":52552,"corporation":false,"usgs":true,"family":"Lowry","given":"Marlin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":165127,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Rankl, James G.","contributorId":93026,"corporation":false,"usgs":true,"family":"Rankl","given":"James","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":165130,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Wilson, James F. Jr.","contributorId":23546,"corporation":false,"usgs":true,"family":"Wilson","given":"James","suffix":"Jr.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":165126,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lowham, H. W.","contributorId":8111,"corporation":false,"usgs":true,"family":"Lowham","given":"H. W.","affiliations":[],"preferred":false,"id":165125,"contributorType":{"id":1,"text":"Authors"},"rank":6},{"text":"Ringen, Bruce H.","contributorId":73612,"corporation":false,"usgs":true,"family":"Ringen","given":"Bruce","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":165129,"contributorType":{"id":1,"text":"Authors"},"rank":7}]}}
,{"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":"<p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p><p>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.</p>","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":12122,"text":"ofr84463 - 1987 - Hydrology of area 8, eastern Coal Province, West Virginia and Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:06:46","indexId":"ofr84463","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":"84-463","title":"Hydrology of area 8, eastern Coal Province, West Virginia and Ohio","docAbstract":"The hydrology of Area 8 in the Ohio River basin in northwestern West Virginia and southeastern Ohio, is influenced by geology and geologic structure. Rocks underlying the area consist of alternating beds of sandstone, siltstone, shale, limestone, and mudstone. Minable coal is contained within the Pennsylvania and Permian rocks. Coal production in 1980 totaled 6.7 million tons from underground mines and one million tons from surface mines. There is a wide range of soil types (29 soil associations) in five land-resource areas. Precipitation averages about 41 inches annually and is greatest at higher altitudes along the eastern boundary of the area. Average annual runoff ranges from 13 to 29 inches per year. The principal land uses are forest and agriculture. Estimated water use during 1980 was 1,170 million gallons per day. Surface-water quality ranges from excellent to poor. The highest iron, manganese and sulfate concentrations were present in mined areas. Well yields range from less than 1 to 350 gallons per minute. Groundwater from the Mississippian rocks contain lesser amounts of dissolved solids than water from the Lower Pennsylvanian rocks. Water high in chloride content is present in some valley areas. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84463","usgsCitation":"Friel, E., Ehlke, T.A., Hobba, W., Ward, S., and Schultz, R.A., 1987, Hydrology of area 8, eastern Coal Province, West Virginia and Ohio: U.S. Geological Survey Open-File Report 84-463, v, 78 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/ofr84463.","productDescription":"v, 78 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":95065,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0463/report.pdf","size":"26930","linkFileType":{"id":1,"text":"pdf"}},{"id":146288,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0463/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a13e4b07f02db601f80","contributors":{"authors":[{"text":"Friel, E.A.","contributorId":90743,"corporation":false,"usgs":true,"family":"Friel","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":165156,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ehlke, T. A.","contributorId":106477,"corporation":false,"usgs":true,"family":"Ehlke","given":"T.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165158,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hobba, W.A. Jr.","contributorId":77518,"corporation":false,"usgs":true,"family":"Hobba","given":"W.A.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":165155,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Ward, S.M.","contributorId":93920,"corporation":false,"usgs":true,"family":"Ward","given":"S.M.","email":"","affiliations":[],"preferred":false,"id":165157,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Schultz, R. A.","contributorId":108126,"corporation":false,"usgs":true,"family":"Schultz","given":"R.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":165159,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}}
