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Geomorphometric analysis of river basins in East European Russia using SRTM and ASTER GDEM data:200000 was created for the first time on the basis of a basin approach for the East of the Russian Plain European

Accumulation of 137Cs and 40K by plants of forest ecosystems: The estimation of plant species factor. Case study: Mixed forests of the east European plain in the center of the East European Plain. It has been found that shoots and roots' phytomass has the maximum

Accumulation of Cs-137 and K-40 by Plants of Forest Ecosystems: The Estimation of Plant Species Factor. Case Study: Mixed Forests of the East European Plain in the center of the East European Plain. It has been found that shoots and roots' phytomass has the maximum

Early Cambrian Syenite and Monzonite Magmatism in the Southeast of the East European Platform: Petrogenesis and Tectonic Setting aulacogen, in the southeastern part of the East European Platform (EEP). They have Early Cambrian ages

The impact of contemporary changes in climate and land use/cover on tendencies in water flow, suspended sediment yield and erosion intensity in the northeastern part of the Don River basin, SW European Russia regions of the East European (Russian)Plain. Sheet, rill and gully erosion occurring chiefly in snowmelt

Use of the data of remote sensing for definition of hydrophysical parameters of soils of the East and the South of the European Russia-physical parameters of main zonal soils of the East and the South of the European Russia. The system is based

Insights into the late Holocene vegetation history of the East European forest-steppe: case study Sudzha (Kursk region, Russia)© 2019, Springer-Verlag GmbH Germany, part of Springer Nature. Today, the East European forest

PALEOGEOGRAPHIC RESEARCHES OF LATE GLACIAL AND EARLY HOLOCENE IN THE NORTHWEST OF THE EAST EUROPEAN PLAINPALEOGEOGRAPHIC RESEARCHES OF LATE GLACIAL AND EARLY HOLOCENE IN THE NORTHWEST OF THE EAST EUROPEAN

The response of water flow, suspended sediment yield and erosion intensity to contemporary long-term changes in climate and land use/cover in river basins of the Middle Volga Region, European Russia developed geographic regions of the East European Plain within European Russia, where noticeable changes

Diatom complexes in the bottom sediments of rubskoe lake (The east european plain, Russia)
Diatom complexes in the bottom sediments of rubskoe lake (The east european plain, Russia)

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