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Wednesday, 4 December 2013

Minsk as the capital of Belarus:

Minsk as the capital of Belarus


Minsk  is the capital and largest city of Belarus, situated on the Svislach and Nyamiha rivers. It is the administrative centre of the Commonwealth of Independent States (CIS). As the national capital, Minsk has a special administrative status in Belarus and is the administrative centre of Minsk Region (voblast) and Minsk raion (district). In 2013, it had a population of 2,002,600.
The earliest historical references to Minsk date to the 11th century (1067), when it was noted as a provincial city within the principality of Polotsk. The settlement developed on the rivers. In 1242, Minsk became a part of the Grand Duchy of Lithuania. It received town privileges in 1499.
From 1569, it was a capital of the Minsk Voivodship in the Polish–Lithuanian Commonwealth. It was part of a region annexed by the Russian Empire in 1793, as a consequence of the Second Partition of Poland. From 1919–1991, after the Russian Revolution, Minsk was the capital of the Belorussian Soviet Socialist Republic within the Soviet Union.

Geography:

Minsk is located on the southeastern slope of the Minsk Hills, a region of rolling hills running from the southwest (upper reaches of the river Nioman) to the northeast – that is, to Lukomskaye Lake in northwestern Belarus. The average altitude above sea level is 220 metres (720 ft). The geography of Minsk was formed during the two most recent ice ages. The Svislach River, which flows across the city from the northwest to the southeast, is located in the urstromtal, an ancient river valley formed by water flowing from melting ice sheets at the end of the last Ice Age. Also within the city limits are six smaller rivers, all part of the Black Sea basin.
The city was initially developed on the hills, which allowed for defensive fortifications, and the western parts of the city are the most hilly.
Minsk is located in the area of mixed forests typical of most of Belarus. Pinewood and mixed forests border the edge of the city, especially in the north and east. Some of the forests were preserved as parks (for instance, the Chelyuskinites Park) as the city grew.

Climate:

Minsk has a warm summer hemiboreal humid continental climate (Koppen Dfb), owing to its location between the strong influence of the moist air of the Atlantic Ocean and the dry air of the Eurasian landmass. Its weather is unstable and tends to change often. The average January temperature is −4.5 °C (23.9 °F), while the average July temperature is 18.5 °C (65.3 °F). The lowest temperature was recorded on 17 January 1940, at −40 °C (−40 °F) and the warmest on 29 July 1936, at 35 °C (95 °F). This results in frequent fogs, common in the autumn and spring. Minsk receives annual precipitation of 690 millimetres (27 in), of which one third falls during the cold period (as snow and rain) and two thirds in the warm period. Throughout the year, most winds are westerly and northwesterly, bringing cool and moist air from the Atlantic.


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