Mt. Waddington, Complete West Ridge
Total Page:16
File Type:pdf, Size:1020Kb

Load more
Recommended publications
-
Stability of Leaning Column at Devils Tower National Monument, Wyoming
Stability of Leaning Column at Devils Tower National Monument, Wyoming By Edwin L. Harp and Charles R. Lindsay U.S. Geological Survey Open-File Report 2006–1130 U.S. Department of the Interior U.S. Geological Survey U.S. Department of the Interior DIRK KEMPTHORNE, Secretary U.S. Geological Survey P. Patrick Leahy, Acting Director U.S. Geological Survey, Reston, Virginia 2006 For product and ordering information: World Wide Web: http://www.usgs.gov/pubprod Telephone: 1-888-ASK-USGS For more information on the USGS—the Federal source for science about the Earth, its natural and living resources, natural hazards, and the environment: World Wide Web: http://www.usgs.gov Telephone: 1-888-ASK-USGS Harp, Edwin L., and Lindsay, Charles R., 2006, Stability of Leaning Column at Devils Tower National Monument, Wyoming: U.S. Geological Survey Open-file Report 2006–1130, 10 p. Any use of trade, firm, or product names is for descriptive purposes only and does not imply endorsement by the U.S. Government. Although this report is in the public domain, permission must be secured from the individual copyright owners to reproduce any copyrighted material contained within this report. Cover photograph: Devils Tower with leaning column visible (red arrow) at lower left edge of vertical shadow on tower face. ii Contents Abstract .....................................................................................................................................................................................................1 Introduction ...............................................................................................................................................................................................1 -
Alaska Range
Alaska Range Introduction The heavily glacierized Alaska Range consists of a number of adjacent and discrete mountain ranges that extend in an arc more than 750 km long (figs. 1, 381). From east to west, named ranges include the Nutzotin, Mentas- ta, Amphitheater, Clearwater, Tokosha, Kichatna, Teocalli, Tordrillo, Terra Cotta, and Revelation Mountains. This arcuate mountain massif spans the area from the White River, just east of the Canadian Border, to Merrill Pass on the western side of Cook Inlet southwest of Anchorage. Many of the indi- Figure 381.—Index map of vidual ranges support glaciers. The total glacier area of the Alaska Range is the Alaska Range showing 2 approximately 13,900 km (Post and Meier, 1980, p. 45). Its several thousand the glacierized areas. Index glaciers range in size from tiny unnamed cirque glaciers with areas of less map modified from Field than 1 km2 to very large valley glaciers with lengths up to 76 km (Denton (1975a). Figure 382.—Enlargement of NOAA Advanced Very High Resolution Radiometer (AVHRR) image mosaic of the Alaska Range in summer 1995. National Oceanic and Atmospheric Administration image mosaic from Mike Fleming, Alaska Science Center, U.S. Geological Survey, Anchorage, Alaska. The numbers 1–5 indicate the seg- ments of the Alaska Range discussed in the text. K406 SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD and Field, 1975a, p. 575) and areas of greater than 500 km2. Alaska Range glaciers extend in elevation from above 6,000 m, near the summit of Mount McKinley, to slightly more than 100 m above sea level at Capps and Triumvi- rate Glaciers in the southwestern part of the range. -
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. -
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. -
The American Alpine Club Guidebook to Membership Alpinist Magazine
