The relationship between sediment yield and drainage basin area the
basin area for rivers with undisturbed or slightly disturbed
basins. Rivers with intensively cultivated
The relationship between sediment yield and drainage basin area the
basin area for rivers with undisturbed or slightly disturbed
basins. Rivers with intensively cultivated
Cartographic model of river basins of European Russia in
area. Accuracy verification of identifying the
basin boundaries showed a good agreement of areal
Erosion processes of the forest and forest-steppe zones in the Eastern Part of the Russian Plain processes of soil and gully erosion in this region. The river
basin is taken as an
area unit (more than 3000
GEOMORPHOLOGIC POSITIONS OF DEBRIS FLOW BASINS IN THE LOVOZERSKIYE TUNDRY MOUNTAINOUS AREA, the debris flow
basins were divided into the following groups: 1) catchment
areas of temporary streams
Morphological typology of small watershed in river basins of cultivation area network and an average slope. An elementary catchment
area is used as an operating-territorial unit. Ward
Correlation of Upper Permian deposits in the Volga-Urals region and Kuznetsk basin, and to trace them in the neighboring
areas of the Angaraland - Kuznetsk
basin. The correlation is based
Erosion processes of the forest and forest-steppe zones in the Eastern Part of the Russian Plain processes of soil and gully erosion in this region. The river
basin is taken as an
area unit (more than 3000