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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 ...
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Sentinel Range
The Sentinel Range is a major mountain range situated northward of Minnesota Glacier and forming the northern half of the Ellsworth Mountains in Antarctica. The range trends NNW-SSE for about and is 24 to 48 km (15 to 30 mi) wide. Many peaks rise over and Vinson Massif (4892 m) in the southern part of the range is the highest elevation on the continent.Sentinel Range.
SCAR Composite Antarctic Gazetteer.
Sentinel Range comprises a main ridge (featuring Vinson Massif in its southern portion) and a number of distinct heights, ridges and mountains on its east side, including (south to north) ,
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Ellsworth Mountains
The Ellsworth Mountains are the highest mountain ranges in Antarctica, forming a long and wide chain of mountains in a north to south configuration on the western margin of the Ronne Ice Shelf in Marie Byrd Land. They are bisected by Minnesota Glacier to form the Sentinel Range to the north and the Heritage Range to the south. The former is by far the higher and more spectacular with Mount Vinson () constituting the highest point on the continent.Bockheim, J.G., Schaefer, C.E., 2015. ''Soils of Ellsworth Land, the Ellsworth Mountains''. In: Bockheim, J.G. (Ed.), ''The Soils of Antarctica. World Soils Book Series'', Springer, Switzerland, pp. 169–181. The mountains are located within the Chilean Antarctic territorial claim but outside of the Argentinian and British ones. Discovery The mountains were discovered on November 23, 1935, by Lincoln Ellsworth in the course of a trans-Antarctic flight from Dundee Island to the Ross Ice Shelf. He gave them the descriptive name Sentinel ...
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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 ...
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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 ...
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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 ...
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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 ...
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Ellen Glacier
The Ellen Glacier is a glacier in the central Sentinel Range of the Ellsworth Mountains of Antarctica. It drains the eastern slopes of Mount Anderson and Long Gables and flows generally southeast for to Barnes Ridge, where it leaves the range and enters the south flowing Rutford Ice Stream. It was first mapped by the United States Geological Survey from surveys and U.S. Navy air photos, 1957–59, and was named by the Advisory Committee on Antarctic Names for Lieutenant Colonel Cicero J. Ellen of the U.S. Air Force, who was in command of many of the air operations when the South Pole Station was established by air drop in the 1956–57 season. Tributary glaciers * Pulpudeva Glacier * Crosswell Glacier * Patton Glacier * Rumyana Glacier * Delyo Glacier * Burdenis Glacier * Gerila Glacier * Fonfon Glacier * Arapya Glacier See also * List of glaciers in the Antarctic * Glaciology Glaciology (; ) is the scientific study of glaciers, or more generally ice and natu ...
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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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Mountain Passes Of Ellsworth 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 and ...
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