Pleistocene Volcanism in the Anahim Volcanic Belt, West-Central British Columbia
Total Page:16
File Type:pdf, Size:1020Kb
Load more
Recommended publications
-
Wildfire Consultation Report Appendix.Pdf
Appendix Appendix Contents 50 Issues / Gaps - Partner Agencies 54 Statistics from Emergency Operations 54 Public Information (Communications) 61 EOC Activation Levels & Orders/Alerts Issued 71 Presentation and Interview with Robert Gray, Fire Ecologist 72 Climate Maps from Environment Canada 72 Documentaries & Interviews Reviewed 73 Cariboo Regional District Population Statistics 76 Consultation Meeting Overview 79 Top Five Topics by Meeting Location based on number of recorded comments Meeting Profiles: 81 100 Mile House 83 108 Mile Ranch 85 150 Mile House 87 Alexis Creek 89 Anahim Lake 91 Big Lake 93 Forest Grove 95 Horsefly 97 Interlakes 99 Kersley 101 Lac la Hache 103 Likely 105 McLeese Lake 107 Miocene 109 Nazko 113 Nimpo Lake 115 Quesnel 117 Riske Creek 119 Tatla Lake 121 Watch Lake 123 Wells 125 West Fraser 127 Wildwood 129 Williams Lake 131 Facebook Live 133 Comments from All Consultations By community meeting: 133 100 Mile House 136 108 Mile Ranch 144 150 Mile House 148 Alexis Creek 150 Anahim Lake 152 Big Lake 156 Forest Grove 159 Horsefly 161 Interlakes 167 Kersley 167 Lac la Hache 170 Likely 172 McLeese Lake 173 Miocene 177 Nazko 183 Nimpo Lake 186 Quesnel 189 Riske Creek 193 Tatla Lake 196 Watch Lake 199 Wells 200 West Fraser 203 Wildwood 206 Williams Lake 215 Facebook Live / Recording 218 Received Emails, Calls, and Facebook Messages/Comments 234 Survey Results 300 Information from Other Sources 301 Cellular Coverage Maps 302 Weather Forecasts - July 6 and 7 306 Seasonal Weather Forecast 317 Ranks of Fires 319 Canadian Wildland Fire Information System 321 Cariboo Fire Centre Prep July 6-7 326 Post-Wildfire Hazard Risk Assessment - C10784 Plateau 332 Alberta Wildfire Trend 334 Samples of Evacuation Communications 343 Community Descriptions 350 Glossary 351 Additional Citations Issues / Gaps - Partner Agencies Issues and gaps which are generally outside the jurisdiction of the Cariboo Regional District, along with suggested solutions (where applicable). -
Late Prehistoric Cultural Horizons on the Canadian Plateau
LATE PREHISTORIC CULTURAL HORIZONS ON THE CANADIAN PLATEAU Department of Archaeology Thomas H. Richards Simon Fraser University Michael K. Rousseau Publication Number 16 1987 Archaeology Press Simon Fraser University Burnaby, B.C. PUBLICATIONS COMMITTEE Roy L. Carlson (Chairman) Knut R. Fladmark Brian Hayden Philip M. Hobler Jack D. Nance Erie Nelson All rights reserved. No part of this publication may be reproduced or transmitted in any form or by any means, electronic or mechanical, including photocopying, recording or any information storage and retrieval system, without permission in writing from the publisher. ISBN 0-86491-077-0 PRINTED IN CANADA The Department of Archaeology publishes papers and monographs which relate to its teaching and research interests. Communications concerning publications should be directed to the Chairman of the Publications Committee. © Copyright 1987 Department of Archaeology Simon Fraser University Late Prehistoric Cultural Horizons on the Canadian Plateau by Thomas H. Richards and Michael K. Rousseau Department of Archaeology Simon Fraser University Publication Number 16 1987 Burnaby, British Columbia We respectfully dedicate this volume to the memory of CHARLES E. BORDEN (1905-1978) the father of British Columbia archaeology. 11 TABLE OF CONTENTS Page Acknowledgements.................................................................................................................................vii List of Figures.....................................................................................................................................iv -
TCHAD : Carte De Référence Du Tibesti (Février 2018)
