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Pavilion Lake
Code: GC3P2XW Geological & Views Written and Researched by Angela Wynton Pavilion Lake Site Identification Nearest Community: Cache Creek, B.C. (Southeast) & Clinton, B.C. (Northeast) Geocache Location: N 50°50.962' W 121°42.734' Altitude: 810m/ 2657ft Date Established: Evans Photo: Kurt 1956 adding Pavilion Lake in 2001; 355 hectares Ownership: Provinicial Park Accuracy: The history of Pavilion Lake stretches beyond another 2 meters world and is a magical treasure.1 Some 10,000 years ago, Overall Difficulty: 2 beneath the watchful guard of the statuesque Chimney Overall Terrain: 3.5 Access Information and Rock, carbonate structures were developing along Restrictions: the floor of the lake with the help of micro-organisms – and From Highway 97 turn west onto the a spectacular underwater garden was slowly been sculpted.2 scenic route Highway 99 South at the Hat The formations, known as microbialites, were common Creek Heritage Ranch; follow the road for between 2.5 billion and 540 million years ago, but have about 30 kilometers to Marble Canyon Provincial Park at the easternmost seldom formed since that time. Although there are a few wetlands of the lake and continue a few world lakes that have these more recent spectacular kilometers to Pavilion Lake formations, including nearby Kelly Lake, they remain rare. Parking Advice: Park at pull off First discovered by scuba divers in the 1990’s, the magnificence of these ancient microbialites has been a constant source of interest and observation. So unique is the For more information or to report a underwater garden in Pavilion Lake, since 2004 the North problem with this site please contact: American Space Agency (NASA), the Canadian Space Agency (CSA), the Vancouver Aquarium, Donnie Reid and Gold Country Communities Society Darlene Lim, the principle investigator, have joined PO. -
A Field Guide to Forest Site Identification and Interpretation for the Cariboo Forest Region
A FIELD GUIDE TO FOREST SITE IDENTIFICATION AND INTERPRETATION FOR THE CARIBOO FOREST REGION O. A. Steen and R. A. Coupé Ministry of Forests Research Program 1997i AUTHORS AND AFFILIATIONS Ordell Steen, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Ray Coupé, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Canadian Cataloguing in Publications Data Steen, O. A. A field guide to forest site identification and interpretation for the Cariboo Forest Region Includes bibliographical references: p. ISBN 0-7726-3495-5 1. Bioclimatology British Columbia Cariboo Region. 2. Forest site quality British Columbia Cariboo Region. 3. Biogeography British Columbia Cariboo Region. 4. Forest ecology British Columbia Cariboo Region. 5. Forest management British Columbia Cariboo Region. 6. Cariboo Forest Region (B. C.). I. Coupé, R., 1952- . II. British Columbia. Ministry of Forests. Research Branch. QH541.5.F6S73 1998 581.7'37'09711 C989600637 © 1997 Province of British Columbia Published by the Research Branch, Ministry of Forests, 712 Yates Street, Victoria, B. C. V8W 3E7 Citation: Steen, O.A and R.A. Coupé. 1997. A field guide to forest site identification and interpretation for the Cariboo Forest Region. B.C. Min. For., Victoria, B.C. Land Manage. Handb. No. 39. Copies of this and other Ministry of Forests titles are available from Crown Publications Inc., 521 Fort Street, Victoria, B.C. V8W 1E7 ii ACKNOWLEDGEMENTS The classification and interpretations presented in this field guide have evolved over the past 20 years through the collective work of several individuals involved in the many phases of the Cariboo Forest Region ecological classification project. -
PF810348.Pdf
