{"pageNumber":"4850","pageRowStart":"121225","pageSize":"25","recordCount":184582,"records":[{"id":28536,"text":"wri864072 - 1986 - Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","interactions":[],"lastModifiedDate":"2012-02-02T00:08:48","indexId":"wri864072","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":"86-4072","title":"Evaluation of the U.S. Geological Survey's gaging-station network in Illinois","docAbstract":"Data collected at 97 of the 176 gaging stations operated in Illinois during 1983 were used to describe rainfall-runoff processes, to monitor and forecast floods, and to monitor and regulate lake levels, discharge from reservoirs, or discharge of navigable streams. Stream-gaging stations on the Illinois River at Havana, East Branch Du Page River, and interior streams of the Mississippi River floodplain; peak-flow stations on small watersheds; and stage-only stations upstream from unsafe high-hazard dams should be considered for inclusion in future stream-gaging programs. The accuracy of regression models for peak-flow and 1-day mean flood-volume characteristics would not be considerably improved if the density of gaging stations and length of record at those gaging stations are increased. Model error masks tradeoffs between accuracy, density, and record length. The large number of streamflow records presently available is sufficient for fairly accurately determining most streamflow characteristics. The accuracy of streamflow records reported for stream gaging stations and peak-flow stations varies widely. The accuracy of streamflow records for 12 stream-gaging stations and 11 peak-flow stations is substantially less than the accuracy of records for the other 143 gaging stations considered. Based on an evaluation of relative worth, 26 gaging stations are candidates for some type of action if budgetary limitations so demand. A candidate stream-gaging stations could be operated during only part of a year, converted to a peak-flow station, or discontinued. Candidate peak-flow stations should be discontinued. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey, Water Resources Division,","doi":"10.3133/wri864072","usgsCitation":"Mades, D., and Oberg, K.A., 1986, Evaluation of the U.S. Geological Survey's gaging-station network in Illinois: U.S. Geological Survey Water-Resources Investigations Report 86-4072, vii, 88 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri864072.","productDescription":"vii, 88 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":124298,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4072/report-thumb.jpg"},{"id":57349,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4072/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa4c2","contributors":{"authors":[{"text":"Mades, D. M.","contributorId":40230,"corporation":false,"usgs":true,"family":"Mades","given":"D. M.","affiliations":[],"preferred":false,"id":199981,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Oberg, K. A.","contributorId":67553,"corporation":false,"usgs":true,"family":"Oberg","given":"K.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":199982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"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":"<p>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.</p>","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":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":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}]}}
,{"id":44426,"text":"wri864120 - 1986 - Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon aquifer in Alabama, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864120","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":"86-4120","title":"Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon 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 of 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. The map presented, one of a series that portray the potentiometric surface, groundwater withdrawals, and recharge areas for aquifers in Alabama that are included in the regional system, deals with the Lisbon aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864120","usgsCitation":"Williams, J.S., Planert, M., and DeJarnette, S.S., 1986, Potentiometric surface, ground-water withdrawals, and recharge area for the Lisbon aquifer in Alabama, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 86-4120, 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/wri864120.","productDescription":"1 map : col. ; 55 x 36 cm., on sheet 59 x 97 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173786,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81725,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4120/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db6811f6","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":229745,"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":229747,"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":229746,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44428,"text":"wri864147 - 1986 - Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"wri864147","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":"86-4147","title":"Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona","docAbstract":"The Salt River Valley is a major agricultural and metropolitan area in semiarid south-central Arizona. Groundwater in the permeable sedimentary deposits underlying the area is a major water supply for agricultural, municipal, and industrial users. Groundwater levels have declined as much as 400 ft in recent years. Management of the remaining groundwater resources and their protection from contamination will require knowledge of the hydrogeologic framework and the water-bearing characteristics of the sedimentary units in the groundwater system. The rocks in the eastern part of the Salt River Valley are divided into six units--crystalline rocks, extrusive rocks, red units, lower unit, middle unit, and upper unit. The crystalline and extrusive rocks underlie the basin and form virtually impermeable hydrologic boundaries. The red, lower, middle and upper sedimentary units contain most of the groundwater. The red unit contains usable quantities of ground water, principally near Scottsdale, where it yields as much as 1 ,000 gallons/min (gpm) of water to wells. The lower unit, which makes up the largest volume of sedimentary deposits, consists mostly of mudstone, clay, silt, and evaporite deposits that may be as much as 10,000 ft thick in the central part of the basin. Wells tapping the mudstone, clay, silt yield 50 (gpm) or less but the conglomerate and the sand and gravel may yield as much as 3,500 gpm. The middle unit is the principal water-bearing unit in the basin and consists mostly of silt, siltstone, and silty sand and gravel. The unit is as much as 1,000 ft thick in the central part