Landforms of British Columbia 1976

Total Page:16

File Type:pdf, Size:1020Kb

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. This bulletin is an authoritative account of the major land subdivisions of British Columbia. It defines the boundaries of the vario’us mountain, plateau, or plain areas, many of them for the first time. Agreement has been reached with the Canadian Permanent Committee on Geographical Names, with Provincial Govern- ment officials, and with geologists and the various sorts of map-makers whose knowledge of the Province is most thorough. In particular, close attention has been paid to H. S. Bostock’s “ Physiography of the Canadian Cordillera, with Special Reference to the Area North of the Fifty-fifth Parallel,” which has heretofore been the chief authority, and any departures from that work have been fully discussed with Dr. Bostock. The form of presentation, and much of the subject-matter, is a reflection of the mind and the interests of the writer, who is a field geologist with a broad knowl- edgeof the Province. Thus the reader is aware throughout of the principal processes that have formed the land as we now see it, and of the reasons for much of the character of the scenery and landforms. Concluding are five short essaysthat are written to clarify the text, and a complete glossary of terms. This bulletin is more than an enunciation of physical boundaries and is, it is hoped, a source book for the better knowledge and understanding of the face of British Columbia. The average reader will surely find much to interest him, though he may care little about the precise boundaries of the Spat&i Plateau, the Tagish Highland, or of other places he may never visit. Literally thousands of air photographs have been examined in the preparation of this bulletin, and many of the finest photographs available have been chosen to illustrate each subdivision mentioned in the table of contents. It is suggestedthat the reader study the photographs and their captions and refer to the text (Chapter II) for further description. The five essaysof Chapter III are written to be read alone, but constant reference to the illustrations and descriptive text makes them more interesting. This is not the sort of bulletin to be read and digested at one sitting. The technical references are believed to be complete. There are, however, publications such as The Canadian Alpine Journal, Canadian Geographic Journal, and others that have not been mentioned but will furnish interesting auxiliary read- ing. This bulletin, it should go without saying, should spur interest in the general study of geology and physiography. H. SARGENT, Chief, Mineralogical Branch. TABLE OF CONTENTS P.&GE Chapter I.-Introduction . -----.- -- . ..---- . ----.-..--..---- ----- ---.----.---.--- ------.---- ---- 13 Development of Landforms .--------.-.------..---------.-. ------ -.--.--- -- ------- -------------.- -- 13 Influence of Process.....--- ------- --------- -- .--- ------ ----..-.- --- -------- -..- -------------- 14 Influence of Bedrock--------.--.-.-.----- --- ------------------.. ---- ---- ------ ----- ---------- 15 Influence of Orogenic History.--------------- -- -----------------------. ---------- ----- 21 Summary of Physiographic History of British Columbia.-..-------------------...- 22 System of Subdivision.----...-.---.-.-... ~.----- .-.-.- ---~--~------- ---------.-.. -- ---.. ----- ----...- 23 Previous Work- ---------- --.-.-------- ------- ---------.-------------------------..--------- ------ 23 Sources of Information .--.-.-.-.-.---- ------.- -------- --------. --- -----.-.------------ -----.. 24 Selection of Boundaries----------.- ---- .-....- ------.-.--- .--.-...---- ------- ---.-- --- ----.- 24 Illustrations .--.----------.----------.------ ----.--- ----.-..- ------- ..------.---..-.-........--.---.-.------- 25 Bibliography --.-----..--.-.-.-..--..--------.-..-----.---------------.--.- -- -.-. - -----..-..--..-.-.-------- 26 Chapter II.-Physiographic Subdivisions of British Columbia-..---------..--------..-- 27 A. Canadian Cordillera..--------.-.. ---- -------- ---- -.------- ------.--.-.-.....-.....-.-.....-.-..-- 27 I. Western System..... ..