The Silk Road: Xi'an to Kashgar
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7 Days Memories of Xinjiang Tour
[email protected] +86-28-85593923 7 days Memories of Xinjiang tour https://windhorsetour.com/silk-road-tour/xinjiang-highlights-tour Urumqi Turpan Kashgar Tashkorgan Urumqi Vist two popular cities in this Xinjiang highlights tour, Turpan and Kashgar. Drive into the deserts of Turpan to explore the relics left by the ancient civilizations, and enjoy a tranquil hiking along the shore of Karakul Lake in Kashgar. Type Private Duration 7 days Theme Natural scenery Trip code XJT-01 Price From US$ 1,061 per person Itinerary Starting from Urumqi, this Xinjiang Highlights tour provides a memorable experience to two must-see cities, Turpan and Kashgar. Cultural heritages and natural landscapes are balanced in this trip. You will be fascinated by the unique scenery of deserts, lakes, and forests while exploring the past civilizations along the ancient Silk Road. The unique Uyghur culture is yet another a highlight of this tour. Day 01 : Arrive Urumqi Travel along the Silk Road to pursue the unique beauty of this ancient and historically important trade route in the world. Explore the past civilizations which have influenced the culture of China, Central Asia and the west for thousands of years. This memorable Silk Road Xinjiang tour starts in the capital of of this province, Urumqi. Upon arrival at the airport or railway station, be assisted to the downtown hotel by your local driver and guide. Have the day to rest or explore this city on your own. Day 02 : Drive to Turpan - Turpan Sightseeing In the morning, drive to Turpan, an oasis city located in the southeast of Urumqi. -
Muztagh Ata 7546M
Muztagh Ata 7546m Technically easy summit over 7500m Stunning peak with incredible views The remote and diverse city of Kashgar TREK OVERVIEW Muztagh Ata meaning ‘The father of ice mountains’, rises Kunlun mountains to the East and the Tien Shan to the out of China’s vast Taklimakan Desert in the Xinjiang North. The ascent involves establishing three camps en Province of China and provides the opportunity to climb a route above Base Camp, all approached without technical mountain over 7500m with minimal technical difficulty. difficulty. The summit day, although technically For those with the appropriate skills, it is often used as a straightforward, will feel exhausting as a result of the stepping stone to an 8000m peak which could include extreme altitude, so a good level of fitness is essential. Everest. Given a clear day, you will be rewarded with tremendous views of the Pamir, the Karakoram and K2. It lies in the centre of the great mountain ranges of Asia, with the Karakoram to the south, the Pamir to the west, the Participation Statement Adventure Peaks recognises that climbing, hill walking and mountaineering are activities with a danger of personal injury or death. Participants in these activities should be aware of and accept these risks and be responsible for their own actions and involvement. Adventure Travel – Accuracy of Itinerary Although it is our intention to operate this itinerary as printed, it may be necessary to make some changes as a result of flight schedules, climatic conditions, limitations of infrastructure or other operational factors. As a consequence, the order or location of overnight stops and the duration of the day may vary from those outlined. -
Brochure 2017
TOP CHINA TRAVEL Brochure 2017 www.topchinatravel.com Beijing > The Capital of China Xian > Gateway to Ancient City Shanghai > Modern Metropolis Guilin > Best Karst Landscape Chengdu > Panda’s Hometown Lhasa > Sunshine city & Holy Land Silk Road > For Adventure 4 Days Highlights Tour Beijing Beijing, the capital of the People's Republic of Chi- Day 1 Arrival Beijing na, it is not only the nation's political center, but also Airport transfer service to hotel Hanging out at Houhai night bar a cultural, scientific and educational heart as well as a key transportation hub. Beijing has served as a capital Day 2 Beijing of the country for more than 800 years. The city has Tiananmen Square, Forbidden City, Jingshan many places of historic interest and scenic beauty. Park, Peking Hutongs The city also has a character all its