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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. -
NATURE January 7, 1933
10 NATURE jANUARY 7, 1933 Mount Everest By Col. H. L. CROSTHWAIT, c.I.E. OUNT EVEREST, everyone knows, is the would be through Nepal, but even if the Nepalese M highest mountain in the world. It was Government were willing to permit the passage discovered, and its height determined, during the of its country, the route would be through operations of the Great Trigonometrical Survey trackless leach- infested jungles impossible for of India in the course of carrying out the geodetic pack transport. Added to this, the snow line is triangulation of that country in the years 1849-50. about 2,000 ft. lower on the south side than on The figure adopted, namely, 29,002 ft. above the north, for it is subject to the full force of the mean sea level, was derived from the mean of a monsoon and is probably more deeply eroded and, large number of vertical angles observed to the in consequence, more inaccessible than from the peak from six different stations situated in the Tibet side. For these reasons successive expe plains of India south of Nepal. These stations ditions have taken the longer route, about 350 were at distances varying from 108 to liS miles. miles from Darjeeling via the Chumbi valley, It was not until some months afterwards, when Kampa Dzong and Sheka Dzong, made possible the necessary computations had been completed, since the Tibetan objection to traversing its that the great height of Everest was first realised. territory has been overcome. The actual discovery was made in the computing This route possessed the advantage of passing office at Dehra Dun. -
Damage from the April-May 2015 Gorkha Earthquake Sequence in the Solukhumbu District (Everest Region), Nepal David R
Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard To cite this version: David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard. Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal. GSA Annual Meeting, Sep 2016, Denver, United States. hal-01373311 HAL Id: hal-01373311 https://hal.archives-ouvertes.fr/hal-01373311 Submitted on 28 Sep 2016 HAL is a multi-disciplinary open access L’archive ouverte pluridisciplinaire HAL, est archive for the deposit and dissemination of sci- destinée au dépôt et à la diffusion de documents entific research documents, whether they are pub- scientifiques de niveau recherche, publiés ou non, lished or not. The documents may come from émanant des établissements d’enseignement et de teaching and research institutions in France or recherche français ou étrangers, des laboratoires abroad, or from public or private research centers. publics ou privés. DAMAGE FROM THE APRIL-MAY 2015 GORKHA EARTHQUAKE SEQUENCE IN THE SOLUKHUMBU DISTRICT (EVEREST REGION), NEPAL LAGESON, David R.1, FORT, Monique2, BHATTARAI, Roshan Raj3 and HUBBARD, Mary1, (1)Department of Earth Sciences, Montana State University, 226 Traphagen Hall, Bozeman, MT 59717, (2)Department of Geography, Université Paris Diderot, 75205 Paris Cedex 13, Paris, France, (3)Department of Geology, Tribhuvan University, Tri-Chandra Campus, Kathmandu, Nepal, [email protected] ABSTRACT: Rapid assessments of landslides Valley profile convexity: Earthquake-triggered mass movements (past & recent): Traditional and new construction methods: Spectrum of structural damage: (including other mass movements of rock, snow and ice) as well as human impacts were conducted by many organizations immediately following the 25 April 2015 M7.8 Gorkha earthquake and its aftershock sequence. -
The 1921 British Mount Everest Expedition Limited Edition Platinum Prints
The 1921 British Mount Everest Expedition Limited Edition Platinum Prints (1) ‘Monks and the Administrator at Shekar Tschöde Monastery.’ Photographer: Charles Kenneth Howard-Bury (1881-1963) Celluloid Negative, MEE21/0339 TO ORDER For provenance and edition information please contact: [email protected] The 1921 British Mount Everest Expedition Limited Edition Platinum Prints (2) ‘Members of Expedition at 17,300 ft. Camp.’ Top, left to right: Wollaston, Howard-Bury, Heron, Raeburn. Bottom, left to right: Mallory, Wheeler, Bullock, Morshead. Photographer: Alexander Frederick Richmond Wollaston (1875-1930) Celluloid Negative, MEE21/0396 TO ORDER For provenance and edition information please contact: [email protected] The 1921 British Mount Everest Expedition Limited Edition Platinum Prints (3) ‘A group of Bhutias, Linga.' Photographer: George Leigh Mallory (1886-1924) Celluloid Negative, MEE21/0587 TO ORDER For provenance and edition information please contact: [email protected] The 1921 British Mount Everest Expedition Limited Edition Platinum Prints (4) ‘The Abbot of Shekar Chote.’ Photographer: Charles Kenneth Howard-Bury (1881-1963) Celluloid Negative, MEE21/0327 TO ORDER For provenance and edition information please contact: [email protected] The 1921 British Mount Everest Expedition Limited Edition Platinum Prints (5) Above: Untitled. Photographer: George Leigh Mallory (1886-1924) Celluloid Negative, MEE21/0907 Below: ‘Looking down Arun Valley from slopes south of Shiling.’ Photographer: George Leigh Mallory (1886-1924) Celluloid Negative, MEE21/0641 -
