Koote Nay National

Total Page:16

File Type:pdf, Size:1020Kb

Koote Nay National KOOTENAY One of the famous landmarks of Kootenay Park varied. The terrain of mountains, glaciers, alpine is Marble Canyon, approximately 53 miles north meadows, slopes, river valleys and lakes supplies NATIONAL PARK of Radium Hot Springs. The canyon was formed by many habitats, each with its distinctive association the waters of Tokumm Creek eroding the rock at a BRITISH COLUMBIA of plants and animals. KOOTE NAY shattered break in the earth's crust. One of the The effect of altitude on plant growth is easily Location major breaks or faults here is the Stephen-Denis seen. The lower transitional forests of lodgepole Kootenay National Park is situated on the fault. pine, blue Douglas fir, western red cedar, trembling western slopes of the Rockies in southeastern The Ochre Beds, or "paint pots", are also in this aspen, black cottonwood and a few Engelmann British Columbia, 107 miles north of the City of area. Springs bring this peculiar colouration of iron spruce soon give way, as one travels upward, to the NATIONAL Cranbrook. It includes the remarkable scenic val­ oxide to the surface, staining everything they cover sub-alpine forest of Engelmann spruce and alpine leys of the Kootenay and Vermilion Rivers. The with the rusty-red hue. Miners once hauled this fir, in which lodgepole pine and blue Douglas fir Park is a region 543 square miles in area notable coloured rock to the railway and sold it as a base are very minor elements. for snowcapped peaks and glaciers whose melt- for paint. There are many other kinds of trees in these PARK waters pour down rock faces and canyons into Radium Hot Springs are the result of surface forests. Some of these are water birch, western broad valleys with forested slopes. waters seeping deep along the Redwall fault to very white birch, rocky mountain juniper and western Kootenay National Park is one of Canada's 19 hot rock masses. The steam rises through cracks white spruce. BRITISH COLUMBIA National Parks which form a chain of nature and fissures, condenses into water, and returns to At timberline the forests end and the true alpine sanctuaries extending from Mount Revelstoke in the surface as hot water. flowers, in all their variety and colour, become the British Columbia to Terra Nova in Newfoundland. The Park is particularly noted for its icefields, dominating attraction. These Parks have been established for the preser­ towering glaciers, and the magnificent rock basin Many shrubs are as attractive as the trees or vation of selected areas in their natural state for lakes along the lofty peaks of the continental divide. other vegetation—at times dominating the land­ the benefit, education and enjoyment of present The rugged eastern escarpment of Vermilion Range scape with their colours. A few are serviceberry or and future generations of Canadians. is known as the "Rock Wall". The Banff-Winder­ saskatoon berry, ground juniper, buffalo berry, For thousands of years this stream has been eroding labrador tea, mountain alder, rusty menziesia, the walls of Marble Canyon. This vast area of more than 29,000 square mere Highway and many miles of trails provide white mountain rhododendron, and oval-leaved miles is administered by the National and Historic convenient access to these areas of unspoiled nature. blueberry. Many kinds of willows are present and Wildlife Parks Branch, Department of Indian Affairs and Plantlife some like the Barratt's willow have very large, The Park supports a large variety of animal life Northern Development. Evergreen forests clothe the mountains and val­ attractive catkins. but unless you have learned how to observe the leys. The vegetation of the Park is luxuriant and NATURAL FEATURES The wildflower display of the Park is a sight to smaller animals, such as the cinereous shrew, Geological behold. If one had to study and pick out each kind jumping mouse, white-footed mouse, and meadow separately the variety would be bewildering. You vole, you will see only the large ones. An incomplete This Park borders a 65-mile section of the Banff- will find them, each in its particular place or habitat list includes wapiti or American elk, black bear, Windermere Highway between the Columbia Valley whether it be in the lowest river valley or on the grizzly bear, moose, white-tailed deer, mountain and Vermilion Pass on the Continental Divide. The edges of a high glacier. No matter where a par­ lion, mule deer, bighorn sheep, mountain goat, highway crosses Brisco, Mitchell, and Vermilion ticular flower or plant lives, you can usually travel coyote, wolverine, lynx, beaver, red squirrel, Ranges and two passes, Sinclair (4,875 feet) and easy trails to reach and see it. golden-mantled ground squirrel, hoary marmot, Vermilion (5,416 feet). The Vermilion and Koot­ and pika. enay Rivers drain through this region. Only a few of the wildflowers will be mentioned. They are all gems when found singly or in masses All National Parks are wildlife sanctuaries in The