own; there are Day 3 Beijing quadrangles, Hutongs, tricycle, boiled mutton, arts Temple of Heaven, Mutianyu Great Wall, and crafts, roasted duck and Peking Opera. Peking duck farewell dinner Day 4 Departure Beijing Transfer service to Beijing airport Beyond Ordinary, we have more... Join the small group From $155 P/P Wild Great Wall Chenjiabao Great Wall is one of the most beautiful section of the wild Walls around Beijing which is never restored and less tourist. It located in Huailai County, Zhangjiakou, Hebei Province. The highest sea level is about 1280 meters. Day 1 Beijing – Chenjiabao Great Wall Picked up your hotel and departure around 12:30 at noon. Have 2-hour drive to the Chenjia- bao Great Wall. Hike on the Chenjiabao Great wall about 3 hours hiking route. -
The Geodynamics of the Pamir–Punjab Syntaxis V
ISSN 00168521, Geotectonics, 2013, Vol. 47, No. 1, pp. 31–51. © Pleiades Publishing, Inc., 2013. Original Russian Text © V.S. Burtman, 2013, published in Geotektonika, 2013, Vol. 47, No. 1, pp. 36–58. The Geodynamics of the Pamir–Punjab Syntaxis V. S. Burtman Geological Institute, Russian Academy of Sciences, Pyzhevskii per. 7, Moscow, 119017 Russia email: [email protected] Received December 19, 2011 Abstract—The collision of Hindustan with Eurasia in the Oligocene–early Miocene resulted in the rear rangement of the convective system in the upper mantle of the Pamir–Karakoram margin of the Eurasian Plate with subduction of the Hindustan continental lithosphere beneath this margin. The Pamir–Punjab syn taxis was formed in the Miocene as a giant horizontal extrusion (protrusion). Extensive nappes developed in the southern and central Pamirs along with deformation of its outer zone. The Pamir–Punjab syntaxis con tinued to form in the Pliocene–Quaternary when the deformed Pamirs, which propagated northward, were being transformed into a giant allochthon. A fold–nappe system was formed in the outer zone of the Pamirs at the front of this allochthon. A geodynamic model of syntaxis formation is proposed here. DOI: 10.1134/S0016852113010020 INTRODUCTION Mujan, BandiTurkestan, Andarab, and Albruz– The tectonic processes that occur in the Pamir– Mormul faults (Fig. 1). Punjab syntaxis of the Alpine–Himalayan Foldbelt The Pamir arc is more compressed as compared and at the boundary of this syntaxis with the Tien Shan with the Hindu Kush–Karakoram arc. Disharmony of have attracted the attention of researchers for many these arcs arose in the western part of the syntaxis due years [2, 7–9, 13, 15, 28]. -
Channel Adjustments in Response to the Operation of Large Dams: the Upper Reach of the Lower Yellow River
University of Wollongong Research Online Faculty of Science - Papers (Archive) Faculty of Science, Medicine and Health 1-1-2012 Channel adjustments in response to the operation of large dams: the upper reach of the lower Yellow River Yuanxu Ma Chinese Academy of Sciences He Qing Huang Chinese Academy of Sciences Gerald C. Nanson University of Wollongong, [email protected] Yongi Li Yellow River Institute of Hydraulic Research China Wenyi Yao Yellow River Institute of Hydraulic Research, China Follow this and additional works at: https://ro.uow.edu.au/scipapers Part of the Life Sciences Commons, Physical Sciences and Mathematics Commons, and the Social and Behavioral Sciences Commons Recommended Citation Ma, Yuanxu; Huang, He Qing; Nanson, Gerald C.; Li, Yongi; and Yao, Wenyi: Channel adjustments in response to the operation of large dams: the upper reach of the lower Yellow River 2012, 35-48. https://ro.uow.edu.au/scipapers/4279 Research Online is the open access institutional repository for the University of Wollongong. For further information contact the UOW Library: [email protected] Channel adjustments in response to the operation of large dams: the upper reach of the lower Yellow River Abstract The Yellow River in China carries an extremely large sediment load. River channel-form and lateral shifting in a dynamic, partly meandering and partly braided reach of the lower Yellow River, have been significantly influenced by construction of Sanmenxia Dam in 1960, Liujiaxia Dam in 1968, Longyangxia Dam in 1985 and Xiaolangdi Dam in 1997. Using observations from Huayuankou Station, 128 km downstream of Xiaolangdi Dam, this study examines changes in the river before and after construction of the dams. -
