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Colorado River Basin Above Dolores River: U.S. Geological Survey Water Data Report CO-83-2, 287 p., 6 fig., 6 tab., https://doi.org/10.3133/wdrCO832.","productDescription":"287 p., 6 fig., 6 tab.","costCenters":[],"links":[{"id":258747,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wdr/1983/co-83-2/report.pdf","size":"21319","linkFileType":{"id":1,"text":"pdf"}},{"id":258748,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wdr/1983/co-83-2/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0be4b07f02db5fc072","contributors":{"authors":[{"text":"Ugland, R.C.","contributorId":14044,"corporation":false,"usgs":true,"family":"Ugland","given":"R.C.","email":"","affiliations":[],"preferred":false,"id":256659,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Steinheimer, J.T.","contributorId":81121,"corporation":false,"usgs":true,"family":"Steinheimer","given":"J.T.","email":"","affiliations":[],"preferred":false,"id":256662,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Blattner, J.L.","contributorId":44541,"corporation":false,"usgs":true,"family":"Blattner","given":"J.L.","affiliations":[],"preferred":false,"id":256660,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Kretschman, R.G.","contributorId":75623,"corporation":false,"usgs":true,"family":"Kretschman","given":"R.G.","email":"","affiliations":[],"preferred":false,"id":256661,"contributorType":{"id":1,"text":"Authors"},"rank":4}]}} ,{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","interactions":[{"subject":{"id":9672,"text":"ofr84612 - 1984 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"ofr84612","publicationYear":"1984","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"id":1}],"supersededBy":{"id":57994,"text":"pp1369 - 1986 - Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","indexId":"pp1369","publicationYear":"1986","noYear":false,"title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado"},"lastModifiedDate":"2020-06-12T20:58:33.037696","indexId":"ofr84612","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-612","title":"Hydrology, geomorphology, and dam-break modeling of the July 15, 1982, Lawn Lake Dam and Cascade Lake Dam failures, Larimer County, Colorado","docAbstract":"On July 15, 1982, Lawn Lake Dam, a 26-foot-high earthfill irrigation dam built in 1903 in Rocky Mountain National Park, Colorado, failed, due to piping, releasing 674 acre-feet of water with a peak discharge of 18,000 cubic feet per second down the Roaring River. Three people were killed, and damages were estimated at $31 million. Cascade Lake Dam, downstream from Lawn Lake Dam, subsequently failed as a result of the flood, increasing the peak flow at this point from 7,210 cubic feet per second to 16,000 cubic feet per second. The flood wave took 3.28 hours to travel 12.5 miles to Lake Estes, where all the floodwater was stored. The channel of the Roaring River was scoured as much as 50 feet and widened 300 feet. An alluvial fan of 42.3 acres, containing 10 million cubic feet of material, was deposited at the mouth of the Roaring River, damming the Fall River and forming a 17-acre lake. Various methods were used to indirectly compute peak discharge, attenuation of flow, and flood traveltime. A version of the National Weather Service dam-break flood model was used to evaluate its performance on high-gradient streams, to provide supplemental hydrologic information, and to evaluate various scenarios of dam-break development. 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R.D.","contributorId":36551,"corporation":false,"usgs":true,"family":"Jarrett","given":"R.D.","email":"","affiliations":[],"preferred":false,"id":160099,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Costa, J. E.","contributorId":28977,"corporation":false,"usgs":true,"family":"Costa","given":"J.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":160098,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":9751,"text":"ofr84645 - 1984 - Estimation of the sensitivity of CSEM coupling to coil movement and resistivity changes of simple models","interactions":[],"lastModifiedDate":"2012-02-02T00:06:06","indexId":"ofr84645","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-645","title":"Estimation of the sensitivity of CSEM coupling to coil movement and resistivity changes of simple models","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84645","usgsCitation":"Kauahikaua, J., 1984, Estimation of the sensitivity of CSEM coupling to coil movement and resistivity changes of simple models: U.S. Geological Survey Open-File Report 84-645, 18 p. :ill. ;28 cm., https://doi.org/10.3133/ofr84645.","productDescription":"18 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":141245,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0645/report-thumb.jpg"},{"id":37500,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0645/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb205","contributors":{"authors":[{"text":"Kauahikaua, Jim","contributorId":47366,"corporation":false,"usgs":true,"family":"Kauahikaua","given":"Jim","email":"","affiliations":[],"preferred":false,"id":160234,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9610,"text":"ofr84623 - 1984 - Ground-water data for Michigan 1983","interactions":[],"lastModifiedDate":"2016-12-29T10:55:50","indexId":"ofr84623","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-623","title":"Ground-water data for Michigan 1983","docAbstract":"

Water levels, locations, depths, and aquifers tapped are given for 115 observation wells. Tabulated data include extremes of water levels for 1983 and for the period of record, pumpage of most major ground-water users in the State, and quality data on selected wells. The largest reported user of ground-water, the city of Lansing, pumped 8.1 billion gallons from the Saginaw Formation and glacial deposits.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"Lansing, MI","doi":"10.3133/ofr84623","collaboration":"Prepared in cooperation with the Michigan Department of Natural Resources","usgsCitation":"Huffman, G., 1984, Ground-water data for Michigan 1983: U.S. Geological Survey Open-File Report 84-623, iv, 47 p., https://doi.org/10.3133/ofr84623.","productDescription":"iv, 47 p.","costCenters":[{"id":382,"text":"Michigan Water Science Center","active":true,"usgs":true}],"links":[{"id":141717,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0623/report-thumb.jpg"},{"id":37340,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0623/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United 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Mahd adh Dhahab is a late Precambrian epithermal gold-silver-base metal deposit located in the west-central part of the Arabian Shield. North-trending quartz veins containing base and precious metals cut an east-striking, north-dipping homoclinal sequence of volcanic, volcaniclastic, and epiclastic rocks of intermediate to felsic composition. Ore was localized where the veins cut competent, coarse-grained, fragmental units directly below incompetent and impermeable tuff units. The proximity of an epizonal rhyolite porphyry stock to these contacts also was important in localizing ore. Ore minerals include native gold and silver, gold-silver tellurides, chalcopyrite, sphalerite, and minor galena, and five stages of mineralization have been identified.

