{"pageNumber":"4858","pageRowStart":"121425","pageSize":"25","recordCount":184582,"records":[{"id":57445,"text":"wdrMS841 - 1986 - Water resources data for Mississippi, water year 1984","interactions":[],"lastModifiedDate":"2025-08-28T13:43:22.200534","indexId":"wdrMS841","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"MS-84-1","title":"Water resources data for Mississippi, water year 1984","docAbstract":"<p>Water resources data for the 1987 water year for Mississippi consist of records of stage, discharge, and water quality of streams; stage, and water quality of lakes and reservoirs; and water levels and water quality of ground-water wells. This report contains records of water discharge at 78 gaging stations; stage records for 18 of these gaging stations; stage only at 5 gaging stations; water quality for 11 stations, 3 precipitation quality stations, and 120 wells; and water levels for 498 observation wells. Also included are peak-discharge data for 56 crest-stage partial record stations, discharge data at 263 low-flow partial-record stations, and water quality data at 2 partial-record or miscellaneous sites. Locations of these sites are shown on Figures 4-6. Additional water data were collected at various sites, not part of the systematic data collection program, and are published as miscellaneous measurements. These data represent that part of the National Water Data System operated by the U.S. Geological Survey and cooperating State and Federal agencies in Mississippi. </p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrMS841","collaboration":"Prepared in cooperation with the State of Mississippi and with other agencies","usgsCitation":"Tharpe, E., Morris, F., and Oakley, W.T., 1986, Water resources data for Mississippi, water year 1984: U.S. Geological Survey Water Data Report MS-84-1, vii, 340 p., https://doi.org/10.3133/wdrMS841.","productDescription":"vii, 340 p.","costCenters":[],"links":[{"id":494989,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1984/ms-84-1/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":174618,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1984/ms-84-1/report-thumb.jpg"}],"country":"United 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 \"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ce4b07f02db5fcc94","contributors":{"authors":[{"text":"Tharpe, E.J.","contributorId":57534,"corporation":false,"usgs":true,"family":"Tharpe","given":"E.J.","email":"","affiliations":[],"preferred":false,"id":257033,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Morris, F.","contributorId":17299,"corporation":false,"usgs":true,"family":"Morris","given":"F.","affiliations":[],"preferred":false,"id":257032,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Oakley, W. T.","contributorId":76331,"corporation":false,"usgs":true,"family":"Oakley","given":"W.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":257034,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":4266,"text":"cir944 - 1986 - The Conterminous United States Mineral Assessment Program; background information to accompany folio of geologic, geophysical, geochemical, mineral-occurrence, mineral-resource potential, and mineral-production maps of the Charlotte 1 degree x 2 degrees Quadrangle, North Carolina and South Carolina","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir944","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"944","title":"The Conterminous United States Mineral Assessment Program; background information to accompany folio of geologic, geophysical, geochemical, mineral-occurrence, mineral-resource potential, and mineral-production maps of the Charlotte 1 degree x 2 degrees Quadrangle, North Carolina and South Carolina","docAbstract":"This Circular and the folio of separately published maps described herein are part of a series of reports compiled under the Conterminous United States Mineral Assessment Program ICUSMAP). The folio on the Charlotte 1 degree ? 2 degree quadrangle, North Carolina and South Carolina, includes (1) a geologic map; (2) four geophysical maps; (3) geochemical maps for metamorphic heavy minerals, copper, lead and artifacts, zinc, gold, tin, beryllium, niobium, tungsten, molybdenum, titanium, cobalt, lithium, barium, antimony-arsenic-bismuth-cadmium, thorium-cerium-monazite, and limonite; (4) mineral-occurrence maps for kyanite-sillimanite-lithium-mica-feldspar-copper-lead-zinc, gold-quartz-barite-fluorite, iron-thorium-tin-niobium, and construction materials-gemstones; (5) mineral-resource potential maps for copper-lead-zinc-combined base metals, gold, tin-tungsten, beryllium-molybdenum-niobium, lithium-kyanite- sillimanitebarite, thorium (monazite)-uranium, and construction materials; and (6) mineral-production maps. \r\n\r\nThe Charlotte quadrangle is mainly within the Piedmont physiographic province and extends from near the Coastal Plain on the southeast into the Blue Ridge province on the northwest for a short distance. Parts of six lithotectonic belts are present--the Blue Ridge, the Inner Piedmont, the Kings Mountain belt, the Charlotte belt, the Carolina slate belt, and the Wadesboro basin. Igneous, metamorphic, and sedimentary rocks are present and range in age from Proterozoic to Mesozoic; alluvial sediments of Quaternary age occur along rivers and larger streams. \r\n\r\nRocks of the Blue Ridge include Middle Proterozoic granitoid gneiss intruded by Late Proterozoic granite; Late Proterozoic paragneiss, schist, and other metasedimentary and metavolcaniclastic rocks (Ashe and Grandfather Mountain Formations); Late Proterozoic and Early Cambrian metasedimentary rocks (Chilhowee Group); and Early Cambrian sedimentary rocks (Shady Dolomite). Paleozoic granites intrude the Proterozoic rocks. The Inner Piedmont contains noncarbonate metasedimentary rocks and amphibolite of medium to high metamorphic grades. These rocks are intruded by the Toluca Granite and Henderson Gneiss of Cambrian and Ordovician(?) age. The Charlotte belt consists largely of Late Proterozoic to Late Paleozoic granitic and gabbroic plutonic rocks and intervening enclaves of metasedimentary and metavolcanic rocks. \r\n\r\nThe narrow Kings Mountain belt is located between the Charlotte and the Inner Piedmont belts and contains mainly Late Proterozoic metasedimentary rocks and plutonic rocks similar to those of the Charlotte belt. The Carolina slate belt, flanking the Charlotte belt on the east, contains weakly metamorphosed volcanic and sedimentary rocks. East of this belt, at the southeast corner of the quadrangle, is the Wadesboro basin, which has continental sedimentary rocks of Triassic age. Layered rocks westward from and in the Charlotte belt are complexly folded, are steeply dipping, and in the Blue Ridge and Inner Piedmont are contained within major thrust slices. Rocks of the Carolina slate belt are gently folded. Rocks of the Wadesboro basin occur in downfaulted blocks. \r\n\r\nThe geophysical surveys of the Charlotte quadrangle consisted of Bouguer gravity, aeromagnetic, and aeroradioactivity surveys and used both newly obtained data and information from prior work. The gravity survey disclosed a distinct northeast-trending, northwest-decreasing gradient, which is part of the major gravity gradient that extends the length of the Appalachian Mountains. Granitic plutons of the Charlotte belt, in particular, are marked by gravity lows, and gabbro plutons, by highs. Several of the geologic belts display distinct magnetic character. The aeroradioactivity surveys showed a swath of consistently high gamma-ray intensities along the central part of the Inner Piedmont belt; these high intensities correspond to the so-called monazite belt. Oval patterns of high gamma-ray readi","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir944","usgsCitation":"Gair, J.E., Goldsmith, R., Daniels, D.L., Griffitts, W.R., DeYoung, J.H., and Lee, M.P., 1986, The Conterminous United States Mineral Assessment Program; background information to accompany folio of geologic, geophysical, geochemical, mineral-occurrence, mineral-resource potential, and mineral-production maps of the Charlotte 1 degree x 2 degrees Quadrangle, North Carolina and South Carolina: U.S. Geological Survey Circular 944, iii, 18 p. :ill., map ;26 cm., https://doi.org/10.3133/cir944.","productDescription":"iii, 18 p. :ill., map ;26 cm.","costCenters":[],"links":[{"id":117490,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0944/report-thumb.jpg"},{"id":31378,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0944/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4acce4b07f02db67ecbe","contributors":{"authors":[{"text":"Gair, Jacob Eugene","contributorId":14387,"corporation":false,"usgs":true,"family":"Gair","given":"Jacob","email":"","middleInitial":"Eugene","affiliations":[],"preferred":false,"id":148639,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Goldsmith, Richard","contributorId":33283,"corporation":false,"usgs":true,"family":"Goldsmith","given":"Richard","email":"","affiliations":[],"preferred":false,"id":148640,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Daniels, D. L.","contributorId":69114,"corporation":false,"usgs":true,"family":"Daniels","given":"D.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":148642,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Griffitts, W. R.","contributorId":10428,"corporation":false,"usgs":true,"family":"Griffitts","given":"W.","middleInitial":"R.","affiliations":[],"preferred":false,"id":148638,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"DeYoung, J. H.","contributorId":75908,"corporation":false,"usgs":true,"family":"DeYoung","given":"J.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":148643,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Lee, M. P.","contributorId":40198,"corporation":false,"usgs":true,"family":"Lee","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":148641,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}}
