Cassiar Iskut-Stikine Land and Resource Management Plan
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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. -
Winter Newsletter — 2021
Khaye Winter Newsletter — 2021 INTRODUCTION Message from the President . 1 Message from the Vice President . 3 Save the Dates . 4 COVID-19 Updates . 5 Memorandum of Understanding . 9 Tahltan Stewardship Initiative . 11 New Tahltans . 15 Condolences . 16 NEW STAFF Adam Amir – Director of Multimedia . 17 Ombrielle Neria – Communications Specialist . 18 TAHLTAN ONTRACK Tahltan OnTrack . 19 TahltanWorks becomes Tahltan OnTrack . 21 FEATURE Tahltan Nation & Silvertip Mine Impact-Benefit Agreement . .. 23 DIRECTORS’ REPORTS Lands – Nalaine Morin . 26 Wildlife – Lance Nagwan . 27 Fisheries – Cheri Frocklage . .. 29 Language – Pamela Labonte . 31 Culture & Heritage – Sandra Marion . 33 Education & Training – Cassandra Puckett . 35 Employment & Contracting – Ann Ball . 37 Membership & Genealogy – Shannon Frank . .. 38 Dease Lake Community – Freda Campbell . 39 PERSONAL PROFILES Elder – Allen Edzerza . 41 Culture – Stan Bevan . 42 Healthy Active Tahltans – Lane Harris & Brandi MacAulay . 43 Inspiring Young Tahltans – Megan Rousseau & Nathan Nole . 45 UPDATES TNDC Update . 47 Treaty 8 Update . 49 Contents 1910 Declaration of the Tahltan Tribe WE THE UNDERSIGNED MEMBERS OF THE TAHLTAN TRIBE, speaking for ourselves, and our entire tribe, hereby make known to all whom it may concern, that we have heard of the Indian Rights movement among the Indian tribes of the Coast, and of the southern interior of B.C. Also, we have read the Declaration made by the chiefs of the southern interior tribes at Spences Bridge on the 16th July last, and we hereby declare our complete agreement with the demands of same, and with the position taken by the said chiefs, and their people on all the questions stated in the said Declaration, and we furthermore make known that it is our desire and intention to join with them in the fight for our mutual rights, and that we will assist in the furtherance of this object in every way we can, until such time as all these matters of moment to us are finally settled. -
Holocene Tephras in Lake Cores from Northern British Columbia, Canada
935 Holocene tephras in lake cores from northern British Columbia, Canada Thomas R. Lakeman, John J. Clague, Brian Menounos, Gerald D. Osborn, Britta J.L. Jensen, and Duane G. Froese Abstract: Sediment cores recovered from alpine and subalpine lakes up to 250 km apart in northern British Columbia con- tain five previously unrecognized tephras. Two black phonolitic tephras, each 5–10 mm thick, occur within 2–4 cm of each other in basal sediments from seven lakes in the Finlay River – Dease Lake area. The upper and lower Finlay tephras are slightly older than 10 220 – 10 560 cal year B.P. and likely originate from two closely spaced eruptions of one or two large volcanoes in the northern Cordilleran volcanic province. The Finlay tephras occur at the transition between deglacial sediments and organic-rich postglacial mud in the lake cores and, therefore, closely delimit the termination of the Fraser Glaciation in northern British Columbia. Sediments in Bob Quinn Lake, which lies on the east edge of the northern Coast Mountains, contain two black tephras that differ in age and composition from the Finlay tephras. The lower Bob Quinn tephra is 3–4 mm thick, basaltic in composition, and is derived from an eruption in the Iskut River volcanic field about 9400 cal years ago. The upper Bob Quinn tephra is 12 mm thick, trachytic in composition, and probably 7000–8000 cal years old. A fifth tephra occurs as a cryptotephra near the top of two cores from the Finlay River area and is correlated to the east lobe of the White River tephra (ca. -
Draft Navigability Report for Stikine River
United States Department of the Interior IJ:::.~ ~ .. BUREAU OF LAND MANAGEMENT "\ TAKE PRIDE" Alaska State Office INAMERICA 222 W. 7th Avenue, # 13 Anchorage, Alaska 99513-7599 http://www.ak.blm.gov To: File AA-085787 (1864) From: Navigable Waters Specialist Subject: Navigability ofStikine River, Southeast Alaska On February 17, 2005, the State of Alaska (State) filed an application for a recordable disclaimer of interest for the bed of the Stikine River from its mouth to the United States-Canada International Boundary, a distance of approximately 27 miles. The State also applied for lands underlying "all named interconnecting sloughs including Binkleys Slough, Red Slough, Guerin Slough, King Slough, Andrew Slough, Hooligan Slough, Shakes Slough, Shakes Lake, North Arm, and Ketili River, between the ordinary high water lines of the left and right banks .... " The State included with its application a legal description of the river, supporting evidence, and a map dated April 5, 2004 