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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. -
TREATY 8: a British Columbian Anomaly
TREATY 8: A British Columbian Anomaly ARTHUR J. RAY N THE ANNALS OF NATIVE BRITISH COLUMBIA, 1999 undoubtedly will be remembered as the year when, in a swirl of controversy, Ithe provincial legislature passed the Nisga'a Agreement. The media promptly heralded the agreement as the province's first modern Indian treaty. Unmentioned, because it has been largely forgotten, was the fact that the last major "pre-modern" agreement affecting British Columbia -Treaty 8 - had been signed 100 years earlier. This treaty encompasses a sprawling 160,900-square-kilometre area of northeastern British Columbia (Map 1), which is a territory that is nearly twenty times larger than that covered by the Nisga'a Agreement. In addition, Treaty 8 includes the adjoining portions of Alberta and the Northwest Territories. Treaty 8 was negotiated at a time when British Columbia vehemently denied the existence of Aboriginal title or self-governing rights. It therefore raises two central questions. First, why, in 1899, was it ne cessary to bring northeastern British Columbia under treaty? Second, given the contemporary Indian policies of the provincial government, how was it possible to do so? The latter question raises two other related issues, both of which resurfaced during negotiations for the modern Nisga'a Agreement. The first concerned how the two levels of government would share the costs of making a treaty. (I will show that attempts to avoid straining federal-provincial relations over this issue in 1899 created troublesome ambiguities in Treaty 8.) The second concerned how much BC territory had to be included within the treaty area. -
Proquest Dissertations
The Distribution of Woodland Caribou (Rangifer tar and us caribou) and Moose (Alces alces) in the Fort St. James Region of Northern British Columbia, 1800-1950 Domenico Santomauro B.A., University of Bologna, Italy, 2003 Thesis Submitted In Partial Fulfillment Of The Requirements For The Degree Of Master in Natural Resources and Environmental Studies The University of Northern British Columbia September 2009 © Domenico Santomauro, 2009 Library and Archives Bibliothgque et 1*1 Canada Archives Canada Published Heritage Direction du Branch Patrimoine de l'6dition 395 Wellington Street 395, rue Wellington Ottawa ON K1A0N4 Ottawa ON K1A 0N4 Canada Canada Your file Votre r6f£rence ISBN: 978-0-494-60853-1 Our file Notre reference ISBN: 978-0-494-60853-1 NOTICE: AVIS: The author has granted a non- L'auteur a accorde une licence non exclusive exclusive license allowing Library and permettant a la Bibliotheque et Archives Archives Canada to reproduce, Canada de reproduire, publier, archiver, publish, archive, preserve, conserve, sauvegarder, conserver, transmettre au public communicate to the public by par telecommunication ou par I'lnternet, preter, telecommunication or on the Internet, distribuer et vendre des theses partout dans le loan, distribute and sell theses monde, a des fins commerciales ou autres, sur worldwide, for commercial or non- support microforme, papier, electronique et/ou commercial purposes, in microform, autres formats. paper, electronic and/or any other formats. The author retains copyright L'auteur conserve la propriete du droit d'auteur ownership and moral rights in this et des droits moraux qui protege cette these. Ni thesis. Neither the thesis nor la these ni des extraits substantiels de celle-ci substantial extracts from it may be ne doivent etre imprimes ou autrement printed or otherwise reproduced reproduits sans son autorisation. -
Lt. Aemilius Simpson's Survey from York Factory to Fort Vancouver, 1826