\n

Vein-related alteration consisting of quartz-sericite-pyrite, chloritic, argillic, and silicic halos was superimposed on broad zones of pervasive silicic, potassic, and argillic alteration that surrounds the rhyolite intrusive body. Quartz-sericite-pyrite alteration associated with the earliest stage of mineralization was followed by broad, pervasive, stratigraphically controlled potassic alteration. Subsequent mineralization was accompanied by quartz-sericitepyrite alteration and was followed by the main stage of mineralization that formed strong chloritic alteration halos. Development of broad zones and halos of argillic alteration also may have been related to the main stage of mineralization. Development of silicic halos was characteristic of the late stages of mineralization. Broad, pervasive propylitic alteration was then superimposed on all alteration types and represents cooling and inward encroachment of the hydrothermal system. All alteration, except the early silicic alteration is interpreted to have been related to circulating meteoric fluids heated by the rhyolite.

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1984 - The base of the Upper Jurassic Morrison Formation in east-central Utah","interactions":[],"lastModifiedDate":"2012-02-02T00:09:50","indexId":"b1561","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1561","title":"The base of the Upper Jurassic Morrison Formation in east-central Utah","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1561","usgsCitation":"O'Sullivan, R., 1984, The base of the Upper Jurassic Morrison Formation in east-central Utah: U.S. Geological Survey Bulletin 1561, iii, 17 p. ill., map ;23 cm., https://doi.org/10.3133/b1561.","productDescription":"iii, 17 p. ill., map ;23 cm.","costCenters":[],"links":[{"id":165829,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1561/report-thumb.jpg"},{"id":63314,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1561/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aaae4b07f02db669753","contributors":{"authors":[{"text":"O'Sullivan, Robert Brett","contributorId":26695,"corporation":false,"usgs":true,"family":"O'Sullivan","given":"Robert Brett","affiliations":[],"preferred":false,"id":214621,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":35806,"text":"b1550 - 1984 - Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado","interactions":[{"subject":{"id":11127,"text":"ofr77607 - 1977 - Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado","indexId":"ofr77607","publicationYear":"1977","noYear":false,"title":"Preliminary data on some Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (granite) in Colorado"},"predicate":"SUPERSEDED_BY","object":{"id":35806,"text":"b1550 - 1984 - Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado","indexId":"b1550","publicationYear":"1984","noYear":false,"title":"Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado"},"id":1}],"lastModifiedDate":"2012-02-02T00:09:40","indexId":"b1550","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1550","title":"Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/b1550","usgsCitation":"Sheridan, D.M., and Raymond, W.H., 1984, Precambrian deposits of zinc-copper-lead sulfides and zinc spinel (gahnite) in Colorado: U.S. Geological Survey Bulletin 1550, iv, 31 p. ill., maps ;23 cm., https://doi.org/10.3133/b1550.","productDescription":"iv, 31 p. ill., maps ;23 cm.","costCenters":[],"links":[{"id":167708,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/bul/1550/report-thumb.jpg"},{"id":63727,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/bul/1550/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ad1e4b07f02db6810a5","contributors":{"authors":[{"text":"Sheridan, Douglas M.","contributorId":13966,"corporation":false,"usgs":true,"family":"Sheridan","given":"Douglas","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":215257,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Raymond, William H.","contributorId":48555,"corporation":false,"usgs":true,"family":"Raymond","given":"William","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":215258,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":30188,"text":"wri844188 - 1984 - Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","interactions":[{"subject":{"id":70175961,"text":"wri844188A - 1984 - Ground-water contamination by crude oil at the Bemidji, Minnesota, research site- An introduction: Chapter A in Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","indexId":"wri844188A","publicationYear":"1984","noYear":false,"chapter":"A","title":"Ground-water contamination by crude oil at the Bemidji, Minnesota, research site- An introduction: Chapter A in Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study"},"predicate":"IS_PART_OF","object":{"id":30188,"text":"wri844188 - 1984 - Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","indexId":"wri844188","publicationYear":"1984","noYear":false,"title":"Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study"},"id":1},{"subject":{"id":70175964,"text":"wri844188D - 1984 - Determination of hydraulic conductivity in three dimensions and its relation to dispersivity: Chapter D in Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","indexId":"wri844188D","publicationYear":"1984","noYear":false,"chapter":"D","title":"Determination of hydraulic conductivity in three dimensions and its relation to dispersivity: Chapter D in Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study"},"predicate":"IS_PART_OF","object":{"id":30188,"text":"wri844188 - 1984 - Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","indexId":"wri844188","publicationYear":"1984","noYear":false,"title":"Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study"},"id":2}],"lastModifiedDate":"2016-05-13T10:10:31","indexId":"wri844188","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-4188","title":"Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study","docAbstract":"

The U.S. Geological Survey has begun a research project to improve understanding of the mobilization, transport, and fate of petroleum contaminants in the shallow subsurface and to use this understanding to develop predictive models of contaminant behavior.

