{"pageNumber":"4527","pageRowStart":"113150","pageSize":"25","recordCount":165626,"records":[{"id":1675,"text":"wsp2271 - 1985 - Pesticides in the nation's rivers, 1975-1980, and implications for future monitoring","interactions":[],"lastModifiedDate":"2012-02-02T00:05:23","indexId":"wsp2271","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2271","title":"Pesticides in the nation's rivers, 1975-1980, and implications for future monitoring","docAbstract":"Water samples were taken four times per year and bed-sediment samples two times per year during 1975-80 at 160 to 180 stations on major rivers of the United States. Samples were analyzed for 18 insecticides and 4 herbicides, which together accounted for about one-third of the total amount of all pesticides applied to major crops during 1975-80. Fewer than 10 percent of almost 3,000 water samples and fewer than 20 percent of almost 1,000 bed-sediment samples contained reportable concentrations of any of the compounds. The patterns of detection result from a combination of widely variable detection capabilities, chemical properties, and use. Most detections in water samples were of relatively persistent yet soluble compounds: atrazine (4.8 percent of samples), diazinon (1.2), and lindane (1.1). Most detections in bed-sediment samples were of the hydrophobic and persistent insecticides: DDE (17 percent of samples), DDD (12), dieldrin (12), chlordane (9.9), and DDT (8.5). Only for atrazine in water, and for DDE, DDD, DDT, and chlordane in bed sediments, were geographic patterns of detection correlated (pH<0.10) with use on farms. Detections of organochlorine insecticides in both water and bed sediments appear to have erratically but gradually decreased during 1975-80. For the 1975-79 period, more stations had downtrends than had uptrends in bed-sediment levels of organochlorines. No clear trends were evident in concentrations of organophosphate insecticides or herbicides in either water or bed sediments. Findings suggest that future pesticide monitoring efforts must be responsive to changes in pesticides used and to geographic patterns of use. Different types of monitoring approaches are necesssary for chemicals having different chemical and physical properties. Before an effective dynamic monitoring effort can be designed, however, selected case studies are needed to characterize and refine sampling and analytical capabilities for different types of chemicals, river environments, and sample types.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2271","usgsCitation":"Gilliom, R.J., Alexander, R.B., and Smith, R.A., 1985, Pesticides in the nation's rivers, 1975-1980, and implications for future monitoring: U.S. Geological Survey Water Supply Paper 2271, iv, 26 p. :ill., maps ;28 cm., https://doi.org/10.3133/wsp2271.","productDescription":"iv, 26 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":138236,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2271/report-thumb.jpg"},{"id":26750,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2271/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b23e4b07f02db6ae018","contributors":{"authors":[{"text":"Gilliom, Robert J. rgilliom@usgs.gov","contributorId":488,"corporation":false,"usgs":true,"family":"Gilliom","given":"Robert","email":"rgilliom@usgs.gov","middleInitial":"J.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true}],"preferred":true,"id":143955,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Alexander, Richard B. 0000-0001-9166-0626 ralex@usgs.gov","orcid":"https://orcid.org/0000-0001-9166-0626","contributorId":541,"corporation":false,"usgs":true,"family":"Alexander","given":"Richard","email":"ralex@usgs.gov","middleInitial":"B.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true}],"preferred":true,"id":143956,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Smith, Richard A. 0000-0003-2117-2269 rsmith1@usgs.gov","orcid":"https://orcid.org/0000-0003-2117-2269","contributorId":580,"corporation":false,"usgs":true,"family":"Smith","given":"Richard","email":"rsmith1@usgs.gov","middleInitial":"A.","affiliations":[{"id":451,"text":"National Water Quality Assessment Program","active":true,"usgs":true},{"id":503,"text":"Office of Water Quality","active":true,"usgs":true},{"id":37778,"text":"WMA - Integrated Modeling and Prediction Division","active":true,"usgs":true}],"preferred":true,"id":143957,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40565,"text":"ofr8032 - 1985 - Federal coal resource occurrence and coal development potential maps of the Samson Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:51","indexId":"ofr8032","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"80-32","title":"Federal coal resource occurrence and coal development potential maps of the Samson Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr8032","usgsCitation":"Berge Exploration Inc., 1985, Federal coal resource occurrence and coal development potential maps of the Samson Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 80-32, 12 maps, 2 data sheets :photocopy ;58 x 47 cm. +1 pamphlet (ii, 33 leaves : ill., maps ; 28 cm.), https://doi.org/10.3133/ofr8032.","productDescription":"12 maps, 2 data sheets :photocopy ;58 x 47 cm. +1 pamphlet (ii, 33 leaves : ill., maps ; 28 cm.)","costCenters":[],"links":[{"id":171865,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0032/report-thumb.jpg"},{"id":76609,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-01.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76610,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-02.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76611,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-03.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76612,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-04.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76613,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-05.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76614,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-06.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76615,"rank":406,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-07.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76616,"rank":407,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-08.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76617,"rank":408,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-09.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76618,"rank":409,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-10.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76619,"rank":410,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-11.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76620,"rank":411,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-12.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76621,"rank":412,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-13.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76622,"rank":413,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0032/plate-14.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":76623,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0032/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6c89","contributors":{"authors":[{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":530326,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":2128,"text":"wsp2259 - 1985 - The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah","interactions":[{"subject":{"id":19845,"text":"ofr8467 - 1984 - The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah","indexId":"ofr8467","publicationYear":"1984","noYear":false,"title":"The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah"},"predicate":"SUPERSEDED_BY","object":{"id":2128,"text":"wsp2259 - 1985 - The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah","indexId":"wsp2259","publicationYear":"1985","noYear":false,"title":"The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah"},"id":1}],"lastModifiedDate":"2017-08-31T17:07:40","indexId":"wsp2259","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2259","title":"The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah","docAbstract":"<p>The ground-water system was studied in the Trail Mountain area in order to provide hydrologic information needed to assess the hydrologic effects of underground coal mining. Well testing and spring data indicate that water occurs in several aquifers. The coal-bearing Blackhawk-Star Point aquifer is regional in nature and is the source of most water in underground mines in the region. One or more perched aquifers overlie the Blackhawk-Star Point aquifer in most areas of Trail Mountain.