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Roygos Ridge
Roygos Ridge ( bg, рид Ройгос, ‘Rid Roygos’ \'rid 'roy-gos\) is a mostly ice-covered ridge extending 9.6 km in a southeast-northwest direction, 3.2 km wide and rising to 1247 mReference Elevation Model of Antarctica.
Polar Geospatial Center. University of Minnesota, 2019
on the east coast of Darbel Bay, in , . It has rou ...
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Mount Lyttleton
Mount Lyttleton () is a conspicuous, almost entirely snow-covered mountain near the head of Cardell Glacier, on the west coast of Graham Land, Antarctica. It was photographed from the air by the Ronne Antarctic Research Expedition under Finn Ronne, 1947–48, and was named by the UK Antarctic Place-Names Committee in 1960 for Westcote R. Lyttleton (1877–1956), New Zealand Works Director of Triplex Safety Glass Triplex Safety Glass was a British brand of toughened glass and laminated glass. The marque is often seen on vehicle and aircraft windscreens. History The Triplex Safety Glass Company Ltd was founded in 1912 by Kent-born Reginald Delpech (30 Marc ..., London, who first introduced laminated safety glass for use in goggles in about 1912. References Mountains of Graham Land Graham Coast {{GrahamCoast-geo-stub ...
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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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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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Shanty Point
Shanty Point () is a small point within Darbel Bay, lying close west of the mouth of Cardell Glacier on the west coast of Graham Land. Photographed by Hunting Aerosurveys Ltd. in 1955–57, and mapped from these photos by the Falkland Islands Dependencies Survey (FIDS). So named by the United Kingdom Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and ... (UK-APC) because, when seen from a distance, a large rectangular boulder on the point has the appearance of a small hut with a crooked chimney. Headlands of Graham Land Loubet Coast {{LoubetCoast-geo-stub ...
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Mount Bain
Mount Bain () is a mountain, 2,090 m, standing between Hopkins and Erskine Glaciers on the west coast of Graham Land. It was named by the United Kingdom Antarctic Place-Names Committee The UK Antarctic Place-Names Committee (or UK-APC) is a United Kingdom government committee, part of the Foreign and Commonwealth Office, responsible for recommending names of geographical locations within the British Antarctic Territory (BAT) and ... (UK-APC) in 1958 for James S. Bain of London, who specialized in the development of polar and high altitude rations, with special emphasis on plastic vacuum packaging, between 1948 and 1956. Mountains of Graham Land Loubet Coast {{LoubetCoast-geo-stub ...
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Karia Peak
Karia Peak ( bg, връх Кария, vrah Kariya, ) is the rounded ice-covered peak rising to 1637 mReference Elevation Model of Antarctica.
Polar Geospatial Center. University of Minnesota, 2019
in the west foothills of Bruce Plateau on Loubet Coast in Graham Land, Antarctica. It has steep and partly ice-free west and south slopes, and surmounts Erskine Glacier to the south and a tributary to that glacier to the west and north. The peak is named after the ancient town of Karia in Northeastern Bulgaria.


Location

Karia Peak is located at , which is 5.6 km south-southeast of Mount Lyttleton, 10 km southwest of Purmerul Peak and 13.2 km north-northeast of Mount Bain. British mapping in 1976.


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Raizdos
Raizdos (Ῥαίζδος, the Latin form would be Rhaezdus) was possibly a king of the Odrysians in Thrace in the early 3rd century BC. He is attested in an inscription from Delphi as the father of Kotys III, who was king sometime between 276 and 267 BC (the date of the inscription). The date and the names suggest the possibility that Raizdos was the son of Kotys II, himself attested in an inscription from Athens dated to 330 BC (perhaps before he became king, if he is to be identified as a son of Seuthes III). Several scholars have considered the name "Raizdos" a variant orthography of "Roigos", a Thracian royal name found on 3rd-century BC coins and in a graffito in the Kazanlăk Tomb, naming "Roigos, son of Seuthes."P. Todorova, "Sin na Sevt III pogreban v Kazanlăškata grobnica," 5/16/2008 https://news.bg/culture ; Dana 2015: 250 Even if the two names are variant forms of the same name, it remains uncertain whether Kotys III's father Raizdos can be identified with Roigos, son ...
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Thracians
The Thracians (; grc, Θρᾷκες ''Thrāikes''; la, Thraci) were an Indo-European languages, Indo-European speaking people who inhabited large parts of Eastern Europe, Eastern and Southeast Europe, Southeastern Europe in ancient history.. "The Thracians were an Indo-European people who occupied the area between northern Greece, southern Russia, and north-western Turkey. They shared the same language and culture... There may have been as many as a million Thracians, diveded among up to 40 tribes." Thracians resided mainly in the Balkans (mostly Present (time), modern day Bulgaria, Turkey and Greece) but were also located in Anatolia, Anatolia (Asia Minor) and other locations in Eastern Europe. The exact origin of Thracians is unknown, but it is believed that proto-Thracians descended from a purported mixture of Proto-Indo-Europeans and Early European Farmers, arriving from the rest of Asia and Africa through the Asia Minor (Anatolia). The proto-Thracian culture developed int ...
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Cardell Glacier
Cardell Glacier () is a glacier draining the north slopes of Roygos Ridge and flowing northwestwards into Darbel Bay between Shanty Point and Panther Cliff, on the west coast of Graham Land, Antarctica. History Cardell Glacier was photographed by Hunting Aerosurveys Ltd in 1955–57, and mapped from these photos by the Falkland Islands Dependencies Survey. The glacier was named by the UK Antarctic Place-Names Committee in 1959 for John D.M. Cardell, English ophthalmic surgeon, who evolved the first satisfactory snow goggle design combining adequate protection and ventilation with safety and sufficient visual field. 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 Loubet Coast {{Lo ...
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