Wilson Glacier (Mount Rainier)
   HOME

TheInfoList



OR:

The Wilson Glacier is a medium-sized tributary
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 dis ...
located on the southeast flank of
Mount Rainier Mount Rainier (), indigenously known as Tahoma, Tacoma, Tacobet, or təqʷubəʔ, is a large active stratovolcano in the Cascade Range of the Pacific Northwest, located in Mount Rainier National Park about south-southeast of Seattle. With a s ...
in
Washington Washington commonly refers to: * Washington (state), United States * Washington, D.C., the capital of the United States ** A metonym for the federal government of the United States ** Washington metropolitan area, the metropolitan area centered o ...
. Named after A.D. Wilson, who was part of an early ascent of Mount Rainier, the body of ice has an area of and has a volume of 1.9 billion feet3 (54 million m3). The glacier is directly feeds ice to the adjacent, but much larger
Nisqually Glacier The Nisqually Glacier is one of the larger glaciers on the southwestern face of Mount Rainier in the U.S. state of Washington (U.S. state), Washington. The glacier is one of the most easily viewed on the mountain, and is accessible from the Paradi ...
. Starting from the head at , the glacier flows downhill southward. One part of the glacier meets the Nisqually Glacier at and the other part of the glacier ends on a cliff in between the Wilson and Nisqually Glacier at . Meltwater from the glacier feeds the
Nisqually River The Nisqually River is a river in west central Washington in the United States, approximately long. It drains part of the Cascade Range southeast of Tacoma, including the southern slope of Mount Rainier, and empties into the southern end of Pu ...
.


See also

*
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 deform ...


References

{{Glaciers of Mount Rainier Glaciers of Mount Rainier Glaciers of Washington (state)