Bigla Ridge
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Bigla Ridge
Bigla Ridge ( bg, text=хребет Бигла, italic=yes, ‘Hrebet Bigla’ \'hre-bet 'bi-gla\) is the rocky, partly ice-free ridge extending 19 km in northwest-southeast direction, 8.8 km wide and rising to 1644 m ( Stancheva Peak) on Foyn Coast, Antarctic Peninsula. The ridge is crescent-shaped facing southwest and surmounting Sleipnir Glacier to the northwest and Beaglehole Glacier to the southwest, with its southeast half forming Heros Peninsula. The feature is named after Bigla Peak in the Balkan Mountains, Bulgaria. Location Bigla Ridge is centred at . British mapping in 1974 and 1976. Maps * British Antarctic Territory: Graham Land. Scale 1:250000 topographic map. BAS 250 Series, Sheet SQ 19-20. London, 1974. * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 66 64. Directorate of Overseas Surveys, Tolworth, UK, 1976. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Commi ...
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Stancheva Peak
Stancheva Peak ( bg, връх Станчева, vrah Stancheva, ) is an ice-covered peak that forms the west extremity of Bigla Ridge on Foyn Coast, Antarctic Peninsula. It rises to 1644 mReference Elevation Model of Antarctica.
Polar Geospatial Center. University of Minnesota, 2019
and has precipitous rocky northwest, southeast and southwest slopes. It surmounts to the north and to the south. The feature is named after Kameliya Stancheva, participant in the 1996/97 Bulgarian Antarctic campaign, for her su ...
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Foyn Coast
The Foyn Coast () is that portion of the east coast of the Antarctic Peninsula between Cape Alexander and Cape Northrop. It was discovered in 1893 by a Norwegian expedition under Captain Carl Anton Larsen, who named it for Svend Foyn, a Norwegian whaler of Tønsberg whose invention of the grenade harpoon greatly facilitated modern whaling Whaling is the process of hunting of whales for their usable products such as meat and blubber, which can be turned into a type of oil that became increasingly important in the Industrial Revolution. It was practiced as an organized industry .... References Coasts of Graham Land {{FoynCoast-geo-stub ...
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Antarctic Peninsula
The Antarctic Peninsula, known as O'Higgins Land in Chile and Tierra de San Martín in Argentina, and originally as Graham Land in the United Kingdom and the Palmer Peninsula in the United States, is the northernmost part of mainland Antarctica. The Antarctic Peninsula is part of the larger peninsula of West Antarctica, protruding from a line between Cape Adams (Weddell Sea) and a point on the mainland south of the Eklund Islands. Beneath the ice sheet that covers it, the Antarctic Peninsula consists of a string of bedrock islands; these are separated by deep channels whose bottoms lie at depths considerably below current sea level. They are joined by a grounded ice sheet. Tierra del Fuego, the southernmost tip of South America, is about away across the Drake Passage. The Antarctic Peninsula is in area and 80% ice-covered. The marine ecosystem around the western continental shelf of the Antarctic Peninsula (WAP) has been subjected to rapid climate change. Over the past 50 ...
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Sleipnir Glacier
Sleipnir Glacier () is a glacier 10 nautical miles (18 km) long, flowing into the west side of Cabinet Inlet between Balder and Spur Points, on the east coast of Graham Land, Antarctica. The Vologes Ridge is in the central portion of the glacier. The feature was charted in 1947 by the Falkland Islands Dependencies Survey (FIDS), who named it after the horse of the mythological Norse god Odin. It was photographed from the air during 1947 by the Ronne Antarctic Research Expedition The Ronne Antarctic Research Expedition (RARE) was an expedition from 1947–1948 which researched the area surrounding the head of the Weddell Sea in Antarctica. Background Finn Ronne led the RARE which was the final privately sponsored exp ... (RARE) under Ronne. Maps * British Antarctic Territory: Graham Land. Scale 1:250000 topographic map. BAS 250 Series, Sheet SQ 19-20. London, 1974. * British Antarctic Territory. Scale 1:200000 topographic map. DOS 610 Series, Sheet W 66 64. Di ...
