Mfre Main Stem Salmon River Itinerary
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Riggins & Salmon River Canyon
RRiiggggiinnss && SSaallmmoonn RRiivveerr CCaannyyoonn EEccoonnoommiicc DDeevveellooppmmeenntt SSttrraatteeggyy (FINAL DRAFT) Prepared for the City of Riggins February 2006 by James A. Birdsall & Associates The Hingston Roach Group, Inc. Bootstrap Solutions FINAL DRAFT [Inside cover.] RIGGINS AREA ECONOMIC DEVELOPMENT STRATEGY FEBRUARY 2006 FINAL DRAFT CONTENTS 1. Introduction......................................................................................1 Planning Process and Project Phases ..............................................................1 Riggins History and Assets. ..............................................................................2 2. Socio-Economic Trends....................................................................4 Population. ..........................................................................................................4 Age Composition................................................................................................5 Education & Enrollment...................................................................................5 Industry Trends..................................................................................................6 Employment, Wages & Income.......................................................................7 Business Inventory.............................................................................................9 Retail Trends.......................................................................................................9 Tourism -
Instream Flow Characterization of Upper Salmon River Basin Streams, Central Idaho, 2004
Prepared in cooperation with the Bureau of Reclamation Instream Flow Characterization of Upper Salmon River Basin Streams, Central Idaho, 2004 Ellis River Challis Fork Salmon Yankee Squaw T h o m Valley p s o n Creek Creek Creek Creek Elk Salmon River Stanley Iron Creek Salmon River Redfish Lake Obsidian July Salmon of Creek Fourth Champion Creek River Alturas Fork Lake Pole Creek Creek East Creek Beaver Smiley Scientific Investigations Report 2005–5212 U.S. Department of the Interior U.S. Geological Survey Instream Flow Characterization of Upper Salmon River Basin Streams, Central Idaho, 2004 By Terry R. Maret, Jon E. Hortness, and Douglas S. Ott Prepared in cooperation with the Bureau of Reclamation Scientific Investigations Report 2005-5212 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior Gale A. Norton, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia: 2005 For sale by U.S. Geological Survey, Information Services Box 25286, Denver Federal Center Denver, CO 80225 For more information about the USGS and its products: Telephone: 1-888-ASK-USGS World Wide Web: http://www.usgs.gov/ Any use of trade, product, or firm names in this publication is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted materials contained within this report. Suggested citation: Maret, T.R., Hortness, J.E., and Ott, D.S., 2005, Instream flow characterization of upper Salmon River Basin streams, Central Idaho, 2004: U.S. -
Lower Wisconsin River Main Stem
LOWER WISCONSIN RIVER MAIN STEM The Wisconsin River begins at Lac Vieux Desert, a lake in Vilas County that lies on the border of Wisconsin and the Lower Wisconsin River Upper Pennisula in Michigan. The river is approximately At A Glance 430 miles long and collects water from 12,280 square miles. As a result of glaciation across the state, the river Drainage Area: 4,940 sq. miles traverses a variety of different geologic and topographic Total Stream Miles: 165 miles settings. The section of the river known as the Lower Wisconsin River crosses over several of these different Major Public Land: geologic settings. From the Castle Rock Flowage, the river ♦ Units of the Lower Wisconsin flows through the flat Central Sand Plain that is thought to State Riverway be a legacy of Glacial Lake Wisconsin. Downstream from ♦ Tower Hill, Rocky Arbor, and Wisconsin Dells, the river flows through glacial drift until Wyalusing State Parks it enters the Driftless Area and eventually flows into the ♦ Wildlife areas and other Mississippi River (Map 1, Chapter Three ). recreation areas adjacent to river Overall, the Lower Wisconsin River portion of the Concerns and Issues: Wisconsin River extends approximately 165 miles from the ♦ Nonpoint source pollution Castle Rock Flowage dam downstream to its confluence ♦ Impoundments with the Mississippi River near Prairie du Chien. There are ♦ Atrazine two major hydropower dams operate on the Lower ♦ Fish consumption advisories Wisconsin, one at Wisconsin Dells and one at Prairie Du for PCB’s and mercury Sac. The Wisconsin Dells dam creates Kilbourn Flowage. ♦ Badger Army Ammunition The dam at Prairie Du Sac creates Lake Wisconsin. -
2015 Idaho Wolf Monitoring Progress Report
2015 IDAHO WOLF MONITORING PROGRESS REPORT Photo by IDFG Prepared By: Jason Husseman, Idaho Department of Fish and Game Jennifer Struthers, Idaho Department of Fish and Game Edited By: Jim Hayden, Idaho Department of Fish and Game March 2016 EXECUTIVE SUMMARY At the end of 2015, Idaho’s wolf population remained well-distributed and well above population minimums required under Idaho’s 2002 Wolf Conservation and Management Plan. Wolves range in Idaho from the Canadian border south to the Snake River Plain, and from the Washington and Oregon borders east to the Montana and Wyoming borders. Dispersing wolves are reported in previously unoccupied areas. The year-end population for documented packs, other documented groups not qualifying as packs and lone wolves was estimated at 786 wolves. Biologists documented 108 packs within the state at the end of 2015. In addition, there were 20 documented border packs counted by Montana, Wyoming, and Washington that had established territories overlapping the Idaho state boundary. Additional packs are suspected but not included due to lack of documentation. Mean pack size was 6.4 wolves, nearly identical to the 2014 average of 6.5. Reproduction (production of at least 1 pup) was documented in 69 packs, representing the minimum number of reproductive packs extant in the state. Determination of breeding pair status was made for 53 packs at year’s end. Of these, 33 packs (62%) met breeding pair criteria, and 20 packs did not. No determination of breeding pair status was made for the remaining 55 packs. Mortalities of 358 wolves were documented in Idaho in 2015, and remained essentially unchanged from 2014 (n = 360). -
A Geological Reconnaissance Between
Pamphlet No. 74 November 1945 STATE OF IDAHO Charles C. Gossett,· Governor IDAHO BUREAU OF MINES AND GEOLOGY , A. w. Fahrenwald, Director . A· GEOLOGICAL RECONNAISSANCE BETWEEN·· THE slm· AID SALMON RIVERS NOBTI. OF BIGGIIS, mAIO By Warren R. Wagner University of Idaho Moscow, Idaho TABLE OF CONTENTS Page Introduction .................................................................................... ~................................................................................................................. 1 ~~S:p~~ .. ~.:~~~.. ::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::::~::::::::::::::::::::::::::::::::::::::::::::::::::::::::::: ~ Acknowledgement ............................... ,.. ~ ........ ~ ..................................................•.. ~ .......... :.................................................................... 1 Geography and· physiography ..................................................................................................................................................................... l' Location ................................................................................................................................................................................................. 1 Surface features ........... :..................................................................................................................................................................... 1 Climate ................................................................................................................................................................................................ -
Watershed Technical Analysis
