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University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY of the SCOTT GLACIER and WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA
This dissertation has been /»OOAOO m icrofilm ed exactly as received MINSHEW, Jr., Velon Haywood, 1939- GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA. The Ohio State University, Ph.D., 1967 Geology University Microfilms, Inc., Ann Arbor, Michigan GEOLOGY OF THE SCOTT GLACIER AND WISCONSIN RANGE AREAS, CENTRAL TRANSANTARCTIC MOUNTAINS, ANTARCTICA DISSERTATION Presented in Partial Fulfillment of the Requirements for the Degree Doctor of Philosophy in the Graduate School of The Ohio State University by Velon Haywood Minshew, Jr. B.S., M.S, The Ohio State University 1967 Approved by -Adviser Department of Geology ACKNOWLEDGMENTS This report covers two field seasons in the central Trans- antarctic Mountains, During this time, the Mt, Weaver field party consisted of: George Doumani, leader and paleontologist; Larry Lackey, field assistant; Courtney Skinner, field assistant. The Wisconsin Range party was composed of: Gunter Faure, leader and geochronologist; John Mercer, glacial geologist; John Murtaugh, igneous petrclogist; James Teller, field assistant; Courtney Skinner, field assistant; Harry Gair, visiting strati- grapher. The author served as a stratigrapher with both expedi tions . Various members of the staff of the Department of Geology, The Ohio State University, as well as some specialists from the outside were consulted in the laboratory studies for the pre paration of this report. Dr. George E. Moore supervised the petrographic work and critically reviewed the manuscript. Dr. J. M. Schopf examined the coal and plant fossils, and provided information concerning their age and environmental significance. Drs. Richard P. Goldthwait and Colin B. B. Bull spent time with the author discussing the late Paleozoic glacial deposits, and reviewed portions of the manuscript. -
GLACIERS of NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range
Glaciers of Asia— GLACIERS OF NEPAL—Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range By Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi SATELLITE IMAGE ATLAS OF GLACIERS OF THE WORLD Edited by RICHARD S. WILLIAMS, JR., and JANE G. FERRIGNO U.S. GEOLOGICAL SURVEY PROFESSIONAL PAPER 1386–F–6 CONTENTS Glaciers of Nepal — Glacier Distribution in the Nepal Himalaya with Comparisons to the Karakoram Range, by Keiji Higuchi, Okitsugu Watanabe, Hiroji Fushimi, Shuhei Takenaka, and Akio Nagoshi ----------------------------------------------------------293 Introduction -------------------------------------------------------------------------------293 Use of Landsat Images in Glacier Studies ----------------------------------293 Figure 1. Map showing location of the Nepal Himalaya and Karokoram Range in Southern Asia--------------------------------------------------------- 294 Figure 2. Map showing glacier distribution of the Nepal Himalaya and its surrounding regions --------------------------------------------------------- 295 Figure 3. Map showing glacier distribution of the Karakoram Range ------------- 296 A Brief History of Glacier Investigations -----------------------------------297 Procedures for Mapping Glacier Distribution from Landsat Images ---------298 Figure 4. Index map of the glaciers of Nepal showing coverage by Landsat 1, 2, and 3 MSS images ---------------------------------------------- 299 Figure 5. Index map of the glaciers of the Karakoram Range showing coverage -
A Statistical Analysis of Mountaineering in the Nepal Himalaya