--..----------- -----------.----------.-.--.........-...--..-..--.---..- 28 Outer Mountain Area.-.-----.-.. ---.- ---.--.-------.-------.------.--.---.--..-----.- 28 St. Elias Mountains .--..--....--------- -------- ---- ---- ----~~~--~.------ ----... 28 Fairweather Ranges------..----------------------..--.---..-------..- 29 Icefield Ranges-------V----.-.------ -- --------------..- ...-----------.--- 29 Alsek Ranges.---- - .-.------- ---- -------------. --..-.--.-- - --------- ----- 29 Duke Depression-.------. ------ .---- --- -.-... - -.-....-.------- --------... 29 Insular Mountains .-..--.--..--..-~~-~-----~-.....~~~~~.-..-..- - ----------- --- 30 Queen Clmd&te Mountains .-----------.--- ---- -.- ------------ ----. 30 Queen Charlotte Ranges------ -------------~ ---.- ------- -.--- 30 &idegate Plateau.---.-.------- -------. -..-....- - -...-.--- - ----- 30 Vancouver Island Mountains .~~~~~~~~~~~-.-.~~~.------- ------ -.-.- 31 Vancouver Island Ranges.--- ---- -...---..------- ---- -.-.- 31 Alberni Basin ..-..---.-.-----------------------..-------------.---32 Estevan Coastal Plain .-------------.-.-.-.....---------- ---..- 32 Coastal Trough .-------.-.-----.------- - -.-- ------- ----.---------.--.--- ----. .--.-------- 32 Hecate Depression.---- ..----.--.------- -----.--- ---- -..--.-- -- --------- ----- 33 Queen Charlotte Lowland .----- -.-.-.------------.----------------.- 33 Argonaut Plair-- ------...-------..-...--..-.-..-------..----.----34 Nahwitti Lowland ..------------- --------..-. - --..---.----------- ------ 34 Suquash Basin..-..--- ------- ------.-.---.--.---.----- ----- ------ 34 Hecate Lowland..-------------.---------------------..- - ------------.-- 34 Milbanke Strandflat------------.------.-.-.-.-- ----- --------- 35 Georgia Depression.--------------.------.-------.--------.--.-- ---.--.-------.- 35 Georgia Lowland .---....------------------------------..-- -- ------.. -.- 36 Fraser Lowland ..--------- -------------------- -.-------------- ---- 36 Nanaimo Lowland .---------------- ----- ---- -----------------.-------- 37 Coast Mountain Area--------.-----..----------- ---------------- ---- ------- -- --.- ---- 38 Coast Mountains .-.---- -...-------------.-.----------------...- ------ ---------- 38 Boundary Ranges---------------------------------- -----...--.-------- 39 Kitimat Ranges.--.------------------------------- -----------.---.------- 41 Pacific Ranges-- .-.----.------ ------- -- ------- ------- .---.------------ 42 Chilcotin Ranges------ ----------------. -.----------.-.-- 43 Cascade Mountains..------.-.-.-- ----- -- -------------- ------~ -.----- 43 Physiographic History of the Western System--------------------.---.--- 45 5 PAGE Chapter II.-Physiographic Subdivisions of British Columbia-Co&nued A. Canadian Cordillera-Continz.& II. Interior System.-------- ------- ..-----.-- --.--------- -...------.------- ---.----- ------ ----- 46 Northern Plateau and Mountain Area .--.-------.------- -----------------.--- 46 Yukon Plateau ..-.--- -.-...-.--- ---- -....---.-------..----- ----.----- -- ----------- 47 Tagish Highland.----.-.------...------- ------ ---!---- ---- --- -------..-- 47 Teslin Plateau------ -- --------.--------- ---------------------- ------------- 47 Nisutlin Plateau.-----.--...--...-.---- --- ---... - ---- ------ --------- ------ 48 Liard Plair------.------..---- --------~~-- ..--.... -- ---- -- ------..-- --.-------- - ---- 48 Central Plateau and Mountain Area ..-.--------------- ---..--.---------------- 49 Stikine Plateau.-.-----..-.--...-- ----.-- ..-.-. ------.--- ------.------------ ----- 49 Tahltan Highland .-.-.---..--......-----~~~------~---- ------------ ----- 49 Taku Plateau.-.----...---.....--.... ------~~~--- -.-.---- .----- ------------- 50 Kawdy Plateau..-...---.-.- -. ..-..---- ---- -- --..- -- --..------------.---- 5 1 Atsutla Range.----..-...-..-- --- ---- -- --...-.-.----- ----------.--- 52
Recommended publications
  • Incorporating Human Impacts Into Habitat Suitability Models