Trout Creek Watershed Stormwater Management Plan SECTION III: WATERSHED TECHNICAL ANALYSIS A. Watershed Modeling An initial step this study of the Trout Creek watershed was the selection of a stormwater simulation model to be used in the analysis. To provide a reasonable estimate of existing flows within the watershed to serve as a baseline for the study of stormwater management and to effectively evaluate the hydrologic response of the watershed to various changes in stormwater management it was necessary to select a model which: • Modeled design storms of various durations and frequencies to produce routed hydrographs which could be combined • Was adaptable to the size of subwatersheds in this study • Could evaluate specific physical characteristics of the rainfall-runoff process • Did not require an excessive amount of input data yet yielded reliable results The model selected for use in this study was the U. S. Army Corps of Engineers, Hydrologic Engineering Center, Hydrologic Modeling System (HEC-HMS) for the following reasons: • It had been developed at the Hydrologic Engineering Center specifically for the analysis of the timing of surface flow contributions to peak rates at various locations in a watershed • Although originally developed as an urban runoff simulation model, data requirements make it easily adaptable to a rural situation • Input parameters provide a flexible calibration process • It has the ability to analyze reservoir or detention basin routing effects • It is accepted by the Pennsylvania Department of Environmental Protection Although other models, such as TR-20, may provide essentially the same results as the HEC-HMS, HMS’s ability to compare subwatershed contributions in a peak flow presentation table make it specifically attractive for this study. -
Waterbody Classifications, Streams Based on Waterbody Classifications
Waterbody Classifications, Streams Based on Waterbody Classifications Waterbody Type Segment ID Waterbody Index Number (WIN) Streams 0202-0047 Pa-63-30 Streams 0202-0048 Pa-63-33 Streams 0801-0419 Ont 19- 94- 1-P922- Streams 0201-0034 Pa-53-21 Streams 0801-0422 Ont 19- 98 Streams 0801-0423 Ont 19- 99 Streams 0801-0424 Ont 19-103 Streams 0801-0429 Ont 19-104- 3 Streams 0801-0442 Ont 19-105 thru 112 Streams 0801-0445 Ont 19-114 Streams 0801-0447 Ont 19-119 Streams 0801-0452 Ont 19-P1007- Streams 1001-0017 C- 86 Streams 1001-0018 C- 5 thru 13 Streams 1001-0019 C- 14 Streams 1001-0022 C- 57 thru 95 (selected) Streams 1001-0023 C- 73 Streams 1001-0024 C- 80 Streams 1001-0025 C- 86-3 Streams 1001-0026 C- 86-5 Page 1 of 464 09/28/2021 Waterbody Classifications, Streams Based on Waterbody Classifications Name Description Clear Creek and tribs entire stream and tribs Mud Creek and tribs entire stream and tribs Tribs to Long Lake total length of all tribs to lake Little Valley Creek, Upper, and tribs stream and tribs, above Elkdale Kents Creek and tribs entire stream and tribs Crystal Creek, Upper, and tribs stream and tribs, above Forestport Alder Creek and tribs entire stream and tribs Bear Creek and tribs entire stream and tribs Minor Tribs to Kayuta Lake total length of select tribs to the lake Little Black Creek, Upper, and tribs stream and tribs, above Wheelertown Twin Lakes Stream and tribs entire stream and tribs Tribs to North Lake total length of all tribs to lake Mill Brook and minor tribs entire stream and selected tribs Riley Brook -
Channel Changes and Flood Frequency on the Upper Main Stem of the Nooksack River, Whatcom County, Washington
Western Washington University Western CEDAR WWU Graduate School Collection WWU Graduate and Undergraduate Scholarship Winter 1993 Channel Changes and Flood Frequency on the Upper Main Stem of the Nooksack River, Whatcom County, Washington Roger G. Bertschi Western Washington University, [email protected] Follow this and additional works at: https://cedar.wwu.edu/wwuet Part of the Geology Commons Recommended Citation Bertschi, Roger G., "Channel Changes and Flood Frequency on the Upper Main Stem of the Nooksack River, Whatcom County, Washington" (1993). WWU Graduate School Collection. 