Geomorphology and Glacial Activity of Scimitar Glacier, Southern BC Coast

Total Page:16

File Type:pdf, Size:1020Kb

Geomorphology and Glacial Activity of Scimitar Glacier, Southern BC Coast Late Holocene glacial history of Scimitar Glacier, Mt. Waddington area, British Columbia Coast Mountains, Canada by Jessica Aileen Craig B.Sc., University of Victoria, 2010 A Thesis Submitted in Partial Fulfillment of the Requirements for the Degree of MASTER OF SCIENCE in the Department of Geography © Jessica Aileen Craig, 2012 University of Victoria All rights reserved. This thesis may not be reproduced in whole or in part, by photocopy or other means, without the permission of the author. ii Supervisory Committee Late Holocene glacial history of Scimitar Glacier, Mt. Waddington area, British Columbia Coast Mountains, Canada By Jessica Aileen Craig B.Sc. University of Victoria, 2009 Supervisory Committee Dr. Dan J. Smith, (Department of Geography) Supervisor Dr. John J. Clague (Department of Geography) Departmental Member iii Supervisory Committee Dr. Dan J. Smith, (Department of Geography) Supervisor Dr. John J. Clague (Department of Geography) Departmental Member Abstract Scimitar Glacier originates below the northeast face of Mt. Waddington in the southern British Columbia Coast Mountains and flows 18 km down valley to calve into a proglacial lake. The purpose of this research was to describe the late Holocene glacier history of Scimitar Glacier using stratigraphic analysis in conjunction with dendroglaciologic and radiocarbon dating techniques. Downwasting of the glacier surface has exposed stacked till units separated by wood-bearing horizons in the proximal slopes of lateral moraines flanking the glacier at several locations. Historical moraine collapse and erosional breaching has also revealed the remains of standing trees buried in sediments from a lake originally ponded against the distal moraine slope. Radiocarbon dating of detrital wood remains revealed that Scimitar Glacier expanded down-valley at least three times in the late Holocene. The earliest period of expansion occurred 3167-2737 cal yr BP in association with the regional Tiedemann Advance. Following this the glacier receded and downwasted prior to advancing to reconstruct the lateral moraine in 1568-1412 cal yr BP during the First Millennial Advance. The most recent phase of moraine construction was initiated during late Little Ice Age glacial expansion before 1742 AD and extended until at least 1851 AD, after which Scimitar Glacier began to recede and downwaste. iv Field investigations at Scimitar Glacier allowed for the construction of a late Holocene history of glacier expansion and lateral moraine construction that spans the last 3000 years. This record is comparable to that recorded at other glaciers in this region, and confirms the long-term relationship between regional climate trends and glacier behaviour in this setting. v Table of Contents Supervisory Committee ...................................................................................................... ii Abstract .............................................................................................................................. iii Table of Contents .................................................................................................................v List of Tables ..................................................................................................................... vi List of Figures ................................................................................................................... vii Acknowledgements ............................................................................................................ ix Chapter 1 – Introduction ..................................................................................................1 1.1 Introduction ...............................................................................................................1 1.2 Research Purpose and Objectives .............................................................................2 1.3 Thesis Format............................................................................................................3 Chapter 2 – Study Area ....................................................................................................4 2.1 Introduction ................................................................................................................4 2.2 The Waddington Range .............................................................................................4 2.3 Previous Research .....................................................................................................7 2.4 Summary .................................................................................................................10 Chapter 3 – Scimitar Glacier ..........................................................................................12 Chapter 4 – Research Methods ......................................................................................14 4.1 Introduction .............................................................................................................14 4.2 Aerial Photographic Interpretation Methods ..........................................................14 4.3 Field Methods ..........................................................................................................15 4.4 Laboratory Preparation and Analysis .......................................................................15 Chapter 5 – Observations ................................................................................................17 5.1 Prior Exploration and Aerial Photograph Interpretation .........................................17 5.2 Living tree-ring chronologies .................................................................................26 5.3 Dendroglaciological samples ..................................................................................26 5.3.1 Site 1 - Umbra Mountain .................................................................................27 5.3.2 Site 2 – Radiant Falls .......................................................................................31 5.3.3 Site 3 - Dispatch Lake ......................................................................................33 Stratigraphic interpretation ...................................................................................48 Chapter 6 – Discussion ....................................................................................................50 6. 