Guidebook to Permafrost and Related Features of the Northern Yukon Territory and Mackenzie Delta, Canada
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Tc-Forty-Mile-Cheda-Dek-Guide.Pdf
Published 2011. ISBN 978-1-55362-538-4 For more information about Forty Mile, Fort Cudahy and Fort Constantine Historic Site, visit the Dänojà Zho cultural centre in Dawson or contact: Tr’ondëk Hwëch’in Heritage P. O. Box 599, Dawson City, Y0B 1G0 1242 Front Street, Dawson City Main office phone: (867) 993-7100 Dänojà Zho office phone: (867) 993-6768 Fax: (867) 993-6553 Email: [email protected] Tr’ondëk Hwëch’in website: www.trondek.ca Forty Mile web site: http://trondekheritage.com/our-places/forty-mile/ Yukon Historic Sites P. O. Box 2703, Whitehorse, Yukon Y1A 2C6 Phone: (867) 667-5386 Fax: (867) 667-8023 www.tc.gov.yk.ca/historicsites.html Cover images: Map, Yukon Archives H-1393 YG photo Yukon Archives, Alaska Historical Library #4221 Forty Mile circa 1890. Guide to Forty Mile The Forty Mile townsite is part of the Forty trading post and store established in 1893. Mile, Fort Cudahy and Fort Constantine Both of these sites are across the Fortymile Historic Site. The site is located at the River from the townsite of Forty Mile. The mouth of the Fortymile River where ground is marshy and the remains are fragile it empties into the Yukon River, 67 km so it recommended that visitors restrict their upstream from the Alaska/Yukon border activities to the Forty Mile townsite. and 88 km downriver from Dawson City. The Forty Mile, Fort Cudahy and Fort Generations of First Nation people camped Constantine Historic Site is protected under at the mouth of the Fortymile River to the Tr’ondëk Hwëch’in Final Agreement hunt and fish in the area. -
Sensors and Measurements Discussion
“Measurements for Assessment of Hydrate Related Geohazards” Report Type: Topical No: 41330R07 Starting March 2002 Ending September 2004 Edited by: R.L. Kleinberg and Emrys Jones September 2004 DOE Award Number: DE-FC26-01NT41330 Submitting Organization: ChevronTexaco Energy Technology Company 2811 Hayes Road Houston, TX 77082 DISCLAIMER “This report was prepared as an account of work sponsored by an agency of the United States Government. Neither the United States Government nor any agency thereof, nor any of their employees, makes any warranty, expressed or implied, or assumes any legal liability or responsibility for the accuracy, completeness, or usefulness of any information, apparatus, product, or process disclosed, or represents that its use would not infringe privately owned rights. Reference herein to any specific commercial product, process, or service by trade name, trademark, manufacturer, or otherwise does not necessarily constitute or imply its endorsement, recommendation, or favoring by the United States Government or any agency thereof. The views and opinions of the authors expressed herein do not necessarily state or reflect those of the United States Government or any agency thereof.” ii Abstract Natural gas hydrate deposits are found in deep offshore environments. In some cases these deposits overlay conventional oil and gas reservoirs. There are concerns that the presence of hydrates can compromise the safety of exploration and production operations [Hovland and Gudmestad, 2001]. Serious problems related to the instability of wellbores drilled through hydrate formations have been document by Collett and Dallimore, 2002]. A hydrate-related incident in the deep Gulf of Mexico could potentially damage the environment and have significant economic impacts. -
Yukon Aviation System Review (Yukon, 2016-17) Draft Plan #5 (100%): Phase 5 – Aviation System Review & Investment Recommendations
Government of Yukon Yukon Aviation System Review (Yukon, 2016-17) Draft Plan #5 (100%): Phase 5 – Aviation System Review & Investment Recommendations Project Number: 163601098 Date: May 23, 2017 Prepared for: From: Department of Highway and Stantec Public Works 202-107 Main Street Aviation Branch Whitehorse, YT, Y1A 2A7 Government of Yukon (867) 633-2400 Box 2703 Whitehorse, Yukon Y1A 2C6 Yukon Aviation System Review May 23, 2017 Sign Off Sheet This document entitled Yukon Aviation System Review, Draft Plan #5 was prepared by (“Stantec”) for the account of The Yukon Government (the “Client”). Any reliance on this document by any third party is strictly prohibited. The material in it reflects Stantec’s professional judgment in light of the scope, schedule and other limitations