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Sepúlveda Point
Sepúlveda Point () is the south entrance point of Recess Cove, in Charlotte Bay Charlotte Bay is a bay on the west coast of the Antarctic Peninsula indenting the west coast of Graham Land in a southeast direction for , between Reclus Peninsula and Cape Murray. Its head is fed by the glaciers Nobile, Bozhinov, Krebs, We ... on the Danco Coast. The feature was named "Punta Sepúlveda" by the Chilean Antarctic Expedition of 1952, after Teniente (Lt.) Hernan Sepúlveda Gore, of the patrol ship ''Lientur'' which worked in the area. References Headlands of Graham Land Danco Coast {{DancoCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Recess Cove
Recess Cove () is a cove 2.5 nautical miles (4.6 km) wide in the east side of Charlotte Bay, along the west coast of Graham Land. Surveyed by the Falkland Islands Dependencies Survey The British Antarctic Survey (BAS) is the United Kingdom's national polar research institute. It has a dual purpose, to conduct polar science, enabling better understanding of global issues, and to provide an active presence in the Antarctic on ... (FIDS), this cove forms a recess in the side of Charlotte Bay. Coves of Graham Land Danco Coast {{DancoCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Charlotte Bay
Charlotte Bay is a bay on the west coast of the Antarctic Peninsula indenting the west coast of Graham Land in a southeast direction for , between Reclus Peninsula and Cape Murray. Its head is fed by the glaciers Nobile, Bozhinov, Krebs, Wellman and Renard. The bay was discovered by Adrien de Gerlache during the 1897–99 Belgian Antarctic Expedition and named after Charlotte Dumeiz, the fiancée of Georges Lecointe, Gerlache's executive officer, hydrographer and second-in-command of the expedition. Charlotte Bay hut A Falkland Islands Dependency Survey (British Antarctic Survey from 1962) hut was built at Portal Point (), between Brabant Island and the Danco Coast. In the 1956–57 season, Wally Herbert, leader of a later British expedition, mapped the area from Hope Bay, and arrived at the Charlotte Bay hut for a scheduled pick up by the ''Shackleton''. With no radio, Herbert had no way of knowing that the ''Shackleton'' had hit an iceberg and was returning to the ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Danco Coast
The Danco Coast () is the portion of the west coast of the Antarctic Peninsula between Cape Sterneck and Cape Renard. This coast was explored in January and February 1898 by the Belgian Antarctic Expedition under Adrien de Gerlache, who named it for Lieutenant Emile Danco who died on the expedition. The coast is bordered by the Aguirre Passage which separates it from Lemaire Island. Places on the Danco Coast * Brabazon Point * Salvesen Cove Geology The Danco Coast Tectonic Block includes the Upper Permian-Triassic Trinity Peninsula Group, consisting of over 1000 m of metaturbidites folded during the Gondwanide orogeny. This group is overlain by the Lower Cretaceous Antarctic Peninsula Volcanic Group, with up to 2000 m of basaltic and andesitic lavas, tuffs and agglomerates, which were folded and faulted during the Tertiary. These two groups were intruded by the Berriasian- Cenomanian granite and gabbro sills of the Andean Instrusive Suite. A system of hypabbysa ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Graham Land
A headland, also known as a head, is a coastal landform, a point of land usually high and often with a sheer drop, that extends into a body of water. It is a type of promontory. A headland of considerable size often is called a cape.Whittow, John (1984). ''Dictionary of Physical Geography''. London: Penguin, 1984, pp. 80, 246. . Headlands are characterised by high, breaking waves, rocky shores, intense erosion, and steep sea cliff. Headlands and bays are often found on the same coastline. A bay is flanked by land on three sides, whereas a headland is flanked by water on three sides. Headlands and bays form on discordant coastlines, where bands of rock of alternating resistance run perpendicular to the coast. Bays form when weak (less resistant) rocks (such as sands and clays) are eroded, leaving bands of stronger (more resistant) rocks (such as chalk, limestone, and granite) forming a headland, or peninsula. Through the deposition of sediment within the bay and the erosion of t ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
