DOCSLIB.ORG

STEFAN LOOSE TRAVEL HANDBÜCHER N TIBET 0 300 Km

Total Page：16

File Type：pdf, Size：1020Kb

Download full-text PDF Read full-text
STEFAN LOOSE TRAVEL HANDBÜCHER N TIBET 0 300 Km 54 Karten und Pläne I Stopover-Ziele in China l Highlights I Reiserouten fair und grün reisen l Budget-Tipps TIBET STEFAN LOOSE TRAVEL HANDBÜCHER N TIBET 0 300 km Ruoqiang 11 Tsaparang XINJIANG Eindrucksvolles Zeugnis des alten 13 Riwoche Tsuglagkhang Guge-Königreichs S. 291 1 Jokhang in Lhasa Außergewöhnliches, festungsähnliches Der bedeutendste Pilgertempel Kloster im alten Kham S. 314 T Tibets S. 151 a k l Quiemo Ganden QINGHAI Hotan a m 3 a k a e Grandioses Gelugpa-Kloster hoch n - W ü s t 2 Potala-Palast in Lhasa über dem Kyi-Chu-Tal S. 191 Der prachtvolle Winterpalast 10 KailashYutian des Dalai Lama S. 156 Delingha Der heiligste aller heiligen Ulan Berge S. 279 Golmud Nam Tso 4 K Der höchstgelegene Salzsee u n l u n - der Welt S. 201 K e t t e AKSAI M t . K u k u 4772 s h i r i Khunu La CHIN 8 Tashilhunpo in Shigatse Chumarhe 12 Basum Tso (Draksum Tso) Das größte aktive Kloster Alpiner See inmitten grüner n Tibets S. 247 Fung´go La Wälder S. 304 a 5010 h Ch B um a S a y rh a e n n k l u Marchudram Babtshug a u n D r a K a n Gyelje Podrang - K Pangong Changtang g l e t Tso a Tomä t e ( T a Jekundo Rutok ALI Qinghai-Tibet- n g g In d u u Gomo Plateau l a Sershül s Dorsedong S h Gar/Ali/ Tso a n SICHUAN Shiquanhe 5206 Tanggula-Pass ) Jinsha Jiang Tsaka G TIBET (Yangzi) j Oma Sharda e Gegye/ l a t Gertse/Luma Ringbo NAGCHU u Napuk Amdo S n Namru g Tso Nyanrong Dege/Derge Tongtso Ngochu Nak Bachen/Drachen Tsarang d Sog Gyamda Tsada/Tholing i Ngangla Nyima Serling Tso Tsaparang s Bangoin Driru/Biru Tengchen e Ringtsho Chamdo Montser (Palgon) - Nagchu Riwoche Gonjo (Akar) Mt. Kailash K 6714 Tsochen Dangra N Palbar/Tsokha Barga e Kering y a CHAMDO t Taro Tso Yutso n Yendum/Traya La-nga Tso Hor/Horchu t Tso c h Lhorong/Zito Joshimath e Shantsa e n Yichen Ngom Chu MaphamYutso Tashi Targo Nam Tso) l h a - (Mekong) 7816 n g T h 7728 (Manasarovar-See) ( Namtso T h a Atsa/Lhari a n Chamoli Nanda Devi T n - Damshung g l h a Purang Gurla Mandhata r h e H a n c Reting Zogang/ n y a Draksum Tso Pome Darchula i s N NYINGCHI NagWamda Chu h Yangpachen Lhundrub Meldro m - in Bau - Markam/ i m Gungkar Kongpo Bayi Ra-ok a a SHIGATSE Tsurphu Gartok Pithoragarh l Drongpa/ l a Namling Ganden Gyamda Nyangtri (Salween) Zhongba Saga/ j a u a Raga Tsangp ) LHASA h a) (Nyingchi) Dadeldhura li Kyakyaru o C Lhasa tr Champawat a j Tadruka yi Sangri Y apu rn Riwoche Ngamring K Samye arl hm a a ung T po (Bra K Ya sang Mustang rlun Lhatse Shigatse Gongkar Tsethang Mahendranagar NEPAL