Faroe Islands

The population of the Faroe Islands is largely descended from Viking settlers who arrived in the 9th century. The islands have been connected politically to Denmark since the 14th century. A high degree of self-government was granted the Faroese in 1948, who have autonomy over most internal affairs while Denmark is responsible for justice, defense, and foreign affairs. The Faroe Islands are not part of the European Union.

Geography of Faroe Islands

The Land

Composed of volcanic rocks covered by a thin layer of moraine or peat soil, the islands are high and rugged with perpendicular cliffs—the highest at Mount Slaettara (Slaettaratindur; 2,894 feet [882 metres]) on Eystur Island—and flat summits separated by narrow ravines. The coasts are deeply indented with fjords, and the narrow passages between islands are agitated by strong tidal currents.

The climate is oceanic and mild, with little variation in temperature and frequent fog and rain; annual precipitation totals 60 inches (1,600 mm). The warm North Atlantic Current keeps the harbours free of ice. Natural vegetation is moss, grass, and mountain bog. The islands are naturally treeless because of the cool summers, strong westerly winds, and frequent gales, but some hardy trees have been planted in sheltered plantations. There are no toads, reptiles, or indigenous land mammals; hares, rats, and mice came on ships. Seabirds are numerous and were in earlier times economically important—the puffin as food and the eider for feathers.

Disclaimer

This is not the official site of this country. Most of the information in this site were taken from the U.S. Department of State, The Central Intelligence Agency, The United Nations, [1],[2], [3], [4], [5],[6], [7], [8], [9], [10], [11], [12], [13], [14],[15], [16], [17], [18], [19], [20], [21], [22], [23], [24],[25], [26], [27], [28], [29], [30],[31], [32], [33], [34], and the [35].

Other sources of information will be mentioned as they are posted.