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Smilyan Bastion
Smilyan Bastion ( bg, Смилянски рид, ‘Smilyanski Rid’ \'smi-lyan-ski 'rid\) is the rounded ice-covered buttress extending 13 km in southeast-northwest direction and 16 km in south-southwest to north-northeast direction, and rising to 1525 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 on the west side of on in , |
Smilyan
Smilyan (Bulgarian: Смилян) is a village in Smolyan Municipality, located in the Smolyan Province of southern Bulgaria. It is located 176.862 km from Sofia and the village covers an area of 29.248 km2. As of 2019, the village had a population of 1583 people. It is known for its premium quality beans, of which limited quantities are produced. Honours Smilyan Bastion on Loubet Coast, 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 contine ... is named after the village. References Villages in Smolyan Province {{Smolyan-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mountains Of Graham Land
A mountain is an elevated portion of the Earth's crust, generally with steep sides that show significant exposed bedrock. Although definitions vary, a mountain may differ from a plateau in having a limited summit area, and is usually higher than a hill, typically rising at least 300 metres (1,000 feet) above the surrounding land. A few mountains are isolated summits, but most occur in mountain ranges. Mountains are formed through tectonic forces, erosion, or volcanism, which act on time scales of up to tens of millions of years. Once mountain building ceases, mountains are slowly leveled through the action of weathering, through slumping and other forms of mass wasting, as well as through erosion by rivers and glaciers. High elevations on mountains produce colder climates than at sea level at similar latitude. These colder climates strongly affect the ecosystems of mountains: different elevations have different plants and animals. Because of the less hospitable terrain and ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Composite Antarctic Gazetteer
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 , - , G ... [...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] |
Quervain Peak
Quervain Peak () is a peak in the central part of the Boyle Mountains in Graham Land, Antarctica. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1956–59, it was named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Alfred de Quervain, a Swiss glaciologist who in 1909 first applied photogrammetric methods to the measurement of surface glacier A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires dis ... flow. References Mountains of Graham Land Loubet Coast {{LoubetCoast-geo-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hayduta Buttress
Hayduta Buttress ( bg, рид Хайдута, ‘Rid Hayduta’ \'rid hay-'du-ta\) is the rounded, mostly ice-covered buttress 13.5 km long in E-W direction and 7.5 km wide, rising to 1287 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 on the west side of Hemimont Plateau on Fallières Coast in , . The feature ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Armula Peak
Armula Peak ( bg, връх Армула, vrah Armula, ) is the ice-covered peak rising to 1142 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in the west foothills of Hemimont Plateau, in , . The feature has steep and partly ice-free south slopes, and surmounts |
Klebelsberg Glacier
Klebelsberg Glacier () is a glacier, long and wide, situated at the south side of Finsterwalder Glacier and flowing from Hemimont Plateau northwestward between Armula Peak and Smilyan Bastion on Graham Land, Antarctica, toward the head of Lallemand Fjord. With Finsterwalder Glacier and Haefeli Glacier, its mouth merges with Sharp Glacier where the latter enters the fjord. It was first surveyed from the plateau in 1946–47 by the Falkland Islands Dependencies Survey, and named by them for Raimund von Klebelsberg ''Raimund'' is thought to be a variant of the name Raymond. Raimund may refer to: * Ferdinand Raimund (1790-1836), Austrian actor and dramatist * Raimund Theater, a theatre in the Mariahilf district of Vienna, Austria People with the given name R ..., an Austrian glaciologist. References Glaciers of Loubet Coast {{LoubetCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Hemimont Plateau
Hemimont Plateau ( bg, плато Хемимонт, plato Hemimont, ) is the long and narrow ice-covered plateau of elevation about 1600 m in southern Graham Land, Antarctica bordering Avery Plateau on the north. It is situated midway between Loubet Coast and Fallières Coast on the west, and Bowman Coast on the east, and extends 100 km from the heads of Finsterwalder Glacier and Demorest Glacier on the north to Neny Glacier on the south. Its higher southern part rises to 1862 m and features McLeod Hill (1741 m), Beacon Hill (1770 m) and Armadillo Hill (1775 m).Reference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 The plateau is named after the |
Sharp Glacier
Sharp Glacier is a glacier flowing north to the head of Lallemand Fjord, close east of the Boyle Mountains, in Graham Land. Mapped by Falkland Islands Dependencies Survey (FIDS) from surveys and air photos, 1948–59. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Robert P. Sharp Robert Phillip Sharp (24 June 1911 – 25 May 2004) was an American geomorphologist and expert on the geological surfaces of the Earth and the planet Mars. Sharp served as the chairman of the Division of Geological Sciences at California Ins ..., American geologist who has undertaken numerous studies on glaciers and their flow. References * Glaciers of Loubet Coast {{LoubetCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Forel Glacier
Forel Glacier () is a glacier wide and long, flowing southwest into Blind Bay, on the west coast of Graham Land, Antarctica. It was first roughly surveyed in 1936 by the British Graham Land Expedition under John Rymill. Its lower reaches were surveyed in 1949 by the Falkland Islands Dependencies Survey, and the glacier named by them for François-Alphonse Forel François-Alphonse Forel (February 2, 1841 – August 7, 1912) was a Swiss physician and scientist who pioneered the study of lakes, and is thus considered the founder, and the Father of limnology.Prof. F. A. Forel. Nature 89, 638–639 (1912). ..., a noted Swiss glacier physicist and author, and first President of the International Commission of Glaciers in 1894. References Glaciers of Loubet Coast {{LoubetCoast-glacier-stub ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
