Belarus, country of eastern Europe. Until it became independent in 1991, Belarus, formerly known as Belorussia or White Russia, was the smallest of the three Slavic republics included in the Soviet Union (the larger two being Russia and Ukraine).

While Belarusians share a distinct ethnic identity and language, they never previously enjoyed unity and political sovereignty, except during a brief period in 1918. Belarusian history is thus less an isolable national narrative than a study of regional forces, their interplay, and their effects on the Belarusian people. The territory that is now Belarus underwent partition and changed hands repeatedly; as a result, much of the history of Belarus is inseparable from that of its neighbours. Since independence Belarus has retained close ties to its most dominant neighbour, Russia.
In 1999 the two countries signed the Union State Foundation Treaty, which aimed to create a politically integrated confederation with a common currency; the precise nature of the partnership, however, remained unclear well into the 21st century. The legacy of Belarus’s Soviet past also continued to manifest itself, both in the persistent prominence of communist political parties and in the country’s authoritarian style of government. About one-fifth of the population of Belarus resides in the centrally located capital, Minsk, a sprawling modern city that was almost entirely rebuilt after its near destruction in World War II.

Belarus is a landlocked country bordered by Lithuania and Latvia to the northwest, by Russia to the north and east, by Ukraine to the south, and by Poland to the west. In area, it is roughly one-third the size of its southern neighbour, Ukraine.

The topography of Belarus was largely shaped by glaciation during the Pleistocene Epoch (i.e., about 2,600,000 to 11,700 years ago). Much of the country consists of flat lowlands separated by low level-topped hills and uplands. The highest point, Dzyarzhynskaya Hill, is only 1,135 feet (346 metres) above sea level, and more than half the surface area of Belarus lies below 660 feet (200 metres).
The higher areas are formed by ridges of glacial morainic material dating from the Valday glaciation, the last advance of Pleistocene ice in eastern Europe. The largest of the ridges, the Belarusian Ridge, extends northeastward from the Polish border on the southwest to north of Minsk, where it widens into the Minsk Upland before turning eastward to link up with the Smolensk-Moscow Upland. Running transverse to the main Belarusian Ridge, the Ashmyany Upland, consisting of terminal moraines from the same glacial period, lies between Minsk and Vilnius, in neighbouring Lithuania. The surfaces of its ridges tend to be flat or gently rolling and covered by light sandy podzolic soils; they are largely cleared of their original forest cover.
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