Eutsuk Lake Rainbow Trout: Biology, Population Significance and Fishery Management

Total Page:16

File Type:pdf, Size:1020Kb

Eutsuk Lake Rainbow Trout: Biology, Population Significance and Fishery Management Eutsuk Lake Rainbow Trout: Biology, Population Significance and Fishery Management prepared by: Joseph S. De Gisi Box 2518 Smithers, BC V0J 2N0 for: BC Parks Skeena District Box 5000 Smithers, BC V0J 2N0 December 2002 Eutsuk Lake Rainbow Trout Table of Contents List of Figures.....................................................................................................................iii List of Tables ......................................................................................................................iii List of Appendices..............................................................................................................iv 1. Introduction..................................................................................................1 1.1. Document Organization ..........................................................................................2 1.2. Concepts and Definitions.........................................................................................2 2. Sources and Methods ...................................................................................5 2.1. Occurrence of the Large Lake Piscivore Ecotype ..................................................5 2.2. Life History of British Columbia Piscivorous Rainbow Trout ..............................5 2.2.1. Eutsuk Lake Fish Population and Habitat Datasets.............................................5 2.2.1.1. Lake Survey 1982.........................................................................................5 2.2.1.2. Angling Guides 1982....................................................................................6 2.2.1.3. MELP Tagging 1986 ....................................................................................6 2.2.1.4. Anglers 1994 ................................................................................................6 2.2.1.5. Hatfield Consultants 1997.............................................................................6 2.2.1.6. Keeley 1999 .................................................................................................7 2.2.1.7. Miscellaneous Fish Data...............................................................................7 2.3. Habitats Of Importance to Eutsuk Rainbow Trout ...............................................7 2.3.1. Eutsuk Lake Physiochemistry ............................................................................7 2.3.1.1. Comparable Physiochemical Data.................................................................7 2.3.2. Adjacent Stream Habitat ....................................................................................8 2.4. Management of Piscivorous Rainbow Trout in British Columbia ........................8 2.5. Post-Release Angling Mortality of Salmonids ........................................................8 3. Results and Discussion .................................................................................9 3.1. What is the relative rarity of this ecotype in the province? ...................................9 3.2. How do the characteristics of Eutsuk Lake piscivorous rainbow trout, and fish production environment of Eutsuk Lake, compare to other occurrences of this ecotype?.................................................................................. 12 3.2.1. Life History ..................................................................................................... 12 3.2.2. Fish Production Environment........................................................................... 13 3.3. Are there known habitats located within or adjacent to the park which may require focused management?............................................................ 21 3.3.1. Stream Habitats Adjacent to the Eutsuk Basin.................................................. 21 3.3.1.1. Eutsuk River (Eutsuk Lake Outlet).............................................................. 21 3.3.1.2. Eutsuk Lake Tributaries .............................................................................. 25 3.3.1.2.1. Fifth-Order Tributaries ......................................................................... 25 3.3.1.2.2. Fourth-Order Tributaries ...................................................................... 26 i Eutsuk Lake Rainbow Trout 3.3.1.2.3. Third- and Lower-Order Tributaries ..................................................... 26 3.3.1.3. Potential Impacts to Streams in the Eutsuk Lake Drainage .......................... 29 3.3.2. Eutsuk Lake Physiochemistry .......................................................................... 30 3.3.3. Nechako Reservoir........................................................................................... 30 3.4. How are sport fisheries exploiting other populations of this ecotype managed in British Columbia? ............................................................................. 32 3.4.1. Monitoring....................................................................................................... 32 3.4.2. Method and Harvest Regulation ....................................................................... 32 3.5. Is post-release mortality an important consideration in regulating angling on Eutsuk Lake?....................................................................................... 36 3.5.1. Experimental Time Frame................................................................................ 36 3.5.2. Experimental Evidence About Post-Release Mortality...................................... 37 3.5.3. Other Considerations........................................................................................ 