Siberia

Background

Siberia is a vast geographic region in northern Asia that extends from the Ural Mountains in the west to the Pacific Ocean in the east, with the Ural River often used as part of its southwestern boundary. It covers more than 13.1 million square kilometres, making up about three-quarters of Russia’s territory, while containing roughly a quarter of the country’s population. The region includes major cities such as Novosibirsk, Krasnoyarsk, and Omsk, and is known for its severe continental climate and long, cold winters.

In Russian affairs, Siberia matters because of its size, resource base, and transport connections across the country’s interior and eastern territories. The region is commonly treated as a major economic macro-region rather than a single political unit, and the Russian government divides it among several federal districts, including the officially named Siberian Federal District, parts of the Ural Federal District, and the Far Eastern Federal District. Its economic significance is tied to extractive industries, large-scale industry, and freight movement, with links to Pacific-facing logistics and export routes that connect inland production with external markets.

Historically, Siberia became part of Russian state territory through the conquest that began after the fall of the Khanate of Sibir in 1582 and ended with the annexation of Chukotka in 1778. Since then, it has remained a core part of Russia’s sovereign territory, though it is a geographic and historical concept rather than a fixed political entity with precise borders. In recent economic reporting, the region has been associated with declining coal extraction and exports, alongside reduced cargo throughput at Far Eastern ports, reflecting its continuing role in Russia’s industrial and trade performance.