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LCT - Silk Road & Xinjiang - 15D-01
www.lilysunchinatours.com 15-day Silk Road and Xinjiang Tour Tour code: LCT - Silk Road & Xinjiang - 15D-01 Attractions: Overview: This two-week trip will take you to explore the most mysterious parts of China, Gansu and Xinjiang Province, to pursue the old Silk Road. Starting from Lanzhou, you will visit a number of historical places and natural wonders until the last city Karmay. A private guide and driver will be arranged to navigate your way through the exotic places to make sure everything go well. Highlights: 1. Take a boat to visit the hidden gem of Lanzhou - Bingling Thousand -Buddha Caves; 2. Immerse yourself in the magnificence of the Rainbow Mountains in Zhangye Danxia Landform Park; 3. Meet the unbreakable pass - Jiayuguan Pass; 4. Appreciate the murals and paintings inside the Mogao Caves; 5. Explore the ruins of Jiaohe Ancient Town and taste the yummy Xinjiang fruits; 6. Unveil the secrets of Karez Irrigation System; 7. Experience the Grand Bazaar of Xinjiang and feel the hospitality of local people; 8. Relax at the picturesque Heavenly Lake and listen to the beautiful legends; 9. Pay a visit to a Tuva Family and enjoy the raw, primitive grassland scenery; 10. Challenge yourself with the “horrible” Urho Ghost City in Karamy. Detailed Itinerary: Day 1: Welcome to Lanzhou! A private car & driver will be arranged to pick you uppon your arrival and transfer you to your hotel. You may spend the rest of the day adjust or have some activities on uyour own. Tel: +86 18629295068 / 1-909-666-8151 (toll free) Email: [email protected] www.lilysunchinatours.com Day 2: Bingling Thousand-Buddha Caves, Gansu Provincial Museum 08:00: Your Lanzhou local expert will meet you at your hotel lobby and take you to explore the amazing Lanzhou city. -
Palaeoclimate, Glacier and Treeline Reconstruction Based On
Zurich Open Repository and Archive University of Zurich Main Library Strickhofstrasse 39 CH-8057 Zurich www.zora.uzh.ch Year: 2018 Palaeoclimate, glacier and treeline reconstruction based on geomorphic evidences in the Mongun-Taiga massif (south-eastern Russian Altai) during the Late Pleistocene and Holocene Ganyushkin, Dmitry ; Chistyakov, Kirill ; Volkov, Ilya ; Bantcev, Dmitry ; Kunaeva, Elena ; Brandová, Dagmar ; Raab, Gerald ; Christl, Marcus ; Egli, Markus Abstract: Little is known about the extent of glaciers and dynamics of the landscape in south-eastern Russian Altai. The effects of climate-induced fluctuations of the glaciers and the upper treeline of the Mongun-Taiga mountain massif were, therefore, reconstructed on the basis of in-situ, multiannual observations, geomorphic mapping, radiocarbon and surface exposure dating, relative dating (such as Schmidthammer and weathering rind) techniques and palaeoclimate-modelling. During the maximal advance of the glaciers, their area was 26-times larger than now and the equilibrium line of altitude (ELA) was about 800m lower. Assuming that the maximum glacier extent took place during MIS 4, then the average summer temperatures were 2.7℃ cooler than today and the amount of precipitation 2.1 times higher. Buried wood trunks by a glacier gave ages between 60 and 28 cal ka BP and were found 600-700m higher than the present upper treeline. This evidences a distinctly elevated treeline during MIS 3a and c. With a correction for tectonics we reconstructed the summer warming to have been between 2.1 and 3.0℃. During MIS 3c, the glaciated area was reduced to less than 0.5 km² with an increase of the ELA of 310-470m higher than today. -
Present Glaciers of Tavan Bogd Massif in the Altai Mountains, Central Asia, and Their Changes Since the Little Ice Age
