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","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864189","usgsCitation":"Doriski, T.P., 1987, Potentiometric-surface of the water-table, Magothy, and Lloyd aquifers on Long Island, New York, in 1984: U.S. Geological Survey Water-Resources Investigations Report 86-4189, 8 Plates: 36.59 x 22.39 inches or smaller, https://doi.org/10.3133/wri864189.","productDescription":"8 Plates: 36.59 x 22.39 inches or smaller","costCenters":[],"links":[{"id":411103,"rank":10,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36611.htm","linkFileType":{"id":5,"text":"html"}},{"id":81703,"rank":9,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-8.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81702,"rank":8,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-7.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81701,"rank":7,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81700,"rank":6,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81696,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81699,"rank":5,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81697,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81698,"rank":4,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4189/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":173585,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"country":"United States","state":"New York","otherGeospatial":"Long Island","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -73.9402237135873,\n 40.535165012909374\n ],\n [\n -73.32737821143094,\n 40.585714917518914\n ],\n [\n -72.20674643605918,\n 40.85113756952231\n ],\n [\n -71.84254110906322,\n 41.08647309372546\n ],\n [\n -72.28028789631803,\n 41.17615490662308\n ],\n [\n -72.64799519761131,\n 40.9913822898217\n ],\n [\n -73.16278541942312,\n 41.00459756051177\n ],\n [\n -73.19780516240344,\n 40.94114010013382\n ],\n [\n -73.36589992870944,\n 40.951720582036614\n ],\n [\n -73.54800259220742,\n 40.94378537953705\n ],\n [\n -73.7336072300036,\n 40.88291715045801\n ],\n [\n -73.89119607341503,\n 40.78488113258558\n ],\n [\n -73.99625530235596,\n 40.72652073479111\n ],\n [\n -74.05929083972103,\n 40.64951285822099\n ],\n [\n -74.01726714814431,\n 40.58305534791833\n ],\n [\n -73.9402237135873,\n 40.535165012909374\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad3e4b07f02db68202b","contributors":{"authors":[{"text":"Doriski, Thomas P.","contributorId":20301,"corporation":false,"usgs":true,"family":"Doriski","given":"Thomas","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":229718,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44414,"text":"wri864315 - 1987 - Hydrology of Island Ford Lake, Hillsborough County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864315","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4315","title":"Hydrology of Island Ford Lake, Hillsborough County, Florida","language":"ENGLISH","doi":"10.3133/wri864315","usgsCitation":"Henderson, S., 1987, Hydrology of Island Ford Lake, Hillsborough County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4315, 3 maps on 1 sheet : col. ; 29 x 44 cm. and smaller, on sheet 81 x 102 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864315.","productDescription":"3 maps on 1 sheet : col. ; 29 x 44 cm. and smaller, on sheet 81 x 102 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173692,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4315/report-thumb.jpg"},{"id":81710,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4315/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a17e4b07f02db604911","contributors":{"authors":[{"text":"Henderson, S.E.","contributorId":70806,"corporation":false,"usgs":true,"family":"Henderson","given":"S.E.","email":"","affiliations":[],"preferred":false,"id":229723,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44416,"text":"wri864330 - 1987 - Chemical characteristics of water in the surficial aquifer system, Broward County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864330","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4330","title":"Chemical characteristics of water in the surficial aquifer system, Broward County, Florida","docAbstract":"Water quality data was collected in 1981 and 1982 during the drilling of test holes at 27 sites throughout Broward County, Florida. Determinations were made for the following physical properties and chemical constituents: pH, alkalinity, specific conductance, major ions, selected nutrients and dissolved iron, aluminum, and manganese. Determinations for the trace elements-arsenic, barium, cadmium, chromium, lead, zinc, selenium, and mercury-were made at 14 wells. Water in the surficial aquifer system between the coastal ridge and the conservation areas is potable and usually is a calcium bicarbonate type for the first 140 ft or more below land surface. Between depths of 140 and 230 ft, groundwater generally grades into a mixed-ion water type. In some areas, diluted seawater occurs beneath the mixed water zone. Dissolved iron concentrations between the coastal ridge and the conservation areas are variable but generally exceed 1,000 micrograms/L. Beneath the conservation areas and the western