RUSSIAN JOURNAL OF EARTH SCIENCES, VOL. 17, ES1002, doi:10.2205/2017ES000590, 2017


Figure 6. The secondary disturbances in the Derzig river valley. A – the rockfall (1 in Figure 2); B – the thrown from cliff boulder; the arrow shows the direction of its motion (2 in Figure 2); C – the crack of downfall at the valley slope (3 in Figure 2); D – the crack with traces of the thrown sand at the river bottom (4 in Figure 2).


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Citation: Ovsyuchenko A. N., E. A. Rogozhin, A. V. Marakhanov, Yu. V. Butanaev, A. S. Larkov, S. S. Novikov (2017), Environmental effects of the 2011–2012 Tuva earthquakes (Russia): Application of ESI 2007 macroseismic scale in the Siberian mountains, Russ. J. Earth Sci., 17, ES1002, doi:10.2205/2017ES000590.


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