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.
Published 1998 by Administrator in U.S. Dept. of the Interior, U.S. Geological Survey
Shipping list no.: 98-0352-PAugust 1998--T.p. versoIncludes bibliographical references (p. 34-35)
|Statement||U.S. Dept. of the Interior, U.S. Geological Survey|
|Publishers||U.S. Dept. of the Interior, U.S. Geological Survey|
|The Physical Object|
|Pagination||xvi, 126 p. :|
|Number of Pages||43|
|2||Water-resources investigations report -- 98-4137|
nodata File Size: 10MB.
Sediment accretion rates along Grove Creek were also estimated by radioisotope methods.
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.
: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.
During September and October 1987, streambed sediments were collected in the lower Kansas River basin of Kansas and Nebraska as part of the US Geological Survey's National Water-Quality Assessment Program.
The LANL plutonium is identifiable intermittently along the 35-km reach of the Rio Grande to Cochiti Reservoir.
Daily Stream Flow - graphs or data tables anytime within the period of record• Since 1994, the Coeur d'Alene Tribe Fish, Water and Wildlife Program has conducted an extensive mark-recapture study Peters et al.