Columbia Icefield

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The Columbia Icefield is the largest ice field in North America's Rocky Mountains.<ref name="britannica"/> Located within the Canadian Rocky Mountains astride the Continental Divide along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of Banff National Park and partly in the southern end of Jasper National Park.<ref name="britannica"/><ref name="pc-athabasca"/> It is about Template:Convert in area, Template:Convert in depth and receives up to Template:Convert of snowfall per year.<ref name="pc-athabasca"/>

HistoryEdit

File:Mt. Alberta from the Columbia Icefield.jpg

Mount Alberta from a high shoulder of the Columbia Icefield; on the way to The Twins (N & S). The ramp to the right leads to the Stutfields (E & W)

The Columbia Icefield was formed during the Great Glaciation, or Illinoisan period (238,000 to 126,000 BCE).<ref name="sandford-23">Sandford 1993, p. 23.</ref> The initial advancement of the ice field ended during the latter millennia of the Early Wisconsinan period (73,000 to 62,000 BCE), around the time Homo sapiens began to appear on the earth.<ref name="sandford-23"/> The next major advance of the ice field occurred during the Late Wisconsinan period (18,000 to 9,000 BCE), which marked the end of the major intercontinental land mass bridges.<ref name="sandford-23"/> During the Crowfoot Glacier advance (9,000 to 7,000 BCE), humans were beginning to learn farming along the Tigris, Euphrates, and Nile rivers.<ref name="sandford-23"/> The last major period of advance occurred during the Little Ice Age, which lasted from about 1200 AD to 1900 AD. Around 1800, the Athabasca Glacier peaked, then went through a period of recession, and then advanced again until 1840, when it began receding until the present day.<ref name="sandford-23"/>

The Columbia Icefield was one of the last major geological features in western Canada to be visited and recorded by Europeans, due to its isolation and harsh weather conditions.<ref name="sandford-56">Sandford 1993, p. 56.</ref> In April 1827, Scottish botanist David Douglas was crossing Athabasca Pass—a major trading route located north of the Icefield—when he climbed one of the adjacent mountain peaks. He reported his first ascent in his journal, describing it to be Template:Convert in height.<ref name="sandford-56"/> In the summer of 1884, geology professor Arthur Philemon Coleman explored the Great Divide from Banff to Jasper in search of Douglas' giant peak.<ref name="sandford-56"/> While unsuccessful, he did discover the route that would become the Icefield Parkway.<ref name="sandford-56"/> In July 1898, British explorer J. Norman Collie and his friends Hugh Stutfield and Herman Wooley set off in search of Douglas' giants, equipped by the famous Banff outfitter Bill Peyto. On the morning of August 18, Collie and Wooley climbed the east side of Mount Athabasca, moved up the glacier when the ridge gave way to crumbling rock, and made their way to the summit, where they discovered an ice field that extended to almost every horizon.<ref name="sandford-56"/> Collie later wrote:

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In 1900, former British clergyman James Outram came to the Canadian Rockies to recover his health after a nervous breakdown.<ref name="sandford-58">Sandford 1993, p. 58.</ref> The following year he made the first ascent of Mount Assiniboine (Template:Convert), then considered the "Matterhorn of the Rockies".<ref name="sandford-58"/> In 1902, Outram made ten first ascents of peaks over Template:Convert and discovered four new mountain passes in the Columbia Icefield area.<ref name="sandford-58"/> Two of his first ascents in 1902 were Mount Columbia (Template:Convert) and Mount Bryce (Template:Convert), one of the most dangerous and difficult summits in the Rocky Mountains.<ref name="sandford-58"/>

Following World War I, other mountaineering firsts occurred. In 1923, American climbers James Munroe Thorington and W. S. Ladd joined Austrian guide Conrad Kain to summit the daunting North Twin Peak (Template:Convert), Mount Columbia, and Mount Saskatchewan (Template:Convert) in five days.<ref name="sandford-58"/> The following year, another American expedition led by William O. Field and guide Edward Feuz climbed both the North Twin Peak and the South Twin Peak (Template:Convert) in twenty-four hours—a combined distance of about Template:Convert.<ref name="sandford-58"/> In 1927, A. J. Ostheimer discovered a new route to the North Peak Summit, made first ascents of Stutfield Peak (Template:Convert) and Mount Kitchener (Template:Convert), and became the first climber to traverse the Snow Dome (Template:Convert) in 36 hours.<ref name="sandford-58-59">Sandford 1993, pp. 58–59.</ref> During his 63-day visit to the Columbia Icefield, Ostheimer and his two companions walked over a Template:Convert and climbed thirty peaks—twenty-five of which were first ascents.<ref name="sandford-59">Sandford 1993, p. 59.</ref>

In March 1932, three men undertook a remarkable skiing journey from Jasper to Banff that covered about Template:Convert.<ref name="sandford-59"/> When Cliff White, Joe Weiss, and Russell Bennet reached the Columbia Icefield, they climbed to the summit of Snow Dome, and then made a downhill run descent of almost Template:Convert which lasted for Template:Convert—the longest continuous ski run in Canadian history up to that point.<ref name="sandford-60">Sandford 1993, p. 60.</ref> Their accomplishment played a major role in generating worldwide interest in the Canadian Rockies.<ref name="sandford-60"/> Today, mountaineers and skiers from around the world come to the Columbia Icefield to explore some of the classic routes discovered by these early pioneers of mountaineering.<ref name="sandford-60"/>

GlaciersEdit

The icefield feeds six major glaciers:

Parts of the Columbia Icefield and part of other icefields and glaciers are visible from the Icefields Parkway.

The icefield was first reported in 1898 by J. Norman Collie and Hermann Woolley after they had completed the first ascent of Mount Athabasca.<ref name=peakfinder/>

The Athabasca River and the North Saskatchewan River originate in the Columbia Icefield, as do tributary headwaters of the Columbia River.<ref name="atlas"/> As the icefield is atop a triple Continental Divide these waters flow ultimately north to the Arctic Ocean, east to Hudson Bay (and thence to the North Atlantic Ocean), and south and west to the Pacific Ocean.<ref name="huck"/> Hudson Bay, in some watershed divisions, is considered to be in the Arctic watershed, in which case this would arguably not be a triple continental divide point.

MountainsEdit

File:Mts. Athabasca and Andromeda from Wilcox Pass2.jpg

Mts. Athabasca & Andromeda, Athabasca Glacier and a sliver of the Columbia Icefield from Wilcox Pass

File:Mts. Columbia & King Edward.jpg

Mts. Columbia & King Edward from Colum. Icefield

Some of the highest mountains in the Canadian Rockies are located around the edges:

ClimateEdit

Columbia Icefield has an alpine climate (Köppen: ETf), because the weather station is located at an altitude of Template:Cvt. The average annual temperature is Template:Convert. The month of July is the warmest with an average temperature of Template:Convert.

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ReferencesEdit

CitationsEdit

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SourcesEdit

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GalleryEdit

Snow Dome and skiing the Columbia Icefield.jpg

Snow Dome and the Columbia Icefield
Columbia Icefield; Mt. Bryce right, our tent left.jpg

Columbia Icefield; Mt. Bryce right, our tent left
Skiing the Columbia Icefield, Doug.jpg

Skiing the Columbia Icefield
Skiing the Columbia Icefield, Linda.jpg

Peaks to the West of the Icefield

External linksEdit

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Columbia Icefield Glacier Adventure (Brewster)
Columbia Icefield (Bivouac)
Columbia Icefield Flickr

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