Ablation Zone: the lower altitude region of a glacier where there is a net loss of ice mass due to melting, sublimation, evaporation, ice calving or avalanche.  The ablation zone of a glacier such as the Wedge Glacier has meltwater features such as englacial streams and a glacier window.  An englacial stream refers to meltwater flowing inside a glacier.  A glacier window is a cave-like opening at the mouth of a glacier where meltwater runs out.

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 on a glacier. 

Russet Lake sits in a wide, glacier carved valley at the base of The Fissile.  In the direction opposite The Fissile, up on a plateau less than a kilometre away are two small tarns called Adit Lakes.  Adit Lakes sit in a broad, boulder strewn alpine zone with an incredible view of Spearhead Range.  Just a few metres from Adit Lakes the plateau drops off quickly into the huge valley that separates the Spearhead Range and Fitzsimmons Range.

Aiguille: a tall, narrow, characteristically distinct spire of rock. From the French word for "needle". Used extensively as part of the names for many peaks in the French Alps.  Around Whistler and in Garibaldi Park you will find several distinct aiguilles.  Shown here is the prominent aiguille that stands like a tower at the summit of Rethel Mountain above Wedgemount Lake.  Standing near the hut at Wedgemount Lake, Rethel is the towering mountain directly across the lake.

Alpine Zone or Alpine Tundra is the area above the treeline, often characterized by stunted, sparse forests of krummholz and pristine, turquoise lakes.  Mount Sproatt is an excellent example of an alpine zone in Whistler.  Dozens of alpine lakes, rugged and rocky terrain and hardy krummholz trees everywhere you look.  The hostile, cold and windy climate in the alpine zones around Whistler make tree growth difficult.  Added to that, the alpine areas are snow covered the majority of the year. 

Arête: a thin ridge of rock formed by two glaciers parallel to each other. Sometimes formed from two cirques meeting. From the French for edge or ridge.  Around Whistler and in Garibaldi Provincial Park you will see dozens of excellent examples.  At the Wedge-Weart Col above and beyond Wedgemount Lake is a prominent arête that links these two highest mountains in Garibaldi Park.  Wedge Mountain is 2892 metres(9488 feet) and Mount Weart is 2835 metres(9301 feet).

Twentyone Mile Creek begins its long and steep journey from Rainbow Lake, high up and between Mount Sproatt and Rainbow Mountain.  Cutting between the two mountains, Twentyone Mile Creek flattens out somewhat, passes under Alta Lake Road, then winds its way through a deep and dark forest before flowing into the River of Golden Dreams near the end of Lorimer Road.  This hidden forest extends from Rainbow Park to Emerald Forest and between Alta Lake Road and the River of Golden Dreams.

Armchair Glacier is one of the many easily identifiable mountain features around Whistler.  Along with Wedge Mountain and Black Tusk, Armchair Glacier has a distinct shape that it is named after.  Armchair Glacier can be seen from a considerable distance and from many places in Whistler.  In the winter it is a solid white ridge with three peaks and in the summer the ridge and peaks are bare rock and the glacier can be seen as a solid, horizontal line below. 

The Barrier formed as a result of huge lava flows from Clinker Peak on the west shoulder of Mount Price during the last ice age.  About thirteen thousand years ago, the Cheakamus River valley was filled by an enormous glacier, part of the Cordilleran Ice Sheet.  Lava flowed from Clinker Peak and pressed up against the massive glacier.  The lava ponded and formed what geologists call an ice-marginal lava flow.  

Whistler, the surrounding mountains, and Garibaldi Provincial Park are home to two types of bears.  Black bears and grizzly bears.  Black bears are frequently seen throughout the valley and often in Whistler Village.  Grizzly bears, on the other hand, are rarely seen, and only deep in the wilderness, well away from Whistler Village.  Black bears around Whistler are generally skittish and will flee into the forest when approached by people.

Bench: a flat section in steep terrain.  Characteristically narrow, flat or gently sloping with steep or vertical slopes on either side.  A bench can be formed by various geological processes.  Natural erosion of a landscape often results in a bench being formed out of a hard strip of rock edged by softer, sedimentary rock.  The softer rock erodes over time, leaving a narrow strip of rock resulting in a bench.  Coastal benches form out of continuous wave erosion of a coastline.  

