White Sturgeon
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Ecosystem Status and Trends Report for the Strait of Georgia Ecozone
C S A S S C C S Canadian Science Advisory Secretariat Secrétariat canadien de consultation scientifique Research Document 2010/010 Document de recherche 2010/010 Ecosystem Status and Trends Report Rapport de l’état des écosystèmes et for the Strait of Georgia Ecozone des tendances pour l’écozone du détroit de Georgie Sophia C. Johannessen and Bruce McCarter Fisheries and Oceans Canada, Institute of Ocean Sciences 9860 W. Saanich Rd. P.O. Box 6000, Sidney, B.C. V8L 4B2 This series documents the scientific basis for the La présente série documente les fondements evaluation of aquatic resources and ecosystems scientifiques des évaluations des ressources et in Canada. As such, it addresses the issues of des écosystèmes aquatiques du Canada. Elle the day in the time frames required and the traite des problèmes courants selon les documents it contains are not intended as échéanciers dictés. Les documents qu’elle definitive statements on the subjects addressed contient ne doivent pas être considérés comme but rather as progress reports on ongoing des énoncés définitifs sur les sujets traités, mais investigations. plutôt comme des rapports d’étape sur les études en cours. Research documents are produced in the official Les documents de recherche sont publiés dans language in which they are provided to the la langue officielle utilisée dans le manuscrit Secretariat. envoyé au Secrétariat. This document is available on the Internet at: Ce document est disponible sur l’Internet à: http://www.dfo-mpo.gc.ca/csas/ ISSN 1499-3848 (Printed / Imprimé) ISSN 1919-5044 (Online / En ligne) © Her Majesty the Queen in Right of Canada, 2010 © Sa Majesté la Reine du Chef du Canada, 2010 TABLE OF CONTENTS Highlights 1 Drivers of change 2 Status and trends indicators 2 1. -
KR/KL Burbot Conservation Strategy
January 2005 Citation: KVRI Burbot Committee. 2005. Kootenai River/Kootenay Lake Conservation Strategy. Prepared by the Kootenai Tribe of Idaho with assistance from S. P. Cramer and Associates. 77 pp. plus appendices. Conservation strategies delineate reasonable actions that are believed necessary to protect, rehabilitate, and maintain species and populations that have been recognized as imperiled, but not federally listed as threatened or endangered under the US Endangered Species Act. This Strategy resulted from cooperative efforts of U.S. and Canadian Federal, Provincial, and State agencies, Native American Tribes, First Nations, local Elected Officials, Congressional and Governor’s staff, and other important resource stakeholders, including members of the Kootenai Valley Resource Initiative. This Conservation Strategy does not necessarily represent the views or the official positions or approval of all individuals or agencies involved with its formulation. This Conservation Strategy is subject to modification as dictated by new findings, changes in species status, and the completion of conservation tasks. 2 ACKNOWLEDGEMENTS The Kootenai Tribe of Idaho would like to thank the Kootenai Valley Resource Initiative (KVRI) and the KVRI Burbot Committee for their contributions to this Burbot Conservation Strategy. The Tribe also thanks the Boundary County Historical Society and the residents of Boundary County for providing local historical information provided in Appendix 2. The Tribe also thanks Ray Beamesderfer and Paul Anders of S.P. Cramer and Associates for their assistance in preparing this document. Funding was provided by the Bonneville Power Administration through the Northwest Power and Conservation Council’s Fish and Wildlife Program, and by the Idaho Congressional Delegation through a congressional appropriation administered to the Kootenai Tribe by the Department of Interior. -
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. -
Link to Full Text