THE AMERICAN ALPINE CLUB GUIDEBOOK TO MEMBERSHIP ALPINIST MAGAZINE ith each print edition of Alpinist, we aim to create a work of art, paying attention to every detail— from our extended photo captions to our carefully Wselected images and well-crafted stories. Inside our pages, we strive to offer our readers an experience like that of exploratory climbing, a realm of words and images where they can wander, discover surprising new viewpoints, and encounter moments of excitement, humor, awe and beauty. By publishing the work of climbers from a wide range of ages, technical abilities, nations and cultures—united by their passion for adventure and wild places—we hope to reflect and enhance the sense of community within the climbing life. Over time, back issues have become collectors’ items, serving as historical references and ongoing inspirations. Like our readers, we believe that great writing and art about climbing demand the same boldness, commitment and vision as the pursuit itself. JOIN US. Exclusive AAC Member Pricing 1 Year - $29.95 | 2 Years - $54.95 Alpinist.com/AAC ALPINIST IS A PROUD PARTNER OF THE AMERICAN ALPINE CLUB Stay Connected! @AlpinistMag @Alpinist @AlpinistMag ALP_2019_AAC Ad FIN.indd 1 6/26/19 4:14 PM WELCOME, ALL 5 You Belong Here ARTIST SPOTLIGHT 8 Brooklyn Bell on Art for the In-betweens MEMBERSHIP THROUGH THE LENS 10 Inspiration, Delivered Directly NAVAJO RISING 23 An Indigenous Emergence Story WHEN WOMEN LEAD 27 Single Pitch Instructors for the 21st Century GLACIAL VIEWS 29 A Climate Scientist Reflects & Other Research Stories CLIMBERS FOR CLIMATE 32 Taking a Stand on Climate Change, Together 1CLIMB, INFINITE POTENTIAL 34 Kevin Jorgeson Breaks Down Walls by Building Them ON PUSHING 37 24 Hours Into the Black, the AAC Grief Fund AN ODE TO MOBILITY 40 The Range of Motion Project Tackles Cotopaxi YOSEMITE'S CAMP 4 43 The Center of the Climbing Universe REWIND THE CLIMB 47 The Tragedy of the 1932 American K2 Expedition BETA 48 Everything a Club Member Needs to Know PARTING SHOT 72 Jeremiah Watt on Travel & Life a Greg Kerzhner climbing Mr. -
Devils Tower National Monument Newspaper 2018
National Park Service Devils Tower National Monument U.S. Department of the Interior Offcial Newspaper 2018 Edition Welcome to Devils Tower National Monument! Welcome to America’s first national monument! Devils Tower is an Things To Do iconic formation, a monolith rising • Explore the visitor center above the surrounding countryside. As you explore the monument • Watch the prairie dogs (p. 4) today, the Tower you see will • Attend a ranger program (p. 5) be remarkable, everlasting in its powerful appearance. Yet depending • Become a Junior Ranger (p. 5) on the time of day and the weather, • Take a hike (p. 8) the formation can look dramatically di°erent. Often, it is yellow-green against a clear blue sky, but in • Look for wildlife (p. 4) shadow the Tower is black and seems to stand a little taller. When • Climb the Tower (p. 6) fog rolls in, it is shrouded in mist, only peeking out occasionally to say hello. If you visit in the winter, the Tower will be covered in a • Camp in the Belle Fourche dusting of snow. And if you stay for the sunset, the sun’s rays will River Campground (p. 5) turn its face orange, refecting the colors of the sky. In this way, the • Visit the Sacred Circle of Smoke formation is remarkably dynamic, appearing different as the day Sculpture progresses and the seasons change – if you come back, you may see a di°erent Tower than the one you see today. But Devils Tower is • See the stars (p. 5) also timeless, changing only on a scale imperceptible to human eyes. -
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. -
Ghosts of K2 the Epic Saga of the First Ascent Mick Conefrey
The GHOSTS of K2 The Epic Saga of the First Ascent Mick Conefrey O NEW O RLD A Oneworld Book First published in North America, Great Britain and the Commonwealth by Oneworld Publications, 2015 Copyright © Mick Conefrey 2015 The moral right of Mick Conefrey to be identified as the Author of this work has been asserted by him in accordance with the Copyright, Designs, and Patents Act 1988 All rights reserved Copyright under Berne Convention A CIP record for this title is available from the British Library ISBN 978-1-78074-595-4 ISBN 978-1-78074-596-1(eBook) Typeset by Tetragon, London Maps Drawn by Adam T. Burton Printed and bound by CPI Group (UK) Ltd, Croydon, CR0 4YY Oneworld Publications 10 Bloomsbury Street London WC1B 3SR England To Michael F. Contents List of Illustrations ix Prologue: The Mountain with No Name xi 1 The Beast and the Prince 1 2 The Harvard Boys 31 3 A Climbing Party 67 4 High Ambition 93 5 The Fall Out 107 6 Unfinished Business 133 7 Teamwork 149 8 Man Down 165 9 The Old Road 183 10 The Flowers of Italy 205 11 The Spoils of Victory 233 12 The Base Lie? 247 Epilogue: Living up to Your Name? 273 Acknowledgements 291 Notes 293 Bibliography 303 Index 309 vii List of Illustrations Map 1 K2, 1902 7 Map 2 The overland route to K2 40 Map 3 The ridges around K2 48 Map 4 Fritz Wiessner’s camps, K2 81 Map 5 K2, 1953 137 Map 6 The Gilkey Rescue, 10 August 1953 170 Map 7 The final Italian camps on K2 215 ix Prologue The Mountain with No Name On a small hill, next to a huge mountain on the border of Pakistan and China, there’s a unique monument: a stone cairn some 10 ft high. -
Journal of Mining and Geological Sciences
UNIVERSITY OF MINING AND GEOLOGY “ST. IVAN RILSKI” JOURNAL OF MINING AND GEOLOGICAL SCIENCES Volume 61 Part I: Geology and Geophysics Sofia, 2018 ISSN 2535-1176 Editor-in-chief Prof. Dr. Pavel Pavlov University of Mining and Geology “St. Ivan Rilski” 1, Prof. Boyan Kamenov Str., 1700 Sofia, Bulgaria e-mail: [email protected]; http://www.mgu.bg/nis EDITORIAL BOARD Prof. Dr. Lyuben Totev Part I: Geology and Geophysics Deputy editor, UMG “St. Ivan Rilski” Prof. Dr. Viara Pojidaeva Prof. Dr. Yordan Kortenski Deputy editor, UMG “St. Ivan Rilski” Chairperson of an editorial board, UMG “St. Ivan Rilski” Assoc. Prof. Dr. Stefka Pristavova Prof. Dimitar Sinyovski, DSc. Deputy editor, UMG “St. Ivan Rilski” UMG “St. Ivan Rilski” Prof. Dr. Yordan Kortenski Prof. Dr. Maya Stefanova UMG “St. Ivan Rilski” Institute of Organic Chemistry, Bulgarian Academy of Assoc. Prof. Dr. Elena Vlasseva Sciences UMG “St. Ivan Rilski” Assoc. Prof. Dr. Nikolai Stoyanov Assoc. Prof. Dr. Antoaneta Yaneva UMG “St. Ivan Rilski” UMG “St. Ivan Rilski” Prof. Dr. Radi Radichev Prof. Dr. Desislava Kostova UMG “St. Ivan Rilski” UMG “St. Ivan Rilski” Prof. Stoyan Groudev, DSc UMG “St. Ivan Rilski” Prof. Dr. Strashimir Srtashimirov UMG “St. Ivan Rilski” Prof. Dr. Ognyan Petrov Institute of Mineralogy and Crystallography, Bulgarian Academy of Sciences Technical secretary: Kalina Marinova Printig: Publishing House “St. Ivan Rilski” All rights reserved. Reproduction in part or whole without permission is strictly prohibited. 2 C O N T E N T S Part 1 – Geology, Mineralogy and Mineral Deposits -
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. -
Shawangunk Watch Fall 2015
Shawangunk WATCH Friends of the Shawangunks and The Shawangunk Conservancy August, 2015 Volume 20 Number 2 The Mine Hole panther rock v grannies v rock climbing Preserving Open Space in the Shawangunks since 1963 photograph: John Hayes John photograph: The Fawn Keith LaBudde PRIL AND I were having breakfast, staring into the woods, when four legs of a deer appeared. (Its upper body was obscured by witch-hazel.) And suddenly the legs were joined by a fawn. Because of the some- what erratic way in which it moved, we guessed the fawn was at most a couple of days old. They browsed for a few minutes, and then the fawn nursed for a few more. The doe then stepped over a large log ly- ing on the ground and continued to browse. What was the fawn going to do? It couldn’t go over the log whose diameter almost matched the fawn’s height. After hesitating, it walked eight feet to the cut end of the log, rounded it and rejoined its mother. Then off they both went into the woods. Later that morning, as I was doing a “garlic-mus- tard walk,” trying to remove this invasive plant from an area near the house, I moved around a large maple tree, and almost stepped on a fawn, presumably the one we had seen earlier. It was curled up at the base of the tree, and appeared to be asleep. I hurried back to the house and told Pril to come quickly with her camera. The fawn was just as I had left it. -
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.