Bergschrund or abbreviated schrund: a crevasse that forms from the separation of moving glacier ice from the stagnant ice above. Characterized by a deep cut, horizontal, along a steep slope. Often extending extremely deep, over 100 metres down to bedrock. Extremely dangerous as they are filled in winter by avalanches and gradually open in the summer.  The Wedgemount Glacier at Wedgemount Lake is a great way to view bergschrund up close in Whistler. 

Bivouac or Bivy: a primitive campsite or simple, flat area where camping is possible.  Traditionally used to refer to a very primitive campsite comprised of natural materials found on site such as leaves and branches or simply sleeping under the stars.  Often used interchangeably with the word camp, however, bivouac implies a shorter, quicker and much more basic and naturally constructed camp setup.  

Cairn: a pile of rocks used to indicate a route or a summit.  The word cairn originates from the Scottish Gaelic word carn.  A cairn can be either large and elaborate or as simple as a small pile of rocks.  To be effective a cairn marking a trail has to just be noticeable and obviously man-made.  In the alpine areas around Whistler, above the treeline, cairns are the main method of marking a route.  In the spring and fall when snow covers alpine trails, cairns mark many routes.

Chimney: a gap between two vertical faces of rock or ice.  Often a chimney offers the only viable route to the summit of a mountain.  An example of this is Black Tusk in Garibaldi Provincial Park in Whistler.  The final ascent of Black Tusk requires climbing a near vertical chimney with crumbling rock all around.  Black Tusk is the extraordinarily iconic and appropriately named mountain that can be seen from almost everywhere in Whistler. 

Cirque: a glacier-carved bowl or amphitheatre in the mountains.  To form, the glacier must be a combination of size, a certain slope and more unexpectedly, a certain angle away from the sun. In the northern hemisphere, this means the glacier must be on the northeast slope of the mountain, away from the suns rays and the prevailing winds. Thick snow, protected in this way, grows thicker into glacial ice, then a process of freeze-thaw called nivation, chews at the lower rocks, hollowing out a deep basin.

The Cloudraker Skybridge and the Raven’s Eye Cliff Walk are new additions to the summit of Whistler Mountain.  The Cloudraker Skybridge stretches 130 metres from just steps from the top of the Peak Express Chair across to the West Ridge.  The Raven’s Eye Cliff Walk is a viewing platform that extends over 12 metres up and out from the West Ridge.  Both of these exhilarating viewing areas tower way above Whistler Bowl.

The Coast Mountains run from the Yukon down to Vancouver along the west coast of British Columbia in a band that averages 300 kilometres wide(190 miles).  The length of the Coast Mountains is roughly 1600 kilometres(1000 miles).  They are often referred to as the BC Coastal Range or the Coast Range.  The Coast Mountains are comprised of three mountain ranges, the Pacific Ranges, the Kitimat Ranges, and the Boundary Ranges.

Col: a ridge between two higher peaks, a mountain pass or saddle.  More specifically is the lowest point on a mountain ridge between two peaks.  Sometimes called a saddle or notch.  The Wedge-Weart Col is a popular destination at the top of Wedgemount Glacier.  The Wedge-Weart Col connects these two highest peaks in Garibaldi Provincial Park and is easily visible from much of the area around Wedgemount Lake.

Crevasse: is a split or crack in the glacier surface, often with near vertical walls.  Crevasses form out of the constant movement of a glacier over irregular terrain.  Crevasses are both revered for their dramatic beauty and feared for their inherent danger.  Crevasses are often dozens of metres deep and less than a metre wide.  The fear of slipping into one of these treacherously narrowing chasms is well founded. 

Deadfall means a tangled mass of fallen trees and branches.  There are several name variations for fallen trees that are commonly used in Whistler.  Windthrow, blowdown and windsnap are used somewhat interchangeably with deadfall.  Deadfall is a more generalized term that literally means dead and fallen, as in a dead and fallen tree.  Windthrow and blowdown, however are more specifically used to refer to trees blown over and uprooted by strong winds during storms. 

