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Expeditions & Treks 2008/2009
V4362_JG_Exped Cover_AW 1/5/08 15:44 Page 1 Jagged Globe NEW! Expeditions & Treks www.jagged-globe.co.uk Our new website contains detailed trip itineraries 2008 for the expeditions and treks contained in this brochure, photo galleries and recent trip reports. / 2009 You can also book securely online and find out about new trips and offers by subscribing to our email newsletter. Jagged Globe The Foundry Studios, 45 Mowbray Street, Sheffield S3 8EN United Kingdom Expeditions Tel: 0845 345 8848 Email: [email protected] Web: www.jagged-globe.co.uk & Treks Cover printed on Take 2 Front Cover: Offset 100% recycled fibre Mingma Temba Sherpa. sourced only from post Photo: Simon Lowe. 2008/2009 consumer waste. Inner Design by: pages printed on Take 2 www.vividcreative.com Silk 75% recycled fibre. © 2007 V4362 V4362_JG_Exped_Bro_Price_Alt 1/5/08 15:10 Page 2 Ama Dablam Welcome to ‘The Matterhorn of the Himalayas.’ Jagged Globe Ama Dablam dominates the Khumbu Valley. Whether you are trekking to Everest Base Camp, or approaching the mountain to attempt its summit, you cannot help but be astounded by its striking profile. Here members of our 2006 expedition climb the airy south Expeditions & Treks west ridge towards Camp 2. See page 28. Photo: Tom Briggs. The trips The Mountains of Asia 22 Ama Dablam: A Brief History 28 Photo: Simon Lowe Porter Aid Post Update 23 Annapurna Circuit Trek 30 Teahouses of Nepal 23 Annapurna Sanctuary Trek 30 The Seven Summits 12 Everest Base Camp Trek 24 Lhakpa Ri & The North Col 31 The Seven Summits Challenge 13 -
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. -
Island Peak Climbing with Everest Base Camp Trek - 19 Days
GPO Box: 384, Ward No. 17, Pushpalal Path Khusibun, Nayabazar, Kathmandu, Nepal Tel: +977-01-4388659 E-Mail: [email protected] www.iciclesadventuretreks.com Island peak climbing with Everest Base Camp Trek - 19 Days Go for Island peak climbing with Everest Base Camp Trek if you are looking to jump a step ahead from trekking to mountaineering. Island peak (Imja Tse) is the most attainable climbing peak. Situated only 10 km away from Mt. Everest summit of Island peak provides 360-degree panorama of many of the highest mountains in the world. Island peak, the most climbed climbing peak of Himalaya is an extension of south end of Mt. Lhotse Shar. If you are looking for trekking in Nepal and want to test mountaineering in Nepal, then Island peak climbing is the perfect ice climbing trip to try first among the 33 "trekking peaks" of Nepal. Although Himalayan Peaks should not be underestimated, Island Peak has the potential to offer the fit and experienced hill walkers a window into the world of mountaineering in the greater ranges. Our Island Peak Climbing with Everest Base Camp provides an excellent experience for first stage mountaineering to novice adventure lovers. Our Island peak climbing with EBC Trek program starts in Kathmandu. We spend a day in Kathmandu preparing for the venture with brief UNESCO heritage sites visit. We take an exhilarating flight to Lukla and start trekking through the classic EBC trekking trail through different beautiful Sherpa villages. During the trek, we spend two nights in Namche and Dingboche to aid acclimatization. Also, we trek to Everest Base Camp to acclimatize ourselves for our Island peak climbing target. -
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 Base Camp with Island Peak Climbing
Everest Base Camp with Island Peak Climbing Trip Facts Destination Nepal Duration 16 Days Group Size 2-12 Trip Code DWTIS1 Grade Very Strenuous Activity Everest Treks Region Everest Region Max. Altitude Island Peak (6,183m) Nature of Trek Lodge to Lodge /Camping Trekking Activity per Day Approximately 4-6 hrs walking Accomodation Lodge/Tea house/Camping during the trek/climb Start / End Point Kathmandu / Kathmandu Meals Included All Meals (Breakfast, Lunch & Dinner) during the trek Best Season Feb, Mar, Apri, May, June, Sep, Oct, Nov & Dec Transportation Domestic flight (KTM-Lukla-KTM) and private vehicle (Transportation) A Leading Himalayan Trekking & Adventure Specialists TRULY YOUR TRUSTED NEPAL’S TRIP