26 February, 1969 Notes on the open file report on the Bonaparte River Map Area, (92P), British Columbia, by R.B. Campbell and H.W. Tipper. The Bonaparte River map area is bounded by longitudes 1200 and 1220 West and by latitudes 510 and 520 North. The present report is based on field work carried out from 1963 to 1965. The information in this report was obtained in part from air photo interpretation and aerial reconnaissance by helicopter, but mostly from ground traverses. The informati on in the S.1H. L quarter is derived mainly from Trettin's report of 1961. PHYSIOGRAPHY Bonaparte River map area is part of the interior plateau and is sub-divided into several plateaux and highland regions. The sub-divisions are as follows: 1. Fraser Plateau which comprises about three-quarters of the map area, mainly the western part. It is essentially a flat or gently rolling region lying between 4,000 and 5,000 ft. elevation. In the sout h-west quarter the l·Tarble Range rises abruptly to 7,500 ft. The flattest part of the plateau, in the west half, is underlain by flat lying Pliocene and/or Miocene lavas. 2. The Thompson Plateau. This is distinguished from the Fraser Plateau by slightly greater relief and the absence of extensive flat lava areas. The Eastern boundary of Thompson plateau is approximately the North Thompson Valley. 'I'hompson plateau is underlain b:l folded and block faulted lat'e Palaeozoic, Mesozoic and early Tertiary volcanic sedimentary and grantiic rocks. 3. Quesnel and Shushwap Highlands. -
A Field Guide to Forest Site Identification and Interpretation for the Cariboo Forest Region
A FIELD GUIDE TO FOREST SITE IDENTIFICATION AND INTERPRETATION FOR THE CARIBOO FOREST REGION O. A. Steen and R. A. Coupé Ministry of Forests Research Program 1997i AUTHORS AND AFFILIATIONS Ordell Steen, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Ray Coupé, Research Ecologist, Cariboo Forest Region, Ministry of Forests, 200 - 640 Borland Street, Williams Lake, B.C. V2G 4T1 Canadian Cataloguing in Publications Data Steen, O. A. A field guide to forest site identification and interpretation for the Cariboo Forest Region Includes bibliographical references: p. ISBN 0-7726-3495-5 1. Bioclimatology British Columbia Cariboo Region. 2. Forest site quality British Columbia Cariboo Region. 3. Biogeography British Columbia Cariboo Region. 4. Forest ecology British Columbia Cariboo Region. 5. Forest management British Columbia Cariboo Region. 6. Cariboo Forest Region (B. C.). I. Coupé, R., 1952- . II. British Columbia. Ministry of Forests. Research Branch. QH541.5.F6S73 1998 581.7'37'09711 C989600637 © 1997 Province of British Columbia Published by the Research Branch, Ministry of Forests, 712 Yates Street, Victoria, B. C. V8W 3E7 Citation: Steen, O.A and R.A. Coupé. 1997. A field guide to forest site identification and interpretation for the Cariboo Forest Region. B.C. Min. For., Victoria, B.C. Land Manage. Handb. No. 39. Copies of this and other Ministry of Forests titles are available from Crown Publications Inc., 521 Fort Street, Victoria, B.C. V8W 1E7 ii ACKNOWLEDGEMENTS The classification and interpretations presented in this field guide have evolved over the past 20 years through the collective work of several individuals involved in the many phases of the Cariboo Forest Region ecological classification project. -
Title Page 2005 Kelly Lake.Cdr
TYPE OF WORK IN EXTENT OF WORK PROJECT COSTS THIS REPORT (IN METRIC UNITS) ON WHICH CLAIMS APPORTIONED (incl. support) GEOLOGICAL (scale, area) Ground, 1:5,000; 1:10,000 ~10 square km Mar 42, 106, 109, 113; Stag 1-2; William 1 $ 44,335.66 Photo interpretation GEOPHYSICAL (line-kilometres) Ground Magnetic Electromagnetic Induced Polarization Radiometric Seismic Other Airborne GEOCHEMICAL (number of samples analysed for ...) Soil Silt Rock 99 samples analyzed for whole rock constituents Mar 42, 106, 109, 113; Stag 1-2; William 1 $ 2,920.50 Other DRILLING (total metres; number of holes, size) Core Non-core RELATED TECHNICAL Sampling/assaying Petrographic Mineralographic Metallurgic PROSPECTING (scale, area) PREPARATORY/PHYSICAL Line/grid (kilometres) Topographic/Photogrammetric (scale, area) Legal surveys (scale, area) Road, local access (kilometres)/trail Trench (metres) Underground dev. (metres) Other TOTAL COST $47,256.16 GRAYMONT WESTERN CANADA INC. 2010 GEOLOGIC MAPPING AND SAMPLING OF THE KELLY LAKE LIMESTONE DEPOSITS, MARBLE RANGE WEST OF CLINTON, BRITISH COLUMBIA Clinton Mining Division MAR 42, 66-69, 101-102, 105-106, 109, 113 WILLIAM 1, MARY 1, AND STAG 1-5, 9-11 Geographic Coordinates 51° 08' 00" N 121° 52' 05" W NTS Sheet 92P/04 Owner & Operator: Graymont Western Canada Inc. 260, 4311 - 12 Street NE Calgary, Alberta T2E 4P9 Consultant: Dahrouge Geological Consulting Ltd. 18, 10509 - 81 Avenue Edmonton, Alberta T6E 1X7 Authors: P. Kluczny, B.Sc., P.Geol. Date Submitted: March 21, 2011 TABLE OF CONTENTS Page 1. Introduction ................................................. 