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No abstract available. 

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K.","contributorId":37757,"corporation":false,"usgs":true,"family":"Maurer","given":"D.","email":"","middleInitial":"K.","affiliations":[],"preferred":false,"id":181201,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19851,"text":"ofr84432 - 1984 - Flow-duration hydrographs for selected streamflow stations on South Dakota streams","interactions":[],"lastModifiedDate":"2012-02-02T00:07:36","indexId":"ofr84432","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":"84-432","title":"Flow-duration hydrographs for selected streamflow stations on South Dakota streams","docAbstract":"Duration hydrographs showing the percent of time which specified discharges were equaled or exceeded on nine South Dakota streams are presented. Accompanying tables list the values plotted on the hydrographs and the 10, 30, 70, and 90 percent exceedence values for the streams. (USGS)","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84432","usgsCitation":"Little, J., 1984, Flow-duration hydrographs for selected streamflow stations on South Dakota streams: U.S. Geological Survey Open-File Report 84-432, iv, 129 p. :ill., map ;28 cm., https://doi.org/10.3133/ofr84432.","productDescription":"iv, 129 p. :ill., map ;28 cm.","costCenters":[],"links":[{"id":152652,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0432/report-thumb.jpg"},{"id":49330,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0432/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4786e4b07f02db485767","contributors":{"authors":[{"text":"Little, J.R.","contributorId":42976,"corporation":false,"usgs":true,"family":"Little","given":"J.R.","email":"","affiliations":[],"preferred":false,"id":181629,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":20223,"text":"ofr84280 - 1984 - Improved digital filters for the calculation of Schlumberger sounding curves by convolution","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr84280","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":"84-280","title":"Improved digital filters for the calculation of Schlumberger sounding curves by convolution","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84280","usgsCitation":"Murakami, Y., Zerilli, A., and Bisdorf, R., 1984, Improved digital filters for the calculation of Schlumberger sounding curves by convolution: U.S. Geological Survey Open-File Report 84-280, 19 p. ;28 cm., https://doi.org/10.3133/ofr84280.","productDescription":"19 p. ;28 cm.","costCenters":[],"links":[{"id":152812,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0280/report-thumb.jpg"},{"id":49762,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0280/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e49fde4b07f02db5f5d9c","contributors":{"authors":[{"text":"Murakami, Yutaka","contributorId":67531,"corporation":false,"usgs":true,"family":"Murakami","given":"Yutaka","email":"","affiliations":[],"preferred":false,"id":182276,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Zerilli, Andrea","contributorId":98330,"corporation":false,"usgs":true,"family":"Zerilli","given":"Andrea","email":"","affiliations":[],"preferred":false,"id":182277,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Bisdorf, R.J.","contributorId":42960,"corporation":false,"usgs":true,"family":"Bisdorf","given":"R.J.","email":"","affiliations":[],"preferred":false,"id":182275,"contributorType":{"id":1,"text":"Authors"},"rank":3}]}} ,{"id":19434,"text":"ofr84219 - 1984 - Geology of volcanogenic uranium deposits within the Tallahassee Creek Conglomerate, Tallahassee Creek uranium district, Colorado","interactions":[],"lastModifiedDate":"2012-02-02T00:07:34","indexId":"ofr84219","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":"84-219","title":"Geology of volcanogenic uranium deposits within the Tallahassee Creek Conglomerate, Tallahassee Creek uranium district, Colorado","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84219","usgsCitation":"Hon, K., 1984, Geology of volcanogenic uranium deposits within the Tallahassee Creek Conglomerate, Tallahassee Creek uranium district, Colorado: U.S. Geological Survey Open-File Report 84-219, iii, 58 p. :maps ;28 cm., https://doi.org/10.3133/ofr84219.","productDescription":"iii, 58 p. :maps ;28 cm.","costCenters":[],"links":[{"id":152686,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0219/report-thumb.jpg"},{"id":48910,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0219/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4ac9e4b07f02db67c738","contributors":{"authors":[{"text":"Hon, Ken","contributorId":19163,"corporation":false,"usgs":true,"family":"Hon","given":"Ken","affiliations":[],"preferred":false,"id":180894,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"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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Operation of a coal-tar distillation and wood-preserving facility in St. Louis Park, Minnesota, during 1918-72 contaminated ground water with coal-tar derivatives and inorganic chemicals. Coal-tar derivatives entered the groundwater system through three major paths: (1) Spills and drippings that percolated to the water table, (2) surface runoff and plant process water that was discharged to wetlands south of the former plant site, and (3) movement of coal tar directly into bedrock aquifers through a multiaquifer well on the site.

