O'Higgins Glacier
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O'Higgins Glacier is a
glacier A glacier (; or ) is a persistent body of dense ice, a form of rock, that is constantly moving downhill under its own weight. A glacier forms where the accumulation of snow exceeds its ablation over many years, often centuries. It acquires ...
located in
Bernardo O'Higgins National Park Bernardo O'Higgins National Park () is the largest of the protected areas in Chile, covering an area of , in both the Aysén del General Carlos Ibáñez del Campo Region, Aysén and Magallanes and Antartica Chilena Region, Magallanes and Antárti ...
,
Chile Chile, officially the Republic of Chile, is a country in western South America. It is the southernmost country in the world and the closest to Antarctica, stretching along a narrow strip of land between the Andes, Andes Mountains and the Paci ...
. It is one of the principal glaciers of the
Southern Patagonian Ice Field The Southern Patagonian Ice Field (), located at the Southern Patagonic Andes between Chile and Argentina, is the world's second largest contiguous extrapolar ice field. It is the bigger of two remnant parts of the Patagonian Ice Sheet, which c ...
. The summit of the active
Lautaro Lautaro (Anglicized as 'Levtaru') ( " swift hawk") (; 1534 – April 29, 1557) was a young Mapuche toqui known for leading the indigenous resistance against Spanish conquest in Chile and developing the tactics that would continue to be empl ...
volcano is the top of the
accumulation zone On a glacier, the accumulation zone is the area above the firn line, where snowfall accumulates and exceeds the losses from ablation, ( melting, evaporation, and sublimation). The annual equilibrium line separates the accumulation and ablation ...
of the glacier. The bulk of the glacier is part of the icefield plateau. It flows eastward into O'Higgins Lake and is about wide at the terminus.


See also

* Pío XI Glacier *
List of glaciers A glacier ( ) or () is a persistent body of dense ice that is constantly moving under its own weight; it forms where the accumulation of snow exceeds its ablation (melting and sublimation) over many years, often centuries. Glaciers slowly defor ...


References

Glaciers of Aysén Region {{chile-glacier-stub