Response of Elk and Stone's Sheep to Prescribed Fire In
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Glaciers of the Canadian Rockies
Glaciers of North America— GLACIERS OF CANADA GLACIERS OF THE CANADIAN ROCKIES By C. SIMON L. OMMANNEY SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, Jr., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–J–1 The Rocky Mountains of Canada include four distinct ranges from the U.S. border to northern British Columbia: Border, Continental, Hart, and Muskwa Ranges. They cover about 170,000 km2, are about 150 km wide, and have an estimated glacierized area of 38,613 km2. Mount Robson, at 3,954 m, is the highest peak. Glaciers range in size from ice fields, with major outlet glaciers, to glacierets. Small mountain-type glaciers in cirques, niches, and ice aprons are scattered throughout the ranges. Ice-cored moraines and rock glaciers are also common CONTENTS Page Abstract ---------------------------------------------------------------------------- J199 Introduction----------------------------------------------------------------------- 199 FIGURE 1. Mountain ranges of the southern Rocky Mountains------------ 201 2. Mountain ranges of the northern Rocky Mountains ------------ 202 3. Oblique aerial photograph of Mount Assiniboine, Banff National Park, Rocky Mountains----------------------------- 203 4. Sketch map showing glaciers of the Canadian Rocky Mountains -------------------------------------------- 204 5. Photograph of the Victoria Glacier, Rocky Mountains, Alberta, in August 1973 -------------------------------------- 209 TABLE 1. Named glaciers of the Rocky Mountains cited in the chapter -
Synoptic Taxonomy of Major Fossil Groups
APPENDIX Synoptic Taxonomy of Major Fossil Groups Important fossil taxa are listed down to the lowest practical taxonomic level; in most cases, this will be the ordinal or subordinallevel. Abbreviated stratigraphic units in parentheses (e.g., UCamb-Ree) indicate maximum range known for the group; units followed by question marks are isolated occurrences followed generally by an interval with no known representatives. Taxa with ranges to "Ree" are extant. Data are extracted principally from Harland et al. (1967), Moore et al. (1956 et seq.), Sepkoski (1982), Romer (1966), Colbert (1980), Moy-Thomas and Miles (1971), Taylor (1981), and Brasier (1980). KINGDOM MONERA Class Ciliata (cont.) Order Spirotrichia (Tintinnida) (UOrd-Rec) DIVISION CYANOPHYTA ?Class [mertae sedis Order Chitinozoa (Proterozoic?, LOrd-UDev) Class Cyanophyceae Class Actinopoda Order Chroococcales (Archean-Rec) Subclass Radiolaria Order Nostocales (Archean-Ree) Order Polycystina Order Spongiostromales (Archean-Ree) Suborder Spumellaria (MCamb-Rec) Order Stigonematales (LDev-Rec) Suborder Nasselaria (Dev-Ree) Three minor orders KINGDOM ANIMALIA KINGDOM PROTISTA PHYLUM PORIFERA PHYLUM PROTOZOA Class Hexactinellida Order Amphidiscophora (Miss-Ree) Class Rhizopodea Order Hexactinosida (MTrias-Rec) Order Foraminiferida* Order Lyssacinosida (LCamb-Rec) Suborder Allogromiina (UCamb-Ree) Order Lychniscosida (UTrias-Rec) Suborder Textulariina (LCamb-Ree) Class Demospongia Suborder Fusulinina (Ord-Perm) Order Monaxonida (MCamb-Ree) Suborder Miliolina (Sil-Ree) Order Lithistida -
Stratigraphy, Structure, and Tectonic History of the Pink Mountain Anticline, Trutch (94G) and Halfway River (94B) Map Areas, Northeastern British Columbia
Stratigraphy, Structure, and Tectonic History of the Pink Mountain Anticline, Trutch (94G) and Halfway River (94B) Map Areas, Northeastern British Columbia Steven J. Hinds* and Deborah A. Spratt University of Calgary, 2500 University Dr. NW, Calgary AB, T2N 1N4 [email protected] ABSTRACT Pink Mountain Anticline stands out in front of the Foothills of northeastern British Columbia (57ºN, 123ºW). Geologic mapping and prestack depth-migrated seismic sections show that it is localized above and west of a northwest-trending subsurface normal fault. Along with isopach maps they demonstrate episodic normal movement during deposition of the Carboniferous Stoddart Group, Triassic Montney Formation and possibly the Jurassic-Cretaceous Monteith- Gething formations. West of this step, during Laramide compression, a pair of backthrusts nucleated on either side of a minor east-west trending Carboniferous fault and propagated across it in an en échelon pattern. One backthrust ramped laterally across the area and separated the Pink Mountain and Spruce Mountain structures, which both are contained within a 30+ km long pop-up structure above the Besa River Formation detachment. Glomerspirella fossils confirm the existence of the Upper Jurassic Upper Fernie Formation and Upper Jurassic to Lower Cretaceous Monteith Formation at Pink Mountain. Economic Significance of the Pink Mountain Area Since the building of the Alaska Highway during the early 1940’s, various companies have carried out petroleum, coal, and mineral surveys of the study area. To the east of Pink Mountain, several shallow gas fields such as the Julienne Creek and Julienne Creek North gas fields (Figure 1) were successfully drilled and produced gas from Triassic sandstone and carbonate rocks that were gently folded during the formation of the northern Rocky Mountains. -
A History of Fish in the Northeastern British Columbia
HISTORICAL FISHERIES INFORMATION FROM THE MUSKWA-KECHIKA MANAGEMENT AREA Prepared By: Alicia Woods SS#2 Site 13 Comp 17 Fort St. John, BC V1J 4M7 For: Fisheries Branch Ministry of Environment, Lands and Parks Rm. 400 10003-110th Avenue Fort St. John, BC V1J 6M7 January 2001 Muskwa-Kechika Historical Fisheries Research Project SUMMARY The primary purpose of this research project was to compile and preserve historical fisheries information within the Muskwa-Kechika Management Area. This report outlines and describes, by watershed, fisheries related activities that took place over the past decades. Information gathered for this project came from personal interviews and other research. Interviews were conducted with persons from Fort St. John, Fort Nelson, Dawson Creek and other communities. The expectation of this project is to document and preserve information, that would otherwise be lost, and make it accessible for further research. In addition to preserving the past, this research will be able to provide a different outlook on past fisheries issues, and possibly bring forth new ideas and management strategies. Funding for this project was obtained through an application from BC Environment, Fisheries Section, Fort St. John, to the Muskwa-Kechika Trust Fund. ACKNOWLEDGMENTS Much appreciation and thanks to Nick Baccante, for direction and knowledge on this project, Paul Mitchell-Banks for his knowledge and including me on his many excursions, the Fish and Wildlife staff at the Ministry of Environment, Lands and Parks, and Rob Woods for his immeasurable amount of knowledge of the area. The author also wishes to acknowledge the Guide Outfitters of northeastern British Columbia, Fort Nelson First Nations Band, Prophet River First Nations Band and the many locals that volunteered their time and offered their knowledge to this project. -
Besa River Formation, Western Liard Basin, British Colum- Bia (NTS 094N): Geochemistry and Regional Correlations
BESA RIVER FORMATION, WESTERN LIARD BASIN, BRITISH COLUM- BIA (NTS 094N): GEOCHEMISTRY AND REGIONAL CORRELATIONS Filippo Ferri1, Adrian S. Hickin1 and David H. Huntley2 ABSTRACT The Besa River Formation in the northern Toad River map area contains correlatives of the subsurface Muskwa Member, which is being exploited for its shale gas potential. In the Caribou Range, more than 285 m of fine-grained carbonaceous siliciclastic sediments of the Besa River Formation were measured along the northwestern margin of the Liard Basin (the upper 15 m and lower 25 m of the section are not exposed). The formation has been subdivided into six informal lithostratigraphic units comprised primarily of dark grey to black, carbonaceous siltstone to shale. The exception is a middle unit comprising distinctive pale grey weathering siliceous siltstone. A handheld gamma-ray spectrometer was used to produce a gamma- ray log across the section, which delineated two radioactive zones that are correlated with the Muskwa and Exshaw markers in the subsurface. Rock-Eval geochemistry indicates that there are several zones of high organic carbon, with levels as high as 6%. Abundances of major oxides and trace elements show distinct variability across the section. The concentration of major oxides generally correlates with lithological subdivisions, whereas some of the trace-element abundances display a relationship with organic carbon content, suggesting that these levels are tied to redox conditions at the time of deposition. Ferri, F., Hickin, A. S. and Huntley, D. H. (2011): Besa River Formation, western Liard Basin, British Columbia (NTS 094N): geochemistry and regional correlations; in Geoscience Reports 2011, BC Ministry of Energy and Mines, pages 1-18. -
