Interagency Report 522
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/ofr325","usgsCitation":"Water Resources Division, U.S. Geological Survey, and Saudi Arabia. Deputy Ministry for Mineral Resources, 1983, Landsat image map of the Judayyidat Ar'ar quadrangle, sheet 31E, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 325, 21.26 x 33.07 inches, https://doi.org/10.3133/ofr325.","productDescription":"21.26 x 33.07 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":312758,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","projection":"Transverse Mercator","country":"Saudi Arabia","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n 40.5,\n 32\n ],\n [\n 40.5,\n 31\n ],\n [\n 42,\n 31\n ],\n [\n 42,\n 32\n ],\n [\n 40.5,\n 32\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"567a823ee4b0a04ef490fcf5","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":583141,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Saudi Arabia. Deputy Ministry for Mineral Resources","contributorId":147327,"corporation":true,"usgs":false,"organization":"Saudi Arabia. Deputy Ministry for Mineral Resources","id":583142,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011195,"text":"70011195 - 1983 - Ichnofossils of the alluvial Willwood Formation (lower Eocene), Bighorn Basin, northwest Wyoming, U.S.A","interactions":[],"lastModifiedDate":"2025-06-16T22:38:28.101382","indexId":"70011195","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Ichnofossils of the alluvial Willwood Formation (lower Eocene), Bighorn Basin, northwest Wyoming, U.S.A","docAbstract":"The ichnofossil assemblage of the lower Eocene Willwood Formation consists of at least nine distinct endichnia that are preserved in full relief. Four forms (three ichnogenera and four ichnospecies) are new and represent fodinichnia and domichnia of oligochaete worms, an insect or spider, an unknown vertebrate (probably a mammal), and domichnia of an unidentified organism. Other potential trace makers of the ichnofauna include insects, mollusks, and decapods.
In contrast to an Egyptian Oligocene fluvial ichnofauna produced largely by animals that burrowed in stream channel deposits, the Willwood assemblage is principally of flood-plain origin. Though the ichnofauna occurs in a variety of paleosol types, most of the fossils are restricted in distribution to specific sediment and soil types and, within paleosols, to specific identifiable horizons. This attribute will make them valuable indiced of paleoenvironment once they are better known in other ancient alluvial sequences.
The environment suggested by the Willwood trace fossils (damp, but not wet soils with fluctuating water tables) is consistent with the warm temperate to subtropical (possibly monsoonal) conditions that are interpreted for the Willwood Formation by independent evidence of body fossils and paleopedology.
","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(83)90050-0","issn":"00310182","usgsCitation":"Bown, T.M., and Kraus, M.J., 1983, Ichnofossils of the alluvial Willwood Formation (lower Eocene), Bighorn Basin, northwest Wyoming, U.S.A: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 43, no. 1-2, p. 95-128, https://doi.org/10.1016/0031-0182(83)90050-0.","productDescription":"34 p.","startPage":"95","endPage":"128","costCenters":[],"links":[{"id":221573,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"country":"United States","state":"Wyoming","otherGeospatial":"northwest Wyoming","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -109.80507183883824,\n 44.989270996122485\n ],\n [\n -109.80507183883824,\n 43.36281120582049\n ],\n [\n -107.40183701322437,\n 43.36281120582049\n ],\n [\n -107.40183701322437,\n 44.989270996122485\n ],\n [\n -109.80507183883824,\n 44.989270996122485\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","volume":"43","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a37ffe4b0c8380cd61358","contributors":{"authors":[{"text":"Bown, T. M.","contributorId":106858,"corporation":false,"usgs":true,"family":"Bown","given":"T.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":360511,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kraus, M. J.","contributorId":44605,"corporation":false,"usgs":false,"family":"Kraus","given":"M.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":360510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":70011415,"text":"70011415 - 1983 - Paleoclimatic analyses of middle Eocene through Oligocene planktic foraminiferal faunas","interactions":[],"lastModifiedDate":"2025-06-16T15:34:48.019564","indexId":"70011415","displayToPublicDate":"2003-04-22T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":2996,"text":"Palaeogeography, Palaeoclimatology, Palaeoecology","printIssn":"0031-0182","active":true,"publicationSubtype":{"id":10}},"title":"Paleoclimatic analyses of middle Eocene through Oligocene planktic foraminiferal faunas","docAbstract":"Quantitative faunal analyses and oxygen isotope ranking of individual planktic foraminiferal species from deep sea sequences of three oceans are used to make paleoceanographic and paleoclimatic inferences. Species grouped into surface, intermediate and deep water categories based on δ18O values provide evidence of major changes in water-mass stratification, and individual species abundances indicate low frequency cool-warm oscillations. These data suggest that relatively stable climatic phases with minor cool-warm oscillations of ∼0.5 m.y. frequency are separated by rapid cooling events during middle Eocene to early Oligocene time.
