Bell Rock (Antarctica)
Goodenough Glacier () is a broad sweeping glacier to the south of the Batterbee Mountains, flowing from the west shore of Palmer Land, Antarctica, into George VI Sound and the George VI Ice Shelf. It was discovered in 1936 by A. Stephenson, W.L.S. Fleming, and George C.L. Bertram of the British Graham Land Expedition under John Rymill, while exploring George VI Sound, and was named by Rymill after Margaret Goodenough, wife of Admiral Sir William Goodenough, the latter being one of Rymill's principal supporters in raising funds for the expedition. Bell Rock (Antarctica), Bell Rock is a very conspicuous and isolated nunatak located on the glacier. References

Glaciers of Palmer Land {{PalmerLand-geo-stub ...
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Glacier
A glacier (; ) is a persistent body of dense ice that is constantly moving under its own weight. A glacier forms where the accumulation of snow exceeds its Ablation#Glaciology, ablation over many years, often Century, centuries. It acquires distinguishing features, such as Crevasse, crevasses and Serac, seracs, as it slowly flows and deforms under stresses induced by its weight. As it moves, it abrades rock and debris from its substrate to create landforms such as cirques, moraines, or fjords. Although a glacier may flow into a body of water, it forms only on land and is distinct from the much thinner sea ice and lake ice that form on the surface of bodies of water. On Earth, 99% of glacial ice is contained within vast ice sheets (also known as "continental glaciers") in the polar regions, but glaciers may be found in mountain ranges on every continent other than the Australian mainland, including Oceania's high-latitude oceanic island countries such as New Zealand. Between lati ...
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