{"pageNumber":"2122","pageRowStart":"53025","pageSize":"25","recordCount":68919,"records":[{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","interactions":[{"subject":{"id":8871,"text":"ofr78556I - 1982 - Drainage areas of surface water bodies of central Maine coastal river basins","indexId":"ofr78556I","publicationYear":"1982","noYear":false,"chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins"},"predicate":"IS_PART_OF","object":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"id":1}],"isPartOf":{"id":7104,"text":"ofr78556 - 1978 - Drainage areas in Maine","indexId":"ofr78556","publicationYear":"1978","noYear":false,"title":"Drainage areas in Maine"},"lastModifiedDate":"2026-03-06T17:41:50.444588","indexId":"ofr78556I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"78-556","chapter":"I","title":"Drainage areas of surface water bodies of central Maine coastal river basins","docAbstract":"<p>The report contains drainage-area values for: lakes and ponds included in the MIDAS (Maine Informational Display Analysis System) File 906-Z, streams that drain an area greater than 25 square miles, dam sites, and locations where hydrologic data are available. Supplemental information includes State and Federal location systems used to identify these lake and stream sites.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr78556I","collaboration":"Prepared in cooperation with the Maine Department of Environmental Protection","usgsCitation":"Fontaine, R.A., 1982, Drainage areas of surface water bodies of central Maine coastal river basins: U.S. Geological Survey Open-File Report 78-556, v, 27 p., https://doi.org/10.3133/ofr78556I.","productDescription":"v, 27 p.","costCenters":[],"links":[{"id":422920,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":142628,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1978/0556-i/report-thumb.jpg"}],"country":"United States","state":"Maine","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -70.14536238431826,\n              44.57917477028707\n            ],\n            [\n              -70.14536238431826,\n              43.6956341707274\n            ],\n            [\n              -68.91970281136494,\n              43.6956341707274\n            ],\n            [\n              -68.91970281136494,\n              44.57917477028707\n            ],\n            [\n              -70.14536238431826,\n              44.57917477028707\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db699dcc","contributors":{"authors":[{"text":"Fontaine, Richard A. rfontain@usgs.gov","contributorId":2379,"corporation":false,"usgs":true,"family":"Fontaine","given":"Richard","email":"rfontain@usgs.gov","middleInitial":"A.","affiliations":[],"preferred":true,"id":158466,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9881,"text":"ofr82307 - 1982 - Hydrotectonics; principles and relevance","interactions":[],"lastModifiedDate":"2012-02-02T00:06:10","indexId":"ofr82307","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-307","title":"Hydrotectonics; principles and relevance","docAbstract":"Hydrotectonics combines the principles of hydraulics and rock mechanics. The hypothesis assumes that: (1) no faults are truly planar, (2) opposing noncongruent wavy wallrock surfaces form chambers and bottlenecks along the fault, and (3) most thrusting occurs beneath the water table. These physical constraints permit the following dynamics. \r\n\r\nShear displacement accompanying faulting must constantly change the volume of each chamber. Addition of ground water liquefies dry fault breccia to a heavy incompressible viscous muddy breccia I call fault slurry. When the volume of a chamber along a thrust fault decreases faster than its fault slurry can escape laterally, overpressurized slurry is hydraulically injected into the base of near-vertical fractures in the otherwise impervious overriding plate. Breccia pipes commonly form where such fissures intersect. \r\n\r\nAlternating decrease and increase in volume of the chamber subjects this injection slurry to reversible surges that not only raft and abrade huge clasts sporadically spalled from the walls of the conduit but also act as a forceful hydraulic ram which periodically widens the conduit and extends its top. If the pipe perforates a petroleum reservoir, leaking hydrocarbons float to its top. \r\n\r\nSudden faulting may generate a powerful water hammer that can be amplified at some distal narrow ends of the anastomosing plumbing system, where the shock may produce shatter cones. If vented on the Earth's surface, the muddy breccia, now called extrusion slurry, forms a mud volcano. \r\n\r\nThis hypothesis suggests that many highly disturbed features presently attributed to such catastrophic processes as subsurface explosions or meteorite impacts are due to the rheology of tectonic slurry in an intermittently reactivated pressure-relief tube rooted in a powerful reciprocating hydrotectonic pump activated by a long-lived deep-seated thrust fault.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82307","usgsCitation":"Kopf, R.W., 1982, Hydrotectonics; principles and relevance: U.S. Geological Survey Open-File Report 82-307, 30 p., ill. ;28 cm., https://doi.org/10.3133/ofr82307.","productDescription":"30 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140947,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0307/report-thumb.jpg"},{"id":37669,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0307/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c928","contributors":{"authors":[{"text":"Kopf, R. W.","contributorId":69544,"corporation":false,"usgs":true,"family":"Kopf","given":"R.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":160450,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44256,"text":"wri811102 - 1982 - Total hardness of water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States","interactions":[],"lastModifiedDate":"2022-04-21T21:17:50.337364","indexId":"wri811102","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-1102","title":"Total hardness of water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States","docAbstract":"<p>No abstract available.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri811102","usgsCitation":"Sprinkle, C.L., 1982, Total hardness of water from the upper permeable zone of the Tertiary limestone aquifer system, southeastern United States: U.S. Geological Survey Water-Resources Investigations Report 81-1102, 1 Plate: 34.78 x 44.40 inches, https://doi.org/10.3133/wri811102.","productDescription":"1 Plate: 34.78 x 44.40 inches","costCenters":[],"links":[{"id":399472,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_11886.htm"},{"id":366137,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1981/1102/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":168136,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/1102/report-thumb.jpg"}],"scale":"1000000","country":"United States","state":"Alabama, Florida, Georgia","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -87.323,\n              24.512\n            ],\n            [\n              -80,\n              24.512\n            ],\n            [\n              -80,\n              33.054\n            ],\n            [\n              -87.323,\n              33.054\n            ],\n            [\n              -87.323,\n              24.512\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629a7e","contributors":{"authors":[{"text":"Sprinkle, Craig L.","contributorId":41802,"corporation":false,"usgs":true,"family":"Sprinkle","given":"Craig","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229427,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":9550,"text":"ofr82514 - 1982 - Results of an aquifer test near Lynndyl, Utah","interactions":[],"lastModifiedDate":"2017-09-01T15:05:38","indexId":"ofr82514","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-514","title":"Results of an aquifer test near Lynndyl, Utah","docAbstract":"<p>An aquifer test was conducted near Lynndyl, Utah, to determine the hydraulic characteristics of a deep artesian aquifer and its associated confining bed. A well completed in the aquifer was pulped continuously for 25 days and measurements of drawdown and recovery were made in 34 observation wells located within a 10-mile radius of the pumped well. Data from the tests were analyzed using the Hantush modified and Neuman and Witherspoon ratio methods for leaky confined aquifers in which the storage of water in the confining beds was taken into account.