of the basin and as much as 700 ft is saturated. The unit will yield as much as 1,000 gpm where the saturated thickness is at least 500 ft. Locally, north of Mesa, the unit yields as much as 4,000 gpm. The upper unit is gravel, sand, and silt and is saturated only in a small area in the southwestern part of the basin. Where saturated, the unit may yield as much as 4,500 gpm. The upper unit transmits recharge derived from sheet flow, from flood flow in ephemeral streams, and from irrigation to the water table. (Author 's abstract)","language":"ENGLISH","doi":"10.3133/wri864147","usgsCitation":"Laney, R., and Hahn, M.E., 1986, Hydrogeology of the eastern part of the Salt River Valley area, Maricopa and Pinal Counties, Arizona: U.S. Geological Survey Water-Resources Investigations Report 86-4147, 8 maps on 4 sheets ; sheets 97 x 86 cm. and smaller, folded in envelope 32 x 25 cm., https://doi.org/10.3133/wri864147.","productDescription":"8 maps on 4 sheets ; sheets 97 x 86 cm. and smaller, folded in envelope 32 x 25 cm.","costCenters":[],"links":[{"id":172360,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81729,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81730,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81727,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81728,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4147/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ee4b07f02db614e97","contributors":{"authors":[{"text":"Laney, R. L.","contributorId":83889,"corporation":false,"usgs":true,"family":"Laney","given":"R. L.","affiliations":[],"preferred":false,"id":229752,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hahn, Mary Ellen","contributorId":83188,"corporation":false,"usgs":true,"family":"Hahn","given":"Mary","email":"","middleInitial":"Ellen","affiliations":[],"preferred":false,"id":229751,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44431,"text":"wri864166 - 1986 - Quality of water resources of the Ouachita National Forest, Arkansas","interactions":[],"lastModifiedDate":"2012-02-02T00:10:32","indexId":"wri864166","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":"86-4166","title":"Quality of water resources of the Ouachita National Forest, Arkansas","docAbstract":"Surface water and groundwater quality was documented in the Ouachita National Forest by collecting surface water quality data at 15 points and groundwater quality data at 11 sites from April 1984 through August 1985. The data were compared to drinking water standards and the results are tabulated. Surface water in the Ouachita National Forest is relatively abundant. It is low in mineralization and chemically suitable for most uses with minimal treatment. Groundwater is relatively scarce. The low yields of wells limit the use of groundwater primarily to domestic use. The water is chemically suitable for most purposes but may require treatment for the removal of iron. (Peters-PTT)","language":"ENGLISH","doi":"10.3133/wri864166","usgsCitation":"Cole, E.F., and Morris, E.E., 1986, Quality of water resources of the Ouachita National Forest, Arkansas: U.S. Geological Survey Water-Resources Investigations Report 86-4166, 2 maps ; 26 x 43 cm. and 22 x 27 cm., on sheet 89 x 113 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864166.","productDescription":"2 maps ; 26 x 43 cm. and 22 x 27 cm., on sheet 89 x 113 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":172453,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81733,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4166/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8ae4b07f02db6515d1","contributors":{"authors":[{"text":"Cole, Elizabeth F.","contributorId":72449,"corporation":false,"usgs":true,"family":"Cole","given":"Elizabeth","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229756,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, E. E.","contributorId":93493,"corporation":false,"usgs":true,"family":"Morris","given":"E.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229757,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44433,"text":"wri854305 - 1986 - Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84","interactions":[],"lastModifiedDate":"2022-12-15T21:01:05.133802","indexId":"wri854305","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":"85-4305","title":"Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84","docAbstract":"Previous water level maps of shallow aquifers in the Powder River structural basin in Wyoming were based on water levels from wells completed in different stratigraphic intervals within thick sequences of sedimentary rocks. A potentiometric surface using water levels from a single aquifer had never been mapped throughout the basin. The sandstone aquifers in the Fort Union Formation of Paleocene age and the Wasatch Formation of Eocene age are discontinuous and lenticular, and do not extend even short distances. Coal aquifers are more continuous and the Wyodak-Anderson coal bed, in the Fort Union Formation, has been mapped in much of the Powder River structural basin in Wyoming. Water level altitudes in the Wyodak-Anderson coal bed and other stratigraphically equivalent coal beds were mapped to determine if they represent a continuous potentiometric surface in the Powder River structural basin. The potentiometric surface, except in the vicinity of the Wyodak mine east of Gillette, represents a premining condition as it was based on water level measurements made during 1973-84 that were not significantly affected by mining. The map was prepared in cooperation with the U.S. Bureau of Land Management. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854305","usgsCitation":"Daddow, P.B., 1986, Potentiometric-surface map of the Wyodak-Anderson coal bed, Powder River structural basin, Wyoming, 1973-84: U.S. Geological Survey Water-Resources Investigations Report 85-4305, 1 Plate: 41.93 × 35.61 inches, https://doi.org/10.3133/wri854305.","productDescription":"1 Plate: 41.93 × 35.61 inches","costCenters":[],"links":[{"id":173276,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":410576,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36439.htm","linkFileType":{"id":5,"text":"html"}},{"id":81734,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4305/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Wyoming","otherGeospatial":"Powder River structural basin, Wyodak-Anderson coal bed","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -107,\n              45\n            ],\n            [\n              -107,\n              43.317\n            ],\n            [\n              -105.094,\n              43.317\n            ],\n            [\n              -105.094,\n              45\n            ],\n            [\n              -107,\n              45\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db681e8b","contributors":{"authors":[{"text":"Daddow, Pamela