Everest 1935: the Forgotten Adventure
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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. -
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 -
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. -
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. -
KAMA CHU VALLEY and KANGSHUNG GLACIER TREK 2019 PHOTOS PART 5 Wordpress
TIBET: KAMA CHU AND KHARTA VALLEY TREK AND FRIENDSHIP HIGHWAY TIBET Qomolangma National park May, 2019 PART 5 by WILLIAM D BOEHM MT Everest from near Tingri on the way to Rongbuk, Below Tsibri Mountqins, schists like ribs before Tingri DAY22-23 DAY 8,9 May 29 Somale Yuna village in the Kharta Valley to Rongbuk and North Face of Mt Everest back to Tingri on the Friendship Highway. From Somale we drove back to the village of Phadhruchi then back to Old Tingri also known as Zhaxizongxiang at the road junction. We turned west this time and drove southwest into the Rongphu Valley for several hours to ascend into the North Face of Mt Everest and the Rongbuk Glacier to stay at a small lodge at the Rongbuk Monastery. Transferred our gear to an electric bus to overnight near the Rongphu Monastery situated 15 km below the Base Camp. Access to Everest Base Camp used by the famous interwar British expeditions is currently restricted to mountaineers with the necessary permits. Saw a beautiful evening sunset on the north face of North Face of Mt Everest from Ronbuk of Everest. At Rongphu we stayed in the square lodge at5176 m (16,981 ft). Bathroom pretty bad, three concrete holes per male and female side, no doors, open for anyone to see you squat, awful odor. Hi winds swept down the mountain and was very cold that evening filming the mountain. Didn’t sleep that night trying to catch every third breath, long night at this high altitude. Early morning with the window open, a yak stuck its head in to check us out. -
The Mount Everest Expedition Author(S): C
The Mount Everest Expedition Author(s): C. K. Howard-Bury Source: The Geographical Journal, Vol. 59, No. 2 (Feb., 1922), pp. 81-99 Published by: geographicalj Stable URL: http://www.jstor.org/stable/1781386 Accessed: 26-06-2016 20:43 UTC Your use of the JSTOR archive indicates your acceptance of the Terms & Conditions of Use, available at http://about.jstor.org/terms JSTOR is a not-for-profit service that helps scholars, researchers, and students discover, use, and build upon a wide range of content in a trusted digital archive. We use information technology and tools to increase productivity and facilitate new forms of scholarship. For more information about JSTOR, please contact [email protected]. The Royal Geographical Society (with the Institute of British Geographers), Wiley are collaborating with JSTOR to digitize, preserve and extend access to The Geographical Journal This content downloaded from 128.163.2.206 on Sun, 26 Jun 2016 20:43:02 UTC All use subject to http://about.jstor.org/terms The Geographical Journal Vol. LIX No. 2 February 1922 THE MOUNT EVEREST EXPEDITION Lieut.-Colonel C. K. Howard-Bury, D.S.O., Chief of the Expedition Read at the Joint Meeting of the Society and the Alpine Club at the Queeris Hall% 20 December 1921. Maps followingp. 152. OF previously Mount Everest known, and andthe thecountry maps thatof that surrounded district itwere very vague little and was inaccurate. Mount Everest was discovered and measured from the plains of India from a distance of about 150 miles about the year 1850, but it was not given the name of Mount Everest until 1858, in honour of Colonel Everest, who was the Surveyor-General in India at the time of its discovery. -
The Structural Geometry, Metamorphic and Magmatic Evolution of the Everest Massif, High Himalaya of Nepal–South Tibet
Journal of the Geological Society, London, Vol. 160, 2003, pp. 345–366. Printed in Great Britain. The structural geometry, metamorphic and magmatic evolution of the Everest massif, High Himalaya of Nepal–South Tibet M. P. SEARLE1,R.L.SIMPSON1,R.D.LAW2,R.R.PARRISH3 &D.J.WATERS1 1Department of Earth Sciences, Oxford University, Parks Road, Oxford OX1 3PR, UK (e-mail: [email protected]. uk) 2Department of Geological Sciences, Virginia Tech., Blacksburg, Virginia 24061, USA 3Department of Geology, Leicester University, Leicester LE1 7RH, and NERC Isotope Geosciences Laboratory, Keyworth, Nottingham, NG12 5GG Abstract: This paper presents a new geological map together with cross-sections and lateral sections of the Everest massif. We