Five major climatic phases are evident in the water-mass stratification between middle Eocene through Oligocene time. Phase changes occur at P14/P15, P15/P16, P20/P21 and P21/P22 Zone boundaries and are marked by major faunal turnovers, rapid cooling in the isotope record, hiatuses and changes in the eustatic sea level. A general cooling trend between middle Eocene to early late Oligocene is indicated by the successive replacement of warm middle Eocene surface water species by cooler late Eocene intermediate water species and still cooler Oligocene intermediate and deep water species. Increased water-mass stratification in the latest Eocene (P17), indicated by the coexistence of surface, intermediate and deep dwelling species groups, suggest that increased thermal gradients developed between the equator and poles nearly coincident with the development of the psychrosphere. This pattern may be related to significant ice accumulation between late Eocene and early late Oligocene time.
","language":"English","publisher":"Elsevier","doi":"10.1016/0031-0182(83)90049-4","issn":"00310182","usgsCitation":"Keller, G., 1983, Paleoclimatic analyses of middle Eocene through Oligocene planktic foraminiferal faunas: Palaeogeography, Palaeoclimatology, Palaeoecology, v. 43, no. 1-2, p. 73-94, https://doi.org/10.1016/0031-0182(83)90049-4.","productDescription":"22 p.","startPage":"73","endPage":"94","costCenters":[],"links":[{"id":220902,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"43","issue":"1-2","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"505a73c7e4b0c8380cd77234","contributors":{"authors":[{"text":"Keller, G.","contributorId":72527,"corporation":false,"usgs":true,"family":"Keller","given":"G.","affiliations":[],"preferred":false,"id":361031,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011581,"text":"70011581 - 1983 - Accumulation of fossil fuels and metallic minerals in active and ancient rift lakes","interactions":[],"lastModifiedDate":"2025-08-27T16:27:51.597754","indexId":"70011581","displayToPublicDate":"2003-04-08T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3525,"text":"Tectonophysics","active":true,"publicationSubtype":{"id":10}},"title":"Accumulation of fossil fuels and metallic minerals in active and ancient rift lakes","docAbstract":"A study of active and ancient rift systems around the world suggests that accumulations of fossil fuels and metallic minerals are related to the interactions of processes that form rift valleys with those that take place in and around rift lakes. The deposition of the precursors of petroleum, gas, oil shale, coal, phosphate, barite, Cu-Pb-Zn sulfides, and uranium begins with erosion of uplifted areas, and the consequent input of abundant nutrients and solute loads into swamps and tectonic lakes. Hot springs and volcanism add other nutrients and solutes. The resulting high biological productivity creates oxidized/reduced interfaces, and anoxic and H2S-rich bottom waters which preserves metal-bearing organic tissues and horizons. In the depositional phases, the fine-grained lake deposits are in contact with coarse-grained beach, delta, river, talus, and alluvial fan deposits. Earthquake-induced turbidites also are common coarse-grained deposits of rift lakes.
Postdepositional processes in rifts include high heat flow and a resulting concentration of the organic and metallic components that were dispersed throughout the lakebeds. Postdepositional faulting brings organic- and metal-rich sourcebeds in contact with coarse-grained host and reservoir rocks. A suite of potentially economic deposits is therefore a characteristic of rift valleys.