,{"id":26877,"text":"wri864068 - 1986 - Hydrogeology of the surficial and intermediate aquifers of central Sarasota County, Florida","interactions":[],"lastModifiedDate":"2023-01-06T22:46:21.647008","indexId":"wri864068","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":"86-4068","title":"Hydrogeology of the surficial and intermediate aquifers of central Sarasota County, Florida","docAbstract":"<p>The geohydrologic units underlying a 300 sq mi area in central Sarasota County, Florida, consist of the surficial aquifer, intermediate aquifers (Tamiami-upper Hawthorn and lower Hawthorn-upper Tampa aquifers) and confining units, the Floridan aquifer system, and the sub-Floridan confining unit. The saturated thickness of the surficial aquifer ranges from about 40 to 75 ft and the water table is generally within 5 ft of land surface. The Tamiami-upper Hawthorn is the uppermost intermediate aquifer. The top of the aquifer ranges from about 50 ft to about 75 below sea level and has an average thickness of about 100 ft. The lower Hawthorne-upper Tampa aquifer is the lowermost intermediate aquifer. The top of the aquifer ranges from about 190 to about 220 ft below sea level and its thickness ranges from about 200 to 250 ft. The quality of water in the surficial and the two intermediate aquifers is acceptable for potable use except near the coast. Water from the Floridan aquifer system is used primarily for agricultural purposes because it is too mineralized for most other uses; therefore, the surficial and intermediate aquifers are developed for water supply. The artesian pressure of the various aquifers generally increases with depth. A more detailed geohydrologic description is presented for the Ringling-MacArthur Reserve, a 51 sq mi area in the central part of the county that may be used by Sarasota County as a future water supply. Average annual rainfall is 56 inches and evapotranspiration is about 42 in at the Reserve. The area has a high water table, many sloughs and swamps, and undeveloped land, making it an attractive site as a potential source of water.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864068","usgsCitation":"Duerr, A.D., and Wolansky, R., 1986, Hydrogeology of the surficial and intermediate aquifers of central Sarasota County, Florida: U.S. Geological Survey Water-Resources Investigations Report 86-4068, iv, 48 p., https://doi.org/10.3133/wri864068.","productDescription":"iv, 48 p.","costCenters":[],"links":[{"id":411538,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36525.htm","linkFileType":{"id":5,"text":"html"}},{"id":124161,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4068/report-thumb.jpg"},{"id":55770,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4068/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Florida","county":"Sarasota County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -82.367,\n              27.217\n            ],\n            [\n              -82.367,\n              27.117\n            ],\n            [\n              -82.2,\n              27.117\n            ],\n            [\n              -82.2,\n              27.217\n            ],\n            [\n              -82.367,\n              27.217\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e47a3e4b07f02db496768","contributors":{"authors":[{"text":"Duerr, A. D.","contributorId":29821,"corporation":false,"usgs":true,"family":"Duerr","given":"A.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":197168,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wolansky, R. M.","contributorId":89163,"corporation":false,"usgs":true,"family":"Wolansky","given":"R. M.","affiliations":[],"preferred":false,"id":197169,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27072,"text":"wri854209 - 1986 - Water-quality variability in four reservoirs in Phillips and Valley Counties, Montana, May through August 1981","interactions":[],"lastModifiedDate":"2021-12-27T22:28:21.193797","indexId":"wri854209","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":"85-4209","title":"Water-quality variability in four reservoirs in Phillips and Valley Counties, Montana, May through August 1981","docAbstract":"Four reservoirs in Phillips and Valley Counties were studied from May to August, 1981 (1) to describe the variation in water quality that occurs from late spring (May) to late summer (August) and during 24-hrs in late summer and (2) to describe possible causes for the variation. All the reservoirs had distinct thermal gradients but lacked true stratification as a result of circulation induced by wind. Such mixing helps prevent oxygen depletion in bottom waters during the summer. The smallest dissolved-oxygen concentrations occurred in the near-bottom water of the reservoirs and during the night. Nighttime dissolved-oxygen concentrations in reservoirs 19 and 24 were much less than in reservoirs 1 and 9. Similar trends occurred with pH. Most chemical constituents in the water generally became more concentrated from May to August because of continuous water losses from evapotranspiration. This was noted by increase in the concentration of major dissolved constituents and by increase in specific conductance. All the reservoirs contained similar types of planktonic organisms, but in different proportions. Most of the fecal bacteria existing in the reservoirs presumably originated from livestock and waterfowl waste. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854209","usgsCitation":"Ferreira, R.F., and Lambing, J., 1986, Water-quality variability in four reservoirs in Phillips and Valley Counties, Montana, May through August 1981: U.S. Geological Survey Water-Resources Investigations Report 85-4209, vi, 85 p., https://doi.org/10.3133/wri854209.","productDescription":"vi, 85 p.","costCenters":[],"links":[{"id":393482,"rank":2,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36359.htm"},{"id":55942,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":121499,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4209/report-thumb.jpg"}],"country":"United States","state":"Montana","county":"Phillips County, Valley County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -108.0889892578125,\n              47.76148371616669\n            ],\n            [\n              -106.490478515625,\n              47.76148371616669\n            ],\n            [\n              -106.490478515625,\n              48.99463598353405\n            ],\n            [\n              -108.0889892578125,\n              48.99463598353405\n            ],\n            [\n              -108.0889892578125,\n              47.76148371616669\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685924","contributors":{"authors":[{"text":"Ferreira, R. F.","contributorId":80690,"corporation":false,"usgs":true,"family":"Ferreira","given":"R.