rocks, especially through the Sinclair Pass blanketing a mountain slope or alpine meadow. which neither hunting or trapping is permitted. area, present a perplexing series of problems to Even their names promise visual pleasure—mari- Under these conditions some animals which you geologists. Exposed rock formations range from posa lily, purple clematis, dwarf Canadian prim­ may observe, especially along the highways, often the Lower Cambrian to Middle Devonian in age. rose, western anemone, white globe-flower, appear quite tame. This attitude in wild animals is These rocks were formed up to 550 million years balsam-root, avalanche or snow lily, yellow quite deceptive however, and bears especially are ago and were exposed by the upheavals that lifted Evergreen forests fill the Simpson River Valley and mountain-avens, alpine saxifrage, butterwort and not to be trusted. Under no circumstances should a up the Rocky Mountains in more recent geological clothe its slopes to treeline. Venus'-slipper orchid. bear or other animal be fed or approached closely. times. Some animals may be seen more easily from of nature. A walk along a quiet stream or up the Preservation certain vantage points; consult the Park Wardens slopes to timberline will reveal different facets of National Parks are selected areas set apart as if you need advice on getting a good view of wildlife. natural history. A trip into the high country will nature sanctuaries and special care is taken to Mountain goat frequently display their agility reward the visitor with an unequaled view of the maintain them in their natural state. For this on the slopes of Mount Wardle, while bighorn tops of the mountains. Massive peaks and glaciers reason all birds, animals, wildlife, trees, rocks and sheep visit the vicinity of Radium Hot Springs glistening in the clear mountain air provide a panor­ throughout the year. ama of geological features not soon forgotten. fossils are to remain undisturbed. Even the wild- flowers are not to be picked; they are to be left for Birdlife GENERAL INFORMATION others to enjoy. Feeding, touching or molesting wild Like plants and other animals, birds frequent animals is not permitted. This is in the interests of habitats of their choice and must be looked for in Park Administration the animal, as well as the human who could re­ these places. Some of the common birds found at A resident Superintendent is in charge at the ceive serious injury. lower elevations in the transitional forest of lodge- Park Office near Radium Junction. Park War­ Please help protect your own Park for future pole pine and blue Douglas fir are red-shafted Barrow's Goldeneye, one of the ducks dens stationed in the three districts of the Park enjoyment. It is part of your national inheritance. nicker, yellow-bellied sapsucker, western wood seen in the Park. are responsible for the protection of all natural pewee, mountain bluebird, tree-swallow, warbling Prevent Fire features and for the safety and guidance of visi­ vireo, western tanager, red-eyed vireo, dusky Campfires may be kindled only in fireplaces How You Can Learn More About the Park tors. A detachment of the Royal Canadian Moun­ flycatcher, Oregon junco, pine siskin, audubon provided for this purpose and must be completely ted Police assists in the maintenance of law and Numa Creek Valley—from Marble Canyon. warbler, spruce grouse and Cassin's finch. To help you know the Park better and obtain extinguished before campers leave the site. Visitors order. greater enjoyment from your visit, the National observing an unattended fire should attempt to The sub-alpine forest of Engelmann spruce and Season alpine fir is home to such distinctive birds as boreal Parks provide an Interpretation Service. This in­ extinguish it if possible and promptly report it to chickadee, Tennessee warbler, Lincoln sparrow, cludes conducted tours and nature talks illustrated Camping the nearest Park employee. Fire in a National Park The Aquacourt and the Banff-Windermere with coloured slides and films to explain the pur­ can cause damage that cannot be repaired in a Highway are open all year but the main visitor hermit thrush, varied thrush, ruby-crowned kinglet, Within the Park there are five campgrounds pose and the natural phenomena of the Park. hundred years. season is between early June and late September. Canada or gray jay, Bohemian waxwing and adjacent to the highway and one on a bench of evening grosbeak. The evening programs are presented at different locations according to a seasonal schedule. Redstreak Mountain near Radium Hot Springs. Mountain Climbing Some of the birds characteristic of the high alp- Redstreak, McLeod Meadows and Marble Canyon Well marked nature trails are maintained for For the protection of mountain climbers, all lands, above timberline, are white-tailed ptarmigan, campgrounds are fully serviced and camping fees convenient access< to unspoiled natural areas as mountain travel off the Park trails must be reg­ water pipit, grey-crowned rosy finch, and golden are charged.
