Forbes Glacier (Mac. Robertson Land)
Exploration
The glacier was mapped by Norwegian cartographers from aerial photographs taken by the Lars Christensen Expedition (1936–37) and called "Brygga" (the wharf). It was renamed by the Australian Antarctic Names and Medals Committee after A. Forbes of the Australian National Antarctic Research Expeditions, who perished on a field trip at Heard Island in 1952.
Origin
The Forbes Glacier originates on the east of the Casey Range, about 25 kilometres (16 mi) south of the Holme Bay coast. Tributaries flow east and north through the nunataks of the range, and join into a stream of ice about 5 kilometres (3.1 mi) wide. In the uppermost part of the glacier near the Casey Range the ice in the center of the glacier travels north at 59 metres (194 ft) per year. The area east of the Casey Range has fine-grained ice with a polygonal texture in the zone between the accumulation and ablation areas.
Mouth
The Forbes Glacier enters the sea between two rocky outcrops. That on the east has no flora, but that on the west contains a large, high outcrop of typical granite of the Mawson area with nine species of lichen and one of moss (Bryum antarcticum).
See also
References
- ^ Forbes Glacier USGS.
- ^ Koshiro Kizaki 1969, p. 376.
- ^ Koshiro Kizaki 1969, p. 375.
- ^ Filson 1966, p. 10.
- ^ Filson 1966, pp. 10–11.
Sources
- Filson, Rex B. (1966), The Lichens and Mosses of Mac. Robertson Land (PDF), Antarctic Division, Department of External Affairs Australia, retrieved 2023-11-28
- "Forbes Glacier", Geographic Names Information System, United States Geological Survey, United States Department of the Interior, retrieved 2012-03-29
This article incorporates public domain material from "Forbes Glacier". Geographic Names Information System. United States Geological Survey.
- Koshiro Kizaki (1969), "Fabric Analysis of Surface Ice near Casey Range, East Antarctica", Journal of Glaciology, 8 (54), Cambridge University Press
67°39′S 62°22′E / 67.650°S 62.367°E