38 3.5.4. Summary ......................................................................................................... 39 3.6. Based on available information, is it possible to confidently evaluate whether the current management of Eutsuk Lake rainbow trout angling will provide long term sustainability of both population abundance and size of angled trout?..................................................................... 40 3.6.1. Visitor Use Statistics........................................................................................ 40 3.6.2. Volunteer Creel Cards...................................................................................... 41 3.6.3. Angling Guide Reports .................................................................................... 42 3.6.4. Fishery Totals .................................................................................................. 42 3.6.5. Summary ......................................................................................................... 43 3.7. If available information is insufficient, what supplementary data should be sought to allow management of the population? ................................. 49 3.8. In the absence of supplementary data, what would be a prudent approach to management of the rainbow trout fishery?...................................... 49 4. References...................................................................................................50 ii Eutsuk Lake Rainbow Trout List of Figures Figure 1. Mean length at age for Eutsuk Lake rainbow trout.............................................. 16 Figure 2. Limnological characteristics of lakes supporting the pelagic piscivorous rainbow trout ecotype .................................................................................................. 19 Figure 3. Upstream view of Eutsuk River .......................................................................... 22 Figure 4. Aerial downstream view of Redfern Rapids........................................................ 23 Figure 5. Aerial upstream/lateral view of Redfern Rapids.................................................. 23 Figure 6. Downstream view of Redfern Rapids from river left bank .................................. 24 Figure 7. Downstream view of Redfern Rapids from center of river. ................................. 24 Figure 8. Aerial upstream view of Tesla Creek showing its confluence with glacially-silty Chezko River......................................................................................... 28 Figure 9. Aerial upstream view of Chezko River rapids roughly 0.7 channel km downstream of the Tesla Creek confluence. ................................................................. 28 List of Tables Table 1. North American lakes which reportedly support indigenous populations of the pelagic piscivorous rainbow trout ecotype.............................................................. 11 Table 2. Life history characteristics of North American indigenous populations of the pelagic piscivorous rainbow trout ecotype.............................................................. 14 Table 3. Length at age for piscivorous and non-piscivorous rainbow trout ......................... 15 Table 4. Fish community characteristics of lakes which appear to support indigenous populations of the pelagic piscivorous rainbow trout ecotype....................................... 17 Table 5. Water chemistry parameters for North American lakes which likely support indigenous populations of the pelagic piscivorous rainbow trout ecotype..................... 18 Table 6. Third- and lower-order tributaries to Eutsuk Lake which have received fish sampling attention. ...................................................................................................... 27 Table 7. Management of pelagic piscivorous rainbow trout populations............................
Recommended publications
  • The Toxicological Effects of the Mount Polley Tailings Impoundment Breach on Freshwater Amphipods
    THE TOXICOLOGICAL EFFECTS OF THE MOUNT POLLEY TAILINGS IMPOUNDMENT BREACH ON FRESHWATER AMPHIPODS RAEGAN D. PLOMP Bachelor of Science, University of Lethbridge, 2017 A thesis submitted in partial fulfilment of the requirements for the degree of MASTER OF SCIENCE in BIOLOGICAL SCIENCES Department of Biological Sciences University of Lethbridge LETHBRIDGE, ALBERTA, CANADA © Raegan Plomp, 2019 THE TOXICOLOGICAL EFFECTS OF THE MOUNT POLLEY TAILINGS IMPOUNDMENT BREACH ON FRESHWATER AMPHIPODS RAEGAN D. PLOMP Date of Defence: September 6, 2019 Dr. G. Pyle Professor Ph.D. Supervisor Dr. S. Wiseman Associate Professor Ph.D. Thesis Examination Committee Member Dr. R. Laird Associate Professor Ph.D. Thesis Examination Committee Member Dr. Laura Chasmer Assistant Professor Ph.D. Internal External Examiner Department of Geography Dr. T. Russell Associate Professor Ph.D. Chair, Thesis Examination Committee ii Abstract The bioavailability and toxicity of metals to amphipods is influenced by exposure route and co-toxic mechanisms. Metal bioavailability was studied in amphipods at sites affected by the 2014 Mount Polley Mining Corporation tailings impoundment breach. The area around the lake was also subjected to wildfire in 2017. Bioavailability was more correlated with sediment than waterborne metal concentrations with Cu correlating well with distance from the breach. Copper-sediment bioavailability to amphipods in combination with wildfire runoff was studied resulting in non-additive toxicity. Hyalella azteca exposed to Cu-enriched sediment with fire extract (FE) experienced a more-than- additive effect on survival and amphipod whole-body Cu concentration but no significant reduction in growth or acetylcholinesterase activity compared to the Cu-contaminated sediment or FE alone, respectively.