The Himalaya by the Numbers A Statistical Analysis of Mountaineering in the Nepal Himalaya Richard Salisbury Elizabeth Hawley September 2007 Cover Photo: Annapurna South Face at sunrise (Richard Salisbury) © Copyright 2007 by Richard Salisbury and Elizabeth Hawley No portion of this book may be reproduced and/or redistributed without the written permission of the authors. 2 Contents Introduction . .5 Analysis of Climbing Activity . 9 Yearly Activity . 9 Regional Activity . .18 Seasonal Activity . .25 Activity by Age and Gender . 33 Activity by Citizenship . 33 Team Composition . 34 Expedition Results . 36 Ascent Analysis . 41 Ascents by Altitude Range . .41 Popular Peaks by Altitude Range . .43 Ascents by Climbing Season . .46 Ascents by Expedition Years . .50 Ascents by Age Groups . 55 Ascents by Citizenship . 60 Ascents by Gender . 62 Ascents by Team Composition . 66 Average Expedition Duration and Days to Summit . .70 Oxygen and the 8000ers . .76 Death Analysis . 81 Deaths by Peak Altitude Ranges . 81 Deaths on Popular Peaks . 84 Deadliest Peaks for Members . 86 Deadliest Peaks for Hired Personnel . 89 Deaths by Geographical Regions . .92 Deaths by Climbing Season . 93 Altitudes of Death . 96 Causes of Death . 97 Avalanche Deaths . 102 Deaths by Falling . 110 Deaths by Physiological Causes . .116 Deaths by Age Groups . 118 Deaths by Expedition Years . .120 Deaths by Citizenship . 121 Deaths by Gender . 123 Deaths by Team Composition . .125 Major Accidents . .129 Appendix A: Peak Summary . .135 Appendix B: Supplemental Charts and Tables . .147 3 4 Introduction The Himalayan Database, published by the American Alpine Club in 2004, is a compilation of records for all expeditions that have climbed in the Nepal Himalaya. -
The Characterization Analysis of Rob Hall in Everest: Never Let Go Film 2015
Indonesian EFL Journal, Vol. 2(1) January 2016 AISEE p-ISSN 2252-7427 e-ISSN 2541-3635 The Association of Indonesian Scholars of English Education THE CHARACTERIZATION ANALYSIS OF ROB HALL IN EVEREST: NEVER LET GO FILM 2015 Risna Budiarti Department of English Education, University of Kuningan, Indonesia Email: [email protected] Nani Ronsani Thamrin Department of English Education, University of Kuningan, Indonesia E-mail: [email protected] APA Citation: Budiarti, R., & Thamrin, N. R. (2016). The characterization analysis of Rob Hall in Everest: Never Let Go film 2015. Indonesian EFL Journal, 2(1), 71-79 Received: 12-11-2015 Accepted: 23-12-2015 Published: 01-01-2016 Abstract: This research focuses on Rob Hall’s characterizations and moral values found in “Everest: Never Let Go” Film. The aims of this research are to find out Rob Hall’s characterizations portrayed in the Film Everest: Never Let Go and the moral values of the Film. The researcher used the theory about psychological analysis (based on Sigmund Freud in Schultz, 2005) to find out Rob characters through his words or sentences in script of Everest; Never Let Go Film and semiotics theory (based on Roland Barthes, 1968, 1990, 1991) to find out the characteristics of Rob Hall through pictures or signs which show his character in Film “Everest: Never Let Go” with print screen of each pictures or signs, and theory of moral value based on George and Uyanga (2014). Qualitative descriptive method was used by the researcher to find out the characteristic of Rob Hall in Everest: Never Let Go Film and the moral values of Rob Hall characterized in the Film. -
Aim for Emotionally Sticky Goals to Get Your Team to the Top
Aim for Emotionally Sticky Goals to Get Your Team to the Top Skills and Professional Development 1 / 4 The riskiest thing you will ever encounter on the mountain is your own team. In January, I had the pleasure of meeting Cathy O’Dowd at a company event in Madrid, Spain. O’Dowd is a South African rock climber, mountaineer, and motivational speaker. She is famous for being the first woman to summit Everest from both the south and north sides. Her first Everest ascent was in 1996 — the year that eight climbers died after being caught in a storm high on the mountain. This is the tragedy that became the subject of Jon Krakauer’s best-selling book Into Thin Air and the 2015 Hollywood movie Everest. O’Dowd was a perfect fit as a speaker for our European sales kick-off meeting because the business unit had elected to use the mountain climbing metaphor as its underlying theme. The cover slide for every presentation was of a mountain profile with climbers making their way up the slope. Our regional director even took the stage at one point wearing traditional German alpine climbing gear that included lederhosen, boots, a climbing ax, and a coil of rope slung across his chest. O’Dowd's remarks on the first day of our conference centered on the gripping tale of her 1996 South African Everest expedition. She began her talk by observing that if you ever find yourself at the base of Everest, with the ambition to reach the top, you should take stock of two important numbers. -