B.","contributorId":7762,"corporation":false,"usgs":true,"family":"Daddow","given":"Pamela","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":229761,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44437,"text":"wri864010 - 1986 - Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864010","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":"86-4010","title":"Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system","docAbstract":"An investigation was conduced to define the configuration and hydrology of the rock surface upon which the sand aquifers and confining beds of the Southeastern Coastal Plain aquifer system were deposited. The base of the Southeastern Coastal Plain aquifer system consists of crystalline rocks, saprolite, Paleozoic rocks, Triassic sedimentary rocks (some of which are intruded by basalt), and Jurassic sedimentary rocks. The permeability of these rocks is extremely low and little exchange of water occurs upward to the overlying Cretaceous aquifers. Porosity values are in the range of 10% or less in some of the rocks, indicating little water is stored in them. The transmissivity values are extremely low, indicating very slow movement of water in these rocks. The small volume of water moving at a very slow rate has a long residence time and is usually mineralized to a greater degree than water in the more permeable overlying sediments. (Peters-PTT)","language":"ENGLISH","doi":"10.3133/wri864010","usgsCitation":"Wait, R.L., and Davis, M.E., 1986, Configuration and hydrology of the Pre-Cretaceous rocks underlying the southeastern Coastal Plain aquifer system: U.S. Geological Survey Water-Resources Investigations Report 86-4010, 1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864010.","productDescription":"1 map : col. ; 35 x 60 cm., on sheet 80 x 79 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173280,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4010/report-thumb.jpg"},{"id":81750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b13e4b07f02db6a3499","contributors":{"authors":[{"text":"Wait, Robert L.","contributorId":12839,"corporation":false,"usgs":true,"family":"Wait","given":"Robert","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229765,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Davis, Marvin E.","contributorId":36553,"corporation":false,"usgs":true,"family":"Davis","given":"Marvin","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229766,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44438,"text":"wri864014 - 1986 - Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864014","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":"86-4014","title":"Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984","docAbstract":"The Mississippi River Valley alluvial aquifer, is a major source of water for most of eastern Arkansas. Agriculture is largely dependent on the aquifer as approximately 3.3 billion gallon per day are withdrawn for that purpose. Much smaller withdrawals also occur for industrial, public supply, and domestic use. The purpose of the report is to illustrate, using the spring and fall potentiometric surface maps, the water levels in the alluvial aquifer under pre-pumping and post-pumping conditions, respectively, and to illustrate, using the depth-to-water and saturated thickness maps, the effect of heavy pumpage in the alluvial aquifer. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864014","usgsCitation":"Plafcan, M., and Edds, J., 1986, Water level and saturated thickness maps of the alluvial aquifer in eastern Arkansas, 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4014, 4 maps on 1 sheet : col. ; 78 x 46 cm. and smaller, sheet 98 x 107 cm., https://doi.org/10.3133/wri864014.","productDescription":"4 maps on 1 sheet : col. ; 78 x 46 cm. and smaller, sheet 98 x 107 cm.","costCenters":[],"links":[{"id":173366,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81751,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4014/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa12f","contributors":{"authors":[{"text":"Plafcan, Maria","contributorId":20338,"corporation":false,"usgs":true,"family":"Plafcan","given":"Maria","email":"","affiliations":[],"preferred":false,"id":229767,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Edds, Joe","contributorId":48532,"corporation":false,"usgs":true,"family":"Edds","given":"Joe","email":"","affiliations":[],"preferred":false,"id":229768,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44439,"text":"wri864033 - 1986 - Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota","interactions":[],"lastModifiedDate":"2022-02-18T22:25:36.58533","indexId":"wri864033","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":"86-4033","title":"Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota","docAbstract":"<p>Five aquifers in crystalline rocks of Archean and Proterozoic age in Minnesota include in descending order the North Shore Volcanic, Sioux Quartzite, Proterozoic metasedimentary, Biwabik Iron formation and undifferentiated Precambrian aquifers. The North Shore Volcanic aquifer generally yields &lt; 15 gal/min to wells from interflow sediments and fractures in the basaltic lava flows along the northern shore of Lake Superior and along the upper St. Croix River. Dissolved solids concentrations range from 91 to 74,300 mg/L, and the water is of several chemical types. The Sioux Quartzite aquifer yields from 1 to 450 gal/min to wells open to joints and fractures and loose sand zones in the predominantly pink orthoquartzite in southwestern Minnesota. Dissolved solids concentrations range from 237 mg/L in water from wells in outcrop areas to 2,300 mg/L from wells where the Sioux Quartzite aquifer underlies Cretaceous rocks or thick Des Moines drift. The water generally is a calcium sulfate type. The Proterozoic metasedimentary aquifer generally yields &lt; 20 gal/min to wells in weathered regolith and fractures in thin-bedded gray to black argillite in north-central Minnesota. Dissolved solids concentrations generally range from 126 to 340 mg/L, and the water is a calcium magnesium bicarbonate type. The Biwabik Iron formation aquifer yields 1,000 gal/min to wells in leached zones in the ferruginous chert and interbedded hematite and magnitite iron ore in north-central Minnesota. Dissolved solids range from 157 to 388 mg/L in water that is a calcium magnesium bicarbonate type. The undifferentiated Precambrian aquifer generally yields &lt; 25 gal/min to wells from fractures and the weathered regolith developed on a variety of crystalline-rock types. Wells have been developed in parts of the aquifer throughout the State except in the southeast where it is too deeply buried. Dissolved solids concentrations average &lt; 400 mg/L in central and northeastern Minnesota, but average about 700 mg/L in the northwest and 900 mg/L in the south west. The water is a calcium magnesium bicarbonate type in central and northeastern Minnesota and a variety of mixed water types in northwestern and Southwestern Minnesota.