\n

In the drift, Platteville, and St. Peter aquifers, ground water flows laterally from west to east and vertically downward. Near the former plant site, creosote-like organic fluids have migrated vertically downward through the drift and are being partially dissolved by ground water. Ground water has preferentially mobilized low-molecular-weight compounds such as phenolic compounds, alkyl-benzenes, and naphthalene, although polynuclear aromatic hydrocarbons as heavy as benzo(a)pyrene have been mobilized at low concentrations. Sorption of high-molecular-weight compounds has retarded their migration down the hydraulic gradient compared to low-molecular-weight compounds in the plume. Some simple phenolic compounds are being degraded to methane and carbon dioxide by bacteria under anaerobic conditions in the drift-PlattevilleSt. Peter aquifer system. Other low-molecular-weight aromatic compounds are apparently being degraded by aerobic bacteria at the periphery of the plume where oxygen is available. Intermediate degradation products such as volatile fatty acids are likely present, but complete conversion of the organic contaminants to innocuous inorganic substances has not been demonstrated. Near and south of 36th and Wooddale Avenues, contaminants enter the St. Peter aquifer where the Glenwood confining unit has been eroded in a buried bedrock valley. Contaminants previously entered the Prairie du Chien-Jordan aquifer through at least one multiaquif er well (W38). Other sources of contaminants and the low concentrations of contaminants hamper delineation of the maximum areal extent of contaminants that are resistant to biologic degradation. These biorefractory compounds will probably continue to migrate down the hydraulic gradients in the drift and Platteville and St. Peter aquifers.

\n

Of particular concern with respect to the health risk to humans are the polynuclear aromatic hydrocarbons, which are a major constituent of coal tar and are found in municipal wells near the site that are completed in the Prairie du Chien-Jordan aquifer. The Prairie du Chien-Jordan aquifer lies 250 to 500 feet below land surface and is relatively well protected from nearsurface sources of contamination by overlying rocks. However, the aquifer has been contaminated since at least 1932 because coal-tar derivatives have entered the aquifer through multiaquifer wells. The most significant single source of contamination in the aquifer is a well drilled on the site in 1917 (well W23) that has contained liquid coal-tar since at least 1958. The introduction, dissolution, and movement of this coal-tar in ground water has contaminated nearby municipal wells. The composition of the tar in well W23, and the ratio of concentrations of individual compounds in water from well W23 to those in municipal well SLP15, are consistent with known hydrologic, chemical, and biologic processes, and the conclusion that contaminants in well SLP15 are due primarily to contaminants introduced at well W23. Most of the major polynuclear aromatic hydrocarbons in the tar, although slightly soluble in water and strongly sorbed by aquifer materials, have moved greater distances at higher concentrations than have the lower-molecular-weight, more soluble compounds such as phenolic compounds and naphthalene. The latter are apparently being degraded by bacteria.

\n

The direction and rate of contaminant movement within the Prairie du Chien-Jordan aquifer changes with time because the ground-water-flow system continually adjusts to hydraulic stresses caused by ground-water withdrawals and flow through multiaquifer wells. Contaminants can move rapidly through the Prairie du Chien-Jordan because the upper part of the aquifer is a carbonate rock having fracture and solution-channel permeability, low effective porosity, and relatively small surface area for sorption. Consequently, the concentration and composition of contaminants in water pumped from individual industrial and municipal wells completed in the aquifer fluctuate with time. Although contaminants have been in the aquifer for at least 50 years and their spatial distribution is complex, concentrations remain highest near their points of introduction through multiaquifer wells near and on the site of the former plant.

\n

Contaminants reached the Ironton-Galesville aquifer through at least two deep multiaquifer wells (W23 and W38), but the extent of contamination in this aquifer, and in the underlying Mount Simon-Hinckley aquifer, is not known.

