Trek to Everest Base Camp
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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 -
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. -
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. -
SLEEPING in EVEREST BASE CAMP TREK ITINERARY Itinerary
SLEEPING IN EVEREST BASE CAMP TREK ITINERARY Taking the journey to the base of the World’s highest peak, with our award-winning team, will be the highlight of any trekkers career! Our unique itinerary includes extra acclimatization at the critical point as well as 4 guides for every group of ten trekkers. The journey in the Everest Region, also known as the Solukhumbu Region, begins in the small village of Lukla. From here, the total distance to Everest Base Camp and back is just over 82 miles or 132km, covering over 6,000m/ 20,000 feet of elevation. This makes this spectacular journey to Mount Everest a challenging and rewarding experience. This trek should not be taken lightly. When going to these levels of altitude, your body’s acclimatization to the lack of oxygen is the real key to success, and because of this, we have added an extra day to our itinerary, which has given us 95% success rate. This also gives you a safer and more enjoyable experience into high altitude. We will also cover the daily distances on the trail at a very slow and steady pace, to aid the acclimatization process. Even though we are giving you the best chance of success with our acclimatization schedule, you still need to play your part and come physically prepared for this adventure. We recommend 5 to 6 days a week training in the lead up to your trip. We are your best resource for information on the trek and are available five days a week in support of your journey to Everest Base Camp. -
Nuptse 7,861M / 25,790Ft
NUPTSE 7,861M / 25,790FT 2022 EXPEDITION TRIP NOTES NUPTSE EXPEDITION TRIP NOTES 2022 EXPEDITION DETAILS Dates: April 9 to May 20, 2022 Duration: 42 days Departure: ex Kathmandu, Nepal Price: US$38,900 per person Crossing ladders in the Khumbu Glacier. Photo: Charley Mace. During the spring season of 2022, Adventure Consultants will operate an expedition to climb Nuptse, a peak just shy of 8,000m that sits adjacent to the world’s highest mountain, Mount Everest, and the world’s fourth highest mountain, Mount Lhotse. Sitting as it does, in the shadows of its more famous partners, Nuptse receives a relatively low number of EXPEDITION OUTLINE ascents. Nuptse’s climbing route follows the same We congregate in Nepal’s capital, Kathmandu, line of ascent as Everest as far as Camp 2, from where we meet for a team briefing, gear checks where we cross the Western Cwm to establish a and last-minute purchases before flying by fixed Camp 3 on Nuptse. From that position, we ascend wing into Lukla Airport in the Khumbu Valley. We directly up the steep North East Face and into trek the delightful approach through the Sherpa Nuptse’s summit. The terrain involves hard ice, homelands via the Khumbu Valley Along the way, sometimes weaving through rocky areas and later we enjoy Sherpa hospitality in modern lodges with lower angled snow slopes. good food, all the while being impressed by the spectacular scenery of the incredible peaks of the The Nuptse climb will be operated alongside the lower Khumbu. Adventure Consultants Everest Expedition and therefore will enjoy the associated infrastructure We trek over the Kongma La (5,535m/18,159ft), a and legendary Base Camp support. -
Blackrock Trek Everest Base Camp
Blackrock trek Everest Base Camp Pass through breathtaking mountain scenery, original Buddhist carvings and the legendary monastery of the Tengboche, and experience day-to-day life on the world’s tallest mountain! actionchallenge on Everest The Everest Base Camp challenge takes us through some of the most breathtaking mountain scenery the world has to offer! It’s an incredible sixteen day adventure, which will only keep you out of the office for ten days! We follow the contours of valleys along glacial rivers, we trek up through stunning rhododendron forests and pass through some of the highest villages on earth. The spirit of the mountains is intertwined with the spirit of the Sherpa people; colourful prayer flags flutter in the wind, prayer wheels spin and intricately carved mani stones line our route. From high above Namche we watch the sun rise over the snow capped peaks of the Himalayan giants, at night we see the mountain of Nuptse bathed in the ethereal light of the full moon and from Kala Patthar we catch an awe-inspiring view of the summit of Everest. As we ascend above the tree line the expedition buzz is palpable. Team spirit and determination drives us along the Khumbu glacier to reach the hallowed ground of mountaineers, Everest Base Camp. Standing on the roof of the world is an incredible shared moment that will last a lifetime. This is a true challenge that bonds us together and, back in Kathmandu, we enjoy a special dinner to celebrate our incredible journey to Everest, the greatest mountain on earth. -
