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Kudoglu Point
Kudoglu Point ( bg, нос Кудоглу, ‘Nos Kudoglu’ \'nos 'ku-do-glu\) is the sharp and low ice-free point projecting 150 m from the west side of Ioannes Paulus II Peninsula northwestwards into Barclay Bay, Livingston Island in Antarctica. It is named after the Bulgarian merchant and dedicated philanthropist Dimitar Kudoglu (1862-1940). Location Kudoglu Point is located at , which is 800 m northeast of Dreyfus Point and 2.28 km south of Mercury Bluff. British mapping in 1968, and Bulgarian in 2005, 2009 and 2017. Maps * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of Bulgaria, 2005. * L.L. IvanovAntarctica: Livingston Island and Greenwich, Robert, Snow and Smith Islands Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific C ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Ioannes Paulus II Peninsula
Ioannes Paulus II Peninsula ( bg, Полуостров Йоан Павел II, Poluostrov Yoan Pavel II, ) is an ice-covered peninsula on the north coast of Livingston Island in the South Shetland Islands, Antarctica that is bounded by Hero Bay to the east and Barclay Bay to the west. It extends 13 km in length in north–south direction and is 8 km wide. Its north extremity is formed by the ice-free Cape Shirreff, an area visited by early 19th century sealers. The peninsula's interior is occupied by Oryahovo Heights. The feature is named after Pope John Paul II (1920–2005) for his contribution to world peace and understanding among people. Location The peninsula is located at (British mapping in 1822 and 1968, Chilean in 1971, Argentine in 1980, Spanish mapping in 1991, and Bulgarian topographic survey Tangra 2004/05 and mapping in 2005 and 2009). See also * Oryahovo Heights * Cape Shirreff * Porlier Bay * Livingston Island Maps * L.L. Ivanov et al. Antarctica ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Barclay Bay
Barclay Bay () is a bay in Drake Passage between Cape Shirreff and Essex Point on the north side of Livingston Island, in the South Shetland Islands. Its head is fed by Etar Snowfield. The name appears on an 1825 chart of the British sealing expedition under James Weddell, and is now established in international usage. Maps South Shetland Islands.Scale 1:200000 topographic map No. 5657. DOS 610 – W 62 60. Tolworth, UK, 1968. * Islas Livingston y Decepción. Mapa topográfico a escala 1:100000. Madrid: Servicio Geográfico del Ejército, 1991. * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of Bulgaria, 2005. * L.L. IvanovAntarctica: Livingston Island and Greenwich, Robert, Snow and Smith Islands Scale 1:120000 topographic map. Troyan: Manfred Wörner Foundation, 2009. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientifi ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Livingston Island
Livingston Island (Russian name ''Smolensk'', ) is an Antarctic island in the Southern Ocean, part of the South Shetlands Archipelago, a group of Antarctic islands north of the Antarctic Peninsula. It was the first land discovered south of 60° south latitude in 1819, a historic event that marked the end of a centuries-long pursuit of the mythical ''Terra Australis Incognita'' and the beginning of the exploration and utilization of real Antarctica. The name Livingston, although of unknown derivation, has been well established in international usage since the early 1820s. Geography Livingston Island is situated in West Antarctica northwest of Cape Roquemaurel on the Antarctic mainland, south-southeast of Cape Horn in South America, southeast of the Diego Ramírez Islands (the southernmost land of South America), due south of the Falkland Islands, southwest of South Georgia Islands, and from the South Pole.L. IvanovGeneral Geography and History of Livingston Island.In ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctica
Antarctica () is Earth's southernmost and least-populated continent. Situated almost entirely south of the Antarctic Circle and surrounded by the Southern Ocean, it contains the geographic South Pole. Antarctica is the fifth-largest continent, being about 40% larger than Europe, and has an area of . Most of Antarctica is covered by the Antarctic ice sheet, with an average thickness of . Antarctica is, on average, the coldest, driest, and windiest of the continents, and it has the highest average elevation. It is mainly a polar desert, with annual precipitation of over along the coast and far less inland. About 70% of the world's freshwater reserves are frozen in Antarctica, which, if melted, would raise global sea levels by almost . Antarctica holds the record for the lowest measured temperature on Earth, . The coastal regions can reach temperatures over in summer. Native species of animals include mites, nematodes, penguins, seals and tardigrades. Where vegetation o ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Dreyfus Point