geosciences Article Present Glaciers of Tavan Bogd Massif in the Altai Mountains, Central Asia, and Their Changes since the Little Ice Age Dmitry A. Ganyushkin 1,* , Kirill V. Chistyakov 1, Ilya V. Volkov 1, Dmitry V. Bantcev 1, Elena P. Kunaeva 1,2, Tatyana A. Andreeva 1, Anton V. Terekhov 1,3 and Demberel Otgonbayar 4 1 Institute of Earth Science, Saint-Petersburg State University, Universitetskaya nab. 7/9, Saint-Petersburg 199034, Russia; [email protected] (K.V.C.); [email protected] (I.V.V.); [email protected] (D.V.B.); [email protected] (E.P.K.); [email protected] (T.A.A.); [email protected] (A.V.T.) 2 Department of Natural Sciences and Geography, Pushkin Leningrad State University, 10 Peterburgskoe shosse, St Petersburg (Pushkin) 196605, Russia 3 Institute of Limnology RAS, Saint Petersburg, Sevastyanov St. 9, St Petersburg 196105, Russia 4 Institute of Natural Science and Technology, Khovd State University of Mongolia, Hovd 84000, Khovd, Mongolia Mongolian Republic; [email protected] * Correspondence: [email protected] or [email protected]; Tel.: +7-921-3314-598 Received: 17 August 2018; Accepted: 7 November 2018; Published: 12 November 2018 Abstract: The Tavan Bogd mountains (of which, the main peak, Khuiten Uul, reaches 4374 m a.s.l.) are situated in the central part of the Altai mountain system, in the territories of Russia, Mongolia and China. The massif is the largest glacierized area of Altai. The purposes of this study were to provide a full description of the scale and structure of the modern glacierized area of the Tavan Bogd massif, to reconstruct the glaciers of the Little Ice Age (LIA), to estimate the extent of the glaciers in 1968, and to determine the main glacial trends, and their causes, from the peak of the LIA. -
Xinjiang, NW China
CORE Metadata, citation and similar papers at core.ac.uk Provided by UCL Discovery Impact of recent climate change on Lake Kanas, South of the Altay Mountains (Xinjiang, N.W. China) inferred from diatom and geochemical evidence Xueru Lin, Patrick Rioual, Handong Yang, Xiaozhong Huang X. Lin, X. Huang MOE Key Laboratory of Western China’s Environmental System, Lanzhou University, Lanzhou 730 000, China. P. Rioual Key Laboratory of Cenozoic Geology and Environment, Institute of Geology & Geophysics, Chinese Academy of Sciences, Beijing 100 029, China e-mail: [email protected] H. Yang Environmental Change Research Centre, University College London, Pearson Building, Gower Street, WC1E 6BT, London, United Kingdom Keywords: global warming, glacier meltwater Abstract Global warming is one of the most important environmental problems the world is facing and the changes it is causing on ecosystems is drawing great attention from scientists. In particular, how lake ecosystems, which are an important part of continental ecosystems, will change is a problem that needs to be investigated. In this study, we combined geochemical and diatom analyses of a sediment core retrieved from Lake Kanas (N.W. China) to assess how climate change has affected this ecosystem over the past ~100 years. Our results show that the aquatic ecosystem of Lake Kanas was sensitive to changes in the regional climate over the past ~100 years. The lake has been affected by change in its hydrology (e.g. influx of glacier meltwater, variations in precipitation) and change in its hydrodynamics (water column stability). The variations in abundance and composition of the diatom assemblages observed in the sedimentary record have been subtle and are complex to interpret. -
Glacial Geomorphology of the Altai and Western Sayan Mountains, Central Asia Robin Blomdinab, Jakob Heymanb, Arjen P