Recommended publications
  • Kootenay National Park Visitor Guide
    Visitor Guide 2021 – 2022 Paint Pots Trail Également offert en français Z. Lynch / Parks Canada 1 Welcome Welcome 2 Plan your adventure 3 Be a responsible visitor 4 Radium Hot Springs area Kootenay 6 Kootenay National Park map National Park 8 Make the most of your visit 10 Camping On April 21, 1920, the Government of Canada agreed to build a road connecting the Bow and Columbia 10 Interpretive programs and activities valleys. As part of the agreement, eight kilometres of land on either side of the road was set aside for a 11 Stay safe national park. 12 Conservation stories The first cars to travel along the new highway bounced over bumps and chugged up steep hills, 13 National park regulations but according to a 1924 guidebook, “every mile is a surprise and an enchantment.” A century later, Kootenay National Park continues to surprise and enchant. Visitors can relax in the soothing mineral pools at Radium Hot Springs, stroll through canyons, picnic beside glacial-blue rivers or backpack along one of the Rockies’ most scenic hiking trails. The park’s diverse ecosystems support a variety of wildlife, and newly unearthed Burgess Shale fossils reveal exquisite details about life half a Did you know? billion years ago. Kootenay National Park lies within the traditional lands of the Ktunaxa and Shuswap. Vermilion Crossing Z. LynchIconic / Parks 55 Canada km backcountry route: Z. Lynch / Parks Canada Rockwall Trail Z. Lynch / Parks Canada Ktunaxa Nation Shuswap Indian Band Columbia Valley Métis Association A place of global importance The Ktunaxa (k-too-nah-ha), also known as The Kenpesq’t (ken-pesk-t) community, currently Kootenay National Park is an important place for The United Nations Educational, Scientific, and Kootenay, have occupied the lands adjacent to the known as the Shuswap Indian Band, is part of the British Columbia Métis based on a history of trade Cultural Organization (UNESCO) recognizes four Kootenay and Columbia Rivers and the Arrow Lakes Secwépemc (seck-wep-em) Nation occupying relationships and expeditions.
    [Show full text]
  • Bc7 Report.Pdf
    ROGER DUHAMEL, F.R.S.C. QUEEN’S PRINTER AND CONTROLLER OF STATIONERY OTTAWA, 1961’ Cat. No. A57-417 ACKNOWLEDGMENTS The British Columbia Department of Agriculture surveyed the soils of the Upper Columbia River valley. The Water Resources Branch, Department of Northern Affairs and National Resources, provided financial assistance, maps and aerial photographs. The Provincial Department of Lands and Forests also supplied maps and data. The Provincial Department of Mines provided chemical analyses. The Canada Department of Agriculture drafted the final copy of the soi1 map for lithographing and published this report. Dr. A. Leahey, Research Branch, Canada Department of Agriculture, assisted in the classification and correlation of the soils and critically reviewed the manuscript. Over a number of years the soils were mapped by P. N. Sprout, A. J. Green, A. L. van Ryswyk, J. D. Lindsay and J. S. D. Smith. The late Dr. W. E. Cockfield, Geological Survey of Canada, made annual field visits and provided information regarding the deposits from which the soils were derived. Mr. A. McLean, Ecologist, Canada Range Experimental Farm, Kamloops, wrote the section on native vegetation. Dr. C. A. Rowles, Professor of Soi1 Science, University of British Columbia,. made field visits and gave valuable advice. The British Columbia Department of Agriculture Reclamation Committee, of which the senior author is secretary, estimated the farm duty of water of each potentially irrigable soi1 type. Mr. J. W. Awmack, District Agriculturist, Cranbrook, and other officiais of the British Columbia and Canada departments of agriculture provided advice, descriptive material, and other assistance. 3 96489-O-l& CONTENTS PAGE LIST OF ILLUSTRATIONS .......................................
