Schubert Inlet ( 70°52′S70°55′W / 70.867°S 70.917°W ) is an ice-filled inlet in Antarctica.
Schubert Inlet is 14 nautical miles (16 mi; 26 km) long and 5 nautical miles (5.8 mi; 9.3 km) wide, indenting the west coast of Alexander Island, lying between the Colbert Mountains north of the inlet and the Walton Mountains south of the inlet. The inlet receives ice flowing into it throughout the whole year, mainly because the inlet is adjacent to the Wilkins Ice Shelf, which lies immediately west.
The inlet was first mapped from air photos taken by the Ronne Antarctic Research Expedition in 1947–48, by Searle of the Falkland Islands Dependencies Survey in 1960. It was named by the United Kingdom Antarctic Place-Names Committee for Franz Schubert (1797–1828), Austrian composer.
Thurston Island is a largely ice-covered, glacially dissected island, 135 nautical miles long and 55 nautical miles wide, lying between Amundsen Sea and Bellingshausen Sea a short way off the northwest end of Ellsworth Land, Antarctica. The island is separated from the mainland by Peacock Sound, which is occupied by the west portion of Abbot Ice Shelf.
Skelton Glacier is a large glacier flowing from the polar plateau into the Ross Ice Shelf at Skelton Inlet on the Hillary Coast, south of Victoria Land, Antarctica.
The Hauberg Mountains are a group of mountains of about 35 nautical miles extent, located 12 nautical miles north of Cape Zumberge and 30 nautical miles south of the Sweeney Mountains in eastern Ellsworth Land, Antarctica.
The Abbot Ice Shelf is an ice shelf 250 nautical miles long and 40 nautical miles wide, bordering Eights Coast from Cape Waite to Pfrogner Point in Antarctica. Thurston Island lies along the northern edge of the western half of this ice shelf; other sizable islands lie partly or wholly within this shelf.
Martin Peninsula is a peninsula about 60 nautical miles long and 20 nautical miles wide that is ice-covered except for a few rock outcrops along its margins, located between Getz Ice Shelf and Dotson Ice Shelf on the coast of Marie Byrd Land, Antarctica. The farthest point of the peninsula is Jacobsen Head.
The Getz Ice Shelf is an ice shelf over 300 nautical miles long and from 20 to 60 nautical miles wide, bordering the Hobbs Coast and Bakutis Coast of Marie Byrd Land, Antarctica, between the McDonald Heights and Martin Peninsula. Several large islands are partially or wholly embedded in the ice shelf.
The Beethoven Peninsula is a deeply indented, ice-covered peninsula, 60 miles (100 km) long in a northeast–southwest direction and 60 miles (100 km) wide at its broadest part, forming the southwest part of Alexander Island, which lies off the southwestern portion of the Antarctic Peninsula. The south side of the peninsula is supported by the Bach Ice Shelf whilst the north side of the peninsula is supported by the Wilkins Ice Shelf. The Mendelssohn Inlet, the Brahms Inlet and the Verdi Inlet apparently intrude into it. The Bach Ice Shelf, Rossini Point and Berlioz Point are some distance away, on the Ronne Entrance from the Southern Ocean. Beethoven Peninsula is one of the eight peninsulas of Alexander Island.
The Ickes Mountains are a series of coastal mountains that extend west from Strauss Glacier for 15 nautical miles in Marie Byrd Land, Antarctica.
Gilbert Glacier is a glacier about 20 nautical miles (37 km) long flowing south from Nichols Snowfield into Mozart Ice Piedmont, situated in northern Alexander Island, Antarctica.
