KSM PROJECT 2009 Wildlife Habitat Suitability Baseline Report
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Physiography Geology
BRITISH COLUMBIA DEPARTMENT OF MINES HON. W. K. KIERNAN, Minister P. J. MULCAHY, Deputy Minister NOTES ON PHYSIOGRAPHY AND GEOLOGY OF (Bli BRITISH COLUMBIA b OFFICERS OF THE DEPARTMENT VICTCRIA, B.C. 1961 PHYSIOGRAPHY Physiographic divisions and names are established by the Geographic Board of Canada. Recently H. S. Bostock, of the Geological Survey of Canada, studied the physiography of the northern Cordilleran region; his report and maps are published CI I c Fig. 1. Rglief map of British Columbia. in Memoir 247 of the Geological Survey, Department of Mines and Resources, Ottawa. The divisions shown on the accompanying sketch, Figure 2, and the nomenclature used in the text are those proposed by Bostock. Most of the Province of British Columbia lies within the region of mountains and plateaus, the Cordillera of Western Canada, that forms the western border of the North American Continent. The extreme northeastern comer of the Province, lying east of the Cordillera, is part of the Great Plains region. The Rocky Mountain Area extends along the eastern boundary of the Province for a distance of 400 miles, and continues northwestward for an additional 500 miles entirely within the Province. The high, rugged Rocky Mountains, averaging about 50 miles in width, are flanked on the west by a remarkably long and straight valley, known as the Rocky Mountain Trench, and occupied from south to north by the Kootenay, Columbia, Canoe, Fraser, Parsnip, Finlay, Fox, and Kechika Rivers. Of these, the first four flow into the Pacific Ocean and the second four join the Mackenzie River to flow ultimately into the Arctic Ocean. -
Indian and Non-Native Use of the Bulkley River an Historical Perspective
Scientific Excellence • Resource Protection & Conservation • Benefits for Canadians DFO - Library i MPO - Bibliothèque ^''entffique • Protection et conservation des ressources • Bénéfices aux Canadiens I IIII III II IIIII II IIIIIIIIII II IIIIIIII 12020070 INDIAN AND NON-NATIVE USE OF THE BULKLEY RIVER AN HISTORICAL PERSPECTIVE by Brendan O'Donnell Native Affairs Division Issue I Policy and Program Planning Ir, E98. F4 ^ ;.;^. 035 ^ no.1 ;^^; D ^^.. c.1 Fisher és Pêches and Oceans et Océans Cariad'â. I I Scientific Excellence • Resource Protection & Conservation • Benefits for Canadians I Excellence scientifique • Protection et conservation des ressources • Bénéfices aux Canadiens I I INDIAN AND NON-NATIVE I USE OF THE BULKLEY RIVER I AN HISTORICAL PERSPECTIVE 1 by Brendan O'Donnell ^ Native Affairs Division Issue I 1 Policy and Program Planning 1 I I I I I E98.F4 035 no. I D c.1 I Fisheries Pêches 1 1*, and Oceans et Océans Canada` INTRODUCTION The following is one of a series of reports onthe historical uses of waterways in New Brunswick and British Columbia. These reports are narrative outlines of how Indian and non-native populations have used these -rivers, with emphasis on navigability, tidal influence, riparian interests, settlement patterns, commercial use and fishing rights. These historical reports were requested by the Interdepartmental Reserve Boundary Review Committee, a body comprising representatives from Indian Affairs and Northern Development [DIAND], Justice, Energy, Mines and Resources [EMR], and chaired by Fisheries and Oceans. The committee is tasked with establishing a government position on reserve boundaries that can assist in determining the area of application of Indian Band fishing by-laws. -
An#Integrated#Assessment#Of#The#Cumulative#Impacts#Of#Climate# Change'and'industrial'development'on'salmon'in'western'bc!! Stiki
