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Mississippi; Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:11:00","indexId":"ofr8614","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-14","title":"Land use and land cover and associated maps for Helena, Arkansas; Mississippi; Tennessee","language":"ENGLISH","doi":"10.3133/ofr8614","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Helena, Arkansas; Mississippi; Tennessee: U.S. Geological Survey Open-File Report 86-14, maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm., https://doi.org/10.3133/ofr8614.","productDescription":"maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm.","costCenters":[],"links":[{"id":169005,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b10e3","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":531242,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43609,"text":"ofr81866 - 1986 - Land use and land cover and associated maps for Grangeville, Oregon; 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The Sacramento and San Joaquin Rivers and many interconnecting sloughs meandered back and forth across the tidelands, frequently overflowing their banks. Approximately 1 ,100 miles of levees were constructed to form about 60 tracts or islands that protect these lands from periodic flooding. The levees were constructed of sand, silt, and peat dredged from the channel bottom and are subject to erosion and failure. Owing to compaction, oxidation of the peat, and other related conditions, the islands are subsiding at rates of up to 0.25 ft/yr. The altitude of the land surface of the islands is often below sea level and below the surface water level in the channel. This condition causes stresses that may contribute to high groundwater levels and levee failure. The U.S. Army Corps of Engineers requested that the U.S. Geological Survey install and maintain continuous recorders to monitor water levels in each of four wells. 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Nebraska","interactions":[],"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr824","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"82-4","title":"Land use and land cover and associated maps for Torrington, Wyoming; Nebraska","language":"ENGLISH","doi":"10.3133/ofr824","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Torrington, Wyoming; Nebraska: U.S. Geological Survey Open-File Report 82-4, maps ;45 x 67 cm., https://doi.org/10.3133/ofr824.","productDescription":"maps ;45 x 67 cm.","costCenters":[],"links":[{"id":172916,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aec41","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":531447,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":43939,"text":"ofr8617 - 1986 - Land use and land cover and associated maps for Russellville, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:11:05","indexId":"ofr8617","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-17","title":"Land use and land cover and associated maps for Russellville, Arkansas","language":"ENGLISH","doi":"10.3133/ofr8617","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Land use and land cover and associated maps for Russellville, Arkansas: U.S. Geological Survey Open-File Report 86-17, maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm., https://doi.org/10.3133/ofr8617.","productDescription":"maps :photocopy ;56 x 92 cm., on sheet 76 x 107 cm.","costCenters":[],"links":[{"id":168852,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b25e4b07f02db6af466","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":531487,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44121,"text":"ofr85746 - 1986 - USSR oil and gas map; geologic evaluation of potential for exploration and development","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"ofr85746","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-746","title":"USSR oil and gas map; geologic evaluation of potential for exploration and development","language":"ENGLISH","doi":"10.3133/ofr85746","issn":"ma","usgsCitation":"Grace, J., 1986, USSR oil and gas map; geologic evaluation of potential for exploration and development: U.S. Geological Survey Open-File Report 85-746, 1 map :photocopy ;55 x 84 cm., on sheet 62 x 90 cm., https://doi.org/10.3133/ofr85746.","productDescription":"1 map :photocopy ;55 x 84 cm., on sheet 62 x 90 cm.","costCenters":[],"links":[{"id":162425,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81503,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1985/0746/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a26e4b07f02db60f884","contributors":{"authors":[{"text":"Grace, John D. (compiler)","contributorId":104544,"corporation":false,"usgs":true,"family":"Grace","given":"John D.","suffix":"(compiler)","affiliations":[],"preferred":false,"id":229189,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44407,"text":"wri864183 - 1986 - Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985","interactions":[],"lastModifiedDate":"2022-02-22T21:54:39.615731","indexId":"wri864183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4183","title":"Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985","docAbstract":"The potentiometric surface map of the Floridan aquifer system in the northwest Florida Water Management District depicts the level to which water rose in tightly cased wells that tap the Floridan aquifer system in May 1985. The surface was mapped by determining the altitude of water levels in a network of wells and is represented on maps by contours that connect points of equal altitude. The northwest Florida Water Management District consists of about 12,000 sq mi, including all or part of 16 counties in northwest Florida. The Florida aquifer system is the principal source of freshwater for north Florida.