Kyirong/ g Tsangpo (Brahmaputra) Nakartse Yamdok Zayul/Kyigang Dzongka Palku Shekar Sakya Gyantse Yumtso Nang Bareilly Annapurna (New Tingri) 9DhengadhiMount Everest Dhaulagiri 8091 Tso 6 Yumbulhakhang bei Tsethang 8167 LOKHA /SHANNAN Trekking zum Basislager des höchsten Khangmar Die originalgetreu wiederaufgebaute Bergs der Welt Pokhara S. 262 Nyalam Gyalkar Tsona/ Luntse/Kyitang Pasinghat Zholshar Tempelburg der Yarlung-Könige S. 226 Mt. Everest Gampa a Shahjahanpur j ra Zhangmu a ut Tezu G Butwal 8848 Jomolhari l ap an H i m a g Sitapur Kathmandu SIKKIM hm a 7314 INDIENra (G Jiri BHUTAN B an Kumbum Chörten in Gyantse Paro Dibrugarh g 7 Bhaktapur e INDIEN s Dromo/ ) Der symbolische Erlösungsweg Thimpu 5 Samye Lucknow Hetauda Yadong MYANMAR bis ins NirvanaDarjeeling S. 238 Das älteste Kloster des Landes S. 214 Kanpur Gorakhpur (BIRMA) Shiliguri Tezpur Jorhat 3., vollständig überarbeitete Auflage Reiseziele und Routen Traveltipps von A bis Z Land und Leute Lhasa und Umgebung Lhoka Shigatse Westtibet (Ngari) Osttibet (Kham) Stippvisiten in Chinas Metropolen Oliver Fülling Anhang TIBET STEFAN LOOSE TRAVEL HANDBÜCHER 2 1 TIBE DIE HIG HL IG T HTS © MAURITIUS IMAGES / ALAMY © PICTURE ALLIANCE / MAXPPP TPG © CORBIS / PURBU ZHAXI / XINHUA PRESS 1 tibetischen JOKH A NG INLH B uddhismus. S.151 A S A Tibets Nationalheiligtum unddaspulsierendeZentrumdes Tibets Die Highlights DIE HIG HL IG HTS 1 1 3 2 POTALA-PALAST IN LHASA Im gewaltigen Winterpalast des Dalai Lama manifestiert sich 2 der Höhepunkt tibetischer Baukunst. S. 156 4 DIE HIGHLIGHTS DIE HIG HL IG HTS 5 © PICTURE ALLIANCE / MARTIN RUETSCHI G N I 3 LL IVER FÜ L © O KLOSTER GANDEN 3 Das Gründungskloster der Gelugpa thront auf einem Berg in 4300 m Höhe. Auf der Kora, dem heiligen Umwandlungsweg um Ganden, bieten sich spektakuläre Aussichten über das Kyi-Chu-Tal. S. 191 NAM TSO Wie ein Ozean 4 breitet sich der paradiesisch gelegene See aus. Eingebettet in eine Bergwelt aus Sechs- und Siebentausendern gehört er zu den heiligsten Seen Tibets. S. 201 I NSK Y D DY SZTOF Y Z / KR S GE MA Y I 3 TT © GE 6 DIE HIGHLIGHTS © CORBIS / MICHELE FALZONE DIE HIG HL IG HTS 4 7 MAN 5 KLOSTER SAMYE Das älteste FREE L E 5 Kloster Tibets ist ein Symbol CHA für den Aufbau des Universums. / MI S Hier fand das Konzil von Samye statt, RBI CO auf dem sich die indische Tantra- © schule als buddhistische Richtung in Tibet durchsetzte. S. 214 YUMBULHAKHANG 6 Die Tempelburg der Yarlung- Könige hoch über dem Tal der Yarlung Chu ist das älteste Bauwerk Tibets und ein beliebter Ort, um Glücksbringer zu verstreuen. S. 226 G N I LL IVER FÜ 5 L © O 8 DIE HIGHLIGHTS © OLIVER FÜLLING DIE HIG HL IG HTS 6 9 UTH 7 A fan E T / S S GE