Mount Everest, the Reconnaissance, 1921
MOUNT EVEREST The Summit. Downloaded from https://www.greatestadventurers.com MOUNT EVEREST THE RECONNAISSANCE, 1921 By Lieut.-Col. C. K. HOWARD-BURY, D.S.O. AND OTHER MEMBERS OF THE MOUNT EVEREST EXPEDITION WITH ILLUSTRATIONS AND MAPS LONGMANS, GREEN AND CO. 55 FIFTH AVENUE, NEW YORK LONDON: EDWARD ARNOLD & CO. 1922 Downloaded from https://www.greatestadventurers.com PREFACE The Mount Everest Committee of the Royal Geographical Society and the Alpine Club desire to express their thanks to Colonel Howard-Bury, Mr. Wollaston, Mr. Mallory, Major Morshead, Major Wheeler and Dr. Heron for the trouble they have taken to write so soon after their return an account of their several parts in the joint work of the Expedition. They have thereby enabled the present Expedition to start with full knowledge of the results of the reconnaissance, and the public to follow the progress of the attempt to reach the summit with full information at hand. The Committee also wish to take this opportunity of thanking the Imperial Dry Plate Company for having generously presented photographic plates to the Expedition and so contributed to the production of the excellent photographs that have been brought back. They also desire to thank the Peninsular and Oriental Steam Navigation Company for their liberality in allowing the members to travel at reduced fares; and the Government of India for allowing the stores and equipment of the Expedition to enter India free of duty. J. E. C. EATON Hon. A. R. } Secretaries. HINKS Downloaded from https://www.greatestadventurers.com CONTENTS PAGE INTRODUCTION. By SIR FRANCIS YOUNGHUSBAND, K.C.S.I., K.C.I.E., President of the Royal Geographical Society 1 THE NARRATIVE OF THE EXPEDITION By LIEUT.-COL. -
Mount Everest, the Reconnaissance, It Was, Claimed Eric Shipton
The Forgotten Adventure: Mount Everest, The Reconnaissance, 1935. T o n y A s t i l l . F o r e w o r d b y L o r d H u n t . I ntroduction b y S i r E d m u n d H i l l a r y . S outhhampton : L e s A l p e s L i v r e , 2005. 359 PAGES, NUMEROUS BLACK & WHITE PHOTOGRAPHS, AND 2 FOLDING MAPS PLUS A UNIQUE DOUBLE DUST-JACKET OF A 1 9 3 5 c o l o r topographic c o u n t o u r m a p o f Mt. E v e r e s t ’ s n o r t h f a c e i n T i b e t b y M i c h a e l S p e n d e r . £ 3 0 . It was, claimed Eric Shipton famously, “a veritable orgy of moun tain climbing.” In May 1935, Britain’s best mountaineers, including Shipton, longtime climbing partner Bill Tilman, plus 15 Sherpas, among them a 19-year-old novice, Tenzing Norgay, embarked from Darjeeling on the fourth-ever Mt. Everest expedition. In large part because no expedition book was later penned by Shipton, their 27-year-old leader, the 1935 Everest Reconnaissance Expedi tion has remained largely unknown and unlauded. No more! Seven decades later, The Forgotten Adventure reveals the never-before-told climbing adventures of three of the twentieth-century mountaineerings most revered icons reveling in the Himalayan glory of their youth. -
Everest Kangshung Face Trek
Everest Kangshung Face Trek Day 01: Arrive in Lhasa (3,650 m / 11,972 ft) Upon your arrival in Lhasa, a representative from Upper-Himalayan Treks and Adventure will meet you at an agreed upon location. From here we will travel to a hotel and check into our rooms. Due to the altitude of Lhasa (11,972 ft), we recommend taking the rest of the day to acclimate. Day 02: Go Sightseeing in Lhasa: Potala Palace, Norbulingka Palace and Tibet Traditional Hospital: 5 - 6 hours Today, we visit the former residences of the Dalai Lama. Potala Palace was built in the 17th century and is known for its views of Lhasa. The palace is filled with numerous state rooms, chapels, and remarkable works of art. Norbulingka Palace was the summer residence of the Dalai Lama. It hosts the largest garden in Tibet. From Norbulingka Palace, we visit a traditional Tibetan hospital, which is the center for research and production of traditional Tibetan medicine. We spend the -
Present Perfect Or Past Simple? Present Perfect Past Simple Comparing
Table Of Contents: Present Perfect or Past Simple? Present Perfect Past Simple Comparing How do you choose between the Present Perfect and Past Simple? Both Present Perfect and Past Simple are used to talk about a completed action. The difference is the following: Present Perfect denotes recent actions and events which are connected with the present. Past Simple denotes actions and events in finished time periods (last week, yesterday, at the weekend, etc.). Compare: via http://www.lingvistov.ru/blog/grammar/present-perfect-vs-past-simple-exercises/ Present Perfect or Past Simple? So, how do you choose between the Present Perfect and Past Simple? Present Perfect The Present Perfect is used to talk about an action that took place in the recent past and is still relevant to the present moment. GrammarTOP.com Jack has lived in Madrid for 10 years so far (and he still lives there). I’ve just finished reading this book, it’s so amazing (this happened recently and now I share my impressions). The structure is: have / has + Past Participle The common usages of Present Perfect are: 1. to put emphasis on the result: – She has broken a cup. 2. to express an action that started in the past and continues up to the present: – I have worked for this company for 10 years. 