Ecotours – BC Walk with the Grizzlies
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
RBA Cragg Fonds
Kamloops Museum and Archives R.B.A. Cragg fonds 1989.009, 0.2977, 0.3002, 1965.047 Compiled by Jaimie Fedorak, June 2019 Kamloops Museum and Archives 2019 KAMLOOPS MUSEUM AND ARCHIVES 1989.009, etc. R.B.A. Cragg fonds 1933-1979 Access: Open. Graphic, Textual 2.00 meters Title: R.B.A. Cragg fonds Dates of Creation: 1933-1979 Physical Description: ca. 80 cm of photographs, ca. 40 cm of negatives, ca. 4000 slides, and 1 cm of textual records Biographical Sketch: Richard Balderston Alec Cragg was born on December 5, 1912 in Minatitlan, Mexico while his father worked on a construction contract. In 1919 his family moved to Canada to settle. Cragg gained training as a printer and worked in various towns before being hired by the Kamloops Sentinel in 1944. Cragg worked for the Sentinel until his retirement at age 65, and continued to write a weekly opinion column entitled “By The Way” until shortly before his death. During his time in Kamloops Cragg was active in the Kamloops Museum Association, the International Typographical Union (acting as president on the Kamloops branch for a time), the BPO Elks Lodge Kamloops Branch, and the Rock Club. Cragg was married to Queenie Elizabeth Phillips, with whom he had one daughter (Karen). Richard Balderson Alec Cragg died on January 22, 1981 in Kamloops, B.C. at age 68. Scope and Content: Fonds consists predominantly of photographic materials created by R.B.A. Cragg during his time in Kamloops. Fonds also contains a small amount of textual ephemera collected by Cragg and his wife Queenie, such as ration books and souvenir programs. -
Barkerville Gold Mines Ltd
BARKERVILLE GOLD MINES LTD. CARIBOO GOLD PROJECT AUGUST 2020 ABOUT THE CARIBOO GOLD PROJECT The Cariboo Gold Project includes: • An underground gold mine, surface concentrator and associated facilities near Wells The Project is located in the historic • Waste rock storage at Bonanza Ledge Mine Cariboo Mining District, an area where • A new transmission line from Barlow Substation to the mine site mining has been part of the landscape • Upgrades to the existing QR Mill and development of a filtered stack tailings since the Cariboo Gold Rush in the 1860s. facility at the QR Mill Site • Use of existing roads and development of a highway bypass before Wells The Project is being reviewed under the terms of the BC Environmental Assessment Act, 2018. CARIBOO GOLD PROJECT COMPONENTS • Underground mine and ore crushing • Water management and treatment CARIBOO GOLD • Bulk Fill Storage Area • New camp MINE SITE • Electrical substation • Offices, warehouse and shops in the • Above ground concentrator and paste concentrator building backfill plant • Mill upgrades for ore processing • Filtered stack tailings storage facility - no QR MILL SITE • New tailings dewatering (thickening tailings underwater and no dams and filtering) plant • New camp BONANZA LEDGE • Waste rock storage MINE • Movement of workers, equipment and • Concentrate transport to QR Mill via Highway TRANSPORTATION supplies via Highway 26, 500 Nyland 26 and 500 Nyland Lake Road. ROUTES Lake Road, Quesnel Hydraulic Road • New highway bypass before Wells (2700 Road) • Movement of waste -
Fish 2002 Tec Doc Draft3
BRITISH COLUMBIA MINISTRY OF WATER, LAND AND AIR PROTECTION - 2002 Environmental Indicator: Fish in British Columbia Primary Indicator: Conservation status of Steelhead Trout stocks rated as healthy, of conservation concern, and of extreme conservation concern. Selection of the Indicator: The conservation status of Steelhead Trout stocks is a state or condition indicator. It provides a direct measure of the condition of British Columbia’s Steelhead stocks. Steelhead Trout (Oncorhynchus mykiss) are highly valued by recreational anglers and play a locally important role in First Nations ceremonial, social and food fisheries. Because Steelhead Trout use both freshwater and marine ecosystems at different periods in their life cycle, it is difficult to separate effects of freshwater and marine habitat quality and freshwater and marine harvest mortality. Recent delcines, however, in southern stocks have been attributed to environmental change, rather than over-fishing because many of these stocks are not significantly harvested by sport or commercial fisheries. With respect to conseration risk, if a stock is over fished, it is designated as being of ‘conservation concern’. The term ‘extreme conservation concern’ is applied to stock if there is a probablity that the stock could be extirpated. Data and Sources: Table 1. Conservation Ratings of Steelhead Stock in British Columbia, 2000 Steelhead Stock Extreme Conservation Conservation Healthy Total (Conservation Unit Name) Concern Concern Bella Coola–Rivers Inlet 1 32 33 Boundary Bay 4 4 Burrard -
BC Geological Survey Assessment Report 34415