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864033","collaboration":"Prepared in cooperation with the U.S. Environmental Protection Agency","usgsCitation":"Anderson, H.W., 1986, Hydrogeologic and water-quality characteristics of crystalline-rock aquifers of Archean and Proterozoic age, Minnesota: U.S. Geological Survey Water-Resources Investigations Report 86-4033, 3 Plates: 42.08 x 30.11 inches or smaller, https://doi.org/10.3133/wri864033.","productDescription":"3 Plates: 42.08 x 30.11 inches or smaller","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science 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,{"id":44440,"text":"wri864040 - 1986 - Ground-water availability in the Black River Basin, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864040","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":"86-4040","title":"Ground-water availability in the Black River Basin, New York","docAbstract":"There are three maps in this set, which were prepared in 1966-68 as part of a study on the water resources of the Black River basin in cooperation with the New York State Department of Environmental Conservation. The data presented on the maps show well locations, well yield from bedrock aquifers, and well yield from unconsolidated aquifers. The well location map shows locations of all wells represented in the initial report. The well yields given on the bedrock aquifer map were recorrelated with the most recent New York State geologic maps; the well yields shown on the unconsolidated aquifer map are correlated with a surficial geology map of the area. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864040","usgsCitation":"Waller, R.M., 1986, Ground-water availability in the Black River Basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4040, 3 maps ; 65 x 100 cm., on sheets 76 x 104 cm., folded in envelope 33 x 26 cm., https://doi.org/10.3133/wri864040.","productDescription":"3 maps ; 65 x 100 cm., on sheets 76 x 104 cm., folded in envelope 33 x 26 cm.","costCenters":[],"links":[{"id":173473,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81755,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81756,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81757,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4040/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d37f","contributors":{"authors":[{"text":"Waller, Roger Milton","contributorId":22320,"corporation":false,"usgs":true,"family":"Waller","given":"Roger","email":"","middleInitial":"Milton","affiliations":[],"preferred":false,"id":229770,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44441,"text":"wri864041 - 1986 - Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York","interactions":[],"lastModifiedDate":"2022-04-06T18:25:17.387303","indexId":"wri864041","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":"86-4041","title":"Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York","docAbstract":"<p>New York State 's need to develop a groundwater management program for protection of its aquifers led in 1985 to a cooperative program between the U.S. Geological Survey and the New York State Department of Environmental Conservation (through regional planning agencies) to publish data from previous studies. The two maps presented are from original compilations done in a 1967 study. Sheet 1 depicts the surficial geology as mapped in 1967; sheet 2 shows the groundwater availability (well yield) throughout the basin. These maps are presented at 1:250 ,000 scale for compatibility with published maps of adjacent river basins.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864041","usgsCitation":"Frimpter, M.H., 1986, Surficial geology and ground-water availability in the Allegheny River basin and part of the Lake Erie basin, New York: U.S. Geological Survey Water-Resources Investigations Report 86-4041, 2 Plates: 30.19 × 20.31 inches and 30.82 × 20.40 inches, https://doi.org/10.3133/wri864041.","productDescription":"2 Plates: 30.19 × 20.31 inches and 30.82 × 20.40 inches","costCenters":[],"links":[{"id":173474,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81759,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4041/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81758,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4041/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":398249,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36505.htm"}],"scale":"250000","country":"United States","state":"New York","otherGeospatial":"Allegheny River basin, Lake Erie basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -79.749,\n              42\n            ],\n            [\n              -78,\n              42\n            ],\n            [\n              -78,\n              42.557\n            ],\n            [\n              -79.749,\n              42.557\n            ],\n            [\n              -79.749,\n              42\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae2e4b07f02db688c46","contributors":{"authors":[{"text":"Frimpter, Michael H.","contributorId":8074,"corporation":false,"usgs":true,"family":"Frimpter","given":"Michael","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229771,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44442,"text":"wri864046 - 1986 - Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984","interactions":[],"lastModifiedDate":"2023-03-13T19:56:15.075174","indexId":"wri864046","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":"86-4046","title":"Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864046","usgsCitation":"Whiteman, K.J., 1986, Ground-water levels in three basalt hydrologic units underlying the Columbia Plateau, Washington and Oregon, spring 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4046, 4 Plates: 36.62 x 35.41 inches or smaller, https://doi.org/10.3133/wri864046.","productDescription":"4 Plates: 36.62 x 35.41 inches or smaller","costCenters":[],"links":[{"id":173649,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":414040,"rank":6,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36510.htm","linkFileType":{"id":5,"text":"html"}},{"id":81763,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81762,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81761,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81760,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4046/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Oregon, Washington","otherGeospatial":"Columbia Plateau","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -121.633,\n              