1 Chernivtsy „Yurii Fedkovych“ National University, Scientific Library, Ukraine 2 Department of Physical Geography and Natural Management, Chernivtsi “Yurii Fed’kovych” National
University, str. Kotsubynskogo 2, 58012, Chernivtsi, Ukraine
DOI:
10.4316/GEOREVIEW.2013.22.1.68
Pages:
11 - 17
Abstract:
Holocene landslide-gravitational seismodislocations in
the Kelmenetsky part of the Dniester area were formed due to strong
platform tremor Mw >4.5, which took place in between 1.000 BC and
XVI-XVII centuries. They are presented as different sizes fragments of
limestone oncoid cliff. The results of seismodislocation’s measurements, mechanism and
causes of their formation should be considered in seismicity of the
territory to protect the environment and population from serious
consequences of future earthquakes.
