The Illecillewaet Glacier is a glacier in British Columbia, Canada. It is located inside Glacier National Park in the Selkirk Mountains, a sub-range of the Columbia Mountains. After the construction of the Canadian Pacific Railway near the glacier’s terminus, and the building of a hotel nearby, the glacier became a prominent tourist destination in the Canadian west. Easily accessible by road and railway, it is one of the most-studied glaciers in North America. Its retreat over the last one hundred years has been extensively documented.
Physical characteristics
The glacier is located south of Mount Sir Donald in the Selkirk Mountains, west of Rogers Pass in British Columbia. The outflow of the glacier forms the headwaters of the Illecillewaet River. The Illecillewaet névé feeds three other glaciers: the Asulkan, Geikie and Deville. As of 2002, the accumulation area of the glacier is while its ablation area is, for a total size of. Its estimated mean depth is, and its highest point is measured at. The exposed bedrock downslope of the glacier's terminus shows the effects of glacial plucking.
Although First Nations people were present in valleys to the east and west, evidence of aboriginal settlement in the Illecillewaet area has not been found. The first European to visit the glacier was Major A.B. Rogers, a railway surveyor, who examined the area in 1882 and 1883 in search of a viable pass. With the completion of the transcontinental Canadian Pacific Railway through nearby Rogers Pass in 1885, the glacier and its surrounding area became one of western Canada's first tourist destinations. Glacier National Park was established in 1886, and Glacier House, a small hotel, was built near the north end of the glacier in the same year. The hotel was expanded in 1892 and 1904, and by 1907 the glacier was described as the "most visited glacier in the Americas". At this point, the glacier was called the "Great Glacier" by CPR promoters. The name "Illecillewaet" is an Okanagan First Nations word for "big water", and referred to the river before being applied to the glacier. It gradually replaced "Great" and was adopted by Parks Canada in the 1960s. The new influx of visitors to the glacier brought with it both mountaineers and glaciologists. The first recorded ascent of the glacier was by A. O. Wheeler with Edward Feuz and Charles Clarke in 1901, although it had most likely been climbed earlier. Wheeler and the Alpine Club of Canada built a hut near Glacier House for mountaineering use. Feuz was one of several Swiss guides hired by the CPR to accompany visitors to the glacier and up nearby peaks.
Vaux family
The Vaux family were well-off Quakers from Pennsylvania. The family first visited Glacier House and Illecillewaet Glacier in 1887. On a subsequent trip, they noticed a visible retreat of the glacier's terminus. The Vaux children, William, George, Jr., and Mary were amateur photographers and began a study of the glacier using pictures taken from fixed points. William and George, Jr. presented their findings to the National Academy of Sciences in the U.S. Their study and methods were considered a "breakthrough" in the new field of glaciology. Mary Vaux would continue to visit the area every summer until her death in 1940. On a more anecdotal level, the Vaux family carefully photographed the glacier and surrounding area, first using glass plates which were transported up and down the mountain and sent back to Philadelphia; and later more modern Mamiyamedium format cameras. There is continuing photographic evidence to support their more scientific measurements. George Vaux, Jr.’s grandson Henry Vaux, Jr., noted the static nature of the glacier's alpine area, related to its short growing seasons. The only two major differences between contemporary times and the early 1900s are the retreat of the glacier and the presence of the Trans-Canada Highway. Thus, he saw trees that were observed by his grandfather from the same perspective, and there is little difference "except for the glaciers, most of which are back at least two kilometres, and of man-made things."
In 1916, the CPR constructed the Connaught Tunnel, which bypassed the Glacier House site. The numbers of visitors declined, and, in 1925, the hotel was closed. It was demolished in 1929. For a thirty-year period, the previously popular glacier was mostly unvisited. In 1962, the new Trans Canada Highway was completed and its route closely followed that of the original CPR line. Once again, Illecillewaet was joined with a major transportation route. Parks Canada began to improve facilities at the glacier; the Illecillewaet campground was opened and new trails were constructed giving access to the glacier, now located significantly farther away. The latter half of the century saw more glaciological studies as the glacier's retreat became more pronounced.
Glaciological studies
Although sparse compared with studies of European glaciers, studies of the Illecillewaet are detailed by North American standards. The first scientific study of the glacier was performed by the Vaux family from 1887 to 1912. George, William, and Mary Vaux with others, including A.O. Wheeler and C.E. Webb measured the glacial retreat mostly with annual photos from fixed points. The period of World War I and the Great Depression saw fewer observations; the closing of Glacier House in 1925 drastically reduced the number of visitors to the area. The federal Dominion Water and Power Bureau started assessing the glacier in 1945 using baseline measurements. The Bureau conducted yearly studies from 1945 to 1950, and every two years from 1950 to 1960. There were no measurements taken from 1960 to 1972, when Parks Canada began surveying. A study which examines rock lichen in order to determine glacial retreat was begun in 1996. Satellite imagery has also been used to measure the glacier's size.
Retreat
Since scientific research began in the late 1800s, Illecillewaet Glacier has been retreating and shrinking, with shorter periods of small advances. Between 1887 and 1962 the terminus of the glacier retreated almost. Parks Canada research indicates that there was a period of advancement from 1972 to 1986, with the terminus advancing. In total, there was a net retreat of in the period of 1887 to 1984. The glacier lost about 28% of its mass by 1951; it regained maybe 1% by 1986.
