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The Tuya-Teslin Areal Northern British Columbia
BRITISH COLUMBIA DEPARTMENT OF MINES HON. E. C. CARSON, Minister JOHN F. WALKER, Dopulu Minis/#, BULLETIN No. 19 THE TUYA-TESLIN AREAL NORTHERN BRITISH COLUMBIA by K. DeP. WATSON and W. H.MATHEWS 1944 CONTENTS. P*GS SUMMARY.................................................................................................................................... 5 CHAPTER I.-Introduction ....................................................................................................... 6 Location............................................................................................................................. 6 Access................................................................................................................................. 7 Field-work .......................................................................................................................... 7 Acknowledgments ............................................................................................................. 7 Previous Work.................................................................................................................. 8 CHAPTER11.- I Topography ........................................................................................................................ 9 Kawdy Plateau.......................................................................................................... 9 Trenches ...................................................................................................................... 9 Teslin -
British Columbia Geological Survey Geological Fieldwork 1989
GEOLOGY BETWEEN NINA LAKE AND OSILINKA RIVE,R, NORTH-CENTRAL BRITISH COLUMBIA (93N/15, NORTH HALF AND 94C/2, SOUTH HALF) By Filippo Ferri and David M. Melville KEYWORDS: Regionalmapping, Germansen Landing, The northern and eastem sections of the map are bounded, Omineca Belt. Intermontane Superterrane, Slide Mountain respectively, by the Osilinka and 0mine:ca rivers. At lheir Group, Paleozoicstratigraphy, lngenika Group, metamor- confluence the terrainis a relatively subdued and tree covzred phism, lead-zinc-silr,er-baritemineralization area. This is in contrast to the Wolverine Range east oithe OminecaRiverand arugged, unnamedrangeof mountai'ls to the southwest. The southern part of the map area was first mapped at a INTRODUCTION 6-mile scale in the 1940s by Amstrong; (1949).Gahrlelse (1975) examined the northem half in the course of 1:250 000 In 1989 theManson Creek 150 000 mappingproject mapping of the east half of the Fort Grahame map area. encompassed the north half of the Germansen Landing map Monger (1973), and Monger and Patersan (1974) described area (93Ni15) and the south half of the End Lake map area rocks in the map area during a reconnaissance sunfey of (94Ci2). As with previous years, the main aims of this project Paleozoic stratigraphy. To the northwest, Roots (1954) pub- were: to provide a detailed geologicalbase map of the area, to lished a 4-mile map of the Fort Graham west-half sheet. update the mineral inventory database, and to place known Many ofthe correlations made in this paper arewith stratigra- mineral occurrences within a geological framework. phy described by Gabrielse (1963, 1969:1,Nelson and Eirad- ford (1987) and other workers in the Casiar area whera: the The centreof the map area is located some 260kilometres miogeoclinal stratigraphy is quite similar and well known. -
Paper 08 (Colour).Vp
