1 edition of Sediment-transport investigations of the upper Yellowstone River, Montana, 1999 through 2001 found in the catalog.
Sediment-transport investigations of the upper Yellowstone River, Montana, 1999 through 2001
Stephen R. Holnbeck
|Statement||by Stephen R. Holnbeck ; in cooperation with Park Conservation District, Montana Department of Transportation, and the U.S. Army Corps of Engineers|
|Series||Scientific investigations report -- 2005-5234|
|Contributions||Park Conservation District (Mont.), Montana. Dept. of Transportation, United States. Army. Corps of Engineers, Geological Survey (U.S.), Governor"s Upper Yellowstone River Task Force (Mont.)|
|The Physical Object|
|Format||[electronic resource] /|
|Pagination||viii, 69 p. :|
|Number of Pages||69|
Aug 17 32 m3/s m3/s m3/s ( cfs) (18, cfs) ( cfs) Figure 2. An example (for the year ) of the combined hydrograph of the three tributaries contributing to the Buffalo River. investigations, a pilot STA based on a limited number of sed-iment samples collected in and a full-scale STA based. Welcome to the new New features include: Split screen display — allows users to scroll the journal article and the article figures simultaneously; Faceted searching — added facets for journal, journal section, article type, book series and GeoRef keywords; Integrated OpenGeoSci Map view search results — allows users to limit search by geographic location.
Measurements of suspended- and bedload-sediment transport for the Tanana River in the vicinity of Fairbanks, Alaska, show that suspended-sediment load, G in tons per day, relates to water discharge, Q, in cubic feet per scond, as:GS = x QThe bedload transport rate is approximately one percent of the suspended-sediment transport median particle size of suspended sediment. Geology of the Powder River Basin, Wyoming and Montana, with reference to subsurface disposal of radioactive wastes [Trace Element Investigations Report TEI], by H.M. Beikman. 85 p. [Number assigned after report was published].
Presenter: Dr. Craig Jones Sea Engineering, Inc. April 9, Sediment transport in the Tanana River in the vicinity of Fairbanks, Alaska, USGS Open-File Report [Robert L. Burrows, Bruce Parks, William W. Emmett] on *FREE* shipping on qualifying offers. Measurements of the sediment load of the Tanana River in the vicinity of Fairbanks, Alaska, show that suspended-sediment transport rate in tons per dayAuthors: William W. Emmett, Bruce Parks, Robert L. Burrows.
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Sediment-Transport Investigations of the Upper Yellowstone River, Montana, through Data Collection, Analysis, and Simulation of Sediment Transport Scientific Investigations Report By Stephen R. Holnbeck.
The full report is in Adobe Acrobat® Portable Document Format (PDF). Sediment-Transport Investigations of the Upper Yellowstone River, Montana, through Data Collection, Analysis, and Simulation of Sediment Transport By Stephen R. Holnbeck U.S. Department of the Interior U.S.
Geological Survey In cooperation with Park Conservation District, Montana Department of Transportation, and the. Sediment-Transport Investigations of the Upper Yellowstone River, Montana, through Data Collection, Analysis, and Simulation of Sediment Transport Article January with 5 Reads.
In the wake of back-to-back, year flood events, Montana’s Governor appointed the Upper Yellowstone River Task Force in November The Task Force was directed to bring together landowners, sportsmen/women, and community leaders, and to provide a forum for the discussion of the issues, competing values, and uses that impact the River.
Sediment-Transport Investigations of the Upper Yellowstone River, Montana, Through Data Collection, Analysis, And Simulation of Sediment Transport [electronic Resource] of. Suspended sediment transport patterns on the inner shelf – S. Pedro de Moel (Portugal) Sediment-Transport Investigations of the Upper Yellowstone River, Montana, through Data C.
Sediment Transport in Kulim Montana, Kedah, Malaysia Chun Kiat, Chang and Aminuddin, Ab. Ghani Sediment Transport is a book that covers a wide variety of subject matt ers.
Physicists, engineers, mathematicians, statisticians, and geologists have been investigating sedi- 6 Sep 7 Sep 8 Oct 9 Bechteler W., Vogel G., Vollmers H.J.
() Model investigations on the sediment transport of a lower alpine river. In: Armanini A., Di Silvio G. (eds) Fluvial Hydraulics of Mountain Regions. Lecture Notes in Earth Sciences, vol Cited by: 1. proportion of the total sediment transport to come from the Upper Clark Fork Arm of the reservoir.