The Journal of the Hakluyt Society August 2014 Lt. Aemilius Simpson’s Survey from York Factory to Fort Vancouver, 1826 Edited by William Barr1 and Larry Green CONTENTS PREFACE The journal 2 Editorial practices 3 INTRODUCTION The man, the project, its background and its implementation 4 JOURNAL OF A VOYAGE ACROSS THE CONTINENT OF NORTH AMERICA IN 1826 York Factory to Norway House 11 Norway House to Carlton House 19 Carlton House to Fort Edmonton 27 Fort Edmonton to Boat Encampment, Columbia River 42 Boat Encampment to Fort Vancouver 62 AFTERWORD Aemilius Simpson and the Northwest coast 1826–1831 81 APPENDIX I Biographical sketches 90 APPENDIX II Table of distances in statute miles from York Factory 100 BIBLIOGRAPHY 101 LIST OF ILLUSTRATIONS Fig. 1. George Simpson, 1857 3 Fig. 2. York Factory 1853 4 Fig. 3. Artist’s impression of George Simpson, approaching a post in his personal North canoe 5 Fig. 4. Fort Vancouver ca.1854 78 LIST OF MAPS Map 1. York Factory to the Forks of the Saskatchewan River 7 Map 2. Carlton House to Boat Encampment 27 Map 3. Jasper to Fort Vancouver 65 1 Senior Research Associate, Arctic Institute of North America, University of Calgary, Calgary AB T2N 1N4 Canada. 2 PREFACE The Journal The journal presented here2 is transcribed from the original manuscript written in Aemilius Simpson’s hand. It is fifty folios in length in a bound volume of ninety folios, the final forty folios being blank. Each page measures 12.8 inches by seven inches and is lined with thirty- five faint, horizontal blue-grey lines. -
Rainbows on the Firesteel
on RAINBOWSthe FIRESTEEL Pretty nice rainbow trout – 22 inches – LARRY’S SHORT STORIES #77 – n the wild and remote areas of western Canada, they use Son Russell and I fi shed this magnifi cent river for a couple Ithe term ‘fl y-out’ fi shing; as the only way to get you to of days – fi rst, at the outlet of the lake, where 100 fi sh per most of the best streams and lakes is to ‘fl y-out’ from base person was the expected day. Then we fi shed the main camp – in a small plane, with fl oats attached to the landing part of the river, below and between some falls, where we gear. At the end of the day’s fi shing, you fl y back and caught fewer, but bigger fi sh. Russell is a more serious make plans to fi sh a different river ‘tomorrow’ -- in another fl y fi sherman than myself. I took one fl y rod, he took fi ve. remote location. The daily plane rides between base camp Mostly we used and the fi sheries become something to look forward to, as dry fl ies and "...6,000 rainbow they provide a spectacular view of the scenery and wildlife. the fi sh would When fi shing the rivers, there are often three choices – readily take trout per mile..." each generally being a single destination for the day; you them, even if can fi sh the outlet of the lake, where the river begins, the there were no apparent rises. Everything was catch and inlet, or along the course of the river -- if the pools are release, with barbs down, but we did enjoy fresh rainbow large and deep enough to accommodate the landing trout during two different shore lunches. -
Sidenius Creek Archaeological Inventory Project: Potential Model - - - Muskwa-Kechika Management Area
SIDENIUS CREEK ARCHAEOLOGICAL INVENTORY PROJECT: POTENTIAL MODEL - - - MUSKWA-KECHIKA MANAGEMENT AREA March, 2001 Prepared for: Muskwa-Kechika Trust Fund Project # M-K 2000-01-63 Prepared by: BC Regional Office Big Pine Heritage Consulting & Research Ltd. #206-10704 97th Ave. Fort St. John, BC V1J 6L7 Credits: Report Authors – Rémi Farvacque, Jeff Anderson, Sean Moffatt, Nicole Nicholls, Melanie Hill; Report Production – Jeff Anderson, Rémi Farvacque, Sean Moffatt; Archival Research – Nicole Nicholls, Vandy Bowyer, Elvis Metecheah, Chris Wolters; Interview Personnel – Maisie Metecheah, Elvis Metecheah, Colleen Metecheah, Nicole Nicholls, Rémi Farvacque; Project Director – Rémi Farvacque ACKNOWLEDGEMENTS i We wish to thank the following individuals