Minsk (Belarusian: ????? /m?insk/; Polish: Minsk; Russian: ????? /mi?sk/), is the capital and largest city in Belarus, situated on the Svislach and Niamiha rivers. Minsk is also a headquarters of the Commonwealth of Independent States (CIS). As the national capital, Minsk has a special administrative status in Belarus and is also the administrative centre of Minsk voblast (province) and Minsk raion.
The earliest references to Minsk date to the 11th century (1067). In 1242, Minsk became a part of the Grand Duchy of Lithuania, and it received its town privileges in 1499. From 1569, it was a capital of the Minsk Voivodship in the Polish-Lithuanian Commonwealth. It was annexed by Russia in 1793, as a consequence of the Second Partition of Poland. From 1919–1991, Minsk was the capital of the Byelorussian SSR.********************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 the Lukomskaye lake in northwestern Belarus. The average altitude above sea level is 220 m. 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 urstrohmtal, an ancient river valley formed by water flowing from melting ice sheets at the end of the last Ice Age. Minsk was initially founded on the hills. However, in the 20th century, it grew to include the relatively flat plains in the southeast. The western parts of the city are the most hilly.**************************Minsk is located in the area of mixed forests typical for most of Belarus. Pinewood and mixed forests are still present at the edge of the city, especially in the north and east. Some of the forests were transformed into parks (for instance, the Chelyuskinites Park) as the city grew.
**********************
Minsk has a moderate climate, 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, however, unstable and tends to change often. The average January temperature is -6.1 Celsius (21 °F), while the average July temperature is 17.8 °C (64 °F). The lowest temperature was recorded on 17 January, 1940 (-40 °C) (-40 °F) and the warmest on 29 July, 1936 (35 °C) (95 °F). The air is often moist, with humidity levels at 80-90%,especially during the cold season. There are on average 135 humid days a year, compared with only 6 dry days. This results in frequent fogs, common in the autumn and spring. Minsk receives annual precipitation of 646 mm (25.4 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.****************After World War II, Minsk was rebuilt, but not reconstructed. The historical centre was replaced in the 1940s and 1950s by Stalinist architecture, which favoured grand buildings, broad avenues and wide squares. Subsequently, the city grew rapidly as a result of massive industrialisation. Since the 1960s Minsk's population has also grown apace, reaching 1 million in 1972 and 1.5 million in 1986. This rapid population growth was primarily driven by mass migration of young, unskilled workers from rural areas of Belarus, as well as by migration of skilled workers from other parts of the Soviet Union. To house the expanding population, Minsk spread beyond its historical boundaries. Its surrounding villages were absorbed and rebuilt as mikroraions, districts of high-density apartment housing.**********************hroughout the 1990s, after the fall of Communism, the city continued to change. As the capital of a newly-independent country, Minsk quickly acquired the attributes of a major city. Embassies were opened, and a number of Soviet administrative buildings became government centers. During the early and mid-1990s, Minsk was hit by an economic crisis and many development projects were halted, resulting in high unemployment and underemployment. Since the late 1990s, there have been improvements in transport and infrastructure, and a housing boom has been underway since 2002. On the outskirts of Minsk, new mikroraions of residential development have been built. Metro lines have been extended, and the road system (including the Minsk ring road) has been improved. Owing to the small size of the private sector in Belarus, most development has so far been financed by the government.
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Basic Dark T-Shirt
The classic heavyweight t-shirt. Tagless design for ultimate comfort. Pre-shrunk, 6.1 ounce 100% cotton. Double-needle stitched bottom and sleeve hems. Loose, classic fit, wears well on anyone. (note: Brown version has a tag). Imported.
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Wyvern-passant Minsk
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Minsk (Belarusian: ????? /m?insk/; Polish: Minsk; Russian: ????? /mi?sk/), is the capital and largest city in Belarus, situated on the Svislach and Niamiha rivers. Minsk is also a headquarters of the Commonwealth of Independent States (CIS). As the national capital, Minsk has a special administrative status in Belarus and is also the administrative centre of Minsk voblast (province) and Minsk raion.
The earliest references to Minsk date to the 11th century (1067). In 1242, Minsk became a part of the Grand Duchy of Lithuania, and it received its town privileges in 1499. From 1569, it was a capital of the Minsk Voivodship in the Polish-Lithuanian Commonwealth. It was annexed by Russia in 1793, as a consequence of the Second Partition of Poland. From 1919–1991, Minsk was the capital of the Byelorussian SSR.********************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 the Lukomskaye lake in northwestern Belarus. The average altitude above sea level is 220 m. 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 urstrohmtal, an ancient river valley formed by water flowing from melting ice sheets at the end of the last Ice Age. Minsk was initially founded on the hills. However, in the 20th century, it grew to include the relatively flat plains in the southeast. The western parts of the city are the most hilly.**************************Minsk is located in the area of mixed forests typical for most of Belarus. Pinewood and mixed forests are still present at the edge of the city, especially in the north and east. Some of the forests were transformed into parks (for instance, the Chelyuskinites Park) as the city grew.
**********************
Minsk has a moderate climate, 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, however, unstable and tends to change often. The average January temperature is -6.1 Celsius (21 °F), while the average July temperature is 17.8 °C (64 °F). The lowest temperature was recorded on 17 January, 1940 (-40 °C) (-40 °F) and the warmest on 29 July, 1936 (35 °C) (95 °F). The air is often moist, with humidity levels at 80-90%,especially during the cold season. There are on average 135 humid days a year, compared with only 6 dry days. This results in frequent fogs, common in the autumn and spring. Minsk receives annual precipitation of 646 mm (25.4 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.****************After World War II, Minsk was rebuilt, but not reconstructed. The historical centre was replaced in the 1940s and 1950s by Stalinist architecture, which favoured grand buildings, broad avenues and wide squares. Subsequently, the city grew rapidly as a result of massive industrialisation. Since the 1960s Minsk's population has also grown apace, reaching 1 million in 1972 and 1.5 million in 1986. This rapid population growth was primarily driven by mass migration of young, unskilled workers from rural areas of Belarus, as well as by migration of skilled workers from other parts of the Soviet Union. To house the expanding population, Minsk spread beyond its historical boundaries. Its surrounding villages were absorbed and rebuilt as mikroraions, districts of high-density apartment housing.**********************hroughout the 1990s, after the fall of Communism, the city continued to change. As the capital of a newly-independent country, Minsk quickly acquired the attributes of a major city. Embassies were opened, and a number of Soviet administrative buildings became government centers. During the early and mid-1990s, Minsk was hit by an economic crisis and many development projects were halted, resulting in high unemployment and underemployment. Since the late 1990s, there have been improvements in transport and infrastructure, and a housing boom has been underway since 2002. On the outskirts of Minsk, new mikroraions of residential development have been built. Metro lines have been extended, and the road system (including the Minsk ring road) has been improved. Owing to the small size of the private sector in Belarus, most development has so far been financed by the government.
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