CENTRAL SIBERIAN PLAIN ITS DISTINCTIVE FEATURES
The Central Siberian Plateau or more properly called also by the name of East Siberian Plateau, it is a bit higher than that of West Siberian Plateau and it forms a, the Yenisei rivers in this case forms the natural boundary between West Siberian lowland and the East Siberian highland. Eastward from the Yenisei, the ground elevations begin to rise and land becomes mountain and hilly terrain.
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The region is interlaced with broad fluvial lowlands along (0:46) the Siberian rivers. In the eastern section of Siberia, the mountains become high and much more rugged towards this region. The highest peak in the eastern part of the country is Gora Teng.
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