and groups who provided assistance, guidance, and financial support. Sincere thanks is owed to the Chief & council, staff, and members of the Halfway River First Nation (HRFN) who graciously provided us with facilities and support when conducting interviews, and to the community members who were eager to discuss this project with us. Financial support was provided by the Muskwa-Kechika Management Area Advisory Board (Project # M-K 2000-01-63). Robert Jackson (Council, HRFN) and Chris Bazant (Oil & Gas Landsperson, HRFN) provided guidance that was greatly appreciated. Ethnographic research was assisted by Elvis Metecheah & Chris Wolters, and the Treaty and Aboriginal Rights Research archives staff at Treaty 8 offices, Fort St. John, BC Assistance in the field was provided by Maisie, Elvis, and Colleen Metecheah (members of the HRFN). A thank you goes to McElhanney Land Surveyors, Fort St. John, for their expedient and generous delivery of data sets and printing services. Frontispiece: False-colour elevation model of study area. -
M.Y. Williams Fonds
M.Y. Williams fonds Compiled by Christopher Hives (1988) Last revised February 2019 University of British Columbia Archives Table of Contents Fonds Description o Title / Dates of Creation / Physical Description o Biographical Sketch o Scope and Content o Note Series Descriptions o Biographical/Personal Material series o Family History series o Publications series o Field Notebooks/Diaries series o Reports series o Manuscripts / Research Notes series o Correspondence series o Reprint series o Miscellaneous Subjects series o Maps series o Card Indexes series o Miscellaneous Printed/Published Material series o Photographs series File List Catalogue entry (UBC Library catalogue) Fonds Description M.Y. Williams fonds. – 1875-1973. 15.78 m of textual records and published materials. ca. 462 photographs: b&w; 20.5 x 25.5 or smaller. 3 albums. ca. 350 maps. Biographical Sketch From: Okulitch, V.J. "Merton Yarwood Williams (1883-1974)", Royal Society of Canada, Proceedings (Vol. 12, 1974), pp. 84-88: Professor Merton Yarwood Williams Ph.D., D.Sc., died on 3 February 1974 in Vancouver, B.C. in his ninetieth year. With his passing, the University of British Columbia lost one of its original faculty members and the geology profession lost a pioneer in stratigraphic and petroleum exploration in western Canada. "M.Y.," as he was affectionately referred to by colleagues and friends, was born near Bloomfield, Ontario, on 21 June 1883. Both his parents were of Loyalist descent and their ancestors moved to Ontario at the time of the American Revolution. He graduated from Picton High School in 1902 and then taught school for three years before deciding to enter Queen's University at Kingston. -
British Columbia Geological Survey Geological Fieldwork 1989
GEOLOGY BETWEEN NINA LAKE AND OSILINKA RIVE,R, NORTH-CENTRAL BRITISH COLUMBIA (93N/15, NORTH HALF AND 94C/2, SOUTH HALF) By Filippo Ferri and David M. Melville KEYWORDS: Regionalmapping, Germansen Landing, The northern and eastem sections of the map are bounded, Omineca Belt. Intermontane Superterrane, Slide Mountain respectively, by the Osilinka and 0mine:ca rivers. At lheir Group, Paleozoicstratigraphy, lngenika Group, metamor- confluence the terrainis a relatively subdued and tree covzred phism, lead-zinc-silr,er-baritemineralization area. This is in contrast to the Wolverine Range east oithe OminecaRiverand arugged, unnamedrangeof mountai'ls to the southwest. The southern part of the map area was first mapped at a INTRODUCTION 6-mile scale in the 1940s by Amstrong; (1949).Gahrlelse (1975) examined the northem half in the course of 1:250 000 In 1989 theManson Creek 150 000 mappingproject mapping of the east half of the Fort Grahame map area. encompassed the north half of the Germansen Landing map Monger (1973), and Monger