,{"id":15640,"text":"ofr8737 - 1987 - Preliminary hydrologic data for wells tested in Nash Draw, near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:07:02","indexId":"ofr8737","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":"87-37","title":"Preliminary hydrologic data for wells tested in Nash Draw, near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico","docAbstract":"Hydrologic testing was conducted at wells WIPP-25, WIPP-26, WIPP-27, WIPP-28, WIPP-29, and WIPP-30 in Nash Draw near the Waste Isolation Pilot Plant site in southeastern New Mexico. The three water-bearing zones tested were the Magenta Dolomite Member of the Rustler Formation, Culebra Dolomite Member of the Rustler Formation, and the Rustler Formation-Salado Formation contact zone. Inflatable packers were used in a variety of test configurations. Tests conducted include bailing, recovery after perforation, shut in, slug, flow, and pressure pulse. Water pressure response in the tested zone was monitored by a pressure-transducer system. Preliminary hydrologic-test data are tabulated in chronological order for each well. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8737","usgsCitation":"Richey, S.F., 1987, Preliminary hydrologic data for wells tested in Nash Draw, near the proposed Waste Isolation Pilot Plant site, southeastern New Mexico: U.S. Geological Survey Open-File Report 87-37, iv, 131 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8737.","productDescription":"iv, 131 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":147698,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0037/report-thumb.jpg"},{"id":44604,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db667b0d","contributors":{"authors":[{"text":"Richey, S. F.","contributorId":98740,"corporation":false,"usgs":true,"family":"Richey","given":"S.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":171478,"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":41024,"text":"ofr87451 - 1987 - Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1987","interactions":[],"lastModifiedDate":"2012-02-02T00:05:04","indexId":"ofr87451","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":"87-451","title":"Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1987","docAbstract":"A May 1987 potentiometric surface map of the Upper Floridan aquifer in west-central Florida depicts water levels for the annual low water-level period. Water levels in most wells measured in May 1987 were lower than in September 1986. May levels averaged about 0.5 foot higher than September levels in latitudes north of the Hillsborough-Pasco County line and about 6 feet lower in southern areas. The average water-level change between May 1986 and May 1987 in individual wells was more than 3 feet. Average water levels in most wells measured in May 1987 were more than 2 feet higher than May 1986 levels in the north and more than 4 feet higher in the south. (USGS)","language":"ENGLISH","doi":"10.3133/ofr87451","usgsCitation":"Lewelling, B., 1987, Potentiometric surface of the upper Floridan Aquifer, west-central Florida, May 1987: U.S. Geological Survey Open-File Report 87-451, 1 map :photocopy ;79 x 56 cm., on sheet 92 x 69 cm., https://doi.org/10.3133/ofr87451.","productDescription":"1 map :photocopy ;79 x 56 cm., on sheet 92 x 69 cm.","costCenters":[],"links":[{"id":136751,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":78905,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0451/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682c71","contributors":{"authors":[{"text":"Lewelling, B. R.","contributorId":17969,"corporation":false,"usgs":true,"family":"Lewelling","given":"B. R.","affiliations":[],"preferred":false,"id":224346,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29442,"text":"wri824003 - 1987 - Evaluation of selected surface-water-quality stations in Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri824003","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":"82-4003","title":"Evaluation of selected surface-water-quality stations in Wyoming","docAbstract":"The U.S. Geological Survey, in cooperation with the Wyoming Department of Agriculture, has conducted a surface-water-quality program in Wyoming since 1965. The purpose has been to determine the chemical quality of the water in terms of the major dissolved constituents (salinity). Changing agricultural techniques and energy development have stimulated a need for an expanded program involving additional types of data. This report determines the adequacy of the data collected thus far to describe the chemical quality. The sampling program was evaluated by determining how well the data describe the dissolved-solids load of the streams. Monthly mean loads were estimated at 16 stations throughout the network where daily streamflow and daily specific conductance were available. Monthly loads were then compared with loads estimated from daily streamflow and data derived from analyses of samples collected on a monthly basis at these same stations. Agreement was good. Solute-load hydrographs were constructed for 37 stations and from some reaches where streamflow records were available. Because stations where no discharge records are available are not amenable to this type of analysis, data collected at these stations are of limited usefulness. This report covers analyses of data for all qualifying sites in Wyoming except those in the Green River Basin, which were analyzed in U.S. Geological Survey Water Resources Investigations 77-103. The salinity in most of the streams evaluated is adequately described by the data collected. Reduced sampling is feasible, and time and money can be diverted to collecting other data. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824003","usgsCitation":"Rucker, S., and DeLong, L.L., 1987, Evaluation of selected surface-water-quality stations in Wyoming: U.S. Geological Survey Water-Resources Investigations Report 82-4003, vi, 72 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824003.","productDescription":"vi, 72 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119600,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4003/report-thumb.jpg"},{"id":58288,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4003/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4890","contributors":{"authors":[{"text":"Rucker, S.J.","contributorId":41472,"corporation":false,"usgs":true,"family":"Rucker","given":"S.J.","email":"","affiliations":[],"preferred":false,"id":201534,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeLong, L. L.","contributorId":44530,"corporation":false,"usgs":true,"family":"DeLong","given":"L.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":201535,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29206,"text":"wri864017 - 1987 - Hydrologic monitoring of selected streams in coal fields of central and southern Utah — Summary of data collected, August 1978-September 1984","interactions":[],"lastModifiedDate":"2025-01-13T19:40:23.306101","indexId":"wri864017","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":"86-4017","title":"Hydrologic monitoring of selected streams in coal fields of central and southern Utah — Summary of data collected, August 1978-September 1984","docAbstract":"The U.S. Geological Survey conducted a coal-hydrology monitoring program in coal-field areas of central and southern Utah during August 1978-September 1984 to determine possible hydrologic impacts of future mining and to provide a better understanding of the hydrologic systems of the coal resource areas monitored. Data were collected at 19 gaging stations--18 stations in the Price, San Rafael, and Dirty Devil River basins, and 1 in the Kanab Creek Basin. Streamflow data were collected continuously at 11 stations and seasonally at 5 stations. At the other three stations streamflow data were collected continuously during the 1979 water year and then seasonally for the rest of their periods of record. Types of data collected at each station included quantity and quality of streamflow; suspended sediment concentrations; and descriptions of stream bottom sediments, benthic invertebrate, and phytoplankton samples. Also, base flow measurements were made annually upstream from 12 of the gaging stations. Stream bottom sediment sampled at nearly all the monitoring sites contained small to moderate quantities of coal, which may be attributed chiefly to pre-monitoring mining. Streamflow sampled at several sites contained large concentrations of sulfate and dissolved solids. Also, concentrations of various trace elements at 10 stations, and phenols at 18 stations, exceeded the criteria of the EPA for drinking water. This may be attributed to contemporary (water years 1979-84) mine drainage activities. The data collected during the complete water years (1979-84) of monitoring do provide a better understanding of the hydrologic systems of the coal field areas monitored. The data also provide a definite base by which to evaluate hydrologic impacts of continued or increased coal mining in those areas. (Author 's abstract)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864017","usgsCitation":"Price, D., and Plantz, G., 1987, Hydrologic monitoring of selected streams in coal fields of central and southern Utah — Summary of data collected, August 1978-September 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4017, Report: vii, 102 p.; 1 Plate: 22.28 × 23.43 inches, https://doi.org/10.3133/wri864017.","productDescription":"Report: vii, 102 p.; 1 Plate: 22.28 × 23.43 inches","costCenters":[],"links":[{"id":394077,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36487.htm"},{"id":58066,"rank":3,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4017/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":124282,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4017/report-thumb.jpg"},{"id":58065,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4017/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -112.577,\n              37.198\n            ],\n            [\n              -112.0670,\n              37.198\n            ],\n            [\n              -112.0670,\n              37.541\n            ],\n            [\n              -112.577,\n              37.541\n            ],\n            [\n              -112.577,\n              