    INCORPORATING HUMAN IMPACTS INTO HABITAT SUITABILITY MODELS: A LITERATURE REVIEW Report Prepared for The Taku River Tlingit First Nation By Jean L. Polfus Research Assistant Round River Conservation Studies April 21, 2008 INCORPORATING HUMAN IMPACTS INTO HABITAT SUITABILITY MODELS Polfus Acknowledgments A diversity of people have assisted with the development and refinement of this report, the need for which was identified in collaborative discussions on habitat modeling between Taku River Tlingit Land and Resources Department and the British Columbia Integrated Land Management Bureau. I wish to acknowledge Kim Heinemeyer, Norm McLean and Kerrith McKay for initiating the project. The format and design of this report benefited from the influence of a literature review of the effects of energy development on ungulates by Mark Hebblewhite, who also provided guidance and advice. I thank the Heb Lab for general discussion and ideas about habitat suitability models. Kim Heinemeyer has provided helpful feedback and suggestions on earlier versions of the report. Please cite as: Polfus, J. L. 2008. Incorporating Human Impacts into Habitat Suitability Models: A Literature Review. Report prepared for the Taku River Tlingit First Nation. Cover photos: woodland caribou © Matt Grant, grizzly © Kevin Bernier, mountain goats © Sandra Leidholdt Page 2 INCORPORATING HUMAN IMPACTS INTO HABITAT SUITABILITY MODELS Polfus Table of Contents Acknowledgments..............................................................................................................
    [Show full text]
  • Ecological Subsections of Glacier Bay National Park & Preserve, Sitka National Historic Park, Klondike Gold Rush National Historic Park
    ECOLOGICAL SUBSECTIONS OF GLACIER BAY NATIONAL PARK & PRESERVE, SITKA NATIONAL HISTORIC PARK, KLONDIKE GOLD RUSH NATIONAL HISTORIC PARK Mapping and Delineation by: Gregory Nowacki, Michael Shephard, William Pawuk, Gary Fisher, James Baichtal, David Brew, Evert Kissinger and Terry Brock, USDA Forest Service Photographs by: USDA Forest Service Alaska Region Inventory and Monitoring Program 2525 Gambell Anchorage, Alaska 99503 Alaska Region Inventory & Monitoring Program 2525 Gambell Street, Anchorage, Alaska 99503 (907) 257-2488 Fax (907) 264-5428 Ecological Subsections of Glacier Bay National Park & Preserve Klondike Gold Rush National Historic Park Sitka National Historic Park 2001 Excerpts from Ecological Subsections of Southeast Alaska and Neighboring Areas of Canada Gregory Nowacki, Michael Shephard, William Pawuk, Gary Fisher, James Baichtal, David Brew, Evert Kissinger and Terry Brock USDA Forest Service, Alaska Region Technical Publication R10-TP-75 October 2001 Table of Contents TABLE OF CONTENTS ..............................................................................1 ECOLOGICAL SUBSECTION DELINEATION CRITERIA AND MAPPING..2 HIERARCHICAL ARRANGEMENT AND FINAL CORRECTION..................4 GLACIER BAY NATIONAL PARK AND PRESERVE ...................................1 Icefields...................................................................................................1 SAINT ELIAS—FAIRWEATHER .....................................................................1 Recently Deglaciated Areas .................................................................3
    [Show full text]
  • Babine Lake Region and Covers the Central Part of the Babine Porphyry Belt
    T L a a k ke la M o r r is o n L a k e H a La u k te e te Hearne Hill East Hautete Lake H a tc h e r y A r m Natowite B a Old Fort Lake L b a in Mountain ke e Smithers Landing Nizik McKendrick Lake Island Ba b in e L H a a g a k n e A r m Ministry of Employment and Investment Energy and Minerals Division Geological Survey Branch TILL GEOCHEMISTRY OF THE OLD FORT MOUNTAIN MAP AREA, CENTRAL BRITISH COLUMBIA (NTS 93Ml1) By Victor M. Levson, Stephen J. Cook, Jennifer Hobday, Dave H. Huntley, Erin K. O'Brien, Andrew J. Stumpf and Gordon Weary OPEN FILE 1997- 1Oa INTRODUCTION - - - - This paper describes selected results of a till in low-lying drift-covered regions of the northern Interior geochemical sampling program conducted in the Old Fort Plateau. For example, prior till and lake sediment Mountain map area (NTS 93 M/1) by the British geochemistry surveys in the Nechako River map ania Columbia Geological Survey as part of a comprehensive (NTS 93F) to the south were successful in delineating survey of the entire Babine copper porphyry belt. The several areas of known mineralization (Cook et al., 1995; results of complimentary lake sediment geochemistry ad Levson and Giles, 1997) and in revealing locations of new bedrock geology mapping progms are presented by Cook mineralized zones. For this reason, till geochemical et al. (1997%b) and MacIntyre et al. (1997%b in pocket), studies in the Babine porphyry belt have been conducted in respectively.