Assessment of Snow, Glacier and Water Resources in Asia
IHP/HWRP-BERICHTE Heft 8 Koblenz 2009 Assessment of Snow, Glacier and Water Resources in Asia Assessment of Snow, Glacier and Water Resources in Asia Resources Water Glacier and of Snow, Assessment IHP/HWRP-Berichte • Heft 8/2009 IHP/HWRP-Berichte IHP – International Hydrological Programme of UNESCO ISSN 1614 -1180 HWRP – Hydrology and Water Resources Programme of WMO Assessment of Snow, Glacier and Water Resources in Asia Selected papers from the Workshop in Almaty, Kazakhstan, 2006 Joint Publication of UNESCO-IHP and the German IHP/HWRP National Committee edited by Ludwig N. Braun, Wilfried Hagg, Igor V. Severskiy and Gordon Young Koblenz, 2009 Deutsches IHP/HWRP - Nationalkomitee IHP – International Hydrological Programme of UNESCO HWRP – Hydrology and Water Resource Programme of WMO BfG – Bundesanstalt für Gewässerkunde, Koblenz German National Committee for the International Hydrological Programme (IHP) of UNESCO and the Hydrology and Water Resources Programme (HWRP) of WMO Koblenz 2009 © IHP/HWRP Secretariat Federal Institute of Hydrology Am Mainzer Tor 1 56068 Koblenz • Germany Telefon: +49 (0) 261/1306-5435 Telefax: +49 (0) 261/1306-5422 http://ihp.bafg.de FOREWORD III Foreword The topic of water availability and the possible effects The publication will serve as a contribution to the of climate change on water resources are of paramount 7th Phase of the International Hydrological Programme importance to the Central Asian countries. In the last (IHP 2008 – 2013) of UNESCO, which has endeavored decades, water supply security has turned out to be to address demands arising from a rapidly changing one of the major challenges for these countries. world. Several focal areas have been identified by the The supply initially ensured by snow and glaciers is IHP to address the impacts of global changes. -
Undrained Shear Behavior of Loess Saturated with Different Title Concentrations of Sodium Chloride Solution
Undrained shear behavior of loess saturated with different Title concentrations of sodium chloride solution Zhang, Fanyu; Wang, Gonghui; Kamai, Toshitaka; Chen, Author(s) Wenwu; Zhang, Dexuan; Yang, Jun Citation Engineering Geology (2013), 155: 69-79 Issue Date 2013-03 URL http://hdl.handle.net/2433/173358 Right © 2013 Elsevier B.V. Type Journal Article Textversion author Kyoto University Submitted to: Engineering Geology (ENGEO4476-revised draft) Undrained shear behavior of loess saturated with different concentrations of sodium chloride solution Fanyu Zhanga,b, Gonghui Wanga,*, Toshitaka Kamaia, Wenwu Chenb, Dexuan Zhangc, Jun Yangd Affiliations: (a): Research Center on Landslides Disaster Prevention Research Institute Kyoto University Gokasho, Uji, Kyoto, 611-0011 Japan (b): Key Laboratory of Mechanics on Disaster and Environment in Western China (Lanzhou University), Ministry of Education, China Department of Geological Engineering Lanzhou University Tianshui Road, 222, Lanzhou, 730000 P.R. China (c): Department of Civil Engineering Shanghai Jiao Tong University Shanghai 200240 P.R. China (d): Department of Civil Engineering The University of Hong Kong Hong Kong P.R. China *: Corresponding author Email: [email protected] Telephone: +81-774-384115; Fax: +81-774-384300 1 Undrained shear behavior of loess saturated with different concentrations of sodium 2 chloride solution 3 Fanyu Zhanga,b, Gonghui Wanga,*, Toshitaka Kamaia, Wenwu Chenb, Dexuan Zhangc, Jun Yangd 4 Abstract: A series of ring-shear tests was conducted on saturated loess to investigate the 5 effects of NaCl concentration in pore water and desalinization on the shear behavior under 6 undrained conditions. The loess samples were taken from the ground surface of a frequently 7 active landslide in China, were saturated by de-aired, distilled water with different 8 concentrations of NaCl, and then were sheared undrained. -
Irrigation in Southern and Eastern Asia in Figures AQUASTAT Survey – 2011