37.198\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db6064dd","contributors":{"authors":[{"text":"Price, Don","contributorId":30608,"corporation":false,"usgs":true,"family":"Price","given":"Don","email":"","affiliations":[],"preferred":false,"id":201145,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Plantz, G.G.","contributorId":79103,"corporation":false,"usgs":true,"family":"Plantz","given":"G.G.","affiliations":[],"preferred":false,"id":201146,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29444,"text":"wri874011 - 1987 - Sediment discharge in Muddy Creek and the effect of sedimentation rate on the proposed Wolford Mountain reservoir near Kremmling, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:56","indexId":"wri874011","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":"87-4011","title":"Sediment discharge in Muddy Creek and the effect of sedimentation rate on the proposed Wolford Mountain reservoir near Kremmling, Colorado","docAbstract":"Stream-discharge data collected from May 1982 through October 1985 and sediment data collected from March 1985 through October 1985 at stream flow-gaging station 09041500 Muddy Creek at Kremmling, Colorado, were used to determine total-sediment discharge into the proposed Wolford Mountain Reservoir. The data were divided on a seasonal basis, and statistical relations between suspended-sediment discharge and stream discharge were determined for the rising stage, falling stage, and base-flow period. One statistical relation between bedload discharge and stream discharge was determined from all collected data. These relations were used with 3 years of daily stream-discharge data to estimate total-sediment discharge. Total-sediment discharge was largest prior to the annual peak stream discharge during the study period and decreased thereafter. At least 97% of the total-sediment discharge was suspended sediment. Mean annual total-sediment discharge in Muddy Creek near Kremmling was estimated to be 83,000 tons per year for the 1983 through 1985 water years. Water-storage capacity of the proposed Wolford Mountain Reservoir at site C would decrease 10% after 100 years at this rate of mean annual total-sediment discharge. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874011","usgsCitation":"Ruddy, B.C., 1987, Sediment discharge in Muddy Creek and the effect of sedimentation rate on the proposed Wolford Mountain reservoir near Kremmling, Colorado: U.S. Geological Survey Water-Resources Investigations Report 87-4011, iv, 22 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874011.","productDescription":"iv, 22 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159818,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4011/report-thumb.jpg"},{"id":58290,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4011/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc030","contributors":{"authors":[{"text":"Ruddy, B. C.","contributorId":65098,"corporation":false,"usgs":true,"family":"Ruddy","given":"B.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":201538,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":29461,"text":"wri874179 - 1987 - Mean velocity, longitudinal dispersion, and reaeration characteristics of selected streams in the Kentucky River basin","interactions":[],"lastModifiedDate":"2012-02-02T00:09:02","indexId":"wri874179","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":"87-4179","title":"Mean velocity, longitudinal dispersion, and reaeration characteristics of selected streams in the Kentucky River basin","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874179","usgsCitation":"Ruhl, K., and Smoot, J.L., 1987, Mean velocity, longitudinal dispersion, and reaeration characteristics of selected streams in the Kentucky River basin: U.S. Geological Survey Water-Resources Investigations Report 87-4179, vi, 61 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri874179.","productDescription":"vi, 61 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119604,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4179/report-thumb.jpg"},{"id":58307,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4179/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a27e4b07f02db6107c7","contributors":{"authors":[{"text":"Ruhl, K.J.","contributorId":35322,"corporation":false,"usgs":true,"family":"Ruhl","given":"K.J.","email":"","affiliations":[],"preferred":false,"id":201557,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Smoot, J. L.","contributorId":59794,"corporation":false,"usgs":true,"family":"Smoot","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":201558,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29293,"text":"wri874016 - 1987 - Acid-rain damage to carbonate stone; a preliminary quantitative assessment based on the aqueous geochemistry of rainfall runoff","interactions":[],"lastModifiedDate":"2012-03-16T17:16:06","indexId":"wri874016","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":"87-4016","title":"Acid-rain damage to carbonate stone; a preliminary quantitative assessment based on the aqueous geochemistry of rainfall runoff","language":"ENGLISH","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri874016","usgsCitation":"Reddy, M., 1987, Acid-rain damage to carbonate stone; a preliminary quantitative assessment based on the aqueous geochemistry of rainfall runoff: U.S. Geological Survey Water-Resources Investigations Report 87-4016, v, 27 p. :ill., map ;28 cm., https://doi.org/10.3133/wri874016.","productDescription":"v, 27 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":246718,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4016/WRIR87-4016.