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864183","usgsCitation":"Rosenau, J.C., and Meadows, P.E., 1986, Potentiometric surface of the Floridan aquifer system in the Northwest Florida Water Management District, May 1985: U.S. Geological Survey Water-Resources Investigations Report 86-4183, 1 Plate: 36.00 × 23.81 inches, https://doi.org/10.3133/wri864183.","productDescription":"1 Plate: 36.00 × 23.81 inches","costCenters":[],"links":[{"id":172931,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":396288,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36606.htm"},{"id":81695,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4183/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","otherGeospatial":"Northwest Florida Water Management District","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -88.1982421875,\n 29.611670115197377\n ],\n [\n -83.8916015625,\n 29.611670115197377\n ],\n [\n -83.8916015625,\n 31.840232667909365\n ],\n [\n -88.1982421875,\n 31.840232667909365\n ],\n [\n -88.1982421875,\n 29.611670115197377\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682f49","contributors":{"authors":[{"text":"Rosenau, Jack C.","contributorId":88719,"corporation":false,"usgs":true,"family":"Rosenau","given":"Jack","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":229715,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Meadows, Paul E.","contributorId":101631,"corporation":false,"usgs":true,"family":"Meadows","given":"Paul","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229716,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44410,"text":"wri864201 - 1986 - Ground-water availability in the eastern part of the Lake Ontario Basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864201","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4201","title":"Ground-water availability in the eastern part of the Lake Ontario Basin, New York","docAbstract":"A set of three maps show surficial geology, significant unconsolidated aquifers and well yield, and selected well locations for the Lake Ontario basin, New York. In the low areas , glaciers and wave action of former high-level lakes deposited permeable sand and gravel to form aquifers that yield more than 10 gal/min of water to wells. Small quantities of water (less than 2 gal/min) can be pumped from dug wells that top till and fine lake-sediment deposits. (USGS)","language":"ENGLISH","doi":"10.3133/wri864201","usgsCitation":"Miller, T.S., 1986, Ground-water availability in the eastern part of the Lake Ontario Basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4201, 3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm., https://doi.org/10.3133/wri864201.","productDescription":"3 maps ; 66 x 66 cm., on sheets 76 x 76 cm. and 76 x 96 cm., folded in envelope 33 x 25 cm.","costCenters":[],"links":[{"id":173688,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81704,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81705,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81706,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4201/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d355","contributors":{"authors":[{"text":"Miller, Todd S. tsmiller@usgs.gov","contributorId":1190,"corporation":false,"usgs":true,"family":"Miller","given":"Todd","email":"tsmiller@usgs.gov","middleInitial":"S.","affiliations":[{"id":474,"text":"New York Water Science Center","active":true,"usgs":true}],"preferred":true,"id":229719,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44420,"text":"wri864082 - 1986 - Altitude of basement surface in the central coastal plain area of North Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864082","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4082","title":"Altitude of basement surface in the central coastal plain area of North Carolina","docAbstract":"The altitude of the basement surface in the central Coastal Plain of North Carolina ranges from 140 ft above sea level in Wayne County near the Fall Line to 2,400 ft below sea level near the coast in Beaufort County. The slope increases to the east from about 20 ft/mi at the fall line to about 70 ft/mi at the eastern edge of the study area. The irregular nature of the basement surface is demonstrated by: (1) the variable altitudes of the basement surface in the western portion of the study area; (2) the protruding granite/gneiss rock body at a quarry near the Town of Fountain, Pitt County; and (3) the flattening of the basement surface slope observed near the Jones County and Craven County border. Basement rock types in this study area include granite, granite gneiss, metavolcanic, and metasedimentary rocks of Precambrian to Paleozoic age.","language":"ENGLISH","doi":"10.3133/wri864082","usgsCitation":"Lyke, W.L., and Winner, M.D., 1986, Altitude of basement surface in the central coastal plain area of North Carolina: U.S. Geological Survey Water-Resources Investigations Report 86-4082, 1 map and 1 data sheet ; 66 x 84 cm., on sheet 87 x 91 cm. and 57 x 91 cm., folded in envelope 30 x 24 cm., https://doi.org/10.3133/wri864082.","productDescription":"1 map and 1 data sheet ; 66 x 84 cm., on sheet 87 x 91 cm. and 57 x 91 cm., folded in envelope 30 x 24 cm.","costCenters":[],"links":[{"id":173113,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81718,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4082/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81719,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4082/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adde4b07f02db686a74","contributors":{"authors":[{"text":"Lyke, William L.","contributorId":38616,"corporation":false,"usgs":true,"family":"Lyke","given":"William","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229733,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Winner, M. D. Jr.","contributorId":51766,"corporation":false,"usgs":true,"family":"Winner","given":"M.","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229734,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44421,"text":"wri864084 - 1986 - Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864084","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4084","title":"Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985","docAbstract":"Aquifers in the Tertiary Sparta and Memphis Sands are a major source of water supply for much of eastern and south-central Arkansas. Major withdrawals occur from the aquifer for industrial and public supply, with generally lesser but locally