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English map of the Faroe Islands in 1806 The Faroe Islands as seen by the French navigator Yves-Joseph de Kerguelen-Trémarec in 1767. The Danish king tried to solve the problem by giving the Faroes to the courtier Christoffer Gabel (and later on his son, Frederick) as a personal feudal estate. However, the Gabel rule was harsh and repressive ...
The islands' endonym Føroyar, as well as its English name Faroe Islands (alt. Faeroe or the Faroes), derive from the Old Norse Færeyjar. [17] [18] [19] The second element oyar ('islands') is a holdover from Old Faroese; sound changes have rendered the word's modern form as oyggjar.
1988 – The Faroe Islands became a member of FIFA; 1989 – Faroe Islands is host for the Island Games. 1992 – On 6 October, the bank Sjóvinnubankin declares bankruptcy starting the worst economic depression in Faroese history.
This mass migration to the Faroe Islands shows a prior knowledge of the location of Norse settlements, furthering the claim of Grímur Kamban's settlement much earlier. While Kamban is recognized as the first Norse settler of the Faroe Islands (although his surname is of Gaelic origin), he actually re
Faroese people or Faroe Islanders (Faroese: føroyingar; Danish: færinger) are an ethnic group native to the Faroe Islands. [4] The Faroese are of mixed Norse and Gaelic origins. [ 5 ] About 21,000 Faroese live in neighbouring countries, particularly in Denmark , Iceland and Norway .
The Faroe Islands lie on the Eurasian Plate between Scotland, Norway and Iceland. The islands are of volcanic origin and are made up of three layers of basalt, with the top and bottom layers resembling each other. The age of this rock is between 54 and 58 million years, with the oldest material at the bottom.
History of the Faroe Islands by topic (5 C) C. Christian missionaries in the Faroe Islands (1 C, 1 P) D. Defunct organizations based in the Faroe Islands (1 C, 1 P) E.
Mykines belongs to the oldest part of the Faroe Islands and was formed about 60 million years ago. The Faroese basalt is divided into three phases of eruption: the lower and oldest, the middle, and the upper and youngest; the lowest formed by the eruption of low-viscosity lava through long fissures, forming flat volcanoes.