</p><p>The aquifer transmissivity was calculated to be 12,700 feet squared per day, and the storage coefficient was 6.4 x 10<sup>-5</sup>. Calculated average vertical hydraulic conductivity of the confining bed was about 6 x 10<sup>-3</sup> foot per day with the specific storage of the confining bed calculated to be 5.4 x 10<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>-6</sup></span> per foot.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Salt Lake City, UT","doi":"10.3133/ofr82514","collaboration":"Prepared  in  cooperation  with  the Utah Department of Natural Resources and Energy, Division of Water Rights","usgsCitation":"Holmes, W.F., and Wilberg, D.E., 1982, Results of an aquifer test near Lynndyl, Utah: U.S. Geological Survey Open-File Report 82-514, Report: 17 p.; Plate: 12.96 in. x 14.24 in., https://doi.org/10.3133/ofr82514.","productDescription":"Report: 17 p.; Plate: 12.96 in. x 14.24 in.","numberOfPages":"15","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":141683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0514/report-thumb.jpg"},{"id":37279,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0514/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":37280,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0514/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","city":"Lynndyl","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604828","contributors":{"authors":[{"text":"Holmes, Walter F.","contributorId":31737,"corporation":false,"usgs":true,"family":"Holmes","given":"Walter","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":159875,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wilberg, Dale E.","contributorId":101275,"corporation":false,"usgs":true,"family":"Wilberg","given":"Dale","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":159876,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":9508,"text":"ofr82733 - 1982 - A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","interactions":[],"lastModifiedDate":"2012-02-02T00:06:11","indexId":"ofr82733","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-733","title":"A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment","docAbstract":"Monastery Beach, Carmel, California is a pocket beach that sits within 200 m of the head of Carmel Submarine Canyon. Coarse to very coarse sand covers both the beach and adjacent shelf; in the latter area incoming waves have shaped the sand into large oscillation ripples. The accessibility of this area and a variable wave climate produce a unique opportunity to study large-scale coarse-grained ripples in a high-energy environment. These ripples, which only occur in very coarse sand, form under the intense, wave-generated currents that exist during storm conditions. Once formed, these ripples do not significantly change under lower energy waves. On three separate occasions scuba divers measured ripples and collected sand samples from ripple crests near fixed reference stakes along three transects. Ripple wavelength and grain size decreased with an increase in water depth. Sediment sorting was best closest to the surf zone and poorest at the rim of Carmel Canyon. Cobbles and gravel observed in ripple troughs represent lag deposits. \r\n\r\nCarmel Canyon refracts waves approaching Monastery Beach such that wave energy is focused towards the northern and southern portions of the beach, leaving the central part of the beach lower in energy. This energy distribution causes spatial variations in the ripples and grain sizes with the shortest wavelengths and smallest grain sizes being in the central part of the shelf.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82733","usgsCitation":"Hirschaut, D., and Dingler, J., 1982, A field study of large-scale oscillation ripples in a very coarse-grained, high-energy marine environment: U.S. Geological Survey Open-File Report 82-733, 35 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82733.","productDescription":"35 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":140996,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0733/report-thumb.jpg"},{"id":37225,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0733/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aebb3","contributors":{"authors":[{"text":"Hirschaut, D.W.","contributorId":43761,"corporation":false,"usgs":true,"family":"Hirschaut","given":"D.W.","email":"","affiliations":[],"preferred":false,"id":159806,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dingler, J.R.","contributorId":64247,"corporation":false,"usgs":true,"family":"Dingler","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":159807,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":43930,"text":"ofr82245 - 1982 - Land use and land cover and associated maps for Rice Lake, Wisconsin","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr82245","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-245","title":"Land use and land cover and associated maps for Rice Lake, Wisconsin","language":"ENGLISH","doi":"10.3133/ofr82245","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Rice Lake, Wisconsin: U.S. Geological Survey Open-File Report 82-245, maps :photocopy ;45 x 65 cm., https://doi.org/10.3133/ofr82245.","productDescription":"maps :photocopy ;45 x 65 cm.","costCenters":[],"links":[{"id":168483,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5d8","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":531478,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8946,"text":"ofr82431 - 1982 - Ground-water withdrawals and changes in water levels in the Houston District, Texas","interactions":[],"lastModifiedDate":"2016-08-11T14:49:21","indexId":"ofr82431","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-431","title":"Ground-water withdrawals and changes in water levels in the Houston District, Texas","docAbstract":"<p>During 1975-79, total withdrawals of ground water in the Houston district decreased by 9.7 percent. This percentage represents a decrease from 505 million gallons per day (22.1 cubic meters per second) during 1975, to 456 million gallons per day (20.0 cubic meters per second) during 1979. The decrease resulted from an increased use of surface water that became available from Lake Livingston on the Trinity River during late 1976. During 1975-79, withdrawals of ground water decreased in the Pasadena, Katy, Baytown-La Porte, Johnson Space Center, Texas City, and Alta Loma areas but increased in the Houston area. The decreased withdrawals in the Katy area resulted partly from a small decrease in the acreage of rice planted, but mostly from a decrease in water needed for irrigation during 1979. The pumping of ground water increased in the Houston area because of the growth in population.</p>\n<p>From spring 1975 to spring 1980, water levels rose in the southeastern one-half of the district and declined in the northwestern one-half. The maximum rise of water levels in wells in the Chicot aquifer was 110 feet (33.5 meters); the maximum rise in wells in the Evangeline aquifer was 150 feet (45.7 meters). The maximum decline of water levels in wells in the Chicot aquifer was 60 feet (18.3 meters); the maximum decline in wells in the Evangeline aquifer was 70 feet (21.3 meters).</p>\n<p>No significant changes occurred in the chloride concentration in water from wells in the Alta Loma area during 1975-79. The concentration of chloride in water from a well completed in the middle part of the Chicot aquifer at Hitchcock is increasing, probably because of updip migration of the freshwater-saltwater interface.