1 Introduction ............................................................................................................50 6.2 Dating and Interpretation ........................................................................................50 Radiocarbon dating ...................................................................................................50 Tree-ring dating .........................................................................................................53 Interpretation .............................................................................................................54 6.3 Regional Synthesis ..................................................................................................56 Chapter 7 – Conclusions .................................................................................................58 7.1 Summary .................................................................................................................58 7.2 Limitations and Future Research ............................................................................59 vi List of Tables Table 5.1: Vertical and oblique aerial photographs of Scimitar Glacier, 1949-2005. .......22 Table 5.2: Chronology statistics for the locally derived living subalpine fir and whitebark pine chronologies. ..................................................................................................26 Table 5.3: Subfossil wood samples collected at three sites along the margins of Scimitar Glacier in July 2011. ..............................................................................................29 Table 6.1: Summary of radiocarbon-dated dendroglaciological evidence recovered along the margins of Scimitar Glacier at sites 1 and 3. ...................................................52 Table 6.2: Summary of tree-ring ages of samples recovered along the margins of Scimitar Glacier at sites 2 and 3. ..........................................................................................54 vii List of Figures Figure 1.1: View looking down Scimitar Glacier from Fury Gap. Photo by Phyllis Munday (Munday, 1928). ........................................................................................1 Figure 2.1: Map of the Scimitar Glacier study area showing study sites. ...........................5 Figure 2.2: Google Earth image of the Mt. Waddington Range area showing the locations of Confederation, Franklin, Tiedemann, Oval and Jambeau glaciers. Locations of living tree-ring width chronologies used in this study are also indicated. ..................................................................................................................8 Figure 5.1: Historical photo taken by Henry Hall Jr. showing the terminus of Scimitar Glacier as of 1931 (Hall, 1932). .............................................................................18 Figure 5.2: Illustration of lateral recession of Scimitar Glacier from Pocket Valley, 1949- 2005. The locations of the ice margin are derived from overlays of historical aerial photographs (A12973-171, NRCan; R60 26-F47,
Recommended publications
  • Cloudburst Publication 2008 FINAL for Electronic Distribution
    CLOUDBURST FEDERATION OF MOUNTAIN CLUBS OF BC Newsletter—2008 CLOUDBURST Cloudburst is published semi-annually by the Federation of Mountain Clubs of BC. Publication/Mail sales Agreement # 41309018. Printed by Hemlock Printers. Circulation 3500. Articles: We welcome articles which inform our readers about mountain access, recreation, and conservation issues or activities in B.C. Don’t limit yourself to prose: photographs Board of Directors and poems also accepted. Pieces should not exceed 1,000 President: Brian Wood (BCMC) words. Photos should be 150—300 DPI resolution. With Vice President: Peter Rothermel (IMR, ACC-VI) submitted articles please include the author. With submitted Secretary: Pat Harrison (VOA) photos please include location, names of people in the photo Treasurer: Don Morton (ACC-VI) and the name of the photographer. Directors Submission Deadlines: Paul Chatterton (Ind), Dave King (CR, ACC-PG), Bill Perry (IMR), Ken Rodonets (CDMC), Paul Geddes (ACC-Van), Brian Wood Fall/Winter - Oct 15 (BCMC), Peter Rothermel (ACC-VI), Pat Harrison (VOA) Spring/Summer - April 15 Committee Co-Chairs Advertising: The FMCBC invites advertising or classified Recreation and Conservation: Sandra Nichol, Antje Wahl advertising that would be useful to our members. Trails: Pat Harrison, Alex Wallace Rates: $400 back page $300 full page Staff $160 ½ page $80 ¼ page Bookkeeper: Kathy Flood $40 business card Administrative Manager: Jodi Appleton Editor/Production: Jodi Appleton ([email protected]) FMCBC The Federation of Mountain Clubs of British Columbia For More Information (FMCBC) is a non-profit organization representing the inter- www.mountainclubs.org ests of non-mechanized hikers and climbers, and outdoor PO Box 19673 clubs throughout British Columbia.
