'Gannett Glacier' is the largest
glacier in the
Rocky Mountains within the
United States. The glacier is located on the east and north slopes of
Gannett Peak, the highest mountain in
Wyoming, in the
Fitzpatrick Wilderness of
Shoshone National Forest.
[1]
As is true with most glaciers around the world, Gannett Glacier is slowly disappearing.
Photographic evidence clearly demonstrates that there has been an enormous reduction in the area of the glacier since the 1920's. The area of the glacier was estimated in 1950 to be and was measured in 1999 to be . Measurements taken in 1958 and again in 1983 showed a depth reduction of over 25 years.
[2] A general warming pattern and a reduction in moisture is widely believed to be the reason for the
glacier retreating.
[ Vanishing Glaciers in the Wind River Range ] Numerous other glaciers are located in the immediate area including six more that are within the top ten in size within the Rocky Mountains of the U.S.
In a 1989 study, both Gannett and
Dinwoody Glaciers were researched to determine the amount of melt water they supplied to streams. Both glaciers supply melt water which flows into Dinwoody Creek, which in turn flows into the
Wind River. The melt water was found to have contributed increasingly lower amounts to the total water supplied to Dinwoody Creek. This has been attributed to the glaciers thinning and retreating, especially since 1950, when Gannett Glacier was measured to be almost 20 percent larger than in 1999.
[3] The impact on reduced stream flow from Gannett Glacier due to glacial retreat affects more than just the amount of water available for the local ecosystem and downstream agricultural and ranching interests. Cool water fish species including the
Brook Trout,
Cutthroat Trout and
Rainbow Trout could see a loss of habitat and
spawning areas as water temperatures rise due to less glacier ice melt.
Cited references
1. USGS Gannett Peak (WY) Topo Map
2. Glaciers shrinking
3. Glacial Icemelt in the Wind River Range, Wyoming
See also
★
List of glaciers