Debris-Covered Glacier Energy Balance Model for Imja–Lhotse Shar Glacier in the Everest Region of Nepal
The Cryosphere, 9, 2295–2310, 2015 www.the-cryosphere.net/9/2295/2015/ doi:10.5194/tc-9-2295-2015 © Author(s) 2015. CC Attribution 3.0 License. Debris-covered glacier energy balance model for Imja–Lhotse Shar Glacier in the Everest region of Nepal D. R. Rounce1, D. J. Quincey2, and D. C. McKinney1 1Center for Research in Water Resources, University of Texas at Austin, Austin, Texas, USA 2School of Geography, University of Leeds, Leeds, LS2 9JT, UK Correspondence to: D. R. Rounce ([email protected]) Received: 2 June 2015 – Published in The Cryosphere Discuss.: 30 June 2015 Revised: 28 October 2015 – Accepted: 12 November 2015 – Published: 7 December 2015 Abstract. Debris thickness plays an important role in reg- used to estimate rough ablation rates when no other data are ulating ablation rates on debris-covered glaciers as well as available. controlling the likely size and location of supraglacial lakes. Despite its importance, lack of knowledge about debris prop- erties and associated energy fluxes prevents the robust inclu- sion of the effects of a debris layer into most glacier sur- 1 Introduction face energy balance models. This study combines fieldwork with a debris-covered glacier energy balance model to esti- Debris-covered glaciers are commonly found in the Everest mate debris temperatures and ablation rates on Imja–Lhotse region of Nepal and have important implications with regard Shar Glacier located in the Everest region of Nepal. The de- to glacier melt and the development of glacial lakes. It is bris properties that significantly influence the energy bal- well understood that a thick layer of debris (i.e., > several ance model are the thermal conductivity, albedo, and sur- centimeters) insulates the underlying ice, while a thin layer face roughness. -
Everest Book Three the Summit
364910_FM_v1_. 10/13/11 10:44 PM Page iii GORDON KORMAN EVEREST BOOK THREE THE SUMMIT SCHOLASTIC INC. New York Toronto London Auckland Sydney Mexico City New Delhi Hong Kong 364910_FM_v2_. 11/2/11 11:25 PM Page iv For Daisy Samantha Korman My Summit If you purchased this book without a cover, you should be aware that this book is stolen property. It was reported as “unsold and destroyed” to the publisher, and neither the author nor the publisher has received any pay- ment for this “stripped book.” No part of this publication may be reproduced, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording, or otherwise, without written permission of the publisher. For information regarding permission, write to Scholastic Inc., Attention: Permissions Department, 557 Broadway, New York, NY 10012. ISBN 978-0-545-39234-1 Copyright © 2002 by Gordon Korman. All rights reserved. Published by Scholastic Inc. SCHOLASTIC and associated logos are trademarks and/or registered trademarks of Scholastic Inc. 12 11 10 9 8 7 6 5 4 3 2 1 12 13 14 15 16 17/0 Printed in the U.S.A. 40 This edition first printing, March 2012 364910_Text_v1.qxd_. 10/13/11 10:41 PM Page 1 PROLOGUE The wind pounced on them above twenty-five thousand feet. As the youngest expedition in Everest history scrambled up the Geneva Spur, the onslaught be- gan — overpowering, unpredictable gusts that threatened to pluck the climbers off the mountain and hurl them into space. Amazingly, this was nothing new to them. -
Project ICEFLOW