    [Show full text]
  • The Chilcotin Uprising: a Study Of
    THE CHILCOTIN UPRISING: A STUDY OF INDIAN-WHITE RELATIONS IN NINETEENTH CENTURY BRITISH COLUMBIA by EDWARD SLEIGH HEWLETT B.A,, University of British Columbia, 1964 A THESIS SUBMITTED IN PARTIAL FULFILMENT OF THE REQUIREMENTS FOR THE DEGREE OF MASTER OF ARTS in the Department of History We accept this thesis as conforming to the required standard THE UNIVERSITY OF BRITISH COLUMBIA March, 1972 In presenting this thesis in partial fulfilment of the requirements for an advanced degree at the University of British Columbia, I agree that the Library shall make it freely available for reference and study. I further agree that permission for extensive copying of this thesis for scholarly purposes may be granted by the Head of my Department or by his representatives. It is understood that copying or publication of this thesis for financial gain shall not be allowed without my written permission. Department of History The University of British Columbia Vancouver 8, Canada ill ABSTRACT This thesis deals with a disturbance which broke out in April of 1864 when a group of ChJLlcotin Indians massacred seventeen^workmen on a trail being built from Bute Inlet to the interior of British Columbia, The main endeavours of this thesis are three-fold. It seeks to provide an accurate account of the main events: the killings and the para-military expeditions which resulted from them. It attempts to establish as far as possible the causes of the massacres. Finally, it examines the attitudes of whites towards the Indians as revealed in the actions they took and the views they expressed in connection with the uprising and the resulting expeditions to the Chilcotin territory.
    [Show full text]
  • Scottish Coast Range Expedition 2002
    Scottish Coast Range Expedition 2002 West Pillar, Mount Gilbert (Photo: Simon Richardson) Contents 1. Introduction 3 2. The Team 3 3. Gurus, Climbing Literature and Maps 3 4. Climbing 4 5. Conclusion 6 6. Diary of Events 6 7. Expedition Accounts 7 8. Acknowledgments 7 Mt Raleigh, The Cleaver, Mt Gilbert (l-r) (aerial photograph from the west) (Photo: Bivouac.com) Page 2 1. Introduction The primary aim of the expedition was to climb a new line on the unclimbed, 3000’ south face of Mount Gilbert (3098m), situated in the Coast Range of British Columbia, Canada at Lat. 50° 52.0’N, Long. 124° 16.0’W. Secondary objectives included investigating a potential line on the west face of Mount Gilbert as well as other lines on adjacent mountains. 2. The Team Chris Cartwright 39 yr, British, Human Resource Professional Scottish Winter: Approx. 150 new routes, mostly Grade V and above with numerous Grade VII and harder. Highlights include Fubarbundy (VIII 7) on Liathach, Magic Bow Wall (VIII 8) on Sgurr an Fhidhleir, The Crack (VIII 8) on Ben Nevis, The Link Direct (VIII 7) on Lochnagar. Alps: Highlights include ascents of many summer classics plus first ascents of the South Pillar Freney Direct, Crystal Tripper on Aiguille Jardin and winter ascents including the Dru Couloir. Expeditions to Himalayas, Alaska and numerous trips rockclimbing throughout the world. Simon Richardson 43 yr, British, Petroleum Engineer. Scottish Winter: Approx 300 new routes (140 Grade V and harder, 30 Grade VII and harder). Highlights include first ascents of The Cardinal (VIII,8) Beinn a'Bhuird, The Crack (VIII,8) Ben Nevis, Magic Bow Wall (VIII,8) Sgurr an Fhidhleir, Redemption (VIII,7) Lochnagar.