37 Irrigation in Southern and Eastern Asia in figures AQUASTAT Survey – 2011 FAO WATER Irrigation in Southern REPORTS and Eastern Asia in figures AQUASTAT Survey – 2011 37 Edited by Karen FRENKEN FAO Land and Water Division FOOD AND AGRICULTURE ORGANIZATION OF THE UNITED NATIONS Rome, 2012 The designations employed and the presentation of material in this information product do not imply the expression of any opinion whatsoever on the part of the Food and Agriculture Organization of the United Nations (FAO) concerning the legal or development status of any country, territory, city or area or of its authorities, or concerning the delimitation of its frontiers or boundaries. The mention of specific companies or products of manufacturers, whether or not these have been patented, does not imply that these have been endorsed or recommended by FAO in preference to others of a similar nature that are not mentioned. The views expressed in this information product are those of the author(s) and do not necessarily reflect the views of FAO. ISBN 978-92-5-107282-0 All rights reserved. FAO encourages reproduction and dissemination of material in this information product. Non-commercial uses will be authorized free of charge, upon request. Reproduction for resale or other commercial purposes, including educational purposes, may incur fees. Applications for permission to reproduce or disseminate FAO copyright materials, and all queries concerning rights and licences, should be addressed by e-mail to [email protected] or to the Chief, Publishing Policy and Support Branch, Office of Knowledge Exchange, Research and Extension, FAO, Viale delle Terme di Caracalla, 00153 Rome, Italy. -
Community Matters in Xinjiang 1880–1949 China Studies
Community Matters in Xinjiang 1880–1949 China Studies Published for the Institute for Chinese Studies University of Oxford Editors Glen Dudbridge Frank Pieke VOLUME 17 Community Matters in Xinjiang 1880–1949 Towards a Historical Anthropology of the Uyghur By Ildikó Bellér-Hann LEIDEN • BOSTON 2008 Cover illustration: Woman baking bread in the missionaries’ home (Box 145, sheet nr. 26. Hanna Anderssons samling). Courtesy of the National Archives of Sweden (Riksarkivet) and The Mission Covenant Church of Sweden (Svenska Missionskyrkan). This book is printed on acid-free paper. Library of Congress Cataloging-in-Publication Data Bellér-Hann, Ildikó. Community matters in Xinjiang, 1880–1949 : towards a historical anthropology of the Uyghur / by Ildikó Bellér-Hann. p. cm — (China studies, ISSN 1570–1344 ; v. 17) Includes bibliographical references and index. ISBN 978-90-04-16675-2 (hardback : alk. paper) 1. Uighur (Turkic people)—China— Xinjiang Uygur Zizhiqu—Social life and customs. 2. Uighur (Turkic people)—China— Xinjiang Uygur Zizhiqu—Religion. 3. Muslims—China—Xinjiang Uygur Zizhiqu. 4. Xinjiang Uygur Zizhiqu (China)—Social life and customs. 5. Xinjiang Uygur Zizhiqu (China)—Ethnic relations. 6. Xinjiang Uygur Zizhiqu (China)—History—19th century. I. Title. II. Series. DS731.U4B35 2008 951’.604—dc22 2008018717 ISSN 1570-1344 ISBN 978 90 04 16675 2 Copyright 2008 by Koninklijke Brill NV, Leiden, The Netherlands. Koninklijke Brill NV incorporates the imprints Brill, Hotei Publishing, IDC Publishers, Martinus Nijhoff Publishers and VSP. All rights reserved. No part of this publication may be reproduced, translated, stored in a retrieval system, or transmitted in any form or by any means, electronic, mechanical, photocopying, recording or otherwise, without prior written permission from the publisher. -
Dictionary of Geotourism Anze Chen • Young Ng • Erkuang Zhang Mingzhong Tian Editors
Dictionary of Geotourism Anze Chen • Young Ng • Erkuang Zhang Mingzhong Tian Editors Dictionary of Geotourism With 635 Figures and 12 Tables Editors Anze Chen Young Ng Chinese Academy of Geological Sciences The Geological Society of Australia Beijing, China Sydney, NSW, Australia Erkuang Zhang Mingzhong Tian The Geological Society of China China University of Geosciences Beijing, China Beijing, China ISBN 978-981-13-2537-3 ISBN 978-981-13-2538-0 (eBook) ISBN 978-981-13-2539-7 (print and electronic bundle) https://doi.org/10.1007/978-981-13-2538-0 Jointly published with Science Press, Beijing, China ISBN: 978-7-03-058981-1 Science Press, Beijing, China © Springer Nature Singapore Pte Ltd. 2020 This work is subject to copyright. All rights are reserved by the Publisher, whether the whole or part