EROSION PROCESSES AT THE NATURAL MONUMENT “UPPER AND LOWER SUDKI” IN THE BRYANSK

S. N. Kovalev; M. V. Veretennikova; E. F. Zorina

doi:10.15356/0435-4281-2007-4-62-69

EROSION PROCESSES AT THE NATURAL MONUMENT “UPPER AND LOWER SUDKI” IN THE BRYANSK

S. N. Kovalev, M. V. Veretennikova, E. F. Zorina

https://doi.org/10.15356/0435-4281-2007-4-62-69

Abstract

Gullies and balkas on the territory of Bryansk are growing nowadays. Some factors advances their growth: coursing the streets along slopes, using the linear erosion forms as dumping sites or spillways, building of garages alongside the gullies etc. The calculations based on hydrologic and geomorphologic characteristics of gully-balka network of Bryansk territory helped determining the boundary of natural monument "Upper and Lower Sudki (Balkas of Bryansk)".

Keywords

Erosion, erosion relief

About the Authors

S. N. Kovalev

Moscow State University, Moscow
Russian Federation
Geographical Department

M. V. Veretennikova

Moscow State University, Moscow
Russian Federation
Geographical Department

E. F. Zorina

Moscow State University, Moscow
Russian Federation
Geographical Department

References

1. Зорина Е.Ф., Ковалев С.Н., Никольская И.И. Методика определения интенсивности роста оврагов // Геоморфология. 1993. № 3. С. 66–75.

2. Определение основных расчетных гидрологических характеристик. СП 33-101-2003 / Госкомитет РФ по строительству и жилищно-коммунальному комплексу (ГОССТРОЙ России). М.: 2004.

Review

For citations:

Kovalev S.N., Veretennikova M.V., Zorina E.F. EROSION PROCESSES AT THE NATURAL MONUMENT “UPPER AND LOWER SUDKI” IN THE BRYANSK. Geomorfologiya. 2007;(4):62-69. https://doi.org/10.15356/0435-4281-2007-4-62-69