West LeBourdais Project Reconnaissance Geochemical and Geophysical Survey at the QR Claim Group Cariboo Mining Division NTS 093A/12 TRIM 093A072 52°42.6636’ North Latitude, 121°48.8358’ West Longitude Tenure on which work was conducted: 854573 Prepared for Barkerville Gold Mines Ltd (owner/operator) 15th Floor-675 West Hastings Street Vancouver, British Columbia V6B 1N2 By Angelique Justason Tenorex GeoServices 336 Front Street Quesnel, British Columbia V2J 2K3 December 2013 Table of Contents Introduction........................................................................................................................................1 Property Location, Access and Physiography..........................................................................2 Regional Geology............................................................................................................................... 6 Property Geology............................................................................................................................... 7 Exploration History.......................................................................................................................... 8 2011 Exploration ............................................................................................................................ 11 Self Potential Geophysics Overview and Procedures .............................................................. 13 Conclusions and Recommendations ....................................................................................... -
Technical Report on the South Cariboo Property, British Columbia, Canada
TECHNICAL REPORT ON THE SOUTH CARIBOO PROPERTY, BRITISH COLUMBIA, CANADA prepared for KORE Mining Ltd. and Karus Gold Corp. South Cariboo Property, British Columbia, Canada Effective Date: November 15, 2020 Report Date: December 16, 2020 Ron Voordouw, P.Geo. & Henry Awmack, P.Eng. Equity Exploration Consultants Ltd. This page intentionally left blank TABLE OF CONTENTS TABLE OF CONTENTS .......................................................................................................................................................... iii LIST OF TABLES..................................................................................................................................................................... v LIST OF FIGURES ................................................................................................................................................................... v 1.0 SUMMARY ............................................................................................................................................................... 6 1.1 Introduction ........................................................................................................................................................ 6 1.2 Property Description ........................................................................................................................................... 6 1.3 Location, Access and Ownership ........................................................................................................................ -
He University of Northern British Columbia's Quesnel River
WELCOME TO QRRC than 2.5 million chinook QUESNEL WATERSHED OFFERS: The QRRC is a world- and coho salmon and • the Quesnel, Cariboo and the Horsefly Rivers, and a multitude of small class research centre rainbow trout fry annually. lakes and streams; that provides a setting for Strong community pressure • a variety of biogeoclimatic zones and sub-zones within the area; • the 6,060 hectare Cariboo River Protected Area; he University of Northern collaboration involving to save the facility upon • anadromous salmonids such as Chinook, Coho, sockeye, and pink salmon; researchers from UNBC its closure in 1995 and the • non-anadromous fish such as rainbow trout, bull trout, dolly varden and and other kokanee; TBritish Columbia’s Quesnel River awarding of • other fish species such as burbot, mountain whitefish, northern provincial, an endowment pikeminnow, longnose dace, peamouth chub, redside shiner, and suckers; national and fund for • the Cariboo Mountains and its varied wildlife, including grizzly and black Research Centre (QRRC) is ideally bear, wolverine, cougar, lynx, caribou, elk, moose, deer, mountain goat, international Landscape beaver, martin, weasel, waterfowl, raptors and dozens more species of situated for both land and aquatic universities, Ecology by birds; government • historical large-scale hydraulic placer mining such as the Bullion Pit which Forest Renewal is 120 metres deep, 3 kilometres long, and where >9 million cubic metres of based research and university agencies, BC in 2002 gravel were hydraulically removed into the Quesnel River; other Students studying carbon levels in the soil near Likely. resulted in the • current open pit and placer mining operations; • active forest harvesting and management by major licencees; education. -
Barry Lawrence Ruderman Antique Maps Inc