48.112\n            ],\n            [\n              -121.633,\n              44.817\n            ],\n            [\n              -116.367,\n              44.817\n            ],\n            [\n              -116.367,\n              48.112\n            ],\n            [\n              -121.633,\n              48.112\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aa8e4b07f02db6674be","contributors":{"authors":[{"text":"Whiteman, K. J.","contributorId":48147,"corporation":false,"usgs":true,"family":"Whiteman","given":"K.","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229772,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44443,"text":"wri864048 - 1986 - Ground-water availability in the Genesee River Basin, New York and Pennsylvania","interactions":[],"lastModifiedDate":"2012-02-02T00:10:26","indexId":"wri864048","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":"86-4048","title":"Ground-water availability in the Genesee River Basin, New York and Pennsylvania","docAbstract":"New York State 's need to develop a groundwater management strategy for the protection of its aquifers led, in 1985, to a cooperative program between the U.S. Geological Survey and the New York State Department of Environmental Conservation, through the Genesee/Finger Lakes Regional Planning Council, to publish basinwide groundwater availability maps. As a part of this program, several maps that had been compiled during the 1960s, were selected for publication through a grant between the State and several regional planning agencies. These maps depict the surficial geology and groundwater availability of the basin at 1:125,000 scale. Each map consists of two sheets; sheets 1 and 2 depict the groundwater availability and geology of the northern and southern parts of the basin, and sheets 3 and 4 depict well and test-hole locations within the northern and southern parts of the basin. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864048","usgsCitation":"Kammerer, J., and Hobba, W.A., 1986, Ground-water availability in the Genesee River Basin, New York and Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 86-4048, 2 maps on 4 sheets : col. ; sheets 76 x 97 cm. and 69 x 84 cm., folded in envelope 33 x 25 cm., https://doi.org/10.3133/wri864048.","productDescription":"2 maps on 4 sheets : col. ; sheets 76 x 97 cm. and 69 x 84 cm., folded in envelope 33 x 25 cm.","costCenters":[],"links":[{"id":173650,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81764,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81765,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81766,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81767,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4048/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d387","contributors":{"authors":[{"text":"Kammerer, John C.","contributorId":53815,"corporation":false,"usgs":true,"family":"Kammerer","given":"John C.","affiliations":[],"preferred":false,"id":229774,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hobba, William A. Jr.","contributorId":46076,"corporation":false,"usgs":true,"family":"Hobba","given":"William","suffix":"Jr.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":229773,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44444,"text":"wri864058 - 1986 - Altitude of the freshwater-saltwater interface in a regionally extensive coastal plain aquifer of Mississippi, Alabama, and Georgia","interactions":[],"lastModifiedDate":"2017-01-27T08:54:34","indexId":"wri864058","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":"86-4058","title":"Altitude of the freshwater-saltwater interface in a regionally extensive coastal plain aquifer of Mississippi, Alabama, and Georgia","docAbstract":"Geophysical well logs from over 150 oil test and water wells in Mississippi, Alabama, and Georgia were examined and calculations of the dissolved solids concentration in ground water were made using the spontaneous potential deflection as a measure of ionic activity. The values derived from these calculations were used to prepare a map showing the altitude relative to sea level at which the concentration of dissolved solids in the groundwater reached 10,000 mg/L within a regionally extensive aquifer in Mississippi, Alabama, and Georgia. A dissolved solids concentration of 10,000 mg/L is used to delineate the interface between moderately saline and saline water; 10,000 mg/L dissolved solids was designated to delineate the freshwater-saltwater interface. For a finite difference computer flow model being used this interface represents the location where horizontal flow of freshwater is greatly diminished. 10 ,000 mg/L also is the lower limit for dissolved solids concentrations for water in target zones for injection wells. This 10,000 mg/L dissolved solids line is of value as a water quality indicator; although water containing 3,000 to 10,000 mg/L or more of dissolved solids is too saline for agricultural use (upper limit approximately 3,000 mg/L), it may be useful for some industrial purposes. Waters containing dissolved solids concentrations &gt; 10,000 mg/L have little potential for any use involving human activities. 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adce4b07f02db6868a2","contributors":{"authors":[{"text":"Strickland, Donald J.","contributorId":106560,"corporation":false,"usgs":true,"family":"Strickland","given":"Donald","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229776,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mahon, Gary L. 0000-0002-7410-0261 glmahon@usgs.gov","orcid":"https://orcid.org/0000-0002-7410-0261","contributorId":270,"corporation":false,"usgs":true,"family":"Mahon","given":"Gary","email":"glmahon@usgs.gov","middleInitial":"L.","affiliations":[{"id":501,"text":"Office of Science Quality and Integrity","active":true,"usgs":true},{"id":566,"text":"Southeast Ecological Science Center","active":true,"usgs":true},{"id":17705,"text":"Wetland and Aquatic Research Center","active":true,"usgs":true}],"preferred":true,"id":229775,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44445,"text":"wri864059 - 1986 - Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","interactions":[],"lastModifiedDate":"2019-08-20T09:41:43","indexId":"wri864059","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":"86-4059","title":"Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980","docAbstract":"Generalized contours of the altitude of water levels in wells completed in the Catahoula aquifer in central Louisiana, are illustrated by this map. Most water level measurements used in compiling the map were made in 1980; however, in parts of the State where water levels from 1980 were unavailable and where evidence indicated little change in water level, some measurements from as early as 1961 and as late as 1982 were used. Groundwater levels in and