showing the Stikine River.l The State's submissions are more fully described in Attachment A. On June 4, 2007, the State submitted additional information in support of its application for the bed ofthe Stikine River. In this letter, the State asserted that the Tongass National Forest did not include the beds of navigable waters within the exterior boundaries of the reserve and, therefore, did not defeat the State's title to the bed ofthe navigable Stikine River.2 As the State's evidence shows, the Stikine River has been used almost continuously as a highway of commerce since before the Purchase of Alaska in 1867. Both Great Britain and the United States recognized the river's importance as a highway in the Washington Treaty of May 8, 1871. -
Geology and Mineral Deposits Tulsequah Map-Area, British Columbia (104K)
GEOLOGY AND MINERAL DEPOSITS TULSEQUAH MAP-AREA, BRITISH COLUMBIA (104K) 1.(50-1971-6J44 Technical Editor H. M. A. RJCl! Critical Readers J. O. WHUL~R HNll R. B. CAMPBELL Editor D. W>UT1! Text printed OD Georgian Olfset Smooth Finish Set iD Times Roman with 20th Century captioos by CANADIAN GOVEI\NMENT PJuN'TTNG BUReAU Artwork by C,\JlTOCRAPHlC UNIT, GSC 201339 FIGURE 1. View looking 'outhwe'l from the Tohllon Highland ocro" Tohomenie lake to the inner range' of the Coo,1 Mountain<. GEOLOGICAL SURVEY OF CANADA MEMOIR 362 GEOLOGY AND MINERAL DEPOSITS OF TULSEQUAH MAP-AREA, BRITISH COLUMBIA (104K) By J. G. Souther DEPARTMENT OF ENERGY, MINES AND RESOURCES CANADA © Crown Copyrighls reserved AvailabLe by mail from Information Canada, OIlOWO, rrom Geological SOf"ey or Canada. 601 Boolh St., Ollaw" nnd tll the following Jnformalion Canada b()Qk~hops: HALl FA>.' 1735 Barringlon Slreel MONTREAL 1182 SI. Cnlherine SlreeL West OrT,\WA 171 S Ialer Slreel TORONTO '22L Yonge Streel WINNlPEG 393 Ponage Avenue VA1'JCOUV£R 657 GranvilLe Street or through your bookseller A depos\t copy or Ihis publicalion is also 3yailable ror reference in public libraries acros~ Canada Price: $3.00 Calalogue No. M46·362 Price subju.1 to c.hange wilhaut nOlice Tnformiuion Canada Ollawa. 1971 PREFACE Taku River was used as a route to the Yukon during the Klondike gold rush of 1898 and this led to extensive prospecting, but it was not until 1937 that any of the silver-gold showings discovered in the intervening years were brought into production. Declining metal prices resulted in the closure of the last producing mine in 1957, but in recent years extensive geophysical and geochemical surveys have been made by several major exploration com panies and new prospects have been discovered. -
3Nation-BC Collaborative Stewardship Forum: Phase 2 Final Report On
3Nation-BC Collaborative Stewardship Forum: Phase 2 Final Report on Collaborative Governance Review and Research Jodi Gustafson & Kimberly Heinemeyer Round River Conservation Studies 9/28/20 Final Report September 2020, Prepared for The 3 Nations - British Columbia Collaborative Stewardship Forum 3Nation-BC CSF Co-Governance Phase 2 Final Report Round River Conservation Studies CONTENTS Report Summary .................................................................................................................................... iv Recommendations .............................................................................................................................. v Constructive Relationships: ............................................................................................................ v Identifying Shared Values: .............................................................................................................. v Information used in decision-making processes............................................................................ vi A regional framework and shared decision-making ...................................................................... vi Define and implement short term “pilot” projects ....................................................................... vi Acknowledgements ............................................................................................................................... vii 1 Introduction ................................................................................................................................... -
Herent and Collective Aboriginal Title and Rights Shared by All Tahltan People