An#integrated#assessment#of#the#cumulative#impacts#of#climate# change'and'industrial'development'on'salmon'in'Western'BC!! Stikine and Upper Nass Current Social-Ecological Conditions Summary Prepared by: Christina Melymick, Consultant April 2013 The views and conclusions contained in this document are those of the author and should not be interpreted as representing the opinions of the Bulkley Valley Research Centre or the Gordon and Betty Moore Foundation. [email protected] • Box 4274 Smithers, BC V0J 2N0 Canada An#integrated#assessment#of#the#cumulative#impacts#of#climate#change#and#industrial#development#on#salmon#in#Western#BC#! Acknowledgements Thank you to the Gordon and Betty Moore Foundation for supporting this project. Thank you to Jim Pojar for his expansive knowledge and expertise, and for adding to the stack of resources used during research. Thank you to Dave Bustard for taking time from a busy schedule to lend his extensive local knowledge and expertise. Thank you to John Kelson for his eulachon knowledge. Thank you to Richard Overstall for his knowledge and support. Thank you to Rick Budhwa for his support and contribution to the cultural aspects of this report. Thank you to Johanna Pfalz for her support and for providing all the relevant maps. Thank you to Ken Rabnett for support, his breadth of knowledge on the study area. Thank you to Don Morgan for the opportunity to carry out the research and produce this report, and for constant patience, guidance and support through the course of completing this report. Credits Don -
Woodland Caribou Plan for the Horseranch Subpopulation
Provincial Caribou Recovery Program Herd Planning Disclaimer The following herd plans are a result of Phase One planning and are an incomplete product. Additionally, the documents are ‘living’ reports and will be updated regularly as Phase Two progresses. Phase Two planning is currently underway for some herds however still at its early stages of development; many plans reflect this as they are in different stages along their scheduled project continuum. One of the cornerstone guiding principles to the Caribou Recovery Program (the Program) is to use consistent, fact-based approaches for all woodland caribou herds in the province. The Program has refined and adopted a new format to herd planning that will effectively: Provide a consistent approach to managing all woodland caribou herds in BC Recognize the unique circumstances of each herd Build from current (legacy) caribou management plans Consider First Nations’ and stakeholder interests and ideas Be included in larger regional plans Completed herd plans will describe the status of each herd, and the threats faced by that particular herd. The plans will take note of previous actions, and actions that are planned to take place in the future. As we implement the herd plans, the Program will carefully monitor to which extent and magnitude the caribou respond, and modify its actions as accordingly. Herd plans will help us document our decisions and discuss issues with First Nations and with stakeholders. Phase One consisted of: Status of herd or sub-population Identified threats Literature Previous work completed Phase Two will consist of input from: . Engagement with Indigenous communities . Provincial Caribou Science Team . -
MANAGEMENT PLAN November 2003
MANAGEMENT PLAN November 2003 for Stikine Country Protected Areas Mount Edziza Provincial Park Mount Edziza Protected Area (Proposed) Stikine River Provincial Park Spatsizi Plateau Wilderness Provincial Park Gladys Lake Ecological Reserve Ministry of Water, Land Pitman River Protected Area and Air Protection Environmental Stewardship Chukachida Protected Area Division Skeena Region Tatlatui Provincial Park Stikine Country Protected Areas M ANAGEMENT LAN P November 2003 Prepared by Skeena Region Environmental Stewardship Division Smithers BC Stikine Country Protected Areas Management Plan National Library of Canada Cataloguing in Publication Data British Columbia. Environmental Stewardship Division. Skeena Region. Stikine Country Protected Areas management plan Cover title: Management plan for Stikine Country Protected Areas. Issued by: Ministry of Water, Land and Air Protection, Environmental Stewardship Division, Skeena Region. “November 2003” “Mount Edziza Provincial Park, Mount Edziza Protected Area (Proposed), Stikine River Provincial Park, Spatsizi Plateau Wilderness Provincial Park, Gladys Lake Ecological Reserve, Pitman River Protected Area, Chukachida Protected Area, Tatlatui Provincial Park”—Cover. Also available on the Internet. Includes bibliographical references: p. ISBN 0-7726-5124-8 1. Protected areas - British Columbia – Stikine Region. 2. Provincial parks and reserves - British Columbia – Stikine Region. 3. Ecosystem management - British Columbia – Stikine Region. I. British Columbia. Ministry of Water, Land and Air Protection. -