and Patersan (1974) described area (93Ni15) and the south half of the End Lake map area rocks in the map area during a reconnaissance sunfey of (94Ci2). As with previous years, the main aims of this project Paleozoic stratigraphy. To the northwest, Roots (1954) pub- were: to provide a detailed geologicalbase map of the area, to lished a 4-mile map of the Fort Graham west-half sheet. update the mineral inventory database, and to place known Many ofthe correlations made in this paper arewith stratigra- mineral occurrences within a geological framework. phy described by Gabrielse (1963, 1969:1,Nelson and Eirad- ford (1987) and other workers in the Casiar area whera: the The centreof the map area is located some 260kilometres miogeoclinal stratigraphy is quite similar and well known. -
5247 Mackenzie
British Columbia Community Health Service Area 5247 Mackenzie Community Health Service Areas (CHSAs) in British Columbia (B.C.) are administrative bounds nested within Local Health Areas (LHAs) as defined by the B.C. Ministry of Health. This CHSA health profile contains information about the community’s demographics, socio-economic and health/disease status as represented through various community health indicators. The purpose of CHSA health profiles is to help B.C.’s primary care network partners, public health professionals and community organizations better understand the health needs of a specific community and to provide evidence for service provisioning and prevention strategies. Mackenzie (CHSA 5247) is 28,850 km² in size and is located in north central British Columbia, north of Highway 97. It is comprised of the communities of Mcleod Lake and Mackenzie, and the First Nations communities of: Tsay Keh Dene, Kwadacha, and McLeod Lake. Geographical features include Rocky Mountain Trench, Sifton Ranges, Samuel Black Range, Osilinka Ranges, Williston Lake, Omineca Mountains, and Brothers Peaks.[1] Provided by Health Sector Information, Analysis, and Reporting Division, B.C. Ministry of Health Health Authority: 5 Northern Health Service Delivery Area: 52 Northern Interior Local Health Area: 524 Prince George Community Health Service Area: 5247 Mackenzie Primary Care Network N/A community: For more information, visit communityhealth.phsa.ca 5247 MACKENZIE B.C. CHSA Health Prole Version 1.0 Demographics The age and sex distribution of the population in the community impacts the infrastructure supports and services needed in the community. For example, older adults and young families especially benefit from age-friendly public spaces, like well-maintained sidewalks and rest areas. -
Dam(N)Ing BC Or Remembering the Dam(N)Ed: Site C and Mega Dams in the Era of Contested Economies and Environments
Dam(n)ing BC or Remembering the dam(n)ed: Site C and mega dams in the era of contested economies and environments [email protected] deliberate #1? blocking/hiding part of the current Williston reservoir… ….hmmm… SiteCproject.com: initial overview map Site C: continuation of WAC Bennett Dam, Peace Canyon Dam, and Williston Reservoir Preamble... Consumers of electricity • current society needs / wants electricity • only 1% - 3% electricity load saved on Earth Hour Rivers and humans humans have manipulated rivers for millennia • Smith, N. A history of dams, 1971 • Goudie, A.S. The human impact on the natural environment: Past, present, and future (7th edition since the 1980s!) • Wohl, E. & Merritts, D.J. What is a natural river? Geography Compass, 2007 deliberate #2? Note site C reservoir location…hmmm… Vancouver, Burnaby, Richmond, Delta 1,367 sq.kms 1,773 sq.kms 93 sq.kms BC gov’t Dec.16, 2014 announcement slideshow Site C… “…is in the public interest and that the benefits provided by the project outweigh the risks of significant adverse environmental, social and heritage effects.” (BC government newsroom, October 14, 2014) cost$ to pay for electrical power Site C “…would be accompanied by significant environmental and social costs, and the costs would not be borne by those who benefit.” (p.307) “These losses will be borne by the people of the Valley… Those who benefit…will be future electricity consumers all across the province.” (p.307) (Report of the Joint Review Panel: Site C project, 2014) Site C Joint Review Panel Report, 2014 Panel’s -