</p><p>Aquifer tests indicate that the transmissivity of the Blackhawk-Star Point aquifer, which consists mainly of sandstone, siltstone, and shale, ranges from about 20 to 200 feet squared per day in most areas of Trail Mountain. The specific yield of the aquifer was estimated at 0.05, and the storage coefficient is about IxlO\"6 per foot of aquifer where confined.</p><p>The main sources of recharge to the multiaquifer system are snowmelt and rain, and water is discharged mainly by springs and by leakage along streams. Springs that issue from perched aquifers are sources of water for livestock and wildlife on Trail Mountain.</p><p>Water in all aquifers is suitable for most uses. Dissolved solids concentrations range from about 250 to 700 milligrams per liter, and the predominant dissolved constituents generally are calcium, magnesium, and bicarbonate.</p><p> Future underground coal mines will require dewatering when they penetrate the Blackhawk-Star Point aquifer. A finitedifference, three-dimensional computer model was used to estimate the inflow of water to various lengths and widths of a hypothetical dewatered mine and to estimate drawdowns of potentiometric surfaces in the partly dewatered aquifer. The estimates were made for a range of aquifer properties and premining hydraulic gradients that were similar to those on Trail Mountain. The computer simulations indicate that mine inflows could be several hundred gallons per minute and that potentiometric surfaces of the partly dewatered aquifer could be drawn down by several hundred feet during a reasonable life span of a mine. Because the Blackhawk-Star Point aquifer is separated from overlying perched aquifers by an unsaturated zone, mine dewatering alone would not affect perched aquifers. Mine dewatering would not significantly change water quality in the Blackhawk-Star Point aquifer. </p><p>Subsidence will occur above future underground mines, but the effects on the ground-water system cannot be quantified. Subsidence fractures possibly could extend from the roof of a mine into a perched aquifer several hundred feet above. Such fractures would increase down ward percolation of water through the perching bed, and spring discharge from the perched aquifer could decrease. Flow through subsidence fractures also could increase recharge to the Blackhawk-Star Point aquifer and increase inflows to underground mines.  </p>","language":"English","publisher":"U.S. Government Printing Office","publisherLocation":"Washington, D.C.","doi":"10.3133/wsp2259","collaboration":"Prepared in cooperation with the U.S. Bureau of Land Management","usgsCitation":"Lines, G.C., 1985, The ground-water system and possible effects of underground coal mining in the Trail Mountain area, central Utah: U.S. Geological Survey Water Supply Paper 2259, v, 32 p., https://doi.org/10.3133/wsp2259.","productDescription":"v, 32 p.","numberOfPages":"38","costCenters":[{"id":610,"text":"Utah Water Science Center","active":true,"usgs":true}],"links":[{"id":27728,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2259/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138279,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2259/report-thumb.jpg"}],"country":"United States","state":"Utah","otherGeospatial":"Trail Mountain","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a2ae4b07f02db612291","contributors":{"authors":[{"text":"Lines, Gregory C.","contributorId":50502,"corporation":false,"usgs":true,"family":"Lines","given":"Gregory","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":144711,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":38486,"text":"pp1402D - 1985 - Freshwater heads and ground-water temperatures in aquifers of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming","interactions":[],"lastModifiedDate":"2012-02-02T00:09:50","indexId":"pp1402D","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":331,"text":"Professional Paper","code":"PP","onlineIssn":"2330-7102","printIssn":"1044-9612","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"1402","chapter":"D","title":"Freshwater heads and ground-water temperatures in aquifers of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming","language":"ENGLISH","doi":"10.3133/pp1402D","usgsCitation":"Lobmeyer, D., 1985, Freshwater heads and ground-water temperatures in aquifers of the Northern Great Plains in parts of Montana, North Dakota, South Dakota, and Wyoming: U.S. Geological Survey Professional Paper 1402, p. D1-D11; 1 plate in pocket, https://doi.org/10.3133/pp1402D.","productDescription":"p. D1-D11; 1 plate in pocket","costCenters":[],"links":[{"id":123104,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/pp/1402d/report-thumb.jpg"},{"id":65152,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/pp/1402d/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":65153,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/pp/1402d/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b1ae4b07f02db6a8620","contributors":{"authors":[{"text":"Lobmeyer, D.H.","contributorId":106502,"corporation":false,"usgs":true,"family":"Lobmeyer","given":"D.H.","affiliations":[],"preferred":false,"id":219916,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16677,"text":"ofr85662 - 1985 - Stable-isotope study of volcanogenic- and sedimentary-manganese deposits","interactions":[],"lastModifiedDate":"2012-02-02T00:07:18","indexId":"ofr85662","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-662","title":"Stable-isotope study of volcanogenic- and sedimentary-manganese deposits","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85662","usgsCitation":"Yeh, H., Hein, J., and Koski, R., 1985, Stable-isotope study of volcanogenic- and sedimentary-manganese deposits: U.S. Geological Survey Open-File Report 85-662, 16 p. ;28 cm., https://doi.org/10.3133/ofr85662.","productDescription":"16 p. ;28 cm.","costCenters":[],"links":[{"id":150526,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0662/report-thumb.jpg"},{"id":45734,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0662/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e1e4b07f02db5e490f","contributors":{"authors":[{"text":"Yeh, Hsueh-Wen","contributorId":11786,"corporation":false,"usgs":true,"family":"Yeh","given":"Hsueh-Wen","email":"","affiliations":[],"preferred":false,"id":173270,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hein, J.R. 0000-0002-5321-899X","orcid":"https://orcid.org/0000-0002-5321-899X","contributorId":61429,"corporation":false,"usgs":true,"family":"Hein","given":"J.R.","affiliations":[],"preferred":false,"id":173272,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Koski, R.A.","contributorId":16006,"corporation":false,"usgs":true,"family":"Koski","given":"R.A.","email":"","affiliations":[],"preferred":false,"id":173271,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":25598,"text":"wri854166 - 1985 - Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana","interactions":[],"lastModifiedDate":"2016-06-01T10:15:07","indexId":"wri854166","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4166","title":"Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana","docAbstract":"<p>Agricultural irrigation in northern Indiana has increased rapidly since 1975 and might double by the year 2000. A 16.5 square-mile area in north-central Indiana was studied to determine possible effects of increased irrigation on local water supply. In 1982, an average of 2 inches of water was used to irrigate 975 acres of sandy soil overlying highly transmissive outwash deposits. Irrigational pumpage was 75 percent of the summer water use but was less than potential irrigational pumpage because (1) only one-third of the suitable land was irrigated, and (2) precipitation was near normal for the year.</p>\n<p>A three-dimensional digital flow model, calibrated with data collected in 1982, was used to simulate four hypothetical pumping plans representing various irrigational schemes and possible rainfall conditions: (1) 1982 acreage irrigated and 1982 (above normal) precipitation; (2) 1982 acreage irrigated and below-normal precipitation; (3) maximum acreage irrigated and normal precipitation; and (4) maximum acreage irrigated and below-normal precipitation. A fifth pumping plan was used to simulate maximum year-round water use. Plan 5 was not designed to simulate irrigational development but rather a maximum rate of withdrawal sustainable year-round until steady-state is reached.