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Austin, TX","doi":"10.3133/ofr82431","usgsCitation":"Gabrysch, R., 1982, Ground-water withdrawals and changes in water levels in the Houston District, Texas: U.S. Geological Survey Open-File Report 82-431, Report: vi, 39 p.; 10 Plates, https://doi.org/10.3133/ofr82431.","productDescription":"Report: vi, 39 p.; 10 Plates","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":36564,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36565,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36566,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36567,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36568,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36569,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36570,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36571,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36572,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36573,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0431/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36574,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0431/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141122,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0431/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cbe4b07f02db543a1b","contributors":{"authors":[{"text":"Gabrysch, R.K.","contributorId":105691,"corporation":false,"usgs":true,"family":"Gabrysch","given":"R.K.","affiliations":[],"preferred":false,"id":158604,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27999,"text":"wri824074 - 1982 - Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri824074","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4074","title":"Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas","docAbstract":"Strippable reserves of Mulberry coal underlie an area of approximately 300 square miles of Miami, Linn, and Bourbon Counties of eastern Kansas. Although subject to State reclamation law, current and projected strip mining of this relatively thin coal seam could alter and hydrologic environment of the study area. Drained by the Marais des Cygnes and Little Osage Rivers and their tributaries, this area is characterized by low relief and moderately impermeable soils. Streamflows are poorly sustained by ground-water discharge and fluctuate widely due to climatic extremes and usage of surface-water supplies. Because ground-water supplies are generally unreliable in quantity and quality, surface water is used to meet most water requirements in the study area. Primary used of surface waters are for domestic supplies, maintenance of wildlife and recreational areas, and cooling needs at LaCygne Power Plant. The prevailing chemical type of the natural streamflow is calcium bicarbonate, with concentrations of dissolved solids generally less than 500 milligrams per liter and pH near neutral. Additional streamflow and water-quality data are needed to evaluate the premining characteristics of and the anticipated changes in the hydrologic environment as strip mining proceeds within the study area. A network of data-collection stations and a sampling scheme have been established to acquire this additional information. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, WRD,","doi":"10.3133/wri824074","usgsCitation":"Kenny, J.F., Bevans, H., and Diaz, A., 1982, Physical and hydrologic environments of the Mulberry coal reserves in eastern Kansas: U.S. Geological Survey Water-Resources Investigations Report 82-4074, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824074.","productDescription":"50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":122828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4074/report-thumb.jpg"},{"id":56826,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4074/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db685c0f","contributors":{"authors":[{"text":"Kenny, J. F.","contributorId":100378,"corporation":false,"usgs":true,"family":"Kenny","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":199042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bevans, H.E.","contributorId":102892,"corporation":false,"usgs":true,"family":"Bevans","given":"H.E.","email":"","affiliations":[],"preferred":false,"id":199043,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Diaz, A.M.","contributorId":27084,"corporation":false,"usgs":true,"family":"Diaz","given":"A.M.","email":"","affiliations":[],"preferred":false,"id":199041,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":43931,"text":"ofr823 - 1982 - Land use and land cover and associated maps for Ritzville, Washington","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr823","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-3","title":"Land use and land cover and associated maps for Ritzville, Washington","language":"ENGLISH","doi":"10.3133/ofr823","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Land use and land cover and associated maps for Ritzville, Washington: U.S. Geological Survey Open-File Report 82-3, maps ;45 x 61 cm., https://doi.org/10.3133/ofr823.","productDescription":"maps ;45 x 61 cm.","costCenters":[],"links":[{"id":168484,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af5a3","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":531479,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":20718,"text":"ofr82107 - 1982 - Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah","interactions":[],"lastModifiedDate":"2021-11-22T21:41:59.4496","indexId":"ofr82107","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-107","title":"Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah","docAbstract":"<p>The Green River-Moab area encompasses about 7,800 square kilometers or about 25 percent of the Paradox basin. The entire Paradox basin is a part of the Colorado Plateaus that is underlain by a thick sequence of evaporite (salt) beds of Pennsylvanian age. The rock units that underlie the area have been grouped into hydrogeologic units based on their water-transmitting ability. Confining beds consist of evaporite beds of mostly salt, and over- lying and underlying thick sequences of rocks with minimal permeability; above and below these confining beds are aquifers. The upper Mesozoic sand- stone aquifer, probably is the most permeable hydrogeologic unit of the area and is the subject of this investigation. The principal component of ground- water outflow from this aquifer probably is subsurface flow to regional streams (the Green and Colorado Rivers) and is about 100 million cubic meters per year. All other components of outflow are relatively small. The average annual recharge to the aquifer is about 130 million cubic meters, of which about 20 million cubic meters is from local precipitation. For the lower aquifer, all recharge and discharge probably is by subsurface flow and was not estimated.</p><p>The aquifers are generally isolated from the evaporite beds by the bounding confining beds; as a result, most ground water has little if any contact with the evaporites. Brines are present in the confining beds, but solution of beds o£ salt probably is very slow in most parts of the area. No brine discharges' have been identified.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82107","collaboration":"Prepared in cooperaiton with the U.S. Department of Energy","usgsCitation":"Rush, F., Whitfield, M., and Hart, I.M., 1982, Regional hydrology of the Green River-Moab area, northwestern Paradox basin, Utah: U.S. Geological Survey Open-File Report 82-107, Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches, https://doi.org/10.3133/ofr82107.","productDescription":"Report: vii, 86 p.; Table: 2 Plates: 26.00 in. x 28.00 inches","numberOfPages":"92","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":392017,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13639.htm"},{"id":20448,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-2.pdf","text":"Plate 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20447,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-1.pdf","text":"Plate 1","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Map showing generalized hydrogeology of the Green River-Moab area, Northwestern Paradox Basin, Utah"},{"id":20449,"rank":402,"type":{"id":27,"text":"Table"},"url":"https://pubs.usgs.gov/of/1982/0107/plate-3.pdf","text":"Table 2","linkFileType":{"id":1,"text":"pdf"},"linkHelpText":"Rock and hydrogeologic units in the Green River-Moab area and vicinity"},{"id":153242,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0107/report-thumb.jpg"},{"id":50276,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0107/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","otherGeospatial":"Green River - Moab area, Paradox Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.25,\n              38\n            ],\n            [\n              -110.5,\n              38\n            ],\n            [\n              -110.5,\n              39.283\n            ],\n            [\n              -109.25,\n              39.283\n            ],\n            [\n              -109.25,\n              38\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5fe4b07f02db634869","contributors":{"authors":[{"text":"Rush, F. E.","contributorId":56234,"corporation":false,"usgs":true,"family":"Rush","given":"F. E.","affiliations":[],"preferred":false,"id":183122,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whitfield, M.S.","contributorId":69547,"corporation":false,"usgs":true,"family":"Whitfield","given":"M.S.","email":"","affiliations":[],"preferred":false,"id":183123,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Hart, I. M.","contributorId":24806,"corporation":false,"usgs":true,"family":"Hart","given":"I.