Toodoggone Geoscience Partnership: Preliminary Bedrock Mapping Results from the Swannell Range: Finlay River – Toodoggone River Area (NTS 94E/2 and 7), North-Central British Columbia1 By L. Diakow, G. Nixon, B. Lane and R. Rhodes KEYWORDS: P3, public-private partnership, Targeted Toodoggone River in the north and east (Fig. 1). The new Geoscience Initiative II (TGI-II), bedrock mapping, result s reporte d below em phasiz e changes in the Early Ju- stratigraphy, Finlay River, Toodoggone River airborne ras sic stra tig ra phy of the Toodoggone from west to east. gamma-ray spectrometric and magnetic survey, Toodoggone River, Finlay River, Toodoggone formation, Black Lake Intrusive Suite, Cu-Au porphyry, epithermal LITHOSTRATIGRAPHIC UNITS Au-Ag Over the past two field seasons, nearly 600 km2 of the INTRODUCTION Swannell Ranges, situ ated be tween the major drainages of the Toodoggone and Finlay rivers and their conflu ence , The Toodoggone Geoscience Part ner ship was ini tiated have been mapped in detai l, thereby refin ing Juras sic stra - in 2003 to gener ate detai led geoscience infor m ati on, in- tig raphy that was, for the most part, pre viously assigne d to clud ing air borne geo phys ics and bed rock ge ol ogy maps, an un di vided Hazelton Group map unit (Diakow et al., that would sup port min ing ex plo ra tion in pre vi ously ex- 1985, 1993). As a conse quence of mapping in 2004, a re - plored and more re mote ter rain in the east-cen tral gion of pre viously un divided Ju rassic rocks is now iden ti - Toodoggone River and McConnell Creek map ar eas, which fied as part of the Toodoggone form ati on. -
GEOLOGY of the EARLY JURASSIC TOODOGGONE FORMATION and GOLD-SILVER DEPOSITS in the TOODOGGONE RIVER MAP AREA, NORTHERN BRITISH COLUMBIA by Larry J
Province of British Columbia MINERAL RESOURCES DIVISION Ministry oi Energy, Mines and Geological Survey Branch Petroleum Resources Hon. Anne Edwards, Minister GEOLOGY OF THE EARLY JURASSIC TOODOGGONE FORMATION AND GOLD-SILVER DEPOSITS IN THE TOODOGGONE RIVER MAP AREA, NORTHERN BRITISH COLUMBIA By Larry J. Diakow, Andrejs Panteleyev, and Tom G. Schroeter BULLETIN 86 MINERAL RESOURCES DIVISION Geological Survey Branch Canadian Cataloguing in Publication Data Diakow, Larry, I. Geology of the early Jurassic Toodoggone Formation and gold-silvei depositsin the Toodoggone River map area, northern British Columbia VICTORIA BRITISH COLUMBIA (Bulletin, ISSN 0226-7497; 86) CANADA Issued by Geological Survey Branch. Includes bibliographical references: p January 1993 ISBNO-7718-9277-2 1. Geology - Stratigraphic - Jurassic. 2. Gold ores Geological researchfor this -Geology - British Columbia - Toodoggone River Region. 3. Silver ores - British Columbia - Toodoggone River publication was completed during Region. 4. Geology - British Columbia - Toodoggone the period 1981 to 1984. River Region. 5. Toodoggone Formation (B.C.) I. Fanteleyev, Andrejs, 1942- 11. Schroeter, T. G. In. British Columbia. Geological Survey Branch. IV. British Columbia. V. Title. VI. Series: Bulletin (British Columbia. Minisrry of Energy, Mines and Petroleum Resources); 86. TN414C32B731992 551.7'66'0971185 C92-092349.6 Lawyers gold-silver deposit looking northwesterly with Amethyst Gold Breccia (AGB) and Cliff Creek (CC) zones indicated. Cheni Gold Mines camp is in the lower centre and the mill site at the left of the photograph. Flat-lying ash-flow tuffs of the Saunders Member (Unit 6) form the dissected plateauand scarps in the foreground. Silica-clay-alunite capping Alberts Hump, similar to nearby precious metal bearing advanced argillic altered rocks of the A1 deposit (AI), are barely visible to the north of Toodoggone River and 5 kilometres beyond Metsantan Mountain. -
