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Concept
Galite Islands
Summary
The Galite Islands (Tunisian Arabic: جالطة Jalita, French: La Galite, Italian: La Galita) are a rocky group of islands of volcanic origin that belong to Bizerte Governorate, northern Tunisia. They are located northwest of Cape Serrat, the closest point of the Tunisian mainland coast, from which they are separated by the Galite Channel, and almost north-by-northeast of the city of Tabarka, and south of Cape Spartivento in the south of Sardinia. The islands of the group sit atop Banc de Galite.
The centrally situated main island La Galite is long east-west, and up to wide in the east. The area of the group is , most of which La Galite accounts for. The main island has 200m high cliffs and is accessible only in the south on the bay Escueil de Pasque. A few fishermen's families live on the island. The highest peak at 391m is Bout de Somme (Grand Sommet), which is topped by a yellow lookout tower. Piton de l'Es', a prominent cone-shaped peak close to the most southeasterly point of the island, is 360m high.
Besides the main island La Galite, there are two groups of islets or rocks, which are all inaccessible.
The Galitons de l'Ouest, or West Galitons, are southwest of the main island. They consist of the second largest and third largest islands of the Galite Islands, 158m high Le Galiton (area 0.4 km2) and 137m high La Fauchelle, immediately southeast of Le Galiton. On the peak of Le Galiton is a lighthouse, 14m high. In 1980, the Ministry of Agriculture declared Le Galiton a natural reserve, to protect the Mediterranean monk seals.
The smaller Galitons de l'Est, or East Galitons, also called Les Chiens or The Dogs, are at a distance between 1 and northeast of the main island. This group consists of three rocks, which are, from north to south, Gallo, Pollastro and Gallina (meaning "rooster", "chicken" and "hen" in Italian). Gallo is the largest of the three and is 119 m high.
About to the southwest are the Sorelle Rocks, or Écueil des Sorelles, which consist of two shallow rocky patches.
Official source
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