And Its Subsequent Impacts in the Nepal, India and China
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The Call of the Siren: Bod, Baútisos, Baîtai, and Related Names (Studies in Historical Geography II)
The Call of the Siren: Bod, Baútisos, Baîtai, and Related Names (Studies in Historical Geography II) Bettina Zeisler (Universität Tübingen) 1. Introduction eographical or ethnical names, like ethnical identities, are like slippery fishes: one can hardly catch them, even less, pin them G down for ever. The ‘Germans’, for example, are called so only by English speakers. The name may have belonged to a tribe in Bel- gium, but was then applied by the Romans to various tribes of North- ern Europe.1 As a tribal or linguistic label, ‘German (ic)’ also applies to the English or to the Dutch, the latter bearing in English the same des- ignation that the Germans claim for themselves: ‘deutsch’. This by the way, may have meant nothing but ‘being part of the people’.2 The French call them ‘Allemands’, just because one of the many Germanic – and in that case, German – tribes, the Allemannen, settled in their neighbourhood. The French, on the other hand, are called so, because a Germanic and, in that case again, German tribe, the ‘Franken’ (origi- nally meaning the ‘avid’, ‘audacious’, later the ‘free’ people) moved into France, and became the ruling elite.3 The situation is similar or even worse in other parts of the world. Personal names may become ethnic names, as in the case of the Tuyu- hun. 4 Names of neighbouring tribes might be projected onto their overlords, as in the case of the Ḥaža, who were conquered by the Tuyuhun, the latter then being called Ḥaža by the Tibetans. Ethnic names may become geographical names, but then, place names may travel along with ethnic groups. -
VIII. Arbitrary Arrest and Detention
HUMAN RIGHTS UNDER CHINA’S SHADOW Mistreatment of Tibetans in Nepal WATCH Under China’s Shadow Mistreatment of Tibetans in Nepal Copyright © 2014 Human Rights Watch All rights reserved. Printed in the United States of America ISBN: 978-1-62313-1135 Cover design by Rafael Jimenez Human Rights Watch is dedicated to protecting the human rights of people around the world. We stand with victims and activists to prevent discrimination, to uphold political freedom, to protect people from inhumane conduct in wartime, and to bring offenders to justice. We investigate and expose human rights violations and hold abusers accountable. We challenge governments and those who hold power to end abusive practices and respect international human rights law. We enlist the public and the international community to support the cause of human rights for all. Human Rights Watch is an international organization with staff in more than 40 countries, and offices in Amsterdam, Beirut, Berlin, Brussels, Chicago, Geneva, Goma, Johannesburg, London, Los Angeles, Moscow, Nairobi, New York, Paris, San Francisco, Tokyo, Toronto, Tunis, Washington DC, and Zurich. For more information, please visit our website: http://www.hrw.org MARCH 2014 978-1-62313-1135 Under China’s Shadow Mistreatment of Tibetans in Nepal Map of Nepal .................................................................................................................... i Summary ......................................................................................................................... 1 -
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. -
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. -
Minshan Draft Factsheet 13Oct06.Indd
Gift to the Earth 103, 25 October 2006 Gift to the Earth China: Sichuan and Gansu Provinces join efforts to preserve the giant panda and its habitat in the Minshan Landscape SUMMARY The 2004 Panda Survey concluded that 1,600 giant pandas survive in the wild. The pandas are scattered in 20 isolated populations in six major landscapes in southwestern China in the upper Yangtze River basin. Almost half these pandas are found in the Minshan landscape, shared by Sichuan and Gansu provinces. In a major development, the provincial governments of Sichuan and Gansu have each committed to establish new protected areas (PAs), linking corridors and co-managed areas to ensure all the pandas in Minshan are both protected and reconnected to ensure their long term health and survival. This represents the designation of almost 1,6 million hectares of panda habitat. Both provincial governments have also committed to establish PAs for other wildlife totaling an additional 900,000 hectares by 2010. WWF considers the giant panda as a ‘flagship’ species – a charismatic animal representative of the biologically rich temperate forest it WWF, the global conservation organization, recognizes these inhabits which also mobilizes support for conservation of the commitments by the two provincial governments as a Gift to larger landscape and its inhabitants. By conserving the giant panda the Earth – symbolizing a globally significant conservation and its habitat, many other species will also be conserved – including achievement and inspiring environmental leadership. -
Beijing Essence Tour 【Tour Code:OBD4(Wed./Fri./Sun.) 、OBD5(Tues./Thur./Sun.)】
