Trakiya Heights
Encyclopedia
Trakiya Heights are the heights rising to 1336 m (Irakli Peak
) on Trinity Peninsula
, Antarctic Peninsula
. Bounded by Russell West Glacier
to the north, Srem Gap
and Russell East Glacier
to the northeast, Victory Glacier
to the southwest and Zlidol Gate
to the northwest. Surmounting Prince Gustav Channel
, Weddell Sea
to the southeast. Extending 10 km in northwest-southeast direction and 5.9 km in northeast-southwest direction.
The heights are named after the historical region of Trakiya (Thrace)
.
Irakli Peak
Irakli Peak is the peak rising to 1336 m in the northwest part of Trakiya Heights on Trinity Peninsula, Antarctic Peninsula. Situated 1.43 km northeast of Antonov Peak, 3.24 km southwest of Mount Canicula, 3.87 km west-northwest of Mount Daimler and 3.56 km north-northwest of Bozveli Peak...
) on Trinity Peninsula
Trinity Peninsula
Trinity Peninsula is the extreme northern portion of the Antarctic Peninsula, extending northeastward for about from a line connecting Cape Kjellman and Cape Longing. Dating back more than a century, chartmakers used various names for this portion of the Antarctic peninsula, each name having some...
, Antarctic Peninsula
Antarctic Peninsula
The Antarctic Peninsula is the northernmost part of the mainland of Antarctica. It extends from a line between Cape Adams and a point on the mainland south of Eklund Islands....
. Bounded by Russell West Glacier
Russell West Glacier
Russell West Glacier is a glacier, 11 nautical miles long and 4 nautical miles wide, which lies immediately north of Detroit Plateau and flows from Mount Canicula westward into Bone Bay on the north side of Trinity Peninsula...
to the north, Srem Gap
Srem Gap
Srem Gap is the flat saddle of elevation over 700 m extending 1.35 km on Trinity Peninsula, Antarctic Peninsula, which is situated between Russell West Glacier to the northwest and a tributary glacier to Russell East Glacier to the southeast...
and Russell East Glacier
Russell East Glacier
Russell East Glacier is a glacier, 6 nautical miles long and 3 nautical miles wide, which lies at the north end of Detroit Plateau and flows from Mount Canicula eastward into Prince Gustav Channel on the south side of Trinity Peninsula...
to the northeast, Victory Glacier
Victory Glacier
Victory Glacier is a gently sloping glacier, 8 nautical miles long, flowing east-southeast from the north end of Detroit Plateau on Trinity Peninsula to Prince Gustav Channel immediately north of Pitt Point. Bounded by Trakiya Heights to the north and Kondofrey Heights to the south...
to the southwest and Zlidol Gate
Zlidol Gate
Zlidol Gate is the saddle of elevation over 800 m on Trinity Peninsula, Antarctic Peninsula separating Detroit Plateau to the west from Trakiya Heights to the east...
to the northwest. Surmounting Prince Gustav Channel
Prince Gustav Channel
The Prince Gustav Channel was named in 1903 after Crown Prince Gustav of Sweden by Otto Nordenskiöld of the Swedish Antarctic Expedition.The channel is bounded on the west by the Antarctic Peninsula and on the east by James Ross Island...
, Weddell Sea
Weddell Sea
The Weddell Sea is part of the Southern Ocean and contains the Weddell Gyre. Its land boundaries are defined by the bay formed from the coasts of Coats Land and the Antarctic Peninsula. The easternmost point is Cape Norvegia at Princess Martha Coast, Queen Maud Land. To the east of Cape Norvegia is...
to the southeast. Extending 10 km in northwest-southeast direction and 5.9 km in northeast-southwest direction.
The heights are named after the historical region of Trakiya (Thrace)
Thrace
Thrace is a historical and geographic area in southeast Europe. As a geographical concept, Thrace designates a region bounded by the Balkan Mountains on the north, Rhodope Mountains and the Aegean Sea on the south, and by the Black Sea and the Sea of Marmara on the east...
.
Location
Trakiya Heights are located at 63°45′07"S 58°31′10"W. German-British mapping in 1996.Map
- Trinity Peninsula. Scale 1:250000 topographic map No. 5697. Institut für Angewandte Geodäsie and British Antarctic Survey, 1996.