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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

Assessment of anthropogenic pressure on the Volga federal district territory using river basin approach© 2020, MDPI AG. All rights reserved. The analysis of the geoecological state of basin geosystems

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

New opportunities of geoplanning in the rural area with the implementing of geoinformational technologies and remote sensing sensing. The sequence of scientific and technical transfer to basinal arrangement of the area

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