</p>\n<p>Of the four pumping plans that simulated irrigational pumpage, plan 4 had the greatest effect on ground- and surface-water supply. Compared with 1982 pumpage, this plan represented a thirteenfold increase in the volume of water pumped for irrigation from wells and from Turkey Creek, a stream bordering the area of study. The model predicted a potentiometric decline of as much as 20.7 feet over an 8-acre area of the aquifer. This decline was one-fourth of the available drawdown and would not dewater the source aquifer. Streamflow in Turkey Creek would be reduced 39 percent by simulated ground-water and surface-water pumpage but remaining flow would still be twice the 7-day, 10-year low flow. However, the model predicted that flow in two smaller streams would be reduced to zero.</p>\n<p>The rate of pumping used in plan 5 was nearly 4 times the pumping rate in 1982. Potentiometric decline for plan 5 was as much as 40 percent of available drawdown, and predicted streamflow reduction would cause flow in Turkey Creek to decrease below the 7-day, 10-year low flow.</p>\n<p>Results of plans 1, 2, 3, and 4 indicate that the outwash system provides adequate water for current (1982) needs and substantial growth for irrigation. However, maximum irrigational development might cause temporary, local competition for water in several parts of the area. Plan 5 indicates .that water use could increase substantially before effects of pumping would prevail year-round.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Indianapolis, IN","doi":"10.3133/wri854166","collaboration":"Indiana Department of Natural Resources","usgsCitation":"Lindgren, H., Peters, J.G., Cohen, D., and Crompton, E., 1985, Hydrologic effects of ground- and surface-water withdrawals in the Milford area, Elkhart and Kosciusko counties, Indiana: U.S. Geological Survey Water-Resources Investigations Report 85-4166, vi, 75 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854166.","productDescription":"vi, 75 p. :ill., maps ;28 cm.","startPage":"1","endPage":"75","numberOfPages":"81","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":346,"text":"Indiana Water Science Center","active":true,"usgs":true}],"links":[{"id":54342,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4166/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":126873,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4166/report-thumb.jpg"}],"country":"United States","state":"Indiana","county":"Elkhart, Kosciusko","geographicExtents":"{\"type\":\"FeatureCollection\",\"features\":[{\"type\":\"Feature\",\"geometry\":{\"type\":\"Polygon\",\"coordinates\":[[[-85.7874,41.7615],[-85.7591,41.7613],[-85.6606,41.7608],[-85.6589,41.699],[-85.6575,41.6122],[-85.6554,41.5251],[-85.6542,41.4733],[-85.6552,41.4384],[-85.6538,41.3521],[-85.6527,41.2949],[-85.6518,41.2668],[-85.6522,41.1787],[-85.6876,41.179],[-85.6856,41.0896],[-85.6849,41.0465],[-85.9457,41.0424],[-86.017,41.0414],[-86.0179,41.0863],[-86.0758,41.0851],[-86.0777,41.1736],[-86.0539,41.1735],[-86.0574,41.3033],[-86.059,41.4336],[-86.059,41.4367],[-86.0594,41.4644],[-86.0593,41.474],[-86.0593,41.479],[-86.0592,41.4935],[-86.0598,41.4999],[-86.0624,41.7619],[-85.932,41.7623],[-85.7874,41.7615]]]},\"properties\":{\"name\":\"Elkhart\",\"state\":\"IN\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a1be4b07f02db607040","contributors":{"authors":[{"text":"Lindgren, H.A.","contributorId":85627,"corporation":false,"usgs":true,"family":"Lindgren","given":"H.A.","email":"","affiliations":[],"preferred":false,"id":194358,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peters, J. G.","contributorId":56216,"corporation":false,"usgs":true,"family":"Peters","given":"J.","email":"","middleInitial":"G.","affiliations":[],"preferred":false,"id":194356,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Cohen, D.A.","contributorId":17628,"corporation":false,"usgs":true,"family":"Cohen","given":"D.A.","email":"","affiliations":[],"preferred":false,"id":194355,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Crompton, E. J.","contributorId":70412,"corporation":false,"usgs":true,"family":"Crompton","given":"E. J.","affiliations":[],"preferred":false,"id":194357,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}}
,{"id":43549,"text":"ofr8555 - 1985 - Land use and land cover and associated maps for Hancock, Michigan","interactions":[],"lastModifiedDate":"2012-02-02T00:10:28","indexId":"ofr8555","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-55","title":"Land use and land cover and associated maps for Hancock, Michigan","language":"ENGLISH","doi":"10.3133/ofr8555","usgsCitation":"Water Resources Division, U.S. Geological Survey, 1985, Land use and land cover and associated maps for Hancock, Michigan: U.S. Geological Survey Open-File Report 85-55, 5 maps :photocopy ;45 x 77 cm., on sheet 77 x 107 cm., https://doi.org/10.3133/ofr8555.","productDescription":"5 maps :photocopy ;45 x 77 cm., on sheet 77 x 107 cm.","costCenters":[],"links":[{"id":172333,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4b28e4b07f02db6b110d","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":531234,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16118,"text":"ofr85446 - 1985 - Preliminary report on and measured sections of the Middle Jurassic Entrada Sandstone and Wanakah Formation near Placerville, southwestern Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:08","indexId":"ofr85446","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-446","title":"Preliminary report on and measured sections of the Middle Jurassic Entrada Sandstone and Wanakah Formation near Placerville, southwestern Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85446","usgsCitation":"Steele, B., 1985, Preliminary report on and measured sections of the Middle Jurassic Entrada Sandstone and Wanakah Formation near Placerville, southwestern Colorado: U.S. Geological Survey Open-File Report 85-446, i, 57 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr85446.","productDescription":"i, 57 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":148258,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0446/report-thumb.jpg"},{"id":45042,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0446/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4afbe4b07f02db696381","contributors":{"authors":[{"text":"Steele, B.A.","contributorId":78330,"corporation":false,"usgs":true,"family":"Steele","given":"B.A.","email":"","affiliations":[],"preferred":false,"id":172264,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":60922,"text":"mf1383F - 1985 - Mineral deposits and probability of exploration, Medford 1 degree by 2 degrees Quadrangle, Oregon and California","interactions":[],"lastModifiedDate":"2012-02-10T00:10:22","indexId":"mf1383F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1383","chapter":"F","title":"Mineral deposits and probability of exploration, Medford 1 degree by 2 degrees Quadrangle, Oregon and California","language":"ENGLISH","doi":"10.3133/mf1383F","usgsCitation":"Smith, R.M., and Peterson, J., 1985, Mineral deposits and probability of exploration, Medford 1 degree by 2 degrees Quadrangle, Oregon and California: U.S. Geological Survey Miscellaneous Field Studies Map 1383, 4 maps ;44 x 66 cm., on sheets 61 x 95 cm. and 61 x 84 cm. folded in envelope 25 x 32 cm. +1 pamphlet (33 p. ; 28 cm.), https://doi.org/10.3133/mf1383F.","productDescription":"4 maps ;44 x 66 cm., on sheets 61 x 95 cm. and 61 x 84 cm. folded in envelope 25 x 32 cm. +1 pamphlet (33 p. ; 28 cm.)","costCenters":[],"links":[{"id":183708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":88897,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1985/1383f/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88898,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1985/1383f/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88899,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1985/1383f/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":88900,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1985/1383f/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,42 ], [ -124,43 ], [ -122,43 ], [ -122,42 ], [ -124,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a61e4b07f02db635985","contributors":{"authors":[{"text":"Smith, R. M.","contributorId":31816,"corporation":false,"usgs":true,"family":"Smith","given":"R.