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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. -
British Columbia Geological Survey Geological Fieldwork 2003
TRACKING THE ESKAY RIFT THROUGH NORTHERN BRITISH COLUMBIA - GEOLOGY AND MINERAL OCCURRENCES OF THE UPPER ISKUT RIVER AREA (TELEGRAPH CREEK NTS 104G/1, 2, 7, 8, 9, 10) By D.J. Alldrick1, M.L. Stewart1, J.L. Nelson1 and K.A. Simpson2 KEYWORDS: Targeted Geoscience Initiative-II (TGI-II), The two-year study will cover 6,250 km2, extending Bedrock mapping, Eskay Creek, Eskay Rift, Hazelton 125 km north from the Eskay Creek mine to the Spectrum Group, Stuhini Group, Mineral deposits porphyry copper-gold deposit (Figure 2). The paved Stewart-Cassiar Highway (Highway 37) runs northward through the eastern part of the map area. In 2003, the first INTRODUCTION field season, an eight-person team mapped 70 km along the rift sequence between Kinaskan Lake and More The Eskay Creek gold-silver mine, located in Creek, west of the highway (Figure 2). northwest British Columbia, is an unusually high-grade The project area straddles the eastern edge of the ore deposit. The mining industry continues to spend more Coast Mountains and the broad valley of the upper Iskut than $2 million each year on exploration for similar River. This area lies within the Tahltan First Nation deposits in the area. The geologic setting at the minesite is traditional area and they participated directly in this well studied, but large tracts in north-central British project. Topography varys from rounded glacial valleys Columbia require more detailed surveys to determine if along the upper Iskut River, to the extensive Spatsizi favourable sites exist for formation and preservation of Plateau, to high serrated ridges and peaks that are being additional deposits. -
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. -
Newsletters and Other Draft Nations, the Public and Provincial Organizations and Material
SSttiikkiinnee CCoouunnttrryy PPrrootteecctteedd AArreeaass NNeewwsslleetttteerr NNuummbbeerr11 Volume 1 February 2000 Management Planning is commencing for Stikine Country Protected Areas You are urged to become involved and provide your advice. Skeena District Parks Involved Spatsizi Plateau Wilderness Park Mt. Edziza Provincial Park Tatlatui Provincial Park Stikine River Recreation Area Mt. Edziza Recreation Area Kinaskan Lake Provincial Park Gladys Lake Ecological Reserve “The Stikine River Recreation Area near Highway 37.” Background Stikine Country contains some of the most outstanding protected areas in British Columbia. They lie within the traditional territory of the Tahltan First Nations. Each of these protected areas is important in its own right, and together they protect provincial and international values for future generations. These include: Ä largely intact predator/prey ecosystems Ä provincially important populations of caribou, mountain sheep, mountain goats, grizzly bears and wolf Ä spectacular mountain, plateau, river and volcanic landscapes Ä important archaeological sites, cultural and heritage values and activities of the Tahltan First Nations Ä internationally significant wilderness recreation and tourism activities such as nature appreciation, rafting, canoeing, hiking, hunting, angling and horseback riding Planning is proposed to begin shortly and to be completed by the fall of 2001. A systems approach to planning is being undertaken in recognition of the ecosystem connectivity and related issues among this -
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. -
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. -
Dease Liard Sustainable Resource Management Plan
Dease Liard Sustainable Resource Management Plan Background Document January, 2004 Ministry of Sustainable Resource Management Table of Contents Table of Contents................................................................................................................. i List of Tables ...................................................................................................................... ii List of Maps ........................................................................................................................ ii List of Acronyms ...............................................................................................................iii Glossary .............................................................................................................................. v 1. Introduction.................................................................................................................... 1 1.1 Plan Objectives ........................................................................................................ 1 1.2 Background.............................................................................................................. 1 1.3 MSRM Mandate, Principals and Organizational Values......................................... 2 1.4 SRM Planning and Plans Defined............................................................................ 3 1.5 Scope of Dease-Liard SRM Plan ............................................................................. 5 1.6 The Process ............................................................................................................. -
Northwest Transmission Line Project: Skii Km Lax Ha Traditional Use and Knowledge Report