\n

The project site is near Bemidji in northern Minnesota where an accidental spill of 10,500 barrels of crude oil occurred when a pipeline broke on August 20, 1979. Regulatory and remedial actions have been completed. The site is in a remote area with neither man-made hydraulic stresses nor other anthropogenic sources of the compounds of interest. The spill is in the recharge area of a local flow system that discharges to a small closed lake approximately 1,000 feet down the hydraulic gradient. The aquifer is pitted outwash dissected by younger glacial channels and is underlain by poorly permeable till at a depth of about 80 feet. Ground water dissolves oil floating on the water table under the spill site and moves toward the lake. At the water table, ground water enters the lake through lacustrine sediments; at depth, flow may be underneath the lake through the outwash. Contaminant transport has been as rapid as 4 feet per day based on the rate of movement of contaminants monitored through wells installed within a few days of the spill, but average rates are undoubtedly much less.

","language":"English","publisher":"U.S. Geological Survey","publisherLocation":"St. Paul, MN","doi":"10.3133/wri844188","usgsCitation":"1984, Ground-water contamination by crude oil at the Bemidji, Minnesota, research site; US Geological Survey Toxic Waste--ground-water contamination study: U.S. Geological Survey Water-Resources Investigations Report 84-4188, x, 107 p., https://doi.org/10.3133/wri844188.","productDescription":"x, 107 p.","onlineOnly":"N","additionalOnlineFiles":"N","costCenters":[{"id":392,"text":"Minnesota Water Science Center","active":true,"usgs":true}],"links":[{"id":58984,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1984/4188/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":119476,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1984/4188/report-thumb.jpg"}],"country":"United States","state":"Minnesota","city":"Bemidji","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -95.09074687957764,\n 47.57481758275047\n ],\n [\n -95.08894443511963,\n 47.57376082974435\n ],\n [\n -95.0900387763977,\n 47.57295015544948\n ],\n [\n -95.09201288223267,\n 47.57392006786331\n ],\n [\n -95.09074687957764,\n 47.57481758275047\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66d04b","contributors":{"editors":[{"text":"Hult, M. F.","contributorId":29817,"corporation":false,"usgs":true,"family":"Hult","given":"M.","email":"","middleInitial":"F.","affiliations":[],"preferred":false,"id":629067,"contributorType":{"id":2,"text":"Editors"},"rank":1}]}} ,{"id":36445,"text":"fwsobs84_17 - 1984 - Map projections for use with the Geographic Information System","interactions":[],"lastModifiedDate":"2012-02-02T00:09:38","indexId":"fwsobs84_17","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","noYear":false,"publicationType":{"id":18,"text":"Report"},"publicationSubtype":{"id":1,"text":"Federal Government Series"},"seriesTitle":{"id":20,"text":"FWS/OBS","active":false,"publicationSubtype":{"id":1}},"seriesNumber":"84/17","title":"Map projections for use with the Geographic Information System","language":"ENGLISH","publisher":"U.S. Fish and Wildlife Service","usgsCitation":"Lee, J.E., and Walsh, J.M., 1984, Map projections for use with the Geographic Information System: FWS/OBS 84/17, viii, 60 p. : ill.; 28 cm.","productDescription":"viii, 60 p. : ill.; 28 cm.","costCenters":[],"links":[{"id":166570,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/outside_thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a93e4b07f02db65873c","contributors":{"authors":[{"text":"Lee, John E.","contributorId":22829,"corporation":false,"usgs":true,"family":"Lee","given":"John","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":216338,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Walsh, J. Michael","contributorId":72045,"corporation":false,"usgs":true,"family":"Walsh","given":"J.","email":"","middleInitial":"Michael","affiliations":[],"preferred":false,"id":216339,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":1971,"text":"wsp2252 - 1984 - Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas","interactions":[],"lastModifiedDate":"2012-02-02T00:05:24","indexId":"wsp2252","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2252","title":"Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas","docAbstract":"Rhodamine-WT dye, ethylene, and propane were injected at three sites along a 21.6-kilometer reach of the West Fork Trinity River below Fort Worth, Texas. Complete dye concentration versus time curves and peak gas concentrations were measured at three cross sections below each injection. The peak dye concentrations were located and samples were collected at about three-hour intervals for as many as six additional cross sections. These data were analyzed to determine the longitudinal dispersion coefficients as well as the gas desorption coefficients using both standard techniques and a numerical routing procedure. \r\n\r\nThe routing procedure, using a Lagrangian transport model to minimize numerical dispersion, provided better estimates of the dispersion coefficient than did the method of moments. At a steady flow of about 0.76 m2/s, the dispersion coefficient varied from about 0.7 m2/s in a reach contained within a single deep pool to about 2.0 m2/s in a reach containing riffles and small pools. \r\n\r\nThe bulk desorption coefficients computed using the routing procedure and the standard peak method were essentially the same. The liquid film coefficient could also be obtained using the routing procedure. Both the bulk desorption coefficient and the liquid film coefficient were much smaller in the pooled reach than in the reaches containing riffles.