TCHAD : Carte de référence du Tibesti (février 2018) 13°0'0"E 14°0'0"E 15°0'0"E 16°0'0"E 17°0'0"E 18°0'0"E 19°0'0"E 20°0'0"E 21°0'0"E 22°0'0"E 23°0'0"E Curni Ebredaa Al Malaqi Gara Kourni Guelta Mouri Idie Mezafeh Eringi Kourini Ehi Ebesoua Askinoa Biligay 23°0'0"N Tourki Dao 23°0'0"N Bissan Ehi- Bardi Kidi Sigurian Fokiri Tehia Hamadat Mouri Idie Tega Askinoa Manghini Ehi Bissoa Eke Rhoan Fokioure Garako-Karamo Fokiri Tenere Gara Mezora Ehi Mozorki Ehi Fokiri Mali Dourdoura Bir el War Tanoa Odorloptina Domasaka Gara Dohonia ⛜ Oloseri Ehi Yohobe Tiri Ennedi Sanaka Yourokali Gege Kourini Kourina Ouadoi Ennri Sanaka Nangara Ehi Kourina Ziri Goubou Ehi Araye Ehi Aray Passe de Sidi Aidao Ehi Ehi Kourizo Korizo Agala Enneri Aray Dafora Ehi Agalla Tara Oske Enneri Ehi Loga Bai Darda-Morkena Talagoum Abou Ehi Tchouhi Enneri Ache Yebige Enneri Aozou Tuzugu Tioumi-Ahinoa Enneri Kakeron Lama-Kora Gara Lakor Ehi Tchoui Ehi Doma Dougouli Tebidi Tiohodoma Tirke Enneri Sogoyi L I B YE Lemakora Ehi Chilii Bordaa Ehi Chili Koundie Ehi Tihodoma Ennedi Gudu Ennedi Gadu Eoj Wahs Yourgor-Gara Afafi Plateau Col de Mechi Taba Enneri Taar Gebel Afafi Touside-Fosma Enneri Meche Dobious Looteni Koysono Ehi Sohayi Ehi Tekoukoue Enneri Ehi Madoa Ehi Nangara Soo Ehi Ehi Dogolaga Oudji-Emi Yedri Mine Morogue Koui Ergida Elliguemi Ehi Enneri Enneri Kasa Kourea Mamadou Enneri Arabi Sao Yedri Enneri Yedri Ehi Tchedona Ehi Domor Eligemi Dogologa Chedenemia Ehi Kourea-Momodoy Asaserde Oualasena Aray Yedri Tega Taar Fodogoroa Orda Afafi Galliema Enneri Enneri Enneri Fodogoroum -
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. -
Working Paper Or Information Paper
APIRG/19 WP/14 Appendix 3.2J INTERNATIONAL CIVIL AVIATION ORGANIZATION VOLCANIC ASH CONTINGENCY PLAN AFI REGION First Edition - October 2012 THIS DOCUMENT IS ISSUED BY THE DAKAR AND NAIROBI ICAO REGIONAL OFFICES UNDER THE AUTHORITY OF THE APIRG 1 Page 2 of 32 Volcanic Ash Contingency Plan – AFI Region FOREWARD Within and adjacent to the Africa and Indian Ocean (AFI) Region there are areas of volcanic activities which are likely to affect flight in the AFI Region. The major volcanoes in the region are located in the following States: Algeria, Cameroon, Cape Verde Islands, Chad, Comoros Island, Democratic Republic of Congo, Djibouti, Eritrea, Ethiopia, France (Reunion Island), Kenya, Madagascar, Mali, Niger, Nigeria, Rwanda, Sao Tome and Principe, Spain (Canary Islands, Madeira), Sudan, Tanzania and Uganda. The names of the concerned volcano are listed in APPENDIX K (source: Smithsonian Institution). This document is the AFI Air Traffic Management (ATM) Volcanic Ash Contingency Plan which sets out standardised guidelines and procedures for the provision of information to airlines and en-route aircraft before and during a volcanic eruption. Volcanic contamination, of which volcanic ash is the most serious, is a hazard for safe flight operations. Mitigating the hazards posed by volcanic ash in the atmosphere and/or at the aerodrome cannot be resolved in isolation but through collaborative decision-making (CDM) involving all stakeholders concerned. During an eruption volcanic contamination can reach and exceed the cruising altitudes of turbine-powered -
The Archive of Place 00Front.Qxd 4/27/2007 6:48 AM Page Ii
00front.qxd 4/27/2007 6:48 AM Page i The Archive of Place 00front.qxd 4/27/2007 6:48 AM Page ii The Nature | History | Society series is devoted to the publication of high-quality scholarship in environmental history and allied fields. Its broad compass is signalled by its title: nature because it takes the natural world seriously; history because it aims to foster work that has temporal depth; and society because its essential concern is with the interface between nature and society, broadly conceived. The series is avowedly interdisciplinary and is open to the work of anthropologists, ecologists, historians, geographers, literary scholars, political scientists, sociologists, and others whose interests resonate with its mandate. It offers a timely outlet for lively, innovative, and well-written work on the interaction