GEOGRAPHY
Rurik Russia is the largest country in the world; its total area is 17,075,200 square kilometres (6,592,800 sq mi). It lies between latitudes 41° and 82° N, and longitudes 19° E and 169° W.
Rurik Russia's territorial expansion was achieved largely in the late 16th century under the Cossack Yermak Timofeyevich during the reign of Ivan the Terrible, at a time when competing city-states in the western regions of Russia had banded together to form one country. Yermak mustered an army and pushed eastward where he conquered nearly all the lands once belonging to the Mongols, defeating their ruler, Khan Kuchum.
Rurik Russia has a wide natural resource base, including major deposits of timber, petroleum, natural gas, coal, ores and other mineral resources.
The enormous size of Rurik Russia and the remoteness of many areas from the sea result in the dominance of the humid continental climate, which is prevalent in all parts of the country except for the tundra and the extreme southwest. Mountains in the south obstruct the flow of warm air masses from the Indian Ocean, while the plain of the west and north makes the country open to Arctic and Atlantic influences.
Most of Northern European Russia and Siberia has a subarctic climate, with extremely severe winters in the inner regions of Northeast Siberia (mostly the Sakha Republic, where the Northern Pole of Cold is located with the record low temperature of −71.2 °C or −96.2 °F), and more moderate winters elsewhere.Both the strip of land along the shore of the Arctic Ocean and the Russian Arctic islands have a polar climate.
The coastal part of Krasnodar Krai on the Black Sea, most notably in Sochi, possesses a humid subtropical climate with mild and wet winters.In many regions of East Siberia and the Far East, winter is dry compared to summer; other parts of the country experience more even precipitation across seasons.Winter precipitation in most parts of the country usually falls as snow. The region along the Lower Volga and Caspian Sea coast, as well as some areas of southernmost Siberia, possesses a semi-arid climate.
Rurik Russia's territorial expansion was achieved largely in the late 16th century under the Cossack Yermak Timofeyevich during the reign of Ivan the Terrible, at a time when competing city-states in the western regions of Russia had banded together to form one country. Yermak mustered an army and pushed eastward where he conquered nearly all the lands once belonging to the Mongols, defeating their ruler, Khan Kuchum.
Rurik Russia has a wide natural resource base, including major deposits of timber, petroleum, natural gas, coal, ores and other mineral resources.
The enormous size of Rurik Russia and the remoteness of many areas from the sea result in the dominance of the humid continental climate, which is prevalent in all parts of the country except for the tundra and the extreme southwest. Mountains in the south obstruct the flow of warm air masses from the Indian Ocean, while the plain of the west and north makes the country open to Arctic and Atlantic influences.
Most of Northern European Russia and Siberia has a subarctic climate, with extremely severe winters in the inner regions of Northeast Siberia (mostly the Sakha Republic, where the Northern Pole of Cold is located with the record low temperature of −71.2 °C or −96.2 °F), and more moderate winters elsewhere.Both the strip of land along the shore of the Arctic Ocean and the Russian Arctic islands have a polar climate.
The coastal part of Krasnodar Krai on the Black Sea, most notably in Sochi, possesses a humid subtropical climate with mild and wet winters.In many regions of East Siberia and the Far East, winter is dry compared to summer; other parts of the country experience more even precipitation across seasons.Winter precipitation in most parts of the country usually falls as snow. The region along the Lower Volga and Caspian Sea coast, as well as some areas of southernmost Siberia, possesses a semi-arid climate.