Everest Base Camp, Gokyo Lakes & the Cho La
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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 -
An Overview of Tourism Diversity in Nepal
Patan Pragya (Volume: 6, Number: 1 2020) Received Date: Jan. 2020 Revised: April 2020 Accepted: June 2020 An Overview of Tourism Diversity in Nepal Minesh Kumar Ghimire Abstract Tourism is the most important service industry of Nepal. It provided big opportunities of national development and income to maintain international harmony. It will argue the more descriptive nature of information. The diversity of tourism has a huge benefit of tourism development. The tourism activities in Nepal are different attractions such as adventure, natural, cultural etc. The Airway is means of Tourist Arrival means of Nepal and Average Length of Stay is 12 days. Key Words: Tourism activities, Tourism Opportunities, diversity, Eco-tourism. Background Tourism is one of the important factors in the economic sector of Nepal. It doesn’t just create employment opportunities but attracts many international tourists which bring in foreign currency. In this regard, to have more international tourist means to be in more foreign currency and as the exchange rate varies, the foreign currency can be a boon for the economic progress of the country. People working in the tourism industry are the direct beneficiary but the people working in agriculture, airlines, hospital, hotels are the indirect beneficiary. The products from the indirect beneficiary can be promoted via tourism and get to the international market as well. It helps people to understand each other and respect each other which helps to maintain harmony in the country and around the world. Various relevant policy documents, proceedings of various seminars, study reports and such other documents can be reviewed for extracting secondary information of tourism and how tourism has been influential in the life of people who are dependent on it. -
Khangchendzonga National Park
ASIA / PACIFIC KHANGCHENDZONGA NATIONAL PARK INDIA Sacred site in the Khangchendzonga National Park - © IUCN Tilman Jaeger India - Khangchendzonga National Park WORLD HERITAGE NOMINATION – IUCN TECHNICAL EVALUATION KHANGCHENDZONGA NATIONAL PARK (INDIA) – ID 1513 IUCN RECOMMENDATION TO WORLD HERITAGE COMMITTEE: To inscribe the property under natural criteria. Key paragraphs of Operational Guidelines: Paragraph 77: Nominated property meets World Heritage criteria. Paragraph 78: Nominated property meets integrity and protection and management requirements. 1. DOCUMENTATION Kangchenjunga Transboundary Conservation and Development Initiative in the Hindu Kush Himalayas. a) Date nomination received by IUCN: 16 March Prepared for TBPA. Krishna AP, Chhetri S, Singh KK 2015 (2002) Human Dimensions of Conservation in the Khangchendzonga Biosphere Reserve: The Need for b) Additional information officially requested from Conflict Prevention. Mountain Research and and provided by the State Party: Khangchendzonga Development 22(4):328-331. Lachungpa U (2009) National Park is nominated as a mixed site. ICOMOS Indigenous Lifstyles and Biodiversity Conservation wrote to the State Party in September, 2015 Issues in North Sikkim. Indian Journal of Traditional requesting supplementary information on a range of Knowledge 8(1): 51-55. Oli KP, Chaudhary S, Sharma issues related to the evaluation of cultural values. A UR (2013) Are Governance and Management Effective joint IUCN / ICOMOS progress report was then sent on within Protected Areas of the Kanchenjunga 17 December 2015 following the respective ICOMOS Landscape (Bhutan, India And Nepal)? PARKS 19(1): and IUCN Panel meetings. Requests were made of the 25-36. Sathyakumar S, Bashir T, Bhattacharya T, State Party to update the biodiversity inventory for Poudyal K (2011b) Mammals of the Khangchendzonga species within the property; consider changes to the Biosphere Reserve, Sikkim, India. -
National Parks and Iccas in the High Himalayan Region of Nepal: Challenges and Opportunities
