Russia Historical Geography

The Russian Federation stretches across much of the north of the supercontinent of Eurasia. Although it contains a large share of the world's Arctic and sub-Arctic areas, and therefore has less population, economic activity, and physical variety per unit area than most countries, the great area south of these still accommodates a great variety of landscapes and climates. The mid-annual temperature is +5.5°C (42°F). 

Most of the land consists of vast plains, both in the European part and the part of Asian territory that is largely known as Siberia. These plains are predominantly steppe (vast grasslands) to the south and heavily forested to the north, with tundra along the northern coast. The permafrost (areas of Siberia and the Far East) occupies more than half of the territory of Russia. Mountain ranges are found along the southern borders, such as the Caucasus (containing Mount Elbrus, Russia's and Europe's highest point at 5,642 m / 18,511 ft) and the Altai, and in the eastern parts, such as the Verkhoyansk Range or the volcanoes on Kamchatka. The more central Ural Mountains, a north-south range that form the primary divide between Europe and Asia, are also notable.

Russia has an extensive coastline of over 37,000 kilometers (23,000 mi) along the Arctic and Pacific Oceans, as well as more or less inland seas such as the Baltic, Black and Caspian seas. Some smaller bodies of water are part of the open oceans; the Barents Sea, White Sea, Kara Sea, Laptev Sea and East Siberian Sea are part of the Arctic, whereas the Bering Sea, Sea of Okhotsk and the Sea of Japan belong to the Pacific Ocean.