    [Show full text]
  • British Columbia Vegetation and Climate History with Focus on 6 Ka BP
    Document generated on 10/01/2021 4:51 p.m. Géographie physique et Quaternaire British Columbia Vegetation and Climate History with Focus on 6 ka BP Histoire du climat et de la végétation de la Colombie-Britannique, notamment de la période de 6 ka BP Geschichte der Vegetation und des Klimas in British Columbia während des Holozäns, besonders um 6 ka v.u.Z. Richard J. Hebda La paléogéographie et la paléoécologie d’il y a 6000 ans BP au Canada Article abstract Paleogeography and Paleoecology of 6000 yr BP in Canada British Columbia Holocene vegetation and climate is reconstructed from pollen Volume 49, Number 1, 1995 records. A coastal Pinus contorta paleobiome developed after glacier retreat under cool and probably dry climate. Cool moist forests involving Picea, Abies, URI: https://id.erudit.org/iderudit/033030ar Tsuga spp., and Pinus followed until the early Holocene. Pseudotsuga menziesii DOI: https://doi.org/10.7202/033030ar arrived and spread in the south 10 000-9000 BP, and Picea sitchensis - Tsuga heterophylla forests developed in the north. T. heterophylla increased 7500-7000 BP, and Cupressaceae expanded 5000-4000 BP. Bogs began to See table of contents develop and expland. Modern vegetation arose 4000-2000 BP. There were early Holocene grass and Artemisia communities at mid-elevations and pine stands at high elevations in southern interior B.C. Forests expanded downslope and Publisher(s) lakes formed 8500-7000 BP. Modern forests arose 4500-4000 BP while lower and upper tree lines declined. In northern B.C. non-arboreal communities Les Presses de l'Université de Montréal preceded middle Holocene Picea forests.
    [Show full text]
  • The Selkirk Mountains : a Guide for Mountain Climbers and Pilgrims
    J Presentee) to ^be Xibrar^ of tbe xaniversit^ of Toronto bs Her"bert B. Sampson, K,C, Digitized by the Internet Archive in 2011 with funding from University of Toronto http://www.archive.org/details/selkirkmountainsOOwhee THE Selkirk Mountains A Guide for Mountain Climbers and Pilgrims Information by A. O. WHEELER, F.R.G.S., A.C.C., A.C., A.A.C. vo A- Stovel Company, Engravers, Lithographers and Printers, Winnipeg, Man. Arthur O. Wheeler, First President of Alpine Club — CONTENTS Foreword—A. 0. Wlieeler Page 1 One Word More—Elizabeth Parker 2 The Snowy Selkirks—Elizabeth Parker 3-5 CHAPTER I. The Rocky Mountain System—The Selkirks—Early Explorers Later Histor}'—The Railway—Discovery of Rogers Pass—An Alpine Club—Members of British Association Visit the Selkirks, (1884) —Result of Completion of Railway—Government Surveys (1886) —First Scientific Observations of Illecillewaet Glacier Topographical Survey by William Spotswood Green—The Alpine Club, England, and the Swiss Alpine Club—The Appalachian Mountain Club—Triangulation of Railway Belt—Subsequent Mountaineering Pages 6-32 CHAPTER n. Peaks, Passes and Valleys Reached from Glacier—Glacier Park Swiss Guides—Glacier House—Outfits and Ponies—Places and Peaks of Interest Alphabetically Arranged 33-104 CHAPTER m. The Caves of Cheops (Xakimu Caves) —the Valley of the Caves The Approach to the Caves—Formation and Structure—Descrip- tion of Caves—The Mill Bridge Series—The Gorge Series—The Judgment Hall 106-117 CHAPTER IV. •Golden and the Country of the Upper Columbia—Along the Columbia River between Golden and Beavermouth are Several Points of Interest—the Upper Columbia—Travel by Waterway on the Upper Columbia 119-135 CHAPTER V.
