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Columbia River Treaty: Recommendations December 2013
L O CA L GOVERNMEN TS’ COMMI TTEE Columbia River Treaty: Recommendations December 2013 The BC Columbia River Treaty Local Governments’ Committee (the Committee) has prepared these Recommendations in response to the Columbia River Treaty-related interests and issues raised by Columbia River Basin residents in Canada. These Recommendations are based on currently-available information. They have been submitted to the provincial and federal governments for incorporation into current decisions regarding the future of the Columbia River Treaty (CRT). The Committee plans to monitor the BC, Canadian and U.S. CRT-related processes and be directly involved when appropriate. As new information becomes available, the Committee will review this information, seek input from Basin residents, and submit further recommendations to the provincial and federal governments, if needed. The CRT Local Governments’ Committee will post its recommendations and other documents at www.akblg.ca/content/columbia-river-treaty. For more information contact the Committee Chair, Deb Kozak ([email protected] 250 352-9383) or the Executive Director, Cindy Pearce ([email protected] 250 837-3966). Background Beginning in 2024, either the U.S. or Canada can The Columbia River Treaty (Treaty) was ratified terminate substantial portions of the Treaty, by Canada and the United States (the U.S.) in with at least 10 years’ prior notice. Canada—via 1964, resulting in the construction of three the BC Provincial Government—and the U.S. are dams in Canada—Mica Dam north of both conducting reviews to consider whether to Revelstoke; Hugh Keenleyside Dam near continue, amend or terminate the Treaty. Castlegar; and Duncan Dam north of Kaslo—and Local governments within the Basin have Libby Dam near Libby, Montana. -
Kootenai River Resident Fish Mitigation: White Sturgeon, Burbot, Native Salmonid Monitoring and Evaluation
KOOTENAI RIVER RESIDENT FISH MITIGATION: WHITE STURGEON, BURBOT, NATIVE SALMONID MONITORING AND EVALUATION Annual Progress Report May 1, 2016 — April 31, 2017 BPA Project # 1988-065-00 Report covers work performed under BPA contract # 68393 IDFG Report Number 08-09 April 2018 This report was funded by the Bonneville Power Administration (BPA), U.S. Department of Energy, as part of BPA's program to protect, mitigate, and enhance fish and wildlife affected by the development and operation of hydroelectric facilities on the Columbia River and its tributaries. The views in this report are the author's and do not necessarily represent the views of BPA. This report should be cited as follows: Ross et al. 2018. Report for 05/01/2016 – 04/30/2017. TABLE OF CONTENTS Page CHAPTER 1: KOOTENAI STURGEON MONITORING AND EVALUATION ............................... 1 ABSTRACT ................................................................................................................................. 1 INTRODUCTION ........................................................................................................................2 OBJECTIVE ................................................................................................................................3 STUDY SITE ...............................................................................................................................3 METHODS ..................................................................................................................................3 Water -
Ecosystem Classification and Interpretation of the C.3 Sub-Boreal Spruce Zone, Prince Rupert Forest Region, British Columbia
Ecosystem Classification and Interpretation of the c.3 Sub-Boreal Spruce Zone, Prince Rupert Forest Region, British Columbia by J. Pojar', R. Trowbridge', and D. Coates2 'Ministry of Forests 2Ministry of Forests Research Section Silviculture Section Prince Rupert Forest Region Prince Rupert Forest Region Bag 5000 Bag 5000 Smithers. B.C. Smithers, B.C. VOJ 2N0 VOJ 2N0 Province of British Columbia Ministry of Forests ACKNOWLEDGEMENTS Numerous individualsassisted in the various phases ofthis report. D.J. Wilford managed theprogram in its first few years. K. Awmack, A. Banner, M. Blouw, W. Chapman, A. Deas, S. Haeussler, D. Holmes, R. Laird, A. Macadam, K. McKeown, M. O'Neill, L. Ricciotti, 6. Robinson, J. Schwab, 0.Wilford, and D. Yolehelped carry out field work. S. Lindeburghand B.M. Geislercontributed tothe Interpretations sections of theguide. J. van Barneveld and 0. Meidingerreviewed the manuscript and provided many usefulsuggestions. G. Bishop, P. Frank, P. Nystedt,and P. Sowden did most ofthe illustrations. F. Boasand J. Godfrey identified some ofthe bryophytes. Final editing and preparationof the report was by W. Taylor and K. McKeown. M. Romeo, and C. Huismanand J. Taekema did the typing andword processing, respectively. TABLE OF CONTENTS Page 1.0 INTRODUCTION ......................................................... 1 2.0 OBJECTIVES ........................................................... 4 3.0 PRINCIPLES AND PHILOSOPHY ............................................ 5 3.1 Ecosystem ...................................................... -
Ethnohistory of the Kootenai Indians
University of Montana ScholarWorks at University of Montana Graduate Student Theses, Dissertations, & Professional Papers Graduate School 1983 Ethnohistory of the Kootenai Indians Cynthia J. Manning The University of Montana Follow this and additional works at: https://scholarworks.umt.edu/etd Let us know how access to this document benefits ou.y Recommended Citation Manning, Cynthia J., "Ethnohistory of the Kootenai Indians" (1983). Graduate Student Theses, Dissertations, & Professional Papers. 5855. https://scholarworks.umt.edu/etd/5855 This Thesis is brought to you for free and open access by the Graduate School at ScholarWorks at University of Montana. It has been accepted for inclusion in Graduate Student Theses, Dissertations, & Professional Papers by an authorized administrator of ScholarWorks at University of Montana. For more information, please contact [email protected]. COPYRIGHT ACT OF 1976 Th is is an unpublished m a n u s c r ip t in w h ic h c o p y r ig h t su b s i s t s . Any further r e p r in t in g of it s c o n ten ts must be a ppro ved BY THE AUTHOR. MANSFIELD L ib r a r y Un iv e r s it y of Montana D a te : 1 9 8 3 AN ETHNOHISTORY OF THE KOOTENAI INDIANS By Cynthia J. Manning B.A., University of Pittsburgh, 1978 Presented in partial fu lfillm en t of the requirements for the degree of Master of Arts UNIVERSITY OF MONTANA 1983 Approved by: Chair, Board of Examiners Fan, Graduate Sch __________^ ^ c Z 3 ^ ^ 3 Date UMI Number: EP36656 All rights reserved INFORMATION TO ALL USERS The quality of this reproduction is dependent upon the quality of the copy submitted. -
(1987): "Tectonomagmatic Evolution of Cenozoic Extension in the North American Cordillera"
Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Geological Society, London, Special Publications Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera Brian P. Wernicke, Philip C. England, Leslie J. Sonder and Robert L. Christiansen Geological Society, London, Special Publications 1987, v.28; p203-221. doi: 10.1144/GSL.SP.1987.028.01.15 Email alerting click here to receive free e-mail alerts when service new articles cite this article Permission click here to seek permission to re-use all or request part of this article Subscribe click here to subscribe to Geological Society, London, Special Publications or the Lyell Collection Notes © The Geological Society of London 2013 Downloaded from http://sp.lyellcollection.org/ by Frances J Cooper on January 21, 2013 Tectonomagmatic evolution of Cenozoic extension in the North American Cordillera B.P. Wernicke, R.L. Christiansen, P.C. England & L.J. Sonder SUMMARY: The spatial and temporal distributions of Cenozoic extension and magmatism in the Cordillera suggest that the onset of major crustal extension at a particular latitude was confined to a relatively narrow belt (< 100 km, pre-extension) and followed the onset of intermediate and silicic magmatism by no more than a few million years. Extension began in early Eocene time in southern British Columbia, northern Washington, Idaho and Montana. Farther S, extension began at about the Eocene- Oligocene boundary in the Great Basin and slightly later in the Mojave-Sonora Desert region. The intervening area, at the latitude of Las Vegas, remained quiescent until mid- Miocene time. Compositional and isotopic characteristics of most pre-Miocene magmas are consistent with their containing major components of melted continental crust. -
White Paper on COLUMBIA RIVER POST-2024 FLOOD RISK MANAGEMENT PROCEDURE
White Paper on COLUMBIA RIVER POST-2024 FLOOD RISK MANAGEMENT PROCEDURE U.S. Army Corps of Engineers Northwestern Division September 2011 This page intentionally left blank PREFACE The Columbia River, the fourth largest river on the continent as measured by average annual flow, provides more hydropower than any other river in North America. While its headwaters originate in British Columbia, only about 15 percent of the 259,500 square miles of the river’s basin is located in Canada. Yet the Canadian water accounts for about 38 percent of the average annual flow volume, and up to 50 percent of the peak flood waters, that flow on the lower Columbia River between Oregon and Washington. In the 1940s, officials from the United States and Canada began a long process to seek a collaborative solution to reduce the risks of flooding caused by the Columbia River and to meet the postwar demand for energy. That effort resulted in the implementation of the Columbia River Treaty in 1964. This agreement between Canada and the United States called for the cooperative development of water resource regulation in the upper Columbia River Basin. The Columbia River Treaty has provided significant flood control (also termed flood risk management) and hydropower generation benefiting both countries. The Treaty, and subsequent Protocol, include provisions that both expire on September 16, 2024, 60 years after the Treaty’s ratification, and continue throughout the life of the associated facilities whether the Treaty continues or is terminated by either country. This white paper focuses on the flood risk management changes that will occur on that milestone date and satisfies the following purposes: 1. -
ARTICLES Late Cretaceous Through Cenozoic Strike-Slip Tectonics of Southwestern Alaska