OPERATOR. Ever dreamt of summiting a Himalayan peak like Island Peak (6,189m/20,305ft) via Everest Base Camp (5,364m/17,598ft)? The alluring Himalayas in Nepal is a sight to behold. Trekking to the renowned... Discovery World Trekking would like to recommend all our valuable clients that they should arrive in Kathmandu a day earlier in the afternoon before the day we departed and start our Island Peak Climbing via Everest Base Camp the next day, To make sure that you’ll attend our Official Briefing as an important Pre-meeting. The reason we do so is we want to make sure that you get proper mental guidance and necessary information just to have a recheck of equipment and goods for the journey to make sure you haven't forgotten anything and if forgotten, then make sure that you are provided with those things ASAP on that very day. -
Changes of Glaciation in the Sagarmatha National Park (Nepal) During the Last 30 Years
Landform Analysis, Vol. 10: 85–94 (2009) Changes of glaciation in the Sagarmatha National Park (Nepal) during the last 30 years Rudolf Midriak* Matej Bel University, Institute of Science and Research, Research Institute of Landscape and Regions, Cesta na amfiteáter 1, 974 01 Banská Bystrica, Slovak Republic Abstract: Author, as a scientific participant of the first Czech-Slovak Expedition to the Mt. Everest in 1984, focuses on the glaciation in the Sagarmatha National Park (the Central Himalayas, Nepal) in 1978 (Fig. 1 and Table 1) and compares it with the present-day state. Despite overwhelming majority of the papers bearing data on the fastest retreat of the Mt. Everest’s glaciers it can be stated that obvious changes of the covering glaciers were not recorded in the Sagarmatha National Park (34.2% in the year of 1978 and 39.8% in the year of 2009). At present, for 59 sections of 18 valley glaciers (Nangpa, Melung, Lunag, Chhule, Sumna, Langmoche, Ngozumpa, Gyubanar, Lungsampa, Khumbu, Lobuche, Changri Shar, Imja, Nuptse, Lhotse Nup, Lhotse, Lhotse Shar and Ama Dablam) their length of retreat during 30 years was recorded: at 5 sections from 267 m to 1,804m (the width of retreat on 24sections being from 1 m to 224m), while for 7 sections an increase in length from 12 m to 741m was noted (the increase of glacier width at 23 sections being from 1 m to 198 m). More important than changes in length and/or width of valley glaciers are both the depletion of ice mass and an intensive growth of the number lakes: small supraglacial ponds, as well as dam moraine lakes situated below the snowline (289 lakes compared to 165 lakes in the year of 1978). -
Somos Sonar Manuscript-V24 17 July 2014
1 Changes in Imja Tsho in the Mt. Everest Region of Nepal 2 3 M. A. Somos-Valenzuela1, D. C. McKinney1, D. R. Rounce1, and A. C. Byers2, 4 [1] {Center for Research in Water Resources, University of Texas at Austin, Austin, Texas, USA} 5 [2] {The Mountain Institute, Washington DC, USA} 6 Correspondence to: D. McKinney ([email protected]) 7 8 Abstract 9 Imja Tsho, located in the Sagarmatha (Everest) National Park of Nepal, is one of the most 10 studied and rapidly growing lakes in the Himalayan range. Compared with previous studies, the 11 results of our sonar bathymetric survey conducted in September of 2012 suggest that its 12 maximum depth has increased from 90.5 m to 116.3±5.2 m since 2002, and that its estimated 13 volume has grown from 35.8±0.7 million m3 to 61.7±3.7 million m3. Most of the expansion of 14 the lake in recent years has taken place in the glacier terminus-lake interface on the eastern end 15 of the lake, with the glacier receding at about 52.1 m yr-1 and the lake expanding in area by 0.038 16 km2 yr-1. A ground penetrating radar survey of the Imja-Lhotse Shar glacier just behind the 17 glacier terminus shows that the ice is over 200 m in the center of the glacier. The volume of 18 water that could be released from the lake in the event of a breach in the damming moraine on 19 the western end of the lake has increased to 34.1±1.08 million m3 from 21 million m3 estimated 20 in 2002. -
Ghorepani Poon Hill Trek