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":264621,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Peterson, J.A.","contributorId":76308,"corporation":false,"usgs":true,"family":"Peterson","given":"J.A.","email":"","affiliations":[],"preferred":false,"id":264622,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":61287,"text":"mf1692 - 1985 - Map showing depth to bedrock in the Seattle 30' by 60' Quadrangle, Washington","interactions":[],"lastModifiedDate":"2016-08-18T08:54:55","indexId":"mf1692","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1692","title":"Map showing depth to bedrock in the Seattle 30' by 60' Quadrangle, Washington","docAbstract":"<p>Maps depicting thicknesses of sedimentary units (isopach maps) are standard tools for interpretation of processes and patterns of sedimentation within basins (Potter and Pettijohn, 1977, p. 283-287). Isopach maps showing the thickness of unconsolidated sedimentary deposits overlying bedrock may help locate sources of aggregate and potential ground-water aquifers. These maps also aid in the prediction of ground response resulting from earthquakes (Hays, 1980). In the Puget Lowland this latter use is of particular importance. Strong ground motions were highly variable throughout the Puget Sound area during the 1965 Seattle earthquake (M<sub>s</sub> = 6.5); complex topography of the bedrock surface plus thick sections of young unconsolidated and semiconsolidated sediment were responsible for this variability (Langston, 1981; Shakel and Toksoz, 1980). Hall and Othberg (1974) outlined the major patterns of unconsolidated sediment accumulation in Puget Sound, including the unusually thick Sedimentary deposits beneath the city of Seattle.</p>\n<p>Since Hall and Othberg's 1971, study, new geotechnical drilling and marine seismic reflection profiling information have become available and were used to prepare this map, which shows the depth to bedrock in the Seattle 30' by 60' quadrangle (scale 1:100,000). The map shows bedrock depth, in meters, beneath the land surface or the sediment-sea water interface.</p>\n<p>Bedrock throughout the Seattle quadrangle is presumed to be volcanic rock, conglomerate, Sandstone, or Shale and is Tertiary in age. With the exception of a few reports of age or lithology collected from oil wells (Livingston, 1958), the subsurface information used for this map sheds little light on the nature and distribution of the various Tertiary rocks in the subsurface. It is assumed, on the basis of pronounced lithologic differences in drill holes and widespread unconformable relationships with underlying bedrock units seen in marine seismic reflection profiles, that the deposits overlying bedrock are Quaternary in age, but no direct dating of materials has been done to confirm this assumption.</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1692","usgsCitation":"Yount, J.C., Dembroff, G., and Barats, G., 1985, Map showing depth to bedrock in the Seattle 30' by 60' Quadrangle, Washington: U.S. Geological Survey Miscellaneous Field Studies Map 1692, Plate: 40.63 x 39.48 inches, https://doi.org/10.3133/mf1692.","productDescription":"Plate: 40.63 x 39.48 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":326350,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1692.JPG"},{"id":326777,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1692/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"0","country":"United States","state":"Washington","city":"Seattle","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -123,47.5 ], [ -123,48 ], [ -122,48 ], [ -122,47.5 ], [ -123,47.5 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a9ee4b07f02db660374","contributors":{"authors":[{"text":"Yount, J. C.","contributorId":69553,"corporation":false,"usgs":true,"family":"Yount","given":"J.","middleInitial":"C.","affiliations":[],"preferred":false,"id":265327,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Dembroff, G.R.","contributorId":9224,"corporation":false,"usgs":true,"family":"Dembroff","given":"G.R.","affiliations":[],"preferred":false,"id":265325,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Barats, G.M.","contributorId":29789,"corporation":false,"usgs":true,"family":"Barats","given":"G.M.","email":"","affiliations":[],"preferred":false,"id":265326,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":3567,"text":"cir943 - 1985 - Petroleum geology and resources of northeastern Mexico","interactions":[{"subject":{"id":10676,"text":"ofr83712 - 1983 - Petroleum geology and resources of northeastern Mexico","indexId":"ofr83712","publicationYear":"1983","noYear":false,"title":"Petroleum geology and resources of northeastern Mexico"},"predicate":"SUPERSEDED_BY","object":{"id":3567,"text":"cir943 - 1985 - Petroleum geology and resources of northeastern Mexico","indexId":"cir943","publicationYear":"1985","noYear":false,"title":"Petroleum geology and resources of northeastern Mexico"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:21","indexId":"cir943","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"943","title":"Petroleum geology and resources of northeastern Mexico","docAbstract":"Petroleum deposits (primarily gas) in northeastern Mexico occur in two main basins, the Tertiary Burgos basin and the Mesozoic Sabinas basin. About 90 gas fields are present in the Burgos basin, which has undergone active exploration for the past 30-40 years. Production in this basin is from Oligocene and Eocene nearshore marine and deltaic sandstone reservoirs. Most of the fields are small to medium in size on faulted anticlinal or domal structures, some of which may be related to deep-seated salt intrusion. Cumulative production from these fields is about 4 trillion cubic feet gas and 100 million barrels condensate and oil. Since 1975, about 10 gas fields, some with large production rates, have been discovered in Cretaceous carbonate and Jurassic sandstone reservoirs in the Sabinas basin and adjacent Burro-Picachos platform areas. The Sabinas basin, which is in the early stages of exploration and development, may have potential for very large gas reserves. \r\n\r\nThe Sabinas basin is oriented northwesterly with a large number of elongate northwest- or west-trending asymmetric and overturned Laramide anticlines, most of which-are faulted. Some of the structures may be related to movement of Jurassic salt or gypsum. Lower Cretaceous and in some cases Jurassic rocks are exposed in the centers of the larger anticlines, and Upper Cretaceous rocks are exposed in much of the remainder of the basin. A thick section of Upper Cretaceous clastic rocks is partly exposed in tightly folded and thrust-faulted structures of the west-east oriented, deeply subsided Parras basin, which lies south of the Sabinas basin and north of the Sierra Madre Oriental fold and thrust belt south and west of Monterrey. \r\n\r\nThe sedimentary cover of Cretaceous and Jurassic rocks in the Sabinas and Parras basins ranges from about 1,550 m (5,000 ft) to 9,000 m (30,000 ft) in thickness. Upper Jurassic rocks are composed of carbonate and dark organic shaly or sandy beds underlain by an unknown thickness of Late Jurassic and older redbed clastics and evaporites, including halite. Lower Cretaceous rocks are mainly platform carbonate and fine clastic beds with some evaporites (gypsum or anhydrite) deposited in two main rudist reef-bearing carbonate cycles. Upper Cretaceous rocks are mainly continental and marine clastic beds related to early development of the Laramide orogeny. This Upper Cretaceous sequence contains a marine shale and deltaic clastic complex as much as 6,000 m (20,000 ft) or more thick in the Parras basin, which grades northward and eastward to open marine, fine clastic beds. The Burgos basin, which is an extension of the Rio Grande embayment of the western Gulf of Mexico basin province, contains an eastward-thickening wedge of Tertiary continental and marine clastics. These beds are about 1,550 to 3,000 m (5,000-10,000 ft) thick in the outcrop belt on the west side of the basin and thicken to more than 16,000 m (50,000 ft) near the Gulf Coast.