Siberia's terrain is a study in contrasts, encompassing everything from vast wetlands to towering peaks. Here are its five principal landforms:
The world's largest plain: flat, low-lying, crisscrossed by the Ob and Irtysh rivers, blanketed in taiga and wetlands.
An elevated region (500–1,000 m) of rolling hills and plateaus, draped in dense taiga with patches of marsh and tundra.
Part of the Pacific Ring of Fire, featuring the Verkhoyansk, Chersky, and Stanovoy ranges. Rugged peaks, deep valleys, glaciers, and summits over 3,000 m.
The northern fringe: permafrost-locked, treeless plains with mosses, lichens, and dwarf shrubs stretching to the Arctic Ocean.
A complex southern massif of high ranges, intermountain basins, and glaciers, crowned by Mount Belukha (4,506 m), Siberia's highest point.
Together, these landscapes create one of Earth's most geographically diverse regions.