BACKGROUNDER Information about the Conservancy, Park and Partners History on the conservancy: The Cassiar Iskut-Stikine Land and Resource Management Plan (LRMP), which was developed in 2000 and encompasses 5.2 million hectares, recommended the establishment of several new protected areas in northwestern B.C. The LRMP also recommended that if the mineral tenures in an area next to Mount Edziza Provincial Park became inactive, the area should be added to the park. Rather than adding the Ice Mountain area to the existing Mount Edziza Park, recent government-to- government discussions with the Tahltan recommended the area be designated as a conservancy. Conservancies are established to explicitly recognize the importance of an area to First Nations for social, ceremonial and cultural uses. They also enable the continuation of traditional Aboriginal uses and provide flexibility to ensure opportunities for low impact, compatible economic activities. The first conservancies in B.C. were designated in 2006 following government-to-government negotiations with First Nations on land use plans for the central and north coast. Mount Edziza Provincial Park: Mount Edziza Provincial Park was established in 1972 and spans more than 230,000 hectares of the Tahltan Highlands. The remote park, which can only be accessed by trails or a float plane, showcases a spectacular volcanic landscape that includes lava flows, basalt plateaus, cinder fields and cinder cones. The Mount Edziza area has been a major source of obsidian for Indigenous people for the last 9,000 to 10,000 years and is highly valued by the Tahltan people. Obsidian is a volcanic glass-like rock that has many uses including arrowheads and various types of knives. -
Geology of the Hoodoo Mountain Area (NTS 104B/14W)
Geology of the Hoodoo Mountain Area (NTS 104B/14W) by M.G. Mihalynuk1, A. Zagorevski2 and F. Cordey3 KEYWORDS: Hoodoo Mountain, Sphaler Creek, Stikine information is included herein; see Mihalynuk et al. assemblage, Stuhini Group, copper porphyry, Galore (2010, 2011a) for additional unit descriptions and Creek, Dirk prospect, Telena prospect, volcanic-hosted previous work. massive sulphide, Rock and Roll, Andrei Icefield, Iskut River LOCATION AND ACCESS INTRODUCTION Hoodoo Mountain area (NTS 104/14W) can be accessed either via the Bronson airstrip to the immediate Hoodoo Mountain area is located between the south, or via the Espaw camp located at kilometre 91 on enormous copper-gold resource defined at Galore Creek the incomplete Galore Creek access road, immediately and the past-producing gold deposits of the Bronson north of the map area. At the time of our field program, Camp. Reserves at Galore Creek in proven and probable both required air transport from Bob Quinn airstrip categories are 528 Mt grading 0.58% Cu, 0.32 g/t Au and located on Highway 37, approximately 400 km by road 6.02 g/t Ag (Gill et al., 2011). In the Bronson Camp, the from both Smithers and Terrace (Figure 1). Bob Quinn Snip mine produced 32 million grams of gold, 12 million airstrip is 60 km from both Bronson airstrip and Espaw grams silver and nearly 250 000 kilograms copper from Camp. about 1.2 million tonnes between 1991 and 1999; Johnny Mountain produced for less than two years with produced, proven, probable and “possible” categories totalling 0.622 Mt at 19.54 g/t Au (MINFILE, 2011). -
Stratigraphy of the Project Area
I BRITISH &! COLUMBLA Ministry of Employment and Investment ENERGY AND MINERALS DIVISION Hon. Dan Miller. Minister Geological Survey Branch THE STIKINE PROJECT GEOLOGY OF WESTERN TELEGRAPH CREEK MAP AREA, NORTHWESTERN BRITISH COLUMBIA (NTS 104G/5,6, llW, 12 AND 13) By Derek A. Brown1 , Michael H. Gunning2 and Charles J. Greig3 Appendix 3 - Conodont identifications by "I. Orchard, Geological Survey of Canada 1. Geological Surve Branch, British Colunlhia Ministry of Employment andYlnvestment 2. Department of Geology, University of Western Ontario, London, Ontario 3. C.G. Greig and Associates Ltd., Penticton, B.C. BULLETIN 95 Canadian Cataloguing in Publication Data Brawn. Derek Anlhony. 1959- The Stikine project : geology of western Telegraph Creek map area. nonhwenlem British Columbia (NTS.lMG15. 6, IIW. 12and 13) Issued by Geological Survey Branch. Includes bibliographical references: p ISBN 0-7726-2502-6 1, Geology -British Columbia -Telegraph Creek Region 2. Geochemistry - British Columbia - Telegraph Creek VICTORIA Region. 3. Geology. Economic - British Columbia - BRITISH COLUMBIA Telegraph Creek Region. 4. Mines and mineral resources - CANADA British Columbia - Telegraph Creek Region. 1. Gunning. Michael H. 11. Greig.Charles James, 1956- . 111. British Columbia. Ministry of Employment and Investmenl. IV. MAY 1996 BritishColumbia. Geological Survey Branch. V. Title. VI. Title: Geology of western Telegraph Creek maparea, nanhwertern British Columbia (NTS 1WG15.6. 1 IW. 12 and 13). V11. Series: Bulletin (British Columbia. Ministry of Employment and Investment) ;95. QE187.B76 1996 557.11’185 (395-960208-9 Frontispiece. View north along the Scud Glacier. Ambition Mountainis underlain by Permian limestone and metavolcanic rocks. Ministry of Emp/oyment and Inveshent TABLE OF CONTENTS CHAPTER 1 Chemistry ..................... -
Warburton Pike (1861-1915)
