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Anna Agatova, Roman Nepop, Vladimir Myglan, Valentin Barinov, Anna Tainik and Maja Filatova
Archaeological charcoal from ancient nomad iron-smelting furnaces collected in the highland southeastern Russian Altai has great potential as a material for tree ring analysis. Dendrochronological dating was applied to 355 viable samples (>80% of the 448...
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Otgonbayar Demberel, Bayarmaa Munkhbat, Batsuren Dorjsuren, Terry V. Callaghan, Bilguun Tsogoo, Valery A. Zemtsov, Otgontuya Shaarav, Erdenechimeg Gongor, Zolbayar Jargalsaikhan, Nemekhbayar Ganhuyag, Aldynay O. Khovalyg and Sergey N. Kirpotin
Mt. Munkhkhairkhan is the most crucial region for understanding climate and glaciation changes in Mongolia. This study investigated the relationship between glacial area changes and the climate elements of Mt. Munkhkhairkhan in the Mongolian-Altai Mounta...
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Peter Z. Revesz
An Old Hungarian Runic inscription from the Altai Mountains with 40 signs has posed some special challenges for decipherment due to several letter mix-ups and the use of a tamga sign, which is the first reported use of a tamga within this type of script....
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Jaroslav M. Gutak, Dmitry A. Ruban and Natalia N. Yashalova
Marine geoheritage comprises unique geological features of modern and ancient seas and oceans. The Russian Altai (southern Siberia) is a vast and geologically rich area, which was covered by a marginal sea of the Panthalassa Ocean in the Devonian. New ge...
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Dmitry V. Bantcev, Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Alexey A. Ekaykin, Arina N. Veres, Igor V. Tokarev, Natalya B. Shtykova and Tatiana A. Andreeva
The aim of this study was to determine the contribution of snow and glacial ice to the river fluxes, and to identify the type of ice formation in the Tsambagarav massif (the northwestern part of Mongolia). The main method for this study was isotopic anal...
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Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Dmitry V. Bantcev, Elena P. Kunaeva, Tatyana A. Andreeva, Anton V. Terekhov and Demberel Otgonbayar
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. T...
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Marc Jolivet, Philippe Boulvais, Laurie Barrier, Cécile Robin, Gloria Heilbronn, Julie Ledoyen, Quentin Ventroux, Yingying Jia, Zhaojie Guo and Elena A. Bataleva
The Late Mesozoic–Cenozoic topographic and climate evolution of Central Asia remains highly debated. The final retreat of the proto-Paratethys Sea from the western Tarim Basin is thought to correspond in time with the onset of tectonic uplift in th...
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Dmitry A. Ganyushkin, Kirill V. Chistyakov, Ilya V. Volkov, Dmitry V. Bantcev, Elena P. Kunaeva and Anton V. Terekhov
This research is based on multiyear in-situ observations, analysis of satellite and aerial imagery, meteorological data, and mass balance index calculations. Presently, 659 glaciers cover a total area of 322.1 km2. We identified four favorable, two neutr...
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Michael Walther, Avirmed Dashtseren, Ulrich Kamp, Khurelbaatar Temujin, Franz Meixner, Caleb G. Pan and Yadamsuren Gansukh
Understanding paleo?and recent environmental changes and the dynamics of individual drivers of water availability is essential for water resources management in the Mongolian Altai. Here, we follow a holistic approach to uncover changes in glaciers, perm...
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Dickson Cunningham
The Central Asian Orogenic Belt (CAOB) records multiple Phanerozoic tectonic events involving consolidation of disparate terranes and cratonic blocks and subsequent reactivation of Eurasia?s continental interior. The final amalgamation of the CAOB terran...
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