stated in the document and in the contract between Stantec and the Client. The opinions in the document are based on conditions and information existing at the time the document was published and do not consider any subsequent changes. In preparing the document, Stantec did not verify information supplied to it by others. Any use which a third party makes of this document is the responsibility of such third party. Such third party agrees that Stantec shall not be responsible for costs or damages of any kind, if any, suffered by it or any other third party as a result of decisions made or actions taken based on this document. Prepared by (signature) Warren Thompson Reviewed by (signature) Rod Savoie Yukon Aviation System Review May 23, 2017 Table of Contents Executive Summary ................................................................................................................. 1 GLOSSARY .............................................................................................................................. 11 1.0 INTRODUCTION .......................................................................................................... -
Surficial Geology Investigations in Wellesley Basin and Nisling Range, Southwest Yukon J.D
Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon J.D. Bond, P.S. Lipovsky and P. von Gaza Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon Jeffrey D. Bond1 and Panya S. Lipovsky2 Yukon Geological Survey Peter von Gaza3 Geomatics Yukon Bond, J.D., Lipovsky, P.S. and von Gaza, P., 2008. Surficial geology investigations in Wellesley basin and Nisling Range, southwest Yukon. In: Yukon Exploration and Geology 2007, D.S. Emond, L.R. Blackburn, R.P. Hill and L.H. Weston (eds.), Yukon Geological Survey, p. 125-138. ABSTRACT Results of surficial geology investigations in Wellesley basin and the Nisling Range can be summarized into four main highlights, which have implications for exploration, development and infrastructure in the region: 1) in contrast to previous glacial-limit mapping for the St. Elias Mountains lobe, no evidence for the late Pliocene/early Pleistocene pre-Reid glacial limits was found in the study area; 2) placer potential was identified along the Reid glacial limit where a significant drainage diversion occurred for Grayling Creek; 3) widespread permafrost was encountered in the study area including near-continuous veneers of sheet-wash; and 4) a monitoring program was initiated at a recently active landslide which has potential to develop into a catastrophic failure that could damage the White River bridge on the Alaska Highway. RÉSUMÉ Les résultats d’études géologiques des formations superficielles dans le bassin de Wellesley et la chaîne Nisling peuvent être résumés en quatre principaux faits saillants qui ont des répercussions pour l’exploration, la mise en valeur et l’infrastructure de la région. -
August 20 - 31, 2016 Get Caught in the Spell of the Glorious Yukon River This Summer
Aurora Yukon River Expedition August 20 - 31, 2016 Get caught in the spell of the glorious Yukon River this summer. The mysterious land beckons - it is calling you! Canoe through Klondike history, embark on a journey of summer dreams! The historic Yukon River runs through the ancient green-mantled, mountain ranges of the central Yukon. The trip starts at Pelly Crossing with two days on the Pelly River before we swing north to follow the Yukon right to Dawson City. Relaxed paddling on smooth current takes us through a remarkable region full of the lore of the Klondike Goldrush captured perfectly in the poetic words of Robert Service and the yarns of Jack London. The Yukon River has a heart of gold that shares the secrets of its recent history through its outdoor wilderness archives. A paddle down its length is a magical step into the past with the long-abandoned remains of cabins, paddle-wheelers, deserted communities, dredges and placer mines. This river bestows on paddlers not only the beauty and challenge of a northern canoe trip but also a remarkable encounter with the Klondike Gold Rush. The smooth and steady current of the Yukon River is ideal for novice to intermediate paddlers in search of a significant wilderness journey. There are no portages, some excellent hiking & fishing opportunities, beautiful & pristine scenery and surprisingly, very few mosquitoes to worry about at all as there is no standing water anywhere. There are many historic highlights along our journey: Pelly Farm is a remote operating wilderness family home; Stepping Stone, where we will stop for dinner, is an authentic Dawson Trail Roadhouse; Fort Selkirk is a beautifully restored Territorial Historic Site with a history that goes back 8000 years; Kirkman Creek is home to an operating placer mine and a bakery where we can enjoy fresh pie; and, Ancient Voices is a First Nation site where we can hike up to a riverside bluff. -
