Recent variability of erosion at the east of the Russian plane

Morpholithodynamic features of the shallow sandy shores by sea level fluctuation

Geomorphology and paleogeography of the Eurasian arctic shelf in the last interglacial epoch

Geomorphological and landscape indications of the neotectonic movements at the Kerch-Taman region

Transgressive changes in the Russian coast zone of Caspian Sea (by the aerial-cosmic images)

Evaluation of dynamic of South-Bovanenskaya structure surface (Middle Yamal) from 1949 to 1990

Morphological-genetic features of buried chalk karst at the East European Plane

Intensity estimation and features of horizontal channel deformations at the rivers of Permian Prikamye

Solid runoff and channel processes on the rivers of the basin of Don river

Desert varnish on terrasses and pediments of Maghtesh Ramon (Central Negev) and correlation with the age of surfaces

Geomorphological characteristics of Vistula spit of Baltic Sea

Morphology and origin of tropical hills of Indochina

A Mikulino buried balks was inherited from a Middle Pleistocene paleo-landform. It originated at the end of the Moscow glaciation and underwent a series of transformations from flat-bottom hollow or dell to a stable balks system at the interglacial time, then it was filled with sediments during the 1st half of the Valdai glaciation and completely buried during the 2nd half of glaciation, changing from linear hollow to circular flat-bottom depression and finally flat surface. The buried balks are not directly inherited by the present-day landform. The modern erosional form is simpler in pattern and shifted northeastward from the Mikulino one. However, under conditions of the Central Russian Highland the buried small erosional landforms occur rather close to the day surface and may influence indirectly the modern soil and topographic pattern.

Importance of recent vertical tectonic movements in channel formation of middle Belaya River (Central Bashkiria)

Morphotectonics of Upperrhine graben