717. https://cedar.wwu.edu/wwuet/717 This Masters Thesis is brought to you for free and open access by the WWU Graduate and Undergraduate Scholarship at Western CEDAR. It has been accepted for inclusion in WWU Graduate School Collection by an authorized administrator of Western CEDAR. For more information, please contact [email protected]. CHANNEL CHANGES AND FLOOD FREQUENCY ON THE UPPER MAIN STEM OF THE NOOKSACK RIVER, WHATCOM COUNTY, WASHINGTON by Roger G. Bertschi Accepted in Partial Completion of the Requirements for the Degree Master of Science Advisory Committee MASTER'S THESIS In presenting this thesis in partial fulfillment of the requirements for a master's degree at Western Washington University, I agree that the Library shall make its copies freely available for inspection. I further agree that extensive copying of this thesis is allowable only for scholarly purposes. It is understood, however, that any copying or publication of this thesis for commercial purposes, or for financial gain, shall not be allowed without mv permission. Signature Date MASTER’S THESIS In presenting this thesis in partial fulfillment of the requirements for a master’s degree at Western Washington University, I grant to Western Washington University the non-exclusive royalty-free right to archive, reproduce, distribute, and display the thesis in any and all forms, including electronic format, via any digital library mechanisms maintained by WWU. -
The Epic Idaho Roadtrip
THE EPIC IDAHO ROADTRIP As the 14th largest state in the country, it will take more than a long weekend to explore Idaho from top to bottom. The Epic Idaho Road Trip was created as a way to highlight the beautiful scenic byways, vast landscapes, and all the fun adventures, food, and history that Idaho has to offer. This 10-day route includes time to stop and enjoy attractions and activities each day before heading out to your next destination. Total mileage and estimated drive time are notated on each map for planning purposes. The Epic Idaho Road Trip can be easily tailored to fit your specific travel style and interests. Stay an extra day or two in a place you really love. Tackle more adventures from the “Activities to Explore” listing in each section. Or just follow the scenic byways and let the beauty of Idaho speak for itself. Whatever you choose, Idaho is sure to surprise and delight with every curve of the road. visitidaho.org | P29 CANADA Bonners Ferry Sandpoint Coeur d’Alene White Pine Wallace Scenic Byway WA MT Moscow Lewiston Northwest Passage Scenic Byway Grangeville Salmon New McCall Meadows Payette River Scenic Byway Sacajawea Scenic Byway Ponderosa Pine Scenic Byway Rexburg Peaks to Craters WY Scenic Byway Stanley Salmon River Scenic Byway Victor Banks Wildlife Canyon Scenic Byway Idaho Sun Valley Falls Boise OR Sawtooth Scenic Byway Pocatello Twin Falls NV UT visitidaho.org | P30 EPIC THE EPIC IDAHO ROAD TRIP Total Drive Time: 35 Hours 20 Minutes Total Mileage: 1,763 Highway 75 Best Time to Travel: June-September Good For: We go big in Idaho: North America’s + Young Free Spirits deepest gorge, millions of acres of + Adventure Seekers wildlands, jagged peaks, world-class trout streams, and hundreds of alpine lakes. -
Memorandum 6E. Review of Main Stem Restoration Project; Golden
Memorandum To: Bassett Creek Watershed Management Commission From: Barr Engineering Co. Subject: Item 6E – Review of Main Stem Restoration Project; Golden Valley Rd. to Irving Ave. N. – 50% Development Plans (CIP 2012 CR) BCWMC September 19, 2013 Meeting Agenda Date: September 12, 2013 Project: 23270051 2013 626 6E. Review of Main Stem Restoration Project; Golden Valley Rd. to Irving Ave. N. – 50% Development Plans (CIP 2012 CR) Summary Proposed Work: Main Stem of Bassett Creek Restoration Project (CIP 2012 CR) Basis for Commission Review: 50% plan review Change in Impervious Surface: N.A. Recommendation: Conditional Approval The Minneapolis Park and Recreation Board (MPRB) Main Stem of Bassett Creek restoration project (CIP 2012 CR) is being funded by the BCWMC’s ad valorem levy (via Hennepin County) and by a Minnesota Board of Water and Soil Resources Clean Water Fund Grant. The MPRB provided the 50% design plans to the BCWMC for review and comment, as set forth in the BCWMC CIP project flow chart developed by the TAC. Feasibility Study Summary The Feasibility Report for the 2012 Bassett Creek Main