    [Show full text]
  • Wildlife Species Habitat Models and Final Wildlife Suitability Ratings for the Itcha / Ilgachuz Area
    Wildlife Species Habitat Models and Final Wildlife Suitability Ratings for the Itcha / Ilgachuz Area Prepared for: Wildlife Branch Ministry of Environment, Lands and Parks Williams Lake, BC. Prepared By: Stefan Himmer and Damian Power Arctos Wildlife Services Hagensborg, BC. June 1999 TABLE OF CONTENTS 1.0 INTRODUCTION ...................................................................................................................1 1.1 INTRODUCTION ..............................................................................................................1 1.2 STUDY AREA..................................................................................................................1 2.0 METHODS ..............................................................................................................................3 3.0 LITERATURE CITED............................................................................................................4 4.0 WILDLIFE SPECIES ACCOUNTS AND HABITAT RATING METHODS .......................5 4.1 NORTHERN CARIBOU .....................................................................................................5 4.1.1 Name:...........................................................................................................................5 4.1.2 Status:...........................................................................................................................5 4.1.3 Distribution ..................................................................................................................5
    [Show full text]
  • 20. Aboriginal Rights and Interests Effects
    20. ASSESSMENT OF ABORIGINAL AND TREATY RIGHTS AND RELATED INTERESTS 20.1 INTRODUCTION This chapter assesses potential adverse effects on Aboriginal and Treaty rights and related interests which may arise from the Project during construction, operations, decommissioning/reclamation, and post-closure. Underground mining activities have the potential to adversely affect Aboriginal and Treaty rights by interfering with Aboriginal groups’ ability to engage in practices, customs, and traditions that are integral to their distinctive cultures, and/or by interfering with the exercise of rights expressly recognized in a treaty. Interference with Aboriginal and Treaty rights is generally indirect, resulting from changes to environmental conditions that are necessary for the continued exercise of Aboriginal and Treaty rights. The assessment is based on information derived from the Proponent’s engagement with potentially- affected Aboriginal groups, environmental assessments carried out elsewhere in the Application/EIS, and the review of secondary data. Wherever possible, the assessment addresses potential effects on Aboriginal and treaty rights and related interests as understood from the perspective of the Aboriginal groups in question. Baseline reports informing this assessment are appended to the Application/EIS and include: Ethnographic Overview and Traditional Knowledge and Use Desk-Based Research Report (Appendix 17-A) and Saulteau First Nations Knowledge and Use Study for HD Mining Murray River Coal Project (Appendix 17-B). 20.2 REGULATORY AND POLICY FRAMEWORK The Crown has a legal duty to consult with and, where appropriate, accommodate Aboriginal interests when it contemplates a conduct that might adversely impact the potential or established Aboriginal or Treaty right. The Crown delegated procedural aspects of this duty, with respect to the Project, to the Proponent through the Section 11 Order and EIS Guidelines.