edge of Broward County, groundwater in the first 100 ft below land surface generally is either a calcium bicarbonate type or a mixed-ion type. At depths between 100 and 200 ft, diluted residual seawater occurs, except along the far western edge of the county. Residual seawater is least diluted in the north. Dissolved iron concentrations generally are between 300 and 1 ,000 micrograms/L but increase to the east of the conservation areas. Other findings of the investigation include: (1) groundwater in some areas west of the coastal ridge probably would be suitable for most domestic, agricultural, and industrial uses if it were treated for carbonate hardness; (2) groundwater in much of Broward County is chemically altered by natural softening and magnesium enrichment (natural softening increases to the west and is very pronounced beneath the far western edge of the county); and (3) there is evidence of mineralized water from the conservation areas mixing with groundwater east of the levees. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864330","usgsCitation":"Howie, B., 1987, Chemical characteristics of water in the surficial aquifer system, Broward County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4330, 2 maps : col. ; 39 x 70 cm. and 39 x 61 cm., on sheets 81 x 102 cm., https://doi.org/10.3133/wri864330.","productDescription":"2 maps : col. ; 39 x 70 cm. and 39 x 61 cm., on sheets 81 x 102 cm.","costCenters":[],"links":[{"id":173027,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81712,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4330/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81713,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4330/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e4245","contributors":{"authors":[{"text":"Howie, Barbara","contributorId":54248,"corporation":false,"usgs":true,"family":"Howie","given":"Barbara","email":"","affiliations":[],"preferred":false,"id":229728,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44417,"text":"wri864348 - 1987 - Louisiana ground-water map no. 1: Potentiometric surface, 1985, and water-level changes, 1983-85, of the Chicot aquifer in southwestern Louisiana","interactions":[],"lastModifiedDate":"2023-01-10T21:56:46.621062","indexId":"wri864348","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4348","title":"Louisiana ground-water map no. 1: Potentiometric surface, 1985, and water-level changes, 1983-85, of the Chicot aquifer in southwestern Louisiana","docAbstract":"The Chicot aquifer is the principle source of groundwater in southwestern Louisiana and is the most extensively pumped (nearly 1 billion gallons per day) aquifer in the State. Withdrawals from the Chicot aquifer are used primarily for irrigation. Two maps show the generalized potentiometric surfaces of the upper sand unit ('200-ft ' sand in the Lake Charles area) and the ' 500-ft ' sand of the Chicot aquifer. General water level altitudes and flow directions may be inferred from these maps which were prepared in cooperation with the Louisiana Department of Transportation and Development, Office of Public Works. Previous studies of groundwater hydrology in southwestern Louisiana are included in selected references.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864348","usgsCitation":"Fendick, R., and Nyman, D.J., 1987, Louisiana ground-water map no. 1: Potentiometric surface, 1985, and water-level changes, 1983-85, of the Chicot aquifer in southwestern Louisiana: U.S. Geological Survey Water-Resources Investigations Report 86-4348, 2 Plates: 27.00 x 24.87 inches, https://doi.org/10.3133/wri864348.","productDescription":"2 Plates: 27.00 x 24.87 inches","costCenters":[],"links":[{"id":173028,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81715,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4348/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":81714,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4348/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":411674,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36660.htm","linkFileType":{"id":5,"text":"html"}}],"country":"United States","state":"Louisiana","otherGeospatial":"Chicot aquifer","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"coordinates\": [\n [\n [\n -91.5,\n 31\n ],\n [\n -93.907,\n 31\n ],\n [\n -93.907,\n 29.817\n ],\n [\n -91.5,\n 29.817\n ],\n [\n -91.5,\n 31\n ]\n ]\n ],\n \"type\": \"Polygon\"\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a6fe4b07f02db640bc6","contributors":{"authors":[{"text":"Fendick, Robert B. Jr. rfendick@usgs.gov","contributorId":1313,"corporation":false,"usgs":true,"family":"Fendick","given":"Robert B.","suffix":"Jr.","email":"rfendick@usgs.gov","affiliations":[{"id":369,"text":"Louisiana Water Science Center","active":true,"usgs":true}],"preferred":false,"id":229729,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Nyman, Dale J.","contributorId":28584,"corporation":false,"usgs":true,"family":"Nyman","given":"Dale","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":229730,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":57459,"text":"wdrMT862 - 1987 - Water resources data for Montana, water year 1986. Volume 2. Columbia River Basin","interactions":[],"lastModifiedDate":"2020-08-21T17:32:49.53663","indexId":"wdrMT862","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":340,"text":"Water Data Report","code":"WDR","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"MT-86-2","title":"Water resources data for Montana, water year 1986. Volume 2. Columbia River Basin","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wdrMT862","usgsCitation":"Shields, R., Knapton, J.R., White, M.K., Brosten, T., and Lambing, J., 1987, Water resources data for Montana, water year 1986. Volume 2. 