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ﾃ四e Du Port
ﾃ四e du Port is one of the Kerguelen Islands in the southern Indian Ocean, situated in the Golfe des Baleiniers off the north coast of Grande Terre, the main island. It is the fourth largest island in the archipelago (43 km2). The highest point is an inactive volcano named ''K13'', at 340 metres. References * Andrﾃｩ Giret, Dominique Weis, Michel Grﾃｩgoire, Nadine Matielli, Bertrand Moine, Gilbert Michon, James Scoates, Sylvie Tourpin, Guillaume Delpech, Marie-Christine Gerbe, Sonia Doucet, Raynald Ethien et Jean-Yves Cotiﾂｫ L'archipel de Kerguelen : les plus vieilles ﾃｮles dans le plus jeune ocﾃｩan ﾂｻ ''Gﾃｩologues'', 2003, nﾂｰ137, p. 15-23 * Jean-Louis Chapuis, Yves Frenot et Marc Lebouvierﾂｫ Une gamme d'ﾃｮles de rﾃｩfﾃｩrences, un atout majeur pour l'ﾃｩvaluation des programmes de restauration dans l'archipel de Kerguelen ﾂｻ ''Rev. ﾃ営ol. (Terre Vie)'', supplﾃｩment 9, 2002. Port A port is a maritime facility comprising one or more wharves or l ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Kerguelen Islands
The Kerguelen Islands ( or ; in French commonly ' but officially ', ), also known as the Desolation Islands (' in French), are a group of islands in the sub-Antarctic constituting one of the two exposed parts of the Kerguelen Plateau, a large igneous province mostly submerged in the southern Indian Ocean. They are among the most isolated places on Earth, located more than from Madagascar. The islands, along with Adﾃｩlie Land, the Crozet Islands, Amsterdam and Saint Paul islands, and France's Scattered Islands in the Indian Ocean, are part of the French Southern and Antarctic Lands and are administered as a separate district. The main island, Grande Terre, is in area, about three quarters of the size of Corsica, and is surrounded by a further 300 smaller islands and islets, forming an archipelago of . The climate is harsh and chilly with frequent high winds throughout the year. The surrounding seas are generally rough and they remain ice-free year-round. There are no indig ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Indian Ocean
The Indian Ocean is the third-largest of the world's five oceanic divisions, covering or ~19.8% of the water on Earth's surface. It is bounded by Asia to the north, Africa to the west and Australia to the east. To the south it is bounded by the Southern Ocean or Antarctica, depending on the definition in use. Along its core, the Indian Ocean has some large marginal or regional seas such as the Arabian Sea, Laccadive Sea, Bay of Bengal, and Andaman Sea. Etymology The Indian Ocean has been known by its present name since at least 1515 when the Latin form ''Oceanus Orientalis Indicus'' ("Indian Eastern Ocean") is attested, named after Indian subcontinent, India, which projects into it. It was earlier known as the ''Eastern Ocean'', a term that was still in use during the mid-18th century (see map), as opposed to the ''Western Ocean'' (Atlantic Ocean, Atlantic) before the Pacific Ocean, Pacific was surmised. Conversely, Ming treasure voyages, Chinese explorers in the Indian Oce ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
French Southern Territories
The French Southern and Antarctic Lands (french: Terres australes et antarctiques franﾃｧaises, TAAF) is an Overseas Territory (french: Territoire d'outre-mer or ) of France. It consists of: # Adﾃｩlie Land (), the French claim on the continent of Antarctica. # Crozet Islands (), a group in the southern Indian Ocean, south of Madagascar. # Kerguelen Islands (), a group of volcanic islands in the southern Indian Ocean, southeast of Africa. # Saint Paul and Amsterdam Islands (), a group to the north of the Kerguelen Islands. # The Scattered Islands (), a dispersed group of islands around the coast of Madagascar. The territory is sometimes referred to as the French Southern Lands (french: Terres australes franﾃｧaises) or the French Southern Territories, usually to emphasize non-recognition of French sovereignty over Adﾃｩlie Land as part of the Antarctic Treaty System. The entire territory has no permanently settled inhabitants. Approximately 150 (in the winter) to 310 (in the summ ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Golfe Des Baleiniers
Golfe is a Prefecture located in the Maritime Region of Togo. The prefecture's seat is Lomﾃｩ which is also the administrative capital of the Togolese Republic. Cantons A canton is a type of administrative division of a country. In general, cantons are relatively small in terms of area and population when compared with other administrative divisions such as counties, departments, or provinces. Internationally, t ... within Golfe include: Amoutivﾃｩ, Bﾃｨ, Baguida, Agoﾃｨ-Nyivﾃｩ, Sanguﾃｩra, Togblﾃｩkopﾃｩ, Aflao-Gakli, Aflao-Sagbado, Lﾃｩgbassito, and Vakpossito References Prefectures of Togo Maritime Region {{Togo-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Grande-Terre (Kerguelen)
Grande-Terre Island (french: ﾃｮle de Grande-Terre / ﾃｮle de la Grande-Terre ; gcf, label=Antillean Creole, Gwantﾃｨ) is the name of the eastern-half of Guadeloupe proper, in the Lesser Antilles. It is separated from the other half of Guadeloupe island, Basse-Terre, by a narrow sea channel called ''Riviﾃｨre Salﾃｩe'' (in English, Salt River). Pointe de la Grande Vigie, in Grande-Terre, is the northernmost point of Guadeloupe island. To the east lies La Dﾃｩsirade, to the south lies Marie Galante Despite its name, Grande-Terre (literally "Large Land" in French) is smaller than Basse-Terre Island. It was called like that, in contrast with the much smaller Petite Terre Islands ("Small Land" Islands), two very small islands located about 10 km south-east of the Grande-Terre (see map to the left). Grande-Terre's indented coastline is surrounded by coral reefs and the island itself is a limestone plateau. Its surface is a series of rolling hills, white sand beaches and cliffs. The ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Inactive Volcano
A volcano is a rupture in the crust of a planetary-mass object, such as Earth, that allows hot lava, volcanic ash, and gases to escape from a magma chamber below the surface. On Earth, volcanoes are most often found where tectonic plates are diverging or converging, and most are found underwater. For example, a mid-ocean ridge, such as the Mid-Atlantic Ridge, has volcanoes caused by divergent tectonic plates whereas the Pacific Ring of Fire has volcanoes caused by convergent tectonic plates. Volcanoes can also form where there is stretching and thinning of the crust's plates, such as in the East African Rift and the Wells Gray-Clearwater volcanic field and Rio Grande rift in North America. Volcanism away from plate boundaries has been postulated to arise from upwelling diapirs from the core窶杜antle boundary, deep in the Earth. This results in hotspot volcanism, of which the Hawaiian hotspot is an example. Volcanoes are usually not created where two tectonic plates slide ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
