Trinaka Etna · Sicilië

KaartEilandenprovincia di Messina

★ 47 isole Eolie (Eolische Eilanden)

Eilanden UNESCOZeeVulkanisch
isole Eolie (Eolische Eilanden)
Foto: Wikimedia Commons · CC BY-SA

De Eolische Eilanden zijn een eilandengroep, genoemd naar Aiolos, enkele tientallen kilometers ten noorden van Sicilië.

Meer lezen (en)
Geography

The Aeolian Islands are 30 to 80 kilometres (19 to 50 mi) off the north coast of Sicily in the Tyrrhenian Sea. Vulcano is located closest to the Sicilian coast. Lipari and Salina follow to the north, Filicudi and Alicudi to the west, and Panarea and Stromboli to the northeast. In addition to these seven inhabited islands, there are a number of smaller, uninhabited islands and rocky cliffs, such as Basiluzzo, Strombolicchio, Dattilo and Lisca Bianca.
The largest island is Lipari (37.5 km2 [14.5 mi2]), followed by Salina (26.8 km2 [10.3 mi2]), Vulcano (21.2 km2 [8.2 mi2]), Stromboli (12.6 km2 [4.9 mi2]), Filicudi (9.5 km2 [3.7 mi2]) and Alicudi (5.2 km2 [2.0 mi2]). The smallest inhabited island, at 3.4 km2 (1.3 mi2), is Panarea. The highest elevation of the Lipari Islands is Monte Fossa delle Felci on Salina, which reaches a height of 962 m (3,156 ft).

Geology

The seven Aeolian Islands, covering an area of 1,600 km2 (620 sq mi), originated in the Tyrrhenian Basin, a great plain at the bottom of the Tyrrhenian Sea. Emissions of lava from depths of up to 3,600 m (11,800 ft) resulted in the formation of the Aeolian Islands, together with Ustica and a series of submarine volcanoes named Magnani, Vavilov, Marsili and Palinuro, as well as two that are unnamed.
The present shape of the Aeolian Islands is the result of volcanic activity over a period of 260,000 years. There are two active volcanoes – Stromboli and Vulcano. Steaming fumaroles and thermal waters are on most of the islands. The volcanic activity has also left the islands with a very fertile soil that is beneficial in the growth of natural flora.
Geologically the archipelago is defined as a volcanic arc. The origin of the Aeolian Islands is due to movement of the Earth's crust as a result of plate tectonics. The African continental shelf is in constant movement towards Europe. Its subduction underneath the Eurasian plate generates magma, which rises to the surface to form the volcanoes. The "Aeolian Arc" extends for more than 140 km (87 mi). It is a section of a larger area of geological instability across the Mediterranean region, caused by the collision of Africa and Europe, which includes Sicily, Calabria, and Campania together with Greece and the Aegean islands.

Administration

The islands form part of the Sicilian Metropolitan City of Messina. All the islands except Salina comprise the comune of Lipari within that province; Salina forms three separate comunes: Malfa, Leni and Santa Marina Salina.

Architectural control

Curbing urban development has been a key in preserving the Aeolian islands in a natural state. New buildings are severely restricted. Existing residences can be bought and restored but they must be constructed to resemble its whitewashed houses. Traditional houses consist of modular cubes constructed from indigenous building materials like stone, lava, pumice, and tufo. Almost all houses have a huge outdoor terrace, usually shaded by grape and flowering vines.

Van Wikipedia, CC BY-SA 4.0 · Lees het hele artikel

Foto’s
isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden) isole Eolie (Eolische Eilanden)

Van Wikimedia Commons. Tik op een foto voor auteur en licentie.

In het kort

★ UNESCO-werelderfgoed
Hoogte boven zee926 m

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