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). Copyright 2017 by the Geophysical Center RAS. Generated from LaTeX source by ELXpaper, v.1.5 software package. |