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         Faroe Islands Geography:     more detail
  1. Village studies from the Faroe Islands, (University of Durham. Department of Geography. Occasional papers series, no. 12, 1971) by Brian Stephen John, 1971
  2. The Faroe Islands (North Atlantic Studies, 1)
  3. Geography, geology and climate of the Faeröes,: With the historical notes on the botanical investigation of these islands, by C. H Ostenfeld, 1901
  4. The algae-vegetation of the Faeröese coasts,: With remarks on the phyto-geography by Frederik Børgesen, 1905
  5. The Far Islands and Other Cold Places: Travel Essays of a Victorian Lady by Elizabeth Taylor, 1997-09-01

101. IGA - NatWest Island Games
and animal life. The geography and topography of the faroe Islandsmake transport and communication difficult. The faroese have
http://www.islandgames.net/content/members/faroes.html
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International Island Games Association FAROE ISLANDS LOCATION AND COMMUNICATION LINKS
The Faroe Islands are situated in the North Atlantic 430 km south-east of Iceland, 600 km west of Norway and a good 300 km north of Scotland. The Faroe Islands are in the same time zone as Britain. The distance to Copenhagen, the capital of Denmark, with which the Faroe Islands have constitutional links, is about 1,300 km. The islands are of volcanic origin and part of the North Atlantic basalt region stretching from Ireland to Greenland. The Ice Age glaciers formed an archipelago of mountains, deep valleys, narrow fords and straits. The basalt covers older geological strata which may contain oil and gas. The climate is typical oceanic: humid, changeable and windy. In Tórshavn the temperature in the coldest month averages 3°C and in the warmest 11°C. The shortest day is 5 hours and the longest 19’/2 hours. There are no woods, but plenty of grass. A mere 6% of the land is under cultivation while the rest is reserved for the grazing of 70,000 sheep and some cattle and horses. Birds are plentiful, especially sea-birds, but other animal life is sparse. The sea around the Faroe Islands is influenced by the meeting of the warm Gulf Stream and cold northern currents, rich in nutritional matter. This guarantees rather stable ocean temperatures, between 5° and 10°C, favouring fish and animal life.

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