","language":"English","publisher":"Elsevier","doi":"10.1016/0040-1951(83)90038-0","issn":"00401951","usgsCitation":"Robbins, E., 1983, Accumulation of fossil fuels and metallic minerals in active and ancient rift lakes: Tectonophysics, v. 94, no. 1-4, p. 633-658, https://doi.org/10.1016/0040-1951(83)90038-0.","productDescription":"26 p.","startPage":"633","endPage":"658","costCenters":[],"links":[{"id":221452,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"volume":"94","issue":"1-4","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"5059e682e4b0c8380cd4745f","contributors":{"authors":[{"text":"Robbins, Eleanora I.","contributorId":304012,"corporation":false,"usgs":false,"family":"Robbins","given":"Eleanora I.","affiliations":[],"preferred":false,"id":361456,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":70011361,"text":"70011361 - 1983 - Separation of arsenic(III) and arsenic(V) in ground waters by ion-exchange","interactions":[],"lastModifiedDate":"2025-08-13T16:51:14.70697","indexId":"70011361","displayToPublicDate":"2001-11-27T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":2,"text":"Article"},"publicationSubtype":{"id":10,"text":"Journal Article"},"seriesTitle":{"id":3517,"text":"Talanta","active":true,"publicationSubtype":{"id":10}},"title":"Separation of arsenic(III) and arsenic(V) in ground waters by ion-exchange","docAbstract":"The predominant species of arsenic in ground water are probably arsenite and arsenate. These can be separated with a strong anion-exchange resin (Dowex 1 × 8; 100–200 mesh, acetate form) in a 10 cm × 7 mm column. Samples are filtered and acidified with concentrated hydrochloric acid (1 ml per 100 ml of sample) at the sample site. Five ml of the acidified sample are used for the separation. At this acidity, As(III) passes through the acetate-form resin, and As(V) is retained. As(V) is eluted by passage of 0.12M hydrochloric acid through the column (resulting in conversion of the resin back into the chloride form). Samples are collected in 5-ml portions up to a total of 20 ml. The arsenic concentration in each portion is determined by graphite-furnace atomic-absorption spectrophotometry. The first two fractions give the As(III) concentration and the last two the As(V) concentration. The detection limit for the concentration of each species is 1
A nationwide need for information characterizing hydrologic conditions in mined and potential mine areas has become paramount with the enactment of the Surface Mining Control and Reclamation Act of 1977. This report, one in a series covering the coal provinces nationwide, presents information thematically by describing single hydrologic topics through the use of brief texts and accompanying maps, graphs, or other illustrations. The summation of the topical discussions provides a description of the hydrology of the area. Area 54, in north-central Colorado and south-central Wyoming, is 1 of 20 hydrologic reporting areas of the Northern Great Plains and Rocky Mountain coal provinces. Part of the Southern Rocky Mountains and Wyoming Basin physiographic provinces, the 8,380-square-mile area is one of contrasting geology, topography, and climate. This results in contrasting hydrologic characteristics. The major streams, the North Platte, Laramie, and Medicine Bow Rivers, and their principal tributaries, all head in granitic mountains and flow into and through sedimentary basins between the mountain ranges. Relief averages 2,000 to 3,000 feet. Precipitation in the mountains may exceed 40 inches annually, much of it during the winter, which produces deep snowpacks. Snowmelt in spring and summer provides most streamflow. Precipitation in the basins averages 10 to 16 inches annually, insufficient for sustained streamflow; thus, streams originating in the basins are ephemeral. Streamflow quality is best in the mountains where dissolved-solids concentrations generally are least. These concentrations increase as streams flow through sedimentary basins. The increases are mainly natural, but some may be due to irrigation in and adjacent to the flood plains. In the North Platte River, dissolved-solids concentrations are usually less than 300 milligrams per liter; in the Laramie and the Medicine Bow Rivers, the concentrations may average 500 to 850 milligrams per liter. However, water-quality stations on the Laramie and the Medicine Bow Rivers are farther removed from the mountain sources than the stations in the North Platte drainage. Because of the semiarid climate of the basins, soils are not adequately leached. Consequently, flow in ephemeral streams usually has a larger concentration of dissolved solids than that in perennial streams, averaging 1,000 to 1,600 milligrams per liter. Aquifers containing usable ground water are combined into three groups: (1) consolidated and unconsolidated non-coal-bearing Quaternary and Upper Tertiary deposits, (2) Mesozoic and Paleozoic sedimentary rocks, and (3) Lower Tertiary and Upper Cretaceous sedimentary rocks containing coal. These aquifers are used for municipal, domestic, irrigation, and stock supplies. Well yields range from about 5 to 1,000 gallons per minute, and depend on type of aquifer, saturated thickness, and degree of fracturing. The best quality ground water usually comes from the non-coal-bearing Quaternary and Upper Tertiary rocks or the Mesozoic and Paleozoic rocks; often it is dominated by calcium and bicarbonate ions. The coal-bearing formations have a large variability in water chemistry; dominant ions may be bicarbonate or sulfate and sodium, calcium, or magnesium. Dissolved-solids concentrations are generally larger than in the former two groups. The U.S. Geological Survey operates a network of hydrologic stations to observe the streamflow and groundwater conditions. This network currently includes 31 surface-water stations and 35 observation wells; information is available for many other sites observed in the past. Data available include rate of flow, water levels, and water quality; much of the data are available in published reports or from computer storage through the National Water Data Exchange (NAWDEX) or the National Water Data Storage and Retrieval System (WATSTORE). Five formations of Late Cretaceous and early Tertiary age contain coal.