MA I US I T RI MAU © KUMBUM CHÖRTEN IN GYANTSE Bei der Begehung dieses dreidimensionalen Mandalas 7 durchläuft man symbolisch den buddhistischen Erlösungsweg bis ins Nirvana. S. 238 10 DIE HIGHLIGHTS © MAURITIUS IMAGES / MANFRED BAIL 8 (Chamkhang Chenmo)eineriesigeSkulptur desZukunftsbuddhasMaitreya.S.247 Ta SHI L HUN P O Der SitzdesPanchenLamainShigatse birgtinderMaitreya-Halle DIE HIG HL IG HTS 8 11 12 9 DIE HIG HL IG HTS © MAURITIUS IMAGES / PETER GIOVANNINI HT 10 WRIG SON I L / A S GE MA Y I TT © GE MOUNT EVEREST Auch wenn 9 man den höchsten Berg der Welt nicht bezwingen möchte, lohnt sich die Anfahrt zum Mount Everest Base Camp durch die faszinierenden Landschaften des Qomolangma- Nationalparks. S. 262 KAILASH Die Umrundung 10 des Kailash, des wichtigsten Pilgerziels für tibetische Buddhisten, Bönpa, Hindus und Jainas, gehört zu den eindrucksvollsten und nach- haltigsten Erlebnissen einer Reise nach Westtibet. S. 279 OUNOT G L E CH / MI RER PLO EX / F I LA 10 © DIE HIGHLIGHTS 13.
Load more

Recommended publications
  • China Shaping Tibet for Strategic Leverage
    MANEKSHAW PAPER No. 70, 2018 China Shaping Tibet for Strategic Leverage Praggya Surana D W LAN ARFA OR RE F S E T R U T D N IE E S C CLAWS VI CT N OR ISIO Y THROUGH V KNOWLEDGE WORLD Centre for Land Warfare Studies KW Publishers Pvt Ltd New Delhi New Delhi Editorial Team Editor-in-Chief : Lt Gen Balraj Nagal ISSN 23939729 D W LAN ARFA OR RE F S E T R U T D N IE E S C CLAWS VI CT N OR ISIO Y THROUGH V Centre for Land Warfare Studies RPSO Complex, Parade Road, Delhi Cantt, New Delhi 110010 Phone: +91.11.25691308 Fax: +91.11.25692347 email: [email protected] website: www.claws.in CLAWS Army No. 33098 The Centre for Land Warfare Studies (CLAWS), New Delhi, is an autonomous think-tank dealing with national security and conceptual aspects of land warfare, including conventional and sub-conventional conflicts and terrorism. CLAWS conducts research that is futuristic in outlook and policy-oriented in approach. © 2018, Centre for Land Warfare Studies (CLAWS), New Delhi Disclaimer: The contents of this paper are based on the analysis of materials accessed from open sources and are the personal views of the author. The contents, therefore, may not be quoted or cited as representing the views or policy of the Government of India, or Integrated Headquarters of the Ministry of Defence (MoD) (Army), or the Centre for Land Warfare Studies. KNOWLEDGE WORLD www.kwpub.com Published in India by Kalpana Shukla KW Publishers Pvt Ltd 4676/21, First Floor, Ansari Road, Daryaganj, New Delhi 110002 Phone: +91 11 23263498 / 43528107 email: [email protected] l www.kwpub.com Contents Introduction 1 1.