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197509,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lambing, J. H.","contributorId":100860,"corporation":false,"usgs":true,"family":"Lambing","given":"J. H.","affiliations":[],"preferred":false,"id":197510,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61560,"text":"mf1718 - 1986 - Preliminary geologic interpretation of the aeromagnetic map of Afognak and Shuyak Islands, Alaska","interactions":[{"subject":{"id":42148,"text":"ofr8057 - 1980 - Aeromagnetic map of Afognak Island and vicinity, Alaska","indexId":"ofr8057","publicationYear":"1980","noYear":false,"title":"Aeromagnetic map of Afognak Island and vicinity, Alaska"},"predicate":"SUPERSEDED_BY","object":{"id":61560,"text":"mf1718 - 1986 - Preliminary geologic interpretation of the aeromagnetic map of Afognak and Shuyak Islands, Alaska","indexId":"mf1718","publicationYear":"1986","noYear":false,"title":"Preliminary geologic interpretation of the aeromagnetic map of Afognak and Shuyak Islands, Alaska"},"id":1}],"lastModifiedDate":"2012-02-10T00:10:35","indexId":"mf1718","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":"1718","title":"Preliminary geologic interpretation of the aeromagnetic map of Afognak and Shuyak Islands, Alaska","language":"ENGLISH","doi":"10.3133/mf1718","usgsCitation":"Case, J.E., Fisher, M.A., Moore, G.W., and Nelson, S., 1986, Preliminary geologic interpretation of the aeromagnetic map of Afognak and Shuyak Islands, Alaska: U.S. Geological Survey Miscellaneous Field Studies Map 1718, 2 maps on 1 sheet ;34 x 47 cm., sheet 94 x 81 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1718.","productDescription":"2 maps on 1 sheet ;34 x 47 cm., sheet 94 x 81 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106245,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7762.htm","linkFileType":{"id":5,"text":"html"},"description":"7762"},{"id":179862,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"0","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -153.5,58 ], [ -153.5,58.75 ], [ -151.5,58.75 ], [ -151.5,58 ], [ -153.5,58 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c30d","contributors":{"authors":[{"text":"Case, J. E.","contributorId":56625,"corporation":false,"usgs":true,"family":"Case","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":266042,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Fisher, M. A.","contributorId":69972,"corporation":false,"usgs":true,"family":"Fisher","given":"M.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":266044,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Moore, G. W.","contributorId":87946,"corporation":false,"usgs":true,"family":"Moore","given":"G.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":266045,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Nelson, S.W.","contributorId":67869,"corporation":false,"usgs":true,"family":"Nelson","given":"S.W.","email":"","affiliations":[],"preferred":false,"id":266043,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":4308,"text":"cir1010 - 1986 - Goals of the U.S. Geological Survey","interactions":[],"lastModifiedDate":"2012-02-02T00:05:30","indexId":"cir1010","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1010","title":"Goals of the U.S. Geological Survey","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir1010","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, Goals of the U.S. Geological Survey: U.S. Geological Survey Circular 1010, v, 17 p. :ill. ;28 cm., https://doi.org/10.3133/cir1010.","productDescription":"v, 17 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":123270,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/1010/report-thumb.jpg"},{"id":31419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/1010/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4abde4b07f02db674201","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528176,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16276,"text":"ofr86563 - 1986 - Geologic map of the White Rock Peak Quadrangle, Lincoln County, Nevada, and Beaver and Iron counties, Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr86563","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"86-563","title":"Geologic map of the White Rock Peak Quadrangle, Lincoln County, Nevada, and Beaver and Iron counties, Utah","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr86563","usgsCitation":"Toth, M.I., 1986, Geologic map of the White Rock Peak Quadrangle, Lincoln County, Nevada, and Beaver and Iron counties, Utah: U.S. Geological Survey Open-File Report 86-563, 5 p. :map ;28 cm., https://doi.org/10.3133/ofr86563.","productDescription":"5 p. :map ;28 cm.","costCenters":[],"links":[{"id":108718,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_17097.htm","linkFileType":{"id":5,"text":"html"},"description":"17097"},{"id":150475,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1986/0563/report-thumb.jpg"},{"id":45196,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1986/0563/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":45197,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1986/0563/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae3e4b07f02db68986d","contributors":{"authors":[{"text":"Toth, M. I.","contributorId":82695,"corporation":false,"usgs":true,"family":"Toth","given":"M.","email":"","middleInitial":"I.","affiliations":[],"preferred":false,"id":172536,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61303,"text":"mf1633B - 1986 - Geochemical maps of the Anaconda-Pintlar Wilderness, Granite, Deer Lodge, Beaverhead, and Ravalli counties, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:51","indexId":"mf1633B","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":"1633","chapter":"B","title":"Geochemical maps of the Anaconda-Pintlar Wilderness, Granite, Deer Lodge, Beaverhead, and Ravalli counties, Montana","language":"ENGLISH","doi":"10.3133/mf1633B","isbn":"0607814527","usgsCitation":"Zimbelman, D.R., 1986, Geochemical maps of the Anaconda-Pintlar Wilderness, Granite, Deer Lodge, Beaverhead, and Ravalli counties, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1633, 18 maps on 2 sheets ;20 x 27 cm., sheets 88 x 132 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1633B.","productDescription":"18 maps on 2 sheets ;20 x 27 cm., sheets 88 x 132 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":105988,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7398.htm","linkFileType":{"id":5,"text":"html"},"description":"7398"},{"id":186907,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"200000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -113.83333333333333,45.75 ], [ -113.83333333333333,46.1175 ], [ -113.11749999999999,46.1175 ], [ -113.11749999999999,45.75 ], [ -113.83333333333333,45.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae04c","contributors":{"authors":[{"text":"Zimbelman, D. R.","contributorId":43768,"corporation":false,"usgs":true,"family":"Zimbelman","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":265360,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":57318,"text":"wdrFL854 - 1986 - Water resources data, Florida, water year 1985. Volume 4: Northwest Florida","interactions":[],"lastModifiedDate":"2024-06-05T20:17:14.91391","indexId":"wdrFL854","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","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":"FL-85-4","title":"Water resources data, Florida, water year 1985. Volume 4: Northwest Florida","docAbstract":"<p>Water resources data for the 1985 water year in Florida consist of continuous or daily discharge for 285 streams, periodic discharge for 38 streams, miscellaneous discharge for 110 streams, continuous or daily stage for 124 streams, periodic stage for 32 streams, peak discharge for 98 streams and peak stage for 87 streams; continuous or daily elevations for 89 lakes, periodic elevations for 82 lakes; ground-water levels for 473 wells, periodic ground-water levels for 550 wells, and miscellaneous water-level measurements for 2,588 wells; quality-of-water data for 239 surface-water sites and 699 wells.</p><p>The data for northwest Florida include continuous or daily discharge for 46 streams, periodic discharge for 3 streams, miscellaneous discharge for 30 streams, continuous or daily stage for 1 stream, peak discharge for 34 streams, and peak stage for 34 streams; continuous elevations for 5 lakes and periodic elevations for 4 lakes; continuous groundwater levels for 12 wells, and periodic ground-water levels for 165 wells; quality of water for 25 surface-water sites and 20 wells.</p><p>These data represent the National Water Data System records collected by the U.S. Geological Survey and cooperating local, state and federal agencies in Florida.