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Batkun Peak
Batkun Peak ( bg, връх Баткун, vrah Batkun, ) is the peak rising to 881 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in the southeast foothills of on in , . It is situated in the west part of ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Fothergill Point
Fothergill Point is a low rocky coastal point northeast of Cape Worsley, forming the west side of the entrance to Mundraga Bay and the northeast side of the entrance to Odrin Bay on the Nordenskjöld Coast, on the east side of Graham Land, Antarctica. It was named by the UK Antarctic Place-Names Committee for Ian L. Fothergill, leader and meteorological assistant at the Falkland Islands Dependencies Survey station at Hope Bay Hope Bay ( Spanish: ''Bahía Esperanza'') on Trinity Peninsula, is long and wide, indenting the tip of the Antarctic Peninsula and opening on Antarctic Sound. It is the site of the Argentinian Antarctic settlement Esperanza Base, established ..., 1959–63. References SCAR Composite Antarctic Gazetteer Headlands of Graham Land Nordenskjöld Coast {{NordenskjöldCoast-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 ... [...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 Gaze ... [...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] |
Baldwin Peak
Baldwin Peak () is a peak between Lilienthal Glacier and Mount Berry in northern Graham Land. It was photographed by the Falkland Islands and Dependencies Aerial Survey Expedition in 1956–57 and mapped from these photos by the Falkland Islands Dependencies Survey. It was named by the UK Antarctic Place-Names Committee in 1960 for Thomas Scott Baldwin, American inventor of the vent opening which gives control and stability to parachutes. Further reading * Damien Gildea, Mountaineering in Antarctica: complete guide: Travel guide' External References Baldwin Peakon USGS website Baldwin Peakon AADC website Baldwin Peakon SCAR A scar (or scar tissue) is an area of fibrous tissue that replaces normal skin after an injury. Scars result from the biological process of wound repair in the skin, as well as in other organs, and tissues of the body. Thus, scarring is a na ... website satelight image of the Baldwin Peak arealong term updated weather for the Baldwin Peak ar ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Mikov Nunatak
Mikov Nunatak ( bg, Миков нунатак, Mikov nunatak, ) is the rocky ridge 1.35 km long in northwest–southeast direction and 590 m wide, rising to 750 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in the upper course of and linked on the northwest to on in |
Kableshkov Ridge
Kableshkov Ridge ( bg, Каблешков рид, ‘Kableshkov Rid’ \'ka-blesh-kov 'rid\) is the rocky ridge extending 4.5 km in east-southeast direction, 1.5 km wide and rising to 678 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 on in , . It is bounded by |
Gusla Peak
Gusla Peak ( bg, връх Гусла, vrah Gusla, ) is the peak rising to 842 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in the southeast foothills of on in , , at the NNW extremity of a narrow 3.9 ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Detroit Plateau
Detroit Plateau () is a major interior plateau of Graham Land on the Antarctic Peninsula, with heights between . Its northeast limit is marked by the south wall of Russell West Glacier, from which it extends some in a general southwest direction to Herbert Plateau. The plateau was observed from the air by Sir Hubert Wilkins on a flight of December 20, 1928. Wilkins named it Detroit Aviation Society Plateau after the society which aided in the organizing of his expedition, but the shortened form of the original name is approved. The north and east sides of the plateau were charted by the Falkland Islands Dependencies Survey in 1946–47. Dinsmoor Glacier flows east from the south edge of Detroit Plateau. Central plateaus of Graham Land North to south: * Laclavère Plateau * Louis Philippe Plateau * Detroit Plateau * Herbert Plateau * Foster Plateau * Forbidden Plateau * Bruce Plateau * Avery Plateau * Hemimont Plateau Hemimont Plateau ( bg, плато Хемимонт, plato ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Bulgaria
Bulgaria (; bg, България, Bǎlgariya), officially the Republic of Bulgaria,, ) is a country in Southeast Europe. It is situated on the eastern flank of the Balkans, and is bordered by Romania to the north, Serbia and North Macedonia to the west, Greece and Turkey to the south, and the Black Sea to the east. Bulgaria covers a territory of , and is the sixteenth-largest country in Europe. Sofia is the nation's capital and largest city; other major cities are Plovdiv, Varna and Burgas. One of the earliest societies in the lands of modern-day Bulgaria was the Neolithic Karanovo culture, which dates back to 6,500 BC. In the 6th to 3rd century BC the region was a battleground for ancient Thracians, Persians, Celts and Macedonians; stability came when the Roman Empire conquered the region in AD 45. After the Roman state splintered, tribal invasions in the region resumed. Around the 6th century, these territories were settled by the early Slavs. The Bulg ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
Zaychar Glacier
Zaychar Glacier ( bg, ледник Зайчар, lednik Zaychar, ) is the 7.5 km long and 2.7 km wide glacier on Nordenskjöld Coast in Graham Land, Antarctica. It drains the southeast slopes of Detroit Plateau, flowing east-southeastwards between Grivitsa Ridge and Kableshkov Ridge, and entering Odrin Bay in Weddell Sea 5 km northwest of Fothergill Point. The glacier is named after the settlement of Zaychar Zaychar ( bg, Зайчар ) is a village in Ruen Municipality, in Burgas Province, in southeastern Bulgaria. Zaychar Glacier on Graham Land in Antarctica Antarctica () is Earth's southernmost and least-populated continent. Situated alm ... in Southeastern Bulgaria. Location Zaychar Glacier is centred at . British mapping in 1978. Maps British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 64 60. Directorate of Overseas Surveys, UK, 1978. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarc ... [...More Info...] [...Related Items...] OR: [Wikipedia] [Google] [Baidu] |