    [Show full text]
  • Conserving Kispiox Fish Populations and Their Habitat
    Conserving Kispiox Fish Populations and their Habitat Kispiox Watershed Fish Sustainability Plan Stage II Briefing Backgrounder Ken A. Rabnett, Allen Gottesfeld, and Peter Hall Skeena Fisheries Commission March 2003 Conserving Kispiox Fish Populations and their Habitat Table of Contents Kispiox Watershed Fish Sustainability Plan.................................................................. 1 Preamble ......................................................................................................................... 1 Skeena WFSP Process .................................................................................................... 2 Kispiox WFS Plan........................................................................................................... 3 Kispiox Watershed Environmental Setting.................................................................... 6 Location ...................................................................................................................... 6 Hydrology ................................................................................................................... 6 Water Quality.............................................................................................................. 8 Stream Channels ....................................................................................................... 11 Geography................................................................................................................. 13 Geology....................................................................................................................
    [Show full text]
  • British Columbia Ministry of Natural Resource Operations Regional
    T a t s h e n s h in i R i v e r K r e Tutshi Lake l e s v a i ys R ll d iv R r R la e r e k i v G iv e e Swift R L iver Petitot River s r R B a Petitot R l t e Gladys Lake iver if av B A e ic Hall Lake w r h Tagish Lake S R e Teslin Lake w R iv Ri Cro iv e ve i er k e r r w ft Riv e r P S et r re Maxhamish Lake it e o C t Surprise Lake iv er Riv s R R ia u ek iv s her er g re e nc iv n C r y Ra R r illy Peti d A e tot R a e e i l l u k v D v t l c i S e G it B a a r J l R h L d e B G o r h a n ree t r n i a ve it C k y Liard River er a i n k ling iv h R in n m R i R C O l g l iv 'Don e s S e a n K r e r Riv Ts e Atlin Lake er e r k S R e h iver v e nts R i e d k A R e R a i r i n l e s v er V K a h i wig i iv e R C oko a ree R Sl R n k i R i k T M iv a cDame Cre a v e e N k u C ek p r r e y i G o d lu e a ndeb Cr t R ery t T R o i e n ve T s i r r li v w er o e o n od Riv iv u er Gu R r R nda a se R h t i De o R v a e Tuya Lake o Sa Kotcho Lake r i h b I r R v t n e e a b i k v v r n l i i it e e n R R r h R Nahl r in e R iv e l er i iv e R iv v e i r i r T ve i R N r v M ro R u e r t D e e R ud s u i r K e v i r t e e d a l o s r iv le g F o R d o e r K r n a n ive in o e D R d Cr k o v t e u d e e r i r E C n Fort Nelson t e R a ch iv e R o u y v r D o R i e T a i D R v e ek H e a re e k o C n r Cry Lake T l ykl i urn l K h aga iver R la in R t iv u e Nets on S r Cre e S Dease Lake k h e B K Elleh Cre s e utc ek la a h tt o y y Cr R e T C ek r o nta iv Ri e s Creek Fo s r v iv e e lla e r a v e nzi r e R d R r a e e T v g h i i o R
    [Show full text]
  • Alberta with the Establishment of Castle the Following Conservation Achievements
    Annual Report 2017 in Review The Yellowstone to Table of contents Yukon region A letter from Jodi 3 Key advancements 4 in the Y2Y region Dawson Protected areas and 6 connected lands Solutions that help wildlife and 8 Whitehorse people thrive Advancing science and policy 10 Communities coming together 12 for conservation Partner power 14 Fort St. John Funders 16 Prince George Financials 17 Edmonton Global support 18 Banff Vancouver Calgary Our vision Seattle Spokane Missoula An interconnected system of wild lands and water stretching Bozeman from Yellowstone to Yukon, Jackson harmonizing the needs of Boise people with those of nature. Our mission Connecting and protecting habitat from Yellowstone to Yukon so that people and nature can thrive. 2 Cover: Elk nuzzle. Photo credit: Darcy Monchak. Current page: Larches at Avalanche Lake in Glacier National Park. Photo credit: Jacob W. Frank/National Park Service. Big landscape requires big vision A letter from our President and Chief Scientist ellowstone to Yukon (Y2Y) Conservation This annual report throws a spotlight on some YInitiative’s grand vision — of an of the many organizations and individuals interconnected system of wild lands and working toward a sustainable future. These waters from Yellowstone to Yukon, groups and people have contributed time, harmonizing the needs of people with funds and expert knowledge to the bigger those of nature — takes time, resources picture and we thank them for it. and commitment. Effective large-landscape Thanks to your support and shared vision for conservation requires invested and interested a healthy landscape, we are able to make the individuals. It goes beyond financial progress you can read about in these pages.
    [Show full text]
  • Updated Technical Report and Mineral Resource Estimate on the Berg Project, British Columbia
    Updated Technical Report and Mineral Resource Estimate on the Berg Project, British Columbia PRESENTED TO Surge Copper Corp. EFFECTIVE DATE: MARCH 9, 2021 RELEASE DATE: MAY 3, 2021, REVISION 0 ISSUED FOR USE FILE: 704-ENG.VMIN03189-01 REPORT AUTHORS: Cameron Norton, P.Geo. John Huang, PhD., P.Eng. Daniel Lui, P.Geo. Tetra Tech Canada Inc. 150, 1715 Dickson Avenue Kelowna, BC V1Y 9G6 CANADA Tel 250.862.4832 Fax 250.862.2941 Report to: Surge Copper Corp. Updated Technical Report and Mineral Resource Estimate on the Berg Project, British Columbia Effective Date: March 9, 2021 Original signed and sealed by: Prepared By: Cameron Norton, P.Geo. John Huang, Ph.D., P.Eng. Senior Geologist Senior Metallurgist Date: Date: Kelowna, BC V1Y 9G6 Tel 250.862.4832 Fax 250.862.2941 RPT-Berg _NI 43-101_Final.docx UPDATED TECHNICAL REPORT & MINERAL RESOURCE ESTIMATE ON THE BERG PROJECT, BC FILE: 704-ENG.VMIN03189-01 | RELEASE DATE: MAY 3, 2021, REVISION 0 | ISSUED FOR USE TABLE OF CONTENTS 1.0 EXECUTIVE SUMMARY .............................................................................................................. 1 2.0 INTRODUCTION .......................................................................................................................... 4 2.1 Terms of Reference ............................................................................................................................... 4 2.1.1 Report Authors .........................................................................................................................
    [Show full text]
  • Wrangellia Flood Basalts in Alaska, Yukon, and British Columbia: Exploring the Growth and Magmatic History of a Late Triassic Oceanic Plateau
    WRANGELLIA FLOOD BASALTS IN ALASKA, YUKON, AND BRITISH COLUMBIA: EXPLORING THE GROWTH AND MAGMATIC HISTORY OF A LATE TRIASSIC OCEANIC PLATEAU By ANDREW R. GREENE A THESIS SUBMITTED iN PARTIAL FULFILLMENT OF THE REQUIREMENTS FOR THE DEGREE OF DOCTOR OF PHILOSOPHY in THE FACULTY OF GRADUATE STUDIES (Geological Sciences) UNIVERSITY OF BRITISH COLUMBIA (Vancouver) August 2008 ©Andrew R. Greene, 2008 ABSTRACT The Wrangellia flood basalts are parts of an oceanic plateau that formed in the eastern Panthalassic Ocean (ca. 230-225 Ma). The volcanic stratigraphy presently extends >2300 km in British Columbia, Yukon, and Alaska. The field relationships, age, and geochemistry have been examined to provide constraints on the construction of oceanic plateaus, duration of volcanism, source of magmas, and the conditions of melting and magmatic evolution for the volcanic stratigraphy. Wrangellia basalts on Vancouver Island (Karmutsen Formation) form an emergent sequence consisting of basal sills, submarine flows (>3 km), pillow breccia and hyaloclastite (<1 1cm), and subaerial flows (>1.5 km). Karmutsen stratigraphy overlies Devonian to Permian volcanic arc (—‘380-355 Ma) and sedimentary sequences and is overlain by Late Triassic limestone. The Karmutsen basalts are predominantly homogeneous tholeiitic basalt (6-8 wt% MgO); however, the submarine part of the stratigraphy, on northern Vancouver Island, contains picritic pillow basalts (9-20 wt% MgO). Both lava groups have overlapping initial and ENd, indicating a common, ocean island basalt (OIB)-type Pacific mantle source similar to the source of basalts from the Ontong Java and Caribbean Plateaus. The major-element chemistry of picrites indicates extensive melting (23 -27%) of anomalously hot mantle (‘—1500°C), which is consistent with an origin from a mantle plume head.
    [Show full text]
  • British Columbia Surficial Geology Map Index
    60°N 138°W 136°W est. 1895 G E Y 134°W O E LO RV GICAL SU 114O 132°W 120°W 130°W 122°W 60°N 128°W 126°W 124°W British Columbia Geological Survey 114P Atlin Open File 2019-03 version 202001 104M Sheet 1 of 2 104N 104O 094P 59°N 104P 094M 094N 094O 114I 136°W 138°W British Columbia surficial 59°N 104L geology map index Fort Nelson 104K 104J Dease Lake 094I 104I 094L 094K 094J H. Arnold and T. Ferbey 134°W 58°N 58°N Surficial geology index by map scale Scale 1:1,000 to 1:49,999 Scale 1:200,000 to 1:299,999 104F Scale 1:50,000 to 1:99,999 Scale 1:300,000 to 1:1,000,000 104G 094H Scale 1:100,000 to 1:199,999 Scale 1:5,000,000 (entirety of province) 104H 094E 094F 094G Presented here is a surficial geology map index for British Columbia. These maps have been 57°N 57°N produced by the British Columbia Geological Survey, the Geological Survey of Canada (GSC), and 104C Geoscience BC. To be included in this index maps have to be available for digital download. Each map is represented by the actual map extent or footprint rather than a bounding box or NTS sheet that it falls within. This provides an accurate representation of the areal extent of surficial geology mapping for British Columbia. 104B 094A 104A 094D 094C 094B The index is presented by map scale.
    [Show full text]
  • Riparian Management and the Tailed Frog in Northern Coastal Forests
    Forest Ecology and Management 124 (1999) 35±43 Riparian management and the tailed frog in northern coastal forests Linda Dupuis*,1, Doug Steventon Centre for Applied Conservation Biology, Department of Forest Sciences, University of British Columbia, Vancouver, BC, Canada V6T 1Z4 Ministry of Forests, Prince Rupert Region, Bag 5000, Smithers, BC, Canada V0J 2N0 Received 28 July 1998; accepted 19 January 1999 Abstract Although the importance of aquatic environments and adjacent riparian habitats for ®sh have been recognized by forest managers, headwater creeks have received little attention. The tailed frog, Ascaphus truei, inhabits permanent headwaters, and several US studies suggest that its populations decline following clear-cut logging practices. In British Columbia, this species is considered to be at risk because little is known of its abundance, distribution patterns in the landscape, and habitat needs. We characterized nine logged, buffered and old-growth creeks in each of six watersheds (n 54). Tadpole densities were obtained by area-constrained searches. Despite large natural variation in population size, densities decreased with increasing levels of ®ne sediment (<64 mm diameter), rubble, detritus and wood, and increased with bank width. The parameters that were correlated with lower tadpole densities were found at higher levels in clear-cut creeks than in creeks of other stand types. Tadpole densities were signi®cantly lower in logged streams than in buffered and old-growth creeks; thus, forested buffers along streams appear to maintain natural channel conditions. To prevent direct physical damage and sedimentation of channel beds, we suggest that buffers be retained along permanent headwater creeks. Creeks that display characteristics favoring higher tadpole densities, such as those that have coarse, stable substrates, should have management priority over less favorable creeks.
    [Show full text]