The Columbia Icefield is the largest
ice field in North America's
Rocky Mountains.
Located within the
Canadian Rocky Mountains
The Canadian Rockies (french: Rocheuses canadiennes) or Canadian Rocky Mountains, comprising both the Alberta Rockies and the British Columbian Rockies, is the Canadian segment of the North American Rocky Mountains. It is the easternmost part ...
astride the
Continental Divide
A continental divide is a drainage divide on a continent such that the drainage basin on one side of the divide feeds into one ocean or sea, and the basin on the other side either feeds into a different ocean or sea, or else is endorheic, not ...
along the border of British Columbia and Alberta, Canada, the ice field lies partly in the northwestern tip of
Banff National Park
Banff National Park is Canada's oldest National Parks of Canada, national park, established in 1885 as Rocky Mountains Park. Located in Alberta's Rockies, Alberta's Rocky Mountains, west of Calgary, Banff encompasses of mountainous terrain, wi ...
and partly in the southern end of
Jasper National Park.
It is about in area, to in depth and receives up to of snowfall per year.
History

The Columbia Icefield was formed during the Great Glaciation, or Illinoisan period (238,000 to 126,000 BCE).
[Sandford 1993, p. 23.] 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.
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.
During the
Crowfoot Glacier
__NOTOC__
Crowfoot Glacier is located in Banff National Park, Alberta, Canada, northwest of Lake Louise, Alberta, Lake Louise, and can be viewed from the Icefields Parkway. The glacier is situated on the northeastern flank of Crowfoot Mountain ( ...
advance (9,000 to 7,000 BCE), humans were beginning to learn farming along the
Tigris,
Euphrates
The Euphrates () is the longest and one of the most historically important rivers of Western Asia. Tigris–Euphrates river system, Together with the Tigris, it is one of the two defining rivers of Mesopotamia ( ''the land between the rivers'') ...
, and
Nile rivers.
The last major period of advance occurred during the
Little Ice Age
The Little Ice Age (LIA) was a period of regional cooling, particularly pronounced in the North Atlantic region. It was not a true ice age of global extent. The term was introduced into scientific literature by François E. Matthes in 1939. Ma ...
, which lasted from about 1,200 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.
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.
[Sandford 1993, p. 56.] 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 in height.
In the summer of 1884, geology professor
Arthur Philemon Coleman explored the Great Divide from
Banff to
Jasper in search of Douglas' giant peak.
While unsuccessful, he did discover the route that would become the Icefield Parkway.
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.
Collie later wrote:
In 1900, former British clergyman
James Outram came to the Canadian Rockies to recover his health after a nervous breakdown.
[Sandford 1993, p. 58.] The following year he made the first ascent of
Mount Assiniboine
Mount Assiniboine, also known as Assiniboine Mountain, is a pyramidal peak mountain located on the Great Divide, on the British Columbia/Alberta border in Canada.
At , it is the highest peak in the Southern Continental Ranges of the Canadian Ro ...
(), then considered the "Matterhorn of the Rockies".
In 1902, Outram made ten first ascents of peaks over and discovered four new mountain passes in the Columbia Icefield area.
Two of his first ascents in 1902 were
Mount Columbia () and
Mount Bryce (), one of the most dangerous and difficult summits in the Rocky Mountains.
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 (), Mount Columbia, and
Mount Saskatchewan () in five days.
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 () in twenty-four hours—a combined distance of about .
In 1927, A. J. Ostheimer discovered a new route to the North Peak Summit, made first ascents of
Stutfield Peak () and
Mount Kitchener (), and became the first climber to traverse the
Snow Dome () in 36 hours.
[Sandford 1993, pp. 58–59.] During his 63-day visit to the Columbia Icefield, Ostheimer and his two companions walked over a and climbed thirty peaks—twenty-five of which were first ascents.
[Sandford 1993, p. 59.]
In March 1932, three men undertook a remarkable skiing journey from Jasper to Banff that covered about .
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 which lasted for —the longest continuous ski run in Canadian history up to that point.