British Columbia Historical Quarterly
E S. BRITISH COLUMBIA HISTORICAL QUARTERLY 4.) I. • •SS_ S • 5’: .SSS OCTOBER, 1939 5. .5 S • BRITISH COLUMBIA HISTORICAL QUARTERLY Published by the Archives of British Columbia in co-operation with the British Columbia Historical Association. EDITOR. W. KAYE LAMB. ADVISORY BOARD. J. C. GOODFELLOW, Princeton. F. W. Howay, New Westminster. R0BIE L. REID, Vancouver. T. A. RICKARD, Victoria. W. N. SAGE, Vancouver. Editorial communications should be addressed to the Editor, Provincial Archives, Parliament Buildings, Victoria, B.C. Subscriptions should be sent to the Provincial Archives, Parliament Buildings, Victoria, B.C. Price, 50c. the copy, or $2 the year. Members of the British Columbia Historical Association in good standing receive the Quarterly without further charge. Neither the Provincial Archives nor the British Columbia Historical Association assumes any responsibility for statements made by contributors to the magazine. BRITISH COLUMBIA HISTORICAL QUARTERLY “Any country worthy of a future should be interested in its past.” VOL. III. VICTORIA, B.C., OCTOBER, 1939. No. 4 CONTENTS. ARTICLES: PAGE. Pioneer Flying in British Columbia, 1910—1914. ByFrankH.EIlis — 227 The Evolution of the Boundaries of British Columbia. By Willard E. Ireland 263 Sir James Goes Abroad. By W. Kaye Lamb 283 NOTES AND COMMENTS: Contributors to this Issue__ 293 Historic Sites and Monuments — 293 British Columbia Historical Association _-__ 296 Okanagan Historical Society 298 Similkameen Historical Association — 299 Thompson Valley Museum and Historical Association _ 299 ThE NORTHWEST BOOKSHELF: Morton: A History of the Canadian West to 1870—71. By W. N. Sage _301 Index — 305 The McMullen-Templeton machine, which waa completed in April, 1911. -
Paper 08 (Colour).Vp
Toodoggone Geoscience Partnership: Preliminary Bedrock Mapping Results from the Swannell Range: Finlay River – Toodoggone River Area (NTS 94E/2 and 7), North-Central British Columbia1 By L. Diakow, G. Nixon, B. Lane and R. Rhodes KEYWORDS: P3, public-private partnership, Targeted Toodoggone River in the north and east (Fig. 1). The new Geoscience Initiative II (TGI-II), bedrock mapping, result s reporte d below em phasiz e changes in the Early Ju- stratigraphy, Finlay River, Toodoggone River airborne ras sic stra tig ra phy of the Toodoggone from west to east. gamma-ray spectrometric and magnetic survey, Toodoggone River, Finlay River, Toodoggone formation, Black Lake Intrusive Suite, Cu-Au porphyry, epithermal LITHOSTRATIGRAPHIC UNITS Au-Ag Over the past two field seasons, nearly 600 km2 of the INTRODUCTION Swannell Ranges, situ ated be tween the major drainages of the Toodoggone and Finlay rivers and their conflu ence , The Toodoggone Geoscience Part ner ship was ini tiated have been mapped in detai l, thereby refin ing Juras sic stra - in 2003 to gener ate detai led geoscience infor m ati on, in- tig raphy that was, for the most part, pre viously assigne d to clud ing air borne geo phys ics and bed rock ge ol ogy maps, an un di vided Hazelton Group map unit (Diakow et al., that would sup port min ing ex plo ra tion in pre vi ously ex- 1985, 1993). As a conse quence of mapping in 2004, a re - plored and more re mote ter rain in the east-cen tral gion of pre viously un divided Ju rassic rocks is now iden ti - Toodoggone River and McConnell Creek map ar eas, which fied as part of the Toodoggone form ati on.