    [Show full text]
  • The Design of the Ali CMB Polarization Telescope Receiver
    The design of the Ali CMB Polarization Telescope receiver M. Salatinoa,b, J.E. Austermannc, K.L. Thompsona,b, P.A.R. Aded, X. Baia,b, J.A. Beallc, D.T. Beckerc, Y. Caie, Z. Changf, D. Cheng, P. Chenh, J. Connorsc,i, J. Delabrouillej,k,e, B. Doberc, S.M. Duffc, G. Gaof, S. Ghoshe, R.C. Givhana,b, G.C. Hiltonc, B. Hul, J. Hubmayrc, E.D. Karpela,b, C.-L. Kuoa,b, H. Lif, M. Lie, S.-Y. Lif, X. Lif, Y. Lif, M. Linkc, H. Liuf,m, L. Liug, Y. Liuf, F. Luf, X. Luf, T. Lukasc, J.A.B. Matesc, J. Mathewsonn, P. Mauskopfn, J. Meinken, J.A. Montana-Lopeza,b, J. Mooren, J. Shif, A.K. Sinclairn, R. Stephensonn, W. Sunh, Y.-H. Tsengh, C. Tuckerd, J.N. Ullomc, L.R. Valec, J. van Lanenc, M.R. Vissersc, S. Walkerc,i, B. Wange, G. Wangf, J. Wango, E. Weeksn, D. Wuf, Y.-H. Wua,b, J. Xial, H. Xuf, J. Yaoo, Y. Yaog, K.W. Yoona,b, B. Yueg, H. Zhaif, A. Zhangf, Laiyu Zhangf, Le Zhango,p, P. Zhango, T. Zhangf, Xinmin Zhangf, Yifei Zhangf, Yongjie Zhangf, G.-B. Zhaog, and W. Zhaoe aStanford University, Stanford, CA 94305, USA bKavli Institute for Particle Astrophysics and Cosmology, Stanford, CA 94305, USA cNational Institute of Standards and Technology, Boulder, CO 80305, USA dCardiff University, Cardiff CF24 3AA, United Kingdom eUniversity of Science and Technology of China, Hefei 230026 fInstitute of High Energy Physics, Chinese Academy of Sciences, Beijing 100049 gNational Astronomical Observatories, Chinese Academy of Sciences, Beijing 100012 hNational Taiwan University, Taipei 10617 iUniversity of Colorado Boulder, Boulder, CO 80309, USA jIN2P3, CNRS, Laboratoire APC, Universit´ede Paris, 75013 Paris, France kIRFU, CEA, Universit´eParis-Saclay, 91191 Gif-sur-Yvette, France lBeijing Normal University, Beijing 100875 mAnhui University, Hefei 230039 nArizona State University, Tempe, AZ 85004, USA oShanghai Jiao Tong University, Shanghai 200240 pSun Yat-Sen University, Zhuhai 519082 ABSTRACT Ali CMB Polarization Telescope (AliCPT-1) is the first CMB degree-scale polarimeter to be deployed on the Tibetan plateau at 5,250 m above sea level.
    [Show full text]
  • Twenty Million Years of Continuous Deformation Along Thekarakorum Fault, Western Tibet: a Thermochronological Analysis
    Twenty million years of continuous deformation along theKarakorum fault, western Tibet: A thermochronological analysis. Franck Valli, Nicolas Arnaud, Philippe-Hervé Leloup, Edward Sobel, Gweltaz Mahéo, R. Lacassin, Stéphane Guillot, Haibing Li, Paul Tapponnier, Xu Zhiquin To cite this version: Franck Valli, Nicolas Arnaud, Philippe-Hervé Leloup, Edward Sobel, Gweltaz Mahéo, et al.. Twenty million years of continuous deformation along theKarakorum fault, western Tibet: A ther- mochronological analysis.. Tectonics, American Geophysical Union (AGU), 2007, 26, pp.TC4004. 10.1029/2005TC001913. hal-00197561 HAL Id: hal-00197561 https://hal.archives-ouvertes.fr/hal-00197561 Submitted on 17 Dec 2007 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. 20 million years of continuous deformation along the Karakorum fault, Western Tibet: a thermochronological analysis Franck Valli (1), Nicolas Arnaud (2), Philippe Hervé Leloup (3), Edward R. Sobel (4) Gweltaz Mahéo, (3) Robin Lacassin (1) Stéphane Guillot (5), Haibing Li (6-1) Paul Tapponnier (1), Zhiqin Xu (6) (1) UMR7578-CNRS Institut de Physique du Globe de Paris, 75252, Paris, France, (2) Géosciences Montpellier, Université de Montpellier 2, CNRS UMR5243, 34095, Montpellier, France, (3) UMR5570-CNRS Univ. Claude Bernard, 69622, Villeurbanne, France, (4) Univ.