Conversion from short tons to metric tons is shown in Table Figure Results from the Blackfoot (A) and upper Clark Fork (B) Arms of the reservoir for DREAM-1 model Run : James Walden Johnsen. The Marias River cuts its canyon through the mostly soft, highly erodible, dark-gray, sandy shale and thin sandstone beds comprising the shallow-marine Upper Cretaceous Telegraph Creek Formation and overlying shoreline to offshore deposits of the Upper Cretaceous Eagle.
The Third Edition Of This Book Recognises Two Important Developments That Have Taken Place In Recent Years.(1) Mathematical Modelling Of Alluvial River Processes, And(2) Environmental Aspects Relating To Of These Factors Have Been Duly Considered In This Edition.
With Its Detailed Analysis And Clear Presentation, This Book Would Be Extremely Useful For Practising Civil 5/5(1).
the fundamental characteristics of sediment transport processes in the Colorado River basin were deduced by these early investigations. La Rue () concluded that the largest monthly sediment loads were transported during the peak of the spring snowmelt which had large water discharge but.
Research on road sediment transport and erosion control has been carried out on the traveledway, road sideslopes, and roadside ditch. As a result of this work, erosion control techniques are commonly applied to all components of the road prism and adequate filter strip widths are allowed in attempts to filter runoff before it reaches by: 1.
The Yellowstone River flows miles through Montana to its confluence with the Missouri River at the North Dakota border (Figure ).
The Yellowstone River is the longest free-flowing river remaining in the contiguous United States. Erosion, channel change, and sediment transport in the Big Lost River, Idaho Water-Resources Investigations Report By: R.P. Williams and P.J. Krupkin. Sediment Assessment Method: Considerations, Physical and Biological Parameters, and Decision Making DRAFT July Prepared by: Paul Kusnierz, Andy Welch, and Darrin Kron Water Quality Planning Bureau Montana Department of Environmental Quality E.
Sixth Avenue P.O. Box Helena, MT Study Reach. The Missouri River is the longest river in the U.S., flowing 3, km from the Rocky Mountains in the southwestern part of Montana to the Mississippi River in St. Louis, Missouri (Kammerer ).The Missouri River Basin is approximately one‐sixth of the conterminous U.S.
and drains more than 1, km 2 including parts of 10 states and 2 Canadian provinces (Elliott and Author: Rochelle A. Nustad, Adam J. Benthem, Katherine J. Skalak, Richard R. McDonald, Edward R. Schenk, Joe. The Madison and Missouri Rivers are two of the best known trout-fishing streams in the Rocky Mountains yet lie downstream from Hg-rich geothermal springs in Yellowstone National Park (YNP).Mercury is a worldwide contaminant that is derived from natural and anthropogenic sources and is toxic at very low concentrations (Mason et al.,National Research Council,Fitzgerald and Cited by: Project Overview: Main Topics •Volume and spatial distribution of sediment storage change in the river corridor from / to / •Long-term trends in river-bed elevations at gages •Fluvial sediment loads •Comparative trends in precipitation, streamflow, and stage across the basin •Recent dynamics of water-surface elevations and.
Logging roads are the primary source of sediment in forested watersheds in Montana. However, delivery of eroded sediment to streams depends on the distance that the sediment travels downslope from the road. Existing data on sediment travel distances are primarily for granitic terrain, whereas Montana soils are underlain primarily by metasedimentary and glacial parent material.
Sediment Transport in the Yankee Fork Salmon River The Yankee Fork of the Salmon River is one of the larger watersheds in the upper Salmon River subbasin of central Idaho. Mining activities since the late 19th century, specifically placer mining and associated dredging from tohave left the fluvial system in a highly altered and.Authors: Grace, Johnny M.
Publication Year: Publication Series: Miscellaneous Publication Source: In: pp. in Proceedings of the International Erosion Control Association Confere Februray 25 - March 1,Orlando, Florida, USA Abstract.
In recent years, increased concern and societal pressure have focused on environmental impacts of forest roads on soil erosion and water Cited by: 1.Throughout history, societies have sought to regulate water resources.
Today, over three-fourths of the largest river ecosystems in the northern third of the earth are strongly or moderately fragmented by dams, interbasin diversions, and irrigation (Dynesius and Nilsson, ).