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wdrFL854","programNote":"Prepared in cooperation with the State of Florida and with other agencies","usgsCitation":"Meadows, P., Martin, J., and Mixson, P., 1986, Water resources data, Florida, water year 1985. Volume 4: Northwest Florida: U.S. Geological Survey Water Data Report FL-85-4, xiii, 317 p., https://doi.org/10.3133/wdrFL854.","productDescription":"xiii, 317 p.","costCenters":[],"links":[{"id":429524,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-4/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":182134,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1985/fl-85-4/report-thumb.jpg"}],"country":"United States","state":"Florida","otherGeospatial":"northwest Florida","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -87.71648433687562,\n              30.960738174150208\n            ],\n            [\n              -87.71648433687562,\n              29.51793579845939\n            ],\n            [\n              -82.47514993530945,\n              29.51793579845939\n            ],\n            [\n              -82.47514993530945,\n              30.960738174150208\n            ],\n            [\n              -87.71648433687562,\n              30.960738174150208\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fbcbb","contributors":{"authors":[{"text":"Meadows, P.E.","contributorId":10841,"corporation":false,"usgs":true,"family":"Meadows","given":"P.E.","email":"","affiliations":[],"preferred":false,"id":256690,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Martin, J.B.","contributorId":32923,"corporation":false,"usgs":true,"family":"Martin","given":"J.B.","email":"","affiliations":[],"preferred":false,"id":256691,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mixson, P.R.","contributorId":89556,"corporation":false,"usgs":true,"family":"Mixson","given":"P.R.","email":"","affiliations":[],"preferred":false,"id":256692,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61302,"text":"mf1843 - 1986 - Structure contour map of the tops of the Kreyenhagen Formation and Cretaceous strata in the Coalinga area, Fresno and Kings counties, California","interactions":[],"lastModifiedDate":"2016-08-23T10:16:37","indexId":"mf1843","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":"1843","title":"Structure contour map of the tops of the Kreyenhagen Formation and Cretaceous strata in the Coalinga area, Fresno and Kings counties, California","docAbstract":"<p>This structure contour map, originally compiled during a study of the 1983 Coalinga earthquakes, shows the general structural configuration of the upper several kilometers of section in the Coalinga area. It was compiled by using electric well-log data available through April 1982 (Ammann Map Services, 1978; Petroleum Information Corporation, 1982; California Division of Oil and Gas, 1982) and surface geology (Dibblee, 1971; Mansfield, 1971).</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1843","usgsCitation":"Zigler, J., Wentworth, C., and Bartow, J., 1986, Structure contour map of the tops of the Kreyenhagen Formation and Cretaceous strata in the Coalinga area, Fresno and Kings counties, California: U.S. Geological Survey Miscellaneous Field Studies Map 1843, Plate: 42.79 x 40.11 inches, https://doi.org/10.3133/mf1843.","productDescription":"Plate: 42.79 x 40.11 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326147,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1843.JPG"},{"id":327571,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1843/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"California","county":"Fresno County, Kings County","otherGeospatial":"Coalinga area","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -120.5,35.75 ], [ -120.5,36.5 ], [ -119.75,36.5 ], [ -119.75,35.75 ], [ -120.5,35.75 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b0ce4b07f02db69eeee","contributors":{"authors":[{"text":"Zigler, J.L.","contributorId":49860,"corporation":false,"usgs":true,"family":"Zigler","given":"J.L.","email":"","affiliations":[],"preferred":false,"id":265358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Wentworth, C. M. 0000-0003-2569-569X","orcid":"https://orcid.org/0000-0003-2569-569X","contributorId":106466,"corporation":false,"usgs":true,"family":"Wentworth","given":"C. M.","affiliations":[],"preferred":false,"id":265359,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bartow, J. A.","contributorId":16389,"corporation":false,"usgs":true,"family":"Bartow","given":"J. A.","affiliations":[],"preferred":false,"id":265357,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26948,"text":"wri854285 - 1986 - Transport and variability of indicator bacteria in the Apalachicola River and estuary, Florida, 1983-84","interactions":[],"lastModifiedDate":"2012-02-02T00:08:30","indexId":"wri854285","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":"85-4285","title":"Transport and variability of indicator bacteria in the Apalachicola River and estuary, Florida, 1983-84","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854285","usgsCitation":"Elder, J.F., 1986, Transport and variability of indicator bacteria in the Apalachicola River and estuary, Florida, 1983-84: U.S. Geological Survey Water-Resources Investigations Report 85-4285, iv, 29 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854285.","productDescription":"iv, 29 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158247,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4285/report-thumb.jpg"},{"id":55836,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4285/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4ce4b07f02db626c04","contributors":{"authors":[{"text":"Elder, J. F.","contributorId":54143,"corporation":false,"usgs":true,"family":"Elder","given":"J.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":197299,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27100,"text":"wri854023 - 1986 - Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:28:52","indexId":"wri854023","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":"85-4023","title":"Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania","docAbstract":"<p>The water quality of Swatara Creek prior to impoundment by the proposed Swatara Creek Reservoir in south-central Pennsylvania was studied from July 1981 through October 1982. The report, done in cooperation with the Pennsylvania Department of Environmental Resources (PaDER), Bureau of State Parks, presents information on existing water-quality conditions. A discussion of possible water-quality conditions in and downstream from the planned impoundment is also included.</p>\n<p>Precipitation measured near the study area at Lebanon, Pennsylvania from October 1981 through September 1982 was 8 percent below normal. Streamflow for the same period at Swatara Creek at Harper Tavern just downstream from the study area was 15 percent below the average annual flow. Swatara Creek above Highway 895 has been degraded by acid mine drainage. The main inflow to the planned impoundment has 2.1 times the discharge of Lower Little Swatara Creek--a forested and agricultural basin that is also tributary to the proposed impoundment. During the 1982 water year, 17,400 tons of suspended sediment were transported from the study area. About 46 percent of the annual load was transported during 3 days of high flow. Inflows to the planned impoundment from both Lower Little Swatara Creek and Swatara Creek above Highway 895 were poorly buffered. Measured concentrations of alkalinity and acidity were usually less than 10 mg/L (milligrams per liter) and 5 mg/L as CaCO3, respectively. The inflows contain high concentrations of nutrients and metals that would probably stratify in a reservoir. Maximum concentrations of dissolved nitrate and total phosphorus were 2.6 mg/L and 0.31 mg/L, respectively. At Lower Little Swatara Creek; these concentrations are well above those needed for growth of algae. Maximum observed concentrations for total recoverable iron, aluminum, and manganese at Swatara Creek above Highway 895 at Pine Grove were 100,000 ug/L (micrograms per liter), 66,000 ug/L, and 2,300 ug/L, respectively.</p>\n<p>Large increases in metal concentrations along with simultaneous decreases in pH and increases in acidity confirm that mine drainage continues to degrade the water quality of Swatara Creek and may have a large impact on water quality of the planned impoundment. Iron, lead, copper, and zinc concentrations periodically exceeded the U.S. Environmental Protection Agency (U.S. EPA) criteria for freshwater aquatic life. Concentrations of manganese and lead also exceeded the U.S. EPA criteria for domestic water supplies and human health, respectively.</p>\n<p>The water quality of the Swatara Creek Reservoir will depend on characteristics such as (1) the detention time of water in the lake, (2) the timing and extent of thermal and chemical stratification, (3) sedimentation, and (4) the chemical loading and concentrations in the lake. Each of these characteristics may depend in part, on streamflow.</p>\n<p>The impoundment will act as a sediment trap and thus reduce the concentrations of total phosphorus, iron, aluminum, lead, copper, and zinc immediately downstream from the impoundment. Large storm discharges and releases from the hypolimnion of the reservoir to attain the winter-pool level may contain low oxygen concentrations and elevated concentrations of iron, aluminum, lead, copper, and zinc. Unless conservation releases from the multi-level release gates are carefully controlled, low dissolved-oxygen levels and high metal concentrations may degrade the downstream water quality and be detrimental to the aquatic community.