Seton Portage
Seton Portage | |
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Unincorporated community | |
Coordinates: 50°42′26″N 122°17′20″W / 50.70722°N 122.28889°W | |
Country | Canada |
Province | British Columbia |
Regional District | Squamish-Lillooet |
Seton Portage (
Geology
"The Portage" was formed about 10,000 years ago when the flank of the Cayoosh Range, which is the south flank of the valley, let go and slid into the middle of what had been a single lake.[1] The result is a location similar to Interlaken, Switzerland, with two fjord-style lakes flanking a narrow and very short strip of land between them. Remnants of old lake bottom survive as benchlands lining the north banks of Seton and Anderson Lakes. It may be that the glacial moraine at the foot of Seton Lake, which had been at the foot of the Seton Glacier and, after it melted, dammed the older, larger lake in until the slide and its destructive wave (see megatsunami). The inundation then washed part of it away to open Seton Creek and drain the glacial melt to today's lake level, or close to it (since the lake level is 10–12 feet higher because of the power project completed in 1958).
Archaeological issues
Much of neighbouring
One witness to the pre-Gold Rush Portage told of coming over the mountain pass which leads into the valley from the north, and looking down on the Portage looked like "many stars in the sky". Such a description suggest a very large population, but no one knows for sure, and between smallpox and other foreign diseases, raids from neighbouring tribes in pre-Contact decades (see
Because of agriculture and
Population history
Population estimates of the pre-Contact populations of the
As concerns the
The first non-native settlers since the Gold Rush occupied lands at the Portage in the early 1900s, which provoked the
During the late 1940s and 1950s, the construction boom caused by the renewal of that project after World War II brought thousands of long-term temporary residents into the valley, with many of these living in temporary trailer camps and prefab houses in the Portage. Following the end of that project, the non-native population has dwindled to 400, cresting to 500 in summer with seasonal residents and visitors. Band population in total, including Shalath and the Portage together, is about 500.
History
The area was traversed by two
In 1858,
Following the
The valley became an important food supply for the booming goldfields in the
Land claims issues
Access
Access to "The Portage" is via a 1,100-metre-high (3,500 ft) pass from the Bridge River known as the Mission Mountain Road, or a 25 km (16 mi) powerline road from D'Arcy at the farther end of Anderson Lake known as the High Line and in recent times dubbed the Douglas Trail, in reference to the old Douglas Road route from Harrison Lake to Lillooet. There is no road connection along Seton Lake, but that route is used by the British Columbia Railway (now CN); the Seton Lake First Nation operates a railbus, the Kaoham Shuttle, between the Seton communities, beginning at the Seton Portage railway station to and from Lillooet, which is at the farther end of the lake. The service sometimes goes to D'Arcy by prior arrangement.
Preceding station | Canadian National Railway | Following station | ||
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Terminus | Kaoham Shuttle | Shalalth toward Lillooet
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D'Arcy Limited service Terminus
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References
- ^ Seton Portage.ca website Archived 2009-01-13 at the Wayback Machine
- ^ in Short Portage to Lillooet, Irene Edwards, self-published, Lillooet, various editions, out of print; and various other histories
- ^ http://www.for.gov.bc.ca/hfd/pubs/docs/En/En33.pdf [bare URL PDF]
- "B.C. land claims spur native protests", by Kathleen Kenna, Toronto Star, September 8, 1990
- Short Portage to Lillooet, Irene Edwards, self-published, Lillooet, various editions, out of print.
- Halfway to the Goldfields, Lorraine Harris, Sunfire Books, one edition, out of print.
- The Great Years, Lewis Green, Tricouni Books Vancouver 2001
- Bridge River Gold, Emma de Hullu and others, self-published, 1971, out of print