significant amounts withdrawn for agricultural uses. Water level data from wells tapping the artesian aquifer in the Sparta and Memphis Sands indicate steadily declining water levels in some areas where relatively large withdrawals occur. In addition, a simulation of water levels using projected withdrawals to the year 1990 indicated increasing water level declines in the aquifer. Because of the potential quantity and quality problems, the continual monitoring of water levels in the aquifer in the Sparta and Memphis Sands is essential for proper aquifer management and the continuation of the use of the aquifer as a major source of water for much of eastern and south-central Arkansas. The U.S. Geological Survey with the cooperation of the Arkansas Geological Commission has been monitoring water levels in the aquifer in the Sparta and Memphis Sands annually throughout the aquifer 's extent within the State of Arkansas. This report, prepared in cooperation with the Arkansas Geological Commission and the Arkansas Soil and Water Conservation Commission interprets water level data through hydrologic maps of the potentiometric surface and water level changes. The potentiometric surface map is based on water levels collected in the spring of 1985. The water level change map is based on a comparison of water levels collected in the spring of 1980 and 1985. This report includes the Sparta Sand and most of the Memphis Sand aquifer within the State of Arkansas. Little or no data are available in the northeastern part of the State where limited withdrawals from the aquifer occur. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864084","usgsCitation":"Edds, J., and Fitzpatrick, D., 1986, Maps showing altitude of the potentiometric surface and changes in water levels in the aquifer in the Sparta and Memphis Sands in eastern Arkansas, spring 1985: U.S. Geological Survey Water-Resources Investigations Report 86-4084, 1 over-sized sheet, https://doi.org/10.3133/wri864084.","productDescription":"1 over-sized sheet","costCenters":[],"links":[{"id":173196,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81720,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4084/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db60461f","contributors":{"authors":[{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229736,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fitzpatrick, D. J.","contributorId":33313,"corporation":false,"usgs":true,"family":"Fitzpatrick","given":"D. J.","affiliations":[],"preferred":false,"id":229735,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44424,"text":"wri864118 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Providence-Ripley aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864118","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4118","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Providence-Ripley aquifer in Alabama, fall 1982","language":"ENGLISH","doi":"10.3133/wri864118","usgsCitation":"Williams, J.S., Planert, M., and DeJarnette, S.S., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Providence-Ripley aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4118, map : col. ; 53 x 34 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864118.","productDescription":" map : col. ; 53 x 34 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173198,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81723,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4118/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68278a","contributors":{"authors":[{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229739,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":229741,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229740,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":44425,"text":"wri864119 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864119","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4119","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982","docAbstract":"The U.S. Geological Survey began a nationwide program in 1978, termed Regional Aquifer-System Analysis (RASA), to study a number of the major aquifer systems that provide a significant part of the country 's water supply. One of the aquifer systems chosen for study was the thick and extensive sequence of sands for Cretaceous and early Tertiary age that underlies the Coastal Plain of the southeastern United States. This system, which extends from Mississippi eastward to South Carolina, is called the Southeastern Coastal Plain aquifer system. It can be divided geohydrologically into several separate aquifers. This map, one of a series that portray the potentiometric surface, groundwater withdrawal, and recharge areas for the aquifers in Alabama that are included in the regional system, deals with the Nanafalia-Clayton aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864119","usgsCitation":"Williams, J.S., DeJarnette, S.S., and Planert, M., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Nanafalia-Clayton aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4119, 1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864119.","productDescription":"1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173785,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81724,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4119/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db682635","contributors":{"authors":[{"text":"Williams, John S. johnw@usgs.gov","contributorId":329,"corporation":false,"usgs":true,"family":"Williams","given":"John","email":"johnw@usgs.gov","middleInitial":"S.","affiliations":[],"preferred":true,"id":229742,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeJarnette, Sydney S.","contributorId":13947,"corporation":false,"usgs":true,"family":"DeJarnette","given":"Sydney","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229743,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Planert, Michael","contributorId":56659,"corporation":false,"usgs":true,"family":"Planert","given":"Michael","email":"","affiliations":[],"preferred":false,"id":229744,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ]}