Ministerial Order 244/2021
PROVINCE OF BRITISH COLUMBIA ORDER OF THE MINISTER OF ENVIRONMENT AND CLIMATE CHANGE STRATEGY Muskwa-Kechika Management Area Act Ministerial Order No. M244 I, George Heyman, Minister of Environment and Climate Change Strategy, order that the attached Redfern – Keily Park, Northern Rocky Mountains Park and Northern Rocky Mountains Protected Area Management Plans are enacted, pursuant to section 5 (1.1) of the Muskwa- Kechika Management Area Act. June 14, 2021 Date Minister of Environment and Climate Change Strategy (This part is for administrative purposes only and is not part of the Order.) Authority under which Order is made: Act and section: Muskwa-Kechika Management Area Act, S.B.C. 1998, c. 38, s. 5 (1.1) Other: page 1 of 111 Northern Rocky Mountains Park and Northern Rocky Mountains Protected Area Management Plan February 2021 BC Parks Northern Rocky Mountains Park and Northern Rocky Mountains Protected Area Management Plan Approved by: ______________________________ June 14, 2021________ Honourable George Heyman Minister of Environment and Climate Change Strategy Foreword by BC Treaty 8 First Nations WELCOME to our homeland. The Beaver (Dunne-za, Dane-zaa), Cree, Saulteau, Slavey (Dene), and TseK’ hene indigenous groups have occupied these lands since time immemorial. Treaty 8 was signed in the spirit of Peace and Friendship on June 21, 1899. British Columbia Treaty 8 Territory is hundreds of thousands of square kilometres in size and includes 8 groups: Blueberry River First Nations, Doig River First Nation, Fort Nelson First Nation, Halfway River First Nation, McLeod Lake Indian Band, Prophet River First Nation, Saulteau First Nations and West Moberly First Nations. -
Additional Historical Fisheries Information From
ADDITIONAL HISTORICAL FISHERIES INFORMATION FROM THE MUSKWA-KECHIKA MANAGEMENT AREA Prepared By: Alicia D. Woods Woods Environmental Consulting SS#2 Site 13 Comp 17 Fort St. John, BC V1J 4M7 For: Fisheries Branch Ministry of Water, Land and Air Protection Rm. 400 10003-110th Avenue Fort St. John, BC V1J 6M7 December 2001 Muskwa-Kechika Historical Fisheries Research Project 2001 SUMMARY The primary purpose of this research project was to compile and preserve historical fisheries information from within the Muskwa-Kechika Management Area. This is the second year of the project, and this report will outline the information obtained from the 2001 study year. The purpose of the first year of research was to learn more about the stocking and transplanting of fish that occurred historically in the Muskwa-Kechika Management Area. The project soon began to gather a wide variety of historical fisheries information. This year, the goal of the project was try and obtain information that was not collected previously as well as to broaden the aspects of this project by including the historical aboriginal uses of fish in the Muskwa-Kechika Management Area. The Fisheries Section Head, Fort St. John, obtained funding for this project through an application to the Muskwa-Kechika Trust Fund. ACKNOWLEDMENTS I would like to thank Nick Baccante, Jeff Burrows, Paul Mitchell-Banks, and Rachelle Woods for their assistance with this project. I also would like to express my appreciation and thanks to all the residents, Guide Outfitters and First Nations of northeastern British Columbia for allowing me to come into their homes and sharing with me a part of their past. -
Source Rock Characterization of the Carboniferous Golata Formation
Source Rock Characterization of the Carboniferous Golata Formation and Devonian Besa River Formation Outcrops, Liard Basin, Northwest Territories Jonathan Rocheleau Northwest Territories Geoscience Office Kathryn M. Fiess Northwest Territories Geoscience Office Leanne J. Pyle VI Geoscience Services Ltd Fillipo Ferri Oil and Gas Division, BC Ministry of Energy Tiffani A. Fraser Yukon Geological Survey Summary The evaluation of regional stratigraphic relationships and geochemical characteristics of Devonian to Carboniferous age shales in the Liard Basin area of the Northwest Territories is necessary for the assessment of shale gas exploration potential for this region. Field studies of the Golata Formation were conducted at Etanda Lakes and Sheaf Creek in 2012 and 2013, respectively. Besa River Formation field studies were conducted at Nahanni River in 2013 (Figure 1). Geochemical studies currently completed on the Golata and Besa River Formations samples include: 1) Rock Eval/TOC, 2) vitrinite reflectance, ICP-ES and ICP-MS (lithogeochemistry). The Golata Formation at Etanda Lakes and Sheaf Creek is characterized by relatively low uranium abundance, moderate levels of terrigenous input and detrital clays, and relatively high silica content. Combined with outcrop observations, these data support the interpretation that the Golata Formation was deposited in a prodelta environment. Rock-Eval, vitrinite reflectance and TOC data from Etanda Lakes indicates that the Golata Formation is a fair to good source rock. The Besa River Formation at Nahanni River is characterized by enrichment in uranium and vanadium, a relatively low level of terrigenous input, and high silica content. These data indicate that the Besa River shales were deposited in a reducing, anoxic, low energy environment. -
Prophet River Hotsprings Provincial Park
PROPHET RIVER HOTSPRINGS PROVINCIAL PARK PURPOSE STATEMENT AND ZONING PLAN Peace Region 2006 Approved by: _____________________ Date:_____________2006 Andy Ackerman, Regional Manager Environmental Stewardship Division Peace Region ______________________ Date:______________2006 Nancy Wilkin Assistant Deputy Minister Environmental Stewardship Division 1 Figure 1: Regional Context Prophet River Hotsprings Park Tena ka Creek k thto Cree Ga N " 0 ' 0 ° 8 N 5 " Prophet River 0 ' 0 ° Wayside Park 8 5 r e iv R a w sk Mu u skwa M Northern Rocky Mountains Park R iv er r e N Riv " a 0 skw ' Mu r 5 e 4 M a River iv ° N u skw [§Trutch 7 " R t 5 0 ' e 5 ph 4 ro ° P 7 5 T ru t ch Creek Prophet River Hotsprings Park $+97 N " r 0 e ' iv 0 Kw 3 R ° a dacha r N 7 " e v 5 0 i ' 0 R 3 e ° i k 7 A 5 r e iv R r e k e River a ors n gh i Buckikn inghorse River Redfern-Keily Park M uc B Way Park B esa River B es a Riv er N " 0 ' Sikanni Chief 5 1 ° N 7 " S Ecological Reserve 5 0 ik ' an 5 n Sikanni Chief Falls O i 1 Ch ° s p ie 7 f i Protected Area 5 R k i a ve r R iv e r a Cre ik e es k P 124°30'0"W 124°15'0"W 124°0'0"W 123°45'0"W 123°30'0"W 123°15'0"W 123°0'0"W 122°45'0"W Subject Area Subject Area " Other Protected Areas Projection: UTM Zone 10 Datum: NAD83 Highway Road Produced in June 2006 for 1:600,000 Ministry of Environment This is a visual representation by Ministry of Agriculture and Lands 0 2.5 5 7.5 10 12.5 only and should not be used for Integrated Land Management Bureau Kilometers legal purposes PROPHET RIVER HOTSPRINGS PROVINCIAL PARK Purpose Statement and Zoning Plan Primary Role The primary role of the Prophet River Hotsprings Park is to protect locally significant hotsprings and associated wildlife habitat. -
Polar Continental Shelf Program – Science Report 2018 – Logistical
Polar Continental Shelf Program SCIENCE REPORT Logistical support for leading-edge scientific research in Canada and its Arctic Polar Continental Shelf Program SCIENCE REPORT Logistical support for leading-edge scientific research in Canada and its Arctic Polar Continental Shelf Program Science Report 2018: Logistical support for leading-edge scientific research in Canada and its Arctic Contact information Polar Continental Shelf Program Natural Resources Canada 2464 Sheffield Road Ottawa ON K1B 4E5 Canada Tel.: 613-998-8145 Email: [email protected] Website: pcsp.nrcan.gc.ca Cover photographs: (Top) The field camp at the Cape Bounty Arctic Watershed Observatory on Melville Island, Nunavut. (Bottom} Taking a break on some 900 million-year-old sedimentary rocks in the Wernecke Mountains, Yukon, to make notes on a geological map. Section header image: Recording temperature data at the Dr. Neil Trivett Global Atmosphere Watch Observatory in Alert, Nunavut, as part of a permafrost monitoring program that has been ongoing since 1979. Photograph contributors (alphabetically) Émilie Bouchard, University of Galen Halverson, McGill University: Cover Tom Platt, Natural Resources Canada: Saskatchewan: Contents page, page (bottom), pages 40, 41, 48 and 55 page 3 (bottom) pages 36 and 52 Jessica Kidd, LGL Limited - Environmental Emma Randle, Imperial College London: Martin Brazeau, Imperial College London: Research Associates: page 29 page 35 (bottom) pages 34, 35 (top), 45, 47 and 56 Scott Lamoureux, Queen’s University: Cover Kevin Rawlings: -
Geological Survey Canada
MANUSCRIPT AND CJ\qT ""y NOV ~o 1967 SECfION GEOLOGICAL PAPER 67.. 1 Part B SURVEY OF CANADA DEPARTMENT OF ENERGY, . MINES AND RESOURCES EPORT OF ACTIVITIES, Part 8: ovember 1966 to April 1967 PrIce, $1.50 1967 GEOLOGICAL SURVEY OF CANADA CANADA PAPER 67 - 1 Part B REPORT OF ACTIVITIES, Part B: November 1966 to April 1967 DEPARTMENT OF ENERGY, MINES AND RESOURCES © Crown Copyrights reserved Available by mail from the Queen's Printer; Ottawa, from Gcological Survcy of Canada, 601 Booth St., Ottawa, and at the following Canadian Government bookshops: HALIFAX 1735 Barrington Street MONTREAL £terna-Vie Building, 1182 St. Catherine St. West OTIAWA Daly Building, Corner Mackenzie and Rideau TORONTO 221 Yonge Street WINNIPEG Mall Center Bldg., 499 Portage Avenue VANCOUVER 657 Granville Street or through your bookseller Price ~n. 50 Catalogue No. 1\:LrL_67-1B Price subject to change without notice ROGER DUHAMEL, F.R.S.C. Queen's Printer and Controller of Stationery Ottawa, Canada 1967 - iii - CONTENTS Page ABSTRACT ••...•.......•.•....••.....•.••.•..•.••.•.•.••.. vii INTRODUCTION ..•....•.•..•......•....•......•••.••....••. EXPLORATION GEOPHYSICS 1. Magneto -tellurics ..•......•......•••..•... A. Becker 3 2. Detectability of diabase dykes by aeromagnetic surveys ..• •......••.•.••• Peter Hood 3 3. Palaeomagnetism of lower Palaeozoic sediments of southern Ontario ..•.••. D. T.A. Symons 9 4. Overhauser magnetometer progress report ..• ••..•.•.•..•.••••.•••••••• S. Washkurak 10 MINERAL DEPOSITS 5. Study of iron deposits in the Soviet Union ••••••.•••..•.•.•.••.•..•.••.•.. G. A. Gross 11 6. Tin and beryllium in the Cassiar District, Yukon and British Columbia ••.•.••.•... R. Mulligan 13 7. Titaniferous magnetite at Pipestone Lake, Manitoba .••••.....••••.•••••..•• E. R. Rose 13 8. Nickel distribution in serpentinites from Puddy Lake, Ontario P. R. -
Geological Survey Canada
GEOLOGICAL PAPER 68-15 SURVEY OF CANADA DEPARTMENT OF ENERGY MINES AND RESOURCES CARBONIFEROUS AND PERMIAN STRATIGRAPHY OF NORTHEASTERN BRITISH COLUMBIA (Report, 3 figures) E.W. Bamber, G. C. Taylor, R. M. Procter Price, $1.50 1968 GEOLOGICAL SURVEY OF CANADA CANADA PAPER 68-15 CARBONIFEROUS AND PERMIAN STRATIGRAPHY OF NORTHEASTERN BRITISH COLUMBIA E.W. Bamber, G. C. Taylor, R. M. Procter DEPARTMENT OF ENERGY , MINES AND RESOURCES © Crown Copyrights reserved Available by mail from the Queen's Printer, Ottawa, from Gcologica I Survey of Canada, 601 Booth St., Ottawa, and at the following Canadian Government bookshops: HALIFAX 1735 Barrington Street MONTREAL £terna-Vie Building, 1182 St. Catherine St. West OTTAWA Daly Building, Corner Mackenzie and Rideau TORONTO 221 Yonge Street WINNIPEG Mall Center Bldg., 499 Portage Avenue VANCOUVF.R 657 Granville Street or through your bookseller Price $1. 50 Catalogue No. M44-68- l 5 Price subject to change without notice ROGER DUHAMEL, F.R.S.C. Queen's Printer and Controller of Stationery Ottawa, Canada 1968 - iii - CONTENTS Page Abstract..... ...... .. ..... .. ... .. .. .. ... ............... ..... .. v Introduction. 1 Previous Work . 1 Present work and acknowledgments . 3 Stratigraphy. 3 Besa River Formation. 3 Table of formations .... ..... ... ..... ....... ... " . 4 Prophet Formation.... 6 Stoddart Formation (Mattson). 8 Sub-Permain unconformity . 9 Kindle Formation .. .. ........... : . 10 Sub-Fantasque unconformity. 11 Fantasque Formation . 12 Summary. ....... ... ............. ....... ... ..... ................... 13 References . 17 Table I. Surface stratigraphic sections . 22 Table II. Subsurface stratigraphic sections. 24 Illustrations Figure 1. Distribution of Carboniferous and Permian rocks and locations of sections. 2 Figure 2. Diagrammatic east-west cross-section along latitude 58° 00' north . 15 Figure 3. Diagrammatic north-south cross-section at longitude 124° 00' west.