Amalia Glacier
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Amalia Glacier, also known as Skua Glacier, is a
tidewater glacier The tidewater glacier cycle is the typically centuries-long behavior of tidewater glaciers that consists of recurring periods of advance alternating with rapid retreat and punctuated by periods of stability. During portions of its cycle, a tidewate ...
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 and Magallanes and Antártica Chilena regions. Management of this and other national parks in Chile is entrusted to the ...
on the edge of the
Sarmiento Channel Sarmiento Channel is a principal Patagonia channel, which extends in a north–south direction. It begins with the Guia Narrows ('' Angostura Guía'') and is located in Magallanes y Antártica Chilena Region. The kawésqar people sailed its wat ...
. The glacier originates in the
Southern Patagonian Ice Field The Southern Patagonian Ice Field ( es, Hielo Continental or '), 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 P ...
. From 1945 to 1986, its terminus retreated , being, along with the recession of the O'Higgins Glacier, the most dramatic retreat of the glaciers of the mentioned icefield during that period. The glacier partially surrounds Reclus volcano and erodes the northern flank of it.


See also

*
Retreat of glaciers since 1850 The retreat of glaciers since 1850 affects the availability of fresh water for irrigation and domestic use, mountain recreation, animals and plants that depend on glacier-melt, and, in the longer term, the level of the oceans. Deglaciation occur ...


References


External links

* Glaciers of Magallanes Region {{Chile-glacier-stub