    [Show full text]
  • Ecology & Wonder in the Canadian Rocky Mountain Parks World Heritage Site
    Ecology & Wonder Ecology & Wonder in the Canadian Rocky Mountain Parks World Heritage Site Robert William Sandford Frontispiece: The © 2010 Robert W. Sandford Grand Sentinel The Grand Sentinel is a great Published by AU Press, Athabasca University stone tower located just below 1200, 10011 – 109 Street the summit of Sentinel Pass in Edmonton, AB T5J 3S8 Banff National Park. Were it located outside of the dense cluster of astounding natural Library and Archives Canada Cataloguing in Publication features contained within Canada’s mountain parks, it Sandford, Robert W. would be one of the wonders of Ecology & wonder in the Canadian Rocky Mountain Parks World Heritage the world. As it is, it is just one Site / Robert William Sandford. more landscape miracle that can be seen from the summit Includes bibliographical references and index. of the pass. Issued also in electronic format (978-1-897425-58-9). Photograph by R.W. Sandford. ISBN 978-1-897425-57-2 1. Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.)--Environmental conditions. 2. National parks and reserves--Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.)--Management. 3. Environmental protection--Canadian Rocky Mountain Parks World Heritage Site (Alta. and B.C.). I. Title. II. Title: Ecology and wonder. QH106.2.R6S26 2010 333.7’209712332 C2010-900473-6 Cover and book design by Virginia Penny, Interpret Design, Inc. Printed and bound in Canada by Marquis Book Printing. This publication is licensed under a Creative Commons License, Attribution- Noncommercial-No Derivative Works 2.5 Canada, see www.creativecommons.org. The text may be reproduced for non-commercial purposes, provided that credit is given to the original author.
    [Show full text]
  • Canoeing, Kayaking Or Rafting from .•
    ·· .. '. · .. ·· . ·._ ·. ,, canoeing, kayaking or rafting from .•. ·.. .· .. Vermilion Crossing ·· ·•· to Canal Flats ·. ·. ·· .. :.· ·.. INTRODUCTION Using this Pamphlet The section of the Vermilion/Kootenay River System between This pamphlet is intended to assist in planning a river trip. It can also Vermilion Crossing in Kootenay National Park and Canal Flats, be used as an information guide to be taken down the river. It is Bfitish Columbia provides superb opportunities tor canoeing, printed on water-proof paper and can be tied into your boat using the kayaking and rafting. There are lots of rapids, beautiful scenery, hole punched on the upper left corner. good camping opportunities and easy access. No responsibility can be assumed for the misuse of this information The Vermilion River upstream of Vermilion Crossing is not nor the failure of individuals to adequately assess their paddling recommended. It contains a number of waterfalls and chutes. The ability. River conditions may change considerably with water levels. Kootenay River downstream of Canal Flats is slow flowing. Wetland The decision to run this river system, reach or rapid, therefore rests areas along this downstream section provide habitats for a variety of solely with the individual. We hope the pamphlet will help paddlers to birds and wildlife. enjoy this beautiful river system. This pamphlet describes a 168 km section of the river system which has been broken into three portions - or in river talk - reaches. An Access explanation of the river and rapid rating system used in the river Highways 93 and 95 provide easy access to the river between guide is found on page 4.