Northwest Transmission Line Project: Skii km Lax Ha Traditional Use and Knowledge Report Prepared By: Updated December 2009 Rescan™ Environmental Services Ltd. TM Vancouver, British Columbia NORTHWEST TRANSMISSION LINE PROJECT Skii Km Lax Ha Traditional Knowledge and Use Study Executive Summary Executive Summary The purpose of this report is to inventory and describe Skii km Lax Ha Traditional Use (TU) and Traditional Knowledge (TK) related to the proposed Northwest Transmission Line (NTL) Project (the Project). Skii km Lax Ha TU/TK was collected between February and November 2007. Work was then suspended when, on November 26, 2007, NovaGold Resources Inc. and Teck Cominco Limited announced a decision to suspend construction of the Galore Creek mine project. As a result of the loss of this main customer, the Province and British Columbia Transmission Corporation (BCTC) suspended the Project for a year. In November 2008, the Province provided a mandate and additional funding to complete the Environmental Assessment. Work then recommenced and discussions about capacity funding and further data were collected between January and September 2009. A mixed methods approach was used to collect TU/TK information from April to September 2009, including desk-based archival research, direct discussions, and two formal interview sessions and mapping sessions. The key findings are summarized in the report, which indicates that the Project study area was, and to a large extent continues to be, well-travelled and frequently used by the Skii km Lax Ha, whose traditional territories intersect the Project from Cranberry River to Ningunsaw Pass (Laxyiip). Skii km Lax Ha traditional activities involve hunting, trapping, and fishing; important areas include historic and berry/plant/mushroom harvesting sites. -
21 Day Alaska and the Yukon: Full Circle
Tour Code AYFC 21 Day Alaska and the Yukon: Full Circle 21 days Created on: 24 Sep, 2021 Day 1: Arrive in Calgary, AB Your adventure begins as you arrive in Calgary ? a metropolitan Albertan city with western flare. Transfer to your centrally located downtown hotel and enjoy the rest of the day at leisure before our welcome dinner tonight where we?ll get to know our Tour Director and fellow travelers. Overnight: Calgary Included Meal(s): Dinner Day 2: Calgary - Grande Prairie, AB This morning we travel north and pass through Edmonton, Alberta?s bustling capital city. Onboard a luxurious and spacious coach, watch the beauty unfold through Northern Alberta as we travel through pristine wilderness and sprawling fields en route to Grand Prairie, the hub of Alberta?s Peace River Country. Overnight: Grande Prairie Included Meal(s): Breakfast Day 3: Grande Prairie - Fort Nelson, BC Travel through the vast northern prairie region of Alberta en route to Dawson Creek, where the world famous Alaska Highway begins. Surrounded by untouched wilderness, snow capped mountain tops and vast tundra, The Alaska Highway is known as the Legendary Road of the North. Continue on to British Columbia?s picturesque Peace Country with an abundance of natural history and agricultural land. Overnight: Fort Nelson Included Meal(s): Breakfast and Lunch Day 4: Fort Nelson - Watson Lake, YT Venture through peaceful valleys and alpine meadows and dip your toes in Liard Hot Pools, some of Canada?s best natural hot springs located in a lush boreal spruce forest. This evening, tour the spectacular Northern Lights Centre and experience natures? greatest light show, the breathtaking Northern Lights. -
Canadian Volcanoes, Based on Recent Seismic Activity; There Are Over 200 Geological Young Volcanic Centres
Volcanoes of Canada 1 V4 C.J. Hickson and M. Ulmi, Jan. 3, 2006 • Global Volcanism and Plate tectonics Where do volcanoes occur? Driving forces • Volcano chemistry and eruption types • Volcanic Hazards Pyroclastic flows and surges Lava flows Ash fall (tephra) Lahars/Debris Flows Debris Avalanches Volcanic Gases • Anatomy of an Eruption – Mt. St. Helens • Volcanoes of Canada Stikine volcanic belt Presentation Outline Anahim volcanic belt Wells Gray – Clearwater volcanic field 2 Garibaldi volcanic belt • USA volcanoes – Cascade Magmatic Arc V4 Volcanoes in Our Backyard Global Volcanism and Plate tectonics In Canada, British Columbia and Yukon are the host to a vast wealth of volcanic 3 landforms. V4 How many active volcanoes are there on Earth? • Erupting now about 20 • Each year 50-70 • Each decade about 160 • Historical eruptions about 550 Global Volcanism and Plate tectonics • Holocene eruptions (last 10,000 years) about 1500 Although none of Canada’s volcanoes are erupting now, they have been active as recently as a couple of 4 hundred years ago. V4 The Earth’s Beginning Global Volcanism and Plate tectonics 5 V4 The Earth’s Beginning These global forces have created, mountain Global Volcanism and Plate tectonics ranges, continents and oceans. 6 V4 continental crust ic ocean crust mantle Where do volcanoes occur? Global Volcanism and Plate tectonics 7 V4 Driving Forces: Moving Plates Global Volcanism and Plate tectonics 8 V4 Driving Forces: Subduction Global Volcanism and Plate tectonics 9 V4 Driving Forces: Hot Spots Global Volcanism and Plate tectonics 10 V4 Driving Forces: Rifting Global Volcanism and Plate tectonics Ocean plates moving apart create new crust. -
Complete Emergency Management Plan
Approval Message from the Tahltan Chief and Council Approval Emergency Management Plan 2020 Tahltan Emergency Management Program Revision Log: Ver 11 – 1 (rewrite 2020-01-01) By affixing our signatures below, we hereby approve this document: _______________________________ ____________________________________ Chief of Tahltan Council Member(s) of Tahltan Note to the reader: Ensure you have the most current copy of the plan. The most current electronic version resides with Tahltan’s Emergency Program Coordinator Table of Contents 1.0 Purpose and Scope...................................................................................................... 1 2.0 Plan Document Overview ............................................................................................ 1 How to Use the Plan.................................................................................................................1 2.1.1 Base Plan .............................................................................................................................1 2.1.2 Appendix 1 – Contacts.........................................................................................................1 2.1.3 Appendix 2 to 4 - Roles and Responsibilities.......................................................................2 2.1.4 Appendix 5 - Checklists........................................................................................................2 2.1.5 Appendix 6 – Forms.............................................................................................................2