Stem Restoration Project – Golden Valley Road to Irving Avenue North (Barr, June 2011) was completed by the BCWMC to develop approaches to stabilize eroding stream banks along the Main Stem of Bassett Creek. Between Golden Valley Road and Irving Avenue North, Bassett Creek flows through Golden Valley and Minneapolis, and is nearly entirely contained within MPRB-owned land in Theodore Wirth Regional Park, Theodore Wirth Golf Course, and city parks. The goal of the project is to reduce the phosphorus loading to the Main Stem of Bassett Creek by 60 pounds per year and to consolidate sediments in an in-stream pond upstream of Highway 55. -
Surface Water Types and Sediment Distribution Patterns at the Confluence of Mega Rivers: the Solimões-Amazon and Negro Rivers Junction
Surface water types and sediment distribution patterns at the confluence of mega rivers: the Solimões-Amazon and Negro rivers junction Edward Park1, Edgardo M. Latrubesse1 1University of Texas at Austin, Department of Geography and the Environment, Austin, TX, USA Correspondence to: Edward Park, Tel +1-512-230-4603 Fax +1-512-471-5049 University of Texas at Austin, SAC 4.178, 2201 Speedway, Austin, TX 78712, USA Email address: [email protected] This article has been accepted for publication and undergone full peer review but has not been through the copyediting, typesetting, pagination and proofreading process which may lead to differences between this version and the Version of Record. Please cite this article as an ‘Accepted Article’, doi: 10.1002/2014WR016757 This article is protected by copyright. All rights reserved. Abstract Large river channel confluences are recognized as critical fluvial features because both intensive and extensive hydrophysical and geoecological processes take place at this interface. However, identifications of suspended sediment routing patterns through channel junctions and the roles of tributaries on downstream sediment transport in large rivers are still poorly explored. In this paper, we propose a remote sensing-based approach to characterize the spatiotemporal patterns of the post-confluence suspended sediment transport by mapping the surface water distribution in the ultimate example of large river confluence on Earth where distinct water types meet: The Solimões-Amazon (white water) and Negro (black water) rivers. The surface water types distribution was modeled for three different years: average hydrological condition (2007) and two years when extreme events occurred (drought-2005 and flood-2009). -
Middle Fork Salmon River 5 OR 6 DAY EXPEDITION Middle Fork Salmon River 5 OR 6 DAY EXPEDITION
Middle Fork Salmon River 5 OR 6 DAY EXPEDITION Middle Fork Salmon River 5 OR 6 DAY EXPEDITION What to Expect ☞ Day-by-Day Itinerary ☞ Typical Day ☞ Learn About the Rafts ☞ Camping on the River ☞ Physical Requirements Get Ready! ☞ Packing List ☞ Packing Tips ☞ Pre-Trip Travel Information ☞ Payment & Cancellation Western River Expeditions HOURS: Mon-Fri 7:00am—6:00pm MST TOLL-FREE: 800-453-7450 2 7258 Racquet Club Drive EMAIL: [email protected] LOCAL: 801-942-6669 Salt Lake City, Utah 84121 ONLINE: www.westernriver.com FAX: 801–942–8514 MIDDLE FORK SALMON RIVER 5 OR 6 DAY EXPEDITION Middle Fork Salmon River 5 OR 6 DAY EXPEDITION Among river runners, the Middle Fork of the Salmon River is a legend. One-hundred miles of pure, clear, free-flowing river drop 3000 feet through the remote and spectacular River of No Return Wilderness, the largest roadless Wilderness in the lower 48 states. Natural and untamed, the Middle Fork of the Salmon River has shaped its course through a land so rugged that any attempts at settlement have failed. Little remains of man’s brief presence other than prehistoric cave paintings and dilapidated log cabins dotting this land in Idaho. A Middle Fork Salmon River rafting trip draws visitors from around the globe to experience over 100 Idaho whitewater rafting rapids, fish clear alpine waters, relax in natural hot springs, hike to magnificent waterfalls, and camp in mountain meadows. Day-by-Day Itinerary DAY ONE » In the early season (June - July 22), a two-hour bus ride from Stanley, ID to Boundary Creek begins your trip into the Idaho wilderness.