    [Show full text]
  • Getting Around Kootenay National Park 2019 - 2020
    Getting around Kootenay National Park 2019 - 2020 Également offert en français Stanley Glacier, Burgess Shale Fossils Guided Hike Zizka P. Connect with nature Destination BC/Kari Medig Our story Indigenous peoples were the first to discover and for thousands of years, use naturally forming ochre in small streams flowing through the Vermilion Plain. More recently, nineteenth century prospectors followed, mining the ochre by hand to create pigment for paint. The Paint Pots lie near the north end of the Banff-Windermere Highway (93), the road that runs through Kootenay National Park. M. Oliver The highway, completed in 1923, was conceived to draw tourists to the picturesque scenes on either A UNESCO World Heritage Site side of the road, while opening commercial links east of the Rockies. Kootenay is the only national Four of the mountain national parks—Banff, Jasper, park to feature both glacier-clad peaks along the Yoho, and Kootenay—are recognized by the Continental Divide and semi-arid grasslands in the United Nations Educational, Scientific and Cultural Columbia Valley. Organization as part of the Canadian Rocky Apart from ochre deposits, Kootenay boasts a Mountain Parks World Heritage Site, for the benefit geological heritage to inspire any artist – from and enjoyment of all nations. Burgess Shale fossils to the dolomite walls of Marble Among the attributes that warranted this designation Canyon and the rust covered cliffs above Radium were vast wilderness, diversity of flora and fauna, Hot Springs. In 2003, wildfires in the Vermillion Valley outstanding natural beauty and features such as revealed glaciers hanging above the flame-scorched Lake Louise, Maligne Lake, the Columbia Icefield, forest, further enhancing the park’s natural legacy.
    [Show full text]
  • KOOTENAY NATIONAL PARK Mftte BANFF WINDERMERE HIGHWAY Kootenay National Park the Banff Windermere Highway
    KOOTENAY NATIONAL PARK mftte BANFF WINDERMERE HIGHWAY Kootenay National Park The Banff Windermere Highway 6y M.B.WILLIAMS F. A. ACLAND Printer to the King's Most Excellent Majesty Ottawa. 1928 SKETCH MAP -* OF THE *- BANFF-WINDERMERE ROAD CASTLE TO RADIUM HOT SPRINGS SECTION Motor Camp! shown thus Gas Stations . •• - - OTOR highway across the Central Cana- Bienaalow Camps • p .. I dian Rockies from Banff via Vermilion Motor Roeeets i n.. Pass to Windermere Valley, passing through Trails a ••- M= " ^ Rocky Mountains and Kootenay National MILEAGE CHART Parks and giving access to the famous resorts; Banff, CtltMtn hVemilim Summit 10 lt\\n Lake Louise, Valley of the Ten Peaks, Moraine Lake, VtrmilionSummittoMomLCanysii 50 • Mirble Canyon to Black's Camp 5' 3 ' Paradise Valley, Marble Canyon and Sinclair Radium Black's Camp to tUk Crook 4T • Hot Springs. Hawk Crook to Vermilion Crajjuig 5 6 * Vermilion Crossing to Simpoon River. .4'5 ' Direct connections from Spokane, Seattle, Vancou­ 5impsonRivertoWarJle Creek M) • Wardle Creek toKcote'iayCroMino .7 '6 " ver and Victoria, Portland, San Francisco and Los Koo+enayCroMinnto McLeodMeaaCnvs 11 "0 " Angeles with Banff-Windermere Highway on west, McLeoct MeaeloivotoSineljjrjnmmit 9 T " 5iwW5«mmiHaCclumaiiVdlllyRoaa 8 '5 * via Invermere, Cranbrook and Kingsgate, B.C., and CootieMta to Colnmlia Valley Road.. 72'9 Milts on the east from Grand Canyon, Salt Lake City, Colicmb.aValLy Rooa to F,rlands5to 1 • 2 Mile! Helena, the Yellowstone and Glazier National Parks via Coutts or Piegan, Mont., and Lethbridge or Cardston, Alta., to Calgary, the Gateway to the Central Rockies. Extension loop route through southern Cana­ dian Rockies via the Crowsnest Pass, giving access to Waterton Lakes National Park, and also from Lake Louise over famous Kicking Horse Pass through Central Rockies passing through Yoho National Park and visiting Field, Yoho Valley, Emerald Lake, and via the spectacular Kicking Horse Canyon, Golden, B.C., and Columbia River Road.