152 ARCTIC PROFILES Photo: Provincial Archives of British Columbia No. 4510. British Columbia has lost her foremost sportsman, and the eller on huntingtrips to the B .C . interior and other parts of the Dominion is the prer by an author who had achieved con- North. siderable note, by the death of Mr. Warburton Pike. News of August 1889 found Pike embarking by canoe fromFort Res- the demise of the well-known hunter was received in a cable from London, but the manner of his death is unknown. (Daily olution on what he called “an ordinary shooting expedition” Colonist, 30 October 1915) north of Great Slave Lake, where he hoped to “penetrate this unknown land, to see the musk-ox, and find out as much as I Warburton Pike was born into an old Westcountry family could about their habits, and the habits of the Indians who go near Wareham, Dorset, in 1861. He was educated at Rugby inpursuit of them every year. ” Thuscommenced the 14 School inan atmosphere of muscularChristianity, the physical months of hard travel, privation, and adventure described so emphasis of which was not lost on him. From Rugby he went vividly in Pike’s classic book The Barren Ground of Northern up to Brasenose College, Oxford, where he became a close Canada. friendof Earl Haig, the future fieldmarshal. Like many For five months he explored and hunted with the Beaulieu another young Englishman of his time andclass, Pike was at- clan - “the biggest scoundrels I ever had to travel with” - tracted to outdoor life and distantlands. In 1884, drawn by the and Yellowknives as far as the Coppermine country north of raw emptiness of British Columbia, he purchased ground on Lac de Gras. -
Guide to The
DEASE TELEGRAPH LAKE CREEK ISKUT Bob 1. Regional District of Kitimat-Stikine Quinn Lake BRITISH Suite 300, 4545 Lazelle Avenue COLUMBIA Guide to the Terrace, BC, V8G 4E1 Meziadin Junction Stewart 250-615-6100 Cranberry Junction Nass Camp New Aiyansh Hazelton www.rdks.bc.ca Gitwinksihlkw Kitwanga Greenville Rosswood Smithers Terrace Prince Rupert 2. Northern Health Houston Kitimat Prince Suite 600, 299 Victoria Street George STIKINE Prince George, BC, V2L 5B8 250-565-2649 www.northernhealth.ca 3. School District 87 PO Box 190, Lot 5 Commercial Drive Dease Lake, BC, V0C 1L0 250-771-4440 Vancouver www.sd87.bc.ca 4. Tahltan Central Government PO Box 69, Tatl’ah Dease Lake, BC, V0C 1L0 250-771-3274 www.tahltan.org 5. Northern Lights College PO Box 220, Lot 10 Commercial Drive Dease Lake, BC, V0C 1L0 250-771-5500 www.nlc.bc.ca Produced by the Regional District of Kitimat-Stikine COMUNITY CONTACTS in collaboration with the Tahltan Central Government. 2016 Overview TOP EVENTS Located in the picturesque northwest BC, the Stikine region is home to several communities rich in Talhtan First Nations history including Dease Lake, Telegraph Creek, and Iskut. Just 236 kilometers south of the Yukon border, Dease Lake offers access to some 1 Dease Lake Fish Derby – “BC’s Largest Northern Lake Trout Derby” of Canada’s largest natural parks, Spatsizi Wilderness Park and Mount Edziza Park. Discover remote wilderness in the Stikine region 2 4on4 Industry Hockey Tournament with endless recreation opportunities from guided horseback riding in the summer months to cross country skiing in the winter. -
Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum
S A M-R A P Ferr T T M Prepared for Fr Highw An Through R Pecci Associates, I. 825 Custer Avenue Helena, Montana 59604 (406)447-5000 www.rpa-hln.com Prepared by T Gos Associates, I. 1201 Western Avenue, Suite 200 Seattle, WA 98101 www.glosten.com Pametri, I. 700 NE Multnomah, Suite 1000 Portland, OR 97232-4110 T. 503.233.2400 F, 503.233.4825 www.parametrix.com CITATION The Glosten Associates, Inc., Parametrix, Inc. 2011. Southeast Alaska Mid-Region Access Port and Ferry Terminal Technical Memorandum. Prepared by The Glosten Associates, Inc., Seattle, Washington, Parametrix, Inc., Portland, Oregon. April 2011. Port and Ferry Terminal Technical Memorandum TABLE OF CONTENTS EXECUTIVE SUMMARY ....................................................................................................... ES-1 1 INTRODUCTION ................................................................................................................ 1-1 1.1 Purpose of the Mid-Region Access Study ......................................................................... 1-1 1.2 Southeast Alaska Mid-Region Access Study Corridors ..................................................... 1-3 1.2.1 Bradfield Canal Corridor ....................................................................................... 1-3 1.2.2 Stikine River Corridor ........................................................................................... 1-5 1.2.3 Aaron Creek Corridor............................................................................................ 1-5 1.3 Characteristics