~ .......... ~ ~ - - -- .. ~~ -- .... ..... .., - .. - ... ...., .... IX. ADYNAMIC HESEHV01H SIMULATION MODEL-DYHESM:5 i\ 311 c. transverse and longitUdinal direction playa secondary role and only the variations) ." I in the vertical enter lhe first order balances of mass, momentum and energy. 1/ I Departures from this Stilte of horizontalisopyc'nalsare possible, but these \ tI l A DYNAMIC RESERVOIR SIl\olULATION MODEL enter only as isolated events or as \I/eak pe.!lurbatiQ.D.S. In both cases the.•net eJJ;cJ,J CI DYRESM: 5 is e~plured wi(h a parame!efizalion of their inp,ut (0 the vertical s(rUelure"iiild , ) I comparison of the model prediction and field data must thus be confined to ~ ~ .....of.............,.calm when the structure is truly one-dimensional. lorg 1mberger and John C.. Pattetsun .. ~ ,. The constraints imposed by ~uch a one-dimer.:Jional model may best be University of Western Australia quantified by defining a series of non-dimensional llUmbers. The value of the Nedlands, Western Australia Wedderburn number :) LV =.i.!!.. h (.J" I I '( 14.2 • L- '7 y(l .. n, (I) , \ ..,' I / 1. INTRODUCTION where g' is an effective reoufed gravity across the thermocline, h the depth of the mixed layer, L the basin scale, and u· the surface shear velocity, is a measure of """·".',j<}·,t-·;~·'",,,"~~,'ti The dynamic reservoir simulation model, DYRESM, is a one-dimensional the activity within the mixed layer. Spigel and Imberger (I980) have shown thah, numerical model for the prediction of temperature and salinity in small to medium for W > 00) the departure fmm one-dimensionality is minimal and for I ':I sized reservoirs and Jakes. -
Prehistoric Mobile Art from the Mid-Fraser and Thompson River Areas ARNOUDSTRYD
CHAPTER9 Prehistoric Mobile Art from the Mid-Fraser and Thompson River Areas ARNOUDSTRYD he study of ethnographic and archaeological art the majority of archaeological work in the Plateau but from interior British Columbia has never received also appear to be the "heartland" of Plateau art develop Tthe attention which has been lavished on the art of ment as predicted by Duff (1956). Special attention will be the British Columbia coast. This was inevitable given the focused on the previously undescribed carvings recovered impressive nature of coastal art and the relative paucity in recent excavations by the author along the Fraser River of its counterpart. Nevertheless, some understanding of near the town of Lillooet. the scope and significance of this art has been attained, Reports and collections from seventy-one archaeologi largely due to the turn of the century work by members cal sites were checked for mobile art. They represent all of the Jesup North Pacific Expedition (Teit 1900, 1906, the prehistoric sites excavated and reported as of Spring 1909; Boas, 1900; Smith, 1899, 1900) and the more recent 1976, although some unintentional omissions may have studies by Duff (1956, 1975). Further, archaeological occurred. The historic components of continually oc excavations over the last fifteen years (e.g., Sanger 1968a, cupied sites were deleted and sites with assemblages of 1968b, 1970; Stryd 1972, 1973) have shown that prehistoric less than ten artifacts were also omitted. The most notable Plateau art was more extensive than previously thought, exclusions from this study are most of Smith's (1899) and that ethnographic carving represented a degeneration Lytton excavation data which are not quantified or listed from a late prehistoric developmental climax. -
Spring Bloom in the Central Strait of Georgia: Interactions of River Discharge, Winds and Grazing
MARINE ECOLOGY PROGRESS SERIES Vol. 138: 255-263, 1996 Published July 25 Mar Ecol Prog Ser I l Spring bloom in the central Strait of Georgia: interactions of river discharge, winds and grazing Kedong yinl,*,Paul J. Harrisonl, Robert H. Goldblattl, Richard J. Beamish2 'Department of Oceanography, University of British Columbia, Vancouver, British Columbia, Canada V6T 124 'pacific Biological Station, Department of Fisheries and Oceans, Nanaimo, British Columbia, Canada V9R 5K6 ABSTRACT: A 3 wk cruise was conducted to investigate how the dynamics of nutrients and plankton biomass and production are coupled with the