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":159191,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_87_4016.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3445","contributors":{"authors":[{"text":"Reddy, M.M.","contributorId":24363,"corporation":false,"usgs":true,"family":"Reddy","given":"M.M.","email":"","affiliations":[],"preferred":false,"id":201290,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14949,"text":"ofr87735 - 1987 - Missouri ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:06:48","indexId":"ofr87735","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":"87-735","title":"Missouri ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87735","usgsCitation":"Mesko, T.O., and Berkas, W., 1987, Missouri ground-water quality: U.S. Geological Survey Open-File Report 87-735, iv, 9 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87735.","productDescription":"iv, 9 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":145946,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0735/report-thumb.jpg"},{"id":43765,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0735/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699acc","contributors":{"authors":[{"text":"Mesko, T. O.","contributorId":83934,"corporation":false,"usgs":true,"family":"Mesko","given":"T.","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":170302,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Berkas, W.R.","contributorId":59808,"corporation":false,"usgs":true,"family":"Berkas","given":"W.R.","affiliations":[],"preferred":false,"id":170301,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":39662,"text":"pp1368 - 1987 - Late Mississippian gastropods of the Chainman Shale, west-central Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:56","indexId":"pp1368","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1368","title":"Late Mississippian gastropods of the Chainman Shale, west-central Utah","docAbstract":"The Chainman Shale of Mississippian (Osagean to late Chesterian) age, well exposed in the Confusion Range of western Utah, has yielded a profusion of fossils during investigations conducted by the U.S. Geological Survey in the past 30 years. Conspicuous among these fossils are gastropods, which range in age from latest Meramecian to late Chesterian. In west-central Utah, not far from the State boundary, the Chainman outcrop belt stretches from Granite Mountain south to the northern part of the Needle Range, a distance of69 miles (110 km). The Chainman thickens from north to south; the section at Granite Mountain is 1,315 feet (401 m) thick and that at Jensen Wash in the Burbank Hills, 2,203 feet (671 m). \r\n\r\nThe rocks of the Chainman Shale record a general though irregular shallowing of the area from moderate depths of 330 feet (100 m) or so to quite shallow depths of perhaps locally little more than 3-6 feet (1-2 m). Most of the gastropods occur with ammonoids in a facies of shale or shale containing phosphatic limestone concretions, In this lutaceous facies, Glabrocingulum is predominant and Lunulazona and Retispira are common; these genera are represented by a succession of species. A thick limestone unit is present in some areas in the upper part of the formation, particularly in the vicinity of Skunk Spring, where it is 318 feet (97 m) thick. This limestone unit represents a calcareous shoal facies having an entirely different gastropod fauna, characterized by Catazona and species of Naticopsis. \r\n\r\nThe Chainman Shale could be easily zoned by gastropods, but we are not proposing such azonation. A framework of ammonoid and foraminiferal zones already is available, and we prefer to regard the gastropod assemblages as part of this framework. The assemblages are confined to the major ammonoid and foraminiferal zones, and only three of the gastropod species seem to range across major zonal boundaries. These species are Bellerophon (Bellerophon vespertinus Gordon and Yochelson and Straparollus (Euomphalus intermedius Gordon and Yochelson, both of which are present in Mamet Foraminifer Zones 17 and 18, and Bellazona polita n. sp., which locally seems to range from Mamet Foraminifer Zone 16s into the basal part of Zone 17. \r\n\r\nEight assemblages, seven of them in ascending stratigraphic order, are recognized within the gastropod fauna of the Chainman Shale; the eighth assemblage is a facies equivalent of the sixth highest. The seven mud-dwelling assemblages are characterized mainly by species