    [Show full text]
  • A G~Ographic Dictionary of Washington
    ' ' ., • I ,•,, ... I II•''• -. .. ' . '' . ... .; - . .II. • ~ ~ ,..,..\f •• ... • - WASHINGTON GEOLOGICAL SURVEY HENRY LANDES, State Geologist BULLETIN No. 17 A G~ographic Dictionary of Washington By HENRY LANDES OLYMPIA FRAN K M, LAMBORN ~PUBLIC PRINTER 1917 BOARD OF GEOLOGICAL SURVEY. Governor ERNEST LISTER, Chairman. Lieutenant Governor Louis F. HART. State Treasurer W.W. SHERMAN, Secretary. President HENRY SuzzALLO. President ERNEST 0. HOLLAND. HENRY LANDES, State Geologist. LETTER OF TRANSMITTAL. Go,:ernor Ernest Lister, Chairman, and Members of the Board of Geological Survey: GENTLEMEN : I have the honor to submit herewith a report entitled "A Geographic Dictionary of Washington," with the recommendation that it be printed as Bulletin No. 17 of the Sun-ey reports. Very respectfully, HENRY LAKDES, State Geologist. University Station, Seattle, December 1, 1917. TABLE OF CONTENTS. Page CHAPTER I. GENERAL INFORMATION............................. 7 I Location and Area................................... .. ... .. 7 Topography ... .... : . 8 Olympic Mountains . 8 Willapa Hills . • . 9 Puget Sound Basin. 10 Cascade Mountains . 11 Okanogan Highlands ................................ : ....' . 13 Columbia Plateau . 13 Blue Mountains ..................................... , . 15 Selkirk Mountains ......... : . : ... : .. : . 15 Clhnate . 16 Temperature ......... .' . .. 16 Rainfall . 19 United States Weather Bureau Stations....................... 38 Drainage . 38 Stream Gaging Stations. 42 Gradient of Columbia River. 44 Summary of Discharge
    [Show full text]
  • Slocan Lake 2007 - 2010
    BC Lake Stewardship and Monitoring Program Slocan Lake 2007 - 2010 A partnership between the BC Lake Stewardship Society and the Ministry of Environment The Importance of Slocan Lake & its Watershed British Columbians want lakes to provide good water quality, quality of the water resource is largely determined by a water- aesthetics, and recreational opportunities. When these features shed’s capacity to buffer impacts and absorb pollution. are not apparent in our local lakes, people begin to wonder why. Concerns often include whether the water quality is getting Every component of a watershed (vegetation, soil, wildlife, etc.) worse, if the lake has been impacted by land development or has an important function in maintaining good water quality and a other human activities, and what conditions will result from more healthy aquatic environment. It is a common misconception that development within the watershed. detrimental land use practices will not impact water quality if they are kept away from the area immediately surrounding a water- The BC Lake Stewardship Society (BCLSS), in collaboration body. Poor land use practices in a watershed can eventually im- with the Ministry of Environment (MoE), has designed a pro- pact the water quality of the downstream environment. gram, entitled The BC Lake Stewardship and Monitoring Pro- gram, to address these concerns. Through regular water sample Human activities that impact water bodies range from small but collections, we can come to understand a lake's current water widespread and numerous non-point sources throughout the wa- quality, identify the preferred uses for a given lake, and monitor tershed to large point sources of concentrated pollution (e.g.
    [Show full text]
  • The Kootenay Wreck Tour River Above Castlegar
    Underwater Archaeological Society of British Columbia Vol. 22 No.6 Nov-Dec 2011 waterfront. The Ymir was made of wood and is 77’ long x 16’ wide x 6’ deep. It was built and launched at Nel‐ son in 1899 and was used to move Transfer barges around. The super structure is gone but the hull, deck planking and boiler are still in place. Directly off the bow of the Ymir is a fifteen car Railway Transfer barge in about 50’ of water. This is a shore dive and the fact that most of the decking is gone means that the inter‐ nal structure of the barge can be seen. This dive site also happens to be the location of the CPR shipways on Kootenay Lake. The CPR fleet of stern‐ wheelers, tugs and Rail barge would have been built and maintained at this location in the late 1800’s up to 1930. Our next site to visit was the Steam Tug Elco II located in the Columbia The Kootenay Wreck Tour River above Castlegar. The Elco II was by, Bill Meekel 76’ long x 15’ wide x 7’ deep. It was built by the Edgewood Lumber Co in In September 2011, eight UASBC concentrates from the mines around 1924 to move log booms on the Arrow members made a visit to the the lake before the railway was in‐ Lakes to their sawmill. The vessel is a Kootenays to visit some of the wrecks stalled. The barge is 197’ long x 33’ shore dive and is upside down on the in the area.
