While camped at the Lake Louise Tent Campground, Alberta, Canada described in my last post, we had the pleasure of touring the Columbia Icefield and the Athabasca Glacier. Located about an hour north of Lake Louise, the glacier and icefield are located in Jasper National Park.
The Athabasca Glacier covers an area of 6 kilometers, being 3.75 miles long with a depth of between 270 and 1000 feet depending on the location. The glacier is fed by the Columbia Icefield, the largest body of ice in the Rocky Mountains, with its greatest depth estimated to be 1200 feet. The icefield drains into the Pacific, Arctic and Atlantic Oceans.
An icefield is formed when snow that falls on mountain peaks and plateaus accumulates year after year with little summer melt. When the snow reaches a depth of approximately 100 feet, the bottom layers become pressurized into ice. As more snow falls on top and the depth of the ice increases, it eventually overflows into the surrounding valleys and begins to flow downhill and a baby glacier is born.
This glacier and icefield once formed part of an enormous ice sheet that carved the landforms seen today throughout the Rocky Mountains. Its journey lasted many centuries. The knowledgeable tour guides on the snocoach informed us that most of the glaciers in North America are melting and decreasing in size as the summer’s melt each year is greater than the winter’s accumulation. They showed some amazing photos of the remarkable decline of the size of the Athabasca Glacier, just in the past 30-40 years. Apparently, our use of fossil fuels, destruction of our forests and industrial gases such as chlorofluorocarbons are causing a global warning trend called the Greenhouse Effect which is hastening the rates of glacial retreat and leading to the icefield’s loss of volume.
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