Yukon & the Dempster Highway Road Trip
YUKON & THE DEMPSTER HIGHWAY ROAD TRIP Yukon & the Dempster Highway Road Trip Yukon & Alaska Road Trip 15 Days / 14 Nights Whitehorse to Whitehorse Priced at USD $1,642 per person INTRODUCTION The Dempster Highway road trip is one of the most spectacular self drives on earth, and yet, many people have never heard of it. It’s the only road in Canada that takes you across the Arctic Circle, entering the land of the midnight sun where the sky stays bright for 24 hours a day. Explore subarctic wilderness at Tombstone National Park, witness wildlife at the Yukon Wildlife Preserve, see the world's largest non-polar icefields and discover the "Dog Mushing Capital of Alaska." In Inuvik, we recommend the sightseeing flight to see the Arctic Ocean from above. Itinerary at a Glance DAY 1 Whitehorse | Arrival DAY 2 Whitehorse | Yukon Wildlife Preserve DAY 3 Whitehorse to Hains Junction | 154 km/96 mi DAY 4 Kluane National Park | 250 km/155 mi DAY 5 Haines Junction to Tok | 467 km/290 mi DAY 6 Tok to Dawson City | 297 km/185 mi DAYS 7 Dawson City | Exploring DAY 8 Dawson City to Eagle Plains | 408 km/254 mi DAY 9 Eagle Plains to Inuvik | 366 km/227 mi DAY 10 Inuvik | Exploring DAY 11 Inuvik to Eagle Plains | 366 km/227 mi DAY 12 Eagle Plains to Dawson City | 408 km/254 mi Start planning your vacation in Canada by contacting our Canada specialists Call 1 800 217 0973 Monday - Friday 8am - 5pm Saturday 8.30am - 4pm Sunday 9am - 5:30pm (Pacific Standard Time) Email [email protected] Web canadabydesign.com Suite 1200, 675 West Hastings Street, Vancouver, BC, V6B 1N2, Canada 2021/06/14 Page 1 of 5 YUKON & THE DEMPSTER HIGHWAY ROAD TRIP DAY 13 Dawson City to Mayo | 230 km/143 mi DAY 14 Mayo to Whitehorse | 406 km/252 mi DAY 15 Whitehorse | Departure MAP DETAILED ITINERARY Day 1 Whitehorse | Arrival Welcome to the “Land of the Midnight Sun”. -
Cold-Climate Landform Patterns in the Sudetes. Effects of Lithology, Relief and Glacial History
ACTA UNIVERSITATIS CAROLINAE 2000 GEOGRAPHICA, XXXV, SUPPLEMENTUM, PAG. 185–210 Cold-climate landform patterns in the Sudetes. Effects of lithology, relief and glacial history ANDRZEJ TRACZYK, PIOTR MIGOŃ University of Wrocław, Department of Geography, Wrocław, Poland ABSTRACT The Sudetes have the whole range of landforms and deposits, traditionally described as periglacial. These include blockfields and blockslopes, frost-riven cliffs, tors and cryoplanation terraces, solifluction mantles, rock glaciers, talus slopes and patterned ground and loess covers. This paper examines the influence, which lithology and structure, inherited relief and time may have had on their development. It appears that different rock types support different associations of cold climate landforms. Rock glaciers, blockfields and blockstreams develop on massive, well-jointed rocks. Cryogenic terraces, rock steps, patterned ground and heterogenic solifluction mantles are typical for most metamorphic rocks. No distinctive landforms occur on rocks breaking down through microgelivation. The variety of slope form is largely inherited from pre- Pleistocene times and includes convex-concave, stepped, pediment-like, gravitational rectilinear and concave free face-talus slopes. In spite of ubiquitous solifluction and permafrost creep no uniform characteristic ‘periglacial’ slope profile has been created. Mid-Pleistocene trimline has been identified on nunataks in the formerly glaciated part of the Sudetes and in their foreland. Hence it is proposed that rock-cut periglacial relief of the Sudetes is the cumulative effect of many successive cold periods during the Pleistocene and the last glacial period alone was of relatively minor importance. By contrast, slope cover deposits are usually of the Last Glacial age. Key words: cold-climate landforms, the Sudetes 1. -
Rocky Mountain National Park Lawn Lake Flood Interpretive Area (Elevation 8,640 Ft)
1 NCSS Conference 2001 Field Tour -- Colorado Rocky Mountains Wednesday, June 27, 2001 7:00 AM Depart Ft. Collins Marriott 8:30 Arrive Rocky Mountain National Park Lawn Lake Flood Interpretive Area (elevation 8,640 ft) 8:45 "Soil Survey of Rocky Mountain National Park" - Lee Neve, Soil Survey Project Leader, Natural Resources Conservation Service 9:00 "Correlation and Classification of the Soils" - Thomas Hahn, Soil Data Quality Specialist, MLRA Office 6, Natural Resources Conservation Service 9:15-9:30 "Interpretive Story of the Lawn Lake Flood" - Rocky Mountain National Park Interpretive Staff, National Park Service 10:00 Depart 10:45 Arrive Alpine Visitors Center (elevation 11,796 ft) 11:00 "Research Needs in the National Parks" - Pete Biggam, Soil Scientist, National Park Service 11:05 "Pedology and Biogeochemistry Research in Rocky Mountain National Park" - Dr. Eugene Kelly, Colorado State University 11:25 - 11:40 "Soil Features and Geologic Processes in the Alpine Tundra"- Mike Petersen and Tim Wheeler, Soil Scientists, Natural Resources Conservation Service Box Lunch 12:30 PM Depart 1:00 Arrive Many Parks Curve Interpretive Area (elevation 9,620 ft.) View of Valleys and Glacial Moraines, Photo Opportunity 1:30 Depart 3:00 Arrive Bobcat Gulch Fire Area, Arapaho-Roosevelt National Forest 3:10 "Fire History and Burned Area Emergency Rehabilitation Efforts" - Carl Chambers, U. S. Forest Service 3:40 "Involvement and Interaction With the Private Sector"- Todd Boldt; District Conservationist, Natural Resources Conservation Service 4:10 "Current Research on the Fire" - Colorado State University 4:45 Depart 6:00 Arrive Ft. Collins Marriott 2 3 Navigator’s Narrative Tim Wheeler Between the Fall River Visitors Center and the Lawn Lake Alluvial Debris Fan: This Park, or open grassy area, is called Horseshoe Park and is the tail end of the Park’s largest valley glacier. -
Managing Winter Injury to Trees and Shrubs
Publication 426-500 Managing Winter Injury to Trees and Shrubs Diane Relf Extension Specialist, Horticulture, and Bonnie Appleton, Extension Specialist, Horticulture; Virginia Tech Reviewed by David Close, Consumer Horticulture and Master Gardener Specialist, Horticulture, Virginia Tech Introduction evergreen needles or leaves. It is worst on the side facing the wind. This can be particularly serious if plants are It is often necessary to provide extra attention to plants near a white house where the sun’s rays reflect off the in the fall to help them over-winter and start spring in side, causing extra damage. peak condition. Understanding certain principles and cultural practices will significantly reduce winter damage Management: Proper watering can is a critical factor in that can be divided into three categories: desiccation, winterizing. If autumn rains have been insufficient, give freezing, and breakage. plants a deep soaking that will supply water to the entire root system before the ground freezes. This practice is Desiccation especially important for evergreens. Watering when there Desiccation, or drying out, is a significant cause of dam- are warm days during January, February, and March is age, particularly on evergreens. Desiccation occurs when also important. water leaves the plant faster than it is taken up. Several environmental factors can influence desiccation. Needles Also, mulching is an important control for erosion and and leaves of evergreens transpire some moisture even loss of water. A 2-inch layer of mulch will reduce water during the winter months. During severely cold weather, loss and help maintain uniform soil moisture around the ground may freeze to a depth beyond the extent of roots. -
Oliva Vieira 2017.Pdf
Catena 149 (2017) 637–647 Contents lists available at ScienceDirect Catena journal homepage: www.elsevier.com/locate/catena Soil temperatures in an Atlantic high mountain environment: The Forcadona buried ice patch (Picos de Europa, NW Spain) Jesús Ruiz-Fernández a,⁎,MarcOlivab, Filip Hrbáček c, Gonçalo Vieira b, Cristina García-Hernández a a Department of Geography, University of Oviedo, Oviedo, Spain b Centre for Geographical Studies, Institute of Geography and Spatial Planning, Universidade de Lisboa, Lisbon, Portugal c Department of Geography, Masaryk University, Brno, Czech Republic article info abstract Article history: The present study focuses on the analysis of the ground and near-rock surface air thermal conditions at the Received 15 February 2016 Forcadona glacial cirque (2227 m a.s.l.) located in the Western Massif of the Picos de Europa, Spain. Temperatures Received in revised form 13 June 2016 have been monitored