    [Show full text]
  • Corrugated Architecture of the Okanagan Valley Shear Zone and the Shuswap Metamorphic Complex, Canadian Cordillera
    Corrugated architecture of the Okanagan Valley shear zone and the Shuswap metamorphic complex, Canadian Cordillera Sarah R. Brown1,2,*, Graham D.M. Andrews1,3, and H. Daniel Gibson2 1DEPARTMENT OF GEOLOGICAL SCIENCES, CALIFORNIA STATE UNIVERSITY–BAKERSFIELD, 9001 STOCKDALE HIGHWAY, BAKERSFIELD, CALIFORNIA 93311, USA 2DEPARTMENT OF EARTH SCIENCE, SIMON FRASER UNIVERSITY, 8888 UNIVERSITY DRIVE, BURNABY, BRITISH COLUMBIA V5A 1S6, CANADA 3DEPARTMENT OF GEOLOGY AND GEOGRAPHY, WEST VIRGINIA UNIVERSITY, 98 BEECHURST AVENUE, MORGANTOWN, WEST VIRGINIA 26506, USA ABSTRACT The distribution of tectonic superstructure across the Shuswap metamorphic complex of southern British Columbia is explained by east-west– trending corrugations of the Okanagan Valley shear zone detachment. Geological mapping along the southern Okanagan Valley shear zone has identified 100-m-scale to kilometer-scale corrugations parallel to the extension direction, where synformal troughs hosting upper-plate units are juxtaposed between antiformal ridges of crystalline lower-plate rocks. Analysis of available structural data and published geological maps of the Okanagan Valley shear zone confirms the presence of≤ 40-km-wavelength corrugations, which strongly influence the surface trace of the detachment system, forming spatially extensive salients and reentrants. The largest reentrant is a semicontinuous belt of late Paleozoic to Mesozoic upper-plate rocks that link stratigraphy on either side of the Shuswap metamorphic complex. Previously, these belts were considered by some to be autochthonous, implying minimal motion on the Okanagan Valley shear zone (≤12 km); conversely, our results suggest that they are allochthonous (with as much as 30–90 km displacement). Corrugations extend the Okanagan Valley shear zone much farther east than previously recognized and allow for hitherto separate gneiss domes and detachments to be reconstructed together to form a single, areally extensive Okanagan Valley shear zone across the Shuswap metamorphic complex.
    [Show full text]
  • An Act Respecting the Nakusp and Slocan Railway
    1894. RAILWAY, NAKTJSP AND SLOGAN. CLXAP. 43. CHAPTER 43. An Act respecting the Nakusp and Slocan Railway. [llih April, 189i.} 7HEREAS authority was conferred upon the Lieutenant-Governor Preamble. > in Council by the " Railway Aid Act, 1893," to give a guarantee of interest upon the bonds of (amongst other railways) the Nakusp and Slocan Railway Company, hereinafter called the " Company," to the extent, at the rate, and upon the conditions in said Act specified, and power was also conferred to arrange all details, and to enter into all agreements which might be necessary for cariying out the pro­ visions of the said Act: And whereas under and in pursuance of the authority conferred by the said Act, the Lieutenant-Governor in Council duly authorized the execution of the several agreements, copies whereof arc set out in the schedule hereto purporting to be executed by the Minister of Finance or the Chief Commissioner of Lands and Works, as the case may be, viz.:— (1.) Agreement dated the 9th day of August, 1893, between the Nakusp and Slocan Railway Company and the Chief Commissioner of Lands and Works; (2.) Agreement dated the 29th day of August, 1893, between the Nakusp and Slocan Railway Company, the Bank of British Columbia, Messrs. WulfFsohn & Bewicke, Limited, and the Minister of Finance. And whereas pursuant to said agreements the Company has by instrument, dated the 16th day of August, 1893, duly assigned to the Chief Commissioner of Lands and Works all benefit and advantage under the agreement with the Canadian Pacific Railway Company, as provided by the first clause of the said agreement of the 9th August, 1893 : 223 CHAP.
    [Show full text]
  • 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).
    [Show full text]
  • Dionisio Point Excavations
    1HE• Publication of the Archaeological Society of Vol. 31 , No. I - 1999 Dionisio Point Excavations ARCHAEOLOGICAL SOCIETY OF &MIDDEN BRITISH COLUMBIA Published four times a year by the Archaeological Society of British Columbia Dedicated to the protection of archaeological resot:Jrces and the spread of archaeological knowledge. Editorial Committee Editor: Heather Myles (274-4294) President Field Editor: Richard Brolly (689-1678) Helmi Braches (462-8942) arcas@istar. ca [email protected] News Editor: Heather Myles Publications Editor: Robbin Chatan (215-1746) Membership [email protected] Sean Nugent (685-9592) Assistant Editors: Erin Strutt [email protected] erins@intergate. be.ca Fred Braches Annual membership includes I year's subscription to [email protected] The Midden and the ASBC newsletter, SocNotes. Production & Subscriptions: Fred Braches ( 462-8942) Membership Fees I SuBSCRIPTION is included with ASBC membership. Individual: $25 Family: $30 . Seniors/Students: $I 8 Non-members: $14.50 per year ($1 7.00 USA and overseas), Send cheque or money order payable to the ASBC to: payable in Canadian funds to the ASBC. Remit to: ASBC Memberships Midden Subscriptions, ASBC P.O. Box 520, Bentall Station P.O. Box 520, Bentall Station Vancouver BC V6C 2N3 Vancouver BC V6C 2N3 SuBMISSIONs: We welcome contributions on subjects germane ASBC on Internet to BC archaeology. Guidelines are available on request. Sub­ http://home.istar.ca/-glenchan/asbc/asbc.shtml missions and exchange publications should be directed to the appropriate editor at the ASBC address. Affiliated Chapters Copyright Nanaimo Contact: Rachael Sydenham Internet: http://www.geocities.com/rainforest/5433 Contents of The Midden are copyrighted by the ASBC.