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":183121,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":9366,"text":"ofr821060 - 1982 - Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:06:00","indexId":"ofr821060","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-1060","title":"Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas","docAbstract":"In a preliminary survey, Crassostrea virginica from areas of the Corpus Christi Bay system of Texas show significant concentrations of Cd, Cu, Pb, and Zn in their tissues and shells; concentrations of these same metals in associated sediments are also high in certain areas of the bay system. Zn and Cd concentrations in tissue show a high negative correlation to each other, whereas Zn and Pb in tissue and shell show a high positive correlation to one another. Sediment contents of Pb and Zn best reflect tissue values of the heavy metals; sediment concentrations of Cd and Cu show a poor inverse correlation to tissue concentrations. Some possible factors influencing these correlations are suspended-sediment type, physiological changes, water quality, and Ca intake.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr821060","usgsCitation":"Harrison, G., and Martin, E., 1982, Heavy-metal contamination of Crassostrea virginica and associated sediments of the Corpus Christi Bay system, Texas: U.S. Geological Survey Open-File Report 82-1060, 18 p., ill. ;28 cm., https://doi.org/10.3133/ofr821060.","productDescription":"18 p., ill. ;28 cm.","costCenters":[],"links":[{"id":140877,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/1060/report-thumb.jpg"},{"id":37077,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/1060/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db6671d7","contributors":{"authors":[{"text":"Harrison, G.","contributorId":94302,"corporation":false,"usgs":true,"family":"Harrison","given":"G.","email":"","affiliations":[],"preferred":false,"id":159552,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, E.A.","contributorId":44148,"corporation":false,"usgs":true,"family":"Martin","given":"E.A.","email":"","affiliations":[],"preferred":false,"id":159551,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":42106,"text":"ofr82449 - 1982 - Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965","interactions":[],"lastModifiedDate":"2012-02-02T00:11:11","indexId":"ofr82449","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-449","title":"Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965","docAbstract":"The High Plains aquifer in Kansas is a part of a regional system that extends South Dakota to Texas. The aquifer in Kansas underlies an area of 31,000 square miles in the western and south-central part. This aquifer is a hydraulically connected assemblage of unconsolidated water-bearing deposits of Tertiary and Quaternary age. Maps published at a scale of 1:500,000 show the altitude and configuration of the water table in Kansas during 1965. Groundwater moved from higher altitudes in the western part of the High Plains to lower altitudes in the eastern part at a average rate of 10 ft/mi. The upgradient flexure of water table contours along some of the valleys indicates that groundwater was discharged to the streams in those areas. (USGS)","language":"ENGLISH","doi":"10.3133/ofr82449","usgsCitation":"Pabst, M.E., and Stullken, L.E., 1982, Altitude and configuration of the water table in the High Plains Aquifer in Kansas, 1965: U.S. Geological Survey Open-File Report 82-449, 1 map :photocopy ;66 x 87 cm., on sheet 85 x 113 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/ofr82449.","productDescription":"1 map :photocopy ;66 x 87 cm., on sheet 85 x 113 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":176702,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":20565,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0449/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686aec","contributors":{"authors":[{"text":"Pabst, Marilyn E.","contributorId":25566,"corporation":false,"usgs":true,"family":"Pabst","given":"Marilyn","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225948,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Stullken, Lloyd E.","contributorId":60609,"corporation":false,"usgs":true,"family":"Stullken","given":"Lloyd","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":225949,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30236,"text":"wri8119 - 1982 - Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:55","indexId":"wri8119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-19","title":"Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado","docAbstract":"Analysis of major and trace constituents in streams flowing through six semiarid watersheds indicates that the stream chemistry is characterized by saturation with respect to common carbonate minerals (calcium, magnesium, iron, manganese, and lead). The solubility of the carbonate minerals may be a major control on the absolute and relative concentrations of calcium, magnesium, bicarbonate, iron, manganese, and lead; however, other mechanisms probably control the concentrations of cadmium and zinc. Statistical analyses indicate that the mean concentrations of the major ions in the two climatic areas studied are significantly (P=0.05) different from one another, with larger mean concentrations in the more arid area. Trace-metal concentrations were similar from one area to another and indistinguishable from site to site (P=0.05) for lead, cadmium, and zinc. Linear regressions of major ion concentration to specific conductance are similar in both areas for sodium, bicarbonate, sulfate, and chloride. Results of the study may be useful in providing a first approximation of stream chemistry in other watersheds with the same geologic setting, determining watersheds with similar geochemical controls, and determining future changes in stream chemistry in the watersheds studied. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri8119","usgsCitation":"Turk, J.T., and Parker, R.S., 1982, Water-quality characteristics of six small, semiarid watersheds in the Green River coal region of Colorado: U.S. Geological Survey Water-Resources Investigations Report 81-19, iv, 96 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri8119.","productDescription":"iv, 96 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":159804,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1981/0019/report-thumb.jpg"},{"id":59011,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0019/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adbe4b07f02db6859f7","contributors":{"authors":[{"text":"Turk, John T.","contributorId":53363,"corporation":false,"usgs":true,"family":"Turk","given":"John","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":202908,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Parker, Randolph S.","contributorId":58638,"corporation":false,"usgs":true,"family":"Parker","given":"Randolph","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202909,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30408,"text":"wri824044 - 1982 - Flood of June 13-15, 1981, in the Blanchard River basin, northwestern Ohio","interactions":[],"lastModifiedDate":"2012-02-02T00:08:58","indexId":"wri824044","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4044","title":"Flood of June 13-15, 1981, in the Blanchard River basin, northwestern Ohio","docAbstract":"The flood of June 13-15, 1981, in the Blanchard River basin in northwestern Ohio caused major damage in Findlay, Ottawa, and adjacent rural areas. Approximately 25 percent of Findlay and 55 percent of Ottawa were flooded. Estimated crop damage was $12 million in Hancock Country, $7 million in Wyandot Country, and $3 million in Putnam Country.