Beijing Essence Tour 【Tour Code:OBD4(Wed./Fri./Sun.) 、OBD5(Tues./Thur./Sun.)】 【OBD】Beijing Essence Tour Price List US $ per person Itinerary 1: Beijing 3N4D Tour Itinerary 2: Beijing 4N5D Tour Tour Fare Itinerary 1 3N4D Itinerary 2 4N5D O Level A Level B Level A Level B B OBD4A OBD4B OBD5A OBD5B D Valid Date WED/FRI WED/FRI/SUN TUE/THU TUE/THU/SUN 2011.3.1-2011.8.31 208 178 238 198 Beijing 2011.9.1-2011. 11.30 218 188 258 208 2011.12.1-2012. 2.29 188 168 218 188 Single Room Supp. 160 130 200 150 Tips 32 32 40 40 1) Price excludes tips. The tips are for tour guide, driver and bell boys in hotel. Children should pay as much as adults. 2) Specified items(self-financed): Remarks Beijing/Kung Fu Show (US $28/P); [Half price (no seat) for child below 1.0m; full price for child over 1.0m. Only one child without seat is allowed for two adults.] 3) Total Fare: tour fare + specified self-financed fee(US $28/P) The price is based on adults; the price for children can be found on Page 87 Detailed Start Dates (The Local Date in China) Date Every Tues. Every Wed. Every Thur. Every Fri. Every Sun. Month OBD5A/5B OBD4A/4B OBD5A/5B OBD4A/4B OBD4B/OBD5B 2011. 3. 01, 08, 15, 22, 29 02, 09, 16, 23, 30 03, 10, 17, 24, 31 04, 11, 18, 25 06, 13, 20, 27 2011. 4. 05, 12, 19, 26 06, 13, 20, 27 07, 14, 21, 28 01, 08, 15, 22, 29 03, 10, 17, 24 Tour Highlights Tour Code:OBD4A/B Wall】 of China. -
Effect of Modified Pomace on Copper Migration Via Riverbank Soil in Southwest China
Effect of modified pomace on copper migration via riverbank soil in southwest China Lingyuan Chen1,*, Touqeer Abbas2,*, Lin Yang1, Yao Xu1, Hongyan Deng1, Lei Hou3 and Wenbin Li1 1 College of Environmental Science and Engineering, China West Normal University, Nanchong, China 2 Zhejiang Provincial Key Laboratory of Agricultural Resources and Environment, Hangzhou, China 3 College of Resources & Environment, Tibet Agricultural and Animal Husbandry University, Nyingchi, China * These authors contributed equally to this work. ABSTRACT To explore the effects of modified pomace on copper migration via the soil on the banks of the rivers in northern Sichuan and Chongqing, fruit pomace (P) and ethylene diamine tetra-acetic acid (EDTA) modified P (EP) were evenly added (1% mass ratio) to the soil samples of Guanyuan, Nanbu, Jialing, and Hechuan from the Jialing River; Mianyang and Suining from the Fu River; and Guangan and Dazhou from the Qu River. The geochemical characteristics and migration rules of copper in different amended soils were simulated by column experiment. Results showed that the permeation time of copper in each soil column was categorized as EP-amended > P-amended > original soil, and the permeation time of amended soil samples at different locations was Jialing > Suining > Mianyang > Guangan > Dazhou > Nanbu > Guanyuan > Hechuan. Meanwhile, the average flow rate of copper in each soil column showed a reverse trend with the permeation time. Copper in exchangeable, carbonate, and iron–manganese oxide forms decreased with the increase of vertical depth in the soil column, among which the most evident decreases appeared in the carbonate-bonding form. The copper accumulation in different Submitted 8 October 2020 Accepted 1 July 2021 locations presented a trend of Jialing > Suining > Mianyang > Guangan > Dazhou > Published 27 July 2021 Nanbu > Guangyuan > Hechuan, and the copper content under the same soil showed Corresponding author EP-amended > P-amended > original soil. -
Damage from the April-May 2015 Gorkha Earthquake Sequence in the Solukhumbu District (Everest Region), Nepal David R
Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard To cite this version: David R. Lageson, Monique Fort, Roshan Raj Bhattarai, Mary Hubbard. Damage from the april-may 2015 gorkha earthquake sequence in the Solukhumbu district (Everest region), Nepal. GSA Annual Meeting, Sep 2016, Denver, United States. hal-01373311 HAL Id: hal-01373311 https://hal.archives-ouvertes.fr/hal-01373311 Submitted on 28 Sep 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. DAMAGE FROM THE APRIL-MAY 2015 GORKHA EARTHQUAKE SEQUENCE IN THE SOLUKHUMBU DISTRICT (EVEREST REGION), NEPAL LAGESON, David R.1, FORT, Monique2, BHATTARAI, Roshan Raj3 and HUBBARD, Mary1, (1)Department of Earth Sciences, Montana State University, 226 Traphagen Hall, Bozeman, MT 59717, (2)Department of Geography, Université Paris Diderot, 75205 Paris Cedex 13, Paris, France, (3)Department of Geology, Tribhuvan University, Tri-Chandra Campus, Kathmandu, Nepal, [email protected] ABSTRACT: Rapid assessments of landslides Valley profile convexity: Earthquake-triggered mass movements (past & recent): Traditional and new construction methods: Spectrum of structural damage: (including other mass movements of rock, snow and ice) as well as human impacts were conducted by many organizations immediately following the 25 April 2015 M7.8 Gorkha earthquake and its aftershock sequence. -
Geomorphic Processes, Rock Quality and Solid Waste Management—Examples from the Mt
