Challenger Glacier | |
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Type | cirque/tidewater |
Location | Heard Island, Territory of Heard Island and McDonald Islands, Australia |
Coordinates | 53°2′S 73°28′E / 53.033°S 73.467°ECoordinates: 53°2′S 73°28′E / 53.033°S 73.467°E |
Width | 0.8 nautical miles (1.5 km) |
Thickness | 55 metres (180 ft) |
Terminus | eastern side of Corinthian Bay, close west to Saddle Point |
Status | Retreating |
Challenger Glacier is a tidewater glacier on the north side of Heard Island in the southern Indian Ocean. Located 1 nautical mile (2 km) east of Baudissin Glacier, Challenger Glacier is 0.8 nautical miles (1.5 km) wide and flows into the eastern side of Corinthian Bay, close west to Saddle Point. To the east of Challenger Glacier is Downes Glacier, whose terminus is located at Mechanics Bay, between Saddle Point and Cape Bidlingmaier. To the west of Challenger Glacier is Baudissin Glacier, whose terminus is located at the western side of Corinthian Bay, near Sealers Cove.
The glacier appears to have been first charted by the Gauss expedition under Erich von Drygalski, 1901–03, who portrayed a single large glacier flowing into Corinthian Bay. In 1948 the Australian National Antarctic Research Expeditions (ANARE) determined that more than one glacier discharges into Corinthian Bay. ANARE applied the name Challenger Glacier to the easternmost of these glaciers to commemorate the work of the British Challenger Expedition, 1873–76.
The landscape of Heard Island and nearby McDonald Island is constantly changing due to volcanism, strong winds and waves, and climate change. Volcanic activity has been observed in this area since the mid-1980s, with fresh lava flows on the southwest flanks of Heard Island. Satellite imagery shows that McDonald Island increased in size from about 1 to 2.5 square kilometers between 1994 and 2004, as a result of volcanic activity.