1 1.1 Geographic Setting.............................................. 1 1.1.1 Location and Access...................................... 1 1.1.2 Topography, Vegetation and Climate. -
Extended Table 1: In-Situ Protection of All Species-Zone Combinations, Sorted by Increasing Relative Coverage (% of Total of This Species-Zone Combination)
Extended Table 1: In-situ protection of all species-zone combinations, sorted by increasing relative coverage (% of total of this species-zone combination). The absolute coverage (cumulative cover [ha] in protected areas) is also given. The first 25 potential protected areas for each combination are listed by decreasing expected population size. SPECIES CC CC Protected areas sorted by decreasing importance ZONE [%] [ha] PINUMON 0.0 0 (No protected area with a cumulative cover > 2.5ha) MS PSEUMEN 0.2 39 Nunsti, Big Creek, Nazko Lake, White Pelican, Churn Creek SBPS SALILUC 0.9 10 Premier Lake, Kikomun Creek, Kootenay, Columbia Lake IDF PINUFLE 1.0 1 (No protected area with a cumulative cover > 2.5ha) IDF ACERMAC 1.1 6 Birkenhead Lake, Nahatlatch IDF PRUNVIR 1.3 117 Peace - Moberly subzone, Gwillim Lake, Peace River - Bodreau, Bearhole Lake, BWBS Bearhole Lake, Milligan Hills, Chinchaga Lakes, Peace River Corridor-Peace River I, Butler Ridge, Beatton-Doig Canyon and Beatton River, Pine River Breaks, Sukunka Falls, Beatton, Clayhurst PRUNPEN 1.5 3 Peace - Moberly subzone BWBS ABIEGRA 1.5 39 West Arm, Champion Lakes, Syringa, Pilot Bay, Lockhart Creek, Kootenay Lake, ICH Valhalla, Kokanee Creek, King George VI ALNUVIR 1.8 301 Entiako, Tweedsmuir North, Entiako, Kluskoil Lake, Tweedsmuir (South), Nazko SBPS Lake, Nunsti, White Pelican, Narcosli Lake CORYCOR 1.8 195 Fraser River, Schoolhouse Lake Park, Fort George Canyon, Ten Mile Lake, SBS Pinnacles, Cinema Bog, Cottonwood River PINUBAN 2.0 0 (No protected area with a cumulative cover > 2.5ha) -
Deglaciation of the Cordillera of Western Canada at the End of the Pleistocene
Cuadernos de Investigación Geográfica ISSN 0211-6820 2017 Nº 43 (2) pp. 449-466 Geographical Research Letters eISSN 1697-9540 DOI: http://doi.org/10.18172/cig.3232 © Universidad de La Rioja DEGLACIATION OF THE CORDILLERA OF WESTERN CANADA AT THE END OF THE PLEISTOCENE J.J. CLAGUE Department of Earth Sciences, Simon Fraser University, Burnaby, BC V5A 1S6 Canada. ABSTRACT. Nearly all of what is now British Columbia and adjacent areas were covered by an ice sheet at the maximum of the Last Glaciation (MIS 2) about 18,000 years ago. By 11,000 years ago, the Cordilleran Ice Sheet had disappea- red, a victim of warming climate, eustatic sea-level rise along its western mar- gin, and perhaps a reduction in precipitation. Deglaciation proceeded by frontal retreat at the periphery of the ice sheet and by downwasting, complex frontal retreat, and localized stagnation in its interior areas. The chronology of degla- ciation is constrained, albeit with inherent dating errors, by AMS radiocarbon and 10Be surface exposure ages. High-elevation sites at the western margin of the British Columbia Interior Plateau, east of the Coast Mountains, became ice-free between about 15,000 and 12,000 years ago. Ice cover in the southern Coast Mountains was sufficiently extensive during the Younger Dryas Chronozone (12,900-11,700 years ago) that glaciers advanced into low-lying areas north and east of Vancouver. At the same time, however, a labyrinth of dead or dying tongues of glacier ice covered some interior valleys. By 11,000 years ago, ice cover in the Canadian Cordillera was no more extensive than it is today. -