    [Show full text]
  • Download FIA-03-04-0085.Pdf
    Sustainable Forest Management Plan Tatla Lake Operating Area Chilcotin Forest District, Williams Lake TSA Term: April 1, 2003 to December 31, 2004 FIA Project # 1007001 Submitted by: Tsi Del Del Enterprises Ltd. P.O. Box 4225, Williams Lake, B. C. V2G 2V3 Prepared by: DWB Forestry Services Limited Box 98, Lac La Hache, BC, V0K 1T0 March 31, 2003 Tatla Lake Sustainable Forest Management Plan March 31, 2003 The Tatla Lake Sustainable Forest Management Plan was prepared by: _____________________________________ Dave W. Bedford, R.P.F. DWB Forestry Services Ltd. Company Forester _____________________________________ Steve Capling, R.P.F. DWB Forestry Services Ltd. Forester The Tatla Lake Sustainable Forest Management Plan was approved by: _____________________________________ Philippe F. Theriault, R.P.F. Tsi Del Del Enterprises Ltd. Operations Forester _____________________________________ Brian Hansen Tsi Del Del Enterprises Ltd. General Manager Date: March 31, 2003. Tsi Del Del Enterprises Limited Page ii Tatla Lake Sustainable Forest Management Plan March 31, 2003 TABLE OF CONTENTS 1.0 INTRODUCTION ........................................................................................................... 1 1.1 PURPOSE........................................................................................................... 1 1.2 DESCRIPTION OF TATLA PLANNING AREA ............................................................. 2 1.3 MANAGEMENT RESPONSIBILITY ........................................................................... 3 1.4
    [Show full text]
  • 2017 SUMMIT of EXCELLENCE AWARD Don Serl
    2017 SUMMIT OF EXCELLENCE AWARD Don Serl The Banff Mountain Film and Book Festival is proud to announce Don Serl as the 2017 recipient of the Summit of Excellence Award, which recognizes an individual who has made a significant contribution to mountain life in Canada. Regarded as one of Canada’s most accomplished and prolific mountaineers, Serl has about 200 first ascents to his name. “With the Summit of Excellence Award now being presented to deserving recipients outside of the Canadian Rockies, Don Serl was an obvious and easy choice,” said Nancy Hansen, Summit of Excellence selection committee member. “Over several decades, Don has made significant contributions to Canadian mountain climbing and culture and is humble about his achievements, preferring to discuss new ideas and what others have done. He is a wealth of information about climbing on the West Coast and enjoys sharing his knowledge.” Born in Victoria and raised in Kamloops, Serl discovered a love for the mountains at the age of 25. while working as a chemist in Vancouver. In 1974, Serl trained in the Federation of Mountain Clubs of British Columbia (FMCBC) basic mountaineering course where he said his “energies and imagination were unleashed” and by 1975 he completed his initial first ascent on the north face of Mt Cheam in British Columbia. Since then “he has reigned as the preeminent Coast climber” according to author and climbing peer Chic Scott. Heavily influenced by Canadian climber Dick Culbert, Serl’s horizons opened after an Alpine Club of Canada trip into the multi-summitted Waddington Range, followed by numerous expeditionary trips into remote corners of the Coast Mountains in British Columbia.
    [Show full text]
  • Download Download
    "BEING A GIRL WITHOUT BEING A GIRL": Gender and Mountaineering on Mount Waddingtotty 1926-36 KAREN ROUTLEDGE LIVE IN A CITY SHAPED BY MOUNTAINS. I first realize this while standing on top of one. It is 8:00 AM on the summit of Mount Baker, a Cascade Ivolcano just south of the American border. The summer morning is already scorching; snow glitters and melts at my feet. I am looking at the region where I have spent most of my life, but it has become another planet: alien, stunningly beautiful, yet somehow familiar. The view is dizzying; there's so much light, so much heat, so much air. All around me, peaks are stacked upon peaks, layers of paling blue fading into the sun-bleached sky. The sight of all this land at once is overwhelming. I know this place but not like this. Ironically, while Mount Baker's snow-capped plateau is a prominent landmark to Vancouverites, the city is utterly insignificant from here. Vancouver lies buried somewhere to the northwest, a squat grey mass in a valley of haze and smog, a sprawling city limited by mountains in three directions. I look down at this map made real before me and finally understand the extent to which geography shapes the way we live. The mountains that surround Vancouver are far more than landmarks, sources of income, and tourist beacons. We have changed these mountains and been changed by them. From their slopes and summits, countless city people have glimpsed not only their home from a different perspective but also their own lives, values, and priorities.
    [Show full text]
  • Discoveryv47 2019 Final for Website
    Spectacular 2019 Niut Lakes Camp a Smashing Success by Stephen Partington WHAT AN AMAZING SETTING for a Nature loomed large to the west and south Vancouver camp! while the vast Chilcotin Plateau Twelve minutes or so in the heli- stretched invisibly to the east. copter was all it took to hop overtop From here, the Nature Vancouver of the imposing mountains tower- 2019 campsite ofered a stunningly ing above Bluf Lake south of Tatla gorgeous 360-degree view free from Lake and to be deposited near the any signs of humans. Nature was at treeline about 1000 m higher than our doorstep. Te quiet was delicious. the chopper launch pad. No-one needed to hike anywhere— Instant wilderness! we were already there! Helicopter delivery of all goods And there we were—on a small and personnel was key to the com- plateau forested with patches of low fortable establishment of our near- pines at about 2000 m elevation alpine occupation. Not many who and tucked among a series of small attended this camp would have been lakes and ponds. Te rugged Niut happy to make the hike to such a Range peaks of the Coast Mountains place. Our fight was feetingly short View of lakes, Goat Ridge, glacier and Niut Peak from Snow Patch Peak. Photo: Caroline Penn 48 Discovery at a little more than 10 km, but the level as a root embedded within the terrain that we few over was rugged, mantle of the earth. rocky, steep and trackless. Te geologic conditions changed Geology of the Niut Range radically, however, about 5 million years ago when a shift in the ofshore Te Niut Range is a place where plate subduction zones resulted in the immense geological events have appearance of the Cascade Volcanic unfolded.