    [Show full text]
  • The Mystery of the Kailash Trail
    The Mystery of the Kailash Trail Chapter 1 Bharat Bhushan The Mystery of the Kailash Trail Chapter 1 Bharat Bhushan Pre-publication draft manuscript This is not a publication This draft copy is being distributed to invite comments and suggestions Not for sale or distribution Being uploaded or distributed for guidance and suggestions in developing the story All rights reserved. No part of this book may be reproduced or utilised in any form or by any means, electronics or mechanical including photocopying, recording or by any information storage and retrieval system, without permission in writing from the publishers. This is not a publication. This is a pre-publication draft manuscript of a proposed book and is being distributed for editing, comments, critics and suggestions. The distribution is within a limited group of experts, resource persons, people who are familiar with the Kailash region in Tibet, the aspects of the pilgrimage in the various religions and those who are interested in the aspects of development of a story. Those who receive this pre-publication draft manuscript may forward it those who may be able to contribute to the editing and development of the story. There will be errors, mistakes and contextual wrongs galore. Please do not hesitate to point them out and inform the author at [email protected] About the book The oldest mystery known to the Oriental World. It is said that nobody dares to venture out to walk on the Kailash Mountain. And it is also said that those who walked up the mountain, never returned. In all these centuries, they have gone within, never to return.
    [Show full text]
  • AUGUST 2020 Health Code App for Foreigners
    CHINESE CHURCH SUPPORT MINISTRIES CHINA PRAYER LETTER AUGUST 2020 Health Code App for Foreigners Even though a normalcy has returned to most aspects of life in China after COVID-19, some residues of the pandemic’s safety checks and controls remain in place and it seems people accept them as being here to stay. For those that want to access public transport, hotels, shops, restaurants, supermarkets, residential compounds or other public In locations, there are mandatory requirements this to check temperatures and use health apps, or scan QR codes to prove travel history. issue Many locations are also increasingly requiring Health Code App use of ‘health kit code’ apps to demonstrate a for Foreigners person's health condition and travel history. Ngari Prefecture After their initial introduction, health – In Transition apps were quickly updated to allow users to query the health status Ngari Tibetan Relocations of young or elderly family Eziza's Choice members who could not use The Long Walk Seeking to serve, strengthen and support the church and the people of China smartphones. Soon after, a version of whereabouts for the last 14 days and the app came out allowing foreigners whether you’ve had any COVID-19 to also use the app by logging in symptoms. with their passport. However, some foreigners could not register using a The Health Code Traveller Version health app apparently because their app, and its mini programs, offer an English names were too long. English-language interface and the same color-code system as used by On July 1, 2020, China released a Health Chinese locals.
    [Show full text]
  • Late Paleozoic and Mesozoic Evolution of the Lhasa Terrane in the Xainza MARK Area of Southern Tibet
    Tectonophysics 721 (2017) 415–434 Contents lists available at ScienceDirect Tectonophysics journal homepage: www.elsevier.com/locate/tecto Late Paleozoic and Mesozoic evolution of the Lhasa Terrane in the Xainza MARK area of southern Tibet ⁎ Suoya Fana,b, , Lin Dinga, Michael A. Murphyb, Wei Yaoa, An Yinc a Key Laboratory of Continental Collision and Plateau Uplift, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing 100101, China b Department of Earth and Atmospheric Sciences, University of Houston, Houston, TX 77204, USA c Department of Earth, Planetary, and Space Sciences, University of California, Los Angeles, CA 90095-1567, USA ARTICLE INFO ABSTRACT Keywords: Models for the Mesozoic growth of the Tibetan plateau describe closure of the Bangong Ocean resulting in Lhasa terrane accretion of the Lhasa terrane to the Qiangtang terrane along the Bangong-Nuijiang suture zone (BNSZ). Shortening However, a more complex history is suggested by studies of ophiolitic melanges south of the BNSZ “within” the Foreland basin Lhasa terrane. One such mélange belt is the Shiquanhe-Namu Co mélange zone (SNMZ) that is coincident with Suture zone the Geren Co-Namu Co thrust (GNT). To better understand the structure, age, and provenance of rocks exposed Provenance along the SNMZ we conducted geologic mapping, sandstone petrography, and U-Pb zircon geochronology of Geochronology rocks straddling the SNMZ. The GNT is north-directed and places Paleozoic strata against the Yongzhu ophiolite and Cretaceous strata along strike. A gabbro in the Yongzhu ophiolite yielded a U-Pb zircon age of 153 Ma. Detrital zircon age data from Permian rocks in the hanging wall suggests that the Lhasa terrane has affinity with the Himalaya and Qiangtang, rather than northwest Australia.