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/cir943","usgsCitation":"Peterson, J.A., 1985, Petroleum geology and resources of northeastern Mexico: U.S. Geological Survey Circular 943, vi, 30 p. :ill., maps ;26 cm., https://doi.org/10.3133/cir943.","productDescription":"vi, 30 p. :ill., maps ;26 cm.","costCenters":[],"links":[{"id":124747,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1985/0943/report-thumb.jpg"},{"id":30595,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1985/0943/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a91e4b07f02db65697c","contributors":{"authors":[{"text":"Peterson, James A.","contributorId":106872,"corporation":false,"usgs":true,"family":"Peterson","given":"James","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":147167,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":35421,"text":"b1630 - 1985 - Earthquake hazards in the offshore environment","interactions":[],"lastModifiedDate":"2012-02-02T00:09:48","indexId":"b1630","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1630","title":"Earthquake hazards in the offshore environment","language":"ENGLISH","publisher":"U.S. Geological Survey : for sale by the Supt. of Docs, U.S. G.P.O.,","doi":"10.3133/b1630","usgsCitation":"Page, R.A., and Basham, P., 1985, Earthquake hazards in the offshore environment: U.S. Geological Survey Bulletin 1630, v, 69 p. ill., maps ;28 cm., https://doi.org/10.3133/b1630.","productDescription":"v, 69 p. ill., maps ;28 cm.","costCenters":[],"links":[{"id":164664,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1630/report-thumb.jpg"},{"id":63310,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1630/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a51e4b07f02db6297ef","contributors":{"authors":[{"text":"Page, Robert A.","contributorId":17207,"corporation":false,"usgs":true,"family":"Page","given":"Robert","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":214605,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Basham, P.W.","contributorId":90800,"corporation":false,"usgs":true,"family":"Basham","given":"P.W.","email":"","affiliations":[],"preferred":false,"id":214606,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":26936,"text":"wri854162 - 1985 - Sources of water and nitrogen to the Widefield Aquifer, southwestern El Paso County, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri854162","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4162","title":"Sources of water and nitrogen to the Widefield Aquifer, southwestern El Paso County, Colorado","docAbstract":"The Widefield aquifer near Colorado Springs, Colorado, is recharged primarily by Fountain Creek and, to a lesser extent, by infiltration and percolation of water from the land surface and from groundwater inflow. During the past 20 to 30 years, concentrations of nitrate (as nitrogen) in the Widefield aquifer have increased from 0.5 to 3.0 milligrams/L to nearly 10 milligrams/L, and occasionally exceed the drinking-water standard of 10 milligrams/L as nitrogen. During the summer of 1982, the concentrations of nitrite plus nitrate as nitrogen in water in the aquifer ranged from 3.2 to 15 milligrams/L with a mean concentration of 6.9 milligrams/L. In general, the nitrite-plus-nitrate concentrations are greatest near the north end of the aquifer, probably resulting from effluent from Colorado Springs Sewage Treatment Plant being discharged to Fountain Creek. During 1982, 93% of the total estimated 160 tons of nitrogen available to enter the Widefield aquifer was from the Colorado Springs Sewage Treatment Plant. However, a significant proportion of this nitrogen may have been lost through denitrification. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854162","usgsCitation":"Edelmann, P., and Cain, D., 1985, Sources of water and nitrogen to the Widefield Aquifer, southwestern El Paso County, Colorado: U.S. Geological Survey Water-Resources Investigations Report 85-4162, v, 81 p. :ill., maps ;28 cm., https://doi.org/10.3133/wri854162.","productDescription":"v, 81 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":158435,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4162/report-thumb.jpg"},{"id":55827,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4162/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e6e4b07f02db5e758a","contributors":{"authors":[{"text":"Edelmann, Patrick","contributorId":86305,"corporation":false,"usgs":true,"family":"Edelmann","given":"Patrick","affiliations":[],"preferred":false,"id":197276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Cain, Doug","contributorId":101655,"corporation":false,"usgs":true,"family":"Cain","given":"Doug","email":"","affiliations":[],"preferred":false,"id":197277,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":3191,"text":"wsp2185F - 1985 - Water quality of North Carolina streams – Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80 – Variability, loads, and trends of selected constituents","interactions":[],"lastModifiedDate":"2021-11-22T22:43:58.480554","indexId":"wsp2185F","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2185","chapter":"F","title":"Water quality of North Carolina streams – Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80 – Variability, loads, and trends of selected constituents","docAbstract":"<p>Historical water-quality data collected by the U.S. Geological Survey from the Cape Fear River at Lock 1, near Kelly, North Carolina, show increasing concentrations of total-dissolved solids, specific conductance, sulfate, chloride, nitrite plus nitrate nitrogen, magnesium, sodium, and potassium during the past 25 years. Silica and pH show decreasing trends during the same 1957-80 period. These long-term changes in water quality are statistically related to increasing population in the basin and especially to manufacturing employment. Comparisons of water-quality data for present conditions with estimated natural conditions indicate that over 50 percent of the loads of most major dissolved substances in the river at Lock 1 are the result of development impacts in the basin. Over 80 percent of the nutrients plus nitrate nitrogen, ammonia nitrogen, and total phosphorus presently in the streams originate from development. At four sampling stations on the Cape Fear River and its tributaries, recent water-quality data show that most constituents are always within North Carolina water-quality standards and Environmental Protection Agency water-quality criteria. However, iron, manganese and mercury concentrations usually exceed standards.&nbsp;</p>","largerWorkType":{"id":18,"text":"Report"},"largerWorkTitle":"Water quality of North Carolina streams","largerWorkSubtype":{"id":5,"text":"USGS Numbered Series"},"language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2185F","usgsCitation":"Crawford, J.K., 1985, Water quality of North Carolina streams – Water-quality characteristics for selected sites on the Cape Fear River, North Carolina, 1955-80 – Variability, loads, and trends of selected constituents: U.S. Geological Survey Water Supply Paper 2185, vii, 44 p., https://doi.org/10.3133/wsp2185F.","productDescription":"vii, 44 p.","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138336,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2185f/report-thumb.jpg"},{"id":30173,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2185f/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":392027,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25469.htm"}],"country":"United States","state":"North Carolina","otherGeospatial":"Cape Fear River","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -77.87109375,\n              34.243594729697406\n            ],\n            [\n              -76.8438720703125,\n              34.786739162702524\n            ],\n            [\n              -78.9532470703125,\n              36.54494944148322\n            ],\n            [\n              -80.6451416015625,\n              36.558187766360675\n            ],\n            [\n              -77.860107421875,\n              34.22088697429016\n            ],\n            [\n              -77.87109375,\n              34.243594729697406\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a07e4b07f02db5f99ab","contributors":{"authors":[{"text":"Crawford, J. Kent","contributorId":54176,"corporation":false,"usgs":true,"family":"Crawford","given":"J.","email":"","middleInitial":"Kent","affiliations":[],"preferred":false,"id":146405,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26214,"text":"wri844347 - 1985 - Low flows and flow duration of Tennessee streams through 1981","interactions":[],"lastModifiedDate":"2012-02-02T00:08:33","indexId":"wri844347","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4347","title":"Low flows and flow duration of Tennessee streams through 1981","docAbstract":"Estimates of low-flow characteristics and flow duration for the period of record at continuous-record streamflow gages are essential in hydrologic studies and water-resources management. This report provides estimates of low flow for 1, 3, 7, 14, 30, 60, and 90 consecutive days for recurrence intervals of 2, 5, 10 , and 20 years for continuous-record streamflow gages in Tennessee. These estimates were used in correlation methods to estimate low flow at partial-record streamflow sites for 1, 3, and 7 consecutive days for a recurrence interval of 10 years; and 3 consecutive days for a recurrence interval of 20 years. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri844347","usgsCitation":"Bingham, R., 1985, Low flows and flow duration of Tennessee streams through 1981: U.S. Geological Survey Water-Resources Investigations Report 84-4347, iii, 325 p. :ill., map ;28 cm., https://doi.org/10.3133/wri844347.","productDescription":"iii, 325 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":2104,"rank":100,"type":{"id":15,"text":"Index Page"},"url":"https://pubs.water.usgs.gov/wri844347","linkFileType":{"id":5,"text":"html"}},{"id":119111,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/wri_84_4347.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a74e4b07f02db64491c","contributors":{"authors":[{"text":"Bingham, R.H.","contributorId":37301,"corporation":false,"usgs":true,"family":"Bingham","given":"R.H.","email":"","affiliations":[],"preferred":false,"id":195997,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":61207,"text":"mf1383K - 1985 - Maps showing abundance and distribution of mercury in rock samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","interactions":[],"lastModifiedDate":"2016-08-23T10:20:08","indexId":"mf1383K","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1383","chapter":"K","title":"Maps showing abundance and distribution of mercury in rock samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","docAbstract":"<p>This map presents data on the abundance and distribution of mercury in 3,146 rock samples from the Medford quadrangle. Most of the rock samples were collected incidental to geologic, geochemical, and mineral resources studies in the period from 1974 to 1980, but about 6 percent date from earlier investigations (Wells, 1940; 1956; Wells and others 1949).&nbsp;</p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1383K","usgsCitation":"Whittington, C.L., Grimes, D.J., and Leinz, R.W., 1985, Maps showing abundance and distribution of mercury in rock samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California: U.S. Geological Survey Miscellaneous Field Studies Map 1383, 43.33 x 26.78 inches, https://doi.org/10.3133/mf1383K.","productDescription":"43.33 x 26.78 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179843,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1383K.PNG"},{"id":327576,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1383-K/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,42 ], [ -124,43 ], [ -122,43 ], [ -122,42 ], [ -124,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ee4b07f02db5fe096","contributors":{"authors":[{"text":"Whittington, Charles L.","contributorId":52642,"corporation":false,"usgs":true,"family":"Whittington","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265190,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265191,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265192,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":61203,"text":"mf1383J - 1985 - Map showing abundance and distribution of arsenic in oxide residues of stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","interactions":[],"lastModifiedDate":"2016-08-23T10:15:45","indexId":"mf1383J","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"1383","chapter":"J","title":"Map showing abundance and distribution of arsenic in oxide residues of stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California","docAbstract":"<p><span>Stream-sediment sampling in the&nbsp;</span><span>Medford 1<sup><span>o</span></sup><span class=\"apple-converted-space\">&nbsp;</span>x 2<sup><span>o</span></sup><span class=\"apple-converted-space\">&nbsp;</span>quadrangle was undertaken to provide to aid in assessment of the mineral resource potential of the quadrangle. This map presents data on the abundance and distribution of copper in the oxide residues (oxalic-acid leachates) of stream sediments and in the minus-0.18-mm sieve fraction of selected stream sediments collected in the quadrangle.&nbsp;</span></p>","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Reston, VA","doi":"10.3133/mf1383J","usgsCitation":"Whittington, C.L., Leinz, R.W., and Grimes, D.J., 1985, Map showing abundance and distribution of arsenic in oxide residues of stream-sediment samples, Medford 1 degree by 2 degrees Quadrangle, Oregon-California: U.S. Geological Survey Miscellaneous Field Studies Map 1383, 49.67 x 24.19 inches, https://doi.org/10.3133/mf1383J.","productDescription":"49.67 x 24.19 inches","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[],"links":[{"id":179846,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/mf1383J.PNG"},{"id":327568,"rank":1,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/mf/1383-J/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"250000","country":"United States","state":"Oregon","geographicExtents":"{ \"type\": \"FeatureCollection\", \"features\": [ { \"type\": \"Feature\", \"properties\": {}, \"geometry\": { \"type\": \"Polygon\", \"coordinates\": [ [ [ -124,42 ], [ -124,43 ], [ -122,43 ], [ -122,42 ], [ -124,42 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a94e4b07f02db658bac","contributors":{"authors":[{"text":"Whittington, Charles L.","contributorId":52642,"corporation":false,"usgs":true,"family":"Whittington","given":"Charles","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":265178,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Leinz, Reinhard W.","contributorId":60628,"corporation":false,"usgs":true,"family":"Leinz","given":"Reinhard","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265180,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Grimes, David J.","contributorId":36925,"corporation":false,"usgs":true,"family":"Grimes","given":"David","email":"","middleInitial":"J.","affiliations":[],"preferred":false,"id":265179,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":26157,"text":"wri854217 - 1985 - Analyses of flood-flow frequency for selected gaging stations in South Dakota","interactions":[],"lastModifiedDate":"2012-02-02T00:08:34","indexId":"wri854217","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"85-4217","title":"Analyses of flood-flow frequency for selected gaging stations in South Dakota","docAbstract":"Analyses of flood flow frequency were made for 111 continuous-record gaging stations in South Dakota with 10 or more years of record. The analyses were developed using the log-Pearson Type III procedure recommended by the U.S. Water Resources Council. The procedure characterizes flood occurrence at a single site as a sequence of annual peak flows. The magnitudes of the annual peak flows are assumed to be independent random variables following a log-Pearson Type III probability distribution, which defines the probability that any single annual peak flow will exceed a specified discharge. By considering only annual peak flows, the flood-frequency analysis becomes the estimation of the log-Pearson annual-probability curve using the record of annual peak flows at the site. The recorded data are divided into two classes: systematic and historic. The systematic record includes all annual peak flows determined in the process of conducting a systematic gaging program at a site. In this program, the annual peak flow is determined for each and every year of the program. The systematic record is intended to constitute an unbiased and representative sample of the population of all possible annual peak flows at the site. In contrast to the systematic record, the historic record consists of annual peak flows that would not have been determined except for evidence indicating their unusual magnitude. Flood information acquired from historical sources almost invariably refers to floods of noteworthy, and hence extraordinary, size. Although historic records form a biased and unrepresentative sample, they can be used to supplement the systematic record. (Author 's abstract)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/wri854217","usgsCitation":"Benson, R., Hoffman, E., and Wipf, V., 1985, Analyses of flood-flow frequency for selected gaging stations in South Dakota: U.S. Geological Survey Water-Resources Investigations Report 85-4217, vii, 202 