    [Show full text]
  • 93S Area Plan Consultation Summary.Indd
    Kootenay Parc national National Park Kootenay www.parkscanada.gc.ca www.parcscanada.gc.ca Highway 93 South Area Plan Summary Summer 2011 Kootenay National Park, British Columbia Highway 93 South, a 104 km, two-lane scenic highway stretching from Castle Junction to Radium Hot Springs, provides a vital transportation link between Alberta and the Columbia Valley. The road also known as the Banff-Windermere Highway was built as part of an agreement between the federal and provincial governments that established Kootenay National Park in 1920. The road was opened in 1922, becoming the fi rst motor road to cross the central Canadian Rockies. The Highway 93 South corridor is the main focus of visitor activity in Kootenay National Park. In accordance with direction in the Kootenay National Park Management Plan 2010, a draft area plan has been developed for the Kootenay Corridor that addresses ecological issues, visitor experience and education opportunities along Highway 93 South from the Continental Divide to Sinclair Pass. A separate area plan will be developed for the park gateway in the Radium-Sinclair Canyon area. This newsletter provides a summary of key concepts and proposals that are contained in the draft plan. Parks Canada welcomes any comments or suggestions on this material. All input received will be carefully considered during the preparation of the fi nal area plan. Welcoming Visitors to Kootenay National Park The plan proposes the development of a small new day use area on the west side of the highway to provide a sense of arrival for visitors entering the park from Alberta.
    [Show full text]
  • Basinwide Summary: December 1, 2017 (Averages/Medians Based On
    Basinwide Summary: December 1, 2017 Snowpack Summary for December 1, 2017 (Averages/Medians based on 1981-2010 reference period) Elevation Depth SWE Median % Last Year Last Year KOOTENAY in CANADA Network (ft) (in) (in) (in) Median SWE (in) % Median Larch Valley SC 7316 Floe Lake SC 6847 Sunshine Village SC 7316 Mount Assiniboine SC 7316 Sinclair Pass SC 4508 Mount Joffre SC 5784 Lost Creek SC 7087 Thunder Creek SC 6765 Gardiner Headwaters SC 6463 Allison Pass SC 6496 Morrissey Ridge Pillow SC 5906 3.8 4.0 Fernie East SC 3980 Moyie Mountain Pillow SC 6332 3.3 2.0 Basin Index #DIV/0! # of sites 0 0 Elevation Depth SWE Median % Last Year Last Year KOOTENAI MAINSTEM Network (ft) (in) (in) (in) Median SWE (in) % Median Banfield Mountain SNOTEL 5600 11 3.7 3.4 109 1.0 29 Bear Mountain SNOTEL 5400 35 11.2 10.4 108 7.8 75 Poorman Creek SNOTEL 5100 23 6.6 6.3 105 3.0 48 Bristow Creek SC 3900 Lost Soul SC 4800 Basin Index 7.2 107 59 # of sites 3 3 Elevation Depth SWE Median % Last Year Last Year TOBACCO Network (ft) (in) (in) (in) Median SWE (in) % Median Grave Creek SNOTEL 4300 11 2.5 3.0 83 2.0 67 Stahl Peak SNOTEL 6030 27 8.3 9.2 90 13.7 149 Weasel Divide SC 5450 Basin Index 5.4 89 129 # of sites 2 2 Elevation Depth SWE Median % Last Year Last Year FISHER Network (ft) (in) (in) (in) Median SWE (in) % Median Hand Creek SNOTEL 5035 4 1.8 2.2 82 0.3 14 Baree Creek SC 5500 Baree Midway SC 4600 Baree Trail SC 3800 Brush Creek Timber SC 5000 Basin Index 1.8 82 14 # of sites 1 1 Elevation Depth SWE Median % Last Year Last Year YAAK Network (ft) (in)
    [Show full text]
  • APPENDIX G.4 Surface Water Quality and Quantity Technical Data Report
