Perunika Glacier
Perunika Glacier ( bg, ледник Перуника, lednik Perunika, ) is an 8 km long and 3 km wide (average) roughly crescent-shaped glacier in eastern Livingston Island in the South Shetland Islands, Antarctica situated east of Pimpirev Glacier, south of Saedinenie Snowfield, southwest of Kaliakra Glacier, west of Huron Glacier, and north of Balkan Snowfield and the head of Huntress Glacier."Perunika Glacier " SCAR Its head is bounded by to the south-southwest, [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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]   |
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Bowles Ridge
Bowles Ridge ( bg, хребет Боулс, hrebet Bouls, ) is the central ridge of eastern Livingston Island. The ridge extends 6.5 km in the east-west direction and is 1.5 km wide. The summit of the ridge is Mount Bowles which rises to 822m and is located 9.77 km northwest of Great Needle Peak, 6.08 km north by west of Mount Friesland, 8.77 km east-northeast of St. Kliment Ohridski base and 9.25 km south by west of Miziya Peak. ''Bowles Ridge'' is bounded by Kaliakra Glacier and Struma Glacier to the north, by Perunika Glacier to the west and southwest and by Huron Glacier to the southeast and east. It is linked to Friesland Ridge of the Tangra Mountains by Wörner Gap, to Hemus Peak by Dimov Gate, and to Melnik Ridge by Yankov Gap. The ridge is crossed by Omurtag Pass and Pirdop Gate. The feature takes its name from Mount Bowles Mount Bowles is an ice-covered mountain high, the summit of Bowles Ridge in the central part of eastern ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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List Of Glaciers In The Antarctic
There are many glaciers in the Antarctic. This set of lists does not include ice sheets, ice caps or ice fields, such as the Antarctic ice sheet, but includes glacial features that are defined by their flow, rather than general bodies of ice. The lists include outlet glaciers, valley glaciers, cirque glaciers, tidewater glaciers and ice streams. Ice streams are a type of glacier and many of them have "glacier" in their name, e.g. Pine Island Glacier. Ice shelves are listed separately in the List of Antarctic ice shelves. For the purposes of these lists, the Antarctic is defined as any latitude further south than 60° (the continental limit according to the Antarctic Treaty System). List by letters * List of glaciers in the Antarctic: A–H * List of glaciers in the Antarctic: I–Z See also * List of Antarctic and subantarctic islands * List of Antarctic ice rises * List of Antarctic ice shelves * List of Antarctic ice streams * List of glaciers * List of subantar ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Slavic Mythology
Slavic mythology or Slavic religion is the religious beliefs, myths, and ritual practices of the Slavs before Christianisation, which occurred at various stages between the 8th and the 13th century. The South Slavs, who likely settled in the Balkan Peninsula during the 6th–7th centuries AD, bordering with the Byzantine Empire to the south, came under the sphere of influence of Eastern Christianity, beginning with the creation of writing systems for Slavic languages (first Glagolitic, and then Cyrillic script) in 855 by the brothers Saints Cyril and Methodius and the adoption of Christianity in Bulgaria in 863. The East Slavs followed with the official adoption in 988 by Vladimir the Great of Kievan Rus'. The West Slavs' process of Christianization was more gradual and complicated. The Moravians accepted Christianity as early as 831, the Bohemian dukes followed in 845, Slovaks accepted Christianity somewhere between the years 828 and 863, but the Poles accepted it much later ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Perun
In Slavic mythology, Perun (Cyrillic: Перýн) is the highest god of the pantheon and the god of sky, thunder, lightning, storms, rain, law, war, fertility and oak trees. His other attributes were fire, mountains, wind, iris, eagle, firmament (in Indo-European languages, this was joined with the notion of the ''sky of stone''), horses and carts, and weapons (hammer, axe (Axe of Perun), and arrow). He was first associated with weapons made of stone and later with those of metal. Sources Of all historic records describing Slavic gods, those mentioning Perun are the most numerous. As early as the 6th century, he was mentioned in '' De Bello Gothico'', a historical source written by the Eastern Roman historian Procopius. A short note describing beliefs of a certain South Slavic tribe states they ''acknowledge that one god, creator of lightning, is the only lord of all: to him do they sacrifice an ox and all sacrificial animals.'' While the name of the god is not mentioned her ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rhodope Mountains
The Rhodopes (; bg, Родопи, ; el, Ροδόπη, ''Rodopi''; tr, Rodoplar) are a mountain range in Southeastern Europe, and the largest by area in Bulgaria, with over 83% of its area in the southern part of the country and the remainder in Greece. Golyam Perelik is its highest peak at . The mountain range gives its name to the terrestrial ecoregion Rodope montane mixed forests that belongs in the temperate broadleaf and mixed forests biome and the Palearctic realm. The region is particularly notable for its karst areas with their deep river gorges, large caves and specific sculptured forms, such as the Trigrad Gorge. A significant part of Bulgaria's hydropower resources are located in the western areas of the range. There are a number of hydro-cascades and dams used for electricity production, irrigation, and as tourist destinations. In Greece, there are also the hydroelectric power plants of Thisavros and Platanovrysi. The Rhodopes have a rich cultural heritage including a ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Tangra 2004/05