    [Show full text]
  • Climate Change and Hazardous Processes in High Mountains
    Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2012 Climate change and hazardous processes in high mountains Clague, John J ; Huggel, Christian ; Korup, Oliver ; McGuire, Bill Abstract: The recent and continuing reduction in glacier ice cover in high mountains and thaw of alpine permafrost may have an impact on many potentially hazardous processes. As glaciers thin and retreat, existing ice- and moraine-dammed lakes can catastrophically empty, generating large and destructive downstream floods and debris flows. New ice-dammed lakes will form higher in mountain catchments, posing additional hazards in the future. The magnitude or frequency of shallow landslides and debris flows in some areas will increase because of the greater availability of unconsolidated sediment innew deglaciated terrain. Continued permafrost degradation and glacier retreat probably will decrease the stability of rock slopes. Cambio Climático y peligros naturales en altas montañas. La reciente y continua reducción de la cobertura glaciaria en alta montaña y el deshielo del permafrost pueden tener un impacto negativo en muchos procesos potencialmente peligrosos. A medida que los glaciares reducen su espesor y retroceden, los lagos formados por diques de hielo o morenas pueden vaciarse catastróficamente, resul- tando en grandes y destructivas inundaciones o flujos detríticos río abajo. Nuevos diques de hielo vana formarse en zonas más altas de las cuencas montañosas, generando peligros adicionales en el futuro. La magnitud o frecuencia de movimientos en masa superficiales y flujos detríticos va a aumentar en algunas áreas debido a la mayor disponibilidad de materiales no consolidados en nuevos terrenos desglasados.
    [Show full text]
  • Homathko River & Mosley Creek Watersheds
    Homathko River & Mosley Creek Watersheds Level 2 Fish Habitat & Riparian Assessment Procedure & Restoration Prescriptions Final Report G3 Consulting Ltd. Innovation & Excellence in Environmental Science Homathko River & Mosley Creek Watersheds LEVEL 2 FISH HABITAT & RIPARIAN ASSESSMENT PROCEDURE & RESTORATION PRESCRIPTIONS Final Report Prepared for: Tatlayoko Woodlot Association. Tatlayoko Lake, B.C. Submitted by: G3 Consulting Ltd. 1A-12880 Bathgate Way Richmond, BC V6V 1Z4 October 1999 Tatlayoko Woodlot Association Homathko/Mosley Level 2 FHAP & RAPP Final Report CONTENTS 1.0 INTRODUCTION ________________________________________________ 1 1.1 Project Scope __________________________________________________________ 1 Target Species _________________________________________________________ 1 1.2 Study Area Description ___________________________________________________ 2 1.3 Land Use______________________________________________________________ 2 2.0 METHODOLOGY ______________________________________________ 3 2.1 Site Identification, Selection & Confirmation___________________________________ 3 2.2 Site Classification _______________________________________________________ 3 2.3 Restoration & Rehabilitation Options ________________________________________ 3 Stream Bank Stabilization ________________________________________________ 4 Restoration of Primary Fish Habitat _________________________________________ 4 Restoration of Secondary & Tertiary Fish Habitat ______________________________ 4 Restoration of Riparian Habitat ____________________________________________
    [Show full text]
  • [Type the Document Title]
    Climbing to the Clouds Teachers Resources OVERVIEW [Type the document title] [Type the document subtitle] sutherlands 0 | Page Climbing to the Clouds Teachers Resources OVERVIEW CONTENTS Overview General Resources 2 Introduction 2 Overall Interpretive Goals 3 Topics Aboriginal 5 History 8 Conservation 11 Recreation 14 Arts 17 Taking It Further References 20 Appendices Web Resources 21 Recreation Activity Resource: Example of Compass Rose 23 Art Activity Resource: Poem 24 Mount John Clarke Newspaper Article 26 Price Ellison’s Expedition to Crown Mountain Vancouver Sun Article 27 Replica Clothes Pass Everest Test BBC Article 34 1 | Page Climbing to the Clouds Teachers Resources OVERVIEW This website offers an opportunity for students to explore the unique topic of local mountaineering while also pursuing curricula-based studies. This package provides an overview of the curricula links as well as specific student activities. Climbing to the Clouds: A People’s History of BC Mountaineering is about mountaineers, of how they were drawn to explore, map, enjoy, and fight to conserve peaks and wilderness areas in south western British Columbia and beyond. The website offers a vast range of curricula-based subjects for intermediate and high school students to explore. The website was created to provide an opportunity for all to experience far-off mountains, to discover how the mountains have influenced British Columbians and to explore reasons that people climb. The geographic scope is primarily southwestern British Columbia, but does include mountains such as Mount Waddington, Mount Logan and Mount Robson. The ascents of those mountains were historically significant as well as significantly challenging.