Fraser River discharge and a wind event in the Strait of Georgia estuary (B.C.,Canada). The spring bloom was underway in late March and early Apnl, 1991. in the Strait of Georgia estuary. The magnitude of the bloom was greater near the river mouth, indicat- ing an earher onset of the spring bloom there. A week-long wind event (wind speed >4 m S-') occurred during April 3-10 The spring bloom was interrupted, with phytoplankton biomass and production being reduced and No3 in the surface mixing layer increasing at the end of the wind event. Five days after the lvind event (on April 15),NO3 concentrations were lower than they had been at the end of the wind event, Indicating a utilization of NO3 during April 10-14. However, the utilized NO3 did not show up in phytoplankton blomass and production, which were lower than they had been at the end (April 9) of the wind event. During the next 4 d, April 15-18, phytoplankton biomass and production gradu- ally increased, and No3 concentrations in the water column decreased slowly, indicating a slow re- covery of the spring bloom Zooplankton data indicated that grazing pressure had prevented rapid accumulation of phytoplankton biomass and rapid utilization of NO3 after the wind event and during these 4 d. -
Examining Controls on Peak Annual Streamflow And
Hydrol. Earth Syst. Sci., 22, 2285–2309, 2018 https://doi.org/10.5194/hess-22-2285-2018 © Author(s) 2018. This work is distributed under the Creative Commons Attribution 4.0 License. Examining controls on peak annual streamflow and floods in the Fraser River Basin of British Columbia Charles L. Curry1,2 and Francis W. Zwiers1 1Pacific Climate Impacts Consortium, University of Victoria, Victoria, V8N 5L3, Canada 2School of Earth and Ocean Sciences, University of Victoria, Victoria, V8N 5L3, Canada Correspondence: Charles L. Curry ([email protected]) Received: 26 August 2017 – Discussion started: 8 September 2017 Revised: 19 February 2018 – Accepted: 14 March 2018 – Published: 16 April 2018 Abstract. The Fraser River Basin (FRB) of British Columbia with APF of ρO D 0.64; 0.70 (observations; VIC simulation)), is one of the largest and most important watersheds in west- the snowmelt rate (ρO D 0.43 in VIC), the ENSO and PDO ern North America, and home to a rich diversity of biologi- indices (ρO D −0.40; −0.41) and (ρO D −0.35; −0.38), respec- cal species and economic assets that depend implicitly upon tively, and rate of warming subsequent to the date of SWEmax its extensive riverine habitats. The hydrology of the FRB is (ρO D 0.26; 0.38), are the most influential predictors of APF dominated by snow accumulation and melt processes, lead- magnitude in the FRB and its subbasins. The identification ing to a prominent annual peak streamflow invariably oc- of these controls on annual peak flows in the region may be curring in May–July. -
Carrier Sekani Tribal Council Aboriginal Interests & Use Study On
Carrier Sekani Tribal Council Aboriginal Interests & Use Study on the Enbridge Gateway Pipeline An Assessment of the Impacts of the Proposed Enbridge Gateway Pipeline on the Carrier Sekani First Nations May 2006 Carrier Sekani Tribal Council i Aboriginal Interests & Use Study on the Proposed Gateway Pipeline ACKNOWLEDGEMENTS The Carrier Sekani Tribal Council Aboriginal Interests & Use Study was carried out under the direction of, and by many members of the Carrier Sekani First Nations. This work was possible because of the many people who have over the years established the written records of the history, territories, and governance of the Carrier Sekani. Without this foundation, this study would have been difficult if not impossible. This study involved many community members in various capacities including: Community Coordinators/Liaisons Ryan Tibbetts, Burns Lake Band Bev Ketlo, Nadleh Whut’en First Nation Sara Sam, Nak’azdli First Nation Rosa McIntosh, Saik’uz First Nation Bev Bird & Ron Winser, Tl’azt’en Nation Michael Teegee & Terry Teegee, Takla Lake First Nation Viola Turner, Wet’suwet’en First Nation Elders, Trapline & Keyoh Holders