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2252","usgsCitation":"Jobson, H.E., and Rathbun, R.E., 1984, Use of the routing procedure to study dye and gas transport in the West Fork Trinity River, Texas: U.S. Geological Survey Water Supply Paper 2252, iv, 21 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2252.","productDescription":"iv, 21 p. :ill. ;28 cm.","costCenters":[],"links":[{"id":138297,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2252/report-thumb.jpg"},{"id":27347,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2252/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a08e4b07f02db5fa28e","contributors":{"authors":[{"text":"Jobson, Harvey E.","contributorId":27032,"corporation":false,"usgs":true,"family":"Jobson","given":"Harvey","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144455,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Rathbun, R. E.","contributorId":61796,"corporation":false,"usgs":true,"family":"Rathbun","given":"R.","email":"","middleInitial":"E.","affiliations":[],"preferred":false,"id":144456,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":46436,"text":"ofr84799 - 1984 - Map showing aeromagnetic data over the Stillwater Complex and vicinity, Montana","interactions":[],"lastModifiedDate":"2012-02-02T00:04:55","indexId":"ofr84799","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"84-799","title":"Map showing aeromagnetic data over the Stillwater Complex and vicinity, Montana","language":"ENGLISH","doi":"10.3133/ofr84799","usgsCitation":"Blakely, R.J., 1984, Map showing aeromagnetic data over the Stillwater Complex and vicinity, Montana: U.S. Geological Survey Open-File Report 84-799, 3 maps :photocopy ;78 x 67 cm., on sheets 106 x 92 cm., https://doi.org/10.3133/ofr84799.","productDescription":"3 maps :photocopy ;78 x 67 cm., on sheets 106 x 92 cm.","costCenters":[],"links":[{"id":134781,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/thumbnails/usgs_thumb.jpg"},{"id":83377,"rank":400,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0799/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83378,"rank":401,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0799/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":83379,"rank":402,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/of/1984/0799/plate-3.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a8fe4b07f02db6554cd","contributors":{"authors":[{"text":"Blakely, Richard J. 0000-0003-1701-5236 blakely@usgs.gov","orcid":"https://orcid.org/0000-0003-1701-5236","contributorId":1540,"corporation":false,"usgs":true,"family":"Blakely","given":"Richard","email":"blakely@usgs.gov","middleInitial":"J.","affiliations":[{"id":662,"text":"Western Mineral and Environmental Resources Science Center","active":true,"usgs":true},{"id":312,"text":"Geology, Minerals, Energy, and Geophysics Science Center","active":true,"usgs":true}],"preferred":true,"id":233312,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":1696,"text":"wsp2192 - 1984 - Appearance and water quality of turbidity plumes produced by dredging in Tampa Bay, Florida","interactions":[{"subject":{"id":9187,"text":"ofr81541 - 1981 - Appearance and water quality of turbidity plumes created by dredging in Tampa Bay, Florida","indexId":"ofr81541","publicationYear":"1981","noYear":false,"title":"Appearance and water quality of turbidity plumes created by dredging in Tampa Bay, Florida"},"predicate":"SUPERSEDED_BY","object":{"id":1696,"text":"wsp2192 - 1984 - Appearance and water quality of turbidity plumes produced by dredging in Tampa Bay, Florida","indexId":"wsp2192","publicationYear":"1984","noYear":false,"title":"Appearance and water quality of turbidity plumes produced by dredging in Tampa Bay, Florida"},"id":1}],"lastModifiedDate":"2012-02-02T00:05:15","indexId":"wsp2192","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2192","title":"Appearance and water quality of turbidity plumes produced by dredging in Tampa Bay, Florida","docAbstract":"Turbidity plumes in Tampa Bay, Florida, produced during ship-channel dredging operations from February 1977 to August 1978, were monitored in order to document plume appearance and water quality, evaluate plume influence on the characteristics of Tampa Bay water, and provide a data base for comparison with other areas that have similar sediment, dredge, placement, containment, and tide conditions. The plumes investigated originated from the operation of one hopper dredge and three cutterhead-pipeline dredges. \r\n\r\nComposition of bottom sediment was found to vary from 85 percent sand and shell fragments to 60 percent silt and clay. Placement methods for dredged sediment included beach nourishment, stationary submerged discharge, oscillating surface discharge, and construction of emergent dikes. Tidal currents ranged from slack water to flow velocities of 0.60 meter per second. \r\n\r\nPlumes were monitored simultaneously by (1) oblique and vertical 35-millimeter aerial photography and (2) water-quality sampling to determine water clarity and concentrations of nutrients, metals, pesticides, and industrial compounds. Forty-nine photographs depict plumes ranging in length from a few tens of meters to several kilometers and ranging in turbidity level from <10 to 200,000 nephelometric turbidity units. \r\n\r\nThe most visible turbidity plumes were produced by surface