in three distinct geomorphological and topographical sites in the Forcadona area over the Accepted 27 June 2016 period 2006–11. The Forcadona buried ice patch is the remnant of a Little Ice Age glacier located in the bottom of a Available online 1 August 2016 glacial cirque. Its location in a deep cirque determines abundant snow accumulation, with snow cover between 8 and 12 months. The presence of snow favours stable soil temperatures and geomorphic stability. Similarly to Keywords: fi Soil temperatures other Cantabrian Mountains, the annual thermal regime of the soil is de ned by two seasonal periods (continu- Cirque wall temperatures ous thaw with daily oscillations and isothermal regime), as well as two short transition periods. -
Chapter 7 Seasonal Snow Cover, Ice and Permafrost
I Chapter 7 Seasonal snow cover, ice and permafrost Co-Chairmen: R.B. Street, Canada P.I. Melnikov, USSR Expert contributors: D. Riseborough (Canada); O. Anisimov (USSR); Cheng Guodong (China); V.J. Lunardini (USA); M. Gavrilova (USSR); E.A. Köster (The Netherlands); R.M. Koerner (Canada); M.F. Meier (USA); M. Smith (Canada); H. Baker (Canada); N.A. Grave (USSR); CM. Clapperton (UK); M. Brugman (Canada); S.M. Hodge (USA); L. Menchaca (Mexico); A.S. Judge (Canada); P.G. Quilty (Australia); R.Hansson (Norway); J.A. Heginbottom (Canada); H. Keys (New Zealand); D.A. Etkin (Canada); F.E. Nelson (USA); D.M. Barnett (Canada); B. Fitzharris (New Zealand); I.M. Whillans (USA); A.A. Velichko (USSR); R. Haugen (USA); F. Sayles (USA); Contents 1 Introduction 7-1 2 Environmental impacts 7-2 2.1 Seasonal snow cover 7-2 2.2 Ice sheets and glaciers 7-4 2.3 Permafrost 7-7 2.3.1 Nature, extent and stability of permafrost 7-7 2.3.2 Responses of permafrost to climatic changes 7-10 2.3.2.1 Changes in permafrost distribution 7-12 2.3.2.2 Implications of permafrost degradation 7-14 2.3.3 Gas hydrates and methane 7-15 2.4 Seasonally frozen ground 7-16 3 Socioeconomic consequences 7-16 3.1 Seasonal snow cover 7-16 3.2 Glaciers and ice sheets 7-17 3.3 Permafrost 7-18 3.4 Seasonally frozen ground 7-22 4 Future deliberations 7-22 Tables Table 7.1 Relative extent of terrestrial areas of seasonal snow cover, ice and permafrost (after Washburn, 1980a and Rott, 1983) 7-2 Table 7.2 Characteristics of the Greenland and Antarctic ice sheets (based on Oerlemans and van der Veen, 1984) 7-5 Table 7.3 Effect of terrestrial ice sheets on sea-level, adapted from Workshop on Glaciers, Ice Sheets and Sea Level: Effect of a COylnduced Climatic Change. -
Haines Highway Byway Corridor Partnership Plan
HAINES HIGHWAY CORRIDOR PARTNERSHIP PLAN 1 Prepared For: The Haines Borough, as well as the village of Klukwan, and the many agencies, organizations, businesses, and citizens served by the Haines Highway. This document was prepared for local byway planning purposes and as part of the submission materials required for the National Scenic Byway designation under the National Scenic Byway Program of the Federal Highway Administration. Prepared By: Jensen Yorba Lott, Inc. Juneau, Alaska August 2007 With: Whiteman Consulting, Ltd Boulder, Colorado Cover: Haines, Alaska and the snow peaked Takhinska Mountains that rise over 6,000’ above the community 2 TABLE OF CONTENTS 1. INTRODUCTION..............................................................5-9 2. BACKGROUND ON Byways....................................11-14 3. INSTRINSIC QUALITY REVIEW..............................15-27 4. ROAD & TRANSPORTATION SYSTEM...................29-45 5. ToURISM & Byway VISITATION...........................47-57 6. INTERPRETATION......................................................59-67 7. PURPOSE, VISION, GOALS & OBJECTIVES.......69-101 8. APPENDIX..................................................................103-105 3 4 INTRODUCTION 1 Chilkat River Valley “Valley of the Eagles” 5 The Haines Highway runs from the community byway. Obtaining national designation for the of Haines, Alaska to the Canadian-U.S. border American portion of the Haines highway should station at Dalton Cache, Alaska. At the half way be seen as the first step in the development of an point the highway passes the Indian Village of international byway. Despite the lack of a byway Klukwan. The total highway distance within Alaska program in Canada this should not prevent the is approximately 44 miles, however the Haines celebration and marketing of the entire Haines Highway continues another 106 miles through Highway as an international byway.