Field Course on the Chara River Country: Russia Institution

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Field course on the Chara river Country: Russia Institution: Tyumen State Oil and Gas University, Department of Earth Cryology; Institute of Earth Cryosphere of Russian Academy of Science (Siberian Department of Russian Academy of Science) Category: Room course combined with field course Level: PhD, master’s, bachelor’s Course title: Studying the interaction between the permafrost and glaciers Period: 06 July-07August Languages: English, Russian Course instructor: Vladimir S. Sheinkman, associate professor Contact person: Vladimir S. Sheinkman, associate professor E-mail: [email protected] Coordinator: scientific secretary Elena V. Ustinova, tel.: +7 3452 688 785 Short description: Annually, Department of Earth Cryology of Tyumen State Oil and Gas University jointly with Institute of Earth Cryosphere of Russian Academy of Science (Siberian Department of Russian Academy of Science) organizes field course on the Chara river (Zabaykalsky krai) for students. This site is unique thanks to the unique permafrost objects situated next to the Novaya Chara railroad station (three days to go by train from Moscow and two days from Tyumen) among the taiga at the foot of the Kodar ridge (Fig. 1). Fig. 1.The Chara river valley and the Kodar ridge In the cliffs of the river, there are outcrops of ice wedges. (Fig. 2). They are always perfectly seen thanks to the constant river undermining. Fig. 2.Ice wedges in the cliff if the right Chara river bank Besides, right beyond the outcrops, there are moraine fields of ancient glaciers and associated permafrost phenomena. It is possible to reach the headwater of the Sredny Sukan river at the foot of the Pik BAM mountain (3072 m), where the largest glaciers of the South part of Eastern Siberia are situated. These glaciers are specific due to the fact that they gradually become the permafrost component (fig.3, fig, 4). Fig 3. The Kodar ridge glaciers Fig 4. moraine fields of ancient glaciers at the foot of the Kodar ridge As a result, it is possible to give the course students the overview on all the aspect of forming and interaction of all the phenomena described above. Fig. 4. Course instructor Sheinkman with students at the field course on the Kodar ridge glaciers .

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