    FOOTHILLS ZONE 8 WEST PATH DELIVERY 2023 ENVIRONMENTAL AND SOCIO-ECONOMIC ASSESSMENT APPENDIX G.4 Surface Water Quality and Quantity Technical Data Report FOOTHILLS ZONE 8 WEST PATH DELIVERY 2023 ENVIRONMENTAL AND SOCIO-ECONOMIC ASSESSMENT Foothills Zone 8 West Path Delivery 2023 Surface Water Quality and Quantity Technical Data Report Revision 00 Issued for Use February 2021 Prepared for: Foothills Pipe Lines (South BC) Ltd. Calgary, Alberta Prepared by: Stantec Consulting Ltd. Calgary, Alberta FOOTHILLS ZONE 8 WEST PATH DELIVERY 2023 SURFACE WATER QUALITY AND QUANTITY TECHNICAL DATA REPORT Limitations and Sign-off This document entitled Foothills Zone 8 West Path Delivery 2023 Surface Water Quality and Quantity Technical Data Report was prepared by Stantec Consulting Ltd. (“Stantec”) for the account of Foothills Pipe Lines (South BC) Ltd. (the “Client”) to support the regulatory review process for its Section 214 Application under the Canadian Energy Regulator Act (the “Application”) for approval to construct and operate the Foothills Zone 8 West Path Delivery 2023 Project (the “Project”). In connection therewith, this document may be reviewed and used by the Canada Energy Regulator participating in the review process in the normal course of its duties. Except as set forth in the previous sentence, any reliance on this document by any other party or use of it for any other purpose is strictly prohibited. The material in it reflects Stantec’s professional judgment in light of the scope, schedule and other limitations stated in the document and in the contract between Stantec and the Client. The information and conclusions in the document are based on the conditions existing at the time the document was published and does not take into account any subsequent changes.
    [Show full text]
  • Cambrian Geology and Paleontology V
    SMITHSONIAN MISCELLANEOUS COLLECTIONS VOLUME 75. NUMBER 1 CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. 1.—GEOLOGICAL FORMATIONS OF BEAVEKFOOT- BRISCO-STANFORD RANGE, BRITISH COLUMBIA, CANADA (With Plates 1 to 8) BY CHARLES D. WALCOTT (Publication 2756) CITY OF WASHINGTON PUBLISHED BY THE SMITHSONIAN INSTITUTION JUNE 28, 1924 BALTIMORE, MD., 0. S. A. 1 CAMBRIAN GEOLOGY AND PALEONTOLOGY V No. I.—GEOLOGICAL FORMATIONS OF BEAVERFOOT- BRISCO-STANFORD RANGE, BRITISH COLUMBIA, CANADA By CHARLES D. WALCOTT (With Piatf.s i to 8) CONTENTS PAGE Introduction 3 Description of map, plate i 7 Stratigraphic sections ; 9 Sinclair Canyon Section 9 Silurian 1 Ordovician 14 Ozarkian 16 Upper Cambrian 20 Summary 21 Stoddart-Dry Creek Section 21 Ozarkian 22 Upper Cambrian 24 Summary 24 Sabine Mountain Section 25 Silurian 26 Ozarkian 27 Upper Cambrian 28 Grainger Mountain Section 29 Cambrian 30 Lower Cambrian 30 Beltian 30 Notes on Geological Formations of tbe western side of the Beaverfoot- Brisco-Stanford Range 31 Devonian 31 Silurian 32 Wonah Quartzite 32 Ordovician 32 Glenogle formation 32 Sinclair formation 34 Sarbach ? formation 35 Ozarkian 35 Mons formation 35 Smithsonian Miscellaneous Collections, Vol. 75, No. 1. I 2 SMITHSONIAN MISCELLANEOUS COLLECTIONS VOL. 75 PAGE Upper Cambrian 39 Lyell ? 39 Middle and Lower Cambrian 39 Summary - 40 Note on the extension of the pre-Devonian formations of the Beaverfoot- Brisco-Stanford Range north of Kicking Horse Canyon 40 Ordovician-Silurian Boundary 41 Disconformity at the base of the Silurian Beaverfoot formation 43 Variation in thickness of formations 44 Pre-Pleistocene formations of the floor of the Columbia River Valley (" Rocky Mountain Trench ") from Canal Flats to Golden 45 New Formation Names 47 Brisco formation 47 Beaverfoot (redefined) 48 Sabine formation 49 Wonah Quartzite ^9 Sinclair formation 50 Messines formation 50 Pipestone formation 51 ILLUSTRATIONS Plates FACING PLATE PAGE 1.