of Glabrocingulum and Lunulazona, which together account for 80 percent of the gastropod specimens in our Chainman collections. The eighth assemblage, that in the shallow-water carbonate facies, is the one characterized by Catazona and species of Naticopsis. \r\n\r\nThe lowermost gastropod assemblage, that of Lunulazona nodomarginata (McChesney), includes 10 species and is restricted to the northern end of the study area, where it occurs in the upper part of the Goniatites americanus Ammonoid Zone, in beds equivalent to the lower part of Mamet's Foraminifer Zone 16i. We regard the entire G. americanus Zone as late Meramecian in age. All the zones higher in the Chainman are Chesterian in age. The second assemblage is that of Lunulazona costata Sadlick and Neilsen, which includes six gastropod species; it occurs in the Goniatites granos us Ammonoid Zone, equivalent to Mamet's Foraminifer Zone 16s. \r\n\r\nThree gastropod assemblages are recognized within the Paracravenoceras barnettense Ammonoid Zone, equivalent to Mamet's Foraminifer Zone 17. The earliest, that of Lunulazona sadlicki, includes five species; the intermediate, that of Glabrocingulum hosei n. sp., four species; and the highest, that of Glabrocingulum confusionense n, sp., two species (the second being G. hosei). \r\n\r\nTwo laterally equivalent facies-controlled assemblages are present within the Cravenoceras hesperium Ammonoid Zone, most of which is equivalent to Mamet's Foraminifer Zone 18","language":"ENGLISH","doi":"10.3133/pp1368","usgsCitation":"Gordon, M., and Yochelson, E.L., 1987, Late Mississippian gastropods of the Chainman Shale, west-central Utah: U.S. Geological Survey Professional Paper 1368, 112 p., https://doi.org/10.3133/pp1368.","productDescription":"112 p.","costCenters":[],"links":[{"id":119440,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1368/report-thumb.jpg"},{"id":67382,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1368/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1be4b07f02db6a8bdc","contributors":{"authors":[{"text":"Gordon, Mackenzie Jr.","contributorId":13225,"corporation":false,"usgs":true,"family":"Gordon","given":"Mackenzie","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":221936,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Yochelson, Ellis L.","contributorId":90802,"corporation":false,"usgs":true,"family":"Yochelson","given":"Ellis","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":221937,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":13746,"text":"ofr87314 - 1987 - Abstracts of papers presented at the Geographic information systems symposium, June 2-4, 1987, Reston, Virginia","interactions":[],"lastModifiedDate":"2018-06-11T13:16:38","indexId":"ofr87314","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":"87-314","title":"Abstracts of papers presented at the Geographic information systems symposium, June 2-4, 1987, Reston, Virginia","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr87314","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1987, Abstracts of papers presented at the Geographic information systems symposium, June 2-4, 1987, Reston, Virginia: U.S. Geological Survey Open-File Report 87-314, vi, 44 p., https://doi.org/10.3133/ofr87314.","productDescription":"vi, 44 p.","numberOfPages":"50","costCenters":[{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"links":[{"id":146559,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0314/report-thumb.jpg"},{"id":42325,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0314/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a394c","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528945,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":41182,"text":"ofr87464 - 1987 - Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1987","interactions":[],"lastModifiedDate":"2022-08-03T21:30:28.628538","indexId":"ofr87464","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":"87-464","title":"Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1987","docAbstract":"The potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity is shown for May 1987. The Upper Floridan aquifer is the principal source of potable water in the area. Water level measurements were made on approximately 1,000 wells and on several springs. The potentiometric surface is shown mostly by 5-ft contour intervals. In the Fernandina Beach area of Nassau County, a 30-ft interval is used to show a deep cone of depression. The potentiometric surface ranged from 129 ft above sea level in Polk County to 54 ft below sea level in Nassau County. Water levels in key wells ranged from several ft above to several ft below the May average in response to areal patterns of rainfall. Most levels in the district were above the below average levels of May 1986. Rises of about 2 ft from May 1986 levels were common in the southern half of the District, and the potentiometric surface rose as much as 6 to 8 ft in places. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87464","usgsCitation":"Schiner, G.R., 1987, Potentiometric surface of the upper Floridan Aquifer in the St. Johns River Water Management District and vicinity, Florida, May 1987: U.S. Geological Survey Open-File Report 87-464, 1 Plate: 26.60 × 44.99 inches, https://doi.org/10.3133/ofr87464.","productDescription":"1 Plate: 26.60 × 44.99 inches","costCenters":[],"links":[{"id":173283,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79014,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0464/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":404785,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17270.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River Water Management District and vicinity, upper Floridan Aquifer","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83.990478515625,\n              26.598351182358293\n            ],\n            [\n              -80.321044921875,\n              26.598351182358293\n            ],\n            [\n              -80.321044921875,\n              30.675715404167743\n            ],\n            [\n              -83.990478515625,\n              30.675715404167743\n            ],\n            [\n              -83.990478515625,\n              26.598351182358293\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682e4e","contributors":{"authors":[{"text":"Schiner, George R.","contributorId":22743,"corporation":false,"usgs":true,"family":"Schiner","given":"George","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":224617,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":6355,"text":"pp1257 - 1987 - Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal","interactions":[{"subject":{"id":48896,"text":"ofr84431 - 1984 - Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal","indexId":"ofr84431","publicationYear":"1984","noYear":false,"title":"Bedrock aquifers in the Denver basin, Colorado; a quantitative water-resources appraisal"},"predicate":"SUPERSEDED_BY","object":{"id":6355,"text":"pp1257 - 1987 - Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal","indexId":"pp1257","publicationYear":"1987","noYear":false,"title":"Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal"},"id":1}],"lastModifiedDate":"2022-10-12T20:34:52.243768","indexId":"pp1257","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","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":"1257","title":"Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/pp1257","usgsCitation":"Robson, S.G., 1987, Bedrock aquifers in the Denver Basin, Colorado: A quantitative water-resources appraisal: U.S. Geological Survey Professional Paper 1257, Report: v, 73 p.; 5 Plates: 29.00 × 39.00 inches, https://doi.org/10.3133/pp1257.","productDescription":"Report: v, 73 p.; 5 Plates: 29.00 × 39.00 inches","costCenters":[],"links":[{"id":104583,"rank":700,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_4771.htm","linkFileType":{"id":5,"text":"html"},"description":"4771"},{"id":33712,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1257/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33711,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33710,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33709,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33708,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":33707,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1257/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117610,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1257/report-thumb.jpg"}],"country":"United States","state":"Colorado","otherGeospatial":"Denver Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -105.275,\n              38.6389\n            ],\n            [\n              -103.6458,\n              38.6389\n            ],\n            [\n              -103.5458,\n              40.4167\n            ],\n            [\n              -105.275,\n              40.4167\n            ],\n            [\n              -105.275,\n              38.6389\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6be4b07f02db63da79","contributors":{"authors":[{"text":"Robson, Stanley G.","contributorId":73187,"corporation":false,"usgs":true,"family":"Robson","given":"Stanley","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":152569,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55212,"text":"wdrIA861 - 1987 - Water resources data Iowa, water year 1986","interactions":[],"lastModifiedDate":"2016-03-07T14:24:40","indexId":"wdrIA861","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":"IA-86-1","title":"Water resources data Iowa, water year 1986","docAbstract":"<p>Water resources data for the 1986 water year for Iowa consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; ground-water levels and ground-water quality. This report contains discharge records for 110 stream-gaging stations; stage and contents for 8 lakes and reservoirs; water quality for 8 stream-gaging stations; sediment records for 10 streamgaging stations; water levels for 108 observation wells; and chemical analyses for 214 observation wells. Also included are 116 crest-stage partial-record stations. Additional water data were collected at various sites, not part of the systematic data-collection program, and are published as miscellaneous measurements and analyses. The data represent that part of the National Data System operated:\"by the U.S. Geological Survey and cooperating State and Federal agencies in Iowa.