69-11676 Mckenzie, Garry Donald, 1941
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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 -
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. -
Glacial Geology of Adams Inlet, Southeastern Alaska
Institute of Polar Studies Report No. 25 Glacial Geology of Adams Inlet, Southeastern Alaska l/h':'~~~~2l:gtf"'" SN" I" '" '" 7, r.• "'. ~ i~' _~~ ... 1!!JW'IIA8 ~ ' ... ':~ ~l·::,.:~·,~I"~,.!};·'o":?"~~"''''''''''''~ r .! np:~} 3TATE Uf-4lVERSnY by t) '{;fS~MACf< ROAD \:.~i~bYMaUi. OHlOGltltM Garry D. McKenzie " Institute of Polar Studies November 1970 GOLDTHWAIT POLAR LIBRARY The Ohio State University BYRD POLAR RESEARCH CENTER Research Foundation THE OHIO STATE UNIVERSITY Columbus, Ohio 43212 1090 CARMACK ROAD COLUMBUS, OHIO 43210 USA INSTITUTE OF POLAR STUDIES Report No. 25 GLACIAL GEOLOGY OF ADAMS INLET, SOUTHEASTERN ALASKA by Garry D. McKenzie Institute of Polar Studies November 1970 The Ohio State University Research Foundation Columbus, Ohio 43212 ABSTRACT Adams Inlet is in the rolling and rugged Chilkat-Baranof Mountains in the eastern part of Glacier Bay National Monument, Alaska. Rapid deglaciation of the area in the first half of the twentieth century has exposed thick sections of post-Hypsithermal deposits and some of the oldest unconsolidated deposits in Glacier Bay. About 30 percent of the area is underlain by uncon solidated material; 14 percent of the area is still covered with ice. The formations present in Adams Inlet are, from the oldest to the youngest: Granite Canyon till, Forest Creek glaciomarine sediments, Van Horn Formation (lower gravel member), Adams lacustrine-till complex, Berg gravel and sand, Glacier Bay drift, and Seal River gravel. No evidence of an early post-Wisconsin ice advance, indicated by the Muir Formation in nearby Muir Inlet, is present in Adams Inlet. Following deposition of the late Wisconsin Granite Canyon till, the Forest Creek glaciomarine sediments were laid down in water 2 to 20 m deep; they now occur as much as 30 m above present sea level. -
A, Index Map of the St. Elias Mountains of Alaska and Canada Showing the Glacierized Areas (Index Map Modi- Fied from Field, 1975A)
Figure 100.—A, Index map of the St. Elias Mountains of Alaska and Canada showing the glacierized areas (index map modi- fied from Field, 1975a). B, Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the St. Elias Mountains in summer 1995. National Oceanic and Atmospheric Administration image from Mike Fleming, USGS, EROS Data Center, Alaska Science Center, Anchorage, Alaska. K122 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD St. Elias Mountains Introduction Much of the St. Elias Mountains, a 750×180-km mountain system, strad- dles the Alaskan-Canadian border, paralleling the coastline of the northern Gulf of Alaska; about two-thirds of the mountain system is located within Alaska (figs. 1, 100). In both Alaska and Canada, this complex system of mountain ranges along their common border is sometimes referred to as the Icefield Ranges. In Canada, the Icefield Ranges extend from the Province of British Columbia into the Yukon Territory. The Alaskan St. Elias Mountains extend northwest from Lynn Canal, Chilkat Inlet, and Chilkat River on the east; to Cross Sound and Icy Strait on the southeast; to the divide between Waxell Ridge and Barkley Ridge and the western end of the Robinson Moun- tains on the southwest; to Juniper Island, the central Bagley Icefield, the eastern wall of the valley of Tana Glacier, and Tana River on the west; and to Chitistone River and White River on the north and northwest. The boundar- ies presented here are different from Orth’s (1967) description. Several of Orth’s descriptions of the limits of adjacent features and the descriptions of the St. -
Pa 72-32.Pdf
GEOLOGICAL SURVEY OF CANADA CANADA PAPER 72-32 ROCKS AND MINERALS FOR THE COLLECTOR THE ALASKA HIGHWAY; DAWSON CREEK, BRITISH COLUMBIA TO YUKON/ALASKA BORDER Ann P. Sabina DEPARTMENT OF ENERGY, MINES AND RESOURCES @)Crown Copyrights reserved Available by mail from Information Canada, Ottawa from the Geological Survey of Canada 601 Booth St., Ottawa and Information Canada bookshops in HALIFAX - 1687 Barrington Street MONTREAL - 640 St. Catherine Street W. OTTAWA - 171 Slater Street TORONTO - 221 Yonge Street WINNIPEG - 393 Portage Avenue VANCOUVER - 800 Granville Street or through your bookseller Price: $2. 50 Catalogue No. :tv144-72-32 Price subject to change without notice Informa tion Canada Ottawa 1973 - iii - CONTENTS Page Abstract/Resume vii Introduction .................. ... .......................... .... A brief geological history ... ·. 3 Collecting along the route . 3 The Alaska Highway Kiskatinaw River occurrences................................. 5 Pine River occurrences....................................... 5 Peace River Valley occurrences............................... 7 Peace River Valley deposits . 8 Bog iron occurrence . 10 Ornamental quartzite occurrence . 13 Churchill Mine. 16 Toad River hot springs . 17 Liard River hot springs.................................... 19 Smith River occurrence . 20 Liard River placers.......................................... 21 The Campbell Highway . 22 Canada Tungsten Mine........................................ 22 King Jade Mines . 23 Road log to Cas siar, Dease Lake . 24 Cassiar Asbestos Mine . 26 Snowy Creek jade occurrence . 27 McDame Creek jade occurrence . 27 Cassiar gold occurrences . 28 Dease Lake area placers . 30 Dease Lake jade occurrences . 3 1 Fiddler Yukon Mine . 32 Seagull Creek occurrence..................................... 33 Road log along Canol Road to Ross River......... 34 Road log to Atlin . 36 Atlin-Ruffner Mine . 38 Atlin placer deposits . 38 Atlin Lake occurrence . 40 Engineer Mine . -
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. -
Geological Survey of Canada Miscellaneous Report SO
Geological Survey of Canada Miscellaneous Report SO DEPARTMENT OF ENERGY, MINES AND RESOURCES 1992 Geological Survey of Canada Miscellaneous Report 50 ROCKS AND MINERALS FOR THE COLLECTOR The Alaska Highway; Dawson Creek, British Columbia to Yukon/ Alaska border Ann P. Sabina 1992 © Minister of Supply and Services Canada 1992 Available in Canada through authorized bookstore agents and other bookstores or by mail from Canada Communication Group - Publishing Ottawa, Canada KI A OS9 and from Geological Survey of Canada offices: 601 Booth Street Ottawa, Canada KIA OE8 3303-33rd Street N.W., Calgary, Alberta T2L 2A7 100 West Pender Street Vancouver, B.C. V6B IRS A deposit copy of this publication is also available for reforence in public libraries across Canada Cat. No. M41-8/50E ISBN 0-660-14420-4 Price subject to change without notice Author's address Geological Survey of Canada 601 Booth Street Ottawa, Ontario K1AOE8 Aussi disponible enfranr;ais CONTENTS vii Abstract/Resume Introduction 1 A brief geological history 3 How to use this guide 5 The Alaska Highway 5 Kiskatinaw River occurrences 5 Pine River occurrences 7 Peace River Valley occurrences 8 Peace River Valley deposits 13 Tetsa River Ornamental quartzite occurrence 15 Churchill Mine 17 Toad River hot springs 19 Liard River hot springs 19 Smith river occurrence 20 Liard River placers 21 The Campbell Highway 21 Cantung Mine 22 King Jade Mine 22 Side trip to the Cassiar and Dease Lake areas 24 Cassiar Asbestos Mine 25 Snowy Creek jade occmTence 25 McDame Creek jade occurrence 26 Cassiar -
The Alsek River: a Canadian Heritage River
TheA CANADIAN Alsek HERITAGE River RIVER Third Ten-year Monitoring Report: 2009 to 2018 Prepared by: Kluane National Park and Reserve, Parks Canada for The Canadian Heritage Rivers Board JANUARY 2019 Acknowledgments This report was prepared by Mathew Trotter, Resource Management Officer II, and Carmen Wong, Ecologist, Team Leader, both from Parks Canada, Kluane National Park and Reserve. We are very grateful to reviewers from Champagne and Aishihik First Nations, Sheila Greer, Micheal Jim and Monica Krieger, for their input. Parks Canada. 2019. The Alsek River: A Canadian Heritage River. Third Ten-year Monitoring Report: 2009 to 2018. Report to the Canadian Heritage Rivers Board. La rivière Alsek : une rivière du patrimoine canadien. Troisième rapport de surveillance décennal : 2009 2018. Aussi disponible en français For more information, contact: Kluane National Park and Reserve [email protected] © 2019 HER MAJESTY THE QUEEN IN RIGHT OF CANADA as represented by the Chief Executive Officer of Parks Canada. Cat. No. R64-553/2019F-PDF ISBN: 978-0-660-31507-2 Cover Photo: Lowell Glacier with the Alsek River in the foreground. Executive Summary The Alsek River is one of Canada’s most outstanding wilderness rivers. It begins in Kluane National Park and Reserve, Yukon, and flows 250 km through the glaciated valleys of the St. Elias Mountains until it reaches the Pacific Ocean in Glacier Bay National Park and Preserve, Alaska. The entire length of the Alsek River falls within the Kluane / Wrangell–St. Elias / Glacier Bay / Tashenshini–Alsek UNESCO World Heritage Site, which is one of the largest internationally protected land-based ecosystems in the world. -
Preliminary Investigation Into the Geologic Relationships in the Granite Lake Area, Parts of NTS 115A/10, 11, 14, and 15, Southwest Yukon
preliminary investigation into the geologic relationships in the Granite lake area, parts of ntS 115a/10, 11, 14, and 15, southwest Yukon Steve Israel1 Yukon Geological Survey, Whitehorse, YT Rachel Kim Queen’s University, Kingston, ON Israel, S. and Kim, R., 2014. Preliminary investigation into the geologic relationships in the Granite Lake area, parts of NTS 115A/10, 11, 14, and 15, southwest Yukon. In: Yukon Exploration and Geology 2013, K.E. MacFarlane, M.G. Nordling, and P.J. Sack (eds.), Yukon Geological Survey, p. 79-91. aBStraCt Bedrock mapping, during the summer of 2013, within the Granite Lake area was completed as part of the first year of a multi-year project to investigate the geological relationships in southwest Yukon. Several different tectonostratigraphic elements were identified including rocks of the Yukon-Tanana terrane, the Kluane schist, and the Bear Creek assemblage. These were tectonically juxtaposed into a northeast dipping structural stack with the Yukon-Tanana terrane occupying the highest structural level, followed by the Kluane schist and the Bear Creek assemblage. Two plutonic phases of probable mid-Cretaceous and Late Cretaceous age were identified to intrude the Kluane schist and the Yukon- Tanana terrane respectively. A large Paleocene aged batholithic intrusive suite, the Ruby Range suite, intrudes across all tectonic boundaries. Tectonic and stratigraphic relationships observed in southwest Yukon are strikingly similar to those found in southeast Alaska, near Juneau. These similarities increase the potential for Juneau gold-belt type mineralizing systems extending into southwest Yukon. 1 [email protected] Yukon Exploration and GEoloGY 2013 79 Yukon GeoloGical ReseaRch introduCtion terranes across the Tertiary Denali fault to the west/ southwest, and juxtaposed next to the Jura-Cretaceous The Granite Lake area (parts of NTS 115A/10, 11, 14, Dezadeash Formation and the enigmatic Bear Creek and 15) is located east of Haines Junction and north of assemblage across an unnamed fault in the southwest Dezadeash Lake (Fig. -
The Squaw Creek- Rainy Hollow Area
BRITISH COLUMBIA DEPARTMENT OF MINES HON. R. C. MACDONALD,Minister JOHN F. WALKER,Deputy Minister BULLETIN No. 25 THE SQUAW CREEK- RAINY HOLLOW AREA Northern.British Columbia By K. DeP. Watson 1948 4 LIST OF ILLUSTRATIONS . Geological Map of Squaw Creek-Rainy Hollow area ............................................... an pocket Fig. 1. Key-map of north-western British Columbia, showing 1oc:ation of Squaw Creek-Rainy Hollow area................................................................................................. 9 Fig. 2. Map of part of Squaw Creek........................................................................... In pocket Fig. 3. Geological map of part of Maid of Erin' claim facing 42 Fig . 