Current and Future Snow Avalanche Threats and Mitigation Measures in Canada
CURRENT AND FUTURE SNOW AVALANCHE THREATS AND MITIGATION MEASURES IN CANADA Prepared for: Public Safety Canada Prepared by: Cam Campbell, M.Sc.1 Laura Bakermans, M.Sc., P.Eng.2 Bruce Jamieson, Ph.D., P.Eng.3 Chris Stethem4 Date: 2 September 2007 1 Canadian Avalanche Centre, Box 2759, Revelstoke, B.C., Canada, V0E 2S0. Phone: (250) 837-2748. Fax: (250) 837-4624. E-mail: [email protected] 2 Department of Civil Engineering, University of Calgary, 2500 University Drive NW. Calgary, AB, Canada, T2N 1N4, Canada. E-mail: [email protected] 3 Department of Civil Engineering, University of Calgary, 2500 University Drive NW. Calgary, AB, Canada, T2N 1N4, Canada. Phone: (403) 220-7479. Fax: (403) 282-7026. E-mail: [email protected] 4 Chris Stethem and Associates Ltd., 120 McNeill, Canmore, AB, Canada, T1W 2R8. Phone: (403) 678-2477. Fax: (403) 678-346. E-mail: [email protected] Table of Contents EXECUTIVE SUMMARY This report presents the results of the Public Safety Canada funded project to inventory current and predict future trends in avalanche threats and mitigation programs in Canada. The project also updated the Natural Resources Canada website and map of fatal avalanche incidents. Avalanches have been responsible for at least 702 fatalities in Canada since the earliest recorded incident in 1782. Sixty-one percent of these fatalities occurred in British Columbia, with 13% in Alberta, 11% in Quebec and 10% in Newfoundland and Labrador. The remainder occurred in Ontario, Nova Scotia and the Yukon, Northwest and Nunavut Territories. Fifty-three percent of the fatalities were people engaged in recreational activities, while 18% were people in or near buildings, 16% were travelling or working on transportation corridors and 8% were working in resource industries. -
Lithostratigraphy, Palynostratigraphy, and Sedimentology of the Northern Skeena Mountains and Their Implications to the Tectonic
LITHOSTRATIGRAPHY, PALYNOSTRATIGRAPHY, AND SEDIMENTOLOGY OF THE NORTHERN SKEENA MOUNTAINS AND THEIR IMPLICATIONS TO THE TECTONIC HISTORY OF THE CANADIAN CORDILLERA By HARRISON OWEN COOKENBOO B.Sc. Duke University 1981 A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS OF THE DEGREE OF MASTER;? OF SCIENCE in THE FACULTY OF GRADUATE STUDIES Department of Geological Sciences We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA April 1989 Harrison Owen Cookenboo, 1989 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department The University of British Columbia Vancouver, Canada DE-6 (2/88) ABSTRACT: The Skeena Mountains of north-central British Columbia contain exposures of more than 4500 m of Jura-Cretaceous strata deposited in the Bowser Basin. These strata were deposited as a result of tectonism that formed the Canadian Cordillera, and serve as a record of the tectonic history of the Cordillera. The strata of the north-central Bowser Basin have been the subject of an integrated lithostratigraphic, palynostratigraphic and sedimentologic study in order to better understand the depositional history of the basin and the tectonic history of the Cordillera. -
Article Is Available Online USA, 2004