Botanical and Physiographic Reconnaissance of Northern British Columbia
Brigham Young University Science Bulletin, Biological Series Volume 14 Number 4 Article 1 9-1971 Botanical and physiographic reconnaissance of northern British Columbia Stanley L. Welsh Department of Botany, Brigham Young University, Provo, Utah 84601 J. Keith Rigby Department of Geology, Brigham Young University, Provo, Utah 84601 Follow this and additional works at: https://scholarsarchive.byu.edu/byuscib Part of the Anatomy Commons, Botany Commons, Physiology Commons, and the Zoology Commons Recommended Citation Welsh, Stanley L. and Rigby, J. Keith (1971) "Botanical and physiographic reconnaissance of northern British Columbia," Brigham Young University Science Bulletin, Biological Series: Vol. 14 : No. 4 , Article 1. Available at: https://scholarsarchive.byu.edu/byuscib/vol14/iss4/1 This Article is brought to you for free and open access by the Western North American Naturalist Publications at BYU ScholarsArchive. It has been accepted for inclusion in Brigham Young University Science Bulletin, Biological Series by an authorized editor of BYU ScholarsArchive. For more information, please contact [email protected], [email protected]. r?. J Brigham Young University haivm u .UJMlVERSiTvirj Science Bulletin BOTANICAL AND PHYSIOGRAPHIC RECONNAISSANCE OF NORTHERN BRITISH COLUMBIA by Stanley L. Welsh and J. Keith Rigby BIOLOGICAL SERIES — VOLUME XIV, NUMBER 4 SEPTEMBER 1971 BRIGHAM YOUNG UNIVERSITY SCIENCE BULLETIN BIOLOGICAL SERIES Editor: Stanley L. Welsh, Department of Botany, Brigham Young University, Provo, Utah Members of the Editorial Board: Vernon J. Tipton, Zoology Ferron L. Anderson, Zoology Joseph R. Murdock. Botany Wilmer W. Tanner, Zoology Ex officio Members: A. Lester Allen, Dean, College of Biological and Agricultural Sciences Ernest L. Olson, Chairman, University Publications The Brigham Young University Science Bulletin, Biological Series, publishes acceptable papers, particularly large manuscripts, on all phases of biology. -
Toodoggone/Kemess
Moosehorn Lake 590000 600000 610000 Swannell620000 Ranges 630000 640000 Claw Mountain (! (! Tseehee Creek Harmon Creek Moosehorn Creek (! (! Harmon Peak Metsantan Range Adoogacho Creek Hiamadam Creek Peak Range Pulpit Lake Midas Creek µ 6380000 6380000 (! Junkers Creek Breccia Peak Finlay Ranch Russel Property (! Park (! Midas Lake (! Moyez Creek (! Lower Belle Lake Dedeeya Creek Belle Creek (! Contact Peak Peak Range Katharine Creek (! Abesti Creek (!(! (! Upper Belle Lake (! McClair Creek Tuff Peak (! (! Oxide Creek (! Mulvaney Creek (! BONANZA (! (! (! Oxide Peak Jack Lee Creek Ç(! (! Gordonia Gulch (! The MacGregors (! Alberts Hump (! (! (! Mount Gordonia Moyez Creek (! (! (! THESIS II/III (! (! Ç (! PORPHYRY PEARL Belle Creek ^_(! (! Ç(! BV(! (! (! 6370000 (! (! 6370000 (! (! Antoine Louis Creek (! (! (! (! (! (! (! Mount Hartley Metsantan Creek Alberts Hump Creek METS JD Toodoggone Peak (! (! ^_(! (!^_ Mount Estabrook Bronlund Peak Metsantan Creek Mount Katharine (! ! (! ( Katharine Creek (! Metsantan Lake (! Mulvaney Creek (! (! (! Spatsizi McClair Creek Toodoggone Lake Jack Lee Creek Plateau Moosehorn Creek Wilderness Park DUKE Metsantan Pass Kadah Lake (! Toodoggone River MCCLAIR CREEK PLACER ^_ (! Kadah Creek Ç(! (! (! (! Bend Mountain Mount Graves(! Bronlund Creek Lawyers Creek (! (! Lawyers (! (! GOLDEN STRANGER (! (! Property Saunders Creek (! (! (! 6360000 (! (! 6360000 ^_ (! NEW LAW Edozadelly Mountain ^_(! Jock Creek (! (! (! (! (! AGB (! Ç(! (! (! (! CLIFF CREEK (! (! (! Ç (! (! DUKE'S RIDGE ^_(! GOLDEN NEIGHBOR 1 Ç (! -