ICEFLOW: short-term movements in the Cryosphere Bas Altena Department of Geosciences, University of Oslo. now at: Institute for Marine and Atmospheric research, Utrecht University. Bas Altena, project Iceflow geometric properties from optical remote sensing Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall [published] Ensemble matching of repeat satellite images applied to measure fast-changing ice flow, verified with mountain climber trajectories on Khumbu icefall, Mount Everest. Journal of Glaciology. [outreach] see also ESA Sentinel Online: Copernicus Sentinel-2 monitors glacier icefall, helping climbers ascend Mount Everest Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall 0 1 2 km glacier surface speed [meter/day] Khumbu Glacier 0.2 0.4 0.6 0.8 1.0 1.2 Mt. Everest 300 1800 1200 600 0 2/4 right 0 5/4 4/4 left 4/4 2/4 R 3/4 L -300 terrain slope [deg] Nuptse surface velocity contours Western Chm interval per 1/4 [meter/day] 10◦ 20◦ 30◦ 40◦ [outreach] see also Adventure Mountain: Mount Everest: The way the Khumbu Icefall flows Bas Altena, project Iceflow Sentinel-2 Fast flow through icefall ∆H Ut=2000 U t=2020 H internal velocity profile icefall α 2A @H 3 U = − 3+2 H tan αρgH @x MSc thesis research at Wageningen University Bas Altena, project Iceflow Quantifying precision in velocity products 557 200 557 600 7 666 200 NCC 7 666 000 score 1 7 665 800 Θ 0.5 0 7 665 600 557 460 557 480 557 500 557 520 7 665 800 search space zoom in template/chip correlation surface 7 666 200 7 666 200 7 666 000 7 666 000 7 665 800 7 665 800 7 665 600 7 665 600 557 200 557 600 557 200 557 600 [submitted] Dispersion estimation of remotely sensed glacier displacements for better error propagation. -
List of Place-Names in Antarctica Introduced by Poland in 1978-1990
POLISH POLAR RESEARCH 13 3-4 273-302 1992 List of place-names in Antarctica introduced by Poland in 1978-1990 The place-names listed here in alphabetical order, have been introduced to the areas of King George Island and parts of Nelson Island (West Antarctica), and the surroundings of A. B. Dobrowolski Station at Bunger Hills (East Antarctica) as the result of Polish activities in these regions during the period of 1977-1990. The place-names connected with the activities of the Polish H. Arctowski Station have been* published by Birkenmajer (1980, 1984) and Tokarski (1981). Some of them were used on the Polish maps: 1:50,000 Admiralty Bay and 1:5,000 Lions Rump. The sheet reference is to the maps 1:200,000 scale, British Antarctic Territory, South Shetland Islands, published in 1968: King George Island (sheet W 62 58) and Bridgeman Island (Sheet W 62 56). The place-names connected with the activities of the Polish A. B. Dobrowolski Station have been published by Battke (1985) and used on the map 1:5,000 Antarctic Territory — Bunger Oasis. Agat Point. 6211'30" S, 58'26" W (King George Island) Small basaltic promontory with numerous agates (hence the name), immediately north of Staszek Cove. Admiralty Bay. Sheet W 62 58. Polish name: Przylądek Agat (Birkenmajer, 1980) Ambona. 62"09'30" S, 58°29' W (King George Island) Small rock ledge, 85 m a. s. 1. {ambona, Pol. = pulpit), above Arctowski Station, Admiralty Bay, Sheet W 62 58 (Birkenmajer, 1980). Andrzej Ridge. 62"02' S, 58° 13' W (King George Island) Ridge in Rose Peak massif, Arctowski Mountains. -
Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal
HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 17 Number 2 Himalayan Research Bulletin: Article 16 Solukhumbu and the Sherpa 1997 Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Byers, Alton C.. 1997. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal. HIMALAYA 17(2). Available at: https://digitalcommons.macalester.edu/himalaya/vol17/iss2/16 This Research Article is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers The Mountain Institute This study uses repeat photography as the primary Introduction research tool to analyze processes of physical and Repeat photography, or precise replication and cultural landscape change in the Khumbu (M!. Everest) interpretation of historic landscape scenes, is an region over a 40-year period (1955-1995). The study is analytical tool capable of broadly clarifying the patterns a continuation of an on-going project begun by Byers in and possible causes of contemporary landscapellanduse 1984 that involves replication of photographs originally changes within a given region (see: Byers 1987a1996; taken between 1955-62 from the same five photo 1997). As a research tool, it has enjoyed some utility points. The 1995 investigation reported here provided in the United States during the past thirty years (see: the opportunity to expand the photographic data base Byers 1987b; Walker 1968; Heady and Zinke 1978; from five to 26 photo points between Lukla (2,743 m) Gruell 1980; Vale, 1982; Rogers et al. -
