The Arctic

The Arctic

Three continents, Asia, North America, and Europe, reach into the Arctic Circle at their northernmost limits, almost entirely encircling the Arctic Ocean. Despite the region’s extraordinarily harsh climate, it has been inhabited for thousands of years by peoples such as the European Lapps, the Russian Nenet, and the North American Inuit, who draw a living from fishing, herding, and hunting. More recently, particularly in the Russian Arctic, opportunities to exploit oil and other mineral reserves have encouraged immigration. Pollution of the Arctic’s unique ecology and damage to the traditional lifestyles of many native peoples have been the unfortunate results of this activity, and international cooperation is needed to safeguard the future of the region.

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Large quantities of coal, oil, and natural gas are to be found in the basins of the Arctic Ocean, and in northern Canada, Alaska, and the Russian Federation. The cost and difficulty of extraction and, more recently, awareness of damage to the environment, have limited exploitation to coastal regions. The unfrozen waters have stocks of fish including cod, flounder, and haddock. Quotas have now been put in place to restrict the number of fish caught annually. Reindeer are herded in large numbers by many of the native Arctic peoples. Most grain and vegetables are imported from elsewhere.

The landscape

The Arctic Ocean comprises two large ocean basins divided by three submarine ridges, the greatest of which, the Lomonosov Ridge, is a huge underwater mountain range which has an average height of more than 10,000 ft (3000 m). The lands which encircle the Arctic Ocean are underlain by great shield areas of ancient rocks, which were heavily glaciated during the last Ice Age.

Facts of the Arctic

  • The Canadian Shield underlies almost all of the Canadian Arctic. It is a very stable plateau of ancient rock, now covered by glacial lakes and sediment, which supports tundra vegetation.
  • The Arctic Ocean is the world’s smallest ocean with a total area of 5,440,000 sq miles (15,100,000 sq km).
  • At a latitude of more than 75° N, the Arctic Ocean is almost permanently covered by pack ice, though high winds and the movement of the seas may cause the ice to crack and break up.
  • In the more southerly reaches of the Arctic, like Siberia, much of the land is covered by permafrost. In the summer, higher temperatures warm the frozen ground, causing a number of typical phenomena. These include solifluction, the fast downhill movement of top soil layers; freeze/thaw activity, which patterns the ground into regular polygonal shapes, and the formation of large domes with a frozen ice core, known as pingos.
  • A complex and ancient mountain system, extending from the Queen Elizabeth Islands to eastern Greenland was formed more than 245 million years ago.
  • Much of Greenland is covered by a massive ice sheet more than 650,000 sq miles (1,683,400 sq km) in extent. The weight of the ice has depressed the central land area to form a basin lying more than 1000 ft (300 m) below sea level. Only at the edges of the island is bare rock visible.
  • Iceland has five major glaciers, sustained by heavy snowfall. Parts of the ice cap cover active volcanoes, such as Bárdharbunga, which periodically erupt causing the melted ice to form a great lake at the glacier margins.
  • At the boundary of the Arctic ice shelves, sea water flows under the ice causing melting and forming crevasses on the surface. This eventually weakens blocks of ice which break away as icebergs. This process is known as calving.