Joint Review Panel Report
Kemess North Copper-Gold Mine Project Joint Review Panel Report September 17, 2007 KEMESS NORTH COPPER-GOLD MINE PROJECT JOINT REVIEW PANEL 160 ELGIN ST., 22ND FLOOR, OTTAWA, ONTARIO K1A 0H3 September 17, 2007 The Honourable John Baird, P.C., M.P. The Honourable Barry Penner, M.L.A. Minister of the Environment Minister of Environment Room 458, Confederation Building PO Box 9047 – Stn Prov Govt Ottawa, Ontario, K1A 0A6 Room 112 – Parliament Buildings Victoria, BC, V8W 9E2 Dear Ministers: In accordance with the mandate issued on May 19, 2005, the Joint Review Panel has completed its environmental assessment of the Kemess North Copper-Gold Mine Project. The Joint Review Panel is please to submit its report for your consideration. Overall, the Panel has concluded that the Project in its current form would not be in the public interest. The Panel is of the view that the economic and social benefits provided by the Project, on balance, are outweighed by the risks of significant adverse environmental, social and cultural effects, some of which may not emerge until many years after mining operations cease. The Panel therefore recommends that the Project not be approved by your respective governments. Yours truly, Carol Jones, Chair Malcolm Scoble Mark Duiven Kemess North Copper-Gold Mine Project Joint Review Panel Report September 17, 2007 © Her Majesty the Queen in Right of Canada, 2007 All Rights Reserved Library and Archives Canada Cataloguing in Publication Panel Report: Kemess North Copper-Gold Mine Project Issued by the Kemess North Mine Joint Review Panel ISBN 978-0-662-46715-1 Catalogue No.: En106-69/2007E-PDF Printed and Bound in Canada Table of Contents TABLE OF CONTENTS EXECUTIVE SUMMARY........................................................................................ -
Landforms of British Columbia 1976
Landforms of British Columbia A Physiographic Outline bY Bulletin 48 Stuart S. Holland 1976 FOREWORD British Columbia has more variety in its climate and scenery than any other Province of Canada. The mildness and wetness of the southern coast is in sharp contrast with the extreme dryness of the desert areas in the interior and the harshness of subarctic conditions in the northernmost parts. Moreover, in every part, climate and vegetation vary with altitude and to a lesser extent with configuration of the land. Although the Province includes almost a thousand-mile length of one of the world’s greatest mountain chains, that which borders the north Pacitic Ocean, it is not all mountainous but contains a variety of lowlands and intermontane areas. Because of the abundance of mountains, and because of its short history of settlement, a good deal of British Columbia is almost uninhabited and almost unknown. However, the concept of accessibility has changed profoundly in the past 20 years, owing largely to the use of aircraft and particularly the helicopter. There is now complete coverage by air photography, and by far the largest part of the Province has been mapped topographically and geologically. In the same period of time the highways have been very greatly improved, and the secondary roads are much more numerous. The averagecitizen is much more aware of his Province, but, although knowledge has greatly improved with access,many misconceptions remain on the part of the general public as to the precise meaning even of such names as Cascade Mountains, Fraser Plateau, and many others. -