Soils in the Taseko Lakes Area
Soils of the Taseko Lakes area, British Columbia Report No. 36 of the British Columbia Soi1 Survey K.W.G. Valentine, W. Watt, and A.L. Bedwany Soi1 mapping by W.Watt, A.L. Bedwany, L. Farstad, E.B. Wiken, K.W.G. Valentine, and T.M. Lord Land Resource Research Centre Contribution No. 85-35 (Map Sheet 92 0) Research Branch Agriculture Canada 1987 Copies of this publication are available from Maps B.C. Ministry of Environment Victoria, B.C. vav 1x5 0 Minister of Supply and Services Canada 1987 Cat. No.: A57-437E ISBN: O-662-15536-X Produced by Research Program Service caver: Rubbly alpine landscape of Mount Vic and Desperation soils and Rockland on Taseko Mountain. Staff editor: S.V. Balchin CONTENTS ACKNOWLEDGMENTS. .. vii PREFACE . viii GENERALDESCRIPTION OF AREA ....................................... 1 Location and extent .......................................... 1 Settlement and i-e.-sources ..................................... 1 Physiography ................................................. 1 Bedrock geology .............................................. 4 Surficial geology and parent materials ....................... 6 Climate ........................... .......................... 7 Vegetation ................................................... 10 SOIL SURVEYMETHODS. ............................................... 19 Mapping procedures and survey intensity ...................... 19 Accuracy ..................................................... 19 Soi1 associations and map units .............................. 21 SOIL ASSOCIATIONS -
DBC Gold Rush Trail Destination Development Strategy.Pdf
Appendix B GOLD RUSH TRAIL DESTINATION DEVELOPMENT STRATEGY FRASER CANYON Photo: Chris Harris DESTINATION BC GOLD RUSH TRAIL Heather Boyd MANAGEMENT COMMITTEE MANAGER, VANCOUVER, COAST & Kristi Denby MOUNTAINS AND INDUSTRY PROGRAMS GOLD RUSH TRAIL MANAGER [email protected] 250 392 2226 ext. 207 [email protected] Jody Young SENIOR PROJECT ADVISOR, THOMPSON OKANAGAN DESTINATION DEVELOPMENT TOURISM ASSOCIATION [email protected] Ellen Walker-Mathews VICE PRESIDENT, DESTINATION MINISTRY OF TOURISM, ARTS & INDUSTRY DEVELOPMENT AND CULTURE 250 860 5999, ext. 215 Amber Mattock [email protected] DIRECTOR LEGISLATION AND DESTINATION BC GOVERNANCE INDIGENOUS TOURISM 250 356 1489 ASSOCIATION OF BC [email protected] Theodore Assu DIRECTOR OF TRAINING CARIBOO CHILCOTIN COAST & EXPERIENCE DEVELOPMENT TOURISM ASSOCIATION 604 921 1070 Amy Thacker [email protected] CEO 250 392 2226, ext. 200 [email protected] TABLE OF CONTENTS I. EXECUTIVE SUMMARY ........................................................................1 7. STRATEGY AT A GLANCE ...............................................................43 a. Distinctive Destination for the Gold Rush Trail b. Distinctive Direction for the Gold Rush Trail 8. STRATEGIC PRIORITIES ..................................................................44 THEME 1: Strategically Invest In Targeted Infrastructure II. ACRONYMS ...........................................................................................6 Upgrades That Support This Unique Touring -
An Archaeological Perspective on Alpine/Sub-Alpine Land Use in the Clear Range and Pavilion Mountains, South-Central British Columbia
AN ARCHAEOLOGICAL PERSPECTIVE ON ALPINE/SUB-ALPINE LAND USE IN THE CLEAR RANGE AND PAVILION MOUNTAINS, SOUTH-CENTRAL BRITISH COLUMBIA by ANTHONY VANAGS B.A., The University of British Columbia A THESIS SUBMITTED IN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in THE FACULTY OF GRADUATE STUDIES (Department of Anthropology & Sociology) We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA December 2000 © Anthony E. N. Vanags, 2000 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the head of my department or by his or her representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department The University of British Columbia Vancouver, Canada DE-6 (2/88) Abstract This study uses two independent surveys of the Alpine/Sub-alpine environmental zones of the Clear Range and Pavilion Mountain to explore the nature of the archaeological record in the higher elevations of the Southern Interior Plateau of British Columbia. The archaeological site information is derived from the original site records as well as a lithic analysis of associated assemblages. The archaeological material is examined in relation to ethnographic subsistence and settlement patterns, archaeological pattering in Upland Valleys (Upper Hat Creek Valley), and to other investigated Alpine/Sub-alpine areas such as the Cornwall Hills and Potato Mountain. -