\r\n\r\nDuring the flood, the maximum gage height of the Blanchard River at the U.S. Geological Survey gaging station near Findlay was 17.43 feet, gage datum. This was 0.67 foot higher than the previous peak of 16.76 feet, February 11, 1959. The corresponding peak discharge, 13,000 cubic feet per second, was estimated to have a recurrence interval of 50 years. Recurrence intervals of peak flows at other locations on the Blanchard River and on tributary streams were estimated to range from 25 to more than 100 years.","language":"ENGLISH","publisher":"Water Resources Division, U.S. Geological Survey,","doi":"10.3133/wri824044","usgsCitation":"Webber, E., 1982, Flood of June 13-15, 1981, in the Blanchard River basin, northwestern Ohio: U.S. Geological Survey Water-Resources Investigations Report 82-4044, iv, 35 p. :ill., map ;28 cm., https://doi.org/10.3133/wri824044.","productDescription":"iv, 35 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":123878,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4044/report-thumb.jpg"},{"id":59177,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4044/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6676a3","contributors":{"authors":[{"text":"Webber, E.E.","contributorId":18373,"corporation":false,"usgs":true,"family":"Webber","given":"E.E.","email":"","affiliations":[],"preferred":false,"id":203198,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":55526,"text":"wdrLA821 - 1982 - Water resources data, Louisiana, water year 1982: Volume 1. Central and northern Louisiana","interactions":[],"lastModifiedDate":"2025-08-18T16:19:58.690118","indexId":"wdrLA821","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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-82-1","title":"Water resources data, Louisiana, water year 1982: Volume 1. Central and northern Louisiana","docAbstract":"<p>Water resources data for the 1982 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 77 gaging stations (including stage for 65 of these stations); stage only for 64 gaging stations and 9 lakes; contents for 1 reservoir; water quality for 104 surface-water stations (including 31gaging stations) 20 miscellaneous sites, and 8 lakes, and 223 wells; and water levels for 526 observation wells. Also included are data for 209 cres-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. Records for a few pertinent stations in bordering states are also included in this report. 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.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrLA821","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., 1982, Water resources data, Louisiana, water year 1982: Volume 1. Central and northern Louisiana: U.S. Geological Survey Water Data Report LA-82-1, x, 422 p., https://doi.org/10.3133/wdrLA821.","productDescription":"x, 422 p.","costCenters":[],"links":[{"id":181499,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1982/la-82-1/report-thumb.jpg"},{"id":494259,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1982/la-82-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f6e4b07f02db5f1358","contributors":{"authors":[{"text":"Carlson, D.D.","contributorId":10816,"corporation":false,"usgs":true,"family":"Carlson","given":"D.D.","email":"","affiliations":[],"preferred":false,"id":253635,"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":253638,"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":253637,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Stuart, C.G.","contributorId":58644,"corporation":false,"usgs":true,"family":"Stuart","given":"C.G.","email":"","affiliations":[],"preferred":false,"id":253636,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":8538,"text":"ofr82362 - 1982 - Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","interactions":[],"lastModifiedDate":"2012-02-02T00:06:15","indexId":"ofr82362","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-362","title":"Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81","docAbstract":"Test wells and low-flow investigations in the Eagle River valley , Alaska, were used to evaluate the feasibility of developing ground water for a public supply. Aquifers capable of supplying large yield wells were not indicated in any of the drilling areas. The data include: results of low-flow seepage investigations at 22 river sites; geologic materials logs of eight test wells; water-quality data from two observation wells, two springs, and two river sites; and water level and temperature information for the observation wells and streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82362","usgsCitation":"Deeter, G., and George, R., 1982, Hydrologic data from test wells and low-flow investigations in the middle reach of the Eagle River valley, Alaska; 1980-81: U.S. Geological Survey Open-File Report 82-362, iii, 16 p., ill., maps ;28 cm., https://doi.org/10.3133/ofr82362.","productDescription":"iii, 16 p., ill., maps ;28 cm.","costCenters":[],"links":[{"id":141694,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0362/report-thumb.jpg"},{"id":36117,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0362/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa7e4b07f02db66712e","contributors":{"authors":[{"text":"Deeter, Gary","contributorId":60216,"corporation":false,"usgs":true,"family":"Deeter","given":"Gary","email":"","affiliations":[],"preferred":false,"id":157901,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"George, R.S.","contributorId":12854,"corporation":false,"usgs":true,"family":"George","given":"R.S.","email":"","affiliations":[],"preferred":false,"id":157900,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":30206,"text":"wri824062 - 1982 - Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.","interactions":[],"lastModifiedDate":"2022-01-11T20:12:39.281543","indexId":"wri824062","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4062","title":"Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.","docAbstract":"A digital computer flow-routing model was developed for the Potomac River in order to determine the downstream effects of flow releases from the Bloomington and Savage River Reservoirs. Both reservoirs are located above Luke, Maryland approximately 230 miles upstream from Washington, D. C. The downstream effects of reservoir releases were determined by using the unit-response method of flow routing implemented by a diffusion analogy. Results are in the form of unit response coefficients which are used to route flows downstream from Luke. A 24-hour sustained reservoir release input at Luke will result in 35 percent of the flow arriving at Washington, D.C., during the 4th day after the beginning of the release, followed by 61 percent and 4 percent arriving on the 5th and 6th days, respectively. For a 7-day sustained reservoir release, 47 percent of the flow will arrive during the 1st week, and 53 percent will arrive the 2d week. Two methods were used to estimate the amount of water that goes into channel storage between Luke and Washington, D.C., during sustained reservoir releases. Analysis of the flow-routing results indicates channel storage is equivalent to the volume of water releases over a 3.7-day period. Using channel geometry relationships, that volume is equal to 3.2 days ' release. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri824062","usgsCitation":"Trombley, T.J., 1982, Downstream effects of reservoir releases to the Potomac River from Luke, Maryland, to Washington, D.C.: U.S. Geological Survey Water-Resources Investigations Report 82-4062, vi, 41 p., https://doi.org/10.3133/wri824062.","productDescription":"vi, 41 p.","costCenters":[],"links":[{"id":394207,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35580.htm"},{"id":58995,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4062/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123501,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4062/report-thumb.jpg"}],"country":"United States","state":"Maryland, Washington D.C.","otherGeospatial":"Potomac River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.376220703125,\n              38.79690830348427\n            ],\n            [\n              -76.5966796875,\n              38.79690830348427\n            ],\n            [\n              -76.5966796875,\n              39.715638134796336\n            ],\n            [\n              -79.376220703125,\n              39.715638134796336\n            ],\n            [\n              -79.376220703125,\n              38.79690830348427\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db629db7","contributors":{"authors":[{"text":"Trombley, T. J.","contributorId":75161,"corporation":false,"usgs":true,"family":"Trombley","given":"T.