This article was downloaded by: [Stockholm University Library] On: 04 August 2015, At: 10:17 Publisher: Taylor & Francis Informa Ltd Registered in England and Wales Registered Number: 1072954 Registered office: 5 Howick Place, London, SW1P 1WG Journal of Maps Publication details, including instructions for authors and subscription information: http://www.tandfonline.com/loi/tjom20 Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia Robin Blomdinab, Jakob Heymanb, Arjen P. Stroevenb, Clas Hättestrandb, Jonathan M. Harborab, Natacha Gribenskib, Krister N. Janssonb, Dmitry A. Petrakovc, Mikhail N. Ivanovc, Orkhonselenge Alexanderd, Alexei N. Rudoye & Michael Waltherf a Department of Earth, Atmospheric, and Planetary Sciences, Purdue University, West Lafayette, USA b Bolin Centre for Climate Research, Department of Physical Geography and Quaternary Geology, Stockholm University, Click for updates Stockholm, Sweden c Faculty of Geography, Lomonosov Moscow State University, Moscow, Russia d Department of Geography, School of Arts and Sciences, National University of Mongolia, Ulaanbaatar, Mongolia e Department of Geology and Geography, Tomsk State University, Tomsk, Russia f Mongolian Academy of Sciences, Geographical Institute, Ulaanbaatar, Mongolia Published online: 11 Dec 2014. To cite this article: Robin Blomdin, Jakob Heyman, Arjen P. Stroeven, Clas Hättestrand, Jonathan M. Harbor, Natacha Gribenski, Krister N. Jansson, Dmitry A. Petrakov, Mikhail N. Ivanov, Orkhonselenge Alexander, Alexei N. Rudoy & Michael Walther (2014): Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia, Journal of Maps, DOI: 10.1080/17445647.2014.992177 To link to this article: http://dx.doi.org/10.1080/17445647.2014.992177 PLEASE SCROLL DOWN FOR ARTICLE Taylor & Francis makes every effort to ensure the accuracy of all the information (the “Content”) contained in the publications on our platform. -
Abstract Key Words
Preprints (www.preprints.org) | NOT PEER-REVIEWED | Posted: 18 August 2018 doi:10.20944/preprints201808.0332.v1 Peer-reviewed version available at Geosciences 2018, 8, 414; doi:10.3390/geosciences8110414 Present glaciers of Tavan Bogd mountain massif and their changes since the LIA Dmitry A. Ganyushkin 1,*, Kirill V. Chistyakov 1, Ilya V. Volkov 1, Dmitry V. Bantcev 1, Elena P. Kunaeva 12, Tatyana A. Andreeva, Anton V. Terekhov 1,3, Demberel Otgonbayar4 1 Institute of Earth Science, Saint-Petersburg State University, Universitetskaya nab. 7/9, Saint-Petersburg 199034, Russia; [email protected] (K.V.C.); [email protected] (I.V.V.); [email protected] (D.V.B.); [email protected] (T.A.A); [email protected] (A.V.T.) 2 Department of Natural Sciences and Geography, Pushkin Leningrad State University, 10 Peterburgskoe shosse, St Petersburg (Pushkin) 196605, Russia; [email protected] 3 Institute of Limnology RAS, Saint Petersburg, Sevastyanov st., 9 St Petersburg 196105, Russia 4 Khovd State University of Mongolia, Institute of Natural science and technology, Hovd, Khovd province, Jargalant soum, 84000 Khovd, Mongolia Mongolian Republic * Correspondence: [email protected] or [email protected]; Tel.: +7-921-3314-598 Abstract The study is based on the results of long-term field studies, satellite and aerial data analysis. In the maximum of the Little Ice Age (LIA) 243 glaciers with a total area of 353.4 km2 were reconstructed. By the results of interpretation of Corona images by 1968 the number of glaciers increased (236), the total area reduced to 242 km2. In 2010 glaciation was represented by 237 glaciers with a total area of 201 km2. -
Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains
geosciences Article Application of Rock Weathering and Colonization by Biota for the Relative Dating of Moraines from the Arid Part of the Russian Altai Mountains Dmitrii A. Ganyushkin 1,* , Sofia N. Lessovaia 1, Dmitrii Y. Vlasov 2, Gennady P. Kopitsa 3,4 ,László Almásy 5 , Kirill V. Chistyakov 1, Elena G. Panova 1, Ekaterina Derkach 1 and Anastasiya Alekseeva 1 1 Institute of Earth Sciences, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, Russia; [email protected] (S.N.L.); [email protected] (K.V.C.); [email protected] (E.G.P.); [email protected] (E.D.); [email protected] (A.A.) 2 Biological Faculty, St. Petersburg State University, Universitetskaya nab., d. 7/9, 199034 St. Petersburg, Russia; [email protected] 3 B.P. Konstantinov Petersburg Nuclear Physics Institute NRC KI, Orlova roshcha, d. 1, 188300 Gatchina, Russia; [email protected] 4 I.V. Grebenshchikov