    [Show full text]
  • Monarch Mountain, Southwest Face, and Other Ascents
    AAC Publications Monarch Mountain, Southwest Face, and Other Ascents Canada, British Columbia, Coast Mountains ON JULY 28, Micha Rinn from Germany and I flew by helicopter to the col between Monarch Mountain and Page Mountain at the head of the Empire Way Glacier, deep in the Coast Mountains. Our objective was the pronounced spur that runs up the center of the unclimbed 1,250m southwest face of Monarch Mountain (3,555m). It was a line that prompted awe and excitement in equal measure—a veritable Walker Spur leading directly to the summit of the peak. How a Scottish-German climbing team came to know about one of the finest unclimbed features in western Canada requires some explanation. My fascination with Monarch, the second-highest massif in the Coast Mountains, began 20 years ago when Dave Hesleden and I traversed the Serra Group after making the first ascent of the southeast ridge of Asperity Mountain in the Waddington Range. [The route referred to in the AAJ report as the south ridge later came to be called the southeast ridge. It faces more or less south-southeast.]As we tussled with the jagged crest of the Serras, reputedly the most difficult summits in the range, Monarch stood out like a sentinel 70 miles to the north. With a prominence of 2,925m, there is no higher peak until you reach Mt. Fairweather, a thousand miles up the spine of the coastal range. I was smitten by Monarch’s dominance and resolved to climb it. The Coast Mountains had got under my skin, and I made two further trips to the Waddington massif, a couple to the Pantheon Spires, and one to the difficult-to-access Mt.
    [Show full text]
  • Climate Change and Hazardous Processes in High Mountains
    328 Revista de la Asociación Geológica Argentina 69 (3): 328 - 338 (2012) CLIMATE CHANGE AND HAZARDOUS PRocESSES IN HIGH MOUNTAINS John J. CLAGUE1, Christian HUGGEL2, Oliver KORUP3 and Bill McGUIRE4 1Corresponding author: Centre for Natural Hazard Research, Simon Fraser University, Burnaby, BC V5A 1S6, Canada; email: [email protected] 2Glaciology, Geomorphodynamics and Geochronology, Department of Geography, University of Zurich, CH-8057 Zurich, Switzerland; email [email protected] 3Earth and Environmental Sciences, Potsdam University, Karl-Liebknechstraase 24 (Hs 27), Potsdam, Germany; email [email protected] 4Aon Benfield UCL Hazard Centre, University College London, Gower Street, London, UK WC1E 6BT; email [email protected] AbSTRACT The recent and continuing reduction in glacier ice cover in high mountains and thaw of alpine permafrost may have an impact on many potentially hazardous processes. As glaciers thin and retreat, existing ice- and moraine-dammed lakes can catastrophi- cally empty, generating large and destructive downstream floods and debris flows. New ice-dammed lakes will form higher in mountain catchments, posing additional hazards in the future. The magnitude or frequency of shallow landslides and debris flows in some areas will increase because of the greater availability of unconsolidated sediment in new deglaciated terrain. Con- tinued permafrost degradation and glacier retreat probably will decrease the stability of rock slopes. Keywords: climate change, natural hazards, landslides, permafrost, glaciers. RESUMEN Cambio Climático y peligros naturales en altas montañas. La reciente y continua reducción de la cobertura glaciaria en alta montaña y el deshielo del permafrost pueden tener un impacto negativo en muchos procesos potencialmente peligrosos.
    [Show full text]