    [Show full text]
  • RESEARCH New Biostratigraphic Evidence of Late Permian to Late
    RESEARCH New biostratigraphic evidence of Late Permian to Late Triassic deposits from Central Tibet and their paleogeographic implications Gui-chun Wu1,*, Zhan-sheng Ji2, Wei-hua Liao3, and Jian-xin Yao1 1KEY LABORATORY OF STRATIGRAPHY AND PALAEONTOLOGY, MINISTRY OF LAND AND RESOURCES, INSTITUTE OF GEOLOGY, CHINESE ACADEMY OF GEOLOGICAL SCIENCES, BEIJING 100037, CHINA 2CHINESE ACADEMY OF GEOLOGICAL SCIENCES, BEIJING 100037, CHINA 3NANJING INSTITUTE OF GEOLOGY AND PALAEONTOLOGY, CHINESE ACADEMY OF SCIENCES, NANJING, 210008, CHINA ABSTRACT Triassic deposits in the Bangong-Nujiang Suture Zone are important for understanding its tectonic nature and evolutionary history, but have not been systematically studied due to a lack of biostratigraphic data. For a long time, the Upper Triassic Quehala Group featuring clasolite has been regarded as the only rocky unit. In recent years, the silicite-dominated Gajia Formation that bears radiolarian fossils was suggested to represent Ladinian to Carnian deposits. The Upper Permian and Lower Triassic rocks have never been excavated and thus are considered to be absent. This research, however, reveals that fossils aged from the Late Permian to Anisian of the Middle Trias- sic and Norian of the Late Triassic have been preserved in the central Bangong-Nujiang Suture Zone, which provides evidence of Upper Permian to early Middle Triassic deposits and provides new insights on the Upper Triassic strata as well. A new Triassic strata succes- sion is thus proposed for the Bangong-Nujiang Suture Zone, and it demonstrates great similarities with those from Lhasa to the south and Qiangtang to the north. Therefore, we deduce that the Bangong-Nujiang Suture Zone was under a similar depositional setting as its two adjacent terranes, and it was likely a carbonate platform background because limestones were predominant across the Triassic.
    [Show full text]
  • Status of the Tibetan Plateau Observatory (Tibet-Obs) and a 10
    Discussions https://doi.org/10.5194/essd-2020-209 Earth System Preprint. Discussion started: 16 October 2020 Science c Author(s) 2020. CC BY 4.0 License. Open Access Open Data 1 Status of the Tibetan Plateau observatory (Tibet-Obs) and a 2 10-year (2009-2019) surface soil moisture dataset 3 Pei Zhang1,2, Donghai Zheng2, Rogier van der Velde1, Jun Wen3, Yijian Zeng1, Xin Wang4, 4 Zuoliang Wang4, Jiali Chen2,5, Zhongbo Su1 5 1Faculty of Geo-Information Science and Earth Observation (ITC), University of Twente, Enschede, 6 7514AE, the Netherlands 7 2National Tibetan Plateau Data Center, Key Laboratory of Tibetan Environmental Changes and Land Surface 8 Processes, Institute of Tibetan Plateau Research, Chinese Academy of Sciences, Beijing, 100101, China 9 3College of Atmospheric Sciences, Chengdu University of Information Technology, Chengdu, 610225, 10 China 11 4Northwest Institute of Eco-Environment and Resources, Chinese Academy of Sciences, Lanzhou, 730000, 12 China 13 5College of Earth and Environmental Sciences, Lanzhou University, Lanzhou, 730000, China 14 15 Correspondence to: Donghai Zheng ([email protected]), Z. (Bob) Su ([email protected]) 16 Abstract. The Tibetan Plateau observatory of plateau scale soil moisture and soil temperature (Tibet-Obs) 17 was established ten years ago, which has been widely used to calibrate/validate satellite- and model-based 18 soil moisture (SM) products for their applications to the Tibetan Plateau (TP). This paper reports on the status 19 of the Tibet-Obs and presents a 10-year (2009-2019) surface SM dataset produced based on in situ 20 measurements taken at a depth of 5 cm collected from the Tibet-Obs that consists of three regional-scale SM 21 monitoring networks, i.e.