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":202858,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":65479,"text":"i1337 - 1982 - Controlled photomosaic of the Eridania Southeast Quadrangle of Mars","interactions":[],"lastModifiedDate":"2012-02-02T00:13:12","indexId":"i1337","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":320,"text":"IMAP","code":"I","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1337","subseriesTitle":"NONE","title":"Controlled photomosaic of the Eridania Southeast Quadrangle of Mars","language":"ENGLISH","doi":"10.3133/i1337","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1982, Controlled photomosaic of the Eridania Southeast Quadrangle of Mars: U.S. Geological Survey IMAP 1337, 1 remote sensing image ;52 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/i1337.","productDescription":"1 remote sensing image ;52 x 59 cm., on sheet 86 x 66 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":114957,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/imap/1337/report.pdf","size":"27","linkFileType":{"id":1,"text":"pdf"}},{"id":114958,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/imap/1337/plate-1.pdf","size":"7665","linkFileType":{"id":1,"text":"pdf"}},{"id":189929,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/imap/1337/report-thumb.jpg"}],"scale":"2000000","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688bc2","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":533866,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8541,"text":"ofr8215 - 1982 - South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","interactions":[],"lastModifiedDate":"2022-09-19T22:20:37.299269","indexId":"ofr8215","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-15","title":"South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980","docAbstract":"<p>The search for oil and gas on the Outer Continental Shelf (OCS) in the South Atlantic Region began in 1960, when geophysical surveys of the area were initiated. In 1977, a Continental Offshore Stratigraphic Test (COST) well was drilled in the Southeast Georgia Embayment. In March 1978, the first lease sale, Sale 43, was held, resulting in the leasing of 43 tracts. Approximately a year later, in May 1979, the first exploratory drilling began, and by February 1980, six exploratory wells had been drilled by four companies. Hydrocarbons were not found in any of these wells.</p><p>Lease Sale 56, the second lease sale in the South Atlantic Region, was held in August 1981. The sale resulted in the leasing of 47 tracts. Most of the leased tracts are in deep water along the Continental Slope off North Carolina. To date, no drilling has occurred on these tracts, but it is likely that two wells will be drilled or will be in the process of being drilled by the end of 1982. Reoffering Sale RS-2 is scheduled for July 1982, and it will include tracts offered in Lease Sale 56 that were not awarded leases. Lease Sale 78 is scheduled to be held in July 1983.</p><p>The most recent (March 1982) estimates of risked resources for leased lands in the South Atlantic OCS are 27 million barrels of oil and 120 billion cubic feet of gas.</p><p>To date, onshore impacts resulting from OCS exploration have been minimal, and they were associated with Lease Sale 43 exploratory activities. Tenneco, using existing facilities, established a support base in Savannah, Georgia; Getty, Transco, and Exxon used a support base established for them by the city of Brunswick, Georgia. The port at Morehead City, North Carolina, is expected to provide the onshore facilities for exploration in the near future on Lease Sale 56 tracts. Arrangements for the use of these facilities are currently being negotiated.</p><p>In June 1981, the South Atlantic Regional Technical Working Group prepared a Regional Transportation Management Plan for the South Atlantic OCS. The plan is principally an integration of regulatory frameworks, policies, and plans that are applicable to pipeline siting from each of the South Atlantic coastal States and Federal agencies with jurisdiction in the area.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr8215","collaboration":"Prepared for the U.S. Department of the Interior, Minerals Management Service, in cooperation with the U.S. Geological Survey","usgsCitation":"Deis, J.L., Kurz, F.N., and Porter, E.O., 1982, South Atlantic summary report 2: A revision of Outer Continental Shelf oil and gas activities in the South Atlantic (U.S.) and their onshore impacts, a summary report, July 1980: U.S. Geological Survey Open-File Report 82-15, viii, 50 p., https://doi.org/10.3133/ofr8215.","productDescription":"viii, 50 p.","costCenters":[],"links":[{"id":407021,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0015/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":141696,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0015/report-thumb.jpg"}],"country":"United States","otherGeospatial":"Outer Continental Shelf, South Atlantic","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -81.298828125,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              25.48295117535531\n            ],\n            [\n              -76.46484375,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              36.66841891894786\n            ],\n            [\n              -81.298828125,\n              25.48295117535531\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e7510","contributors":{"authors":[{"text":"Deis, Jeffrey L.","contributorId":10423,"corporation":false,"usgs":true,"family":"Deis","given":"Jeffrey","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":157905,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kurz, Frederick N.","contributorId":47785,"corporation":false,"usgs":true,"family":"Kurz","given":"Frederick","email":"","middleInitial":"N.","affiliations":[],"preferred":false,"id":157906,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Porter, Elizabeth O.","contributorId":104491,"corporation":false,"usgs":true,"family":"Porter","given":"Elizabeth","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":157907,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":29812,"text":"wri824000 - 1982 - Ground-water appraisal of the Pine Bush area, Albany County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri824000","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-4000","title":"Ground-water appraisal of the Pine Bush area, Albany County, New York","docAbstract":"The 32-square-mile central part of the Pine Bush was studied to determine the availability of ground water in the surficial sand and to assess the quality of the water, especially with respect to phosphorous, nitrogen, and chloride. The surficial sand is from 5 to 150 feet thick and has a hydraulic conductivity of 68 feet per day. Recharge is solely by precipitation. Depth to water is about 10 feet but ranges from 5 to 20 feet locally. The water table and total precipitation have been declining since 1979. A computer model was used to simulate drawdowns that would be produced by pumping the aquifer at various rates. Results indicate that a single well could yield from 150 to 600 gallons per minute, depending on hydraulic conductivity, which was simulated at 25, 50, and 100 feet per day, allowing a maximum drawdown of 80% of total saturated thickness. Ground water contained low phosphorous (maximum of 0.04 mg). (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri824000","usgsCitation":"Snavely, D.S., 1982, Ground-water appraisal of the Pine Bush area, Albany County, New York: U.S. Geological Survey Water-Resources Investigations Report 82-4000, viii, 54 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri824000.","productDescription":"viii, 54 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":119750,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1982/4000/report-thumb.jpg"},{"id":58613,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1982/4000/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ab0e4b07f02db66d3b9","contributors":{"authors":[{"text":"Snavely, D. S.","contributorId":103692,"corporation":false,"usgs":true,"family":"Snavely","given":"D.