Erratic or Glacier Erratic is a piece of rock that has been carried by glacial ice, often hundreds of kilometres.  Characteristic of their massive size and improbable looking placement.  Erratics are frequently seen around Whistler and Garibaldi Provincial Park.  Either as bizarre curiosities or a place to relax in the sun.  On a sunny day, a large sun-facing erratic will often be warm and sometimes even hot, providing a comfortable and surreal place to rest. 

The Fissile is the stunning Matterhorn-looking mountain that is visible from Village Gate Boulevard in Whistler.  Looking up from Village Gate you will see the distant Peak2Peak Gondola spanning Whistler Mountain and Blackcomb Mountain.  In the background distance you will see The Fissile.  In the bright sunshine of summer it will be vibrantly coloured red.  In the evening it turns dark red then fades into an ominous black.  In the winter months, of course, The Fissile is a striking, white pyramid. 

Fitzsimmons Creek is the beautiful and huge creek that crashes through Whistler Village.  When walking from Whistler Village to the Upper Village, you will cross the nice, covered bridge over Fitzsimmons Creek.  It passes through Whistler Village and pours into Green Lake at the north end of Whistler.  Fitzsimmons Creek originates from Overlord Glacier and Russet Lake, about 12 kilometres up the valley that separates Whistler Mountain and Blackcomb Mountain.

The Fitzsimmons Range is a subsection of the Garibaldi Ranges that covers the area between the valleys of Cheakamus Lake and Fitzsimmons Creek.  Fitzsimmons Creek cuts between Whistler Mountain and Blackcomb Mountain and largely originates from the Fitzsimmons Glacier.  The Fitzsimmons Glacier and Mount Fitzsimmons are part of the Overlord Massif, which gets its name from the highest peak in the area, Overlord Mountain. 

The Garibaldi Ranges are a subdivision of the Pacific Ranges of the Coast Mountains.  Deriving its name from Mount Garibaldi, the Garibaldi Ranges cover the huge stretch of mountains between two enormous river valleys.  The Lillooet River valley on the east side and the Cheakamus River/Green River valley on the west.  Whistler is located on the west edge of the Garibaldi Ranges, while Pemberton near the north end and Vancouver at the south end. 

The Garibaldi Volcanic Belt is a line of mostly dormant stratovolcanoes and subglacial volcanoes largely centred around Whistler and extending through much of the Coast Mountains. Divided into sections with the Mount Garibaldi Area at the southern end and the Mount Cayley area southwest of Whistler.   The Mount Meager Area is west of Pemberton and the Bridge River Cones Area northwest of the Meager Area.   

Inosculation is the technical name for two or more trees that have fused together into a single bizarre looking tree. They are colloquially known as gemels, a name derived from the Latin word gemellus which means "a pair" or "twin". Gemels are a natural phenomenon where trees of the same species grow close enough to rub against each other. Gradually the bark where the two trees contact each other wears away and exposes the cambium.

Glacier Window: the cave-like opening at the mouth of a glacier where meltwater runs out.  Glacier windows are often extraordinarily beautiful.  A blue glow often colours the inside and the walls are filled with centuries old glacial till.  You can often see deep into the clear walls and the enormous magnitude of a glacier can be appreciated from up close.  The popular and easily accessible glacier window at the terminus of the Wedge Glacier at Wedgemount Lake is a stunning example of this.

Green Lake is the marvellously vivid, green coloured lake just north of Whistler Village.  Driving north on the Sea to Sky Highway, Green Lake appears along the highway on your right.  The vivid colour is always impressive and on a sunny day can be spectacular.  One of the best(and easiest) places in Whistler to capture an extraordinary sunrise or sunset photo, is along the Green Lake viewpoint along the edge of the highway.

Hoary Marmots are the cute, pudgy, twenty plus pound ground squirrels that have evolved to live quite happily in the hostile alpine areas around Whistler.  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.

When you hike in the alpine in Whistler and Garibaldi Provincial Park, you will often encounter unbelievably hardy and sometimes mangled looking trees.  Weathering high winds, freezing temperatures, deep snow and usually growing where most other things can't.  These weather battered trees are called krummholz.  Krummholz is a German derived word that comes from two words, krumm and holz. 

Moraines are glacially deposited ridges of debris that accumulate at the sides or terminus of a glacier.  Lateral moraines form at the sides of glaciers and terminal moraines at the terminus of a glacier.  Terminal moraines mark the maximum advance of a glacier.  Moraines are made up of glacial debris ranging in size from enormous boulders to fine glacial flour.  Boulders and rocks in moraines are generally rounded due to the churning and grinding within the glacier as it moved.