Cougar Point Richtheytruly Aregazing One Realizeshow There Issomething Worth Farmore Thangoldorsilver
Code: GC3PB9D Geological & Views Written and Researched by Angela Wynton Cougar Point Site Identification Nearest Community: Clinton B.C., Jesmond B.C. Geocache Location: N 51°04.905' W 121°55.548' Altitude: 1260 m Photo: Jack Taylor Ownership: Crown Land Accuracy: Tucked away between the Fraser River and the Coast 2 meters Mountain Range, in the land of the Secwepmec people, lays an ecological gem. Edge Hills Provincial Park is a Overall Difficulty: 3 wonderland of rare grasslands, mixed-wood forests and Overall Terrain: 3 spectacular views of the remarkable geology of the Fraser Access Information and Canyon. Restrictions: From Clinton follow Kelly Lake Road The park carries a strong cultural heritage, as it is within for 16 km and then turn onto Jesmond the Secwepmec traditional territory.1 And it was here, Road. Follow to the High Bar Road and below the hills southwest of Clinton where the Fraser River turn left onto road. Follow for 5.5 km until pullout on the right. meets Kelly Creek, a young Secwepmec man in 1872 Parking Advice: discovered gold. Park in flat area on right before 23% Grade road sign. The Edge Hills proved to be a mining Mecca, but only temporarily. Generally referred to as the Grange Mine, near the confluence of Kelly Creek and the Fraser River, the first For more information or to report a excavation began in 1881. Over the years gold, silver and problem with this site please contact: copper were mined, but not without difficulty. Numerous mining companies extracted the valuable metals, Gold Country Communities Society but as claims lapsed all mining excavation was shut down PO. -
Table of Contents
Community Profile – Clinton This publication was produced by Community Futures Development Corporation of Thompson Country (CFDCTC) with the full cooperation of the Village of Clinton. Project funding was provided by Human Resources Development Canada (HRDC) and Venture Kamloops. Table of Contents Message From the Mayor 2 Clinton Community Profile 3 Community Overview 3 Geographic Location 3 Climate 4 Trading Area 4 Economic Base 5 Important Economic Activities 5 Demographic Profile 7 Population Characteristics 7 Income Characteristics 8 Employment Characteristics 9 Education Characteristics 10 Construction and Housing Characteristics 10 Employment Services 12 The Business Community 13 Community Infrastructure 13 Transportation Infrastructure 13 Communications Infrastructure 15 Political/Government Infrastructure 16 Utilities 17 Taxation 18 Education 18 Community Services 19 Financial 19 Health Care 19 Emergency Services 20 Police Protection 20 Legal Services 20 Court Services 20 Community Lifestyle 21 Clubs/Groups/Organizations 21 Churches 21 Cultural Facilities 21 Recreational Facilities 22 Key Contacts 23 1 Community Profile – Clinton Message from the Mayor Clinton is the "Gateway to the Cariboo." Initially known as The Junction, it sits at the confluence of the two historic gold rush trails. There are numerous abandoned homesteads, wagon stops and line cabins in the area, all of which create a sense of adventure for the history buff or the outdoor photographer. Names such as Cougar Point, High Bar, Devil's Garden, Porcupine Creek and Clinton Falls stir the imagination and offer endless exploring opportunities. The multitude of fishing lakes in the area can be accessed by day trips from Clinton. Overnight trips can be made to one of the many guest ranches, provincial parks or forest service campsites.