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H.","affiliations":[],"preferred":false,"id":257079,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":44419,"text":"wri864067 - 1987 - Lithology and base of the surficial aquifer system, Palm Beach County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:10:31","indexId":"wri864067","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"86-4067","title":"Lithology and base of the surficial aquifer system, Palm Beach County, Florida","docAbstract":"The surficial aquifer system is a major source of freshwater in Palm Beach County. In 1982, public supply withdrawals from the aquifer system totaled 33,543 million gallons, 77.5% of total public supply withdrawals. To evaluate the aquifer system and its geologic framework, a cooperative study with Palm Beach County was begun in 1982 by the U.S. Geological Survey. The surficial aquifer system in Palm Beach County is composed primarily of sand, sandstone, shell, silt, calcareous clay (marl), and limestone deposited during the Pleistocene and Pliocene epochs. In the western two-thirds of Palm Beach County, sediments in the aquifer system are poorly consolidated sand, shell, and sandy limestone. Owing to interspersed calcareous clays and silt and very poorly sorted materials, permeabilities in this zone of the aquifer system are relatively low. Two other zones of the aquifer system are found in the eastern one-third of the county where the sediments are appreciably more permeable than in the west due to better sorting and less silt and clay content. The location of more detailed lithologic logs for wells in these sections, along with data from nearby wells, allowed enhanced interpretation and depiction of the lithology which had previously been generalized. The most permeable zone of the aquifer system in this area is characterized by highly developed secondary porosity where infiltrating rainwater and solution by groundwater have removed calcitic-cementing materials from the sediments to produce interconnected cavities. Increased permeability in the aquifer system is generally coincident with the eastern boundary of the overlying organic soils and Lake Flirt Marl. Lithologic logs of wells in Palm Beach County indicate that sediments forming the aquifer system were deposited directly on the erosional surface of the Hawthorn Formation in some areas. In other locations in the county, lithologic logs indicate that the base of the aquifer system was formed by fluvial deposits containing erosional materials from the Tamiami and Hawthorn Formations and Caloosahatchee Marl. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri864067","usgsCitation":"Miller, W.L., 1987, Lithology and base of the surficial aquifer system, Palm Beach County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4067, 1 map : col. ; 32 x 37 cm., on sheet 62 x 89 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri864067.","productDescription":"1 map : col. ; 32 x 37 cm., on sheet 62 x 89 cm., folded in envelope 31 x 23 cm.","costCenters":[],"links":[{"id":173112,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81717,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4067/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635c14","contributors":{"authors":[{"text":"Miller, Wesley L.","contributorId":91859,"corporation":false,"usgs":true,"family":"Miller","given":"Wesley","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":229732,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44457,"text":"wri854271 - 1987 - Geohydrologic framework of the coastal plain aquifers of South Carolina","interactions":[],"lastModifiedDate":"2017-01-24T11:04:31","indexId":"wri854271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4271","title":"Geohydrologic framework of the coastal plain aquifers of South Carolina","docAbstract":"The U.S. Geological Survey is conducting a series of investigations of aquifers throughout the United States as a part of the RASA (Regional Aquifer System Analysis) program. These investigations provide a comprehensive regional understanding of groundwater resources throughout the Nation. The Coastal Plain aquifers in South Carolina are being studied as a part of this program. An important part of a description of the groundwater resources is the development of a geohydrologic framework. Such a framework delineates the aquifers through which groundwater flows and the confining units which retard the flow of groundwater between aquifers. The Coastal Plain of South Carolina is underlain by a wedge of sediments that thickens from its inner margin, the Fall Line, to the coast and consists of sand, silt, clay, and