discharge of material with high sand content into unconfined placement areas during times of strong tidal currents. The least visible turbidity plumes were produced by discharge of material with high silt and clay content into areas enclosed by floating turbidity barriers during times of weak tidal currents. Beach nourishment from hopper-dredge unloading operations also produced plumes of low visibility. \r\n\r\nPrimary turbidity plumes were produced directly by dredging and placement operations; secondary plumes were produced indirectly by resuspension of previously deposited material. Secondary plumes were formed both by erosion, in areas of high-velocity tidal currents, and by turbulence from vessels passing over fine material deposited in shallow areas. \r\n\r\nWhere turbidity barriers were not used, turbidity plumes visible at the surface were good indicators of the location of turbid water at depth. Where turbidity barriers were used, turbid bottom water was found at locations having no visible surface plumes.\r\n\r\nA region of rapidly accelerating then decelerating flow near the mouth of Tampa Bay produced a two-part or separated plume. Flow acceleration contracted the width of the visible plume, and subsequent flow deceleration caused plume expansion. The two wide segments of the plume appeared to be separated from each other because of the intervening narrow part. \r\n\r\nWaters ambient to the plumes were tested for clarity in two sections of Tampa Bay. Ambient-water transparency in Tampa Bay was about three times greater near its mouth, in South Tampa Bay, than near its head, in Hillsborough Bay. Two other measures of water clarity, turbidity and suspended solids, showed no statistically significant difference between the two areas, however, indicating that transparency is a more sensitive measure of ambient water clarity than either turbidity or suspended solids. \r\n\r\nThe nutrient and metal concentrations for samples of plume water and water ambient to the plumes in Tampa Bay were statistically equivalent, indicating no detectable changes due to dredging. The concentrations of dissolved copper, lead, mercury, and total mercury, however, were greater in plumes in Hillsborough Bay than in South Tampa Bay. In Hillsborough Bay, six occurrences of the herbicide 2,4-D at concentrations near the detection limit, 0.01 to 0.05 micrograms per liter, were unrelated to dredging activity. \r\n\r\nData recorded for longer than the study period indicate that from 1976 through 1979 few average turbidity characteristics in South Tampa and Hillsborough Bays can be directly attributed to dredging operation","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2192","usgsCitation":"Goodwin, C., and Michaelis, D., 1984, Appearance and water quality of turbidity plumes produced by dredging in Tampa Bay, Florida: U.S. Geological Survey Water Supply Paper 2192, vi, 66 p. :ill. (some col.), maps ;28 cm., https://doi.org/10.3133/wsp2192.","productDescription":"vi, 66 p. :ill. (some col.), maps ;28 cm.","costCenters":[],"links":[{"id":137051,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2192/report-thumb.jpg"},{"id":26778,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2192/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac7e4b07f02db67add0","contributors":{"authors":[{"text":"Goodwin, Carl R.","contributorId":76284,"corporation":false,"usgs":true,"family":"Goodwin","given":"Carl R.","affiliations":[],"preferred":false,"id":143983,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Michaelis, D.M.","contributorId":44896,"corporation":false,"usgs":true,"family":"Michaelis","given":"D.M.","email":"","affiliations":[],"preferred":false,"id":143982,"contributorType":{"id":1,"text":"Authors"},"rank":2}]}} ,{"id":61193,"text":"mf1589B - 1984 - Geologic map of the Ten Lake Wilderness Study Area, Lincoln County, Montana","interactions":[],"lastModifiedDate":"2012-02-10T00:10:50","indexId":"mf1589B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"1589","chapter":"B","title":"Geologic map of the Ten Lake Wilderness Study Area, Lincoln County, Montana","language":"ENGLISH","doi":"10.3133/mf1589B","usgsCitation":"Whipple, J.W., 1984, Geologic map of the Ten Lake Wilderness Study Area, Lincoln County, Montana: U.S. Geological Survey Miscellaneous Field Studies Map 1589, 1 map ;42 x 42 cm., on sheet 66 x 106 cm., folded in envelope 25 x 32 cm., https://doi.org/10.3133/mf1589B.","productDescription":"1 map ;42 x 42 cm., on sheet 66 x 106 cm., folded in envelope 25 x 32 cm.","costCenters":[],"links":[{"id":106091,"rank":700,"type":{"id":15,"text":"Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_7507.htm","linkFileType":{"id":5,"text":"html"},"description":"7507"},{"id":187302,"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\": [ [ [ -115,48.8675 ], [ -115,49 ], [ -114.75,49 ], [ -114.75,48.8675 ], [ -115,48.8675 ] ] ] } } ] }","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ae5e4b07f02db68a575","contributors":{"authors":[{"text":"Whipple, J. W.","contributorId":61477,"corporation":false,"usgs":true,"family":"Whipple","given":"J.","email":"","middleInitial":"W.","affiliations":[],"preferred":false,"id":265163,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25654,"text":"wri834116B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","interactions":[],"lastModifiedDate":"2020-03-27T14:22:19","indexId":"wri834116B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4116","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Southern California","docAbstract":"