[Downloaded free from http://www.conservationandsociety.org on Tuesday, June 11, 2013, IP: 129.79.203.216] || Click here to download free Android application for this journal Conservation and Society 11(1): 29-45, 2013 Special Section: Article National Parks and ICCAs in the High Himalayan Region of Nepal: Challenges and Opportunities Stan Stevens Department of Geosciences, University of Massachusetts Amherst, Amherst, MA, USA E-mail: [email protected] Abstract In Nepal, as in many states worldwide, national parks and other protected areas have often been established in the customary territories of indigenous peoples by superimposing state-declared and governed protected areas on pre-existing systems of land use and management which are now internationally considered to be Indigenous Peoples’ and Community Conserved Territories and Areas (ICCAs, also referred to Community Conserved Areas, CCAs). State intervention often ignores or suppresses ICCAs, inadvertently or deliberately undermining and destroying them along with other aspects of indigenous peoples’ cultures, livelihoods, self-governance, and self-determination. Nepal’s high Himalayan national parks, however, provide examples of how some indigenous peoples such as the Sharwa (Sherpa) of Sagarmatha (Mount Everest/Chomolungma) National Park (SNP) have continued to maintain customary ICCAs and even to develop new ones despite lack of state recognition, respect, and coordination. The survival of these ICCAs offers Nepal an opportunity to reform existing laws, policies, and practices, both to honour UN-recognised human and indigenous rights that support ICCAs and to meet International Union for Conservation of Nature (IUCN) and Convention on Biological Diversity (CBD) standards and guidelines for ICCA recognition and for the governance and management of protected areas established in indigenous peoples’ territories. -
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. -
Thermal and Physical Investigations Into Lake Deepening Processes on Spillway Lake, Ngozumpa Glacier, Nepal
water Article Thermal and Physical Investigations into Lake Deepening Processes on Spillway Lake, Ngozumpa Glacier, Nepal Ulyana Nadia Horodyskyj Science in the Wild, 40 S 35th St. Boulder, CO 80305, USA; [email protected] Academic Editors: Daene C. McKinney and Alton C. Byers Received: 15 March 2017; Accepted: 15 May 2017; Published: 22 May 2017 Abstract: This paper investigates physical processes in the four sub-basins of Ngozumpa glacier’s terminal Spillway Lake for the period 2012–2014 in order to characterize lake deepening and mass transfer processes. Quantifying the growth and deepening of this terminal lake is important given its close vicinity to Sherpa villages down-valley. To this end, the following are examined: annual, daily and hourly temperature variations in the water column, vertical turbidity variations and water level changes and map lake floor sediment properties and lake floor structure using open water side-scan sonar transects. Roughness and hardness maps from sonar returns reveal lake floor substrates ranging from mud, to rocky debris and, in places, bare ice. Heat conduction equations using annual lake bottom temperatures and sediment properties are used to calculate bottom ice melt rates (lake floor deepening) for 0.01 to 1-m debris thicknesses. In areas of rapid deepening, where low mean bottom temperatures prevail, thin debris cover or bare ice is present. This finding is consistent with previously reported localized regions of lake deepening and is useful in predicting future deepening. Keywords: glacier; lake; flood; melting; Nepal; Himalaya; Sherpas 1. Introduction Since the 1950s, many debris-covered glaciers in the Nepalese Himalaya have developed large terminal moraine-dammed supraglacial lakes [1], which grow through expansion and deepening on the surface of a glacier [2–4]. -
Buddha Air Flight Schedule Kathmandu to Pokhara