Barry Lawrence Ruderman Antique Maps Inc. 7407 La Jolla Boulevard www.raremaps.com (858) 551-8500 La Jolla, CA 92037 [email protected] Sketch Map Northwest Cariboo District British Columbia. August 24, 1915. Stock#: 38734 Map Maker: Anonymous Date: 1915 Place: n.p. Color: Uncolored Condition: VG Size: 16 x 11 inches Price: SOLD Description: Detailed map of the Northwest Cariboo District, in British Columbia, drawn on a scale of 3 Miles = 1 inch. The legend shows main roads, old and second class roads and trails. The map focuses on the region between the Fraser River to the west and Barkerville and Quesnel Forks in the east, with Quesnel River running diagonally across the map. The map's primary focus is the hydrographical details of the region, including noting an Old Hydraulic Pit, Hell Dredger, Lower Dredger, Reed Dredger? and Sunker Dredger. Several towns and Post Offices are noted, including Barkersville Stanley Beaver Pass Ho. Cottonwood Quesnel Quesnell Forks The map covers the region which was the scene of the Cariboo Gold Rush of 1861-67. By 1860, there were gold discoveries in the middle basin of the Quesnel River around Keithley Creek and Quesnel Forks, just below and west of Quesnel Lake. Exploration of the region intensified as news of the discoveries got out. Because of the distances and times involved in communications and travel in those times and the Drawer Ref: Western Canada Stock#: 38734 Page 1 of 4 Barry Lawrence Ruderman Antique Maps Inc. 7407 La Jolla Boulevard www.raremaps.com (858) 551-8500 La Jolla, CA 92037 [email protected] Sketch Map Northwest Cariboo District British Columbia. -
Wild Rivers: Central British Columbia
Indian and Affaires indiennes Northern Affairs et du Nord Wild Rivers: Parks Canada Pares Canada Central British Columbia Published by Parks Canada under authority of the Hon. J. Hugh Faulkner, Minister of Indian and Northern Affairs, Ottawa, 1978 QS-7064-000-EE-A1 Les releves de la serie «Les rivieres sauvages» sont egalement publies en francais. Canada Canada metric metrique Metric Commission Canada has granted use of the National Symbol for Metric Conversion. Wild Rivers: Central British Columbia Wild Rivers Survey Parks Canada ARC Branch Planning Division Ottawa, 1978 2 Cariboo and Quesnel rivers: Ishpa Moun tain from Sandy Lake 3 'It is difficult to find in life any event and water, taken in the abstract, fail as which so effectually condenses intense completely to convey any idea of their nervous sensation into the shortest fierce embracings in the throes of a possible space of time as does the rapid as the fire burning quietly in a work of shooting, or running an im drawing-room fireplace fails to convey mense rapid. There is no toil, no heart the idea of a house wrapped and breaking labour about it, but as much sheeted in flames." coolness, dexterity, and skill as man can throw into the work of hand, eye Sir William Francis Butler (1872) and head; knowledge of when to strike and how to do it; knowledge of water and rock, and of the one hundred com binations which rock and water can assume — for these two things, rock 4 ©Minister of Supply and Services Now available in the Wild River Metric symbols used in this book Canada 1978 series: mm — millimetre(s) Available by mail from Printing and Alberta m — metre(s) Publishing, Supply and Services Central British Columbia km — kilometre(s) Canada, Ottawa, K1A 0S9, or through James Bay/Hudson Bay km/h - kilometres per hour your bookseller. -
Eocene Paleo-Physiography and Drainage Directions, Southern Interior Plateau, British Columbia1
215 Eocene paleo-physiography and drainage directions, southern Interior Plateau, British Columbia1 Selina Tribe Abstract: A map of reconstructed Eocene physiography and drainage directions is presented for the southern Interior Plateau region, British Columbia south of 53°N. Eocene landforms are inferred from the distribution and depositional paleoenvironment of Eocene rocks and from crosscutting relationships between regional-scale geomorphology and bedrock geology of known age. Eocene drainage directions are inferred from physiography, relief, and base level elevations of the sub-Eocene unconformity and the documented distribution, provenance, and paleocurrents of early Cenozoic fluvial sediments. The Eocene landscape of the southern Interior Plateau resembled its modern counterpart, with highlands, plains, and deeply incised drainages, except regional drainage was to the north. An anabranching valley system trending west and northwest from Quesnel and Shuswap Highlands, across the Cariboo Plateau to the Fraser River valley, contained north-flowing streams from Eocene to early Quaternary time. Other valleys dating back at least to Middle Eocene time include the North Thompson valley south of Clearwater, Thompson valley from Kamloops to Spences Bridge, the valley containing Nicola Lake, Bridge River valley, and Okanagan Lake valley. During the early Cenozoic, highlands existed where the Coast Mountains are today. Southward drainage along the modern Fraser, Chilcotin, and Thompson River valleys was established after the Late Miocene. Résumé : Cet article présente une carte reconstituée de la géographie physique et des directions de drainage, à l’Éocène, pour la région du plateau intérieur de la Colombie-Britannique, au sud du 53e parallèle Nord. Les formes de terrain à l’Éocène sont déduites de la distribution et du paléoenvironnement de déposition des roches de l’Éocène et à partir de relations de recoupement entre la géomorphologie à l’échelle régionale et la géologie du socle, d’âge connu. -
The Cariboo and Monashee Ranges of British Columbia: an Alpinist’S Guide
