The Cordilleran Ice Sheet covered most of north-west North America for much of the last 2.6 million years. At the Last Glacial Maximum during the Last Glacial Period(26,500 years ago), the Cordilleran Ice Sheet likely covered as much as 2.5 million square kilometres. Stretching from Alaska to Oregon, British Columbia was entirely covered in ice that in many places over two kilometres thick. At the Continental Divide of North America the Cordilleran Ice Sheet merged with the Laurentide Ice Sheet.
The Cordilleran and Laurentide ice sheets combined covered most of North America and held one and a half times more water than the Antarctic Ice Sheet does today. Interestingly, the Cordilleran Ice Sheet did not cover most of Alaska(north of the Alaska Ridge) due to the climate being too dry to produce lasting glaciers. Another remarkable feature of the Cordilleran Ice Sheet is how quickly it disappeared relative to the Laurentide Ice Sheet. It is thought, and it really only is a thought, that the Laurentide took eleven thousand years to disappear, whereas the Cordilleran only about four thousand years. Ice ages are bewilderingly complex and it is hard to get a grasp on how so many barely understood variables combine to move us into and out of ice ages. The best we can do is hone in on more graspable aspects of glaciation and try to piece together an enormous puzzle. Approximately 9000 years ago the Cordilleran Ice Sheet was in rapid retreat and Mount Price was an active volcano. Lava flowing from Mount Price met the ice wall that filled Cheakamus Valley and formed The Barrier. The Barrier allowed Garibaldi Lake to form, where previously it was a valley extending into Cheakamus Valley. The Barrier is just one of many striking geologically formed features of Garibaldi Park close to Whistler. The Table and Black Tusk are two other bizarre and beautiful mountains produced through volcanoes pushing through the enormous Cordilleran Ice Sheet.
The Table is thought to have formed just a few thousand years ago when the Cordilleran Ice Sheet covered much of northwest North America. In 1951 Canadian Geologist Bill Mathews pieced together how this interesting mountain formed. He theorized that magma must have melted a vertical tube through to the surface of the Cordilleran Ice Sheet. The pooling lava cooled and hardened into a flat topped mountain. The lack of glacier erosion around The Table indicates that it formed at the end of the last ice age when the Cordilleran Ice Sheet was in quick retreat. So, looking across from Black Tusk to The Table you can try to visualize the land all around buried in an ice sheet about level with where you are standing. About 12000 years ago, there was a pure white sea of ice all around, and an unseen column of lava melting to the surface like a molten rock lake. What a sight it must have been with a cauldron of lava in the midst of a glacier hundreds of metres thick. While studying The Table as well as others in norther British Columbia, Bill Mathews referred to these flat topped mountains as tuyas. He called them tuyas after the Tuya River and Tuya Range in northern British Columbia.
More Whistler & Garibaldi Park Hiking A to Z!
Coast Douglas-fir trees are medium to extremely large trees that you will encounter in Whistler and Garibaldi Park. They are the second tallest conifer ...
The Garibaldi Volcanic Belt is a line of mostly dormant stratovolcanoes and subglacial volcanoes largely centred around Whistler and extending through much ...
Columnar Jointing: bizarre looking columns of oddly angular rock formations that can be found in many places around Whistler and worldwide. Generally ...
Armchair Glacier is one of the many easily identifiable mountain features around Whistler. Along with Wedge Mountain and Black Tusk, Armchair Glacier has a ...
The second Caterpillar tractor in Parkhurst Ghost Town is considerably harder to find despite being just a few metres from the hulking Caterpillar at the shore ...
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 ...
Overlord Mountain is the highest peak in the Fitzsimmons Range. Overlord is surrounded by several mountains that collectively are named the Overlord ...
Parkhurst Ridge is an incredible place for a lot of reasons. Of course, the view is spectacular with Green Lake's absurdly vivid green coloured water. ...
Cheakamus River is a beautiful, crashing, turquoise coloured river that flows from Cheakamus Lake, through Whistler Interpretive Forest, then down past Brandywine Falls to Daisy Lake, then all the way to ...
Ring Lake is a fantastically serene and wonderfully remote lake similar to Cirque Lake, but considerably farther to hike to reach it. The 10 kilometre(6.2 mile) hike takes you through a rarely hiked forest, ...
The short, winding, and ever-changing hiking trail to Rainbow Falls is the same as the much more popular trailhead for Rainbow Lake. The trailhead is marked as the Rainbow Trail, and the trail quickly ...
The Sproatt East trail is a beautifully wild, steep, but relatively short trail to the magnificent, wide open alpine and summit of Mount Sproatt. Mount Sproatt (1834 metres) towers over Whistler Valley ...
April in Whistler is a wonderful time of year. The winter deep freeze ends and T-shirt weather erupts. The village comes alive with overflowing patios and ...
May is an extraordinarily beautiful time of year in Whistler. The days are longer and warmer and a great lull in between seasons happens. Whistler is fairly ...
June is a pretty amazing month to hike in Whistler and Garibaldi Park. The average low and high temperatures in Whistler range from 9c to 21c(48f/70f). ...
July is a wonderful time to hike in Whistler and Garibaldi Provincial Park. The weather is beautiful and the snow on high elevation hiking trails is long ...
Hiking in Whistler is spectacular and wonderfully varied. Looking at a map of Whistler you see an extraordinary spider web of hiking trails that are unbelievably numerous. Easy trails, moderate trails and challenging hiking trails are all available. Another marvellous ...
Squamish is located in the midst of a staggering array of amazing hiking trails. Garibaldi Provincial Park sprawls alongside Squamish and up and beyond Whistler. Tantalus Provincial Park lays across the valley to the west and the wonderfully remote Callaghan Valley ...
Clayoquot Sound has a staggering array of hiking trails within it. Between Tofino and Ucluelet, Pacific Rim Park has several wilderness and beach trails, each one radically different from the last. The islands in the area are often Provincial parks on their own with ...
Victoria has a seemingly endless number of amazing hiking trails. Most take you to wild and beautiful Pacific Ocean views and others take you to tranquil lakes in beautiful BC Coastal Rainforest wilderness. Regional Parks and Provincial Parks are everywhere you turn in ...
The West Coast Trail was created after decades of brutal and costly shipwrecks occurred along the West Coast of Vancouver Island. One shipwreck in particular was so horrific, tragic and unbelievable that it forced the creation of a trail along the coast, which ...