near the outcrop areas fluctuate 2 ft or less yearly and no significant long-term declines have occurred. The slow downward trend in water level altitude since early 1976 may be caused by pumpage from the Catahoula aquifer by a rural water system approximately 3 miles away. Recharge to the Catahoula aquifer occurs by rainfall on the upland outcrop-subcrop areas. Saltwater occurs throughout the Catahoula aquifer downgradient from the outcrop area. The ' approximate limit of freshwater ' line on the map indicates the downgradient limit of water with a concentration of chloride &lt; 250 mg/L; the line was determined using water quality data and analysis of resistivity curves from geophysical well logs. Water from the Catahoula aquifer is used for municipal, industrial, and domestic purposes. Total pumpage from the aquifer in Louisiana was slightly over 1.1 million gallons/day in 1980. Local cones of depression result from pumpage just east of Anacoco in Vernon Parish and northwest of Jonesville in Catahoula Parish. (Lantz-PTT)","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri864059","usgsCitation":"Martin, A., and Whiteman, C.D., 1986, Generalized potentiometric surface of the Catahoula aquifer in central Louisiana, 1980: U.S. Geological Survey Water-Resources Investigations Report 86-4059, 1 Plate: 35.86 x 22.96 inches, https://doi.org/10.3133/wri864059.","productDescription":"1 Plate: 35.86 x 22.96 inches","costCenters":[],"links":[{"id":366594,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173742,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4059/report-thumb.jpg"}],"country":"United States","state":"Louisiana","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b24e4b07f02db6aecc1","contributors":{"authors":[{"text":"Martin, Angel Jr.","contributorId":42571,"corporation":false,"usgs":true,"family":"Martin","given":"Angel","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":229777,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Whiteman, Charles D. Jr.","contributorId":108081,"corporation":false,"usgs":true,"family":"Whiteman","given":"Charles","suffix":"Jr.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229778,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44446,"text":"wri864062 - 1986 - Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas","interactions":[],"lastModifiedDate":"2016-08-10T15:04:47","indexId":"wri864062","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":"86-4062","title":"Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas","docAbstract":"<p>The Edwards aquifer extends in a narrow belt from Bell County in the northeast to Kinney County in the southwest (index map) and provides water for at least nine counties in south-central Texas. Hydrologic boundaries divide the Edwards aquifer in the Austin area for which Barton Springs is the major discharge point. This part of the Edwards aquifer provides the municipal, industrial, domestic, and agricultural water supplies for about 30,000 people in the Austin area (southern Travis and northern Hays counties). Discharge from Barton Springs sustains streamflow at the mouth of Barton Creek and flows into Town Lake. Much of the land use within the outcrop area of the Edwards aquifer near Austin is rapidly changing from natural woodland and grassland to commercial and residential developments. Because urban development can result in a substantial degradation of the quality of water that recharges the aquifer, the extent of the recharge zone of the Edwards aquifer was delineated to provide information to the City of Austin for their use in formulating a plan for protecting and managing groundwater quality. The purpose of this report is to define and delineate the areal extent of the recharge zone of the Edwards aquifer in southern Travis and northern Hays Counties. The areal boundary of the recharge zone was determined by: (1) geologic mapping of the aquifer area; (2) interpretation of aerial photographs; (3) field verification of existing geologic maps; and (4) streamflow-loss studies.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864062","usgsCitation":"Slagle, D.L., Ardis, A.F., and Slade, R.M., 1986, Recharge zone of the Edwards aquifer hydrologically associated with Barton springs in the Austin area, Texas: U.S. Geological Survey Water-Resources Investigations Report 86-4062, 30.00 x 41.76 inches, https://doi.org/10.3133/wri864062.","productDescription":"30.00 x 41.76 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":173743,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri864062.PNG"},{"id":81769,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4062/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a221","contributors":{"authors":[{"text":"Slagle, Diana L.","contributorId":103730,"corporation":false,"usgs":true,"family":"Slagle","given":"Diana","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229781,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Ardis, Ann F.","contributorId":96672,"corporation":false,"usgs":true,"family":"Ardis","given":"Ann","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":229780,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Slade, Raymond M. Jr.","contributorId":46487,"corporation":false,"usgs":true,"family":"Slade","given":"Raymond","suffix":"Jr.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":229779,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44447,"text":"wri854144 - 1986 - Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida","interactions":[],"lastModifiedDate":"2022-01-04T20:10:19.899943","indexId":"wri854144","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":"85-4144","title":"Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida","docAbstract":"<p>No abstract available.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854144","usgsCitation":"Thagard, M.E., and Seaber, P.R., 1986, Location of potential ground-water quality monitoring wells, West Palm Beach 1° x 2° quadrangle, Florida: U.S. Geological Survey Water-Resources Investigations Report 85-4144, 1 Plates: 39.28 × 22.21 inches, https://doi.org/10.3133/wri854144.","productDescription":"1 Plates: 39.28 × 22.21 inches","costCenters":[],"links":[{"id":173744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":393874,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36307.htm"},{"id":81770,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4144/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Florida","otherGeospatial":"West Palm Beach 1° x 2° quadrangle","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -82,\n              26\n            ],\n            [\n              -80,\n              26\n            ],\n            [\n              -80,\n              27\n            ],\n            [\n              -82,\n              27\n            ],\n            [\n              -82,\n              26\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a69e4b07f02db63bf1e","contributors":{"authors":[{"text":"Thagard, Martha E.","contributorId":68315,"corporation":false,"usgs":true,"family":"Thagard","given":"Martha","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229783,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Seaber, Paul R.","contributorId":67492,"corporation":false,"usgs":true,"family":"Seaber","given":"Paul","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229782,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":44460,"text":"wri854037 - 1986 - Flood of September 12-13, 1982 in Gibson, Carroll, and Madison Counties, western Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"wri854037","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":"85-4037","title":"Flood of September 12-13, 1982 in Gibson, Carroll, and Madison Counties, western Tennessee","docAbstract":"Intense rainfall on September 12-13, 1982, caused severe local flooding along many streams in Gibson County in western Tennessee. The rainfall resulted from remnants of Hurricane Chris combining with a cool front moving across the western half of the State. A maximum 1-hr rainfall intensity of 3.3 in was recorded at Humboldt. Peak discharge exceeded the 100-yr flood on many small streams. The floods caused three deaths and about 15.3 million dollars damage to crops, roads and bridges, businesses, and residential areas. Long-time residents of Gibson County reported that stream stages have not been as high since at least 1922. (USGS)","language":"ENGLISH","doi":"10.3133/wri854037","usgsCitation":"Robbins, C.H., Gamble, C.R., and Bingham, R.H., 1986, Flood of September 12-13, 1982 in Gibson, Carroll, and Madison Counties, western Tennessee: U.S. Geological Survey Water-Resources Investigations Report 85-4037, 1 sheet, https://doi.org/10.3133/wri854037.","productDescription":"1 sheet","costCenters":[],"links":[{"id":123805,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_85_4037.jpg"},{"id":81781,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4037/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49f2e4b07f02db5eec7a","contributors":{"authors":[{"text":"Robbins, Clarence H.","contributorId":44159,"corporation":false,"usgs":true,"family":"Robbins","given":"Clarence","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229807,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gamble, Charles R.","contributorId":6822,"corporation":false,"usgs":true,"family":"Gamble","given":"Charles","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229806,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bingham, Roy H.","contributorId":56632,"corporation":false,"usgs":true,"family":"Bingham","given":"Roy","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":229808,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":44466,"text":"wri854059 - 1986 - Potentiometric map of the lower Wilcox aquifer in Mississippi, fall 1982","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"wri854059","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":"85-4059","title":"Potentiometric map of the lower Wilcox aquifer in Mississippi, fall 1982","docAbstract":"This potentiometric map is the second map of the lower Wilcox aquifer in a series of maps prepared by the U.S. Geological Survey in cooperation with the Mississippi Department of Natural Resources, Bureau of Land and Water Resources, delineating the potentiometric surface of the major aquifers in Mississippi. The potentiometric surface of the lower Wilcox aquifer slopes generally to the west away from the outcrop area and it is marked by a large groundwater cone of depression in the area of Tallahatchie, Quitman, and Panola Counties. Water levels in or near the outcrop of the lower Wilcox aquifer show little longterm change. Heavy withdrawals in the downdip area have caused water level declines of about 1 to 2 feet per year since 1979 in much of the confined part of the aquifer. These water level declines in the area of Tallahatchie, Quitman, and Panola Counties have resulted in a wider cone of depression since 1979. (USGS)","language":"ENGLISH","doi":"10.3133/wri854059","usgsCitation":"Darden, D., 1986, Potentiometric map of the lower Wilcox aquifer in Mississippi, fall 1982: U.S. Geological Survey Water-Resources Investigations Report 85-4059, 1 map : col. ; 77 x 42 cm., on sheet 97 x 71 cm., folded in envelope 30 x 23 cm., https://doi.org/10.3133/wri854059.","productDescription":"1 map : col. ; 77 x 42 cm., on sheet 97 x 71 cm., folded in envelope 30 x 23 cm.","costCenters":[],"links":[{"id":162150,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81798,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4059/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e2e4b07f02db5e4b0f","contributors":{"authors":[{"text":"Darden, Daphne","contributorId":12489,"corporation":false,"usgs":true,"family":"Darden","given":"Daphne","email":"","affiliations":[],"preferred":false,"id":229819,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44467,"text":"wri854091 - 1986 - Divisions of potential fracture permeability, based on distribution of structures and lineaments, in sedimentary rocks of the Rocky Mountains-High Plains region, Western United States","interactions":[],"lastModifiedDate":"2018-11-08T15:50:21","indexId":"wri854091","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":"85-4091","title":"Divisions of potential fracture permeability, based on distribution of structures and lineaments, in sedimentary rocks of the Rocky Mountains-High Plains region, Western United States","docAbstract":"<p>The principal map show geologic structures and lineaments that indicate fracture traces in sedimentary rocks in all or parts of Arizona, Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, Utah, and Wyoming.&nbsp; Fractures associated with geologic structures and lineaments may affect the potential fracture permeability of consolidated rocks.&nbsp; Divisions indicating differences in the potential fracture permeability are delineated on the map.