Dreyfus Point is a rounded low point on the west coast of Ioannes Paulus II Peninsula, western Livingston Island in the South Shetland Islands, Antarctica. The feature is named after Iván Dreyfus, an Air Force engineer who participated in the 1949 Chilean Antarctic Expedition. Location Dreyfus Point is located at which is 2 km north-northeast of Scesa Point, 3.15 km south-southwest of Mercury Bluff, 7 km south-southwest of Cape Shirreff Cape Shirreff is a prominent cape at the north end of the rocky peninsula which separates Hero Bay and Barclay Bay on the north coast of Livingston Island, in the South Shetland Islands of Antarctica. The cape was named by Edward Bransfield in ... and 800 m southwest of Kudoglu Point (British mapping in 1968 and Bulgarian in 2005 and 2009). Maps * L.L. Ivanov et al. Antarctica: Livingston Island and Greenwich Island, South Shetland Islands. Scale 1:100000 topographic map. Sofia: Antarctic Place-names Commission of B ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mercury Bluff
Mercury Bluff is a perpendicular bluff on Gerlovo Beach in the northwest of Ioannes Paulus II Peninsula, Livingston Island in the South Shetland Islands, Antarctica. The area was visited by early 19th century sealers. The feature is named after the British sealing ship ''Mercury'' under Captain Robert Wetherell that operated out of the nearby Shirreff Cove in 1820–21. Location The point is located at which is 3.9 km south-southwest of Cape Shirreff, 2.28 km north of Kudoglu Point and 12 km north-northeast of Rowe Point and 20.85 km east-northeast of Essex Point Essex Point is a point at the northwest end of Byers Peninsula, Livingston Island in the South Shetland Islands, Antarctica. It forms the west side of the entrance to Barclay Bay and the northeast side of the entrance to Svishtov Cove, and is su ... (British mapping in 1821 and 1968, Chilean in 1971, Argentine in 1980, Spanish in 1991, and Bulgarian in 2005 and 2009). Maps * L.L. Ivanov et al. ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Antarctic Place-names Commission
The Antarctic Place-names Commission was established by the Bulgarian Antarctic Institute in 1994, and since 2001 has been a body affiliated with the Ministry of Foreign Affairs of Bulgaria. The Commission approves Bulgarian place names in Antarctica, which are formally given by the President of the Republic according to the Bulgarian Constitution (Art. 98) and the established international practice. Bulgarian names in Antarctica Geographical names in Antarctica reflect the history and practice of Antarctic exploration. The nations involved in Antarctic research give new names to nameless geographical features for the purposes of orientation, logistics, and international scientific cooperation. As of 2021, there are some 20,091 named Antarctic geographical features, including 1,601 features with names given by Bulgaria.Bulgarian Antarctic Gazett ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Composite Gazetteer Of Antarctica
The Composite Gazetteer of Antarctica (CGA) of the Scientific Committee on Antarctic Research (SCAR) is the authoritative international gazetteer containing all Antarctic toponyms published in national gazetteers, plus basic information about those names and the relevant geographical features. The Gazetteer includes also parts of the International Hydrographic Organization (IHO) General Bathymetric Chart of the Oceans (GEBCO) gazetteer for under-sea features situated south of 60° south latitude. , the overall content of the CGA amounts to 37,893 geographic names for 19,803 features including some 500 features with two or more entirely different names, contributed by the following sources: {, class="wikitable sortable" ! Country ! Names , - , United States , 13,192 , - , United Kingdom , 5,040 , - , Russia , 4,808 , - , New Zealand , 2,597 , - , Australia , 2,551 , - , Argentina , 2,545 , - , Chile , 1,866 , - , Norway , 1,706 , - , Bulgaria , 1,450 , - , Ge ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Headlands Of Livingston Island
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 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