Ghorepani Poon Hill Trek https://www.tmgadventure.com/packages/ghorepani-poon-hill-trek/ Trips Facts Trip Code: TMG-AP100 Group Size: 1-20 person Included Meals: Trip Mode: Elevation: 3210m Accomodation: hotel and mountain guesthouse Transport: 207 Start Point: Kathmandu End Point: Kathmandu Best Season: February, March, April, May, August, September, October, November, December Trip Highlights Mountain views of Annapurna I, II, South Gangapurna, Machhapuchhere, and Hiunchuli Rural villages Poon Hill Climb 3381 steps in surprise and rewarded by the panoramic views of Dhaulagiri. Stay of Nepal’s heritage village of Ghandruk, with the view of Annapurna South and Fishtail.eigh Ghandruk village Pokhara city In the list, you see Ghorepani Poon Hill Trek. When it comes to an easy, short trek and scenic trekking trail, ask yourself, is there anything better than the Ghorepani Poon Hill Trek in Nepal or the world? Poon Hill, one of the best viewpoints of the Annapurna Region is so rewarding that all you can say is beautiful. When you reach Poon Hill, a viewpoint, you will see the mountain ranges. Some of the famous mountains that you will see are Dhaulagiri, Annapurna I, Annapurna South, Annapurna II, Annapurna III, Annapurna IV, Gangapurna, Lamjung Himal, Barasikhar, Nilgiri, Tukuche Peak, Hiunchuli, and Manaslu. If you love mountains and their beauties, then you should do the Ghorepani Poon Hill Trek. The trek shows you the views that you have always wanted to see in your life, outside your country. The Annapurna Ranges that you will see take your breath away. When these ranges satisfy your eyes, you find this short trek Ghorepani Poon Hill worth of traveling. -
Ghorepani Poon Hill Trek - 7 Days
GPO Box: 384, Ward No. 17, Pushpalal Path Khusibun, Nayabazar, Kathmandu, Nepal Tel: +977-01-4388659 E-Mail: [email protected] www.iciclesadventuretreks.com Ghorepani Poon Hill Trek - 7 Days Ghorepani Poon Hill Trek at Annapurna region of Nepal would be an ideal walking trip for you if you are looking for short hiking holiday. Poon Hill trek will complete in a week without much rigorous effort as we will be walking across the mountain route. The major highlight of Ghorepani Hike is the magical sunrise Himalayan views from Poon Hill viewpoint that surely makes you spellbound. Poon Hill Trek in Nepal begins as we travel from Kathmandu to Pokhara. Naturally blessed Pokhara is not less than paradise. Pokhara surrounds beautiful mountains, pristine lakes, waterfalls and other attractions. Initially we drive to starting point of the trek at Nayapul.Further, we hike towards Tikhedhunga, Ulleri and Ghorepani as we climb 3300 stone steps and cross the beautiful bamboo and rhododendron forests that blossom in spring (March, April) season. The naming of Ghorepani Poon Hill is derived from two local words ‘Ghore (Horse)’ and ‘Pani (Water)’. This place used to be resting point for ancient traders who found water in the place for their horses. And Poon is the name of the nearby hill. Finally we get ready for hiking up to Poon Hill at dawn for experiencing magical sunrise views. Views of snow capped mountains from Poon Hill can’t be described in words when the warm rays of early sun gradually strikes the Himalayan giants including Mt Dhaulagiri (8,167m), Mt Annapurna I (8,091m), Mt Nilgiri (7,040m), Annapurna south (7,219m),Annapurna II (7,937m), Annapurna III (7,555m), Annapurna IV (7,525m), Hunchuli (6,441m), fishtail or Machapuchare (6,997m), Lamjung Himal (6,986m), Tukuche peak (6,920m), Dhampus Peak (6,012m) among others. -
Climate Change, "Everestification,"
CLIMATE CHANGE, "EVERESTIFICATION," AND THE FUTURE OF MOUNTAINEERING ON ANNAPURNA I by Jamie Leanne Hutchinson A Thesis Submitted in partial fulfillment of the requirements for the degree Master of Environmental Studies The Evergreen State College June 2020 ©2020 by Jamie Hutchinson. All rights reserved. This Thesis for the Master of Environmental Studies Degree by Jamie Hutchinson has been approved for The Evergreen State College by ________________________ Kathleen Saul, Ph. D. Member of the Faculty ________________________ Date ABSTRACT Climate Change, "Everestification", and the Future of Mountaineering on Annapurna I Jamie Hutchinson This study aims to research how climate change is affecting the Annapurna Conservation Area in the Western Region of Nepal. This