Maglenik Heights
Maglenik Heights ( bg, Мъгленишки възвишения, ‘Maglenishki Vazvisheniya’ \'m&-gle-nish-ki v&-zvi-'she-ni-ya\) are the heights rising to 2752 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 at Mount Gozur and including also Roberts Peak, Chapman Peak, Ichera Peak, Voysil Peak, Zimornitsa Peak and Mirovyane Peak in north-central Sentinel Range in Ellsworth Mountains, Antarctica, extending 26 km in north–south direction and 20 km in east–west direction. They are bounded by Ellen Glacier to the south and west, Embree Glacier and Kopsis Glacier to the north, and Rutford Ice Stream and Arapya Glacier to the east, and linked to Bangey Heights to the northwest by Panicheri Gap, and to Barnes Ridge (Antarctica), Barnes Ridge to t ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Kopsis Glacier
Kopsis Glacier ( bg, ледник Копсис, lednik Kopsis, ) is a long and wide glacier on the east side of north-central Sentinel Range in Ellsworth Mountains, Antarctica that is draining northeastwards from Panicheri Gap, Voysil Peak and Mount Gozur to join Embree Glacier northwest of Mirovyane Peak. The glacier is named after the medieval town of Kopsis in Central Bulgaria. Location Kopsis Glacier is centred at . US mapping in 1961, updated in 1988. See also * List of glaciers in the Antarctic * Antarctic Place-names Commission * Glaciology Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. Notes References Kopsis GlacierSCAR Composite Antarctic Gazetteer Bulgarian Antarctic Gazetteer.Antarctic Place-names Commission The Antarctic Place-names Co ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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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 ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Young Glacier
Young Glacier () is a glacier which flows from Mount Gozur and Ichera Peak in Maglenik Heights eastwards for 8 miles (13 km) and terminates at the north end of Barnes Ridge on the east side of Sentinel Range, Ellsworth Mountains in Antarctica. It was first mapped by the United States Geological Survey (USGS) from surveys and U.S. Navy air photos from 1957–59. It was named by the Advisory Committee on Antarctic Names (US-ACAN) for First Lieutenant Dale L. Young of the United States Air Force (USAF), who participated in establishing the South Pole Station in the 1956–57 season. 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 ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US G ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Chapman Peak (Antarctica)
Chapman Peak () is a peak, high, in the Maglenik Heights, on the east side of Ellen Glacier and west of Arapya Glacier, northeast of Mount Jumper in the central Sentinel Range of the Ellsworth Mountains, Antarctica. It was first mapped by the U.S. Geological Survey from surveys and from U.S. Navy air photos, 1957–59, and named by the Advisory Committee on Antarctic Names for Captain John H. Chapman, USAF, who participated in establishing the International Geophysical Year South Pole Station in the 1956–57 season. See also * Mountains in Antarctica This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Antarctica. Some islands in the South Atlantic have also been included and can be found at the end of the list. Antarctica South Atl ... Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarc ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Mountains In Antarctica ...