The Cryosphere, 10, 639–664, 2016 www.the-cryosphere.net/10/639/2016/ doi:10.5194/tc-10-639-2016 © Author(s) 2016. CC Attribution 3.0 License. Numerical simulations of the Cordilleran ice sheet through the last glacial cycle Julien Seguinot1,2,3, Irina Rogozhina3,4, Arjen P. Stroeven2, Martin Margold2, and Johan Kleman2 1Laboratory of Hydraulics, Hydrology and Glaciology, ETH Zürich, Zürich, Switzerland 2Department of Physical Geography and the Bolin Centre for Climate Research, Stockholm University, Stockholm, Sweden 3Helmholtz Centre Potsdam, GFZ German Research Centre for Geosciences, Potsdam, Germany 4Center for Marine Environmental Sciences, University of Bremen, Bremen, Germany Correspondence to: Julien Seguinot ([email protected]) Received: 21 June 2015 – Published in The Cryosphere Discuss.: 7 August 2015 Revised: 2 February 2016 – Accepted: 19 February 2016 – Published: 16 March 2016 Abstract. After more than a century of geological research, 1 Introduction the Cordilleran ice sheet of North America remains among the least understood in terms of its former extent, volume, and dynamics. Because of the mountainous topography on During the last glacial cycle, glaciers and ice caps of the which the ice sheet formed, geological studies have often had North American Cordillera have been more extensive than only local or regional relevance and shown such a complexity today. At the Last Glacial Maximum (LGM), a continuous that ice-sheet-wide spatial reconstructions of advance and re- blanket of ice, the Cordilleran ice sheet (Dawson, 1888), treat patterns are lacking. Here we use a numerical ice sheet stretched from the Alaska Range in the north to the North model calibrated against field-based evidence to attempt a Cascades in the south (Fig.1). -
Belted Kingfisher
Belted King fisher Megaceryle alcyon Laure Wilson Neish lower abundance) occur across the wetland-studded plateaus of Characteristics and Range This spectacular, large kingfisher the Central Interior and Sub-boreal Interior ecoprovinces. with its outrageous "Mohawk" crest and startling staccato rattling call is one of North America's most widespread birds. It Belted Kingfishers prefer clear, fresh or salt water wetlands, breeds across the continent from the Low Arctic south to the especially with rocky shoals and shallower fast-flowing sections, United States Southern Coastal Plains and arid southwest. It is a in close proximity to natural or man-made exposed banks where partial migrant; northern breeders migrate south to winter in they can excavate nest burrows, and with abundant perches from ice-free areas, some moving as far as Central America and the which they can forage for prey, chiefly fish, but also crayfish and Caribbean (Kelly et al. 2009). other larger aquatic invertebrates. Distribution, Abundance, and Habitat The Atlas surveys show Conservation and Recommendations The Breeding Bird Survey the Belted Kingfisher is still widespread throughout the province; shows a long-term decrease in Belted Kingfishers, across Canada comparison with The Birds of British Columbia indicates there and in British Columbia; reasons for the decline are not well has been no appreciable change in distribution, provincially or understood, but declining habitat quality, contaminants, locally, over the past two decades. reduction in available nest sites (especially man-made sites like gravel pits, road cuts and quarry sites), and human disturbance The Probability of Observation model highlights several most are all potential contributors. -
Rangifer Tarandus Caribou) in BRITISH COLUMBIA
THE EARLY HISTORY OF WOODLAND CARIBOU (Rangifer tarandus caribou) IN BRITISH COLUMBIA by David J. Spalding Wildlife Bulletin No. B-100 March 2000 THE EARLY HISTORY OF WOODLAND CARIBOU (Rangifer tarandus caribou) IN BRITISH COLUMBIA by David J. Spalding Ministry of Environment, Lands and Parks Wildlife Branch Victoria BC Wildlife Bulletin No. B-100 March 2000 “Wildlife Bulletins frequently contain preliminary data, so conclusions based on these may be sub- ject to change. Bulletins receive some review and may be cited in publications. Copies may be obtained, depending upon supply, from the Ministry of Environment, Lands and Parks, Wildlife Branch, P.O. Box 9374 Stn Prov Gov, Victoria, BC V8W 9M4.” © Province of British Columbia 2000 Canadian Cataloguing in Publication Data Spalding, D. J. The early history of woodland caribou (Rangifer tarandus caribou) in British Columbia (Wildlife bulletin ; no. B-100) Includes bibliographical references : p. 60 ISBN 0-7726-4167-6 1. Woodland caribou - British Columbia. 