[Sandford 1993, p. 60.] Their accomplishment played a major role in generating worldwide interest in the Canadian Rockies.
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.
Glaciers
The icefield feeds six major
glaciers:
*
Athabasca Glacier
*
Castleguard Glacier
Castleguard Cave is a limestone cave located at the north end of Banff National Park in the Rocky Mountains of Alberta, Canada. With of surveyed passages (as of 2007), it is Canada's longest cave, and its fifth deepest at . Castleguard Cave ...
*
Columbia Glacier
*
Dome Glacier
*
Stutfield Glacier
*
Saskatchewan Glacier
The Saskatchewan Glacier is located in Banff National Park, Alberta, Canada, approximately northwest of the town of Banff, and can be accessed from the Icefields Parkway. Saskatchewan Glacier is the largest outflow glacier from the Columbia I ...
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 Hermann or Herrmann may refer to:
* Hermann (name), list of people with this name
* Arminius, chieftain of the Germanic Cherusci tribe in the 1st century, known as Hermann in the German language
* Éditions Hermann, French publisher
* Hermann, M ...
after they had completed the
first ascent of Mount Athabasca.
[
The Athabasca River and the North Saskatchewan River originate in the Columbia Icefield, as do tributary headwaters of the ]Columbia River
The Columbia River (Upper Chinook: ' or '; Sahaptin: ''Nch’i-Wàna'' or ''Nchi wana''; Sinixt dialect'' '') is the largest river in the Pacific Northwest region of North America. The river rises in the Rocky Mountains of British Columbia, C ...
. As the icefield is atop a triple Continental Divide these waters flow ultimately north to the Arctic Ocean, east to Hudson Bay
Hudson Bay ( crj, text=ᐐᓂᐯᒄ, translit=Wînipekw; crl, text=ᐐᓂᐹᒄ, translit=Wînipâkw; iu, text=ᑲᖏᖅᓱᐊᓗᒃ ᐃᓗᐊ, translit=Kangiqsualuk ilua or iu, text=ᑕᓯᐅᔭᕐᔪᐊᖅ, translit=Tasiujarjuaq; french: b ...
(and thence to the North Atlantic Ocean), and south and west to the Pacific Ocean. 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.
Mountains
Some of the highest mountains in the Canadian Rockies are located around the edges:
* Mount Alberta ()
* Mount Andromeda ()
* Mount Athabasca ()
* Mount Bryce ()
* Mount Castleguard
Castleguard Mountain, also known as Mount Castleguard, is an isolated mountain located near the southern edge of the Columbia Icefield at the northern edge of Banff National Park in Alberta, Canada. In 1918, Irish land surveyor Arthur Oliver Wh ...
()
* Mount Columbia ()
* Mount King Edward ()
* Mount Kitchener ()
* North Twin Peak ()
* South Twin Peak ()
* Snow Dome ()
* Stutfield Peak ()
See also
* Columbia Wetlands
The Columbia Wetlands is a 15,070 hectare wetland in the Columbia Valley region of southeastern British Columbia, Canada. It was designated a wetland of international importance on World Environment Day, June 5, 2005, and is the thirty-sevent ...
* List of glaciers in Canada
References
Citations
Sources
*
*
Gallery
File:Snow Dome and skiing the Columbia Icefield.jpg, Snow Dome and the Columbia Icefield
File:Columbia Icefield; Mt. Bryce right, our tent left.jpg, Columbia Icefield; Mt. Bryce right, our tent left
File:Skiing the Columbia Icefield, Doug.jpg, Skiing the Columbia Icefield
File:Skiing the Columbia Icefield, Linda.jpg, Peaks to the West of the Icefield
External links
*
Columbia Icefield Glacier Adventure
(Brewster)
Columbia Icefield
(Bivouac)
Columbia Icefield
Flickr
{{Authority control
Canadian Rockies
Ice fields of Alberta
Ice fields of British Columbia
Geology of the Rocky Mountains
Tourist attractions in Alberta
Tourist attractions in British Columbia
Great Divide of North America