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":202171,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8447,"text":"ofr82222 - 1982 - Uranium potential of the Burro Canyon Formation in western Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:06:05","indexId":"ofr82222","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-222","title":"Uranium potential of the Burro Canyon Formation in western Colorado","docAbstract":"The Burro Canyon Formation of Early Cretaceous age overlies the Morrison Formation (Late Jurassic) and underlies the Dakota Sandstone (Late Cretaceous) over most of southeastern Utah and southwestern Colorado. It consists mainly of alternating beds of fluvial sandstone and overbank mudstone with sandstone dominating in the lower part of the formation and mudstone in the upper part. At the outcrop, the sandstones in the formation exhibit almost all the characteristics that are considered favorable for the occurrence of sandstone-type uranium deposits, but only a few small deposits have been discovered in the Colorado-Utah area. The major deficiency of the Burro Canyon in these outcrop areas is the absence of a reductant such as carbonaceous debris, humic or humate materials, or pyrite. Reductants were probably removed during a period of extensive oxidation at the time of deposition and during a subsequent erosional episode prior to deposition of the Dakota Sandstone. \r\n\r\nThe formation reaches a lobate, inexactly located eastern margin that extends from near Meeker, Colorado, southward through the Piceance basin to near Aztec, New Mexico, in the northwestern part of the San Juan Basin. Along much of this distance, the formation is in the subsurface and has been penetrated by only a few drill holes. Along this eastern margin, the lobes project eastward where fluvial distributary streams built minor alluvial fans of relatively high-energy deposits out from the main axis of Burro Canyon stream deposition. The lower and distal reaches of these lobes may have survived the period of post depositional erosion and oxidation in a reduced condition because of low relief and the protection of a high water table. If so, the peripheral and distal parts of these lobes may have retained the precipitants necessary to form a uranium deposit. Two of the lobes extend into the southwest margin of the Piceance Basin and are considered the possible location of uranium deposits. Two additional lobes extend into the northwestern part of the San Juan Basin but have not been evaluated in this study.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr82222","usgsCitation":"Craig, L., 1982, Uranium potential of the Burro Canyon Formation in western Colorado: U.S. Geological Survey Open-File Report 82-222, 27 p., 4 over-size sheets, maps ;28 cm., https://doi.org/10.3133/ofr82222.","productDescription":"27 p., 4 over-size sheets, maps ;28 cm.","costCenters":[],"links":[{"id":140506,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0222/report-thumb.jpg"},{"id":36016,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36017,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36018,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36019,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1982/0222/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":36020,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0222/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db688016","contributors":{"authors":[{"text":"Craig, L.C.","contributorId":61419,"corporation":false,"usgs":true,"family":"Craig","given":"L.C.","email":"","affiliations":[],"preferred":false,"id":157731,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8127,"text":"ofr82905 - 1982 - Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling","interactions":[],"lastModifiedDate":"2022-06-27T20:38:26.898567","indexId":"ofr82905","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-905","title":"Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling","docAbstract":"The Tertiary limestone aquifer of the southeastern United States is a sequence of carbonate rocks that underlies all of Florida, south Georgia, and adjacent parts of Alabama and South Carolina. It is the principal source of municipal, industrial, and agricultural water supply in south Georgia and most of Florida. The aquifer, known as the Floridan aquifer in Florida and the principal artesian aquifer in Georgia, Alabama, and South Carolina, includes various carbonate units of Paleocene to early Miocene age that are hydraulically connected in varying degrees. Very locally, in the Brunswick, Ga., area, a thin sequence of rocks of Late Cretaceous age is part of the system. In general the aquifer consists of either one vertically continuous permeable zone or two major permeable zones separated by a less permeable unit of highly variable water-transmitting characteristics. Aquifer conditions range from unconfined to confined depending upon whether the clayey Miocene and younger rocks that form the upper confining unit have been removed by erosion.\r\n\r\nDigital model simulation shows that prior to development, most flow in the aquifer occurred in the unconfined and thinly confined areas of northwest and central Florida and southwest Georgia. Springs in these areas are visible evidence of major flow activity. Spring discharge to streams accounted for about 90 percent of the average predevelopment discharge from the regional aquifer. About 18,100 cubic feet per second left the limestone aquifer as spring flow, and 2,500 cubic feet per second discharged as diffuse upward leakage from the confined areas where the vertical head gradient was upward. Most of the 20,600 cubic feet per second recharge necessary to balance total discharge entered the limestone aquifer in the unconfined and thinly confined areas. Because the areas of greatest recharge before development were near the areas of highest discharge, flow paths were generally short. Much water went into and out of the limestone quickly. A very active shallow flow system at the expense of deep circulation has evolved in unconfined and sligptly confined spring areas. Transmissivities commonly exceed 1,000,000 feet squared per day.\r\n\r\nIn contrast, predevelopment flow in the aquifer in the tightly confined areas of southeast and coastal Georgia, far west Florida, and in south Florida was sluggish. In these areas the aquifer is overlain by several hundred feet of sand and clay, except for the outcrop areas along the updip limit of the aquifer. This thick overburden severely retards discharge from the aquifer, causing lethargic flow. Large-discharge springs are nonexistent. The south Florida and southeast Georgia segments of the flow system, which taken together occupy about 50 percent of the regional system, only accounted for slightly more than 3 percent of the predevelopment regional limestone discharge. Transmissivities are on the average lower (generally less than 250,000 feet squared per day) than those in areas of high-flow activity.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82905","usgsCitation":"Bush, P.W., 1982, Predevelopment flow in the Tertiary limestone aquifer, southeastern United States: A regional analysis from digital modeling: U.S. Geological Survey Open-File Report 82-905, v, 41 p., https://doi.org/10.3133/ofr82905.","productDescription":"v, 41 p.","costCenters":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"links":[{"id":35732,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0905/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":402563,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35647.htm","linkFileType":{"id":5,"text":"html"}},{"id":142050,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0905/report-thumb.jpg"}],"country":"United States","state":"Alabama, Florida, Georgia","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -89,24 ], [ -89,34 ], [ -80,34 ], [ -80,24 ], [ -89,24 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ea30","contributors":{"authors":[{"text":"Bush, Peter W.","contributorId":57820,"corporation":false,"usgs":true,"family":"Bush","given":"Peter","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":157192,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":8220,"text":"ofr82457 - 1982 - Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity","interactions":[],"lastModifiedDate":"2021-10-13T18:08:27.092236","indexId":"ofr82457","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-457","title":"Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity","docAbstract":"New evidence for a possible resurgent dome in the caldera related to eruption of the Bullfrog Member of the Crater Flat Tuff has been provided by recent drilling of a 762-meter (2,501-foot) hole in central Crater Flat. Although no new volcanic units were penetrated by the drill hole (USW-VH-1), the positive aeromagnetic anomaly in the vicinity of the drill hole appears to result in part from the unusually thick, densely welded tuff of the Bullfrog. Major units penetrated include alluvium, basalt of Crater Flat, Tiva Canyon and Topopah Spring Members of the Paintbrush Tuff, and Prow Pass and Bullfrog Members of the Crater Flat Tuff. \r\n\r\nIn addition, the drill hole provided the first subsurface hydrologic information for the area. The water table in the hole is at about 180 meters (600 feet), and the temperature gradient appears slightly higher than normal for the region.