A Perspective of the Cumulative Risks from Climate Change on Mt
International Journal of Environmental Research and Public Health Review A Perspective of the Cumulative Risks from Climate Change on Mt. Everest: Findings from the 2019 Expedition Kimberley R. Miner 1,* , Paul Andrew Mayewski 1, Mary Hubbard 2, Kenny Broad 3,4,5, Heather Clifford 1,6, Imogen Napper 3,7, Ananta Gajurel 3, Corey Jaskolski 4,5 , Wei Li 8, Mariusz Potocki 1,5 and John Priscu 8 1 Climate Change Institute, University of Maine, Orono, ME 04463, USA; [email protected] (P.A.M.); [email protected] (H.C.); [email protected] (M.P.) 2 Department of Earth Sciences, Montana State University, Bozeman, MT 59717, USA; [email protected] 3 National Geographic Society, Washington, DC 02917, USA; [email protected] (K.B.); [email protected] (I.N.); [email protected] (A.G.) 4 Abess Center for Ecosystem Science and Policy, University of Miami, Coral Gables, FL 33146, USA; [email protected] 5 Virtual Wonders, LLC, Wisconsin, Delafield, WI 53018, USA 6 School of Earth and Climate Sciences, University of Maine, Orono, ME 04463, USA 7 International Marine Litter Research Unit, University of Plymouth, Plymouth PL4 8AA, UK 8 Department of Land Resources and Environmental Sciences, Montana State University, Bozeman, MT 59717, USA; [email protected] (W.L.); [email protected] (J.P.) * Correspondence: [email protected] Abstract: In 2019, the National Geographic and Rolex Perpetual Planet Everest expedition success- fully retrieved the greatest diversity of scientific data ever from the mountain. The confluence of geologic, hydrologic, chemical and microbial hazards emergent as climate change increases glacier Citation: Miner, K.R.; Mayewski, P.A.; Hubbard, M.; Broad, K.; Clifford, melt is significant. -
Everest Base Camp Trek 12 D/11 N
Everest Base Camp Trek 12 D/11 N Pre Trek: Travel to Kathmandu (1,300m): To ensure all permit paperwork and other necessary arrangements are completed before you trip it is important that you are in Kathmandu at least 24 hours prior to the trek commencement. The local operator will contact you to collect the required documents early in the afternoon. At 5:00 pm (17:00) a rickshaw will pick you up from your hotel and bring you to the trekking offices for a safety briefing on the nature of the trek, equipment and team composition. You will meet your trek leader and other team members. You can also make your last minute purchases of personal items as you will be flying to the Himalayas tomorrow. At 6:00 pm (18:00) we will make our way to a welcome dinner and cultural show where you will learn about Nepali culture, music and dance and get to know your trekking team. Overnight in Kathmandu (self selected) Included meals: Dinner DAY 01: Kathmandu to Lukla then trek to Phakding (2,652m): 25 minute flight, plus 3 to 4 hour trek. After breakfast you will be escorted to the domestic terminal of Kathmandu airport for an early morning flight to Lukla (2,800m), the gateway destination where our trek begins. After an adventurous flight above the breathtaking Himalaya, we reach the Tenzing-Hillary Airport at Lukla. This is one of the most beautiful air routes in the world culminating in a dramatic landing on a hillside surrounded by high mountain peaks. -
Quaternary Glaciation of Mount Everest
* Manuscript and tables Click here to view linked References Quaternary glaciation of Mount Everest Lewis A. Owena, Ruth Robinsonb, Douglas I. Bennb, c, Robert C. Finkeld, Nicole K. Davisa, Chaolu Yie, Jaakko Putkonenf, Dewen Lig, Andrew S. Murrayh a Department of Geology, University of Cincinnati, Cincinnati, OH 45221, USA b School of Geography and Geosciences, University of St. Andrews, St. Andrews, KY16 9AL, UK c Department of Geology, University Centre in Svalbard, N-9171 Longyearbyen, Norway d Department of Earth and Planetary Sciences, University of California, Berkeley, CA 95064 USA and Centre Européen de Recherche et d'Enseignement des Géosciences de l'Environnement, 13545 Aix en Provence Cedex 4 France e Institute for Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100085, China f Department of Geology and Geological Engineering, 81 Cornell St. - Stop 8358, University of North Dakota, Grand Forks, ND 58202-8358 USA g China Earthquake Disaster Prevention Center, Beijing, 100029,China h Nordic Laboratory for Luminescence Dating, Department of Earth Sciences, University of Aarhus, Risø DTU, DK 4000 Roskilde, Denmark Abstract The Quaternary glacial history of the Rongbuk valley on the northern slopes of Mount Everest is examined using field mapping, geomorphic and sedimentological methods, and optically stimulated luminescence (OSL) and 10Be terrestrial cosmogenic nuclide (TCN) dating. Six major sets of moraines are present representing significant glacier advances or still-stands. These date to >330 ka (Tingri moraine), >41 ka (Dzakar moraine), 24-27 ka (Jilong Moraine), 14-17 ka (Rongbuk moraine), 8-2 ka (Samdupo moraines) and ~1.6 ka (Xarlungnama moraine). The Samdupo glacial stage is subdivided into Samdupo I (6.8-7.7 ka) and Samdupo II (~2.4 ka). -