p. :map ;28 cm., https://doi.org/10.3133/wri854217.","productDescription":"vii, 202 p. :map ;28 cm.","costCenters":[],"links":[{"id":119101,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1985/4217/report-thumb.jpg"},{"id":54951,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1985/4217/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db680da8","contributors":{"authors":[{"text":"Benson, R.D.","contributorId":23955,"corporation":false,"usgs":true,"family":"Benson","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":195915,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Hoffman, E.B.","contributorId":47379,"corporation":false,"usgs":true,"family":"Hoffman","given":"E.B.","email":"","affiliations":[],"preferred":false,"id":195917,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Wipf, V.J.","contributorId":26725,"corporation":false,"usgs":true,"family":"Wipf","given":"V.J.","email":"","affiliations":[],"preferred":false,"id":195916,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":1970,"text":"wsp2264 - 1985 - Simulating unsteady transport of nitrogen, biochemical oxygen demand, and dissolved oxygen in the Chattahoochee River downstream from Atlanta, Georgia","interactions":[],"lastModifiedDate":"2019-12-30T10:24:57","indexId":"wsp2264","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":341,"text":"Water Supply Paper","code":"WSP","active":false,"publicationSubtype":{"id":5}},"seriesNumber":"2264","title":"Simulating unsteady transport of nitrogen, biochemical oxygen demand, and dissolved oxygen in the Chattahoochee River downstream from Atlanta, Georgia","docAbstract":"As part of an intensive water-quality assessment of the Chattahoochee River, repetitive water-quality measurements were made at 12 sites along a 69-kilometer reach of the river downstream of Atlanta, Georgia. Concentrations of seven constituents (temperature, dissolved oxygen, ultimate carbonaceous biochemical oxygen demand (BOD), organic nitrogen, ammonia, nitrite, and nitrate) were obtained during two periods of 36 hours, one starting on August 30, 1976, and the other starting on May 31, 1977. The study reach contains one large and several small sewage outfalls and receives the cooling water from two large powerplants. \r\n\r\nAn unsteady water-quality model of the Lagrangian type was calibrated using the 1977 data and verified using the 1976 data. The model provided a good means of interpreting these data even though both the flow and the pollution loading rates were highly unsteady. A kinetic model of the cascade type accurately described the physical and biochemical processes occurring in the river. All rate coefficients, except reaeration coefficients and those describing the resuspension of BOD, were fitted to the 1977 data and verified using the 1976 data. \r\n\r\nThe study showed that, at steady low flow, about 38 percent of the BOD settled without exerting an oxygen demand. At high flow, this settled BOD was resuspended and exerted an immediate oxygen demand. About 70 percent of the ammonia extracted from the water column was converted to nitrite, but the fate of the remaining 30 percent is unknown. Photosynthetic production was not an important factor in the oxygen balance during either run.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2264","usgsCitation":"Jobson, H.E., 1985, Simulating unsteady transport of nitrogen, biochemical oxygen demand, and dissolved oxygen in the Chattahoochee River downstream from Atlanta, Georgia: U.S. Geological Survey Water Supply Paper 2264, v, 36 p. , https://doi.org/10.3133/wsp2264.","productDescription":"v, 36 p. ","costCenters":[{"id":13634,"text":"South Atlantic Water Science Center","active":true,"usgs":true}],"links":[{"id":138296,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2264/report-thumb.jpg"},{"id":27346,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2264/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Georgia","city":"Atlanta","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -84.9462890625,\n              33.284619968887675\n            ],\n            [\n              -83.91357421875,\n              33.284619968887675\n            ],\n            [\n              -83.91357421875,\n              34.14363482031264\n            ],\n            [\n              -84.9462890625,\n              34.14363482031264\n            ],\n            [\n              -84.9462890625,\n              33.284619968887675\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a80e4b07f02db649345","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144454,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":16599,"text":"ofr85518 - 1985 - Static and cyclic strength properties of Mount St. Helens debris avalanche and ash cloud materials","interactions":[],"lastModifiedDate":"2012-02-02T00:07:17","indexId":"ofr85518","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-518","title":"Static and cyclic strength properties of Mount St. Helens debris avalanche and ash cloud materials","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85518","usgsCitation":"Winters, W., and Kayen, R.E., 1985, Static and cyclic strength properties of Mount St. Helens debris avalanche and ash cloud materials: U.S. Geological Survey Open-File Report 85-518, ii, 182 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr85518.","productDescription":"ii, 182 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":150326,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0518/report-thumb.jpg"},{"id":45603,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0518/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49e0e4b07f02db5e3eaf","contributors":{"authors":[{"text":"Winters, W.J.","contributorId":49796,"corporation":false,"usgs":true,"family":"Winters","given":"W.J.","email":"","affiliations":[],"preferred":false,"id":173137,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Kayen, R. E.","contributorId":14424,"corporation":false,"usgs":true,"family":"Kayen","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":173136,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14089,"text":"ofr8521 - 1985 - Porosity, grain-density, and inferred aragonite-content data from the Miami Limestone, Miami area and lower Florida Keys","interactions":[],"lastModifiedDate":"2012-02-02T00:06:53","indexId":"ofr8521","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-21","title":"Porosity, grain-density, and inferred aragonite-content data from the Miami Limestone, Miami area and lower Florida Keys","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr8521","usgsCitation":"Hester, T., and Schmoker, J., 1985, Porosity, grain-density, and inferred aragonite-content data from the Miami Limestone, Miami area and lower Florida Keys: U.S. Geological Survey Open-File Report 85-21, i, 29 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr8521.","productDescription":"i, 29 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":147138,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0021/report-thumb.jpg"},{"id":42733,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0021/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad6e4b07f02db683cd1","contributors":{"authors":[{"text":"Hester, T.C.","contributorId":93054,"corporation":false,"usgs":true,"family":"Hester","given":"T.C.","email":"","affiliations":[],"preferred":false,"id":168909,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Schmoker, J. W.","contributorId":69964,"corporation":false,"usgs":true,"family":"Schmoker","given":"J. W.","affiliations":[],"preferred":false,"id":168908,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":14413,"text":"ofr85623 - 1985 - Annotated bibliography of selected references on the geology of the Baird Mountains Quadrangle, northwestern Alaska","interactions":[],"lastModifiedDate":"2018-06-20T20:02:14","indexId":"ofr85623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":5,"text":"USGS Numbered Series"},"seriesTitle":{"id":330,"text":"Open-File Report","code":"OFR","onlineIssn":"2331-1258","printIssn":"0196-1497","active":true,"publicationSubtype":{"id":5}},"seriesNumber":"85-623","title":"Annotated bibliography of selected references on the geology of the Baird Mountains Quadrangle, northwestern Alaska","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr85623","usgsCitation":"Karl, S.M., Thompson, W., and Schmidt, J., 1985, Annotated bibliography of selected references on the geology of the Baird Mountains Quadrangle, northwestern Alaska: U.S. Geological Survey Open-File Report 85-623, 48 p. :map ;28 cm., https://doi.org/10.3133/ofr85623.","productDescription":"48 p. :map ;28 cm.","costCenters":[],"links":[{"id":43093,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1985/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":147683,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1985/0623/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac8e4b07f02db67bf75","contributors":{"authors":[{"text":"Karl, Susan M. 0000-0003-1559-7826 skarl@usgs.gov","orcid":"https://orcid.org/0000-0003-1559-7826","contributorId":502,"corporation":false,"usgs":true,"family":"Karl","given":"Susan","email":"skarl@usgs.gov","middleInitial":"M.","affiliations":[{"id":119,"text":"Alaska Science Center Geology Minerals","active":true,"usgs":true}],"preferred":true,"id":169415,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Thompson, W.R.","contributorId":16170,"corporation":false,"usgs":true,"family":"Thompson","given":"W.R.","email":"","affiliations":[],"preferred":false,"id":169414,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Schmidt, J.M.","contributorId":97916,"corporation":false,"usgs":true,"family":"Schmidt","given":"J.M.","email":"","affiliations":[],"preferred":false,"id":169416,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}}
