Musala Glacier on Greenwich Island in the South Shetland Islands, Antarctica is situated northeast of Targovishte Glacier, east-northeast of Zheravna Glacier and southeast of Fuerza Aérea Glacier. It is bounded by St. Kiprian Peak to the south, Vratsa Peak to the southwest, central Breznik Heights to the west, and Ilarion Ridge bordering Hardy Cove to the northeast, extends 2 nautical miles in east-west direction and 1.2 nautical miles in north-south direction, and drains eastwards into Bransfield Strait north of Fort Point.
Panega Glacier on Varna Peninsula, Livingston Island in the South Shetland Islands, Antarctica is situated southeast of the northeastern portion of Saedinenie Snowfield, south of Rose Valley Glacier, southwest of Debelt Glacier and north of lower Kaliakra Glacier. It drains the southeast slopes of Vidin Heights and flows into Moon Bay between Helis Nunatak and Perperek Knoll. The glacier extends 2 nautical miles in the southeast-northwest direction, and 1.6 nautical miles in the southwest-northeast direction. It is named after Zlatna Panega River in northern Bulgaria.
Verila Glacier on Livingston Island in the South Shetland Islands, Antarctica is situated southeast of southern Etar Snowfield, southwest of Berkovitsa and Tundzha Glaciers, and west of Kamchiya Glacier. It is bounded by Rotch Dome to the west, Casanovas Peak and Snow Peak to the north, and Ustra Peak to the southeast. The glacier is roughly crescent-shaped, extending 7 nautical miles in an east-west direction and 2 nautical miles in a north-south direction, and drains southwards into Walker Bay, Bransfield Strait between John Beach and Liverpool Beach at Hannah Point. The glacier's bedrock is connected to Kaliman Island in Walker Bay by a 600 m long moraine tombolo. The area was visited by 19th century British and American sealers.
Huron Glacier is a 4.8 nautical miles } long and 2.2 nautical miles wide glacial flow on Livingston Island in the South Shetland Islands of Antarctica, situated east of Perunika Glacier, southeast of Kaliakra Glacier, south of Struma Glacier, west-northwest of Iskar Glacier and northeast of Huntress Glacier. It is bounded by Bowles Ridge to the north, Wörner Gap to the west and the Tangra Mountains to the south, receiving ice influx from several tributary glaciers draining the mountain's northern slopes between Mount Friesland and Helmet Peak, and running east-northeastwards to empty into Moon Bay south of Elemag Point and north of Yana Point. Camp Academia is situated on upper Huron Glacier, in the northwestern foothills of Zograf Peak.
Bistra Glacier is 1 nautical mile long and 0.4 nautical miles wide glacier on the northwest side of Imeon Range on Smith Island in the South Shetland Islands, Antarctica. It is situated southwest of Chuprene Glacier and northwest of Dragoman Glacier, drains the west slopes of Mount Foster and the north slopes of Slaveykov Peak, and flows northwestwards of Zavet Saddle to enter Drake Passage south of Garmen Point.
Anna Glacier is a glacier flowing southeast between Rose Peak and Rea Peak, tributary to Polonia Glacier/Polonia Ice Piedmont at the head of King George Bay, King George Island. It was named by the Polish Antarctic Expedition (PAE), 1981, after Anna Tokarska, field assistant of PAE geological party to King George Island, 1979–80, and wife of Antoni K. Tokarski.
Usher Glacier is a glacier nearly 4 nautical miles (7 km) long, flowing northwest
into the sea between Stigant Point and Davey Point on the north coast of King George Island, in the South Shetland Islands. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1960 for J. Usher, Master of the Caraquet from Liverpool, who visited the South Shetland Islands in 1821-22.
Cinder Spur is a small spur extending into Legru Bay, 1.5 nautical miles (3 km) west of Low Head on the south coast of King George Island, in the South Shetland Islands. It was so named by the UK Antarctic Place-Names Committee in 1963 because the feature is composed mainly of volcanic cinders.