    [Show full text]
  • Tibet-Travel-Guide-Tibet-Vista.Pdf
    is located in southwest China with Tibetans as the main local inhabitants. It is Tibet situated on the Qinghai-Tibet Plateau, which is called the "roof of the world". Tibet fascinates tourists from home and abroad with its grandiose natural scenery, vast plateau landscape, charming holy mountains and sacred lakes, numerous ancient architectures and unique folk cultures, and the wonders created by the industrious and brave people of various nationalities in Tibet in the course of building their homeland. Tibet is not only a place that many Chinese and foreigners are eager to visit, but also a "paradise" for photographers. Top Spots of Tibet Catalog Lhasa Before you go The Spiritual and Political Capital of Tibet. 02 Best time to Go 03 Why Travel to Tibet Namtso 04-06 Tibet Permit & Visa “Heavenly Lake” of Tibet, its touching beauty 07 Useful Maps should not be missed by any traveler who visits 08 Getting There & Away Tibet. 09 Luggage Allowance 10-11 Food & Drinking Everest Nature Reserve 12 Shopping Once-in-a-life journey to experience the earth's 13 Where to Stay highest mountain. 14-15 High Altitude Sickness 16-17 Festivals & Events Nyingtri 18 What to Pack „Pearl of Tibet Plateau‟, where the climate is 19 Ethics and Etiquette subtropical, rice and bananas are grown, four 20 Money & Credit Card seasons are seen in the mountains. 21-22 Useful Words & No. 22 Tips for Photographing Tsedang The cradle of Tibetan civilization. Experience Real Tibet Mt. Kailash & Lake Manasarovar 23-25 Top Experiences Ttwo of the most far-flung and legendary travel 26-29 Lhasa & Around destinations in the world.
    [Show full text]
  • Tectonic Evolution of the Qiangtang Terrane, Central Tibetan Plateau
    Tectonic evolution of the Qiangtang terrane, Central Tibetan Plateau Zhao Zhongbao Eberhard Karls Universität Tübingen Structural Geology Group 2015 Tectonic evolution of the Qiangtang terrane, central Tibetan Plateau Dissertation der Mathematisch-Naturwissenschaftlichen Fakultät der Eberhard Karls Universität Tübingen zur Erlangung des Grades eines Doktors der Naturwissenschaften (Dr. rer. nat.) vorgelegt von Zhongbao Zhao aus Shanxi, China Tübingen, 2015 Erklärung Ich erkläre hiermit, dass ich die zur Promotion eingereichte Arbeit selbständig verfasst, nur die angegebenen Quellen und Hilfsmittel benutzt und wörtlich oder inhaltlich übernommene Stellen als solche gekennzeichnet habe. Ich erkläre, dass die Richtlinien zur Sicherung guter wissenschaftlicher Praxis der Universität Tübingen (Beschluss des Senats vom 25.5.2000) beachtet wurden. Ich versichere an Eides statt, dass diese Angaben wahr sind und dass ich nichts verschwiegen habe. Mir ist bekannt, dass die falsche Abgabe einer Versicherung an Eides statt mit Freiheitsstrafe bis zu drei Jahren oder mit Geldstrafe bestraft wird. Tübingen, June 2015 Datum der mündlichen Prüfung: 28th. August 2015 Dekan: Prof. Dr. Wolfgang Rosenstiel 1. Berichterstatter: Prof. Dr. Paul D Bons 2. Berichterstatter: Prof. Dr. Genhou Wang II Thesis organization and list of publications This PhD-thesis is organized in a cumulative manner. It is separated into 6 chapters. Here, the general organization of the thesis and a list of included publications are given. Chapter 1 presents an introduction covering the context and the main ideas of the thesis. In Chapter 2-4 three different research papers which were published in the framework of the present study are represented. Chapter 5 represents results from (U-Th)/He thermochronology that are going to be a paper written for concerning on Cretaceous uplifting and shortening of Qiangtang terrane.