Crane Glacier is a narrow glacier which flows 30 miles (50 km) in an east-northeasterly direction along the northwest side of Aristotle Mountains to enter Spillane Fjord south of Devetaki Peak, on the east coast of the Antarctic Peninsula. Sir Hubert Wilkins photographed this feature from the air in 1928 and gave it the name "Crane Channel", after C.K. Crane of Los Angeles, reporting that it appeared to be a channel cutting in an east-west direction across the peninsula. The name was altered to "Crane Inlet" following explorations along the west coast of the peninsula in 1936 by the British Graham Land Expedition, which proved that no through channel from the east coast existed as indicated by Wilkins. Comparison of Wilkins' photograph of this feature with those taken in 1947 by the Falklands Islands Dependencies Survey shows that Wilkins' "Crane Channel" is this glacier, although it lies about 75 miles (120 km) northeast of the position originally reported by Wilkins.
Nansen Ice Sheet is a 30 nautical miles long by 10 nautical miles wide ice shelf. It is nourished by the Priestley and Reeves Glaciers and abuts the north side of the Drygalski Ice Tongue, along the coast of Victoria Land, Antarctica. This feature was explored by the South Magnetic Polar Party of the British Antarctic Expedition, 1907-09 and by the Northern Party of the British Antarctic Expedition, 1910-13. Frank Debenham, geologist with the latter expedition, applied the name Nansen Sheet as the feature is adjacent to Mount Nansen, the dominating summit in the area.
The Latady Mountains are a group of mountains rising west of Gardner Inlet and between Wetmore Glacier and Ketchum Glacier, in southeastern Palmer Land, Antarctica.
Carroll Inlet is an inlet, 40 nautical miles long and 6 nautical miles wide, trending southeast along the coast of Ellsworth Land, Antarctica, between the Rydberg Peninsula and Smyley Island. The head of the inlet is divided into two arms by the presence of Case Island and is bounded to the east by Stange Ice Shelf.
Casey Inlet is an ice-filled inlet at the terminus of Casey Glacier, between Miller Point and Cape Walcott, on the east coast of Palmer Land, Antarctica.
Mozart Ice Piedmont is an ice piedmont, 60 nautical miles (110 km) long-running in a NW-SE direction and 15 nautical miles (28 km) wide in its widest part, on the west coast of Alexander Island, Antarctica. Mapped from air photos taken by the Ronne Antarctic Research Expedition (RARE) in 1947, by Searle of the Falkland Islands Dependencies Survey (FIDS) in 1960. Named by the United Kingdom Antarctic Place-Names Committee (UK-APC) for Wolfgang Amadeus Mozart (1756–1791), famous Austrian composer. Some landforms within this area are named in association with the Mozart Ice Piedmont such as Figaro Nunatak, along with a few other landforms.
Haydn Inlet is an ice-filled inlet indenting the west coast of Alexander Island, Antarctica, lying between Mozart Ice Piedmont and Handel Ice Piedmont. Schubert Inlet lies to the south and the Lassus Mountains are immediately north. Haydn Inlet is 27 nautical miles (50 km) long and 12 nautical miles (22 km) wide at the mouth, narrowing toward the head. It was first seen from the air and roughly mapped by the United States Antarctic Service, 1939–41. It was resighted from the air and photographed by the Ronne Antarctic Research Expedition, 1947–48, and remapped from these photos by D. Searle of the Falkland Islands Dependencies Survey in 1960. The inlet was named by the UK Antarctic Place-Names Committee for Joseph Haydn, the Austrian composer.
Hilton Inlet is an ice-filled inlet, 12 nautical miles wide, which recedes about 22 nautical miles west from its entrance between Cape Darlington and Cape Knowles, along the east coast of Palmer Land, Antarctica.
Lamplugh Island is an ice-capped island, 10 nautical miles long, lying 4 nautical miles north of Whitmer Peninsula, along the coast of Victoria Land, Antarctica.
Lehrke Inlet is an ice-filled inlet, 8 nautical miles wide, which recedes southwest for 17 nautical miles between Cape Boggs and Cape Sharbonneau, along the east coast of Palmer Land, Antarctica.
The Lillie Range in Antarctica extends northward from the Prince Olav Mountains to the Ross Ice Shelf. Mounts Hall, Daniel, Krebs and Mason are in the range.
This article incorporates public domain material from "Schubert Inlet". Geographic Names Information System . United States Geological Survey.