of people and nature through time in North America. General Editor: Graeme Wynn, University of British Columbia Claire Elizabeth Campbell, Shaped by the West Wind: Nature and History Tina Loo, States of Nature: Conserving Canada’s Wildlife in the Twentieth Century Jamie Benidickson, The Culture of Flushing: A Social and Legal History of Sewage John Sandlos, Hunters at the Margin: Native People and Wildlife Conservation in the Northwest Territories James Murton, Creating a Modern Countryside: Liberalism and Land Resettlement in British Columbia 00front.qxd 4/27/2007 6:48 AM Page iii The Archive of Place Unearthing the Pasts of the Chilcotin Plateau . UBC Press • Vancouver • Toronto 00front.qxd 4/27/2007 6:48 AM Page iv © UBC Press All rights reserved. No part of this publication may be reproduced, stored in a retrieval system, or transmitted, in any form or by any means, without prior written permission of the publisher, or, in Canada, in the case of photocopying or other reprographic copying, a licence from Access Copyright (Canadian Copyright Licensing Agency), www.accesscopyright.ca. -
Anahim Volcanic Belt Nazko Cone…A Sleepy Little Volcano, Not Made in Canada: a Tuya Skoatl Point
Geological Wonders of BC Farwell Canyon Wonder: an emotion comparable to surprise that people feel when perceiving something rare or unexpected Tags for 12 wonders for your geo-bucket list So much geology…so many wonders! Sullivan Ore body Main portal of the Sullivan mine near Kimberley when the mine was newly driven in 1915. The mine yielded over $42 billion in metals over its life Sullivan is a sedimentary exhalative (SEDEX) deposit formed around 1.5 Ga ago Since burial, geologic forces have affected the deposit…at depth the sulphides behaved more like tooth paste. Burgess Shale “the world’s most significant fossil discovery” Marrella splendens Specimen length (ex. ant.) = 20 mm 505 Million years ago Ottoia prolifica ate a Haplophrentis carinatus (maximum width of the worm = 1.2 cm) Reconstructions of two "weird wonders" from the Burgess Shale Odontogriphus (left, fossil length = 8 cm) and Nectocaris (right, fossil length = 4 cm, excluding tentacles), BC’s Contribution to Lagerstätten Portalia mira: of uncertain affinity Jade …an alteration product of ultramafic (high magnesium and iron, low silica) rock that is commonly called serpentinite… BC’s Provincial Gemstone Aldergrove BC The Curious Cache Creek Terrane It is characterized by an oceanic-rocks containing Tethyan-type fusulinid bearing limestone Terrane: a crustal block or fragment that is typically bounded by faults and that has a geologic genesis distinct from those of surrounding areas. Geologic Realms…. whoa! Realms = regions of origin The oceanic terranes, shown in red, are “bookmarks” that separate island arc and pericratonic blocks from each other. Hey, Ancient Rice? The Fusulinida is an extinct order within the Foraminifera in which the tests (shells) are composed of tightly packed, secreted microgranular calcite Yabeina colubiana in limestone This cannot be… Terrane theory was first proposed by Jim Monger of the Geological Survey of Canada and Charlie Rouse in 1971 as an explanation for a set of fusilinid fossils found in central British Columbia. -
Estimating Reserves 23 the Developed Professional 28 the Purpose and Goals of Proposed Amendments to the CSPG's By-Laws
17 Understanding Reserves and Resources: Part 3 – Estimating Reserves 23 The Developed Professional 28 The Purpose and Goals of Proposed Amendments to the CSPG's By-Laws $10.00 NOVEMBER 2011 VOLUME 38, ISSUE 10 Canadian Publication Mail Contract – 40070050 RESERVOIR ISSUE 10 • NOVEMBER 2011 1 Since 1927... Follow the Leader. The global industry leader in critical information and insight, IHS continues to invest in the progress of the Canadian energy market so you can get from discovery to drilling in record time. By updating, improving and streamlining our Canadian products and services, we have delivered workflow integration between IHS PETRA® and IHS AccuMap®; created solutions for better access to global resources, from well log databases to subject matter experts; and continued to provide transparency and insight to Canadian energy businesses that need actionable information. See how IHS is investing in Canada at www.followihs.com. Since 1927... November 2011 – VOLUME 38, ISSUE 10 ARTICLES Understanding Reserves and Resources Part 3 – Estimating Reserves ............................................................................................ 