Institute of Silicate Chemistry RAS, nab. Adm. Makarova, d. 2, 199155 St. Petersburg, Russia 5 Centre for Energy Research, Institute for Energy Security and Environmental Safety, Konkoly-Thege ut. 29–33, 1121 Budapest, Hungary; [email protected] * Correspondence: [email protected]; Tel.: +7-921-3314-598 Citation: Ganyushkin, D.A.; Abstract: For the Altai Mountains’ region, especially the arid southeastern part of the Russian Altai, Lessovaia, S.N.; Vlasov, D.Y.; Kopitsa, the data on glacier fluctuations in the Pleistocene and Holocene are still inconsistent. The study area G.P.; Almásy, L.; Chistyakov, K.V.; was the Kargy River’s valley (2288–2387 m a.s.l.), a location that is not currently affected by glaciation Panova, E.G.; Derkach, E.; Alekseeva, and the glacial history of which is poorly studied. -
GEOLOGICAL SOCIETY of HONG KONG NEWSLETTER North
Geological Society of Hong Kong Newsletter Vol.15, No.1 Special Issue GEOLOGICAL SOCIETY OF HONG KONG NEWSLETTER Volume 15, No.1 Special Issue – North Xinjiang Series, August 2009 (16 days), travelling within China (expect the We, a group of 23 GSHK members, just completed a 16-day field excursion to North Xinjiang. While we are still unexpected) and during this sensitive period in immersing in the beauty and uniqueness of the area, Miss Carina Khan has quickly wrapped up a report on ‘North Xinjiang, I would say our trip went by extremely, or Xinjiang Impressions’. even unexpectedly, smoothly with only ad hoc minor Miss Khan’s report is focused on her personal impressions hiccups. We did see intensive security measures in of the trip. More issues with details of geology and landscapes will follow. quite a few places. We had roadblocks, numerous Dr. Margie Chen identity checks etc. throughout the trip, but all that did not deter a single bit of our enthusiasm and North Xinjiang Impressions: excitement, as the sights, the experience were so 18 July – 2 August 2009 completely overwhelming. by Carina Khan Although we were already forewarned by Margie and We are happy to report that the 16-day 2009 North Felix to be prepared for extreme weather, the cold Xinjiang trip of the GSHK turned out to be a fantastic, part did surpass my expectations by at least some unforgettable, and probably one of the best trips that 10ºC. It was near 0ºC in the morning of Day 6, when many of us have ever had. -
Essentials of Endorheic Basins and Lakes: a Review in the Context of Current and Future Water Resource Management and Mitigation Activities in Central Asia
water Review Essentials of Endorheic Basins and Lakes: A Review in the Context of Current and Future Water Resource Management and Mitigation Activities in Central Asia Vadim Yapiyev 1,2,* ID , Zhanay Sagintayev 1, Vassilis J. Inglezakis 3, Kanat Samarkhanov 4 and Anne Verhoef 5 ID 1 School of Engineering, Nazarbayev University, Astana 010000, Kazakhstan; [email protected] 2 National Laboratory Astana, Nazarbayev University, Astana 010000, Kazakhstan 3 Environmental Science & Technology Group (ESTg), Chemical Engineering Department, School of Engineering, Nazarbayev University, Astana 010000, Kazakhstan; [email protected] 4 State Key Laboratory of Desert and Oasis Ecology, The XinJiang Institute of Ecology and Geography, Chinese Academy of Sciences, Urumqi 830011, China; [email protected] 5 Department of Geography and Environmental Science, The University of Reading, Reading RG6 6AB, UK; [email protected] * Correspondence: [email protected]; Tel.: +7-701-440-8516 Received: 31 July 2017; Accepted: 13 October 2017; Published: 21 October 2017 Abstract: Endorheic basins (i.e., land-locked drainage networks) and their lakes can be highly sensitive to variations in climate and adverse anthropogenic activities, such as overexploitation of water resources. In this review paper, we provide a brief overview of one major endorheic basin on each continent, plus a number of endorheic basins in Central Asia (CA), a region where a large proportion of the land area is within this type of basin. We summarize the effects of (changing) climate drivers and land surface–atmosphere feedbacks on the water balance. For the CA region, we also discuss key anthropogenic activities, related water management approaches and their complex relationship with political and policy issues. -