Upper Skeena Fish Passage Culvert Inspection
Upper Skeena Fish Passage Culvert Inspection Ken Rabnett & Tim Wilson Gitksan Watershed Authorities February 2008 Upper Skeena Fish Passage Culvert Inspections 2 Gitksan Watershed Authorities February 2008 Upper Skeena Fish Passage Culvert Inspections Summary The purpose of this report is to present background information and survey results for fish passage inspections along the B.C. Rail grade located in the upper Skeena Watershed. In 2007, Gitksan Watershed Authorities (GWA) was retained by the Pacific Salmon Commission to conduct a Fish Passage and Culvert Inspection (FPCI) on all non-bridged B.C. Rail crossings of fish bearing streams in the upper Skeena Watershed. The upper Skeena Watershed fish passage assessment is the final component of a regional effort to improve fish passage limited by highways, secondary roads, and railway grades throughout high and very high value fish habitat in the Skeena Basin. This fish passage inspection project focused on the BC Rail grade, which enters the Skeena Watershed a few kilometres south of Bear Lake, traverses Bear Lake and River, passes Sustut River on the north bank, and goes upstream on the Skeena River northbank passing into the Stikine drainage. The B.C. Rail grade is 195 km in length within the Skeena Watershed. The primary objective of this project was to focus on increasing the abundance of fish stocks by opening freshwater habitat to salmon spawning and rearing. This project utilized the fish passage culvert inspection procedure developed to evaluate one of the most easily addressed fish habitat constraints: access to existing habitat. The methodology is based on the BC Government fish passage protocol outlined in Fish Passage – Culvert Inspection Procedures. -
Fort St. James Forest District Listing of Scenic Areas – 1999 Versus 2005
Fort St. James Forest District Listing of Scenic Areas – 1999 versus 2005 SCENIC AREAS 1999 SCENIC AREAS 2005 28 Mile Lake 28 Mile Lake Ahdatay Lake Ahdatay Lake Airline Lake Airline Lake Akus Lake Akus Lake Albert Lake Albert Lake Asitka Lake Asitka Lake Axelgold Range (now under Omineca River) Azuklotz Lake Azuklotz Lake Babine Lake (from Nadina District) Bear Lake & River Bear Lake & River (inc. Connelly Range/Thumb) Beaverlodge Lake Beaverpond Lake Bearverpond Lakes Benoit Lakes Benoit Lakes Blackburn Lake Blackburn Lakes Bolcome Lake Chain Bolcome Lake Chain Bone Lake Bone Lake Bugle Lake Bugle Lake Butterfield Lake Butterfield Lake Byrnes Lake Byrnes Lake (inc. Mt. Gordon , Laidlaw, & Grant) Calais Lake Calais Lake Camp (Nilan) Lake Camp (Nilan) Lake Camsell Lake Camsell Lake (inc. Shass Mtn. & Mt. Beals) Canyon Lake Canyon Lake Cariboo Heart Range (now under Kaza & Nanitsch Lakes) Carrall Ridge (now under Takla Lake/Driftwood R.) Carrier Lake Carrier Lake Centre Peak (now under Takla Lake/Driftwood River) Chuchi Lake Chuchi Lake (inc. Tizgay Lake on east side) (inc. Mt. Milligan & Alexander, and Tizgay Lake (East End)) Chuius Mountain (now under Tezzaron Lake) Connelly Range/ Thumb (now under Bear Lake & River) Cripple Lake Cripple Lake Cunningham Lake Cunningham Lake (North side of lake viewshed within a PA) Damshilgwit Lake Damshilgwit Lake (Lake itself within PA (unmapped) but part of viewshed mapped outside PA) Dan Miner Lake Dan Miner Lake Darb Lake Darb Lake Dargie Lake Dargie Lake Dawn Lake Dawn Lake Dem Lake Dem Lake - 1 - June 2005 Fort St. James Forest District Listing of Scenic Areas – 1999 versus 2005 SCENIC AREAS 1999 SCENIC AREAS 2005 Dia Lake Dia Lake Diver Lake & Peak Diver Lake & Peak Dolphin Lake Dolphin Lake Donald Lake Drift Lake Drift Lake (inc. -