Interviewed Dick A’huille, Nak’azdli First Nation Moise and Mary Antwoine, Saik’uz First Nation George George, Sr. Nadleh Whut’en First Nation Rita George, Wet’suwet’en First Nation Patrick Isaac, Wet’suwet’en First Nation Peter John, Burns Lake Band Alma Larson, Wet’suwet’en First Nation Betsy and Carl Leon, Nak’azdli First Nation Bernadette McQuarry, Nadleh Whut’en First Nation Aileen Prince, Nak’azdli First Nation Donald Prince, Nak’azdli First Nation Guy Prince, Nak’azdli First Nation Vince Prince, Nak’azdli First Nation Kenny Sam, Burns Lake Band Lillian Sam, Nak’azdli First Nation Ruth Tibbetts, Burns Lake Band Ryan Tibbetts, Burns Lake Band Joseph Tom, Wet’suwet’en First Nation Translation services provided by Lillian Morris, Wet’suwet’en First Nation. -
Lake Koocanusa, High Level Assessment of a Proposed
BGC ENGINEERING INC. AN APPLIED EARTH SCIENCES COMPANY MINISTRY OF ENERGY, MINES AND PETROLEUM RESOURCES LAKE KOOCANUSA HIGH LEVEL ASSESSMENT OF A PROPOSED DAM FINAL DRAFT PROJECT NO.: 0466001 DATE: November 19, 2020 BGC ENGINEERING INC. AN APPLIED EARTH SCIENCES COMPANY Suite 500 - 980 Howe Street Vancouver, BC Canada V6Z 0C8 Telephone (604) 684-5900 Fax (604) 684-5909 November 19, 2020 Project No.: 0466001 Kathy Eichenberger, Executive Director Ministry of Energy, Mines and Petroleum Resources PO Box 9314, Stn Prov Govt Victoria, BC V8W 9N1 Dear Kathy, Re: Lake Koocanusa, High Level Assessment of a Proposed Dam – FINAL DRAFT BGC is pleased to provide the Ministry of Mines, Energy and Petroleum Resources with the following FINAL DRAFT report. The report details an assessment of a proposed dam on Lake Koocanusa, in southeastern British Columbia. 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. Principal Hydrologist Ministry of Energy, Mines and Petroleum Resources, Lake Koocanusa November 19, 2020 High Level Assessment of a Proposed Dam – FINAL DRAFT Project No.: 0466001 EXECUTIVE SUMMARY The Libby Dam is a 129 m high concrete gravity dam located on the Kootenay River near Libby, Montana. The dam was completed in 1973 and was first filled in 1974, inundating the Kootenay River valley to form the 145 km long Koocanusa Reservoir (Lake Koocanusa). Canadian residents and water users are affected by changes in the Libby Dam operations that affect reservoir water levels, as nearly half (70 km) of the reservoir extends into southeastern British Columbia. -
Mitochondrial DNA Analysis of Burbot Stocks in the Kootenai River Basin of British Columbia, Montana, and Idaho
Transactions of the American Fisheries Society 128:868-874, 1999 © Copyright by the American Fisheries Society 1999 Mitochondrial DNA Analysis of Burbot Stocks in the Kootenai River Basin of British Columbia, Montana, and Idaho VAUGHN L. PARAGAMIAN Idaho Department of Fish and Game, 2750 Kathleen Avenue, Coeur d'Alene, Idaho 83815, USA MADISON S. POWELL* AND JOYCE C. FALER Aquaculture Research Institute, University of Idaho, Moscow, Idaho 83844-2260, USA Abstract.-Differences in mitochondrial haplotype frequency were examined among burbot Lota lota collected from four areas within the Kootenai River Basin of British Columbia, Montana and Idaho. The polymerase chain reaction (PCR) was used to amplify three gene regions of the mi- tochondria) genome: NADH dehydrogenase subunit 1 (ND1), NADH dehydrogenase subunit 2 (ND2), and NADH dehydrogenase subunits 5 and 6 combined (ND5,6). Amplified DNA was screened for restriction fragment length polymorphisms (RFLPs). Simple haplotypes resulting from RFLPs in a single gene region were combined into composite haplotypes. The distribution of composite haplotypes and their frequencies correspond to areas of the Kootenay River basin above and below a presumptive geographic barrier, Kootenai Falls, Montana, and suggest spatially seg- regated populations. A test of geographic heterogeneity among haplotype frequency distributions was highly significant (P < 0.001) when a Monte Carlo simulation was used to approximate a X2 test. Two populations, one above and one below Kootenai Falls emerged when a neighbor-joining method was used to infer a phylogenetic tree based on estimates of nucleotide divergence between all pairs of sample locations. These analyses indicate that burbot below Kootenai Falls form a separate genetic group from burbot above the falls and further suggests that Libby Dam, which created Lake Koocanusa, is not an effective barrier segregating burbot above Kootenai Falls. -
