3 edition of Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming found in the catalog.
Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming
M. E Smith
by U.S. Dept. of the Interior, U.S. Geological Survey, U.S. Geological Survey, Earth Science Information Center, Open-File Reports Section [distributor] in Cheyenne, Wyo, Denver, Colo
Written in English
|Statement||by M.E. Smith and M.L. Maderak ; prepared in cooperation with the City of Evanston and Uinta County|
|Series||Water-resources investigations report -- 93-4032|
|Contributions||Maderak, M. L, Geological Survey (U.S.), Evanston (Wyo.), Uinta County (Wyo.)|
|The Physical Object|
|Pagination||v, 61 p. :|
|Number of Pages||61|
Includes data set from Wind/Bighorn River time-of-travel measurements.] WRI Hydrologic analysis of the valley-fill aquifer, North Platte River valley, Goshen County, Wyoming, by . Geomorphic Responses to Changes Hydraulic Geometry 10 Lane Relationship and Brandt Model 11 Grade 13 Bed Mobility 13 Schumm Model 15 Transport Capacity 16 River Evolution Diagram 17 Channel Evolution Models 18 are cut to or near bedrock. However, bedrock control is.
Geomorphic Processes, Controls, and Transition Zones Guadalupe River channel near Kerrville ÉÉÉÉÉÉÉÉÉ 40 Figure Topography of a portion of the Guadalupe River Gorge ÉÉÉ.. transition zones facilitates assessment of trajectories and probabilities of . The Bear River Range, in north-central Utah, contains a variety of geomorphic elements influenced by the geologic setting and events. Controlling factors of the geologic setting include: (1) a syncline (west) and an anticline with a crestal graben (east) within the part of the mountain range studied, and an adjacent graben valley along the west side of the range; and (2) bedrock of Precambrian.
was selected to represent the channel geomorphic conditions for each probable channel type in the Seneca, Belden, and lower Butt Creek reaches. The resulting classifications are shown on Figure at the end of this section. The geomorphic characteristics of each study site . Western EcoSystems Technology, Inc., Bear River Basin Plan Update Environmental and Recreational Water Use Analysis for the Bear River Basin, Wyoming, Sep, (2, kb) Beaver Creek Bearlodge Ltd, Inc., Beaver Creek Dam and Reservoir Level I, Executive Summary, Oct, ( kb).
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Get this from a library. Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming. [M E Smith; M L Maderak; Evanston (Wyo.). Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming [M.
Smith] on *FREE* shipping on qualifying offers. This volume is produced from digital images created through the University of Michigan University Library's large-scale digitization efforts. The Library seeks to preserve the intellectual content of items in a manner that facilitates and.
Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming (Water-resources investigations report) [M. E Smith] on *FREE* shipping on qualifying offers. GEOMORPHIC AND HYDRAULIC ASSESSMENT OF THE BEAR RIVER IN AND NEAR EVANSTON, WYOMING By M.E.
SMITH anc/M.L. MADERAK_____ U.S. GEOLOGICAL SURVEY Water-Resources Investigations Report Prepared in cooperation with the CITY OF EVANSTON and UINTA COUNTY Cheyenne, Wyoming Cited by: 3. Geomorphic and hydraulic characteristics of the Bear River in and near Evanston, Wyoming, were assessed to assist planners in stabilizing the river channel.
Present-day channel instability is the result of both human-made and natural factors. The primary factor is channelization of the river in Evanston, where several meander loops were cut off artificially during early development of the city.
Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming / By M. Smith, M. Maderak, Geological Survey (U.S.), Uinta County (Wyo.) and Evanston (Wyo.) Abstract.
Buy Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming (SuDoc I /) by M. Smith (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : M. Smith. Buy Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming (Water-resources investigations report) by M.
E Smith (ISBN:) from Amazon's Book Store. Everyday low prices and free delivery on eligible : M. E Smith. Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Kemmerer Field Office Planning Area (planning area) is located in southwestern Wyoming and includes approximately million acres of land in most of Lincoln and Uinta counties and part of Sweetwater County.
Evanston urban system study. Geomorphic and hydraulic assessment of the Bear River in and. near Evanston, Wyoming. U.S. Geological Survey Water-Resources Investigations Report Subcommittee on Rocky Mountain Greater Sandhill Cranes. Management plan of the Pacific and Central.
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Smith and M.L. Maderak ; prepared in cooperation with the City of Evanston and Uinta County. Bear River Commission W.
S., Suite Bountiful, Utah () Created and maintained by StoneFly Technology, Saint George, Utah. Funding provided by: Bear River Commission, Utah Division of Water Rights, Woodruff Narrows Reservoir Company, Wyoming State Engineer's Office, & USBR Provo Area Office.Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming: U.S.
Geological Survey Water-Resources Investigations Report61 p. LLC., Evanston/Bear River regional pipeline level II study: prepared for the WWDO, various pagination.
Geomorphic and sedimentologic characteristics of alluvial reaches in the Black Canyon of the Gunnison National Monument, Colorado / (Denver, Colo.: U.S.
Dept. of the Interior, U.S. Geological Survey: Information Services [distributor], ), by John G. Elliott, Lauren A. Hammack, and United States National Park Service (page images at. such, numerous geomorphic classiﬁcations have been de-veloped for landscapes (Davis, ), hillslopes (Varnes, ), and rivers (Section ).
The form–process paradigm is a potentially powerful tool for conducting quantitative geo-morphic investigations. However, many river classiﬁcations are. Cancellation of Geomorphic and Ecological Fundamentals for River and Stream Restoration for due to COVID considerations With great regret, we cancel the shortcourse at Sagehen Creek Field Station, due to the many complications arising from the COVID pandemic and the challenges in avoiding problems in holding the shortcourse at the station.
River assessment tools are available to the public on the state Agency for Natural Resources, and are based on the fact that streams and rivers are adjusting to channel, flood plain, or watershed changes imposed in years past by human activity. As part of the Vermont Geomorphic Assessment phase 1 protocol, river corridors are defined.
The geomorphic units listed below are common examples that you may encounter in the field. The list is intended to help with consistency of geomorphic unit description but is in no way exhaustive. The River Styles Framework is an open-ended approach, with emphasis. Dinwiddie, G.A.,Hydraulic testing and sampling of water well number 2, Project Wagon Wheel, Sublette County, Wyoming: U.S.
Geological Survey open-file report, 32 p. and Maderak, M.L.,Geomorphic and hydraulic assessment of the Bear River in and near Evanston, Wyoming: U.S. Geological Survey Water-Resources Investigations Report. Bear River Materials produces a wide variety of building materials for any size construction project.
To establish credit with Bear River Materials please visit our Credit Applications page. For Sales or Customer Service, please call For more details visit the locations page.finds that the annual runoff for the Bear River watershed for water years – has averagedacre feet/year.
Flow monitoring stations listed by the California Data Exchange Center () include the South Canal from Bear River, Bear River at Pleasant Grove Road, Bear River at Rollins, Bear River near Wheatland.along the Bear River upstream of Bear Lake and the implications for the timing of sediment transport by Bear River.
New mapping of moraines near the crest of the Bear River Range (west of Bear Lake; Fig. 2) improves the understanding of the former extent of glaciers and their potential inﬂ uence on the lake.