The Conquest of Mount Everest by the Chinese
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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 -
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. -
Catalogue 48: June 2013
Top of the World Books Catalogue 48: June 2013 Mountaineering Fiction. The story of the struggles of a Swiss guide in the French Alps. Neate X134. Pete Schoening Collection – Part 1 Habeler, Peter. The Lonely Victory: Mount Everest ‘78. 1979 Simon & We are most pleased to offer a number of items from the collection of American Schuster, NY, 1st, 8vo, pp.224, 23 color & 50 bw photos, map, white/blue mountaineer Pete Schoening (1927-2004). Pete is best remembered in boards; bookplate Ex Libris Pete Schoening & his name in pencil, dj w/ edge mountaineering circles for performing ‘The Belay’ during the dramatic descent wear, vg-, cloth vg+. #9709, $25.- of K2 by the Third American Karakoram Expedition in 1953. Pete’s heroics The first oxygenless ascent of Everest in 1978 with Messner. This is the US saved six men. However, Pete had many other mountain adventures, before and edition of ‘Everest: Impossible Victory’. Neate H01, SB H01, Yak H06. after K2, including: numerous climbs with Fred Beckey (1948-49), Mount Herrligkoffer, Karl. Nanga Parbat: The Killer Mountain. 1954 Knopf, NY, Saugstad (1st ascent, 1951), Mount Augusta (1st ascent) and King Peak (2nd & 1st, 8vo, pp.xx, 263, viii, 56 bw photos, 6 maps, appendices, blue cloth; book- 3rd ascents, 1952), Gasherburm I/Hidden Peak (1st ascent, 1958), McKinley plate Ex Libris Pete Schoening, dj spine faded, edge wear, vg, cloth bookplate, (1960), Mount Vinson (1st ascent, 1966), Pamirs (1974), Aconcagua (1995), vg. #9744, $35.- Kilimanjaro (1995), Everest (1996), not to mention countless climbs in the Summarizes the early attempts on Nanga Parbat from Mummery in 1895 and Pacific Northwest. -
Human Factors in High-Altitude Mountaineering
Journal of Human Performance in Extreme Environments Volume 12 Issue 1 Article 1 Published online: 5-8-2015 Human Factors in High-Altitude Mountaineering Christopher D. Wickens Alion Science and Technology, [email protected] John W. Keller Alion Science and Technology, [email protected] Christopher Shaw Alion Science and Technology, [email protected] Follow this and additional works at: https://docs.lib.purdue.edu/jhpee Part of the Industrial and Organizational Psychology Commons Recommended Citation Wickens, Christopher D.; Keller, John W.; and Shaw, Christopher (2015) "Human Factors in High-Altitude Mountaineering," Journal of Human Performance in Extreme Environments: Vol. 12 : Iss. 1 , Article 1. DOI: 10.7771/2327-2937.1065 Available at: https://docs.lib.purdue.edu/jhpee/vol12/iss1/1 This document has been made available through Purdue e-Pubs, a service of the Purdue University Libraries. Please contact [email protected] for additional information. This is an Open Access journal. This means that it uses a funding model that does not charge readers or their institutions for access. Readers may freely read, download, copy, distribute, print, search, or link to the full texts of articles. This journal is covered under the CC BY-NC-ND license. Human Factors in High-Altitude Mountaineering Christopher D. Wickens, John W. Keller, and Christopher Shaw Alion Science and Technology Abstract We describe the human performance and cognitive challenges of high altitude mountaineering. The physical (environmental) and internal (health) stresses are first described, followed by the motivational factors that lead people to climb. The statistics of mountaineering accidents in the Himalayas and Alaska are then described. -
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. -
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 -
1953 Conquest of Mount Everest
1953 Conquest of Mount Everest Mount Everest is in the Himalaya mountain range located between Nepal and Tibet, an autonomous region of China. At 8,849 meters (29,032 feet), it is considered the tallest point on Earth. In the 19th century, the mountain was named after George Everest, a former Surveyor General of India. The Tibetan name is Chomolungma, which means “Mother Goddess of the World.” The Nepali name is Sagarmatha. The 1953 British Mount Everest expedition was the ninth to attempt the first ascent and the first confirmed to have succeeded when Sherpa Tenzing Norgay and (later Sir) Edmund Hillary reached the summit on 29 May 1953. Led by Colonel John Hunt, it was organised and financed by the Joint Himalayan Committee. News of the expedition's success reached London in time to be released on the morning of Queen Elizabeth II's coronation on 2nd June. The conquest of Everest caught the imagination of the world. So, there are many commemorative & souvenir issues & first day covers. Consequently, it can make a good philatelic theme. This display shows just a small selection of what is available. This Indian first day cover shows a photo, taken by Edmund Hillary, of Sherpa Tenzing Norgay on the summit. Postcard - Edmund Hillary, Tenzing Norgay & Sir John Hunt’s Expedition Team Sir John Hunt (L), leader of the British Everest expedition, and Sir Edmund Hillary (R) arrive at Lancaster House for reception being given in their honour. Earlier they had been received by Queen Elizabeth who knighted the two men. Edmund Hilary Quotes “People do not decide to become extraordinary. -
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. -
