Abstract
This article is devoted to the development of the slope processes in the Oka river valley in the city of Kolomna. There are considered the modern ecological and engineering-geological condition of floodplain terraces in the city quarter of Kolychevo. The aim of the work was to study the geomorphology of landslide processes. There is considered the identification of the causes of landslides in the Oka river valley. The is considered the identification of representatives of fossil fauna of organogenic limestones of the left Bank of the Oka river to. In this paper, for the first time the «Protopopovskiy» landslide is described in the scientific literature.
Highlights
This article is devoted to the development of the slope processes
The a im of the work was to study the geomorphology of landslide processes
There is considered the identification of the causes of landslides
Summary
За несколько лет сформировался оползень на крутом левом берегу Оки на границе парка им. Рельеф оползневой массы представлен буграми, гребнями и валами ориентированными параллельно берегу реки. Вершина оползня (верхний край сползшей грунтовой массы) приурочена к верхней денудационной части склона с хорошо выраженным выпуклым мезорельефом. В «Протопоповском» оползне обнаружено несколько типов глыб: массивные блоки юрских глинистых сланцев
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