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Harrisburg, PA","doi":"10.3133/wri854023","usgsCitation":"Fishel, D.K., and Richardson, J., 1986, Results of a preimpoundment water-quality study of Swatara Creek, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 85-4023, vi, 84 p., https://doi.org/10.3133/wri854023.","productDescription":"vi, 84 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science 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,{"id":61200,"text":"mf1830B - 1986 - Surficial materials map of the Springfield 1 degree by 2 degrees Quadrangle, Missouri","interactions":[],"lastModifiedDate":"2012-02-10T00:10:32","indexId":"mf1830B","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":"1830","chapter":"B","title":"Surficial materials map of the Springfield 1 degree by 2 degrees Quadrangle, Missouri","language":"ENGLISH","doi":"10.3133/mf1830B","usgsCitation":"Whitfield, J., 1986, Surficial materials map of the Springfield 1 degree by 2 degrees Quadrangle, Missouri: U.S. Geological Survey Miscellaneous Field Studies Map 1830, 1 map ;45 x 71 cm., on sheet 85 x 95 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1830B.","productDescription":"1 map ;45 x 71 cm., on sheet 85 x 95 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106285,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7837.htm","linkFileType":{"id":5,"text":"html"},"description":"7837"},{"id":180492,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -94,37 ], [ -94,38 ], [ -92,38 ], [ -92,37 ], [ -94,37 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae1e4b07f02db688856","contributors":{"authors":[{"text":"Whitfield, J.W.","contributorId":105740,"corporation":false,"usgs":true,"family":"Whitfield","given":"J.W.","email":"","affiliations":[],"preferred":false,"id":265175,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":4521,"text":"cir983 - 1986 - 1986 annual report on Alaska's mineral resources","interactions":[],"lastModifiedDate":"2012-02-02T00:05:43","indexId":"cir983","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"983","title":"1986 annual report on Alaska's mineral resources","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir983","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1986, 1986 annual report on Alaska's mineral resources: U.S. Geological Survey Circular 983, v, 47 p. :ill., maps ;28 cm.28 cm., https://doi.org/10.3133/cir983.","productDescription":"v, 47 p. :ill., maps ;28 cm.28 cm.","costCenters":[],"links":[{"id":117548,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0983/report-thumb.jpg"},{"id":31579,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0983/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"53cd4914e4b0b290850eeddf","contributors":{"authors":[{"text":"Water Resources Division, U.S. Geological Survey","contributorId":128075,"corporation":true,"usgs":false,"organization":"Water Resources Division, U.S. Geological Survey","id":528225,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27098,"text":"wri854202 - 1986 - Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania","interactions":[],"lastModifiedDate":"2017-07-05T11:28:02","indexId":"wri854202","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":"85-4202","title":"Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania","docAbstract":"<p>Nitrate-nitrogen and herbicide ground-water data is being collected by the u.s. Geological Survey as part of the nationwide Rural Clean Water Program designed to determine the effects of agricultural-management practices on water quality. Data collected from September 1982 to October 1983 &middot; in the 188-square mile intensively farmed upper Conestoga River basin indicates high nitrate and detectable herbicide concentrations in ground water are closely associated with agricultural practices and carbonate geology. Maximum nitrate-nitrogen concentrations from 42 wells and one spring ranged from 37 to 40 milligrams per liter in the agricultural areas, and 12 to 19 milligrams per liter in the nonagricultural areas. Median concentrations of nitrate generally were three times higher in wells that penetrated carbonate rock than in wells that penetrated noncarbonate rocks. More than 40 percent of the wells in the carbonate and agricultural areas had dissolved-nitrate concentrations that exceeded 10 milligrams per liter as nitrogen, the criterion established by the U.S. Environmental Protection Agency as excessive for drinking water. Atrazine, simazine, alachlor, and metolachlor were found almost exclusively in the agricultural and carbonate areas.</p>\n<p>Water-quality data collected before and after installation of terraces, manure storage, and nutrient and herbicide management practices is valuable in determining the effectiveness of these agricultural practices, and will provide useful information to protect agricultural land, local water supplies, the Conestoga and Susquehanna Rivers and ultimately the Chesapeake Bay.</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854202","usgsCitation":"Fishel, D.K., and Lietman, P.L., 1986, Occurrence of nitrate and herbicides in ground water in the upper Conestoga River basin, Pennsylvania : water-quality study of the Conestoga River headwaters, Pennsylvania: U.S. Geological Survey Water-Resources Investigations Report 85-4202, iii, 8 p., https://doi.org/10.3133/wri854202.","productDescription":"iii, 8 p.","numberOfPages":"15","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":532,"text":"Pennsylvania Water Science Center","active":true,"usgs":true}],"links":[{"id":158657,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri854202.jpg"},{"id":310314,"rank":1,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4202/report.pdf","text":"Report","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Pennsylvania","otherGeospatial":"Conestoga River Basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -76.12838745117188,\n              40.333983227838104\n            ],\n            [\n              -75.85098266601562,\n              40.142139942215415\n            ],\n            [\n              -76.03775024414062,\n              39.9897471840457\n            ],\n            [\n              -76.431884765625,\n              40.24389506699777\n            ],\n            [\n              -76.12838745117188,\n              40.333983227838104\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4af5e4b07f02db692369","contributors":{"authors":[{"text":"Fishel, David K.","contributorId":34967,"corporation":false,"usgs":true,"family":"Fishel","given":"David","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":197548,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lietman, Patricia L.","contributorId":64227,"corporation":false,"usgs":true,"family":"Lietman","given":"Patricia","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197549,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":4412,"text":"cir979 - 1986 - Symposium proceedings; a national agenda for coal-quality research","interactions":[],"lastModifiedDate":"2018-09-19T17:47:41","indexId":"cir979","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"979","title":"Symposium proceedings; a national agenda for coal-quality research","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir979","usgsCitation":"Schweinfurth, S., 1986, Symposium proceedings; a national agenda for coal-quality research: U.S. Geological Survey Circular 979, vi, 334 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir979.","productDescription":"vi, 334 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":31517,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0979/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":117505,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0979/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae0e4b07f02db687ef4","contributors":{"editors":[{"text":"Garbini, Susan","contributorId":82287,"corporation":false,"usgs":true,"family":"Garbini","given":"Susan","affiliations":[],"preferred":false,"id":745666,"contributorType":{"id":2,"text":"Editors"},"rank":1}],"authors":[{"text":"Schweinfurth, S. P.","contributorId":82288,"corporation":false,"usgs":true,"family":"Schweinfurth","given":"S. P.","affiliations":[],"preferred":false,"id":149072,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26955,"text":"wri854118 - 1986 - Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado","interactions":[],"lastModifiedDate":"2023-01-05T20:44:28.001337","indexId":"wri854118","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":"85-4118","title":"Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado","docAbstract":"<p>The influence of streamflow and basin characteristics on channel geometry was investigated at 18 perennial and ephemeral stream reaches in the Piceance basin of northwestern Colorado. Results of stepwise multiple regression analyses indicated that the variabilities of mean bankfull depth (D) and bankfull cross-sectional flow area (Af) were predominantly a function of bankfull discharge (QB), and that most of the variability in channel slopes (S) could be explained by drainage area (DA). None of the independent variables selected for the study could account for a large part of the variability in bankfull channel width (W).