    [Show full text]
  • 35-2 Spring Cover
    Volume 35, No. 3 BRITISH COLUMBIA Summer 2002 $5.00 HISTORICAL NEWS ISSN 1195-8294 Journal of the British Columbia Historical Federation Sugar and Strike Thomas Basil Humphreys Simpcw and Secwepemc Rambling in BC in 1887 Steamboats: James W. Trahey Award Winners 2001 Stuart Thomon foto, City of Vancouver Archives CVA 99-429 CVA Archives Vancouver City of Thomon foto, Stuart Above: This photo of two anymous young women; one holding a baseball, was taken during a picnic for employees of the BC Sugar Refinery on Bowen Island. In “Not Always Sweet,” starting on page 2, Janet Nicol writes about a bitter labour dispute at Benjamin T. Rogers’s sugar refinery during the First World War. Our Web site, http://www.bchf.bc.ca, is hosted by Selkirk College in Castlegar, BC British Columbia Historical News British Columbia Historical Federation Journal of the PO Box 5254, Station B., Victoria BC V8R 6N4 British Columbia Historical Federation a charitable society under the income tax act Published Winter, Spring, Summer, and Fall. Under the Distinguished Patronage of Her Honour Editor: The Honourable Iona Campagnolo. PC, CM, OBC Fred Braches Lieutenant-Governor of British Columbia PO Box 130 Whonnock BC, V2W 1V9 Honorary President: Helen B. Akrigg, Phone 604.462.8942 Officers [email protected] President: Wayne Desrochers Book Review Editor: 13346 57th Avenue, Surrey BC V3X 2W8 Anne Yandle Phone 604. 599.4206 Fax. 604.507.4202 [email protected] 3450 West 20th Avenue First Vice President: Jacqueline Gresko Vancouver BC, V6S 1E4 5931 Sandpiper Court, Richmond BC V7E 3P8 Phone 604.733.6484 Phone 604.274.4383 [email protected] [email protected] Second Vice President: Roy J.V.
    [Show full text]
  • Visitor Guide 2020-2021
    Visitor Guide 2020 – 2021 Parks Parks Canada / Également offert en français Z. Z. Lynch Sinclair Canyon 1 Welcome 2 Plan your adventure 3 Be a responsible visitor 4 Celebrate Kootenay’s centennial 8 Radium Hot Springs area 10 Kootenay National Park map 12 Make the most of your visit 14 Interpretive programs and activities 15 Camping 17 National park regulations 18 Wildlife need your help 19 Conservation stories 20 Winter 20 Mountain national parks Did you know? Kootenay National Park lies within the traditional lands of the Ktunaxa and Shuswap. Ktunaxa Nation Shuswap Indian Band Z. Lynch / Parks Canada The Ktunaxa (k-too-nah-ha), also known The Kenpesq’t (ken-pesk-t) community, as Kootenay, have occupied the lands currently known as the Shuswap Indian adjacent to the Kootenay and Columbia Band, is part of the Secwépemc Columbia Valley Métis Association Rivers and the Arrow Lakes for more than (seck-wep-em) Nation occupying traditional Kootenay National Park is an important place 10 000 years. For thousands of years before lands in British Columbia and Alberta. for British Columbia Métis based on a history settlers arrived, the Ktunaxa harvested flora The Secwépemc people have used the areas of trade relationships and expeditions. In 1807, and fauna in the area now recognized as now encompassed by Mount Revelstoke, when Kootenae House was established as Kootenay National Park, which lies within Glacier, Yoho, Banff, Jasper and Kootenay the first trading post in the region, a meeting Kyawaȼ ʔamakʔis (Land of the Grouse). national parks for thousands of years prior to place between cultures was born.
    [Show full text]