    [Show full text]
  • Field Key to the Freshwater Fishes of British Columbia
    FIELD KEY TO THE FRESHWATER FISHES OF BRITISH COLUMBIA J.D. McPhail and R. Carveth Fish Museum, Department of Zoology, University of British Columbia, 6270 University Blvd., Vancouver, B.C., Canada, V6T 1Z4 (604) 822-4803 Fax (604) 822-2416 © The Province of British Columbia Published by the Resources Inventory Committee Canadian Cataloguing in Publication Data McPhail, J. D. (John Donald) Field key to the freshwater, fishes of British Columbia Also available through the Internet. Previously issued: Field key to the freshwater fishes of British Columbia. Draft for 1994 field testing, 1994. Includes bibliographical references: p. ISBN 0-7726-3830-6 (Field guide) ISBN 0-7726-3844-6 (Computer file) 1. Freshwater fishes - British Columbia - Identification. I. Carveth, R. II. Resources Inventory Committee (Canada) III. Title. QL626.5.B7M36 1999 597.176'09711 C99-960109-1 Additional Copies of this publication can be purchased from: Government Publications Centre Phone: (250) 387-3309 or Toll free: 1 -800-663-6105 Fax: (250) 387-0388 www.publications.gov.bc.ca Digital Copies are available on the Internet at: http://www.for.gov. bc.ca/ric Text copyright © 1993 J.D. McPhail Illustrations copyright © 1993 D.L. McPhail All rights reserved. Design and layout by D.L. McPhail "Admitted that some degree of obscurity is inseparable from both theology and ichthyology, it is not inconsistent with profound respect for the professors of both sciences to observe that a great deal of it has been created by themselves." Sir Herbert Maxwell TABLE OF CONTENTS Introduction · i Region 1 - Vancouver Island 1 Region 2 - Fraser 27 Region 3 - Columbia 63 Region 4 - MacKenzie 89 Region 5 - Yukon 115 Region 6 - North Coast 127 Region 7 - Queen Charlotte Islands 151 Region 8 - Central Coast 167 Appendix 193 Acknowledgements .
    [Show full text]
  • Cleaning up BC's Dirty Mining Industry
    Vol.35 No.1 | 2016 Published by the Wilderness Committee FREE REPORT Joe Foy The Quesnel Lake watershed risks and health impacts from BC's National Campaign have been looking at reducing the Director, supports an important component mining industry. pressure on mine dams. That sounds Wilderness Committee of the Fraser River sockeye salmon Tailings storage facilities like the like good news – but it isn’t. There @JoeFoyWild run. Fisheries managers are holding one at Mount Polley have become is now an increase in schemes that their breath, waiting to see what long- widespread throughout the province. involve dumping mine wastewater term impacts BC now has 98 into downstream rivers, lakes and the Mount Polley permitted tailings creeks, which are often important hen the tailings pond dam disaster will have ponds at 60 operating salmon habitat. Wbreached at BC's Mount Polley on the run. and closed mines.5 For example, the Gibraltar Mine, Mine in August 2014, it unleashed First Nation Many of them are the located near Williams Lake, was a torrent of mine waste and water. community size of a lake – multiple recently issued a temporary permit Much of this ended up pouring into members who kilometres across. to increase the release of mine one of the province's most important fish for salmon At the Highland tailings pond water up to 5.4 million salmon nurseries – Quesnel Lake. downstream Valley Copper mine cubic metres a year directly into the An estimated 8 million cubic of the spill are located between Logan Fraser River.7 metres of solid mine
    [Show full text]