,{"id":40109,"text":"ofr8038 - 1985 - Federal coal resource occurrence and coal development potential maps of the Casamero Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico","interactions":[],"lastModifiedDate":"2012-02-02T00:10:17","indexId":"ofr8038","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"80-38","title":"Federal coal resource occurrence and coal development potential maps of the Casamero Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico","language":"ENGLISH","doi":"10.3133/ofr8038","usgsCitation":"Berge Exploration Inc., 1985, Federal coal resource occurrence and coal development potential maps of the Casamero Lake 7 1/2-minute Quadrangle, McKinley County, New Mexico: U.S. Geological Survey Open-File Report 80-38, 4 maps, 2 data sheets :photocopy ;58 x 48 cm. +1 pamphlet (i, 15 leaves : map ; 28 cm.), https://doi.org/10.3133/ofr8038.","productDescription":"4 maps, 2 data sheets :photocopy ;58 x 48 cm. +1 pamphlet (i, 15 leaves : map ; 28 cm.)","costCenters":[],"links":[{"id":170556,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1980/0038/report-thumb.jpg"},{"id":69229,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69230,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69231,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69232,"rank":403,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-4.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69233,"rank":404,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-5.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69234,"rank":405,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1980/0038/plate-6.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":69235,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1980/0038/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fee4b07f02db5f6cc0","contributors":{"authors":[{"text":"Berge Exploration Inc.","contributorId":128031,"corporation":true,"usgs":false,"organization":"Berge Exploration Inc.","id":529988,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}}
,{"id":26454,"text":"wri834209 - 1985 - Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 2: Development and application of southwest Suffolk County model","interactions":[],"lastModifiedDate":"2022-01-04T21:27:58.632054","indexId":"wri834209","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"83-4209","title":"Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 2: Development and application of southwest Suffolk County model","docAbstract":"By 1990, sanitary sewers in Nassau County Sewage Disposal Districts 2 and 3 and Suffolk County Southwest Sewer District will discharge to the ocean 140 cu ft of water/sec that would otherwise be returned to the groundwater system through septic tanks and similar systems. To evaluate the effects of this loss on groundwater levels and streamflow, the U.S. Geological Survey developed a groundwater flow model that couples a fine-scale subregional model to a regional model of larger scale. The regional model generates flux boundary conditions for the subregional model, and the subregional model provides detail in the area of concern. Results indicate that the water table will decline by as much as 8 ft along the Suffolk-Nassau county line, with effects decreasing eastward. Base flow is predicted to decrease by as much as 73% in a stream along the county line, but this effect will decrease to zero just east of the sewered area. This report is one of a series describing the predicted hydrologic effects of sewers in southern Nassau and southwest Suffolk Counties. (USGS)","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834209","usgsCitation":"Buxton, H., and Reilly, T.E., 1985, Effects of sanitary sewers on ground-water levels and streams in Nassau and Suffolk Counties, New York; part 2: Development and application of southwest Suffolk County model: U.S. Geological Survey Water-Resources Investigations Report 83-4209, vi, 39 p., https://doi.org/10.3133/wri834209.","productDescription":"vi, 39 p.","costCenters":[],"links":[{"id":393884,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35852.htm"},{"id":55275,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4209/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118719,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4209/report-thumb.jpg"}],"country":"United States","state":"New York","county":"Nassau County, Suffolk County","geographicExtents":"{\n  \"type\": \"FeatureCollection\",\n  \"features\": [\n    {\n      \"type\": \"Feature\",\n      \"properties\": {},\n      \"geometry\": {\n        \"type\": \"Polygon\",\n        \"coordinates\": [\n          [\n            [\n              -73.43742370605467,\n              40.69001034095325\n            ],\n            [\n              -73.06388854980469,\n              40.69001034095325\n            ],\n            [\n              -73.06388854980469,\n              40.84030757074791\n            ],\n            [\n              -73.43742370605467,\n              40.84030757074791\n            ],\n            [\n              -73.43742370605467,\n              40.69001034095325\n            ]\n          ]\n        ]\n      }\n    }\n  ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a29e4b07f02db611ad7","contributors":{"authors":[{"text":"Buxton, H. T.","contributorId":67873,"corporation":false,"usgs":true,"family":"Buxton","given":"H. T.","affiliations":[],"preferred":false,"id":196420,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Reilly, T. E.","contributorId":79460,"corporation":false,"usgs":true,"family":"Reilly","given":"T.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":196421,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}}
,{"id":29303,"text":"wri844223 - 1985 - Trap efficiency of a sediment-control pond below a block-cut coal mine in Fayette County, Pennsylvania","interactions":[],"lastModifiedDate":"2017-06-20T08:17:43","indexId":"wri844223","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1985","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":"84-4223","title":"Trap efficiency of a sediment-control pond below a block-cut coal mine in Fayette County, Pennsylvania","docAbstract":"The U. S. Geological Survey determined the efficiency of a pond constructed to control sediment from a surface coal mine site by measuring runoff and sediment loads at the inlet to and discharge from the pond during storms. The pond is below a 17.9-acre block-cut coal mine in Fayette County, Pennsylvania and has a permanent pool capacity of 60,000 cu ft. The capacity at the principal spillway and the emergency spillway are 128,900 and 175,500 cu ft, respectively. The pond is equipped with a 3-inch flow control valve, used by the mine operator to regulate the pond stage between the permanent pool and the principal spillway. Data were collected during five moderate storms when the 3-inch control valve was intentionally opened. The ration between the quantity of water in the pond at the start of the storm and the quantity to runoff to the pond was calculated for each storm. The ratios were 3.6, 2.5, 8.6, 2.9, and 1.5 for the five storms. The measured trap efficiencies were 98.1, 92.8, 99.6, 99.1, and 98.2%, for the five storms. 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