Gendarme Sea to Sky Hiking Terms
Gendarme: a pinnacle sticking up out of a ridge. A steep sided rock formation along a ridge, “guarding” the summit. From the French ”man-at-arms”.
The picture above is from Levette Lake, a nice mountain lake located in the enormous Squamish Valley that drains the Squamish River into Howe Sound. There are some nice views and minimal elevation gain along the trail. The amazing Tantalus Range and Mount Garibaldi on a sunny day look fantastic from the shores of Levette Lake. There is a nice campground on the shore of the lake that is well laid out and very rustic. It is located just a couple hundred metres from the parking area at the trailhead. The campground is very basic and quite nice. You won't find signs, garbage bins or any annoying signs of humanity to take away from the wonderful view of the lake and Tantalus Range across the lake.
You will encounter gendarme's frequently in Whistler and Garibaldi Provincial Park. Wedgemount Lake, Joffre Lakes, Whistler and Blackcomb mountains all have visible gendarme's. Click the image above to see an aerial video of Wedgemount Lake in Whistler.
Joffre Lakes is one of the most beautiful lakes you are likely to ever see. There are three lakes and they get progressively more beautiful. By the third lake the intense blue is breathtaking. The mighty Matier Glacier rises above the third lake, making the experience even more spectacular. The trail is rough and tricky in some parts, but not terribly difficult. The trail is 5.5k to the third lake so give yourself 1.5 - 2 hours(one way). Lots of trail construction work is being done as a new trail replaces much of the old trail. The old boulder section between the lower and middle lakes has now been covered with a new dirt trail.
Glossary of Hiking Terms Squamish Hiking Terms
Ablation Zone: the annual loss of snow and ice from a glacier as a result of melting, evaporation, iceberg calving, and sublimation which exceeds the accumulation of snow and ice. Located below the firn line. Firn originated from Swiss German and means "last year's snow". It has been compacted and recrystallized making it harder and more compact than snow, though less compact than glacial ice. An excellent place to see an ablation zone is Wedgemount Lake in Garibaldi Provincial Park in Whistler. The Wedgemount Glacier has been receding for decades. In the 1970's the glacier terminated with a steep and vertical wall of ice at the shores of Wedgemount Lake. Today the glacier terminates a couple hundred metres above Wedgemount Lake.
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.
Highpointing: the sport of hiking to as many high points(mountain peaks) as possible in a given area. For example, highpointing the lower 48 states in the United states. This was first achieved in 1936 by A.H. Marshall. In 1966 Vin Hoeman highpointed all 50 states. It is estimated that over 250 people have highpointed all of the US states. Highpointing is similar peakbagging, however peakbagging is the sport of climbing several peaks in a given area above a certain elevation. For example, a highpointer may climb the summit of Wedge Mountain, the highest peak in the Garibaldi Ranges, then move to another mountain range. Whereas a peakbagger may summit Wedge Mountain, then Black Tusk, Panorama Ridge, Mount Garibaldi and many more high summits in the region.
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 quite happily in the alpine, largely by hibernating for 8 months of the year and largely for having a surprisingly varied array of food in such an inhospitable environment. They live off of grasses, berries, lichens, mosses, and roots and flowers. And live quite well it seems, as they always look chubby, which has one great drawback. They are sought after by bears and wolves. They have a wonderful defense system though. They are constantly on watch and whistle loudly at the first sign of danger, alerting the colony. The prevalence of these "whistlers" as they came to be locally called, in the early days of London Mountain resulted in it's name being changed to Whistler Mountain in the 60's. Hiking on Whistler, Blackcomb or Wedgemount Lake in the summer will almost guarantee an encounter with a chubby, jolly little whistler marmot..
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.
Krummholz: low-stunted trees found in the alpine. From the German “twisted wood”. Continuous exposure to hostile, alpine weather causes trees to form in bizarre and stunted ways. Many types of trees have formed into bizarre krummholz trees including spruce, mountain pine, balsam fir, subalpine fir, limber pine and lodgepole pine. The lodgepole pine is commonly found in the alpine regions around Whistler.
Nunatuk: a rock projection protruding through permanent ice or snow. Their distinct appearance in an otherwise barren landscape often makes them identifiable landmarks. Nunatuks are usually crumbling masses of angular rock as they are subject to severe freeze/thaw periods. There is a very prominent nunatuk near the glacier window of the Wedge Glacier. The glacier has been retreating in the past few years, so this massive nunatuk marks the terminus of the glacier now.
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.
Pressure Ridges: wavelike ridges that form on a glacier normally after a glacier has flowed over icefalls. Pressure ridges are a beautiful and hostile looking feature of glaciers that, when approached, become menacingly huge and dangerous.
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.
Tarn: a small alpine lake. The word tarn originates from the Norse word tjorn which translates to English as pond. In the United Kingdom, tarn is widely used to refer to any small lake or pond. In British Columbia however, tarn is used specifically for small mountain lakes. Around Whistler tarns number in the hundreds and many are so small and/or hidden as to remain unnamed. Russet Lake in Garibaldi Provincial Park could be called a tarn, however its relatively large size dominates the area and the term lake seems more appropriate. The nearby Adit Lakes are more accurately called tarns as they are small, shallow and sit in an alpine zone, buried in snow most of the year.