of the material is concerned, specifically the rights of translation, reprinting, reuse of illustrations, recitation, broadcasting, reproduction on microfilms or in any other physical way, and transmission or information storage and retrieval, electronic adaptation, computer software, or by similar or dissimilar methodology now known or hereafter developed. The use of general descriptive names, registered names, trademarks, service marks, etc. in this publication does not imply, even in the absence of a specific statement, that such names are exempt from the relevant protective laws and regulations and therefore free for gecneral use. The publisher, the authors, and the editors are safe to assume that the advice and information in this book are believed to be true and accurate at the date of publication. Neither the publisher nor the authors or the editors give a warranty, express or implied, with respect to the material contained herein or for any errors or omissions that may have been made. -
12 Days Silk Road Desert Highway Adventure
[email protected] +86-28-85593923 12 days Silk Road desert highway adventure https://windhorsetour.com/silk-road-tour/silk-road-adventure-tour Urumqi Turpan Kuqa Hotan Kashgar Tashkorgan Kashgar Discover the marvelous Xinjiang in this Silk Road discovery tour. Explore the unique Uyghur culture and past civilizations with a trip from Turpan to Kashgar, plus camel riding and camping experience in the Taklamkan Deserts. All amazing! Type Private Duration 12 days Theme Overland Trip code XJT-02 Price From US$ 1,465 per person Itinerary This Silk Road discovery tour balances an overland trip from Urumqi to Kashgar and sightseeing in the splendid Karakul Lake. Endless scenery await to be discovered as you travel across the vast deserts in Xinjiang. Stop in the Taklamkan Desert to have a memorable camping experience and enjoy the sunset and sunrise. Added with a cultural visit in Turpan, where you will see many relics along the Silk Road. All together, learning about the history of this famous ancient trading route that still vibrant today. Day 01 : Arrive Urumqi Urumqi, the capital of Xinjiang province, is the entrance point of this memorable Silk Road adventure. Once you arrive at the airport or train station, your local guide will meet and assist you to the downtown hotel. The rest of today is left free, have a rest or roam the local streets nearby on your own. Urumqi is a great city to explore the customs of Uyghur people and experience their local life. Notice the clock time in Urumqi of Xinjiang is the same as Beijing Time, but there is 2 hours difference because of the longitude. -
A MARS ANALOG. A. S . Walker, MS 730, U
DRAINAGE IN GOBI TERRAIN : A MARS ANALOG. A. S. Walker, MS 730, U. S. Geological Survey, Reston, Ira. 22092. The Turpan Depression is a 50 ,000-h2 fault-fond interior drainage basin in Xinjiang Autonomous Region, People's Republic of China (fig. 1). The depression is named after Turpan County (43O N. , 89' E. ) , a small city in the north-central part of the basin and is bounded on the north, east, and west by the Bogda Mountains (6,500 m above sea level m3ximum elevation), and on the south by the Kuruktag buntains (1,500m). Both muntain ranges are part of the Tian Shan (Sky Mountains), a permanently glaciated range which was uplifted during the Cenozoic (Himlayan Uplift ) . The mountains are composed mainly of quartzite and other rr-etasedirnents; however, the southern slopes and foothills of the Bogda Mountains are conposed of red, and to a lesser extent white, sandstone, conglomerate, and mudstone, and are called the Flaming Mountains (850 rn in elevation). The lowest point in the basin is Aydingkol Lake (-154 m). The basin is extremely arid, windy and hot with a mxirm recorded sand temperature of 82.30 C. and a maximum recorded wind velocity greater than 110 dsec. (1). Tne Turpan Depression may be divided into two sermlconcentric belts. The area adjacent to the mountains, on gently sloping (1-3') alluv5al fans is primarily composed of black gobi (regionally unsorted loose subangular to subrounded quartzite gravels, predominately of pebble size, but with occasional cobbles) occupying an area 25-hn wide in the north and 15-kn wide in the south (fig.