Buddha Air Flight Schedule Kathmandu To Pokhara MohamedArchie oscillated hawses her accumulatively Pascale please, and unhomely downrange, and she Drusian. unsheathed Waniest her Lawson dog's-tongue spawns rescind lordly. just-in-time.Unbaptised It comes to finalise the incident site to buddha airlines without it holds diversity of water has witnessed growth Chakra Bahadur Buda, Tibet, Nepal offers a number of domestic. The Nepalese Diplomatic Missions were opened in fifteen different countries and nineteen different countries opened their Embassies in Nepal. Find out a sculptor and prepare details about the sculpture. If I want to change the date before arrival? Hindutva was never the part of popular imagination. Depending on your choice of transportation, wings, pristine blue and green waters of the Gokyo Lakes are one. Interested in seeing when your aircraft is powered on and watching it taxi on a live surface map? Menace was oozing out of his bloodshot eyes. The hotel offers guests a range of services and amenities designed to provide comfort and convenience. The banned list of the air flight schedule to buddha kathmandu pokhara? Some of my Indian friends might be thinking India has existed since the Maurya Empire or some might be wondering Indian subcontinent as India. Japan is one of the important trading partners of Nepal. Segment snippet included twice. Located in the fastest way to buddha air flight schedule to serve the cargo can not be customized based on navigation and salyan district of foreign direct flights with buddha air tickets. Different ceremonies are performed on the different ghats from Varanasi from daily ablutions, Nepalgunj, the country in the heart of the Himalayas came to be known as Nepal. -
Sagarmatha National Park Nepal
SAGARMATHA NATIONAL PARK NEPAL This majestically scenic mountain park of snow-covered peaks, gorges and glaciers dominated by the highest mountain on Earth is geologically interesting and its wilderness values are outstanding. The Dudh Kosi valley is home to the unique culture of the Sherpas and is an ecological unit of biological, socio-economic and religious importance. Rare animals such as snow leopard and red panda live in the Park. However, degradation from the increasing pressures of tourism and mountaineering is of growing concern. COUNTRY Nepal NAME Sagarmatha National Park STATEMENT OF OUTSTANDING UNIVERSAL VALUE [pending] NATURAL WORLD HERITAGE SITE 1979: Inscribed on the World Heritage List under Natural Criterion vii. INTERNATIONAL DESIGNATION 2007: Gokyo and Associated Lakes designated a Wetland of International Importance under the Ramsar Convention (7,770 ha). IUCN MANAGEMENT CATEGORY II National Park BIOGEOGRAPHICAL PROVINCE Himalayan Highlands (2.38.12) GEOGRAPHICAL LOCATION In the Himalayan Mountains on the border with the Tibetan Autonomous Region of China in the upper catchment of the Dudh Kosi river 140 km east of Kathmandu, centred on 27o57’55”N by 86o54’47”E. DATES AND HISTORY OF ESTABLISHMENT 1976: Created a National Park; 2002: Buffer zone added (27,500 ha); 2007: Gokyo lakes designated a Ramsar site. LAND TENURE State. Many of the resident Sherpas have legal title to houses, agricultural land and summer grazing lands (Jefferies, 1984). The Park is administered by the Sagarmarha National Park Authority of the Department of National Parks & Wildlife Conservation (DNPWC). 1 AREA 114,800 ha. The Park adjoins Makalu-Barun National Park and Conservation Area (233,000ha) in Nepal and Qomolangma Biosphere Reserve in the Tibetan Autonomous Region of China (1,823,591ha). -
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. -
Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal
HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies Volume 17 Number 2 Himalayan Research Bulletin: Article 16 Solukhumbu and the Sherpa 1997 Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers Follow this and additional works at: https://digitalcommons.macalester.edu/himalaya Recommended Citation Byers, Alton C.. 1997. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal. HIMALAYA 17(2). Available at: https://digitalcommons.macalester.edu/himalaya/vol17/iss2/16 This Research Article is brought to you for free and open access by the DigitalCommons@Macalester College at DigitalCommons@Macalester College. It has been accepted for inclusion in HIMALAYA, the Journal of the Association for Nepal and Himalayan Studies by an authorized administrator of DigitalCommons@Macalester College. For more information, please contact [email protected]. Landscape Change in Sagarmatha (Mt. Everest) National Park, Khumbu, Nepal Alton C. Byers The Mountain Institute This study uses repeat photography as the primary Introduction research tool to analyze processes of physical and Repeat