region consists of two mountain districts, three hill districts, and encompasses the Annapurna massif. Temperature and Precipitation data was obtained from the Department of Hydrology and Meteorology, Nepal, spanning thirty years (1988-2018). Monthly, Seasonal and Yearly data were aggregated and averaged for both datasets, and statistical analysis was completed using JMP and Excel. Results indicate overall warming in all districts by 1°C, with higher elevations being impacted more than lower. Precipitation tests show strong seasonal intensity in the summer months, sometimes predating monsoon season, with higher elevations receiving less snow than previously recorded. Additional focus was then turned to Annapurna I in order to analyze expedition data for the last thirty years (1989 – 2019). All 8,000-meter peaks within Nepal were studied for expedition size and experience in order to establish climbing trends that lead to "Everestification." Current trends show an increase in expedition size but a overall decrease in inexperienced climbers. -
Survey Re Eport O N the S Seti Rive 2012) Er Floo D,Nepa Al(May Y 5
Survey Report on the Seti River Flood,Nepal(May 5, 2012) November 2012 The Japanese Disaster Survey Team for the Seti River Flood Plate Bird’s eye view of the Seti watershed (Modified from Google Earth) 中国China Himlung 7,126m Jomson AnnapurnaⅣ 7,525m Dhaulagiri 8,167m AnnapurnaⅢ 7,555m Manaslu 8,163m AnnapurnaⅠ 8,091m Chame AnnapurnaⅡ 7,937m Machhapuchhre 6,993m Beni Bharatpur Baglung Pokhara Damauli Bharatpuur Nepネパaーl ル 0 20 40 km インド India Annapurna Peak Ⅳ 45 5 Assumed areas of the rock avalanche 50 10 55 15 Panoramic view of the rock slide on the west-facing slopes of Annapurna Peak IV (Gentle foot slopes can be seen in the center.) 60 20 65 25 70 Earth pillars of lacustrine deposits 30 (Rounded slopes appear in the right section.) 550m 75 850m 35 80 40 The Seti Gorge formed in limestone Rockslide on the west-facing slopes of Annapurna 85 (Mud originating from the rock avalanche can be seen Peak IV at the lower part.) (Collapsed slopes in the center right and fragmented debris can be seen on the foot slopes.) Maximum level of mud flow 20m 35m Seti Gorge channel way Third bending point of Seti River at Kapuche (It breached after the temporary blockage. ) 60m 15m Trees falling toward downstream (There is mud River channel just downstream of the third bending clinging to them.) point at Baraudi 54m 12m Temporary damming-up area near Kapuche (Two Disaster area around the suspension bridge at houses remain on the lower terrace at Yomo.) Karapani (The flood overtopped the left-bank river terrace due to the momentary river blockage.) Contents 1. -
Tain. Its Northern Summit Is 23,440 Feet High and Its Southern One 23,000 Feet
616 THE AMERICAN ALPINE JOURNAL Gaurishankar, South Summit. Gaurishankar is a twin-peaked moun- tain. Its northern summit is 23,440 feet high and its southern one 23,000 feet. Before 1964 six expeditions tried unsuccessfully to climb the moun- tain. The Buddhist Shergas living south of the peak can only see the southern summit and call it Jomo Tseringma. It is considered the most holy mountain of the Sherpas. Our team finally consisted of John Barry, Tim Leach, Swiss Guy Neithardt, Sherpa Pemba Lama and me as leader. We mounted a light-weight expedition taking a minimum of equipment. Though we had permission for either the south or the west ridge to the south summit, we chose the west ridge because it is slightly shorter. The approach march took ten days and went via Barabhise, Charikot and Lamobagar. We hired 48 porters who carried by October 8 to the same Base Camp used by the American expedition in the spring. It was at 16,000 feet. Leach suffered from the altitude and could not rejoin us until October 28. Between October 10 and 18 we four carried loads to Advance Camp at 17,400. feet at the foot of the west ridge. We stocked it with 20 days’ food for four people. Without redescent for further pro- visions, we fixed our 17 ropes between camps, pulling up the ropes as we moved up and stringing them out again. The climb took 23 days. The initial obstacle was a lOOO-foot-deep gap in the ridge below two steep rock and ice towers.