Nepal Everest Base Camp Trek Trip Packet
Nepal Mt. Everest Base Camp Trek TRIP SUMMARY Mt. Everest base camp is a magical place. TRIP DETAILS It’s nestled deep in the Himalayan mountain range, 30 • Price: $2,999 USD miles up the Khumbu valley. Its elevation is over 17,000 feet. Compared to the surrounding peaks, Everest base • Duration: 15 days camp is dwarfed by nearly 12,000 ft. • March 22 - April 5, 2019 • March/April, 2020 One of the most formidable facts about Everest base camp is that it’s constructed on a moving, living glacier. • Difficulty: Moderate-Difficult As the glacier moves down the Khumbu valley, it creeks and moans, giving the adventurous something to brag about. It’s no wonder that it’s found on bucket lists around the globe—as it should be. It’s Volant’s mission to safely escort individuals to base camp and back, while at the same time checking off for their clients one of the most desired bucket list items seen around the world! www.Volant.Travel "1 INCLUSIONS & MAP INCLUSIONS EXCLUSIONS • Scheduled meals in Kathmandu • Items of a personal nature (personal gear, • Round trip airport transfers telephone calls, laundry, internet us, etc.) • Scheduled hotels in Kathmandu • Airfare to Kathmandu • Airfare from Kathmandu to Lukla • Staff/guide gratuities • All meals and overnight accommodations while • Nonscheduled meals in Kathmandu on the trek • Alcoholic beverages • Porters and pack animals • Nepal visa costs: $40 USD, 30 days • Sagarmatha Nat’l Park entrance fee • Trip cancellation insurance • TIMS Card • Evacuation costs, medical, and rescue insurance To begin your adventure in Nepal, you’ll be picked up at Tribhuvan International Airport in Kathmandu by a Volant Travel representative and transferred to your hotel, the Hotel Mulberry. -
Modelling Glacier Change in the Everest Region, Nepal Himalaya Jm Shea, W
Modelling glacier change in the Everest region, Nepal Himalaya Jm Shea, W. W. Immerzeel, P Wagnon, Christian Vincent, S Bajracharya To cite this version: Jm Shea, W. W. Immerzeel, P Wagnon, Christian Vincent, S Bajracharya. Modelling glacier change in the Everest region, Nepal Himalaya. The Cryosphere, Copernicus 2015, 9 (3), pp.1105-1128. 10.5194/tc-9-1105-2015. insu-01284412 HAL Id: insu-01284412 https://hal-insu.archives-ouvertes.fr/insu-01284412 Submitted on 7 Mar 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. The Cryosphere, 9, 1105–1128, 2015 www.the-cryosphere.net/9/1105/2015/ doi:10.5194/tc-9-1105-2015 © Author(s) 2015. CC Attribution 3.0 License. Modelling glacier change in the Everest region, Nepal Himalaya J. M. Shea1, W. W. Immerzeel1,2, P. Wagnon1,3, C. Vincent4, and S. Bajracharya1 1International Centre for Integrated Mountain Development, Kathmandu, Nepal 2Department of Physical Geography, Utrecht University, Utrecht, the Netherlands 3IRD/UJF – Grenoble 1/CNRS/G-INP, LTHE UMR 5564, LGGE UMR 5183, Grenoble, 38402, France 4UJF – Grenoble 1/CNRS, Laboratoire de Glaciologie et Géophysique de l’Environnement (LGGE) UMR 5183, Grenoble, 38041, France Correspondence to: J. -
Peverest Base Camp Trek
Ultimate Island peak PeveRest Base Camp Trek A trekking & climbing experience that blows the mind! Your go to trekking experts for Nepal, Everest and all the adventures inbetween. What's inside? Why trek with EverTrek? 3 Route map 4 Trip overview 5 What’s included 6 Experience needed 7 Your itinerary 8 Equipment list 18 Extend your adventure 22 2 ultimate island peak & eveRest base camptrek 21 days Nepal Trip Duration - 21 Days Accommodation - 15 nights lodge, 2 nights tent, 3 nights hotel Tour Detail - 18 days trekking Max altitude - 6189m (20,305ft) IntroductioN High in the Khumbu region of Nepal, close to Mt Everest and closer still to the steep south face of Mt Lhotse, the aptly named Island Peak (6189m) rises above the glaciated valleys below. With its outrageous location and challenging summit ridge, this peak has been a favourite with our guides, leaders, and clients for a number of years. Ultimate Island Peak and Everest Base Camp Expedition is the ultimate experience in the Everest region for any one looking to attempt a Himalayan peak for the first time. You will not only climb Island Peak at 6189m (20,305ft) but also reach the historic Everest Base Camp (5364m) whilst also climbing 2 of the high passes of Cho La (5,420m) and Kongma La (5,535m) along with the sunrise hike to Kala Patthar (5,545m). One heck of an adventure! 3 clockwise route map of ultimate island peak and eveRest base camp 4 trip overview Trekking via Namche Bazaar we follow the route to Everest Base Camp via the Gokyo valley and Cho La Pass route and into Lobuche beside the Khumbuglacier.