3. to talk about life experiences: – I’ve never traveled alone. 4. to say about an action repeated in an unspecified period between the past and now: – I have visited them many times. 5. when the precise time of action is not important or unknown: – Someone has stolen my bike! Present Perfect is often used with the words like ‘just‘, ‘already‘, recently‘, lately‘, ‘still‘, ‘this week/month/year‘, today’, etc. -
Lhotse – 8516M
Lhotse – 8516m The 4th highest mountain in the world Ascent of Lobuche East to minimise the travel through the Khumbu Icefall Via the Western Cwm, Lhotse Face & Lhotse Couloir EXPEDITION OVERVIEW First climbed by Swiss climber Ernest Reiss in 1956, to this day Lhotse (Tibetan for “South Peak”) has only received just over 600 ascents compared to Everest’s several thousand. Why not join Adventure Peaks in climbing one of the most spectacular and dominating 8000m giants. Director of Adventure Peaks Dave Pritt, an Everest summiteer, has over twenty years’ experience organising and leading high altitude expeditions, including 8000m peaks. He is supported by Stu Peacock, a regular and very talented high altitude mountaineer who has climbed Broad Peak, has led successful expeditions to Cho Oyu and 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. -
Harold William Tilman (1898-1978) a Tribute Peter L10yd and Colin Putt
Harold William Tilman (1898-1978) a tribute Peter L10yd and Colin Putt On I November 1977 the Cutter 'En Avant', a converted seagoing tug, skipper Simon Richardson, in wh ich Tilman was sailing as a member ofa crew of6, left Rio de Janeiro for Port Stanley en route to Smith Island in the South Shetlands. They never J'eached the Falkland Islands and there has been no news of them since that day; it seems unlikely now that we shall ever know how they perished. The loss of his young companions was tragic, but for Bill Tilman this was perhaps a fitting end to a life of action and adventure. He had fought in both world wars, winning front line decorations in each. In the twenties he carved a farm and coffee plantation out of the bush in Kenya. The thirties were the heyday of his African and Asian journeys which continued in the first 5 years after the war. Finally there was the remaJ'kable period of his seafaring ventures in Polar waters starting in 1954 and continuing right up to the end. Had this final expedition reached its objective he would have spent his 80th birthday in the Anta~ctic. It is a unique record. Tilman won the MC in 1917 at the age of 19, bar to the MC later that year, both on the Western front where he was twice wounded; in the Second World War he served in France, Iraq and in the N African campaign before being parachuted into Albania and N Italy to serve with the partisans, for which he was awarded the DSO and made a Freeman of the city of Belluno. -
Eclogites and Other High-Pressure Rocks in the Himalaya: a Review
Downloaded from http://sp.lyellcollection.org/ by guest on September 27, 2021 Eclogites and other high-pressure rocks in the Himalaya: a review PATRICK J. O’BRIEN Department of Earth and Environmental Sciences, University of Potsdam, Karl-Liebknecht-Strasse 24/25, 14469 Potsdam-Golm, Germany 0000-0003-0235-9116 [email protected] Abstract: Himalayan high-pressure metamorphic rocks are restricted to three environments: the suture zone; close to the suture zone; and (mostly) far (>100 km) from the suture zone. In the NW Himalaya and South Tibet, Cretaceous-age blueschists (glaucophane-, lawsonite- or carpholite-bearing schists) formed in the accretionary wedge of the subducting Neo-Tethys. Microdiamond and associated phases from suture-zone ophiolites (Luo- busa and Nidar) are, however, unrelated to Himalayan subduction–collision processes. Deeply subducted and rapidly exhumed Indian Plate basement and cover rocks directly adjacent to the suture zone enclose eclogites of Eocene age, some coesite-bearing (Kaghan/Neelum and Tso Morari), formed from Permian Panjal Trap, con- tinental-type, basaltic magmatic rocks. Eclogites with a granulite-facies overprint, yielding Oligocene–Miocene ages, occur in the anatectic cordierite ± sillimanite-grade Indian Plate mostly significantly south of the suture zone (Kharta/Ama Drime/Arun, north Sikkim and NW Bhutan) but also directly at the suture zone at Namche Barwa. The sequence carpholite-, coesite-, kyanite- and cordierite-bearing rocks of these different units dem- onstrates the transition from oceanic subduction to continental collision via continental subduction. The gran- ulitized eclogites in anatectic gneisses preserve evidence of former thick crust as in other wide hot orogens, such as the European Variscides.