The Tangra 2004/05 Expedition was commissioned by the Antarctic Place-names Commission at the Ministry of Foreign Affairs of Bulgaria, managed by the Manfred Wörner Foundation, and supported by the Bulgarian Antarctic Institute, the Institute of Mathematics and Informatics at the Bulgarian Academy of Sciences, Bulgarian Posts, Uruguayan Antarctic Institute, Peregrine Shipping (Australia), and Petrol Ltd, TNT, Mtel, Bulstrad, Polytours, B. Bekyarov and B. Chernev (Bulgaria). Expedition team Dr. Lyubomir Ivanov (team leader), senior research associate, Institute of Mathematics and Informatics at the Bulgarian Academy of Sciences; chairman, Antarctic Place-names Commission; author of the 1995 Bulgarian Antarctic ''Toponymic Guidelines'' introducing in particular the present official system for the Romanization of Bulgarian; participant in four Bulgarian Antarctic campaigns, and author of the first Bulgarian Antarctic topographic maps. Doychin Vas ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Glacier Terminus
A glacier terminus, toe, or snout, is the end of a glacier at any given point in time. Although glaciers seem motionless to the observer, in reality glaciers are in endless motion and the glacier terminus is always either advancing or retreating. The location of the terminus is often directly related to glacier mass balance, which is based on the amount of snowfall which occurs in the accumulation zone of a glacier, as compared to the amount that is melted in the ablation zone. The position of a glacier terminus is also impacted by localized or regional temperature change over time. Tracking Tracking the change in location of a glacier terminus is a method of monitoring a glacier's movement. The end of the glacier terminus is measured from a fixed position in neighboring bedrock periodically over time. The difference in location of a glacier terminus as measured from this fixed position at different time intervals provides a record of the glacier's change. A similar way of trac ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Deception Island
Deception Island is an island in the South Shetland Islands close to the Antarctic Peninsula with a large and usually "safe" natural harbor, which is occasionally troubled by the underlying active volcano. This island is the caldera of an active volcano, which seriously damaged local scientific stations in 1967 and 1969. The island previously held a whaling station. It is now a tourist destination with over 15,000 visitors per year. Two research stations are operated by Argentina and Spain during the summer season. While various countries have asserted sovereignty, it is still administered under the Antarctic Treaty System. Geography Located within the Bransfield Strait, the island is roughly circular and horseshoe-shaped, with a maximum diameter around . The highest peak, Mont Pond on the east side of the island, has an elevation of , while Mount Kirkwood on the west has an elevation of . Over half (57%) of the island is covered by glaciers up to 10 m thick, ice-cor ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Gurev Gap
Gurev Gap (Gureva Sedlovina \'gu-re-va se-dlo-vi-'na\) is a flat ice-covered saddle of elevation 450 m extending 3 km in south-north direction between Hemus Peak and Gleaner Heights in eastern Livingston Island in the South Shetland Islands, Antarctica. The gap separates the glacial catchments of Kaliakra Glacier to the east, and Saedinenie Snowfield and Perunika Glacier to the west. It is part of the overland route from the St. Kliment Ohridski Base via the Balkan Snowfield, Rezen Saddle and Perunika Glacier to Varna Peninsula. The saddle was first trekked on 24 December 2004 by the Tangra 2004/05 Survey team from Camp Academia, and was named for Vasil Gurev, physicist at St. Kliment Ohridski in 1994/95 and subsequent seasons. Location The midpoint is centred at , which is 1.85 km south of Elhovo Gap, 3.42 km northwest of Yankov Gap, 3.41 km north-northwest of Omurtag Pass, 2.03 km north of Dimov Gate and 4.83 km northeast by north of Rezen Sad ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Hemus Peak
Hemus Peak ( bg, връх Хемус, vrah Hemus, ) is an ice-covered peak rising to off the northwest extremity of Bowles Ridge in eastern Livingston Island. The feature is breast-shaped, long in east-west direction and wide, and overlooks Kaliakra Glacier to the northeast and Perunika Glacier to the southwest. Hemus is an ancient name of Stara Planina (Balkan Mountains), the central mountain range separating northern from southern Bulgaria. Location The peak is located at , which is northwest of Mount Bowles (, summit of Bowles Ridge), north-northwest of Rayna Knyaginya Peak, north-northeast of Chirpan Peak, northeast of Rezen Knoll, m east by north of Aleko Point, and south by east of the summit of Gleaner Heights () (Rough British mapping in 1968, Bulgarian mapping from a 1995-96 ground survey). Maps South Shetland Islands.Scale 1:200000 topographic map. DOS 610 Sheet W 62 60. Tolworth, UK, 1968. * Islas Livingston y Decepción. Mapa topográfico a escala 1:10000 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Pimpirev Beach
Pimpirev Beach ( bg, Пимпирев бряг, Pimpirev bryag, ) is the portion of the northwest coast of South Bay, Livingston Island, Antarctica bounded to the southwest by Ereby Point and to the northeast by the north corner of the bay marked by an ice sea cave located 5.8 km east-northeast of Ereby Point and 1.45 km northwest of Aleko Point. The shoreline, extending 6.5 km in a west-southwest to east-northeast direction, is formed by a narrow beach under the Pimpirev Glacier’s terminus; a number of minor disruptions occur with segments of the ice cap penetrating the sea. Featuring Smolyan Point, a cape located 1.9 km northeast of Ereby Point and ending up with a 25 m wide and 4 m high rock, with conspicuous radial crevasses spreading inland. The central portion of the coast is indented for 250 m by a nameless 710 m wide cove behind Rongel Reef. The beach takes its name from the adjacent Pimpirev Ice Wall, respectively Pimpirev Glacier. Locat ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |