Atlin
Provincial Park and Recreation Area
History
Atlin is a corruption
of "Ah-lah", a native word meaning stormy weather.
Atlin park is
occupied by approximately one third glaciers, Llewellyn Glacier
being the most prominent.
Cultural
Heritage
The area has
been used by the Taku River Tlinget for many years. There are several
archeological sites and cultural sites within the park.
It was gold
that gave Atlin its reason for existence. Hordes of prospectors
poured into Alaska and the Yukon during 1898 spurred by a number
of rich strikes. Many of these became weary of travel and were lured
aside to discoveries that were easier to reach. The gold rush came
to Atlin Lake country in 1898 and was one of the richest offshoots
of the klondike rush. By the end of the mining season of 1899 about
5000 people flocked to the region, and Atlin was a busy and important
town. Although creeks in the present day park must have been prospected,
none bore any gold. Although production was greatest in the early
years, the Atlin field still produces today. Total placer gold production
has exceeded $23 000 000 making it second only to the caribou in
the history of British Columbia.
Conservation
Atlin
Park and Recreation Area contains three important ecosections - Teslin
Plateau, Tagish -Highlands, Boundary Ranges (only partial representation
for all three). It also contains Lake Trout Fishery which is
internationally significant.
Wildlife
This environment
provides exceptional habitat for grizzly and black bear, mountain
goat, caribou, moose, stone sheep, and various wolf population.
There are many
small animals such as the hoary marmot, Arctic ground squirrel,
picas, beaver and the otter. Birds also inhabitant the park area.
The most obvious birds are the various gulls, and the Arctic tern,
there are also blue-grouse, ruffed-grouse and the rock, willow and
white-tailed ptarmigan that have been spotted near the upland.
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Provincial Park and Recreation Area
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