<br></p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854091","usgsCitation":"Cooley, M.E., 1986, Divisions of potential fracture permeability, based on distribution of structures and lineaments, in sedimentary rocks of the Rocky Mountains-High Plains region, Western United States: U.S. Geological Survey Water-Resources Investigations Report 85-4091, 52.52 x 34.88 inches, https://doi.org/10.3133/wri854091.","productDescription":"52.52 x 34.88 inches","costCenters":[],"links":[{"id":162151,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4091/report-thumb.jpg"},{"id":359350,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4091/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Arizona, Colorado, Kansas, Nebraska, New Mexico, Oklahoma, South Dakota, Texas, Utah, Wyoming","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -114.08203125,\n              28.69058765425071\n            ],\n            [\n              -93.7353515625,\n              28.69058765425071\n            ],\n            [\n              -93.7353515625,\n              45.089035564831036\n            ],\n            [\n              -114.08203125,\n              45.089035564831036\n            ],\n            [\n              -114.08203125,\n              28.69058765425071\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a5ee4b07f02db633eac","contributors":{"authors":[{"text":"Cooley, Maurice E.","contributorId":8077,"corporation":false,"usgs":true,"family":"Cooley","given":"Maurice","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":229820,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":44468,"text":"wri854094 - 1986 - Geohydrology of the glacial-outwash aquifer in the Baldwinsville area, Seneca River, Onondaga County, New York","interactions":[],"lastModifiedDate":"2012-02-02T00:10:11","indexId":"wri854094","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":"85-4094","title":"Geohydrology of the glacial-outwash aquifer in the Baldwinsville area, Seneca River, Onondaga County, New York","docAbstract":"Seven sheets of map data comprise this geohydrologic report. Sheet 1, surficial geology, illustrates the distribution of: open water areas; artificial fill; made land; urban land; alluvial silt and sand; alluvial sand and gravel; peat, marl, muck and clay; lake silt and/or clay; delta sand and gravel; beach sand and gravel; outwash sand and gravel; ice contact sand and ground; thick till cover bedrock; and thin till over bedrock over the Baldwinsville Area. Sheet 2, geologic sections, shows the layering of the aforementioned components below the surface layer. Sheet 3 illustrates the water infiltration of soil zone. Sheet 4 depicts the aquifer thickness. Sheet 5 illustrates the potentiometric surface, and Sheet 6 the well yield. Finally, Sheet 7 shows the land use in the region, specifically: industrial and extractive; commercial and services; transportation; farmland; forestland; residential; open public land; and water and wetlands. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri854094","usgsCitation":"Pagano, T.S., Terry, D.B., and Ingram, A.W., 1986, Geohydrology of the glacial-outwash aquifer in the Baldwinsville area, Seneca River, Onondaga County, New York: U.S. Geological Survey Water-Resources Investigations Report 85-4094, 6 maps and 4 cross sections on 7 sheets ; 92 x 122 cm., on sheets 106 x 148 cm. and 92 x 96 cm., folded in envelope 40 x 30 cm., https://doi.org/10.3133/wri854094.","productDescription":"6 maps and 4 cross sections on 7 sheets ; 92 x 122 cm., on sheets 106 x 148 cm. and 92 x 96 cm., folded in envelope 40 x 30 cm.","costCenters":[],"links":[{"id":162262,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81799,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81800,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81801,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81802,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81803,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81804,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81805,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4094/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8857","contributors":{"authors":[{"text":"Pagano, Timothy S.","contributorId":9628,"corporation":false,"usgs":true,"family":"Pagano","given":"Timothy","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":229821,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Terry, David B.","contributorId":102045,"corporation":false,"usgs":true,"family":"Terry","given":"David","email":"","middleInitial":"B.","affiliations":[],"preferred":false,"id":229823,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Ingram, Arlynn W.","contributorId":10015,"corporation":false,"usgs":true,"family":"Ingram","given":"Arlynn","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":229822,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":59513,"text":"mf1338B - 1986 - Geochemical survey of the Little Frog Roadless Area, Polk County, Tennessee","interactions":[],"lastModifiedDate":"2018-10-25T09:56:47","indexId":"mf1338B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":325,"text":"Miscellaneous Field Studies Map","code":"MF","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1338","chapter":"B","title":"Geochemical survey of the Little Frog Roadless Area, Polk County, Tennessee","docAbstract":"<p>The Wilderness Act (Public Law 88-577, September 3, 1964) and related acts require the U.S. Geological Survey and the U.S. Bureau of Mines to survey certain areas on Federal lands to determine the mineral values, if any, that may be present.&nbsp; Results must be made available to the public and be submitted to the President and the Congress.&nbsp; This report presents the results of a geochemical survey of the Little Frog Roadless Area (08-277) in the Cherokee National Forest, Polk County, Tenn.&nbsp; The area was classified as a further planning area during the Second Roadless Area Review and Evaluation (RARE II) by the U.S. Forest Service, January 1979.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/mf1338B","usgsCitation":"Force, E.R., and Siems, D.F., 1986, Geochemical survey of the Little Frog Roadless Area, Polk County, Tennessee: U.S. Geological Survey Miscellaneous Field Studies Map 1338, 48.17 x 41.24 inches, https://doi.org/10.3133/mf1338B.","productDescription":"48.17 x 41.24 inches","costCenters":[],"links":[{"id":358785,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1338-B/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":184964,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/mf/1338-B/report-thumb.jpg"}],"scale":"0","country":"United States","state":"Tennessee","county":"Polk County","otherGeospatial":"Little Frog Roadless Area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -84.45083333333334,35.034166666666664 ], [ -84.45083333333334,35.083333333333336 ], [ -84.36749999999999,35.083333333333336 ], [ -84.36749999999999,35.034166666666664 ], [ -84.45083333333334,35.034166666666664 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aefe4b07f02db691684","contributors":{"authors":[{"text":"Force, E. R.","contributorId":28235,"corporation":false,"usgs":true,"family":"Force","given":"E.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":262143,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Siems, D. F.","contributorId":101239,"corporation":false,"usgs":true,"family":"Siems","given":"D.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":262144,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
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