This is a list of all the Ultra prominent peaks (with topographic prominence greater than 1,500 metres) in Antarctica. Some islands in the South Atlantic have also been included and can be found at the end of the list. Antarctica South Atlantic Sources * * * {{DEFAULTSORT:List Of Ultras Of Antarctica Antarctica Ultras * Ultras Ultras are a type of association football fans who are renowned for their fanatical support. The term originated in Italy, but is used worldwide to describe predominantly organised fans of association football teams. The behavioural tende ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Dropla Gap
Dropla Gap ( bg, седловина Дропла, ‘Sedlovina Dropla’ \ se-dlo-vi-'na dro-'pla\) is the flat, ice-covered saddle of elevation 1073 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in north-central Sentinel Range in Ellsworth Mountains, , extending 1.35 km to link to the ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Barnes Ridge (Antarctica)
Barnes Ridge () is a ridge long, rising to over (Mount Besch) and extending between Young Glacier and Ellen Glacier at the east side of the Sentinel Range, Ellsworth Mountains in Antarctica. It is bounded by Rutford Ice Stream to the east and Arapya Glacier to the west, and connected to Maglenik Heights to the northwest by Dropla Gap. Its eastern slopes are drained by Ranuli Ice Piedmont. The ridge was mapped by the United States Geological Survey from surveys and from U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for Stephen S. Barnes, scientific leader at Byrd Station The Byrd Station is a former research station established by the United States during the International Geophysical Year by U.S. Navy Seabees during Operation Deep Freeze II in West Antarctica. History A joint Army, Navy, Air Force, and Marin ... in 1958. Maps Vinson Massif. Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. An ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Panicheri Gap
Panicheri Gap ( bg, Паничерска седловина, ‘Panicherska Sedlovina’ \pa-ni-'cher-ska se-dlo-vi-'na\) is the flat, ice-covered saddle of elevation 2109 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 in north-central Sentinel Range in Ellsworth Mountains, , linking to the north ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Bangey Heights
The Bangey Heights ( bg, Бангейски възвишения, ‘Bangeyski Vazvisheniya’ \ban-'gey-ski v&-zvi-'she-ni-ya\) are in Antarctica. They are the heights rising to 2997 mReference Elevation Model of Antarctica. Polar Geospatial Center. University of Minnesota, 2019 near Bezden Peak in north-central Sentinel Range in Ellsworth Mountains, extending 12 km in southwest–northeast direction and 10 km in northwest–southeast direction. They are bounded by Patleyna Glacier to the west, Embree Glacier to the northwest and northeast, and Kopsis Glacier to the southeast, and linked to Probuda Ridge to the southwest by Chepino Saddle, and to Maglenik Heights to the south by Panicheri Gap. Their interior is drained by Marsa Glacier and Padala Glacier. The heights are named after the s ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Arapya Glacier
Arapya Glacier ( bg, ледник Арапя, lednik Arapya, ) is the long and wide glacier on the east side of north-central Sentinel Range in Ellsworth Mountains, Antarctica, situated south of Young Glacier. It flows southwards along the west side of Barnes Ridge and east of Chapman Peak and joins Ellen Glacier southwest of Mount Besch. The glacier is named after the seaside locality of Arapya in Southeastern Bulgaria. Location Arapya Glacier is centred at . US mapping in 1961, updated in 1988. See also * List of glaciers in the Antarctic * Glaciology Maps Vinson Massif.Scale 1:250 000 topographic map. Reston, Virginia: US Geological Survey, 1988. Antarctic Digital Database (ADD).Scale 1:250000 topographic map of Antarctica. Scientific Committee on Antarctic Research (SCAR). Since 1993, regularly updated. References Bulgarian Antarctic Gazetteer.Antarctic Place-names Commission. (details in Bulgarianbasic datain English) Arapya Glacier.SCAR Composite Gazetteer of Anta ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |
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Rutford Ice Stream
Rutford Ice Stream () is a major Antarctic ice stream, about long and over wide, which drains southeastward between the Sentinel Range, Ellsworth Mountains and Fletcher Ice Rise into the southwest part of Ronne Ice Shelf. Named by US-ACAN for geologist Robert Hoxie Rutford, a member of several USARP expeditions to Antarctica; leader of the University of Minnesota Ellsworth Mountains Party, 1963-1964. Rutford served as Director of the Division of Polar Programs, National Science Foundation, 1975-1977. The ice stream is situated in a deep trough which is a tectonic feature between the Ellsworth Mountains and the Fletcher Promontory. Because of this the ice stream position may have been stable for millions of years. The bed of the ice stream reaches below sea level. Therefore, between the bed of the ice stream and the height of the Ellsworth Mountains there is a vertical relief of over a distance of only . At the upper (inland) end of the ice stream the ice thickness reache ... [...More Info...]       [...Related Items...]     OR:     [Wikipedia]   [Google]   [Baidu]   |