17 CSPG OFFICE The Developed Professional ............................................................................................... 23 #110, 333 – 5th Avenue SW Calgary, Alberta, Canada T2P 3B6 CSPG University Outreach: Welcome to the New Academic Year ..................... 25 Tel: 403-264-5610 Web: www.cspg.org Office hours: Monday to Friday, 8:30am to 4:00pm Another Great Year at CSPG Mixed Golf ....................................................................... 26 Executive Director: Lis Bjeld The Purpose and Goals of Proposed Amendments to the CSPG By-Laws .......... 28 Tel: 403-513-1235, Email: [email protected] Member Services: Dayna Rhoads Tel: 403-513-1225, Email: [email protected] 23rd Annual CSPG/CSEG 10K and 5K Road Race and Fun Run ............................. -
CANLAVA Mining Corp. 203 – 1312 Ketch Court Coquitlam, B.C
2016 GEOLOGICAL REPORT ON THE NAZKO PROPERTY CARIBOO MINING DIVISION BRITISH COLUMBIA BCGS MAPS 093B.082 AND 093B.092 LATITUDE 52° 55’ 32.3” N AND LONGITUDE 123° 44’ 10.8” W STATEMENT OF WORK EVENT: 5611358 Prepared for: CANLAVA Mining Corp. 203 – 1312 Ketch Court Coquitlam, B.C. V3K 6W1 Prepared by: R. A. (Bob) Lane, P.Geo. Plateau Minerals Corp. Date: June 30, 2016 NAZKO PROPERTY - 2016 ASSESSMENT REPORT TABLE OF CONTENTS 1 EXECUTIVE SUMMARY .............................................................................................. 1 2 INTRODUCTION ........................................................................................................ 2 2.1 LOCATION AND ACCESS ............................................................................................................................. 2 2.2 PHYSIOGRAPHY AND CLIMATE .................................................................................................................. 2 2.3 PROPERTY STATUS AND OWNERSHIP ...................................................................................................... 2 2.4 DEVELOPMENT AND EXPLORATION HISTORY ......................................................................................... 6 3 REGIONAL GEOLOGY ................................................................................................. 6 4 PROPERTY GEOLOGY ................................................................................................ 7 5 MINERALIZATION .................................................................................................... -
Recognizing Ice-Contact Trachyte-Phonolite Lavas at The
RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA by Kristen A. LaMoreaux B.S., Kent State University, 2002 Submitted to the Graduate Faculty of Arts and Sciences in partial fulfillment of the requirements for the degree of Master of Science University of Pittsburgh 2008 UNIVERSITY OF PITTSBURGH ARTS AND SCIENCES This thesis was presented by Kristen A. LaMoreaux It was defended on June 17, 2008 and approved by Dr. Michael Ramsey Dr. Thomas Anderson Thesis Director: Dr. Ian Skilling ii Copyright © by Kristen A. LaMoreaux 2008 iii RECOGNIZING ICE-CONTACT TRACHYTE-PHONOLITE LAVAS AT THE MOUNT EDZIZA VOLCANIC COMPLEX, BRITISH COLUMBIA, CANADA Kristen A. LaMoreaux, M.S. University of Pittsburgh, 2008 Mount Edziza Volcanic Complex (MEVC) lies within the Northern Cordilleran Volcanic Province (NCVP), in northwest British Columbia, Canada. The eruption products have been emplaced in a variety of subaerial, sub-ice and subaqueous environments from about 8Ma to less than 2000 y.b.p. (Souther, 