- Glacier Peak Wilderness
Infobox_protected_area | name = Glacier Peak Wilderness
iucn_category = Ib
caption =
locator_x = 32
locator_y = 14
location =Washington , USA
nearest_city = Seattle, WA
lat_degrees = 48
lat_minutes = 06
lat_seconds = 45
lat_direction = N
long_degrees = 121
long_minutes = 06
long_seconds = 50
long_direction = W
area = 572,000 acres (2315 km²)
established =1964
visitation_num =
visitation_year =
governing_body =United States Forest Service The Glacier Peak Wilderness, created by Congress in the original 1964 wilderness legislation, is located within portions of Chelan County, Snohomish County, and Skagit Counties in the
North Cascades ofWashington . The area, 572,000 acres (2315 km²) in size, 35 miles (56 kilometers) long and 20 miles (32 kilometers) wide, is characterized by heavilyforest edstream courses, steep sidedvalley s, and dramatic glacier-crowned peaks.Ecology
Forest vegetation comprises several species of
fir ,Douglas-fir , hemlock, redcedar as well as stands of mixedpine andDouglas-fir on its eastern slopes. Various species of wildlife inhabit the area and includedeer ,elk , black bear,mountain goat ,cougar ,marten , andlynx . Smaller animals, such as field mice are common. The high mountainlake s often give good catches of fish during their ice-free months. The primary fishery iscutthroat trout , however, other species do exist.Access
No roads approach
Glacier Peak , and one must hike many miles through extremely rough terrain to reach its base. Normally, hikers can reach the volcano from the west via theWhite Chuck Valley , or theSuiattle River Valley; from the east, it may be approached from the western tip ofLake Chelan .Trail conditions
Most years the Wilderness is still buried under 10-20 feet (3-6 m) of
snow in May. Usually most trails and passes are snow free by mid-August, but this varies from year to year. Snow and cold rain can occur in mid-summer.Flood damage
On
October 20 ,2003 , there was a record-settingflood event when over 10 inches (250 mm) ofrain fell on the Wilderness. The warm rain meltedsnow andice driving massive amounts of water, trees and debris into the rivers. Downstream, roads, bridges, campgrounds and trails were damaged and destroyed. The destruction was particularly devastating to thePacific Crest Trail (PCT). Eight trail bridges and one stream ford on a 30-mile section of the trail below Glacier Peak were destroyed. Little or no evidence remains that some of these bridges ever existed. The two most notable losses were bridges over the Upper White Chuck River and the Suiattle River. Both crossings are dangerous fords under the best of conditions. Additionally, five major trails that provided access to the PCT in the area sustained varying degrees of damage from fairly light (North Fork Skykomish Trail) to severe (White Chuck Trail).Kennedy Hot Springs was buried in amudslide and completely destroyed.See also
*
Dome Peak
*Ptarmigan Traverse External links
* [http://www.fs.fed.us/r6/mbs/recreation/special/wilderness/glacier_peak.shtml USFS home page of Wilderness] (adapted PD source)
* [http://www.fs.fed.us/r6/mbs/conditions/trail-flood-damage-status.shtml USFS web page about flood damage] (adapted PD source)
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