The Modernisation of Elite British Mountaineering
The Modernisation of Elite British Mountaineering: Entrepreneurship, Commercialisation and the Career Climber, 1953-2000 Thomas P. Barcham Thesis submitted in partial fulfilment of the requirements of De Montfort University for the degree of Doctor of Philosophy Submission date: March 2018 Contents Abstract ................................................................................................................................................... 4 Acknowledgments ................................................................................................................................... 5 Table of Abbreviations and Acronyms .................................................................................................... 6 Table of Figures ....................................................................................................................................... 7 Chapter 1. Introduction .......................................................................................................................... 8 Literature Review ............................................................................................................................ 14 Definitions, Methodology and Structure ........................................................................................ 29 Chapter 2. 1953 to 1969 - Breaking a New Trail: The Early Search for Earnings in a Fast Changing Pursuit .................................................................................................................................................. -
Everest 1935: the Forgotten Adventure
Everest from the North 'We are going to sail to the top this time and God with us - or stamp to the top with our teeth in the wind.' George Leigh Mallory Letter to Tom LongstajJ, 1924 CHARLES WARREN Everest 1935: The Forgotten Adventure (Plate 5) s the only surviving member of Eric Shipton's reconnaissance expedi A tion to Mount Everest in 1935, I have allowed myself to be persuaded by Michael Ward that I ought to put on record my memories of that expe dition, which never got the publicity it deserved. It seemed at the outset to have a not unreasonable chance of success on the mountain, but my diary notes show that the monsoon season was unsuitable and that we suffered from many altitude-related health problems. Moreover, without the help of oxygen we probably had little real prospect of pulling off 'the moun taineering coup of all time'. However, we carried out valuable survey work and made first ascents of Kharta Phu, Kharta Changri and many other peaks above 20,OOOft. I think it was early in 1935 that Shipton asked me if I would join his proposed reconnaissance to Everest that year. He explained that we would not be expected to climb the mountain itself because it would be too late in the season to do that. The purposes of the expedition would be threefold: firstly, to examine snow conditions during the monsoonperiod; secondly, to carry out a professional survey of the environs of Everest under Michael Spender; and thirdly, to test potential newcomers for an all-out attempt to climb the mountain in 1936. -
Polyphase Deformation, Dynamic Metamorphism, and Metasomatism of Mount Everest’S Summit Limestone, East Central Himalaya, Nepal/Tibet
Polyphase deformation, dynamic metamorphism, and metasomatism of Mount Everest’s summit limestone, east central Himalaya, Nepal/Tibet Travis L. Corthouts, David R. Lageson, and Colin A. Shaw EARTH SCIENCE DEPARTMENT, MONTANA STATE UNIVERSITY, BOZEMAN, MONTANA 59715, USA ABSTRACT New samples collected from a transect across the summit limestone of Mount Everest (Qomolangma Formation) show that multiple distinct deformational events are discretely partitioned across this formation. Samples from the highest exposures of the Qomolangma Formation (Everest summit) preserve a well-developed mylonitic foliation and microstructures consistent with deformation temperatures of ≥250 °C. Thermochronologic and microstructural results indicate these fabrics were ingrained during initial contractile phases of Himalayan oro- genesis, when crustal thickening was accommodated by folding and thrusting of the Tethyan Sedimentary Sequence. In contrast, samples from near the base of the Qomolangma Formation (South Summit) preserve extensional shear deformation, indicate metasomatism at temperatures of ~500 °C, and contain a synkinematic secondary mineral assemblage of muscovite + chlorite + biotite + tourmaline + rutile. Shear fabrics preserved in South Summit samples are associated with activity on the Qomolangma detachment, while the crystallization of secondary phases was the result of reactions between the limestone protolith and a volatile, boron-rich fluid that infiltrated the base of the Qomolangma Formation, resulting in metasomatism. The 40Ar/39Ar dating of synkinematic muscovite indicates the secondary assemblage crystallized at ca. 28 Ma and that shear fabrics were ingrained at ≥18 Ma. This paper presents the first evidence that Everest’s summit lime- stone records multiple phases of deformation associated with discrete stages in Himalayan orogenesis, and that the structurally highest strand of the South Tibetan detachment on Everest was initially active as a distributed shear zone before it manifested as a discrete brittle detachment at the base of the Qomolangma Formation.