Main Arm Kootenay Lake FIM 2011
Foreshore Inventory and 3Mapping KKOOOOTTEENNAAYY LLAAKKEE MMAAIINN AARRMM Prepared For: Regional District of Central Kootenay Prepared By: Ecoscape Environmental Consultants Ltd. September, 2010 File No.: 09-513 #102 – 450 Neave Court Kelowna, BC V1V 2M2 Phone: 250.491.7337 Fax: 250.491.7772 Email: [email protected] FORESHORE INVENTORY AND MAPPING Regional District of Central Kootenay Kootenay Lake Main Arm Prepared For: Regional District of Central Kootenay Box 590, 202 Lakeside Dr. Nelson, BC V1L 5R4 Prepared By: ECOSCAPE ENVIRONMENTAL CONSULTANTS LTD. #102 – 450 Neave Court Kelowna, B.C. V1W 3A1 January 2011 File No. 09-513 #102 – 450 Neave Ct. Kelowna BC. V1V 2M2 ph: 250.491.7337 fax: 250.491.7772 [email protected] 09-513 i January 2011 ACKNOWLEDGEMENTS This project was made possible through collaboration between the Regional District of Central Kootenay and Fisheries and Oceans Canada. The following parties carried out or organized fieldwork for this assessment: Fisheries and Oceans Canada: Bruce MacDonald, Sheldon Romaine, Brian Ferguson, Kristin Murphy, and Darryl Hussey The author of this report was: Jason Schleppe, M.Sc., R.P.Bio. (Ecoscape) The report was reviewed by: Kyle Hawes, B.Sc., R.P.Bio. (Ecoscape) Geographical Information Systems (GIS) mapping and analysis was prepared by: Robert Wagner, B.Sc. (Ecoscape) Recommended Citation: Schleppe, J., 2009. Kootenay Lake Foreshore Inventory and Mapping. Ecoscape Environmental Consultants Ltd.. Project File: 09-513. September, 2010. Prepared for: Regional District Central Kootenay. #102 – 450 Neave Ct. Kelowna BC. V1V 2M2 ph: 250.491.7337 fax: 250.491.7772 [email protected] 09-513 ii January 2011 EXECUTIVE SUMMARY This report has been prepared based upon the belief that it is possible to manage our watersheds and their natural surroundings in a sustainable manner. -
Columbia River Crossing I-5 Immersed Tunnel I-5 Immersed Tunnel Advantages Immersed Tunnel
6 Sections 500 feet long x 170 feet wide 3,000 ft. Columbia River Crossing I-5 Immersed Tunnel I-5 Immersed Tunnel Advantages Immersed Tunnel Navigation clearances Aviation clearances No freeway noise on river front No mile-long elevated bridge ramps dividing Vancouver Aberdeen Casting Basin 165 x 910 feet Baltimore's Fort McHenry Tunnel Completed 1985 1.4 miles 8 lanes – 4 tubes 115,000 vehicles/day I-95 Immersed Tunnel saved Baltimore’s Inner Harbor 1985 1959 freeway plan Vancouver’s Massey Tunnel under Fraser River October 14, 2019 Vancouver’s Fraser River Bridge replaced by Tunnel 10 lanes April 1, 2020 Vancouver’s Columbia River Bridge replaced by Tunnel Øresund Bridge 20 sections x 577ft = 2.2miles & Tunnel 1999 138ft wide Øresund Tunnel Section 20 sections x 577ft =2.2miles 138ft wide Columbia River Tunnel Section 6 sections x 500ft = 0.6miles 170ft wide Immersed Tunnels About six 500 foot immersed tunnel sections could be a simple, elegant, and cost effective solution to the I-5 Columbia River Crossing. The Aberdeen Casting Basin used to build the SR 520 bridge pontoons would be well suited to casting tunnel sections. https://www.wsdot.wa.gov/sites/default/files/2014/11/12/SR520-Factsheet-Pontoons- February2017.pdf In 1985 Baltimore completed the Fort McHenry Immersed Tunnel and saved its famous Inner Harbor from encirclement by I-95 concrete bridge. https://www.baltimorebrew.com/2011/04/29/the-senator-and-the-highway/ Vancouver, Canada rejected a ten lane bridge over the Fraser in favor of an immersed tunnel. https://www.enr.com/blogs/15-evergreen/post/47724-vancouvers-george-massey- tunnel-replacement-may-now-be-a-tunnel-instead-of-a-bridge The 1999 Oresund Bridge & Immersed Tunnel connects Sweden to Denmark.