    [Show full text]
  • River Network Evolution As a Major Control for Orogenic Exhumation: Case Study from the Western Tibetan Plateau ∗ Loraine Gourbet A,E, , Gweltaz Mahéo A, David L
    Earth and Planetary Science Letters 456 (2016) 168–181 Contents lists available at ScienceDirect Earth and Planetary Science Letters www.elsevier.com/locate/epsl River network evolution as a major control for orogenic exhumation: Case study from the western Tibetan plateau ∗ Loraine Gourbet a,e, , Gweltaz Mahéo a, David L. Shuster b,c, Alka Tripathy-Lang b,c, Philippe Hervé Leloup a, Jean-Louis Paquette d a Univ Lyon, Ens de Lyon, Univ Lyon 1, CNRS, UMR 5276 LGL-TPE, F-69342, Lyon, France b Department of Earth and Planetary Science, University of California, Berkeley, 479 McCone Hall, Berkeley, CA 94720-4767, USA c Berkeley Geochronology Center, 2455 Ridge Road, Berkeley, CA 94709, USA d Laboratoire Magmas et Volcans, 5 rue Kessler, 63038 Clermont-Ferrand, France e Geologisches Institut, ETH, Zürich, Switzerland a r t i c l e i n f o a b s t r a c t Article history: The westernmost Tibetan plateau, despite being internally drained, has a high topographic relief. Here, 4 3 Received 2 May 2016 using apatite (U–Th–Sm)/He and He/ He thermochronometry, we reconstruct the exhumation history Received in revised form 19 September of the Rutog batholith during the Neogene. Thermal modeling in 1D using the QTQt program indicates 2016 that relatively slow cooling occurred from 30 Ma to 19 Ma, which we interpret as an exhumation rate of Accepted 21 September 2016 ∼10 m/Ma. This was followed by two pulses of moderate cooling from 19 to 17 Ma and ∼11 to 9Ma Available online 20 October 2016 that correspond to a total exhumation of about 1500 m.
    [Show full text]
  • Development and Progress of Tibet
    11/6/2014 Development and Progress of Tibet ENGLISH.GOV.CN THE STATE COUNCIL THE PEOPLE'S REPUBLIC OF CHINA Old Version | 中文 | 6 Nov 2014 HOME PREMIER NEWS POLICIES STATE COUNCIL SERVICES ARCHIVE HOME >> ARCHIVE >> WHITE PAPER Development and Progress of Tibet VIDEOS www.scio.gov.cn Updated: Development and Progress of Tibet Information Office of the State Council of the People’s Republic of China October 2013 China Youth - Episode 4: Contents The Gap Foreword I. The Development and Progress in Tibet Is the Inevitable Result of History II. Economic Growth and Improvement of the People’s Livelihood III. Political Progress -- the People Are the Masters of Their Own Fate IV. Cultural Preservation and Freedom of Religious Belief V. Social Changes and Development of All Undertakings VI. Environmental Protection and Ecological Improvement Concluding Remarks STATE COUNCIL Foreword PREMIER : Li Keqiang Tibet is located in the southern part of the Qinghai-Tibet Plateau and stands at the VICE-PREMIERS : southwestern border of China. It is an autonomous region of the People’s Republic of Zhang Gaoli, Liu Yandong, Wang Yang, Ma Kai China. STATE COUNCILORS: Yang Jing, Chang Wanquan, Yang Jiechi , Guo Tibet has been an integral part of China since ancient times. Prior to the 1950s, Tibet Shengkun, Wang Yong was a society of feudal serfdom under theocratic rule, a society characterized by a SECRETARY GENERAL : Yang Jing combination of political and religious powers. Government officials, aristocrats and monasteries collectively maintained tight control over Tibet’s resources and wealth, MINISTRIES and the Tibetan people lived in dire misery without any freedom.
    [Show full text]