limestone of Late Cretaceous to Holocene age. These sediments are underlain by pre-Cretaceous rocks consisting of consolidated sedimentary rocks of Triassic age and a complex of metamorphic and igneous rocks similar to those found near the surface in the Piedmont province of the State. The geohydrologic framework that divides the sediments of the South Carolina Coastal Plain into the Coastal Plain aquifer system is delineated by eleven geohydrologic sections and four maps showing the configuration of the top or base of individual aquifers. Although flow within the Coastal Plain aquifer system is three dimensional, simplifying the system by dividing it into a framework of discrete hydrologic units can aid significantly in understanding the hydrology of the system. This framework is the basis for the aquifers used in potentiometric mapping, transmissivity mapping, geochemical analysis, and groundwater flow modeling for the South Carolina RASA program. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri854271","usgsCitation":"Aucott, W.R., Davis, M.E., and Speiran, G.K., 1987, Geohydrologic framework of the coastal plain aquifers of South Carolina: U.S. Geological Survey Water-Resources Investigations Report 85-4271, 5 maps on 2 sheets, 5 sheets of sections ; sheets 132 x 101 cm., folded in envelope 31 x 23 cm., https://doi.org/10.3133/wri854271.","productDescription":"5 maps on 2 sheets, 5 sheets of sections ; sheets 132 x 101 cm., folded in envelope 31 x 23 cm.","costCenters":[{"id":13634,"text":"South Atlantic Water Science 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Thickness of rocks from the surface to the top of the Permian Minnelusa Formation, Powder River basin, Wyoming and Montana: U.S. Geological Survey Open-File Report 87-340, 1 map :photocopy ;55 x 55 cm., on sheet 78 x 79 cm., https://doi.org/10.3133/ofr87340U.","productDescription":"1 map :photocopy ;55 x 55 cm., on sheet 78 x 79 cm.","costCenters":[],"links":[{"id":81460,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0340u/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":172356,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c55a","contributors":{"authors":[{"text":"Fox, J. 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E.","contributorId":79080,"corporation":false,"usgs":true,"family":"Fox","given":"J.","middleInitial":"E.","affiliations":[],"preferred":false,"id":229047,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Higley, Debra K. 0000-0001-8024-9954 higley@usgs.gov","orcid":"https://orcid.org/0000-0001-8024-9954","contributorId":152663,"corporation":false,"usgs":true,"family":"Higley","given":"Debra","email":"higley@usgs.gov","middleInitial":"K.","affiliations":[{"id":164,"text":"Central Energy Resources Science Center","active":true,"usgs":true}],"preferred":true,"id":229046,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":20731,"text":"ofr87450Y - 1987 - Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:07:48","indexId":"ofr87450Y","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-450","chapter":"Y","title":"Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87450Y","usgsCitation":"Ryder, R.T., 1987, Oil and gas resources of the Cincinnati arch, Ohio, Indiana, Kentucky, and Tennessee: U.S. Geological Survey Open-File Report 87-450, i, 30 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr87450Y.","productDescription":"i, 30 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":153963,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0450y/report-thumb.jpg"},{"id":50285,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0450y/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af4e4b07f02db691d97","contributors":{"authors":[{"text":"Ryder, R. T.","contributorId":96673,"corporation":false,"usgs":true,"family":"Ryder","given":"R.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":183145,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":44465,"text":"wri854053 - 1987 - Geologic structure and altitude of the top of the Minnelusa Formation, northern Black Hills, South Dakota and Wyoming, and Bear Lodge Mountains, Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:10:09","indexId":"wri854053","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"85-4053","title":"Geologic structure and altitude of the top of the Minnelusa Formation, northern Black Hills, South Dakota and Wyoming, and Bear Lodge Mountains, Wyoming","docAbstract":"Beginning in 1981, a 3-yr project was conducted to determine the availability and quality of groundwater in the sedimentary bedrock aquifers in the Black Hills of South Dakota and Wyoming. The project was limited to three bedrock units in order of increasing age: the Cretaceous Inyan kara Group, Permian and Pennsylvanian Minnelusa Formation, and Mississippian Madison (or Pahasapa) Limestone. This map shows the altitude of the top of the Minnelusa Formation in the northern Black Hills, and shows the configuration of the structural features in the northern part of the Black Hills and the eastern part of the Bear Lodge Mountains. In general, the Minnelusa Formation dips away from the Black Hills uplift, either to the northeast and the Williston Basin or, south of the Bear Lodge