This report on ground-water levels, springs and depth to ground water in the Basin and Range province of southern California (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.

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No abstract available.

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\"}}]}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a0ae4b07f02db5fb550","contributors":{"authors":[{"text":"Shields, R.R.","contributorId":106916,"corporation":false,"usgs":true,"family":"Shields","given":"R.R.","email":"","affiliations":[],"preferred":false,"id":256541,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Knapton, J. R.","contributorId":84385,"corporation":false,"usgs":true,"family":"Knapton","given":"J.","email":"","middleInitial":"R.","affiliations":[],"preferred":false,"id":256539,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"White, M. K.","contributorId":74395,"corporation":false,"usgs":true,"family":"White","given":"M.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":256538,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Jacobson, M.A.","contributorId":7279,"corporation":false,"usgs":true,"family":"Jacobson","given":"M.A.","email":"","affiliations":[],"preferred":false,"id":256537,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Kasman, M.L.","contributorId":85254,"corporation":false,"usgs":true,"family":"Kasman","given":"M.L.","email":"","affiliations":[],"preferred":false,"id":256540,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25655,"text":"wri834121B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas","interactions":[],"lastModifiedDate":"2021-12-21T20:19:30.884169","indexId":"wri834121B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4121","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas","docAbstract":"

This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Texas (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834121B","collaboration":"Prepared in cooperation with the Texas Bureau of Economic Geology","usgsCitation":"Brady, B.T., Bedinger, M.S., Mulvihill, D.A., Mikels, J., and Langer, W.H., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range Province, Texas: U.S. Geological Survey Water-Resources Investigations Report 83-4121, Report: 7 p.; 1 Plate: 38.65 x 54.85 inches, https://doi.org/10.3133/wri834121B.","productDescription":"Report: 7 p.; 1 Plate: 38.65 x 54.85 inches","costCenters":[{"id":583,"text":"Texas Water Science Center","active":true,"usgs":true}],"links":[{"id":121733,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4121b/report-thumb.jpg"},{"id":393239,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4121b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":54426,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4121b/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"country":"United States","state":"Texas","otherGeospatial":"Basin and Range Province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -106.6552734375,\n 28.844673680771795\n ],\n [\n -101.7333984375,\n 28.844673680771795\n ],\n [\n -101.7333984375,\n 31.87755764334002\n ],\n [\n -106.6552734375,\n 31.87755764334002\n ],\n [\n -106.6552734375,\n 28.844673680771795\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a61","contributors":{"authors":[{"text":"Brady, B. T.","contributorId":93047,"corporation":false,"usgs":true,"family":"Brady","given":"B.","email":"","middleInitial":"T.","affiliations":[],"preferred":false,"id":194532,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194530,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194531,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Mikels, John","contributorId":24817,"corporation":false,"usgs":true,"family":"Mikels","given":"John","email":"","affiliations":[],"preferred":false,"id":194528,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194529,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","interactions":[{"subject":{"id":10555,"text":"ofr8278 - 1982 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium","indexId":"ofr8278","publicationYear":"1982","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois; Part II, geology and hydrology of the glacial drift as related to the migration of tritium"},"predicate":"SUPERSEDED_BY","object":{"id":2414,"text":"wsp2226 - 1984 - Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","indexId":"wsp2226","publicationYear":"1984","noYear":false,"title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium"},"id":1}],"lastModifiedDate":"2022-02-04T19:13:10.348121","indexId":"wsp2226","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2226","title":"Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium","docAbstract":"A low-level radioactive-waste burial site is located in Palos Forest Preserve, about 22 kilometers southwest of Chicago, Illinois. Between 1943 and 1949 the site, named Plot M, was filled with radioactive waste from the first Argonne National Laboratory and from the University of Chicago Metallurgical Laboratory. Since 1973, tritium concentration levels up to 14 nanocuries per liter have been measured in water samples collected from a well 360 meters from the burial site. \r\n\r\nThe U.S. Geological Survey is studying the geologic, hydrologic, and geochemical properties of the glacial drift and underlying bedrock at the Plot M site to determine the factors that control the movement of radionuclides. Test wells were drilled into the drift to collect water and core samples for laboratory analysis, to gather geologic and hydrologic data, and to conduct geophysical surveys. Plot M is located in drift that ranges in thickness from 25 to 45 meters. The drift is a stratified sequence of clay- and silt-rich sediments that contain thin, interstratified sand layers. The silt content of the drift increases with depth. The permeability of the drift, as indicated by field and laboratory hydraulic conductivity tests, ranges from 1.0 x 10 -6 to 1.0 ? 10 -8 centimeters per second. \r\n\r\nA tritium plume, the contaminated zone in the drift in which tritium concentration levels exceed 10 nanocuries per liter of water, extends horizontally northward from Plot M at least 50 meters and vertically downward to bedrock. The center of the plume, where tritium concentration levels are as high as 50,000 nanocuries per liter, is approximately 15 meters beneath the burial site. The size, shape, and 'bull's-eye' concentration pattern indicate that the plume is a single slug and that the site no longer releases tritium into the drift. The leading edge, or front, of the plume (the 10 nanocuries per liter boundary) left the burial site in either the late 1940's or the early 1950's and intersected the underlying bedrock surface before 1973. The calculated movement rate of the front is 6.3 x 10 -6 centimeters per second. \r\n\r\nSeveral key factors that control both the concentration level and the extent of migration of tritium in the drift at Plot M are 1. The limited amount of tritiated waste buried at Plot M. 2. The long period of time that has elapsed since the waste was buried (30-35 years) relative to the radioactive half-life of tritium (12.3 years). 3. The great thickness and low permeability of the glacial drift at the site.","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wsp2226","usgsCitation":"Olimpio, J.C., 1984, Low-level radioactive-waste burial at the Palos Forest Preserve, Illinois: Geology and hydrology of the glacial drift, as related to the migration of tritium: U.S. Geological Survey Water Supply Paper 2226, iv, 34 p., https://doi.org/10.3133/wsp2226.","productDescription":"iv, 34 p.","costCenters":[],"links":[{"id":395461,"rank":3,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_25214.htm"},{"id":28419,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2226/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":138667,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2226/report-thumb.jpg"}],"country":"United States","state":"Illinios","otherGeospatial":"Palos Forest Preserve","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -87.906,\n 41.694\n ],\n [\n -87.917,\n 41.694\n ],\n [\n -87.917,\n 41.704\n ],\n [\n -87.906,\n 41.704\n ],\n [\n -87.906,\n 41.694\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a7fe4b07f02db648815","contributors":{"authors":[{"text":"Olimpio, Julio C.","contributorId":93877,"corporation":false,"usgs":true,"family":"Olimpio","given":"Julio","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":145162,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25656,"text":"wri834119B - 1984 - Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Nevada","interactions":[],"lastModifiedDate":"2023-01-10T21:59:28.784867","indexId":"wri834119B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4119","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Nevada","docAbstract":"