1992). Ice Peak Formation (IPF) trachyte lava flows of approximately 1Ma age (Souther, 1992) are exposed at Ornostay Bluff (OB) and Koosick Bluff (KB). These flows comprise basal flow breccias overlain by massive conchoidally-fractured lava with large, poorly-developed columns, and local flow banding. Edziza Formation (EF) approximately 1Ma (Souther, 1992) phonolite is exposed at Triangle Dome (TD). TD can broadly be divided into an upper and lower zone. The upper zone comprises poorly-developed columns in addition to prominent jointing. In the lower zone the columns are planar and 75cm- 3m-wide in the interior of the complex grading into fan-like and curved subhorizontal columns <75cm-wide in the outer margins of the lower zone. -
Ministry of Energy and Mines BC Geological Survey Assessment
Ministry of Energy and Mines Assessment Report BC Geological Survey Title Page and Summary TYPE OF REPORT [type of survey(s)]: Geological and Geochemical TOTAL COST: $12,214.45 AUT!-IOR(S): R.A. (Bob) Lane NOTICE OF WORK PERMIT NUMBER(S)/DATE(S): -n/a---- ----------- ------- YEAR OF WORK: 2017 STATEMENT OF WORK - CASH PAYMENTS EVENT NUMBER(S)/DATE(S): 5653004 (June 15,2017) ------------------------- PROPERTY NAME: Nazko ------------------------------------------- CLAIM NAME(S) (on which the work was done): 552594, 1041719, 1047066 --------------------------------- COMMODITIES SOUGHT: Au, Ag ---"-------------------------------------- MINERAL INVENTORY MINFILE NUMBER(S), IF KNOWN: ------------------------------ MINING DIVISION: Cariboo NTS/BCGS: 093B.082 and 093B.092 -------------------- LATITUDE: 52 ° 55 • 32.3 " LONGITUDE: 123 ° 44 ' 10.8 " (at centre of work) OWNER(S): 1) CANLAVA Mining Corp. 2) ----------------------- MAILING ADDRESS: 203 - 1312 Keitch Court Coquitlam, B.C. V3K 6W1 OPERATOR(S) [who paid for the work]: 1) CANLAVA Mining Corp. 2) ----------------------- MAILING ADDRESS: 203 - 1312 Keitch Court Coquitlam, B.C. V3K 6W1 PROPERTY GEOLOGY KEYWORDS (lithology, age, stratigraphy, structure, alteration, mineralization, size and attitude): Eocene Ootsa lake Group, rhyolite, basalt, Cretaceous Skeena Group, elastic sedimentary rocks, gold-silver quartz veins REFERENCES TO PREVIOUS ASSESSMENT WORK AND ASSESSMENT REPORT NUMBERS: ------------------36171 Next Page TYPE OF WORK IN EXTENT OF WORK ON WHICH CLAIMS PROJECT COSTS THIS REPORT -
The Cheslatta Lake Suite: Miocene Mafic, Alkaline Magmatism in Central British Columbia1
Color profile: Disabled Composite Default screen 697 The Cheslatta Lake suite: Miocene mafic, alkaline magmatism in central British Columbia1 Robert G. Anderson, Jonah Resnick, James K. Russell, G.J. Woodsworth, Michael E. Villeneuve, and Nancy C. Grainger Abstract: New mapping, mineralogical, and geochemical studies help characterize late Tertiary primitive, alkaline, sodic basanite, alkali olivine basalt, transitional basalt, and diabase in the Nechako River, Whitesail Lake, and McLeod Lake map areas of central British Columbia and distinguish the Miocene Cheslatta Lake suite. The suite encompasses scattered erosional remnants of topographically distinct, columnar-jointed, olivine-phyric basalt and diabase volcanic necks, dykes, and associated lava flows north of the Anahim volcanic belt and west of the Pinchi Fault. Volcanic cen- tres at Alasla Mountain and at Cutoff Creek, near Cheslatta Lake, are proposed as type areas. Olivine, plagioclase, and pyroxene phenocrysts, megacrysts, and (or) xenocrysts; common ultramafic xenoliths; and rare but significant plutonic and metamorphic xenoliths are characteristic. Basanite, transitional basalt, and alkali olivine basalt groundmass contain plagioclase, clinopyroxene, Fe-Ti oxides, feldspathoid, olivine, and apatite. The Cheslatta Lake suite is characterized by its alkaline character, olivine-rich (>10 wt.%) normative mineralogy, and silica-undersaturated nature (>1 wt.% norma- tive nepheline; hypersthene-normative rocks are uncommon). Mg numbers vary between 72–42. Some samples encom- pass