Mountains, to the southwest and the Powder River basin, which is outside the map area. In the map area, the upper beds of the Minnelusa Formation are an aquifer and the lower beds are a confining or semi-confining unit. The upper part of the Minnelusa Formation has a greater percentage of coarse-grained sandstone beds than the lower part. Furthermore, solution and removal of anhydrite, brecciation, and solution of cement binding the sandstone grains may have increased the permeability of the upper part of the Minnelusa Formation in the Black Hills. Wells completed in the upper part of the Minnelusa have yields that exceed 100 gal/min in some areas and at least one large diameter well is reported to flow 1,000 gal/min in some areas and at least one large diameter well is reported to flow 1,000 gal/min. Flowing wells have been completed in the Minnelusa aquifer in most of the study area in South Dakota and in about the northern one-half of Crook County, Wyoming. (Lantz-PTT)","language":"ENGLISH","doi":"10.3133/wri854053","usgsCitation":"Peter, K.D., Kyllonen, D.P., and Mills, K.R., 1987, Geologic structure and altitude of the top of the Minnelusa Formation, northern Black Hills, South Dakota and Wyoming, and Bear Lodge Mountains, Wyoming: U.S. Geological Survey Water-Resources Investigations Report 85-4053, 1 map ; 68 x 82 cm., on sheet 92 x 127 cm., https://doi.org/10.3133/wri854053.","productDescription":"1 map ; 68 x 82 cm., on sheet 92 x 127 cm.","costCenters":[],"links":[{"id":162062,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":81797,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1985/4053/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b16e4b07f02db6a51a8","contributors":{"authors":[{"text":"Peter, Kathy D.","contributorId":101294,"corporation":false,"usgs":true,"family":"Peter","given":"Kathy","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":229818,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kyllonen, David P.","contributorId":97955,"corporation":false,"usgs":true,"family":"Kyllonen","given":"David","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":229817,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mills, K. R.","contributorId":90791,"corporation":false,"usgs":true,"family":"Mills","given":"K.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":229816,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":16386,"text":"ofr87183 - 1987 - X-ray spectrometric determinations of arsenic sorbed onto cellulose after solvent extraction from fused silicate rocks","interactions":[],"lastModifiedDate":"2012-02-02T00:07:01","indexId":"ofr87183","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-183","title":"X-ray spectrometric determinations of arsenic sorbed onto cellulose after solvent extraction from fused silicate rocks","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87183","usgsCitation":"Vivit, D., and Lindsay, J., 1987, X-ray spectrometric determinations of arsenic sorbed onto cellulose after solvent extraction from fused silicate rocks: U.S. Geological Survey Open-File Report 87-183, 9 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87183.","productDescription":"9 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147512,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0183/report-thumb.jpg"},{"id":45339,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0183/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49d6e4b07f02db5de632","contributors":{"authors":[{"text":"Vivit, D.V.","contributorId":28609,"corporation":false,"usgs":true,"family":"Vivit","given":"D.V.","email":"","affiliations":[],"preferred":false,"id":172758,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lindsay, J.R.","contributorId":45452,"corporation":false,"usgs":true,"family":"Lindsay","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":172759,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":44027,"text":"ofr87340I - 1987 - Thickness of the Teapot Sandstone Member of the Upper Cretaceous Mesaverde Formation, Powder River basin, Wyoming and Montana","interactions":[],"lastModifiedDate":"2022-07-14T13:45:11.407927","indexId":"ofr87340I","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"87-340","chapter":"I","title":"Thickness of the Teapot Sandstone Member of the Upper Cretaceous Mesaverde Formation, Powder River basin, Wyoming and Montana","docAbstract":"No abstract available.
","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/ofr87340I","usgsCitation":"Fox, J.E., and Higley, D.K., 1987, Thickness of the Teapot Sandstone Member of the Upper Cretaceous Mesaverde Formation, Powder River basin, Wyoming and Montana: U.S. Geological Survey Open-File Report 87-340, 1 Plate: 30.65 × 30.65 inches, https://doi.org/10.3133/ofr87340I.","productDescription":"1 Plate: 30.65 × 30.65 inches","costCenters":[],"links":[{"id":169127,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":403725,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17208.htm","linkFileType":{"id":5,"text":"html"}},{"id":81445,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1987/0340i/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Montana, Wyoming","otherGeospatial":"upper Cretaceous Mesaverde formation","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -107,\n 42.75\n ],\n [\n -104,\n 42.75\n ],\n [\n -104,\n 45.182\n ],\n [\n -107,\n 45.182\n ],\n [\n -107,\n 42.75\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a54e4b07f02db62c545","contributors":{"authors":[{"text":"Fox, J. 