&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854118","usgsCitation":"Elliott, J.G., and Cartier, K.D., 1986, Hydraulic geometry and streamflow of channels in the Piceance Basin, Rio Blanco and Garfield Counties, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4118, iv, 28 p., https://doi.org/10.3133/wri854118.","productDescription":"iv, 28 p.","costCenters":[],"links":[{"id":411450,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36283.htm","linkFileType":{"id":5,"text":"html"}},{"id":55841,"rank":2,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4118/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":123093,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4118/report-thumb.jpg"}],"country":"United States","state":"Colorado","county":"Garfiled County, Rio Blanco County","otherGeospatial":"Piceance basin","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"coordinates\": [\n          [\n            [\n              -108.667,\n              39.316\n            ],\n            [\n              -107.771,\n              39.316\n            ],\n            [\n              -107.771,\n              40.167\n            ],\n            [\n              -108.667,\n              40.167\n            ],\n            [\n              -108.667,\n              39.316\n            ]\n          ]\n        ],\n        \"type\": \"Polygon\"\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db62a286","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197311,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cartier, K. D.","contributorId":9236,"corporation":false,"usgs":true,"family":"Cartier","given":"K.","email":"","middleInitial":"D.","affiliations":[],"preferred":false,"id":197310,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26298,"text":"wri854227 - 1986 - Benthic invertebrate population characteristics as affected by water quality in coal-bearing regions of Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:17","indexId":"wri854227","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":"85-4227","title":"Benthic invertebrate population characteristics as affected by water quality in coal-bearing regions of Tennessee","docAbstract":"Benthic invertebrate and water quality data collected during previous U.S. Geological Survey studies to provide background hydrologic information on streams draining Tennessee coal reserves, were evaluated to identify possible relations between stream biota and water quality. Linear regressions produced low correlation coefficients relating the number of taxa/sample, total number of organisms/sample, sample diversity, and percentage composition of selected orders of invertebrates, with average water quality parameter values available at sampling stations (r is &lt; 0.62 at p=0.05). Analyses of these data by linear regressions explained little of the variability in benthic invertebrate samples primarily because the distributions of benthic organisms along environmental gradients are nonlinear. Variability in substrate characteristics in the study area and seasonal insect emergence patterns also complicated interpretation of these data. However, analysis of variance tests did indicate significant trends towards reduced number of taxa, number of organisms, and sample diversity at stations with relatively poor water quality conditions. Decreasing percentage composition of Ephemeroptera was generally accompanied by an increase in percent Diptera at stations with higher water quality constituent concentrations and acidic pH ( &gt; than 0.6 units). These trends indicate significant differences in benthic communities at sites with evidence of more severe land use impacts. Additional data on benthic invertebrates, water quality , and physical habitat conditions, along with analyses of data using multivariate statistical methods are needed to define ecological relations between specific groups of invertebrates and environmental conditions. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854227","usgsCitation":"Bradfield, A., 1986, Benthic invertebrate population characteristics as affected by water quality in coal-bearing regions of Tennessee: U.S. Geological Survey Water-Resources Investigations Report 85-4227, iii, 19 p. :map ;28 cm., https://doi.org/10.3133/wri854227.","productDescription":"iii, 19 p. :map ;28 cm.","costCenters":[],"links":[{"id":1996,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri85-4227","linkFileType":{"id":5,"text":"html"}},{"id":123389,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_85_4227.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a53e4b07f02db62b51e","contributors":{"authors":[{"text":"Bradfield, A.D.","contributorId":25927,"corporation":false,"usgs":true,"family":"Bradfield","given":"A.D.","affiliations":[],"preferred":false,"id":196135,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60925,"text":"mf1862 - 1986 - Preliminary map showing the thickness of glacial deposits in Ohio","interactions":[],"lastModifiedDate":"2016-08-23T09:34:33","indexId":"mf1862","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":"1862","title":"Preliminary map showing the thickness of glacial deposits in Ohio","docAbstract":"<p>This map was compiled as part of a U.S. Geological Survey project to portray the character and thickness of glacial deposits east of the Rocky Mountains. It is a preliminary map, compiled at a scale of 1:250,000 from sources of differing type and quality (fig. I, table 1). County drift-thickness maps produced by the Ohio Geological Survey are the most reliable source of data used. These county maps, either published or in manuscript form, were available for 36 of the 72 counties that contain glacial or glacially related deposits more than 50 ft thick. An earlier, reconnaissance drift-thickness map of northwestern Ohio (Ohio Department of Natural Resources, 1960) provided data for parts of 12 additional counties. Published maps of bedrock topography were utilized for 9 counties and for parts of 6 counties. The computation of drift thickness in these counties is less reliable then the drift-thickness maps published by the Ohio Geological Survey because the bedrock topography maps, most of which are at least 20 years old, were compiled from a more limited set of data. In the remaining counties, only well-log data were available. Drift-thickness data in these counties are the least reliable; the determination of thickness trends was commonly guided by the configuration of preglacial drainage channels (as drawn by Stout and others, 1943) and by topography.</p>\n<p>Throughout the glaciated areas of Ohio, and especially near the glacial margin, a network of drainage channels is buried by glacial drift. Some of these channels arc of a preglacial age while others were formed during interglacial periods; some were cut into the bedrock by rivers&mdash; either preglacial rivers or meltwater streams flowing along the glacial margin&mdash;while others, such as the lower Cuyahoga River valley, may have been overdeepened by the erosive power of glacial ice. The thickest deposits of drift in the state occur in the lower Cuyahoga River valley near Lake Erie, and above the buried valley in west-central Ohio that has been historically considered a part of the Teays Valley. The thickest drift reliably measured in Ohio to date is 602 ft in a drill hole near Cleveland.</p>\n<p>In contrast to the extreme variations in drift thickness encountered in the vicinity of buried channels, drift on the upland arcus is generally thinner and the variations in thickness are much less pronounced. Worthy of note, however, are three large areas where the drift sheet is relatively thick. In northwestern Ohio, a large volume of drift was deposited along the flanks of the Erie ice lobe (fig. 2) near the interlobate position with the Saginaw lobe to the northwest; drift thickness there exceeds 200 ft. Thick drift was also deposited in a roughly cast-west band across the Miami lobe. The mechanism that produced this band of thick drift is not obvious, but it may have been influenced in part by bedrock topography. Bedrock control of drift thickness is more clearly indicated to the cast of Columbus, along the eastern flank of the Scioto lobe, where ice slow was resisted by rocks of the Allegheny plateau. The edge of the plateau, or the Allegheny escarpment, is obscured by glacial deposits but its likely position (Fenneman, 1938; Stout and others, 1913; Dove, 1960; and Root and others, 1961) is shown on the map. Southward from the ice margin's reentrant position in southern Richland County, ice flowing eastward from the Scioto lobe encountered the topographically higher plateau, which constrained the ice and caused drift to accumulate in significant thicknesses just to the west of the escarpment.