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G.","contributorId":19983,"corporation":false,"usgs":true,"family":"Spinello","given":"A.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":254916,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nakao, J.H.","contributorId":16088,"corporation":false,"usgs":true,"family":"Nakao","given":"J.H.","affiliations":[],"preferred":false,"id":254915,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Flipse, W.J. Jr.","contributorId":98733,"corporation":false,"usgs":true,"family":"Flipse","given":"W.J.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":254917,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Carcaci, J.G.","contributorId":106195,"corporation":false,"usgs":true,"family":"Carcaci","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":254918,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":46554,"text":"ofr83937 - 1983 - Linear features determined from Landsat imagery in North Dakota","interactions":[],"lastModifiedDate":"2018-02-16T14:00:26","indexId":"ofr83937","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-937","title":"Linear features determined from Landsat imagery in North Dakota","docAbstract":"The report consists of a map (scale 1:500,000) that shows the linear features determined from Landsat imagery in North Dakota. The linear features, sometimes called linear trends or lineaments, are not identified as to type or origin. Most probably represent fractures or fracture zones, which may affect the movement of water or other fluids through the rocks. The linear features are classified as to length--less than 30 miles, 30 to 200 miles, 200 to 500 miles, and more than 500 miles. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83937","usgsCitation":"Cooley, M.E., 1983, Linear features determined from Landsat imagery in North Dakota: U.S. Geological Survey Open-File Report 83-937, 57.0 x 33.0 inches, https://doi.org/10.3133/ofr83937.","productDescription":"57.0 x 33.0 inches","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":170939,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20991,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0937/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"North 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E.","contributorId":89868,"corporation":false,"usgs":true,"family":"Cooley","given":"M.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":233553,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":26368,"text":"wri8174 - 1983 - Water resources of Manatee County, Florida","interactions":[],"lastModifiedDate":"2013-08-12T12:12:40","indexId":"wri8174","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"81-74","title":"Water resources of Manatee County, Florida","docAbstract":"Rapid development of Manatee County in southwest Florida is creating water-resource problems. This report presents an evaluation of the water resources and potential effects of water-resource developments. Most streams in the county have small drainage basins and minimal flow. Streamflow is variable with the base flow occurring from November to May. The Manattee River and its largest tributary, the Braden River, are the principal sources of public supplies. Surface water is generally of good quality and less mineralized than ground water except in the tidally affected and coastal area. The principal aquifers in the county are the surficial, minor artesian, and the Floridan. The Floridan aquifer is the major source of irrigation water in the county. The minor artesian aquifer is a highly developed source of water for small rural supplies. Withdrawals of 20 to 50 million gallons per fay from the Floridan aquifer since the 1950 's have caused declines in the potentiometric surface of about 20 to 50 feet. The quality of ground water is good except in the coastal and southern parts of the county. Water in the Floridan aquifer is generally more mineralized than the other aquifers, generally increasing in mineral content with depth and from the northeast towards the southwest. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri8174","usgsCitation":"Brown, D., 1983, Water resources of Manatee County, Florida: U.S. Geological Survey Water-Resources Investigations Report 81-74, vii, 112 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8174.","productDescription":"vii, 112 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158404,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0074/report-thumb.jpg"},{"id":276460,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0074/report.pdf"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4804e4b07f02db4ceb99","contributors":{"authors":[{"text":"Brown, David P.","contributorId":85590,"corporation":false,"usgs":true,"family":"Brown","given":"David P.","affiliations":[],"preferred":false,"id":196267,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55528,"text":"wdrLA831 - 1983 - Water resources data, Louisiana, water year 1983, volume 1. Central and northern Louisiana","interactions":[],"lastModifiedDate":"2025-02-10T17:46:56.129285","indexId":"wdrLA831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"LA-83-1","title":"Water resources data, Louisiana, water year 1983, volume 1. Central and northern Louisiana","docAbstract":"Water resources data for the 1983 water year for Louisiana consist of records of stage, discharge, and water quality of streams; stage, contents, and water quality of lakes and reservoirs; and water levels and water quality of ground water. This report, in two volumes, contains records for water discharge at 79 gaging stations (including stage for 69 of these stations); stage only for 50 gaging stations and 11 lakes; contents for 1 reservoir; water quality for 110 surface-water stations (including 33 gaging stations), 10 miscellaneous sites, 12 lakes, and 213 wells; and water levels for 679 observation wells. Also included are data for 195 crest-stage and flood profile partial-record stations. Additional water data were collected at various sites not involved in the systematic data-collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Louisiana.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA831","collaboration":"Prepared in cooperation with the Louisiana Department of Transportation and Development and with other State and Federal agencies","usgsCitation":"Carlson, D., Stallworth, G., Dantin, L., and Stuart, C., 1983, Water resources data, Louisiana, water year 1983, volume 1. 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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1373","contributors":{"authors":[{"text":"Carlson, D.D.","contributorId":10816,"corporation":false,"usgs":true,"family":"Carlson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":253643,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stallworth, G.R.","contributorId":107732,"corporation":false,"usgs":true,"family":"Stallworth","given":"G.R.","affiliations":[],"preferred":false,"id":253646,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Dantin, L.J.","contributorId":61891,"corporation":false,"usgs":true,"family":"Dantin","given":"L.J.","email":"","affiliations":[],"preferred":false,"id":253645,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stuart, 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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83611","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of south-central Alabama: U.S. Geological Survey Open-File Report 83-611, 9 Plates:32.24 × 22.31 inches or smaller, https://doi.org/10.3133/ofr83611.","productDescription":"9 Plates:32.24 × 22.31 inches or smaller","costCenters":[],"links":[{"id":172723,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79594,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-9.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79593,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79592,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79591,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79590,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79589,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79588,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79587,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":79586,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0611/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":391774,"rank":11,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_14133.htm"}],"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 -86,\n 31.5\n ],\n [\n -87,\n 31.5\n ],\n [\n -87,\n 32.833\n ],\n [\n -86,\n 32.833\n ],\n [\n -86,\n 31.5\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691cc3","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":530667,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":18886,"text":"ofr83831 - 1983 - Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:07:25","indexId":"ofr83831","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-831","title":"Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine","docAbstract":"Water samples were collected in the vicinity of Jackman, Maine as a part of the study of the relationship of dissolved constituents in water to the sediments subjacent to the water. Each sample was analyzed for specific conductance, alkalinity, acidity, pH, fluoride, chloride, sulfate, phosphate, nitrate, sodium, potassium, calcium, magnesium, and silica. Trace elements determined were copper, zinc, molybdenum, lead, iron, manganese, arsenic, cobalt, nickel, and strontium. The longitude and latitude of each sample location and a sample site map are included in the report as well as a table of the analytical results.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr83831","usgsCitation":"Ficklin, W.H., Nowlan, G., and Preston, D.J., 1983, Analytical results for 544 water samples collected in the Attean Quartz Monzonite in the vicinity of Jackman, Maine: U.S. Geological Survey Open-File Report 83-831, 48 p. :map ;28 cm., https://doi.org/10.3133/ofr83831.","productDescription":"48 p. :map ;28 cm.","costCenters":[],"links":[{"id":150813,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0831/report-thumb.jpg"},{"id":48283,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0831/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":48284,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0831/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67cc04","contributors":{"authors":[{"text":"Ficklin, W. H.","contributorId":89517,"corporation":false,"usgs":true,"family":"Ficklin","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":179921,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nowlan, G.A.","contributorId":99131,"corporation":false,"usgs":true,"family":"Nowlan","given":"G.A.","affiliations":[],"preferred":false,"id":179922,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Preston, D. J.","contributorId":22759,"corporation":false,"usgs":false,"family":"Preston","given":"D.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":179920,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":46551,"text":"ofr82918 - 1983 - Lineaments and fracture traces, Decatur County, Indiana","interactions":[],"lastModifiedDate":"2016-05-24T10:45:50","indexId":"ofr82918","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-918","title":"Lineaments and fracture traces, Decatur County, Indiana","docAbstract":"Lineanents and fracture traces have been mapped throughout Decatur County, Indiana. These lineaments and fracture traces may indicate that solution enlarged vertical fractures in the limestone and dolonite aquifers underlie most of the county. The use of lineament and fracture-trace maps in selecting bedrock-drilling sites results in a significant increase in the number of usable sites. Bedrock wells drilled on or near mapped lineaments and fracture traces have a higher average yield than veils drilled into interfracture areas.
\nParts of Decatur County and several adjacent counties are economically restricted by inadequate water supplies. The Greensburg Municipal Water Works, supplying 35 percent of the county's population, obtains 25 percent of its water from six wells in Greensburg. The remaining 75 percent is pumped from the Flat Rock River. This water is piped 8.25 miles and lifted 183 feet to the treatment station. Although the Flatrock River has adequate flow to supply Greensburg's water needs, a ground-water supply can probably be developed nearer the treatment plant.
\nPleistocene till covers most of the nearly horizontal bedrock. Although averaging about 50 feet thick, this unconsolidated unit does not seem to inhibit the mapping of lineaments and fracture traces. Bedrock is middle Paleozoic limestone, dolomite, and shale. Two sequences of limestone and dolomite, separated by a thin shale unit, constitute the principal aquifer. The extremely variable well yields from this aquifer indicate that the bedrock permeability is also variable.
\nWell placement is important in a fractured bedrock terrane, as fractures are a principal source of water to the well. Here, the most productive bedrock wells are at the mapped intersection of two or more fracture traces or lineaments and at the lowest local altitude. Use of a fracture-trace map will not guarantee a sufficient supply of ground water but will reduce the chance of drilling an inadequate well.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/ofr82918","collaboration":"Indiana Department of Natuarl Resources, Decatur County","usgsCitation":"Greeman, T.K., 1983, Lineaments and fracture traces, Decatur County, Indiana: U.S. Geological Survey Open-File Report 82-918, iv, 1 map ;74 x 70 cm., folded in envelope 31 x 24 cm. +1 pamphlet (21 p. ill., maps ; 28 cm.), https://doi.org/10.3133/ofr82918.","productDescription":"iv, 1 map ;74 x 70 cm., folded in envelope 31 x 24 cm. +1 pamphlet (21 p. ill., maps ; 28 cm.)","startPage":"1","endPage":"18","numberOfPages":"21","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":170765,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0918/report-thumb.jpg"},{"id":83493,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0918/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83494,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0918/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Indiana","county":"Decatur","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.2977,39.4534],[-85.2966,39.268],[-85.4403,39.1954],[-85.5664,39.1325],[-85.688,39.1307],[-85.6881,39.1746],[-85.6878,39.2009],[-85.6873,39.2476],[-85.6865,39.2621],[-85.6859,39.3197],[-85.6852,39.3274],[-85.6851,39.3387],[-85.6849,39.3505],[-85.6302,39.3515],[-85.6296,39.4503],[-85.6302,39.453],[-85.2977,39.4534]]]},\"properties\":{\"name\":\"Decatur\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a51b8","contributors":{"authors":[{"text":"Greeman, Theodore K.","contributorId":30655,"corporation":false,"usgs":true,"family":"Greeman","given":"Theodore","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":233550,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":46852,"text":"ofr82635 - 1983 - Drainage divides, Massachusetts; Westfield and Farmington River basins","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"ofr82635","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"82-635","title":"Drainage divides, Massachusetts; Westfield and Farmington River basins","docAbstract":"Drainage boundaries for selected subbasins in western Hampshire, western Hampden, and southeastern Berkshire Counties, Massachusetts, are delineated on 15 topographic quadrangle maps at a scale of 1:24,000. Drainage basins are shown for all U.S. Geological Survey data-collection sites and for mouths of major rivers. Drainage basins are shown for the outlets of lakes or ponds and for streams where the drainage area is greater than 3 square miles. Successive sites along watercourses are indicated where the intervening area is at least 6 square miles on tributary streams or 10 square miles along the Westfield or Farmington Rivers. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82635","usgsCitation":"Gadoury, R.A., and Wandle, S.W., 1983, Drainage divides, Massachusetts; Westfield and Farmington River basins: U.S. Geological Survey Open-File Report 82-635, 15 maps :photocopy ;58 x 43 cm., https://doi.org/10.3133/ofr82635.","productDescription":"15 maps :photocopy ;58 x 43 cm.","costCenters":[],"links":[{"id":168317,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635e2a","contributors":{"authors":[{"text":"Gadoury, Russell A.","contributorId":99542,"corporation":false,"usgs":true,"family":"Gadoury","given":"Russell","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":234197,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wandle, S. William Jr.","contributorId":99562,"corporation":false,"usgs":true,"family":"Wandle","given":"S.","suffix":"Jr.","email":"","middleInitial":"William","affiliations":[],"preferred":false,"id":234198,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":58005,"text":"ofr83764 - 1983 - Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:12:31","indexId":"ofr83764","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-764","title":"Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982","language":"ENGLISH","doi":"10.3133/ofr83764","usgsCitation":"Morris, F., 1983, Hydrologic monitoring in the area of the Tennessee-Tombigbee Waterway, Mississippi-Alabama : fiscal year 1982: U.S. Geological Survey Open-File Report 83-764, iv, 189 leaves : ill., map ; 29 x 40 cm., https://doi.org/10.3133/ofr83764.","productDescription":"iv, 189 leaves : ill., map ; 29 x 40 cm.","costCenters":[],"links":[{"id":182250,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1ae4b07f02db606700","contributors":{"authors":[{"text":"Morris, Fred","contributorId":54197,"corporation":false,"usgs":true,"family":"Morris","given":"Fred","affiliations":[],"preferred":false,"id":258133,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":55177,"text":"wdrHI822 - 1983 - Water resources data for Hawaii and other Pacific areas, water year 1982: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","interactions":[],"lastModifiedDate":"2025-12-03T16:00:30.006584","indexId":"wdrHI822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"HI-82-2","title":"Water resources data for Hawaii and other Pacific areas, water year 1982: Volume 2. Guam, Northern Mariana Islands, Federated States of Micronesia, Palau, and American Samoa","docAbstract":"Volume 2 of water resources data for the 1982 water year for other Pacific areas consist of records of stage, discharge, and water quality of streams and springs; stage of a lake and a reservoir; and water levels and water quality in wells. This report contains discharge records for 43 gaging stations; stage only record for 2 gaging stations; water quality for 1 gaging station, 36 partial-record stations; water temperature for 42 gaging stations; and water levels for 14 observation wells and water quality for 52 ground-water sites. Also included are 43 low-flow 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. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating Governments and Federal agencies in other Pacific areas.
No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrNY823","usgsCitation":"Hood, J., Johnston, W.H., Zajd, H., and Dixson, H., 1983, Water resources data, New York, water year 1982, volume 3, western New York: U.S. Geological Survey Water Data Report NY-82-3, viii, 208 p., https://doi.org/10.3133/wdrNY823.","productDescription":"viii, 208 p.","costCenters":[],"links":[{"id":380712,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/ny-82-3/report.pdf"},{"id":181006,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/ny-82-3/report-thumb.jpg"}],"country":"United States","state":"New 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Additional surface water samples were collected during 1980 and 1981. Data are given herein for chemical analyses of snowmelt, tributary, river, spring, well, lake, reservoir, lake sediment pore fluid, tufa, lake and river sediment samples. These data provide the basis for consideration of processes which govern the chemical evolution of large closed basin hydrologic systems in the Basin and Range Province of the Southwestern United States.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr83740","usgsCitation":"Benson, L.V., and Spencer, R.J., 1983, A hydrochemical reconnaissance study of the Walker River basin, California and Nevada: U.S. Geological Survey Open-File Report 83-740, iii, 57 p., https://doi.org/10.3133/ofr83740.","productDescription":"iii, 57 p.","costCenters":[],"links":[{"id":405615,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_75702.htm","linkFileType":{"id":5,"text":"html"}},{"id":47466,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1983/0740/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":149290,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1983/0740/report-thumb.jpg"}],"country":"United States","state":"California, Nevada","otherGeospatial":"Walker River basin","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -119.9167,\n 38.0667\n ],\n [\n -118.5,\n 38.0667\n ],\n [\n -118.5,\n 39.1833\n ],\n [\n -119.9167,\n 39.1833\n ],\n [\n -119.9167,\n 38.0667\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae3ed","contributors":{"authors":[{"text":"Benson, L. 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Colorado River Basin above Dolores River","interactions":[],"lastModifiedDate":"2012-02-02T00:12:03","indexId":"wdrCO822","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"CO-82-2","title":"Water Resources Data for Colorado, Water Year 1982, Volume 2. Colorado River Basin above Dolores River","language":"ENGLISH","doi":"10.3133/wdrCO822","usgsCitation":"Ugland, R., Steinheimer, J., Blattner, J., and Kretschman, R., 1983, Water Resources Data for Colorado, Water Year 1982, Volume 2. Colorado River Basin above Dolores River: U.S. Geological Survey Water Data Report CO-82-2, 339 p., 6 Fig., 5 Tab., https://doi.org/10.3133/wdrCO822.","productDescription":"339 p., 6 Fig., 5 