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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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\"}}]}\n","noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4aafe4b07f02db66cd20","contributors":{"authors":[{"text":"Huffman, G.C.","contributorId":44150,"corporation":false,"usgs":true,"family":"Huffman","given":"G.C.","email":"","affiliations":[],"preferred":false,"id":159993,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9230,"text":"ofr84327 - 1984 - Stratigraphy of the Murdama Formation between Afif, Halaban, and As Sawadah, Kingdom of Saudi Arabia","interactions":[],"lastModifiedDate":"2012-02-02T00:06:14","indexId":"ofr84327","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":"84-327","title":"Stratigraphy of the Murdama Formation between Afif, Halaban, and As Sawadah, Kingdom of Saudi Arabia","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84327","usgsCitation":"Greene, R.C., 1984, Stratigraphy of the Murdama Formation between Afif, Halaban, and As Sawadah, Kingdom of Saudi Arabia: U.S. Geological Survey Open-File Report 84-327, ii, 38 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84327.","productDescription":"ii, 38 p. :ill., maps ;28 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C.","contributorId":88347,"corporation":false,"usgs":true,"family":"Greene","given":"R.","email":"","middleInitial":"C.","affiliations":[],"preferred":false,"id":159322,"contributorType":{"id":1,"text":"Authors"},"rank":1}]}} ,{"id":9571,"text":"ofr84846 - 1984 - Telluric traverse data release for the Getchell and Preble disseminated gold deposits, Humboldt County, Nevada","interactions":[],"lastModifiedDate":"2012-02-02T00:06:16","indexId":"ofr84846","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":"84-846","title":"Telluric traverse data release for the Getchell and Preble disseminated gold deposits, Humboldt County, Nevada","language":"ENGLISH","publisher":"U.S. Geological Survey,","doi":"10.3133/ofr84846","usgsCitation":"Hoover, D., Pierce, H.A., and Abrams, G.A., 1984, Telluric traverse data release for the Getchell and Preble disseminated gold deposits, Humboldt County, Nevada: U.S. Geological Survey Open-File Report 84-846, 14 p. :ill., maps ;28 cm., https://doi.org/10.3133/ofr84846.","productDescription":"14 p. :ill., maps ;28 cm.","costCenters":[],"links":[{"id":141828,"rank":0,"type":{"id":24,"text":"Thumbnail"},"url":"https://pubs.usgs.gov/of/1984/0846/report-thumb.jpg"},{"id":37297,"rank":300,"type":{"id":11,"text":"Document"},"url":"https://pubs.usgs.gov/of/1984/0846/report.pdf","linkFileType":{"id":1,"text":"pdf"}}],"noUsgsAuthors":false,"publicationStatus":"PW","scienceBaseUri":"4f4e4adae4b07f02db685830","contributors":{"authors":[{"text":"Hoover, D.B.","contributorId":37734,"corporation":false,"usgs":true,"family":"Hoover","given":"D.B.","email":"","affiliations":[],"preferred":false,"id":159922,"contributorType":{"id":1,"text":"Authors"},"rank":1},{"text":"Pierce, H. A.","contributorId":99951,"corporation":false,"usgs":true,"family":"Pierce","given":"H.","email":"","middleInitial":"A.","affiliations":[],"preferred":false,"id":159923,"contributorType":{"id":1,"text":"Authors"},"rank":2},{"text":"Abrams, G. 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The compilation of pertinent data indicates that information is available for use in the evaluation of the ground-water resources of the 13 counties of coastal Georgia. Included in this report is a fairly complete discussion of previous and ongoing investigations and monitoring networks, and an extensive list of references. Maps at 1:24,000, 1:100,000; and 1:1000,000 scales contain well locations and identifers for all wells in the Ground Water Site Inventory (GWSI) data base of the National Water Data Storage and Retrieval System (WATSTORE). Tabular summaries of selected site information from GWSI, including well identifiers and names , latitude-longitude location, depth of well, altitude of land surface, and use of water are presented. Water-use data from the National Water Use Data System, and water use for irrigation from the University of Georgia, Department of Agriculture survey , are tabulated. 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