Napier Rock is a rock lying 1.75 nautical miles (3.2 km) east-southeast of Point Thomas in Admiralty Bay, King George Island, in the South Shetland Islands. Charted by the French Antarctic Expedition under Charcot, 1908-10. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) in 1960 for Ronald G. Napier (1925–1956) of Falkland Islands Dependencies Survey (FIDS), general assistant and handyman at the Signy Island station in 1955, and then leader at Admiralty Bay until he was drowned on March 24, 1956.
Mount Walker is a snow-covered mountain which rises from the northeast part of Forbidden Plateau, 2 nautical miles (3.7 km) south of the head of Blanchard Glacier, in northern Graham Land, Antarctica. It was surveyed by Falkland Islands Dependencies Survey (FIDS) in 1955. Named by United Kingdom Antarctic Place-Names Committee (UK-APC) for Richard Walker of the Discovery Investigations, First Officer on RRS Discovery II, 1933-37.
Deadmond Glacier is a glacier about 6 nautical miles (11 km) long, flowing from the east side of Evans Peninsula on Thurston Island into Cadwalader Inlet. It was discovered by the U.S. Navy Bellingshausen Sea Expedition in February 1960, and was named by the Advisory Committee on Antarctic Names for Lieutenant Commander Robert B. Deadmond, executive officer of USS Burton Island, forming part of this expedition.
Jardine Peak is a peak, 285 metres (935 ft) high, standing 1 nautical mile (2 km) southwest of Point Thomas on the west side of Admiralty Bay, King George Island, in the South Shetland Islands. It was named by the UK Antarctic Place-Names Committee in 1960 for D. Jardine of the Falkland Islands Dependencies Survey, a geologist at Admiralty Bay in 1949, who travelled extensively on King George Island.
The Gemel Peaks are two peaks 1.3 nautical miles (2.4 km) northeast of Horatio Stump on Fildes Peninsula, King George Island, in the South Shetland Islands. They were charted and named "Twin Peak" or "Twin Peaks" by Discovery Investigations personnel on the Discovery II in 1935. To avoid duplication, this name was rejected by the UK Antarctic Place-Names Committee in 1960 and a new name substituted; "Gemel" means twin.
Lizard Hill is a narrow, curving rock ridge, 355 metres (1,165 ft) high, standing 2 nautical miles (4 km) southwest of Trepassey Bay and 0.5 nautical miles (1 km) east of Ridge Peak, on Tabarin Peninsula, Antarctica. The hill was probably first seen by the Swedish Antarctic Expedition, 1901–04, under Otto Nordenskjöld, and was first charted in 1946 by the Falkland Islands Dependencies Survey, who applied the descriptive name.
Hauken Rock is a rock lying nearly 1 nautical mile (2 km) east of the Ornen Rocks and 2 nautical miles (4 km) northeast of Cape Melville, the eastern extremity of King George Island, in the South Shetland Islands. It was named by the UK Antarctic Place-Names Committee in 1960 from association with Ornen Rocks. Hauken and Ørnen, the first two modern whale catchers, accompanied the floating factory ship Admiralen to the South Shetland Islands in January–February 1906.
Richthofen Pass is a pass, 1 nautical mile (1.9 km) wide, between Mount Fritsche and the rock wall north of McCarroll Peak, on the east coast of Graham Land. Discovered and photographed in 1902 by the Swedish Antarctic Expedition under Nordenskjold, who named it Richthofen Valley for Baron Ferdinand von Richthofen, German geographer and geologist. The feature was found to be a pass by the Falkland Islands Dependencies Survey (FIDS) in 1955.
Landfall Peak is a prominent peak-shaped landmark near the extreme west end of Thurston Island, Antarctica, about 8 nautical miles (15 km) east-northeast of Cape Flying Fish and 0.5 nautical miles northwest of Mount Gimber. It was discovered by members of the United States Antarctic Service in flights from the USS Bear in February 1940, and photographed at that time by E.B. Perce. The peak was plotted from air photos taken by U.S. Navy Operation Highjump in December 1946, and was observed by personnel of the U.S. Navy Bellingshausen Sea Expedition in February 1960. It was so named by the Advisory Committee on Antarctic Names because rock exposures on the peak serve as a mark for ships approaching Thurston Island from the west.