Tab.","costCenters":[],"links":[{"id":181438,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-2/report-thumb.jpg"},{"id":88282,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/co-82-2/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd0e7","contributors":{"authors":[{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":257416,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinheimer, J.T.","contributorId":81121,"corporation":false,"usgs":true,"family":"Steinheimer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":257419,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blattner, J.L.","contributorId":44541,"corporation":false,"usgs":true,"family":"Blattner","given":"J.L.","affiliations":[],"preferred":false,"id":257417,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kretschman, R.G.","contributorId":75623,"corporation":false,"usgs":true,"family":"Kretschman","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":257418,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":25798,"text":"wri834232 - 1983 - Time of travel and dispersion study in the Androscoggin River basin, Maine","interactions":[],"lastModifiedDate":"2012-02-02T00:08:28","indexId":"wri834232","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-4232","title":"Time of travel and dispersion study in the Androscoggin River basin, Maine","docAbstract":"In a series of dye tracer studies at discharge ranging from 45 to 212 cubic meters per second, time of travel and dispersion characteristics were determined at 12 sampling sites along 123 kilometers of the Androscoggin River (Rumford to Prejepscot Dam). Dye-cloud centroid traveltimes ranged from approximately 120 hours at high discharge to 410 hours at flows approaching 95 percentile duration. Longitudinal dispersion coeficients ranged from 21.3 to 76.7 square meters per second. In the 37.2 kilometer unsteady flow reach from Gulf Island Dam to Prejepscot Dam, the concept of mass flow versus time was applied to relate centroid traveltime to average discharge at five sites. This information was used to develop traveltime versus discharge relationships, traveltime versus distance relationships, and longitudinal dispersion coefficients. In Gulf Island Pond, a 70.4 million cubic meter impoundment, three complete dye clouds were traced. The range of observed centroid traveltime through the pound was 110 hours at a mean discharge of 84 cubic meters per second to 260 hours at 59 cubic meters per second. Traveltimes are dependent upon reservoir stratification and mixing as well as discharge. During 1981, inflowing dye-tagged water at 19.0 and 19.5 degrees Celsius was observed to seek its own temperature density level during movement along the thalweg. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri834232","usgsCitation":"Parker, G., Westerman, G., Hunt, G., and Morrill, G., 1983, Time of travel and dispersion study in the Androscoggin River basin, Maine: U.S. Geological Survey Water-Resources Investigations Report 83-4232, vii, 135 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri834232.","productDescription":"vii, 135 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":157894,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4232/report-thumb.jpg"},{"id":54543,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4232/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4c6c","contributors":{"authors":[{"text":"Parker, G.W.","contributorId":100374,"corporation":false,"usgs":true,"family":"Parker","given":"G.W.","email":"","affiliations":[],"preferred":false,"id":195121,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Westerman, G.S.","contributorId":22387,"corporation":false,"usgs":true,"family":"Westerman","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":195119,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hunt, G.S.","contributorId":20360,"corporation":false,"usgs":true,"family":"Hunt","given":"G.S.","email":"","affiliations":[],"preferred":false,"id":195118,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Morrill, G.L.","contributorId":89175,"corporation":false,"usgs":true,"family":"Morrill","given":"G.L.","email":"","affiliations":[],"preferred":false,"id":195120,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":41962,"text":"ofr83653 - 1983 - Aeromagnetic map of the Eureka and Saline valleys area, California and Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:05:05","indexId":"ofr83653","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1983","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":"83-653","title":"Aeromagnetic map of the Eureka and Saline valleys area, California and Nevada","language":"ENGLISH","doi":"10.3133/ofr83653","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1983, Aeromagnetic map of the Eureka and Saline valleys area, California and Nevada: U.S. Geological Survey Open-File Report 83-653, 1 map :photocopy ;62 x 36 cm., https://doi.org/10.3133/ofr83653.","productDescription":"1 map :photocopy ;62 x 36 cm.","costCenters":[],"links":[{"id":136663,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":79722,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1983/0653/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afce4b07f02db69667c","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":530734,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ]}