Icelandic Travel
LÝÐVELDIÐ ÍSLAND
Iceland has a population of 325,671 and a total area of 103,000 km2 (40,000 sq mi), which makes it the most sparsely populated country in Europe.
63°02' N, 25°01' W
Geologically, Iceland is part of the Mid-Atlantic Ridge, a ridge along which the oceanic crust spreads and forms new oceanic crust. This part of the mid-ocean ridge is located above a mantle plume, causing Iceland to be subaerial (above the surface of the sea). The ridge marks the boundary between the Eurasian and North American Plates, and Iceland was created by rifting and accretion through volcanism along the ridge.
242.724
Iceland is volcanically and geologically active. The interior consists mainly of a plateau characterised by sand and lava fields, mountains and glaciers, while many glacial rivers flow to the sea through the lowlands. 242.724 earthquakes recorded since 1996.
Iceland has a population of 325,671 and a total area of 103,000 km2 (40,000 sq mi), which makes it the most sparsely populated country in Europe.
63°02' N, 25°01' W
Geologically, Iceland is part of the Mid-Atlantic Ridge, a ridge along which the oceanic crust spreads and forms new oceanic crust. This part of the mid-ocean ridge is located above a mantle plume, causing Iceland to be subaerial (above the surface of the sea). The ridge marks the boundary between the Eurasian and North American Plates, and Iceland was created by rifting and accretion through volcanism along the ridge.
242.724
Iceland is volcanically and geologically active. The interior consists mainly of a plateau characterised by sand and lava fields, mountains and glaciers, while many glacial rivers flow to the sea through the lowlands. 242.724 earthquakes recorded since 1996.