Thirteen Nations on Mount Everest John Cleare 9
Thirteen nations on Mount Everest John Cleare In Nepal the 1971 pre-monsoon season was notable perhaps for two things, first for the worst weather for some seventy years, and second for the failure of an attempt to realise a long-cherished dream-a Cordee internationale on the top of the world. But was it a complete failure? That the much publicised International Himalayan Expedition failed in its climbing objectives is fact, but despite the ill-informed pronouncements of the headline devouring sceptics, safe in their arm-chairs, those of us who were actually members of the expedition have no doubt that internationally we did not fail. The project has a long history, and my first knowledge of it was on a wet winter's night in 1967 at Rusty Baillie's tiny cottage in the Highlands when John Amatt explained to me the preliminary plans for an international expedi tion. This was initially an Anglo-American-Norwegian effort, but as time went by other climbers came and went and various objectives were considered and rejected. Things started to crystallise when Jimmy Roberts was invited to lead the still-embryo expedition, and it was finally decided that the target should be the great South-west face of Mount Everest. However, unaware of this scheme, Norman Dyhrenfurth, leader of the successful American Everest expedition of 1963-film-maker and veteran Himalayan climber-was also planning an international expedition, and he had actually applied for per mission to attempt the South-west face in November 1967, some time before the final target of the other party had even been decided. -
Everest – South Col Route – 8848M the Highest Mountain in the World South Col Route from Nepal
Everest – South Col Route – 8848m The highest mountain in the world South Col Route from Nepal EXPEDITION OVERVIEW Join Adventure Peaks on their twelfth Mt Everest Expedition to the world’s highest mountain at 8848m (29,035ft). Our experience is amongst the best in the world, combined with a very high success rate. An ultimate objective in many climbers’ minds, the allure of the world’s highest summit provides a most compelling and challenging adventure. Where there is a will, we aim to provide a way. Director of Adventure Peaks Dave Pritt, an Everest summiteer, has a decade of experience on Everest and he is supported by Stu Peacock, a regular and very talented high altitude mountaineer who has led successful expeditions to both sides of Everest as well as becoming the first Britt to summit Everest three times on the North Side. The expedition is a professionally-led, non-guided expedition. We say non-guided because our leader and Sherpa team working with you will not be able to protect your every move and you must therefore be prepared to move between camps unsupervised. You will have an experienced leader who has previous experience of climbing at extreme high altitude together with the support of our very experienced Sherpa team, thus increasing your chance of success. Participation Statement Adventure Peaks recognises that climbing, hill walking and mountaineering are activities with a danger of personal injury or death. Participants in these activities should be aware of and accept these risks and be responsible for their own actions and involvement. Adventure Travel – Accuracy of Itinerary Although it is our intention to operate this itinerary as printed, it may be necessary to make some changes as a result of flight schedules, climatic conditions, limitations of infrastructure or other operational factors.