1 edition of Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana found in the catalog.

Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana

cuenca del Río Camaná-Majes

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Published by Administrator in U.S. Dept. of the Interior, U.S. Geological Survey

    Places:
  • United States
    • Subjects:
    • U.S. Dept. of the Interior, U.S. Geological Survey


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      • Shipping list no.: 98-0352-PAugust 1998--T.p. versoIncludes bibliographical references (p. 34-35)

        StatementU.S. Dept. of the Interior, U.S. Geological Survey
        PublishersU.S. Dept. of the Interior, U.S. Geological Survey
        Classifications
        LC Classifications1998
        The Physical Object
        Paginationxvi, 126 p. :
        Number of Pages43
        ID Numbers
        ISBN 10nodata
        Series
        1
        2Water-resources investigations report -- 98-4137
        3

        nodata File Size: 10MB.


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Estimated 1996-97 and long-term average annual loads for suspended sediment and selected trace metals in streamflow of the upper Clark Fork basin from Warm Springs to Missoula, Montana by U.S. Dept. of the Interior, U.S. Geological Survey Download PDF EPUB FB2


Sediment accretion rates along Grove Creek were also estimated by radioisotope methods.

Hydrology Data Description

1995, Water-quality, bed-sediment, and biological data October 1993 through September 1994 and statistical summaries of data for streams in the upper Clark Fork Basin, Montana: U. The maximum age of the floodplain sediment at the 2-ft level is about 80 years. Targeted remediation in this reach would be an effective approach to positively influencing the downstream stations. 1990 Stratigraphy and Chemistry of Metal- Contaminated Floodplain Sediments, Upper Clark Fork River Valley, Montana KUZEL, LAURA S.

Contact Information: Questions about data can be directed to: Website: Restoration Planning: Stream flow data are useful primarily for restoration projects that involve channel design. The geographic area covered by the study extended from the headwaters of the Rio Grande in southern Colorado to Elephant Butte Reservoir in southern New Mexico. Blacktail Creek at Butte - From: 1988-10-03 To: 2000-08-30 Count: 154• 1993 The Role of Fe and Mn Oxy-hydroxides in Contaminated Coarse-Grained River Sediment BENNER, SHAWN G.

It is intended to store water chemistry, biological and physical habitat data. 1988 Particle-size and chemical control of metals in Clark Fork River bed sediment BROOKS, REBEKAH M.

Influence of remediation in a mine‐impacted river: metal trends over large spatial and temporal scales, Ecological Applications

:also by J. Connectivity for both Cu and Cd was strong at small spatial scales.1997, Water-quality, bed-sediment, and biological data October 1995 through September 1996 and statistical summaries of data for streams in the upper Clark Fork basin, Montana: U.

Mean depth of bankfull channel, in feet 11 Sites include with flood frequency calculations include: Blacktail Creek at Butte Silver Bow Cr below Blacktail Cr at Butte, MT Smith Gulch near Silver Bow, MT German Gulch Creek near Ramsay, MT Silver Bow Creek at Opportunity, MT Silver Bow Creek at Warm Springs, MT Warm Springs Creek at Warm Springs, MT Racetrack Cr below Granite Cr near Anaconda, MT Clark Fork at Deer Lodge, MT Cottonwood Creek at Deer Lodge, MT Little Blackfoot River near Garrison, MT Clark Fork at Goldcreek, MT Clark Fork Tributary near Drummond, MT Morris Creek near Drummond, MT Flint Creek near Southern Cross, MT Flint Creek at Maxville, MT Boulder Creek at Maxville, MT Clark Fork at Drummond, MT Edwards Gulch at Drummond, MT Clark Fork near Clinton, MT Middle Fork Rock Cr near Philipsburg, MT Rock Creek near Clinton, MT Clark Fork at Turah Bridge near Bonner, MT Blackfoot River near Bonner, MT Marshall Creek near Missoula, MT Clark Fork above Missoula, MT Restoration Planning: This information provides a long-term baseline against which we will be able to measure improvements in water, sediment and benthic metals levels as a result of remediation and restoration.

Temporal, taxonomic and spatial patterns were observed. Information on data reliability is available at Reference: U. There was no significant difference in the relative abundance of fishes in Coeur d'Alene Lake from 1997 to 1998.

For location data for each station, go to the site map options from the pull-down menu on the station home page links below to obtain gage location, gage datum, watershed area, and period of record.