" .--- ~, , - /.. ./ . - n L~O J t-7.7/ ~ / (C/ / ' '0! L/ 'L ' x/(,' i J(ff /t1cz/j7 ARTICLES Late Cretaceous through Cenozoic Strike-Slip Tectonics of Southwestern Alaska l and William Marti 1. Miller, Dwight C. Bradley, Thomas K. Bundtzen McClellcmd2 u.s. Geological Survey, 4200 University Drive, Anchorage, Alaska 99508, u.S. (e-mail: mlmillerCtYusgs. gov) ABSTRACT New geologic mapping and geochronology show that margin-parallel strike-slip faults on the western limb of the southern Alaska orocline have experienced multiple episodes of dextral motion since -100 Ma. These faults are on the upper plate of a subduction zone -350-450 km inboard of the paleotrench. In southwestern Alaska, dextral displacement is 134 km on the Denali fault, at least 88-94 km on the Iditarod-Nixon Fork fault, and perhaps tens of kilometers on the Dishna River fault. The strike-slip regime coincided with Late Cretaceous sedimentation and then folding in the Kuskokwim basin, and with episodes of magmatism and mineralization at ~ 70, -60, and -30 Ma. No single driving mechanism can explain all of the -95 million-year history of strike-slip faulting. Since -40 Ma the observed dextral sense of strike slip has run contrary to the sense of subduction obliquity. This may be explained by northward motion of the Pacific Plate driving continental margin slivers into and/or around the oroclinal bend. From 44 to 66 Ma, oroclinal rotation, perhaps involving large-scale flexural slip, may have been accompanied by westward escape of crustal blocks along strike-slip faults. However, reconstructions of this period involve unproven assumptions about the identity of the subducting plate, the position of subducting ridges, and the exact timing of oroclinal bending, thus obscuring the driving mechanisms of strike slip. -
Columbia Lake Quick Fact Sheet
COLUMBIA LAKE QUICK REFERENCE SHEET JUST A FEW AMAZING THINGS ABOUT OUR AMAZING LAKE! . Maximum length – 13.5 km (8.4 mi) . Maximum width – 2 km (1.2 mi) . Typical depth – 15 ft . Average July water temperature – 18 C – making it the largest warm water lake in East Kootenay . Surface Elevation – 808m (2,650 ft) .Area – 6,815 acres (2,758 hectares) . Freezing – last year, it was observed the lake froze on December 7, 2016 and thawed on March 29, 2017. Columbia Lake is fed by several small tributaries. East side tributaries include Warspite and Lansdown Creeks. West Side tributiaries include Dutch, Hardie, Marion and Sun Creeks. Columbia Lake also gets a considerable amount of water at the south end where water from the Kootenay river enters the lake as groundwater. The water balance of Columbia Lake is still not fully understood. The Columbia Lake Stewardship Society continues to do research in this area. Columbia Lake got its name from the Columbia River. The river was so named by American sea captain Robert Gray who navigated his privately owned ship The Columbia Rediviva through its waters in May 1792 trading fur pelts. Columbia Lake is the source of the mighty Columbia River, the largest river in the Pacific Northwest of North America. The Columbia River flows north from the lake while the neighbouring Kootenay flows south. For approximately 100 km (60 mi) the Columbia River and the Kootenay River run parallel and when they reach Canal Flats, the two rivers are less than 2 km (1.2 mi) apart. Historically the Baillie- Grohman Canal connected the two bodies of water to facilitate the navigation of steamboats (although only three trips were ever made through it). -
Ch1 Overview
RESERVATION OF RIGHTS A number of governments and agencies participated in the development of this Kootenai Subbasin Plan, Part I (Assessment Volume), Part II (Inventory Volume), and Part III (Management Plan Volume), its appendices, and electronically linked references and information (hereafter Plan). The primary purpose of the Plan is to help direct Northwest Power and Conservation Council funding of projects that respond to impacts from the development and operation of the Columbia River hydropower system. Nothing in this Plan, or the participation in its development, is intended to, and shall not be interpreted to, compromise, influence, or preclude any government or agency from carrying out any past, present, or future duty or responsibility which it bears or may bear under any authority. Nothing in this Plan or the participation in its development constitutes a waiver or release of any rights, including the right to election of other remedies, or is intended to compromise, influence, or preclude any government or agency from developing and prosecuting any damage claim for those natural resource impacts identified in the Plan which are not directly and exclusively resulting from, or related to, the development and operation of the Columbia River hydropower system. Nothing in this Plan or the participation in its development is intended to, and shall not be interpreted to, waive any rights of enforcement of regulatory, adjudicatory, or police powers against potentially responsible parties for compliance with applicable laws and regulations pertaining to natural resource damages throughout the Kootenai Subbasin whether or not specifically identified in this Plan. © 2004 Kootenai Tribe of Idaho (KTOI) and Montana Fish, Wildlife & Parks (MFWP) Citation: Kootenai Tribe of Idaho and Montana Fish, Wildlife & Parks. -
