Boulder Glacier
From Wikipedia, the free encyclopedia
| Boulder Glacier | |
|---|---|
 |
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| Type | Mountain glacier |
| Location | Washington, U.S. |
| Coordinates | |
| Area | 950 acres (3.85 km²) est. |
| Length | 1.5 miles (2.4 km) est. |
| Terminus | Moraine |
| Status | Retreating |
Boulder Glacier is located on the southeast slope of Mount Baker, a stratovolcano near the Pacific coast of North America in the Cascade Range of Washington. Boulder Glacier is the sixth largest on Mount Baker with an area of 3.4 km² (Post et al. 1971). It flows from the summit crater between Grant Peak (10781 feet) and Sherman Peak (10140 feet) to about 5000 feet. It is noteworthy for retreating 450 m between 1987 and 2005 leaving newly exposed rock and soil behind.[1]
Between 1850 and 1950, the glacier retreated 2650 m. William Long of the United States Forest Service observed the glacier beginning to advance due to cooler/wetter weather in 1953. This was followed by a 743 m advance by 1979. The 1979 terminus position is where the small stream enters Boulder Creek from the southwest. Observations in 2005 suggest that the lowest several hundred meters of the glacier is stagnant and will likely disappear. In the pictures, this section of the glacier is gray with rock debris and has few crevasses. On the west side of Boulder Creek is a small waterfall revealed by the recent recession of the glacier.
Boulder Glacier may be approached via the Boulder Ridge Trail number 605. The trail passes through a climax community of pacific silver fir and related species of disparate ages with many standing snags. In the fall, a large variety of mushroom species emerge. Near 4300 feet elevation, the trail ascends a lateral glacial moraine. At 4600 feet, the route ascends about 20 feet of Class 2 rock and 120 feet of steep subalpine forest to reach the ridge crest. Soon thereafter, the trail disappears.
Boulder Ridge consists of scenic heather-covered benches and a number of lateral moraines left by vanished glaciers. Glacial retreat has left the upper portion of the ridge barren and unstable and rockfall from the terminus of that portion of the glacier is a hazard to the unwary visitor.
Boulder Glacier is one of the more popular climbing routes on Mount Baker. First climbed on August 24 1891, it is most often ascended in combination with the cleaver between Boulder and Park Glacer to the north to bypass densely crevassed sections of the glacier. At about 10,000 feet elevation, the route passes to the southwest of steep rock and ice to reach the summit ridge east of Grant Peak.
 Boulder Glacier in 2003 with its 1985 terminus in red |
 View of 2004 terminus from above |
 View from Boulder Ridge |
[edit] See also
[edit] References
- Post, A., D. Richardson, W.V. Tangborn, and F.L. Rosselot (1971). "Inventory of glaciers in the North Cascades, Washington". USGS Prof. Paper 705-A: A1-A26.
- Pelto, M., C. Hedlund (2001). "Terminus behavior and response time of North Cascade glaciers, Washington, U.S.A.". Journal of Glaciology 47 (158): 496-506.
- Beckey, Fred (1995). Cascade Alpine Guide: Climbing and High Routes : Rainy Pass to Fraser River. Mountaineers Books; 2nd edition. ISBN 0-89886-423-2.
[edit] External links
- North Cascades: Glacier Retreat North Cascade Glacier Climate Project
- Maps and aerial photos
- WikiSatellite view at WikiMapia
- Topographic map from TopoZone
- Aerial image from TerraServer-USA
- Surrounding area map from Google Maps
- Location in the United States from the Census Bureau