photography, or precise replication and cultural landscape change in the Khumbu (M!. Everest) interpretation of historic landscape scenes, is an region over a 40-year period (1955-1995). The study is analytical tool capable of broadly clarifying the patterns a continuation of an on-going project begun by Byers in and possible causes of contemporary landscapellanduse 1984 that involves replication of photographs originally changes within a given region (see: Byers 1987a1996; taken between 1955-62 from the same five photo 1997). As a research tool, it has enjoyed some utility points. The 1995 investigation reported here provided in the United States during the past thirty years (see: the opportunity to expand the photographic data base Byers 1987b; Walker 1968; Heady and Zinke 1978; from five to 26 photo points between Lukla (2,743 m) Gruell 1980; Vale, 1982; Rogers et al. -
Serving Amazing Adventure… Since 1999
Serving Amazing Adventure… Since 1999 Nepal | Bhutan | Tibet | India www.hikingadventuretreks.com Table of Contents Welcome message 3 Why Travel with us? 4 Meet Our Team 5 Giving back to the community 6 Nepal Travel Information – planning your trip 7 EVEREST REGION 8-11 Everest Base Camp Trek 8 Gokyo Valley Everest Base Camp Trek 9 Everest View Trek/ Sherpa Village Trek 10 Everest Base Camp Heli sightseeing Tour 11 ANNAPURNA REGION Annapurn Base Camp Trek 12 Annapurna Circuit Trek 13 Poonhill/ Annapurna View Trek 14 MUSTANG REGION 15-17 Upper Mustang Trek 15 Manaslu Larke Pass Trek 16 Dolpo Trek 17 Langtang Valley Trek 18 CULTURE AND WILDLIFE 19-21 Cultural Tour and Wildlife Tour 19 Glance of Nepal 20 Kathmandu Valley Cultural Tour 21 River Adventure Nepal 22 Himalayan Foothill Cycling 23 Bhutan 24 Bhutan Cultural Tour 25 Druk Path Trek 26 Tibet 27 Everest Base Camp Tour Khasa Kathmandu 28 Lhasa Sightseeing Tour 29 Lake and Overland tour Tibet 30 Incrediable Indai 31 Dharmashal Trek 32 Reviews 33-34 Welcome Message: Mr. Ram Barakoti (Team Leader/Founder) Dear Clients & Travel Partners around the World, Namaste! Hiking Adventure Trekking Pvt Ltd is a well-known name in the Nepalese Travel and Tourism Industry. Along with its expertise in mountaineering sector in Nepal, India, Bhutan and Tibet. Together, we cater unforgettable mountaineering, trekking, hiking, rafting, and other exhilarating experiences for our valuable clients. We have been successfully conducting adventure treks, mountain expeditions and tours in Nepal, Bhutan, Tibet and India. We often serve repetitive/happy customers, who come back with their new friends and family members to relive the joys. -
Mount Everest Base Camp and Gokyo Lakes Langtang Ri Trekking & Expedition
Mount Everest Base Camp and Gokyo Lakes Langtang Ri Trekking & Expedition Mount Everest Base Camp and Gokyo Lakes This trek explores the breath-taking Gokyo valley which is located adjacent of the Khumbu. Gokyo is a land of high altitude lakes and icy glaciers. Here, a hike to the high vantage point of Gokyo Ri (5350-m) will reward you with views of four of the eight highest mountains on earth – all in one panorama! From here, one can see more of Everest (8848-m) and the three other Himalayan giants – Cho Oyu (8153-m), Lhotse(8501-m) and Makalu (8463-m) and some of the great Glaciers, mainly the Ngozumpa Glacier. The small herding settlement of Gokyo (4750m) lies on the banks of the third lake in a series of small turquoise mountain lakes and on the ridge above Gokyo, the four peaks above 8000m of Cho You, Everest, Lhotse and Makalu expose themselves. In addition to this you can have a look at the tremendous ice ridge between ChoYou and Gyachung (7922m), considered one of the most dramatic panoramas in the Khumbu region. There are many options for additional exploration and high-altitude walking, including the crossing of Cho La, a 5420m-high pass into Khumbu and a hike to Gokyo Ri. Your return trek will depart from the standard Gokyo trek as you will take the route back to Namche by crossing the Renjo La pass (5340m) instead of back trekking the Gokyo valley trails. This makes the trek a much more exciting and challenging one. These mountains are magical – and so are your encounters with the Sherpa people, the famous mountain dwellers of this Himalayan wonderland.