This report on ground-water levels, springs and depth to ground water in the Basin and Range province of Nevada (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984). Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834119B","usgsCitation":"Bedinger, M.S., Harrill, J., Langer, W.H., Thomas, J.M., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to water, Basin and Range Province, Nevada: U.S. Geological Survey Water-Resources Investigations Report 83-4119, Report: 11 p.; 2 Plates: 44.07 x 40.71 inches and 55.63 x 33.73 inches, https://doi.org/10.3133/wri834119B.","productDescription":"Report: 11 p.; 2 Plates: 44.07 x 40.71 inches and 55.63 x 33.73 inches","costCenters":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"links":[{"id":411675,"rank":5,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35765.htm","linkFileType":{"id":5,"text":"html"}},{"id":54427,"rank":4,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4119b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":373622,"rank":3,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119b/plate-2.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118966,"rank":1,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4119b/report-thumb.jpg"},{"id":373623,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4119b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}}],"scale":"500000","datum":"National Geodetic Vertical Datum of 1929","country":"United States","state":"Nevada","otherGeospatial":"Basin and Range province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -120.0146484375,\n 35.02099970111467\n ],\n [\n -114.027099609375,\n 35.02099970111467\n ],\n [\n -114.027099609375,\n 42.00032514831621\n ],\n [\n -120.0146484375,\n 42.00032514831621\n ],\n [\n -120.0146484375,\n 35.02099970111467\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a65","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194536,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Harrill, J. R.","contributorId":10417,"corporation":false,"usgs":true,"family":"Harrill","given":"J. R.","affiliations":[],"preferred":false,"id":194533,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langer, William H. blanger@usgs.gov","contributorId":1241,"corporation":false,"usgs":true,"family":"Langer","given":"William","email":"blanger@usgs.gov","middleInitial":"H.","affiliations":[{"id":387,"text":"Mineral Resources Program","active":true,"usgs":true}],"preferred":false,"id":194534,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Thomas, J. M.","contributorId":62217,"corporation":false,"usgs":true,"family":"Thomas","given":"J.","email":"","middleInitial":"M.","affiliations":[],"preferred":false,"id":194535,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194537,"contributorType":{"id":1,"text":"Authors"},"rank":5}]}} ,{"id":25126,"text":"cir930B - 1984 - International strategic minerals inventory summary report; chromium","interactions":[],"lastModifiedDate":"2018-11-05T10:20:12","indexId":"cir930B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"930","chapter":"B","title":"International strategic minerals inventory summary report; chromium","docAbstract":"Major world resources of chromium, a strategic mineral commodity, are described in this summary report of information in the International Strategic Minerals Inventory {ISMI}. ISMI is a cooperative data-collection effort of earth-science and mineral-resource agencies in Australia, Canada, the Federal Republic of Germany, the Republic of South Africa, and the United States of America. This report, designed to be of benefit to policy analysts, contains two parts. Part I presents an overview of the resources and potential supply of chromium on the basis of inventory information. Part II contains tables of some of the geologic information and mineral-resource and production data that were collected by ISMI participants.","language":"ENGLISH","publisher":"U.S. Dept. of the Interior, Geological Survey,","doi":"10.3133/cir930B","usgsCitation":"DeYoung, J., Lee, M.P., and Lipin, B., 1984, International strategic minerals inventory summary report; chromium: U.S. Geological Survey Circular 930, v. :ill. ;26 cm.; 41 p., https://doi.org/10.3133/cir930B.","productDescription":"v. :ill. ;26 cm.; 41 p.","costCenters":[{"id":245,"text":"Eastern Mineral and Environmental Resources Science Center","active":true,"usgs":true}],"links":[{"id":54106,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/circ/1984/0930b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":122560,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/circ/1984/0930b/report-thumb.jpg"}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49dbe4b07f02db5e0829","contributors":{"authors":[{"text":"DeYoung, J.H. Jr.","contributorId":86367,"corporation":false,"usgs":true,"family":"DeYoung","given":"J.H.","suffix":"Jr.","email":"","affiliations":[],"preferred":false,"id":193259,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Lee, M. P.","contributorId":40198,"corporation":false,"usgs":true,"family":"Lee","given":"M.","email":"","middleInitial":"P.","affiliations":[],"preferred":false,"id":193257,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Lipin, B. R.","contributorId":61031,"corporation":false,"usgs":true,"family":"Lipin","given":"B. R.","affiliations":[],"preferred":false,"id":193258,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":2486,"text":"wsp2228 - 1984 - Evaluation of environmental factors affecting yields of major dissolved ions of streams in the United States","interactions":[],"lastModifiedDate":"2012-02-02T00:05:26","indexId":"wsp2228","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"2228","title":"Evaluation of environmental factors affecting yields of major dissolved ions of streams in the United States","docAbstract":"The seven major dissolved ions in streams-sodium, potassium, magnesium, calcium, chloride, sulfate, and bicarbonate and their sum dissolved solids from 56 basins in the conterminous United States and Hawaii were correlated with bedrock type, annual precipitation, population density, and average stream temperature of their respective basins through multiple linear-regression equations to predict annual yields. The study was restricted to basins underlain by limestone, sandstone, or crystalline rock. Depending on the constituent, yields ranged from about 10 to 100,000 kilograms per square kilometer. Predicted yields were within 1 order of magnitude of measured yields. \r\n\r\nThe most important factor in yield prediction was annual precipitation, which accounted for 58 to 71 percent of all yields. Rock type was second in importance. Yields of magnesium, calcium, bicarbonate, and dissolved solids from limestone basins were 4 to 10 times larger than those from sandstone or crystalline basins as a result of carbonate weathering. Population density was an ineffective indicator of all constituents except sodium and chloride; it accounted for 13 percent of the annual sodium yield and 20 percent of the annual chloride yield. Average stream temperature was significant only for calcium and bicarbonate in limestone basins. Its relationship with yields was consistently negative. Either carbonate dissolution increases at low temperatures, or weathering in northern basins, which contain glacial deposits and have the lowest stream temperatures, is greater than in southern basins. \r\n\r\nAverage ion contributions from atmospheric deposition accounted for 30 percent of the sodium and chloride and 60 percent of the sulfate in annual yields. The amount of sulfate derived from atmospheric contributions was higher in sandstone and crystalline basins (65 and 80 percent, respectively) than limestone basins (38 percent). This disparity is attributed to the lack of available sulfate in crystalline rock and the chemical precipitation of sulfate in the sandstone basins, most of which are in semi-arid or arid areas.","language":"ENGLISH","publisher":"U.S. G.P.O.,","doi":"10.3133/wsp2228","usgsCitation":"Peters, N.E., 1984, Evaluation of environmental factors affecting yields of major dissolved ions of streams in the United States: U.S. Geological Survey Water Supply Paper 2228, iv, 39 p. :ill. ;28 cm., https://doi.org/10.3133/wsp2228.","productDescription":"iv, 39 p. :ill. ;28 cm.","numberOfPages":"43","costCenters":[],"links":[{"id":138714,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wsp/2228/report-thumb.jpg"},{"id":28582,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wsp/2228/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a4be4b07f02db62531f","contributors":{"authors":[{"text":"Peters, Norman E. nepeters@usgs.gov","contributorId":1324,"corporation":false,"usgs":true,"family":"Peters","given":"Norman","email":"nepeters@usgs.gov","middleInitial":"E.","affiliations":[{"id":316,"text":"Georgia Water Science Center","active":true,"usgs":true}],"preferred":true,"id":145273,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":25657,"text":"wri834122B - 1984 - Maps showing ground-water levels, springs, and depth to ground water, Basin and Range province, Utah","interactions":[],"lastModifiedDate":"2022-01-10T21:03:50.927375","indexId":"wri834122B","displayToPublicDate":"1994-01-01T00:00:00","publicationYear":"1984","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":"83-4122","chapter":"B","title":"Maps showing ground-water levels, springs, and depth to ground water, Basin and Range province, Utah","docAbstract":"

