63°52′55″S58°26′08″W / 63.88194°S 58.43556°W / -63.88194; -58.43556
A point forming the south side of the entrance to Chudomir Cove on the coast of Prince Gustav Channel.
Situated 4.3 kilometres (2.7 mi) southwest of Pitt Point and7.56 kilometres (4.70 mi) southeast of Mount Reece.
Named after the town of Kiten in Southeastern Bulgaria, and in connection with the freezer vessel Kiten of the Bulgarian company Ocean Fisheries – Burgas whose ships operated in the waters of South Georgia, Kerguelen, the South Orkney Islands, South Shetland Islands and Antarctic Peninsula from 1970 to the early 1990s.
The Bulgarian fishermen, along with those of the Soviet Union, Poland and East Germany are the pioneers of modern Antarctic fishing industry.[4]
Marmais Point
63°55′22″S58°31′25″W / 63.92278°S 58.52361°W / -63.92278; -58.52361
The ice-covered point on the southeast coast of Trinity Peninsula projecting into Prince Gustav Channel.
Situated 6.3 kilometres (3.9 mi) southwest of Kiten Point, 21.6 kilometres (13.4 mi) north-northeast of Gredaro Point, and 6.65 kilometres (4.13 mi) southeast of Mount Bradley. German-British mapping in 1996.
Named after the Bulgarian duke and military commander Marmais (9th-10th century).[5]
63°54′00″S58°41′00″W / 63.90000°S 58.68333°W / -63.90000; -58.68333
A 12 kilometres (7.5 mi) long and 7.5 kilometres (4.7 mi) wide glacier on the northeast side of Detroit Plateau.
Situated southwest of Znepole Ice Piedmont and north of Aitkenhead Glacier.
Draining the area southwest of Mount Bradley and north of Tufft Nunatak, and flowing southeastwards into Prince Gustav Channel.
Named after the settlement of Dreatin in Western Bulgaria.[9]
The Reference Elevation Model of Antarctica (REMA) gives ice surface measurements of most of the continent. When a feature is ice-covered, the ice surface will differ from the underlying rock surface and will change over time. To see ice surface contours and elevation of a feature as of the last REMA update,
Trinity Peninsula(PDF) (Scale 1:250000 topographic map No. 5697), Institut für Angewandte Geodäsie and British Antarctic Survey, 1996, archived from the original(PDF) on 23 September 2015