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr82457","usgsCitation":"Carr, W.J., 1982, Volcano-tectonic history of Crater Flat, southwestern Nevada, as suggested by new evidence from drill hole USW-VH-1 and vicinity: U.S. Geological Survey Open-File Report 82-457, ii, 25 p., https://doi.org/10.3133/ofr82457.","productDescription":"ii, 25 p.","costCenters":[],"links":[{"id":35850,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0457/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":390476,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_13731.htm"},{"id":141328,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0457/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Crater Flat","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -116.6340,\n              36.667\n            ],\n            [\n              -116.4780,\n              36.667\n            ],\n            [\n              -116.4780,\n              36.871\n            ],\n            [\n              -116.6340,\n              36.871\n            ],\n            [\n              -116.6340,\n              36.667\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0de4b07f02db5fd71b","contributors":{"authors":[{"text":"Carr, W. J.","contributorId":9245,"corporation":false,"usgs":true,"family":"Carr","given":"W.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":157364,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":30462,"text":"wri8169 - 1982 - Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","interactions":[],"lastModifiedDate":"2017-06-07T12:25:54","indexId":"wri8169","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"81-69","title":"Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980","docAbstract":"<p>Parts of the East Branch Mahoning Creek basin, a forested area of 29.6 square miles in west-central Pennsylvania, are disturbed by farming, surface mining, unpaved haul roads, eroding reclaimed areas, and logging. Streamflow was measured and water samples collected at a site upstream from the mouth from June 1979 to June 1980 during base flow and storm periods to evaluate sediment discharges. An additional site on a tributary draining mostly farmland was sampled from December 1979 to June 1980. Samples were analyzed for suspended sediment, turbidity, and specific conductance. Daily mean suspended-sediment concentrations and discharges were computed.</p>\n<p>From June 1979 to June 1980, 3,570 tons of suspended sediment was transported from the basin. This was an average yield of 121 tons per square mile per year. From December 1979 to June 1980, a tributary draining 2.21 square miles of a predominantly agricultural area discharged 328 tons of sediment which was 12 percent of the sediment load transported from the entire basin.</p>\n<p>Monthly sediment discharges averaged 298 tons ranged from 32 tons in July to 1,250 tons in March. The highest daily mean suspended-sediment concentration was 712 milligrams per liter on June 8, 1980. On that date, 267 tons of sediment was discharged from the basin.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri8169","collaboration":"Prepared in cooperation with the  Pennsylvania Department of Environmental Resources, Bureau of Mining and Reclamation","usgsCitation":"Wetzel, K.L., 1982, Sedimentation in the East Branch Mahoning Creek basin, Clearfield and Jefferson Counties, Pennsylvania, June 1979 to June 1980: U.S. Geological Survey Water-Resources Investigations Report 81-69, iv, 33 p., https://doi.org/10.3133/wri8169.","productDescription":"iv, 33 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":159817,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri8169.jpg"},{"id":318653,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1981/0069/report.pdf"}],"country":"United 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,{"id":7490,"text":"ofr82346 - 1982 - Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","interactions":[],"lastModifiedDate":"2017-09-02T09:55:54","indexId":"ofr82346","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1982","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":"82-346","title":"Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah","docAbstract":"<p>Six exploratory wells were drilled into the cap rock underlying Salt Valley, Utah, for geologic, geophysical, and hydrologic data to augment information obtained from three previous test wells. Drilling of three other test holes was abandoned due to caving and loss of drilling tools, Before reaching the zone of saturation; the upper 100 meters of cap rock is unsaturated. Within the saturated part of the cap rock, hydraulic heads generally decrease with depth and to the northwest in this part of the valley.</p><p>Hydraulic conductivity of the cap rock, as determined from pumping tests, ranged from 9.3 X 10<sup>-5</sup> to 2.06 X 10<span id=\"_mce_caret\" data-mce-bogus=\"true\"><sup>-1</sup></span> meters per day; as a result, groundwater flow rates in the cap rock are low. Water ranges from a calcium bicarbonate sulfate type on the western edge of the valley to a calcium magnesium sodium bicarbonate, sulfate, chloride type near the center of the valley. Carbon-14 specific activity for cap-rock water yielded an uncorrected age of about 17,000 to 26,000 years before present near the western edge of the valley and about 41,000 years before present near the center of the valley.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Denver, CO","doi":"10.3133/ofr82346","collaboration":"Prepared in cooperation with the U.S. Department of Energy","usgsCitation":"Wollitz, L.E., Thordarson, W., Whitfield, M.S., and Weir, J.E., 1982, Results of hydraulic tests in U.S. Department of Energy's wells DOE-4, 5, 6, 7, 8, and 9, Salt Valley, Grand County, Utah: U.S. Geological Survey Open-File Report 82-346, vii, 71 p., https://doi.org/10.3133/ofr82346.","productDescription":"vii, 71 p.","numberOfPages":"78","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":140454,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1982/0346/report-thumb.jpg"},{"id":34934,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1982/0346/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Utah","county":"Grand County","otherGeospatial":"Salt Valley","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9be4b07f02db65e092","contributors":{"authors":[{"text":"Wollitz, Leonard E.","contributorId":22340,"corporation":false,"usgs":true,"family":"Wollitz","given":"Leonard","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155857,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thordarson, William","contributorId":23539,"corporation":false,"usgs":true,"family":"Thordarson","given":"William","email":"","affiliations":[],"preferred":false,"id":155858,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Whitfield, Merrick S. Jr.","contributorId":67911,"corporation":false,"usgs":true,"family":"Whitfield","given":"Merrick","suffix":"Jr.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":155859,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Weir, James E. Jr.","contributorId":47419,"corporation":false,"usgs":true,"family":"Weir","given":"James","suffix":"Jr.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":155860,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
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