This report on ground-water levels, springs, and depth to ground water in the Basin and Range province of Utah (see index map) was prepared as part of a program of the U.S. Geological Survey to identify prospective regions for further study relative to isolation of high-level nuclear waste (Bedinger, Sargent, and Reed, 1984), utilizing program guidelines defined in Sargent and Bedinger (1984) . Also included in this report are selected references on pertinent geologic and hydrologic studies of the region. Other map reports in this series contain detailed data on ground-water quality, surface distribution of selected rock types, tectonic conditions, areal geophysics, Pleistocene lakes and marshes, and mineral and energy resources.

","language":"English","publisher":"U.S. Geological Survey","doi":"10.3133/wri834122B","collaboration":"Prepared in cooperation with the Utah Geological Survey","usgsCitation":"Bedinger, M.S., Mason, J.L., Langer, W.H., Gates, J.S., Stark, J., and Mulvihill, D.A., 1984, Maps showing ground-water levels, springs, and depth to ground water, Basin and Range province, Utah: U.S. Geological Survey Water-Resources Investigations Report 83-4122, Report: 12 p.; 1 Plate: 40.63 x 50.36 inches, https://doi.org/10.3133/wri834122B.","productDescription":"Report: 12 p.; 1 Plate: 40.63 x 50.36 inches","costCenters":[],"links":[{"id":393242,"rank":2,"type":{"id":17,"text":"Plate"},"url":"https://pubs.usgs.gov/wri/1983/4122b/plate-1.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":118967,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/wri/1983/4122b/report-thumb.jpg"},{"id":54428,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/wri/1983/4122b/report.pdf","linkFileType":{"id":1,"text":"pdf"}},{"id":394140,"rank":4,"type":{"id":36,"text":"NGMDB Index Page"},"url":"https://ngmdb.usgs.gov/Prodesc/proddesc_35782.htm"}],"country":"United States","state":"Utah","otherGeospatial":"Basin and Range province","geographicExtents":"{\n \"type\": \"FeatureCollection\",\n \"features\": [\n {\n \"type\": \"Feature\",\n \"properties\": {},\n \"geometry\": {\n \"type\": \"Polygon\",\n \"coordinates\": [\n [\n [\n -114.042,\n 37\n ],\n [\n -111.29,\n 37\n ],\n [\n -111.29,\n 42\n ],\n [\n -114.042,\n 42\n ],\n [\n -114.042,\n 37\n ]\n ]\n ]\n }\n }\n ]\n}","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4a19e4b07f02db605a6e","contributors":{"authors":[{"text":"Bedinger, M. S.","contributorId":65452,"corporation":false,"usgs":true,"family":"Bedinger","given":"M.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194540,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Mason, J. L.","contributorId":24389,"corporation":false,"usgs":true,"family":"Mason","given":"J.","email":"","middleInitial":"L.","affiliations":[],"preferred":false,"id":194538,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Langer, W. H.","contributorId":44932,"corporation":false,"usgs":true,"family":"Langer","given":"W.","email":"","middleInitial":"H.","affiliations":[],"preferred":false,"id":194539,"contributorType":{"id":1,"text":"Authors"},"rank":3},{"text":"Gates, J. S.","contributorId":99553,"corporation":false,"usgs":true,"family":"Gates","given":"J.","email":"","middleInitial":"S.","affiliations":[],"preferred":false,"id":194542,"contributorType":{"id":1,"text":"Authors"},"rank":4},{"text":"Stark, J. R.","contributorId":100406,"corporation":false,"usgs":true,"family":"Stark","given":"J. R.","affiliations":[],"preferred":false,"id":194543,"contributorType":{"id":1,"text":"Authors"},"rank":5},{"text":"Mulvihill, D. A.","contributorId":73644,"corporation":false,"usgs":true,"family":"Mulvihill","given":"D.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":194541,"contributorType":{"id":1,"text":"Authors"},"rank":6}]}} ]}