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Beaglehole Glacier
Beaglehole Glacier () is a glacier between Spur Point and Friederichsen Glacier on the east coast of Graham Land. It was named by the UK Antarctic Place-Names Committee after John Cawte Beaglehole, New Zealand historian of the Antarctic and biographer of Captain James Cook. See also * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natural phenomena that involve ice. Glaciology is an interdisciplinary Earth science that integrates geophysics, geology, physical geography, geomorphology, climato ... References * Glaciers of Graham Land Foyn Coast {{FoynCoast-glacier-stub ...
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Heros Peninsula
Heros Peninsula ( bg, полуостров Херос, poluostrov Heros, ) is the partly ice-free 8.9 km wide peninsula projecting from Foyn Coast, Antarctic Peninsula 13 km southeastwards into Cabinet Inlet. It ends in Spur Point to the southeast. The feature is named after the Thracian god Heros (the Thracian Rider). Location Heros Peninsula is centred at . British mapping in 1974. Maps * British Antarctic Territory: Graham Land. Scale 1:250000 topographic map. BAS 250 Series, Sheet SQ 19–20. London, 1974. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly upgraded and updated. References Heros Peninsula.SCAR Composite Antarctic Gazetteer. Bulgarian Antarctic Gazetteer.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 Min ...
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Balkan Mountains
The Balkan mountain range (, , known locally also as Stara planina) is a mountain range in the eastern part of the Balkan Peninsula in Southeastern Europe. The range is conventionally taken to begin at the peak of Vrashka Chuka on the border between Bulgaria and Serbia. It then runs for about , first in a south-easterly direction along the border, then eastward across Bulgaria, forming a natural barrier between the northern and southern halves of the country, before finally reaching the Black Sea at Cape Emine. The mountains reach their highest point with Botev Peak at . In much of the central and eastern sections, the summit forms the watershed between the drainage basins of the Black Sea and the Aegean. A prominent gap in the mountains is formed by the sometimes narrow Iskar Gorge, a few miles north of the Bulgarian capital, Sofia. The karst relief determines the large number of caves, including Magura, featuring the most important and extended European post-Palaeolithic cave ...
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Scientific Committee On Antarctic Research
The Scientific Committee on Antarctic Research (SCAR) is an interdisciplinary body of the International Science Council (ISC). SCAR coordinates international scientific research efforts in Antarctica, including the Southern Ocean. SCAR's scientific work is administered through several discipline-themed ''science groups''. The organisation has observer status at, and provides independent advice to Antarctic Treaty Consultative Meetings, and also provides information to other international bodies such as the Intergovernmental Panel on Climate Change (IPCC) and the United Nations Framework Convention on Climate Change (UNFCCC). History At the International Council of Scientific Unions (ICSU)’s Antarctic meeting held in Stockholm from 9–11 September 1957, it was agreed that a committee should be created to oversee scientific research in Antarctica. At the time there were 12 nations actively conducting Antarctic research and they were each invited to nominate one delegate to ...
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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 ...
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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 ...
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Ridges Of Graham Land
A ridge or a mountain ridge is a geographical feature consisting of a chain of mountains or hills that form a continuous elevated crest for an extended distance. The sides of the ridge slope away from the narrow top on either side. The lines along the crest formed by the highest points, with the terrain dropping down on either side, are called the ridgelines. Ridges are usually termed hills or mountains as well, depending on size. Smaller ridges, especially those leaving a larger ridge, are often referred to as spurs. Types There are several main types of ridges: ;Dendritic ridge: In typical dissected plateau terrain, the stream drainage valleys will leave intervening ridges. These are by far the most common ridges. These ridges usually represent slightly more erosion resistant rock, but not always – they often remain because there were more joints where the valleys formed or other chance occurrences. This type of ridge is generally somewhat random in orientation, often ...
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