Journal of Water Resource and Protection, 2015, 7, 1291-1308 Published Online November 2015 in SciRes. http://www.scirp.org/journal/jwarp http://dx.doi.org/10.4236/jwarp.2015.716105 Geomorphic Processes, Rock Quality and Solid Waste Management—Examples from the Mt. Everest Region of Nepal Eva Posch1,2, Rainer Bell2, Johannes Thomas Weidinger1,3, Thomas Glade2* 1Department of Geography and Geology, University of Salzburg, University of Salzburg, Salzburg, Austria 2Department of Geography, University of Vienna, Vienna, Austria 3ERKUDOK Institute, K-Hof Museums, Gmunden, Austria Received 10 August 2015; accepted 8 November 2015; published 11 November 2015 Copyright © 2015 by authors and Scientific Research Publishing Inc. This work is licensed under the Creative Commons Attribution International License (CC BY). http://creativecommons.org/licenses/by/4.0/ Abstract Sagarmatha National Park and Buffer Zone (SNPBZ) in the Everest region in Nepal is among the most popular destinations for trekking tourism in Nepal. The dramatic growth of the tourism in- dustry has increased pressures on the environment and the National Park is heavily affected by the rapidly growing waste issue. Besides, major mass movements play an important role in the Himalaya and have been observed in SNPBZ. Also, seasonal monsoon floods, debris flows, rock falls, landslides and the creation of glacial lake outburst floods are frequently occurring in the re- gion. This paper explores the reciprocal interactions between the geo-environment and solid waste management in Everest’s SNPBZ. Therefore, geological characteristics and geomorphologi- cal processes, especially the two large rockslides in Lukla and Khumjung, as well as their conse- quences for rock quality, climatic and hydrologic conditions, are analyzed and simultaneously connected to the rapidly growing tourism-induced waste issue. -
EVEREST BASE CAMP TREK ITINERARY Itinerary
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. -
Attribution of Growing Season Evapotranspiration Variability
1 Attribution of growing season evapotranspiration variability 2 considering snowmelt and vegetation changes in the arid alpine 3 basins 4 Tingting Ningabc, Zhi Lid, Qi Fengac* , Zongxing Liac and Yanyan Qinb 5 aKey Laboratory of Ecohydrology of Inland River Basin, Northwest Institute of Eco-Environment and Resources, 6 Chinese Academy of Sciences, Lanzhou, 730000, China 7 bKey Laboratory of Land Surface Process and Climate Change in Cold and Arid Regions, Chinese Academy of 8 Sciences, Lanzhou 730000, China 9 cQilian Mountains Eco-environment Research Center in Gansu Province, Lanzhou, 730000, China 10 dCollege of Natural Resources and Environment, Northwest A&F University, Yangling, Shaanxi, 712100, China 11 * Correspondence to: Qi Feng ([email protected] ) 12 1 / 50 13 Abstract: Previous studies have successfully applied variance decomposition 14 frameworks based on the Budyko equations to determine the relative contribution of 15 variability in precipitation, potential evapotranspiration (E0), and total water storage 2 16 changes (∆S) to evapotranspiration variance (휎퐸푇) on different time-scales; however, 17 the effects of snowmelt (Qm) and vegetation (M) changes have not been incorporated 18 into this framework in snow-dependent basins. Taking the arid alpine basins in the 19 Qilian Mountains in northwest China as the study area, we extended the Budyko 2 20 framework to decompose the growing season 휎퐸푇 into the temporal variance and 21 covariance of rainfall (R), E0, ∆S, Qm, and M. The results indicate that the incorporation 22 of Qm could improve the performance of the Budyko framework on a monthly scale; 2 23 휎퐸푇 was primarily controlled by the R variance with a mean contribution of 63%, 24 followed by the coupled R and M (24.3%) and then the coupled R and E0 (14.1%). -
Characteristics and Changes of Streamflow on The
Journal of Hydrology: Regional Studies 2 (2014) 49–68 Contents lists available at ScienceDirect Journal of Hydrology: Regional Studies j ournal homepage: www.elsevier.com/locate/ejrh Review Characteristics and changes of streamflow on the Tibetan Plateau: A review a,∗ b a a Lan Cuo , Yongxin Zhang , Fuxin Zhu , Liqiao Liang a Key Laboratory of Tibetan Environmental Changes and Land Surface Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, China b Research Applications Laboratory, National Center for Atmospheric Research, Boulder, CO, USA a r t i c l e i n f o a b s t r a c t Article history: Study region: The Tibetan Plateau (TP). Received 5 June 2014 Study focus: The TP exerts great influence on regional and global Received in revised form 7 August 2014 climate through thermal and mechanical forcings. The TP is also Accepted 13 August 2014 the headwater of large Asian rivers that provide water for billions of people and numerous ecosystems. Understanding the character- Keywords: istics and changes of streamflow on the TP will help manage water Streamflow resources under changing environment. Three categories of rivers River basins (the Pacific Ocean, the Indian Ocean, and the interior) on the TP Tibetan Plateau were examined for their seasonal and long term change patterns. Climate change Outstanding research issues were also identified. Human activity New hydrological insights for the region: Streamflow follows the monthly patterns of precipitation and temperature in that all peak in May–September. Streamflow changes are affected by climate change and human activities depending on the basins.