2. Woodland caribou - Habitat - British Columbia. I. British Columbia. Wildlife Branch. II. Title. III. Series: Wildlife bulletin (British Columbia. Wildlife Branch) ; no. B-100 QL737.U55S62 2000 333.95’9658’09711 C00-960085-X Citation: Spalding, D.J. 2000. The Early History of Woodland Caribou (Rangifer tarandus caribou) in British Columbia. B.C. Minist. Environ., Lands and Parks, Wildl. Branch, Victoria, BC. Wildl. Bull. No. 100. 61pp. ii DISCLAIMER The views expressed herein are those of the author(s) and do not necessarily represent those of the B.C. Ministry of Environment, Lands and Parks. In cases where a Wildlife Bulletin is also a species’ status report, it may contain a recommended status for the species by the author. -
Selecting Plants for Pollinators Selecting Plants for Pollinators
Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Columbia Mountains and Highlands ecoregion Revelstoke, Nelson, Blue River, Wells, and Creston Table of CONTENTS Why Support Pollinators? 4 Getting Started 5 Columbia Mountains and Highlands 6 Meet the Pollinators 8 Plant Traits 10 Developing Plantings 12 Farms 13 Public Lands 14 Home Landscapes 15 Plants That Attract Pollinators 16 Notes 21 Habitat hints 22 Habitat and Nesting requirements 23 This is one of several guides for S.H.A.R.E. 24 different regions of North America. We welcome your feedback to assist us in making the future guides Checklist 24 useful. Please contact us at [email protected] Resources and Feedback 25 2 Selecting Plants for Pollinators Selecting Plants for Pollinators A Guide for Gardeners, Farmers, and Land Managers In the Columbia Mountains and Highlands Ecoregion Revelstoke, Nelson, Blue River, Wells, and Creston A NAPPC and Pollinator Partnership Canada™ Publication Columbia Mountains and Highlands 3 Why support pollinators? IN THEIR 1996 BOOK, THE FORGOTTEN POLLINATORS, Buchmann and Nabhan estimated that animal pollinators are needed for the reproduction “Flowering plants of 90% of fl owering plants and one third of human food crops. Each of us depends on these industrious pollinators in a practical way to provide us with the wide range of foods we eat. In addition, pollinators are part of the intricate across wild, web that supports the biological diversity in natural ecosystems that helps sustain our quality of life. farmed and even Abundant and healthy populations of pollinators can improve fruit set and quality, and increase fruit size. -
Landforms of British Columbia 1976
Landforms of British Columbia A Physiographic Outline bY Bulletin 48 Stuart S. Holland 1976 FOREWORD British Columbia has more variety in its climate and scenery than any other Province of Canada. The mildness and wetness of the southern coast is in sharp contrast with the extreme dryness of the desert areas in the interior and the harshness of subarctic conditions in the northernmost parts. Moreover, in every part, climate and vegetation vary with altitude and to a lesser extent with configuration of the land. Although the Province includes almost a thousand-mile length of one of the world’s greatest mountain chains, that which borders the north Pacitic Ocean, it is not all mountainous but contains a variety of lowlands and intermontane areas. Because of the abundance of mountains, and because of its short history of settlement, a good deal of British Columbia is almost uninhabited and almost unknown. However, the concept of accessibility has changed profoundly in the past 20 years, owing largely to the use of aircraft and particularly the helicopter. There is now complete coverage by air photography, and by far the largest part of the Province has been mapped topographically and geologically. In the same period of time the highways have been very greatly improved, and the secondary roads are much more numerous. The averagecitizen is much more aware of his Province, but, although knowledge has greatly improved with access,many misconceptions remain on the part of the general public as to the precise meaning even of such names as Cascade Mountains, Fraser Plateau, and many others.