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Iowa City","doi":"10.3133/wdrIA861","collaboration":"Prepared in cooperation with the Geological Survey Bureau, Iowa Department of Natural Resources, Iowa Department of Transportation and with Federal agencies","usgsCitation":"Melcher, N., Detroy, M., Matthes, W., and Karsten, R., 1987, Water resources data Iowa, water year 1986: U.S. Geological Survey Water Data Report IA-86-1, xv, 333 p., https://doi.org/10.3133/wdrIA861.","productDescription":"xv, 333 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":351,"text":"Iowa Water Science 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,{"id":41150,"text":"ofr87688 - 1987 - Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1987","interactions":[],"lastModifiedDate":"2022-07-20T21:26:07.904016","indexId":"ofr87688","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":"87-688","title":"Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1987","docAbstract":"<p>This map shows the potentiometric surface of the Upper Floridan aquifer in the St. Johns River Water Management District and vicinity for September 1987. The Upper Floridan aquifer is the principal source of potable water in the area. Water level measurements were made on approximately 1,000 wells and on several springs. The potentiometric surface is shown mostly by 5-foot contour intervals. The potentiometric surface ranged from 129 feet above sea level in Polk County to 77 feet below sea level in Nassau County. Water levels in most key wells ranged from 0 to 10 feet below in May 1987 levels in response to the lack of recharge from rainfall and an attendant increase in pumpage. Declines of about 0 to 3 feet from May 1987 levels were common in most areas of the district. However, the largest declines from May 1987 levels, as much as 7 to 10 feet, were mostly in well fields along the coastline. Many levels in the district were equal to or lower than the average levels of September 1986.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87688","usgsCitation":"Bradner, L.A., 1987, Potentiometric surface of the upper Floridan aquifer in the St. Johns River Water Management District and vicinity, Florida, September 1987: U.S. Geological Survey Open-File Report 87-688, 1 Plate: 26.40 × 44.83 inches, https://doi.org/10.3133/ofr87688.","productDescription":"1 Plate: 26.40 × 44.83 inches","costCenters":[],"links":[{"id":170987,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":404168,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17322.htm","linkFileType":{"id":5,"text":"html"}},{"id":78988,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0688/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"St. Johns River Water Management District and vicinity","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -83,\n              26.5\n            ],\n            [\n              -80,\n              26.5\n            ],\n            [\n              -80,\n              31\n            ],\n            [\n              -83,\n              31\n            ],\n            [\n              -83,\n              26.5\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ce5","contributors":{"authors":[{"text":"Bradner, L. A.","contributorId":21925,"corporation":false,"usgs":true,"family":"Bradner","given":"L.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":224574,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":14404,"text":"ofr87762 - 1987 - Wisconsin ground-water quality","interactions":[],"lastModifiedDate":"2012-02-02T00:07:03","indexId":"ofr87762","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":"87-762","title":"Wisconsin ground-water quality","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87762","usgsCitation":"Kammerer, P., 1987, Wisconsin ground-water quality: U.S. Geological Survey Open-File Report 87-762, iv, 7 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87762.","productDescription":"iv, 7 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":147456,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0762/report-thumb.jpg"},{"id":43086,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0762/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":43087,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0762/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d9e4b07f02db5dfb57","contributors":{"authors":[{"text":"Kammerer, P.A.","contributorId":21943,"corporation":false,"usgs":true,"family":"Kammerer","given":"P.A.","affiliations":[],"preferred":false,"id":169397,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
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