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The decline in acidity, however, was not spatially or temporally uniform. The range in acidity and sulfate concentrations decreased during the four-yr period. Variations in the area of constant pH surfaces take the general form of area reductions in both the lower (pH 4.01-4.40) and upper (pH 4.91-5.40) range of values with concomitant area increases in the middle (pH 4.41-4.90) range. The pattern for sulfate is simpler, with area increases occurring in the lower (1.0-1.9 mg/L) range, decreases in the upper (2.5-4.4 mg/L) range, with approximate stability in the middle (2.0-2.4 mg/L) range of values. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr87454","usgsCitation":"Lins, H., Lanfear, K., and Schertz, T., 1987, Patterns of acid deposition variability in the Eastern United States, 1981-84: U.S. Geological Survey Open-File Report 87-454, i, 13 p. :ill. ;28 cm., https://doi.org/10.3133/ofr87454.","productDescription":"i, 13 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":147577,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1987/0454/report-thumb.jpg"},{"id":43464,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1987/0454/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688ad7","contributors":{"authors":[{"text":"Lins, H.F.","contributorId":81508,"corporation":false,"usgs":true,"family":"Lins","given":"H.F.","affiliations":[],"preferred":false,"id":169869,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lanfear, K.J.","contributorId":14392,"corporation":false,"usgs":true,"family":"Lanfear","given":"K.J.","affiliations":[],"preferred":false,"id":169867,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schertz, T. 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","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/wri874162","usgsCitation":"Dacosta, R., and Gómez-Gómez, F., 1987, Potentiometric surface of the alluvial aquifer and hydrologic conditions in the Guayama quadrangle, Puerto Rico, March 1986: U.S. Geological Survey Water-Resources Investigations Report 87-4162, 1 Plate: 28.69 x 21.54 inches, https://doi.org/10.3133/wri874162.","productDescription":"1 Plate: 28.69 x 21.54 inches","costCenters":[],"links":[{"id":168555,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4162/report-thumb.jpg"},{"id":366693,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1987/4162/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","otherGeospatial":"Puerto Rico","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -66.21768951416016,\n 17.92157608317564\n ],\n [\n -66.07624053955078,\n 17.92157608317564\n ],\n [\n -66.07624053955078,\n 17.989835742155027\n ],\n [\n -66.21768951416016,\n 17.989835742155027\n ],\n [\n -66.21768951416016,\n 17.92157608317564\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad4e4b07f02db682ed0","contributors":{"authors":[{"text":"Dacosta, Rafael","contributorId":93060,"corporation":false,"usgs":true,"family":"Dacosta","given":"Rafael","email":"","affiliations":[],"preferred":false,"id":229706,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Gómez-Gómez, Fernando","contributorId":31366,"corporation":false,"usgs":true,"family":"Gómez-Gómez","given":"Fernando","affiliations":[],"preferred":false,"id":229705,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":28917,"text":"wri874037 - 1987 - Modeling nutrient and dissolved-oxygen transport in the Truckee River and Truckee Canal downstream from Reno, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:08:47","indexId":"wri874037","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1987","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":342,"text":"Water-Resources Investigations Report","code":"WRI","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"87-4037","title":"Modeling nutrient and dissolved-oxygen transport in the Truckee River and Truckee Canal downstream from Reno, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri874037","usgsCitation":"Nowlin, J.O., 1987, Modeling nutrient and dissolved-oxygen transport in the Truckee River and Truckee Canal downstream from Reno, Nevada: U.S. Geological Survey Water-Resources Investigations Report 87-4037, xx, 487 p. :ill. ;28 cm., https://doi.org/10.3133/wri874037.","productDescription":"xx, 487 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123080,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1987/4037/report-thumb.jpg"},{"id":57789,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1987/4037/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b05e4b07f02db69989e","contributors":{"authors":[{"text":"Nowlin, Jon O.","contributorId":34937,"corporation":false,"usgs":true,"family":"Nowlin","given":"Jon","email":"","middleInitial":"O.","affiliations":[],"preferred":false,"id":200615,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":21493,"text":"ofr87755 - 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