4 . Cross-sections of part of Maid of Erin claim ......................................................... 45 Fig . 5 . Geological map of part of State of Montana claim ............................................. 49 Fig . 6. Geological map of part of Adamsclaim 51 Fig . 7. Geological map of part of Victoria claim .............................................................. 54 Fig. 8. Geological map of part of Lawrence claim ............................................................. 56 Plate I- A . Coast Mountains; view eastward across head of Clayton Clreek ...................... 63 B . View up valley of Inspector Creek toward Nadahini Mounta.in .......................... 63 Plate II- A . Looking south-westward from Lawrence claim, Rainy Hollow.......................... 64 B . Looking north-westward from Maid of Erin claim, -
The Varsity Outdoor Ckh Journal
The Varsity Outdoor Ckh Journal VOLUME XV111 1975 ISSN 0524-5613 The Vmvet&lh) of Vtituh Columbia Vancouver, Canada PRESIDENT'S MESSAGE During the past year I have been confronted with two frequent questions: "Just what does the V.O.C. do?" and "What do I get for my $10?" In reply to the first question, I say that the V.O.C. provides a mechanism whereby one can meet others with similar interests and pursuits in the outdoors. People in V.O.C. hike; climb mountains cliffs and buildings; go skiing, ski touring, ski mountaineering, and cross country skiing; walk along beaches; play floor hockey; have parties; and most important of all, have a good time. V.O.C.'ers enjoy the outdoors, the mountains, the beaches, the powder slopes and invite others to join them. The second question is a little more dis turbing. I can say that the V.O.C.: produces the VOCene once a week to keep people informed, publishes a climbing schedule, provides equipment and books for loan, entertains you with slide shows on Wednesday at noon, brings in guest speakers, has an annual banquet, and publishes a journal every year. But somehow, I feel that people should be asking, "What can I do to make the club a success? How can I help to make this year even better?" Maybe I am starting to creep over the hill, but it seems that attitudes are changing. Apathy is- creeping everywhere. People like to sit on their butts and have everything done for them. How ever, the old adage is still true - you only get out what you are willing to put in (and that includes your $10). -
Physiographic Divisions of Alaska
PHYSI DIVISIONS 0 ALASKA 0 GEOLOGICAL SURVEY PROFESSIONAL PAPER 482 Physiographic Divisions of Alaska By CLYDE WAHRHAFTIG GEOLOGICAL SURVEY PROFESSIONAL PAPER 482 A classification and brief description with a discussion of high-latitude physiographic processes UNITED STATES GOVERNMENT PRINTING OFFICE, WASHINGTON 1965 UNITED STATES DEPARTMENT OF THE INTERIOR STEWART L. UDALL, Secretary GEOLOGICAL SURVEY Thomas B. Nolan, Director Library of Congress catalog-card No. GS 65-800 For sale by the Superintendent of Documents, U.S. Government Printing Office Washington, D.C. 20402 CONTENTS Page Abstract------------------------------------------- 1 Description of the physiographic divisions--Continued Introduction ______________________________________ _ 2 Intermontane Plateaus--Continued Acknowledgments _________________________________ _ 3 Western Alaska province-Continued The basis for the classification ______________ ·~--------- 3 Kuskokwim Mountains _________________ _ 30 Summary of the geologic history of Alaska ____________ _ 5 Innoko Lowlands ______________________ _ 30 Details of sculpture-physiographic evolution in the last Nushagak-Big River Hille- _____________ _ 30 million years------------------------------------- 8 Holitna Lowland _______________________ _ 31 Glaciated highlands and mountains ______________ _ 13 Nushagak-Bristol Bay Lowland _________ _ 31 Glaciated lowlands _____________________________ _ 13 Seward Peninsula __________________________ _ 31 U nglaciated uplands ___________________________ _ 14 Bering Shelf ______________________________