Mount Garibaldi is the huge, potentially active volcano that Garibaldi Provincial Park is named after.  Mount Garibaldi also lends its name to the Garibaldi Ranges, the group of mountain ranges that fill Garibaldi Park.  A subsection of the Garibaldi Ranges is the Garibaldi Névé, which is the large icefield that stretches out along the east side of Mount Garibaldi.

If you make it to the summit of Wedge Mountain you will notice off in the distance a beautifully symmetrical mountain that stands out among the rest.  Surrounded by glaciers on all sides, Mount James Turner has an almost to perfect cone shape to it.  The third highest mountain in Garibaldi Provincial Park at 2703 metres(8868 feet), it is only surpassed by Wedge Mountain at 2892 metres(9488 feet) and Wedge's neighbour Mount Weart 2835 metres(9301 feet).

Northair Mine is a surreal little world of colourful murals on abandoned cement foundations, surrounded by an astoundingly tranquil little lake in a secluded forest.  Just a short logging road off of the Callaghan Valley Road takes you to this unusual little abandoned mine.  You would have driven by the turnoff if you have been to Whistler Olympic Park or Alexander Falls, both of which are just a couple kilometres away.

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 on Wedgemount Glacier, high up near the summit of Wedge Mountain.  Another nunatuk once stood down the glacier near Wedgemount Lake, however the glacier retreated above it several years ago.

Overlord Mountain is the highest peak in the Fitzsimmons Range.  Overlord is surrounded by several mountains that collectively are named the Overlord Massif.  Massif is a term geologists use to refer to a group of mountains that tends to move as a unit while shifted by movements of the crust.  The Overlord Massif is dominated by Overlord Mountain which is impressively visible from Whistler Village, Whistler Mountain and Blackcomb Mountain.

The Peak2Peak Gondola connects Whistler Mountain and Blackcomb Mountain at a dizzying height of 436 metres(1427 feet).  It runs all winter and in the summer when the mountains are open for sightseeing and hiking.  The Peak2Peak Gondola runs very fast as it carries up to 4100 people per hour at 7.5 metres per second or 16.8 miles per hour!

The Roundhouse Lodge is the centre of activity on Whistler Mountain.  It is where the Whistler Gondola drops off and next to where the Peak 2 Peak Gondola crosses to Blackcomb Mountain.  Restaurants, patios, gift shops and even an Umbrella Bar perched at the edge of the newly expanded patio with incredible mountain views.

The Rubble Creek trailhead is the main access point for many of the best hikes and sights in Garibaldi Provincial Park.  Rubble Creek is located midway between Whistler and Squamish, just 2 kilometres from the Sea to Sky Highway.  The name Rubble Creek is evidently quite appropriate when you reach the parking lot and see the remnants of what must have been a terrific rock slide not that long ago. 

The Spearhead Range is a subsection of the Garibaldi Ranges that runs in an arc that connects Whistler Mountain and Blackcomb Mountain.  The Spearhead Range is effectively the brother of the Fitzsimmons Range which runs east from the summit of Whistler Mountain to Russet Lake.  The Spearhead Range covers the area on the north side or Blackcomb Mountain side of Fitzsimmons Creek. 

 Standing on Black Tusk in Garibaldi Park is a wonderfully surreal experience.  About 170,000 years ago a lava dome formed here within a million year old extinct andesitic stratovolcano.  The ancient cinder-cone has crumbled away exposing the stunning jet-black mountain we see today.  Looking south from Black Tusk you get a beautiful view of another strikingly bizarre mountain, The Table.  Less than one kilometre from the shore of Garibaldi Lake, The Table rises over 530 metres to its extraordinary flat top.

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 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 pale green shub-like growths hanging from trees in the forests around Whistler is called usnea.  These bushy, coral-like fruticose lichens anchor to bark and branches on trees and hang like tinsel on a Christmas tree.  known as old man’s beard, usnea tends to thrive on dead and dying trees and is can appear to be harming their hosts.  They actually do no harm to trees and prefer dying ones for their lack of sunlight blocking canopy growth.