Accumulation Zone Vancouver Hiking Terms
Accumulation Zone: the area where snow accumulations exceeds melt, located above the firn line. Snowfall accumulates faster than melting, evaporation and sublimation removes it. Glaciers can be shown simply as having two zones. The accumulation zone and the ablation zone. Separated by the glacier equilibrium line, these two zones comprise the areas of net annual gain and net annual loss of snow/ice. The accumulation zone stretches from the higher elevations and pushes down, eventually reaching the ablation zone near the terminus of the glacier where the net loss of snow/ice exceeds the gain. The Wedgemount Glacier in Garibaldi Provincial Park in Whistler is an ideal place to see an accumulation zone up close. From across Wedgemount Lake you can see the overall picture of both the accumulation zone and ablation zone of a glacier. The Wedgemount Glacier is also relatively easy and safe to examine closely and hike onto. The left side of the glacier is frequented in the summer and fall months by hikers on their way to Wedge Mountain and Mount Weart. Click the image above to see an aerial view of Overlord Glacier and the accumulation zone is visible to the left of the Fissile. Click the image below to see an aerial video of the Wedge Glacier. Wedgemount Lake itself is a magnificent destination for a day hike or spectacular overnight beneath the dazzling mountain peaks and stars. Many sleep under the stars on one of the many beautiful tent platforms that dot the landscape. Solidly built, wooden tent platforms are everywhere you look at Wedgemount Lake. Strategically positioned, these platforms manage to maintain an amazingly secluded feel despite their numbers. In all Wedgemount Lake has 20 of these tent areas. Most are wooden, but several down by the lake shore are gravel, yet every bit as nice. At a fast hiking pace you can reach Wedgemount Lake from the trailhead in just an hour and a half but at a leisurely or backpack laden pace you will likely take over two hours. The trail is well marked and well used. The steepness of the trail doesn't require any technical skill, however that last kilometre before the lake you will be scrambling on all fours quite a bit. Glossary of Hiking Terms Vancouver Hiking Trails
Highpointing: the sport of hiking to as many high points(mountain peaks) as possible in a given area. For example, highpointing the Hoary Marmot: the cute, invariably pudgy, twenty plus pound ground squirrels that have evolved to live quite happily in the hostile alpine areas of much of the world. In the northwest of North America, marmots have a distinct grey in their hair, a hoary colour, so have been named hoary marmots. They manage to survive Ice Mill: a hole in the glacier formed by swirling water on the surface. These can be large enough for a human to slip into. Nunatuk: a rock projection protruding through permanent ice or snow. Old Man's Beard(Usnea): The lichen seen hanging from tree branches in much of British Columbia. It hangs from tree bark and tree branches looking like greenish-grey hair. A form of lichen, usnea can be found world-wide. There are currently over 85 known species of usnea.
Post Holing: difficult travel through deep snow where feet sink. A common occurrence while hiking in and around Whistler in the spring and early summer months. The alpine trails are often covered in snow well into June and some trails into July. It is not unusual to see hikers in Whistler starting a trail in 25c weather in June with snowshoes strapped to their packs. Post holing can be very frustrating and arduous. The hard crust on top of the snow can sometimes support the weight of footsteps, however, often it is not, and one's foot will plunge deep into the snow.
Pyramidal Peak: a mountaintop that has been carved by glaciation into a distinct, sharp horn-like shape. The Matterhorn in the Alps is a well know example of this striking phenomenon. Retreation Glacier: a deteriorating glacier; annual melt of entire glacier exceeds the flow of the ice. Glaciers around Whistler and Garibaldi Provincial Park are retreation glaciers owing to the past few decades of warming temperatures. Scree: from the Norse “skridha”, landslide. The small, loose stones covering a slope. Also called talus, the French word for slope. Scree is mainly formed from the annual freeze/thaw periods of spring and fall, where water seeps into cracks in the rock and expands when freezing. Seracs: large pinnacles or columns of ice that are normally found in icefalls or on hanging glaciers. Snow Bridge: a structure of snow that fills in an opening such as a crevasse or a creek. Often Surging Glacier: annual flow of the ice exceeds the melt; the movement is measurable over a period of time. Talus: a sloping jumble of boulders at the base of a cliff.
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