1 THE CARIBOO AND MONASHEE RANGES OF BRITISH COLUMBIA: AN ALPINIST’S GUIDE by EARLE R. WHIPPLE Even today, British Columbia is still a wilderness of mountains, valleys, glaciers, forest and plateau. The Columbia Mountains (Interior Ranges; which include the Cariboo and Monashee Ranges) lie within British Columbia, west of the Canadian Rockies and the southern Alberta-British Columbia border. This guide describes the access and mountaineering in these two ranges. Aside from parts of the Coast Range and the northern Rockies, the Cariboo and Monashee Ranges are the most isolated in B.C. However, if one listens to the helicopters from the lodges in these ranges, when camped there, one may question this. Large, active glaciers (now in retreat) with spectacular icefalls exist in the mountains of the western part of the Halvorson Group, the northern Wells Gray Group, the Premier Ranges, the Dominion Group and northern Scrip Range; there is climbing on rock, snow and ice, and routes for those climbers wishing easy, relaxing climbing in beautiful scenery. Good rock climbing on gneiss is in the southern Gold Range and Mt. Begbie in the north. There are also locales offering fine hiking on trails or alpine meadows (Halvorson Group, southern Wells Gray Group, southern Scrip Range, and the Shuswap Group), and backpacking traverses have been worked out through the Halvorson and Dominion Groups, the Scrip Range and the Gold Range. Beautiful lake districts exist in the northern Cariboos, and the Monashees. The area covered by this book starts northwest of the town of McBride, on Highway 16, southeast of Prince George, and extends south to near the border with the U.S.A., staying within the great bend of the Fraser River, and then west of Canoe Reach (lake; formerly Canoe River) and just west of the lower Columbia River south of its great bend. -
Provincial Flood Status Update
Dashboard # Provincial Lead Contact: Media Relations contact: Provincial Flood Status Update Manager, River Forecast Centre & Flood Safety Provincial Information Coordination Officer Date: July 16, 2020, 3:30 pm Freshet 14 George Roman Thomas Winterhoff Manager, River Forecast Centre and Flood Safety Senior Public Affairs Officer [email protected] [email protected] 250-896-2725 778-974-4380 Provincial Summary No severe or widespread flooding is expected this week – however, rainfall in parts of the Central Rockies and Cariboo Mountains continue to cause elevated rivers, streams, and lakes across these regions. A Flood Watch remains in place for the Quesnel River watershed and was issued this morning for tributaries of the Upper Fraser watershed due to potential for some localized issues. Apart from these specific locations, most water bodies in the province are dropping this week and have very low flood risks. Provincial staff, local government staff, First Nations, and other parties continue to monitor the situation and support implementation of flood emergency response as necessary. Weather (Current and Forecast) The Central Interior is experiencing rainy weather today, especially in mountainous areas of the Upper Fraser and Cariboo, where 10 - 40mm of rain has already fallen in the last 24 hours or so, and moderate rain continues to fall. Another low-pressure system moving towards Fort Nelson has started to spread rain across the far northeast. Fortunately, dryer conditions are expected this weekend across most of the province. Next week, the recent trend of unsettled cooler and unsettled summer weather will persist across the central and north, while dry, sunny summer weather will dominate most of the southernmost portions of the province. -
The Effect of School Closure On
Quaternary geology and drift prospecting in the Mount Polley region (NTS 093A) by Sarah Hashmi B.Sc., University of Waterloo, 2012 Thesis Submitted In Partial Fulfillment of the Requirements for the Degree of Master of Science in the Department of Earth Sciences Faculty of Science Sarah Hashmi 2015 SIMON FRASER UNIVERSITY Spring 2015 Approval Name: Sarah Hashmi Degree: Master of Science Title: Quaternary geology and drift prospecting in the Mount Polley region (NTS 093A) Examining Committee: Chair: Dr. Andy Calvert Professor Dr. Brent Ward Senior Supervisor Associate Professor Dr. Alain Plouffe Supervisor Research Scientist, Geological Survey of Canada Dr. Matthew Leybourne Supervisor Adjunct Professor Dr. Raymond Lett External Examiner Emeritus Geoscientist, University of Victoria Date Defended/Approved: March, 25th 2015 ii Partial Copyright License iii Abstract Drift prospecting studies were conducted in the Mount Polley Mine region, integrating surficial mapping, paleoflow measurements and Quaternary stratigraphy to infer glacial history. Eighty seven till samples were taken with the objective of determining the geochemical and mineralogical dispersal in till down-ice from Mount Polley. Surficial mapping identified till as the most abundant surficial material. Colluvium was mapped at high elevations and on steep slopes, and glaciofluvial and alluvial sediments are widespread in the river valleys. The stratigraphic record documents till associated with Fraser Glaciation followed by retreat phase glaciolacustrine and glaciofluvial sediments. Two distinct ice-flow movements have been identified; an initial west, southwestward flow during glacial advance, followed by a northwestward flow. The till sampling survey identified mineralized glacial dispersal up to 10 km to the northwest, Hg and Zn as pathfinder elements and apatite, andradite, chalcopyrite, epidote, gold grains and jarosite as porphyry indicator minerals (PIMs).