SR51 Follow-Up Report on Wildlife and Cattle Grazing in the East
Follow-up Report on Wildlife and Cattle Grazing in the East Kootenay FPB/SR/51 July 2015 Table of Contents Introduction ................................................................................................................................. 1 Approach ...................................................................................................................................... 2 Objective ....................................................................................................................................................... 2 Methods and Scope ..................................................................................................................................... 2 Findings and Discussion ............................................................................................................ 2 Has authorized grazing been reduced since 2008? ..................................................................................... 2 Are the objectives of the elk management plan being met? ......................................................................... 4 Are the net effects of the ecosystem restoration activities meeting the desired target condition? ............... 6 Conclusion ................................................................................................................................... 9 Appendix I: Funding Sources 1997- 2013 ............................................................................... 10 Introduction In 2008, the Board published the complaint investigation -
Spatial Distribution of Impacts to Channel Bed Mobility Due to Flow Regulation, Kootenai River, Usa
SPATIAL DISTRIBUTION OF IMPACTS TO CHANNEL BED MOBILITY DUE TO FLOW REGULATION, KOOTENAI RIVER, USA Michael Burke1, Research Associate, University of Idaho ([email protected]); Klaus Jorde1, Professor, University of Idaho; John M. Buffington1,2, Research Geomorphologist, USDA Forest Service; Jeffrey H. Braatne3, Assistant Professor, University of Idaho; Rohan Benjankar1, Research Associate, University of Idaho. 1Center for Ecohydraulics Research, Boise, ID 2Rocky Mountain Research Station, Boise, ID 3College of Natural Resources, Moscow, ID Abstract The regulated hydrograph of the Kootenai River between Libby Dam and Kootenay Lake has altered the natural flow regime, resulting in a significant decrease in maximum flows (60% net reduction in median 1-day annual maximum, and 77%-84% net reductions in median monthly flows for the historic peak flow months of May and June, respectively). Other key hydrologic characteristics have also been affected, such as the timing of annual extremes, and the frequency and duration of flow pulses. Moreover, Libby Dam has impeded downstream delivery of sediment from the upper 23,300 km2 of a 50,000 km2 watershed. Since completion of the facility in 1974, observed impacts to downstream channel bed and bars in semi-confined and confined reaches of the Kootenai River have included coarsening of the active channel bed, homogenization of the channel bed, disappearance of relatively fine-grained beach bars, and invasion of bar surfaces by perennial vegetative species. These impacts have led to reduced aquatic habitat heterogeneity and reduced abundance of candidate recruitment sites for riparian tree species such as black cottonwood (Populus trichocarpa) and native willows (Salix spp.). Limited quantitative documentation of the pre-regulation substrate composition exists. -
Libby Varq Flood Control Impacts on Kootenay River Dikes
MINISTRY OF ENERGY, MINES AND NATURAL GAS LIBBY VARQ FLOOD CONTROL IMPACTS ON KOOTENAY RIVER DIKES FINAL PROJECT NO: 0640-002 DISTRIBUTION: DATE: November 7, 2012 RECIPIENT: 2 copies BGC: 2 copies OTHER: 1 copy R.2.7.9 #800-1045 Howe Street Vancouver, B.C. Canada V6Z 2A9 Tel: 604.684.5900 Fax: 604.684.5909 November 7, 2012 Project No: 0640-002 Chris Trumpy Ministry of Energy, Mines and Natural Gas PO Box 9053 Station Provincial Government Victoria, BC V8W 9E2 Dear Mr. Trumpy, Re: Libby VARQ Flood Control Impacts on Kootenay River Dikes Please find enclosed a FINAL report for the above-referenced study. If you have any questions or comments, please contact the undersigned at (604) 629-3850. Yours sincerely, BGC ENGINEERING INC. per: Hamish Weatherly, M.Sc., P.Geo. Senior Hydrologist Ministry of Energy, Mines and Natural Gas, November 7, 2012 Libby VARQ Flood Control Impacts on Kootenay River Dikes - FINAL Project No: 0640-002 TABLE OF CONTENTS TABLE OF CONTENTS .......................................................................................................... i LIST OF TABLES .................................................................................................................. ii LIST OF FIGURES ................................................................................................................. ii LIMITATIONS ....................................................................................................................... iv 1.0 INTRODUCTION .........................................................................................................