Harrisson Ice Rises [SEP] continent
Harrisson Ice Rises
The Harrisson Ice Rises () are a local swelling of the ice surface west-southwest of Henderson Island, Antarctica, where the Shackleton Ice Shelf overrides an underlying obstruction. The feature was discovered by the Eastern Sledge Party of the Australasian Antarctic Expedition (1911–14) under Douglas Mawson, who named the feature for Charles T. Harrisson, biologist with the expedition.
Ice Rises (the northernmost ice rise, at 66°21'S)
- Harrisson Ice Rises
- Ross Ice Shelf
- Crary Ice Rise (the southernmost ice rise, at 82°56'S)
- Crosson Ice Shelf
- Davis Ice Rise
- Bach Ice Shelf
- Burgess Ice Rise
- Dvořák Ice Rise
- Ives Ice Rise
- Landy Ice Rises
- George VI Ice Shelf
- Martin Ice Rise
- Wilkins Ice Shelf
- Petrie Ice Rises
- Schaus