Xinjiang,China
+65 9230 4951 XINJIANG,CHINA ITINERARY Depart to Urumqi. DAY 1 Accommodation: 4* Chenmao Yilite hotel or equivalent Urumqi- Heavenly LakeFu YUN『 485KM,Drive time 5.5H』 DAY In the middle of Bogda Peak, 110 km (68miles) east of Urumqi, nestles HeavenlyLake.Covering 4.9 2 square kilometers (1.89 square miles),this crescent-shaped lake deserves its name, Pearl ofHeavenly Mountain (Tianshan Mountain).With melted snow as its source, Heavenly Lakeenjoys crystal water. The burning mountain is famous for its color, and the colorful bay in qitai county is also famous for its color. The rolling hills here are not colorful, but a red ochre made of sintered rock.You can hardly see any other colors when you look around.Every morning twilight, under the sun or sunset glow, as if still burning fiercely, magnificent rare, hence the name. Kalamali Established in April 1982, the reserve covers a total area of 17,000 square kilometers. The rare animals under state protection include Mongolian wild donkey, "pushi mustang", argali, gosling (yellow goat) and so on. Today, the main object of protection here - Mongolian wild donkeys have grown to more than 700, and antelope (yellow sheep) have more than 10,000. In addition, the rare wild animals with hoofs, such as wild camels, broncos, pan sheep and rabbit sun, birds such as the red falcon, golden eagle, great bustard, sand chicken, and reptiles such as the sand lizard, all increased in varying degrees. National highway 216, through this protected area, tourism is very convenient. Accommodation: 4* 黑金大酒店 或 蘊德大酒店 or equivalent Meals: Breakfast Fu Yun - Keketuohai Nationai Geological Park - Burjin『 330KM,Drive time 4.5H』 DAY Keketuohai means “green forests” in Kazakh and “blue day “ on Mongolian.Located in the eastern part 3 of Fuyun County,53KM from the county seat,it is called a fantasy land by visitors.Strange mountains along the irtysh River are characterized by varied granite peaks interpreting beautiful stories with Shezhong Mountains as the most stunning. -
Glacial Geomorphology of the Altai and Western Sayan Mountains, Central Asia
Journal of Maps ISSN: (Print) 1744-5647 (Online) Journal homepage: http://www.tandfonline.com/loi/tjom20 Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia Robin Blomdin, Jakob Heyman, Arjen P. Stroeven, Clas Hättestrand, Jonathan M. Harbor, Natacha Gribenski, Krister N. Jansson, Dmitry A. Petrakov, Mikhail N. Ivanov, Orkhonselenge Alexander, Alexei N. Rudoy & Michael Walther To cite this article: Robin Blomdin, Jakob Heyman, Arjen P. Stroeven, Clas Hättestrand, Jonathan M. Harbor, Natacha Gribenski, Krister N. Jansson, Dmitry A. Petrakov, Mikhail N. Ivanov, Orkhonselenge Alexander, Alexei N. Rudoy & Michael Walther (2016) Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia, Journal of Maps, 12:1, 123-136, DOI: 10.1080/17445647.2014.992177 To link to this article: http://dx.doi.org/10.1080/17445647.2014.992177 View supplementary material Published online: 11 Dec 2014. Submit your article to this journal Article views: 134 View related articles View Crossmark data Citing articles: 2 View citing articles Full Terms & Conditions of access and use can be found at http://www.tandfonline.com/action/journalInformation?journalCode=tjom20 Download by: [Stockholm University Library] Date: 02 March 2016, At: 15:30 Journal of Maps, 2016 Vol. 12, No. 1, 123–136, http://dx.doi.org/10.1080/17445647.2014.992177 SCIENCE Glacial geomorphology of the Altai and Western Sayan Mountains, Central Asia ∗ Robin Blomdina,b , Jakob Heymanb, Arjen P. Stroevenb, Clas Ha¨ttestrandb, Jonathan M. Harbora,b, Natacha