Mcconnell CREEK MAP-AREA, CASSIAR DISTRICT, BRITISH COLUMBIA
.... v CANADA DEPARTMENT OF MINES AND RESOURCES MINES, FORESTS AND SCIENTIFIC SERVICES BRANCH GEOLOGICAL SURVEY OF CANADA MEMOIR 251 McCONNELL CREEK MAP-AREA, CASSIAR DISTRICT, BRITISH COLUMBIA BY C. S. Lord OTTAWA EDMOND CLOUTIER, C.M.G., B.A., L.Ph., KING'S PRINTER AND CONTROLLER OF STATIONERY 1948 Price, 25 cents No. 2488 PLATE I LU :t: t;- . -· - .- " - - .. - ·~ . ~;-~. -~i;1ff!:~ ~ /)?:.,""' ~.~.-~}:~T~·~ )f.~h~~~~'.':~~::~~~ ~-.,-~-;- j."':! ''-·., ~:-r .............t..,. .. · _~;:·;t'~'l'~ ~ ~ "~:«- . -- Lo o kin ~ south1•aslcrly from the norll11rnst end of Connelly Hangc. The µ:e ntlr in tli ned, 'rell-strati fic<l rocks a rc typical members of the Sustut group. In the centre distance is The Thumb, a projecting plug of Tcniarr basalt. The outlet of Bear Lake lies in the right middle distance. CANADA DEPARTMENT OF MINES AND RESOURCES MINES, FORESTS AND SCIENTIFIC SERVICES BRANCH GEOLOGICAL SURVEY OF CANADA MEMOIR 251 McCONNELL CREEK MAP-AREA, CASSIAR DISTRICT, BRITISH COLUMBIA BY C. S. Lord OTI'AWA EDMOND CLOUTIER, C.M.G., B.A., L.Ph., KING'S PRINTER AND CONTROLLER OF STATIONERY 1948 Price, 25 cents No. 2488 CONTENTS PAGE Preface......... .. .. ... ... ....... .... .. .... ... .................... v CHAPTER I Introduction...... 1 General statement . .. ... 1 Accessibility. 1 History............. ...... ... ..... ................... .... .... ..... 2 Physical features..... .. .. ...... .. ............ .. ... ........ .... 3 Glaciation. 4 Climate.. ... .. .............. ....... .. .. ... ...................... .... 5 Flom and fauna. -
Manson Creek Area, British Columbia (94N/9,10,15; 94C/2)
Province of British Columbia MINERAL RESOURCES DIVISION Ministry of Energy, Mines Geological Survey Branch and Petroleum Resources Hon. Anne Edwards, Minister BEDROCK GEOLOGY OF THE GERMANSEN LANDING - MANSON CREEK AREA, BRITISH COLUMBIA (94N/9,10,15; 94C/2) By Filippo Ferri, P.Geo. and David M. Melville, P.Geo. with contributions by M.J. Orchard (GSC) BULLETIN 91 Ferri.Filippo. 1959- . Bedrock geology of !he Germansen Landing-MansonCnek area, British Columbia (94N19. IO. 15: 94CR) (Bulletin. ISSN 02267497 ; 91) Issued by Geological Survey Branch. Ineludes bibliographical references: p. ISBN 0-77262125-X VICTORIA BRITISH COLUMBIA 1. Geology -British Columbia - Germansen Landing Region. CANADA 2. Geology - British Columbia - Manson Creek Region. 3. Gcology. - British Columbia - Germanscn Landing Economic APRIL 1994 Region. 4. Geology. Economic - British Columbia - Manson Creek Region. I. Melville. David M. 11. BritishColumbia. Ministry of Energy, Mines and Perroleurn Resources. Ill. British Columbia. GeologicalSurvey Branch. IV. TiUc. V. Series:Bulletin (British Columbia. Ministry of Energy. Miner and Peuolcum Resources) ; Fieldwork for this research was 91. carried out during the period I987 to 1989 TN27.B7F47 1994 551.7’00971182C94-960168.3 - ABSTRACT TheGermansen Landing-Manson Creek area is sillimanite grade within the Wolverine Metamorphic Com- located within the southern Omineca Mountains of north- plex. Rocks of the Nina Creek group were imbricated and central British Columbia. This region streddles the Inter- emplaced on top of North American rocks during this time montane-Omineca Belt boundary and encompasses rocks period.Middle to Late(?)Jurassic D2 deformation fromfive tectonostratigraphicterranes and subterrenes. refoldedthese rocks into uprightto northeast and These are: North American siliciclastics and carbonates of southwest(?)-verging structures.