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1862","usgsCitation":"Soller, D.R., 1986, Preliminary map showing the thickness of glacial deposits in Ohio: U.S. Geological Survey Miscellaneous Field Studies Map 1862, Plate: 45.55 x 37.23 inches, https://doi.org/10.3133/mf1862.","productDescription":"Plate: 45.55 x 37.23 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326125,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1862.JPG"},{"id":327510,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1862/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Ohio","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -85,38 ], [ -85,42 ], [ -81,42 ], [ -81,38 ], [ -85,38 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cf03","contributors":{"authors":[{"text":"Soller, D. R.","contributorId":25923,"corporation":false,"usgs":true,"family":"Soller","given":"D.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":264629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":58818,"text":"mf1885 - 1986 - Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming","interactions":[],"lastModifiedDate":"2012-02-10T00:10:16","indexId":"mf1885","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":"1885","title":"Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming","language":"ENGLISH","doi":"10.3133/mf1885","usgsCitation":"Agard, S., 1986, Preliminary geologic map of the Bear Hole Quadrangle, Big Horn County, Montana, and Big Horn and Sheridan counties, Wyoming: U.S. Geological Survey Miscellaneous Field Studies Map 1885, 1 map ;58 x 41 cm., on sheet 71 x 74 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1885.","productDescription":"1 map ;58 x 41 cm., on sheet 71 x 74 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106249,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7766.htm","linkFileType":{"id":5,"text":"html"},"description":"7766"},{"id":184581,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"scale":"24000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -108,45 ], [ -108,45.1175 ], [ -107.86749999999999,45.1175 ], [ -107.86749999999999,45 ], [ -108,45 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bd22","contributors":{"authors":[{"text":"Agard, S.S.","contributorId":28668,"corporation":false,"usgs":true,"family":"Agard","given":"S.S.","email":"","affiliations":[],"preferred":false,"id":260902,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":3507,"text":"cir977 - 1986 - Principles of logic and the use of digital geographic information systems","interactions":[],"lastModifiedDate":"2012-02-02T00:05:25","indexId":"cir977","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":307,"text":"Circular","code":"CIR","onlineIssn":"2330-5703","printIssn":"1067-084X","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"977","title":"Principles of logic and the use of digital geographic information systems","docAbstract":"Digital geographic information systems allow many different types of data to be spatially and statistically analyzed. Logical operations can be performed on individual or multiple data planes by algorithms that can be implemented in computer systems. Users and creators of the systems should fully understand these operations. This paper describes the relationships of layers and features in geographic data bases and the principles of logic that can be applied by geographic information systems and suggests that a thorough knowledge of the data that are entered into a geographic data base and of the logical operations will produce results that are most satisfactory to the user. Methods of spatial analysis are reduced to their primitive logical operations and explained to further such understanding.","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/cir977","usgsCitation":"Robinove, C.J., 1986, Principles of logic and the use of digital geographic information systems: U.S. Geological Survey Circular 977, iii, 19 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir977.","productDescription":"iii, 19 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":122960,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1986/0977/report-thumb.jpg"},{"id":21962,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1986/0977/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9fe4b07f02db66103d","contributors":{"authors":[{"text":"Robinove, Charles Joseph","contributorId":71153,"corporation":false,"usgs":true,"family":"Robinove","given":"Charles","email":"","middleInitial":"Joseph","affiliations":[],"preferred":false,"id":147056,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":27002,"text":"wri854171 - 1986 - Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee","interactions":[],"lastModifiedDate":"2012-02-02T00:08:40","indexId":"wri854171","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":"85-4171","title":"Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee","docAbstract":"The National Stream Quality Accounting Network (NASQAN) is a network of stations at which systematic and continuing water quality data are collected. Major objectives of this U.S. Geological Survey program are: (1) to depict areal variability of streamflow and water quality conditions nationwide on a year-by-year basis and (2) to detect long-term changes in streamflow and stream quality. Several NASQAN stations in East Tennessee are downstream from impoundments which have a significant effect on water quality. NASQAN data obtained from the Tennessee River below Watts Bar Dam and the Clinch River below Melton Hill Dam were compared to water quality data from the basins upstream. The comparison indicates that NASQAN data obtained below impoundments may not be adequate to describe a composite picture of water quality in the accounting unit. Detention time of storage in the impoundments is believed to moderate the range of constituent values observed at the NASQAN stations. Data obtained upstream and downstream from Watts Bar Dam indicate that the water sampled at the NASQAN station comes from stratified layers of the impoundment and is not representative of an integrated sample of water from the impoundment. Values of total recoverable iron suggest that, because of adsorption onto sediments in impoundments, some constituents are not accurately described by sampling below impoundments. Relations between water quality constituents and flow at stations on the Clinch River and Tennessee River are not well defined due to regulation. Direct load computations for many constituents were therefore not possible, which diminished the utility of data from these NASQAN stations to account for quantity versus quality of the water. Load computations were only possible for ionic constituents through use of a continuous specific conductance record as an intermediary. Rivers might reflect the decreasing trend in discharge during the 1972-82 water years. Thus the stations below Watts Bar Dam and below Melton Hill Dam do not adequately meet the NASQAN objective to detect and assess long-term changes in stream quality. (Lantz-PTT)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854171","usgsCitation":"Evaldi, R., and Lewis, J., 1986, Water-quality appraisal of NASQAN stations below impoundments, eastern Tennessee: U.S. Geological Survey Water-Resources Investigations Report 85-4171, v, 50 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854171.","productDescription":"v, 50 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":2180,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri85-4171","linkFileType":{"id":5,"text":"html"}},{"id":124347,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4171/report-thumb.jpg"},{"id":55889,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4171/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e4870","contributors":{"authors":[{"text":"Evaldi, R. D.","contributorId":93909,"corporation":false,"usgs":true,"family":"Evaldi","given":"R. D.","affiliations":[{"id":595,"text":"U.S. Geological Survey","active":false,"usgs":true}],"preferred":false,"id":197390,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lewis, J.G.","contributorId":32570,"corporation":false,"usgs":true,"family":"Lewis","given":"J.G.","email":"","affiliations":[],"preferred":false,"id":197389,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26958,"text":"wri864344 - 1986 - Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","interactions":[],"lastModifiedDate":"2021-12-21T20:55:50.903688","indexId":"wri864344","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":"86-4344","title":"Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado","docAbstract":"Sources of sediment data collected by several government agencies through water year 1984 are summarized for Colorado. The U.S. Geological Survey has collected suspended-sediment data at 243 sites; these data are stored in the U.S. Geological Survey 's water data storage and retrieval system. The U.S. Forest Service has collected suspended-sediment and bedload data at an additional 225 sites, and most of these data are stored in the U.S. Environmental Protection Agency 's water-quality-control information system. Additional unpublished sediment data are in the possession of the collecting entities. Annual suspended-sediment loads were computed for 133 U.S. Geological Survey sediment-data-collection sites using the daily mean water-discharge/sediment-transport-curve method. Sediment-transport curves were derived for each site by one of three techniques: (1) Least-squares linear regression of all pairs of suspended-sediment and corresponding water-discharge data, (2) least-squares linear regression of data sets subdivided on the basis of hydrograph season; and (3) graphical fit to a logarithm-logarithm plot of data. The curve-fitting technique used for each site depended on site-specific characteristics. Sediment-data sources and estimates of annual loads of suspended, bed, and total sediment from several other reports also are summarized. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri864344","usgsCitation":"Elliott, J.G., and DeFeyter, K.L., 1986, Sediment-data sources and estimated annual suspended-sediment loads of rivers and streams in Colorado: U.S. Geological Survey Water-Resources Investigations Report 86-4344, Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches, https://doi.org/10.3133/wri864344.","productDescription":"Report: vii, 148 p.; 2 Plates: 26.86 × 21.85 inches and 26.94 × 22.40 inches","costCenters":[],"links":[{"id":55844,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55843,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1986/4344/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":55845,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1986/4344/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158134,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1986/4344/report-thumb.jpg"},{"id":393252,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36657.htm"}],"country":"United States","state":"Colorado","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -109.039306640625,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              37.01132594307015\n            ],\n            [\n              -102.06298828125,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              41.00477542222947\n            ],\n            [\n              -109.039306640625,\n              37.01132594307015\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e499fe4b07f02db5bd219","contributors":{"authors":[{"text":"Elliott, J. G.","contributorId":45341,"corporation":false,"usgs":true,"family":"Elliott","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":197315,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"DeFeyter, K. L.","contributorId":53425,"corporation":false,"usgs":true,"family":"DeFeyter","given":"K.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197316,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":27242,"text":"wri854147 - 1986 - Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","interactions":[],"lastModifiedDate":"2022-08-23T19:38:27.291403","indexId":"wri854147","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":"85-4147","title":"Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980","docAbstract":"<p>Lahontan Reservoir is a major recreational site in the Carson River basin in western Nevada. The reservoir is fed by the Carson River and by the Truckee Canal which transports water from the adjacent Truckee River. Water quality in both rivers is influenced by agriculture and urbanization. Specific conductance tended to increase in a downstream direction. Generally, pH values ranged from 7.0 to 8.8. Dissolved-oxygen concentrations were greater than 5 milligrams/L. Calcium and sodium were the dominant cations and bicarbonate the dominant anion. Suspended-sediment concentrations ranged from 3 to 1,790 milligrams/L. Ultimate carbonaceous biochemical oxygen demand ranged from 1.2 to 19.6 milligrams/L. The codominant algal groups were the blue-greens, greens, and diatoms. Background total nutrient and suspended-sediment loads were about 490 tons nitrogen, 130 tons phosphorus, and 200,000 tons suspended sediment. Total nutrient and suspended-sediment loads to Lahontan Reservoir were about 980 tons nitrogen, 300 tons phosphorus, and 300,000 tons suspended sediment. Loads to the lower Carson River from the reservoir were about 820 tons total nitrogen, 180 tons total phosphorus, and 26,000 tons suspended sediment.&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri854147","usgsCitation":"Garcia, K.T., and Carman, R.L., 1986, Water-quality characteristics and nutrient and suspended-sediment loads, Carson River and Truckee Canal, western Nevada, water year 1980: U.S. Geological Survey Water-Resources Investigations Report 85-4147, vii, 107 p., https://doi.org/10.3133/wri854147.","productDescription":"vii, 107 p.","costCenters":[],"links":[{"id":405483,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_36310.htm","linkFileType":{"id":5,"text":"html"}},{"id":56105,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4147/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":158744,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4147/report-thumb.jpg"}],"country":"United States","state":"Nevada","otherGeospatial":"Carson River and Truckee Canal","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -120,\n              38.717\n            ],\n            [\n              -119,\n              38.717\n            ],\n            [\n              -119,\n              39.6\n            ],\n            [\n              -120,\n              39.6\n            ],\n            [\n              -120,\n              38.717\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e48cce4b07f02db544586","contributors":{"authors":[{"text":"Garcia, K. T.","contributorId":52613,"corporation":false,"usgs":true,"family":"Garcia","given":"K.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":197784,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Carman, R. L.","contributorId":16460,"corporation":false,"usgs":true,"family":"Carman","given":"R.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":197783,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":35462,"text":"b1587 - 1986 - Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida","interactions":[],"lastModifiedDate":"2012-02-02T00:09:45","indexId":"b1587","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1986","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":306,"text":"Bulletin","code":"B","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"1587","title":"Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1587","usgsCitation":"Patterson, S.H., Cameron, C.C., and Schmidt, W., 1986, Geology and mineral-resource potential of Seven Roadless Areas in the Apalachicola National Forest, Liberty County, Florida: U.S. Geological Survey Bulletin 1587, vi, 21 p. ill, maps ;28 cm., https://doi.org/10.3133/b1587.","productDescription":"vi, 21 p. ill, maps ;28 cm.","costCenters":[],"links":[{"id":164645,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1587/report-thumb.jpg"},{"id":63359,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1587/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b32e4b07f02db6b4733","contributors":{"authors":[{"text":"Patterson, Sam H.","contributorId":62996,"corporation":false,"usgs":true,"family":"Patterson","given":"Sam","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":214686,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cameron, Cornelia Clermont","contributorId":20737,"corporation":false,"usgs":true,"family":"Cameron","given":"Cornelia","email":"","middleInitial":"Clermont","affiliations":[],"preferred":false,"id":214684,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmidt, Walter","contributorId":21612,"corporation":false,"usgs":true,"family":"Schmidt","given":"Walter","email":"","affiliations":[],"preferred":false,"id":214685,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
]}