combine field relations, structural geology, petrology, thermobarometry and geochronology to interpret the tectonic evolution of the Everest Himalaya. Lithospheric convergence of India and Asia since collision at c. 50 Ma. resulted in horizontal shortening, crustal thickening and regional metamorphism in the Himalaya and beneath southern Tibet. High temperatures (.620 8C) during sillimanite grade metamorphism were maintained for 15 million years from 32 to 16.9 Æ 0.5 Ma along the top of the Greater Himalayan slab. This implies that crustal thickening must also have been active during this time, which in turn suggests high topography during the Oligocene–early Miocene. Two low-angle normal faults cut the Everest massif at the top of the Greater Himalayan slab. The earlier, lower Lhotse detachment bounds the upper limit of massive leucogranite sills and sillimanite–cordierite gneisses, and has been locally folded. Ductile motion along the top of the Greater Himalayan slab was active from 18 to 16.9 Ma. -
ASIAN ALPINE E-NEWS Issue No 68. July 2020
ASIAN ALPINE E-NEWS Issue No 68. July 2020 Northwest face of Mt Everest and left Lhotse from the remote Kama Valley, Tibet (J Hans) (Willian Boehm’s TIBET and QINGHAI) ① KAMA CHU & KHARTA VALLEY TREK- FRIENDSHIP HIGHWAY TIBET May 2019 Page 2 ~ 14 ② QINGHAI SNOW LEOPARD EXPEDITION TO UPPER MEKONG RIVER September 2019 Page 15 ~ 27 1 TIBET: KAMA CHU AND KHARTA VALLEY TREK AND FRIENDSHIP HIGHWAY TIBET May, 2019 PART 2 Mt Everest, the highest mountain in the world and encompassing Qomologangma National Nature Reserve. After acclimating for several days spent exploring Lhasa, I had the opportunity to spend some time at the new Songtsam Linka, where I met the manager Lhamo and Baima Dorje’s sister, and had a chance to catch up with the new Tibetan lodges being built to the east to connect Yunnan with Kham Tibet and Lhasa. The following morning, we loaded up our gear into a bus and began the several days journey south to Gyantse, then Shigatse (Old Tingri) along the friendship highway. Our journey would continue south another days driving to the village of Kharta on the northern edge of the Himalaya bordering Nepal. We would explore and trek in an isolated area known as the Kama Valley on the eastern edge of Mt Everest along the Kangshung glacier for 8 days, then complete the journey west across southern Tibet driving along the friendship highway towards Paiku Co lake below Gyachung Kang 7952 m (26089 ft) before turning south to Gyirong Town, (Kyirong). We would then cross into Nepal and the final day navigate a very rough dirt road until Kathamandu. -
The Kangshung Face September 26 – October 17, 2015 (22 Days)
Cathy Taylor Ann © Tibet: The Kangshung Face September 26 – October 17, 2015 (22 days) Tibet’s unspoiled Kangshung Valley, dropping directly from the east face of Everest, is a remote and isolated region with magnificent panoramas of a panoply of Himalayan peaks, including three of the five highest mountains on earth: Everest, Lhotse, and Makalu. When mountaineer and explorer Sir Francis Younghusband wrote in The Epic of Mount Everest, he spoke of “the dazzling cliffs of Makalu and Chomolonzo dropping almost a sheer 10,000 feet into the valley below and…powdered white with fresh fallen snow—a spectacle of perhaps unequaled mountain glory.” Our journey begins in the sacred city of Lhasa and travels across the vast Tibetan Plateau to Kharta, from where we head out on an 11-day hiking circuit through fabulous hidden valleys and up to the base camp used by expeditions attempting the East, or Kangshung Face, of Everest. We’ll travel through luxuriant forests of rhododendron, birch, and willow trees, past sparkling lakes and yak herder’s camps, across alpine meadows and glacial moraines, and throughout enjoy a dazzling feast for the eyes—the awesome peaks and glacier faces of the Himalayan giants we have always dreamed of. ________________________________________________________________________________________________________ CATTARA PO Box 1366 ~ Sausalito, CA 94966 Phone/Fax (415) 331-9539 ~ [email protected] - 1 - TRIP DETAILS Very challenging11 days strenuous hiking on rocky, steep terrain at high elevation (max. 17,300'), rugged road travel; 12 nights camping, 9 nights hotels ITINERARY (You will likely need to leave the U.S. on September 24 or 25 depending on the routing in order to arrive in Chengdu on September 26.) Day 1, September 26Chengdu, China Arrive in Chengdu, China, and transfer to the hotel.