The Largest Side Branches Of The Main-Trunk Canyons Of All These
Mountain Streams Are Still Occupied By Glaciers Which
Descend in
showy ranks, their messy, bulging snouts lying back a little distance
in the shadows of the walls, or
Pushing forward among the
cotton-woods that line the banks of the rivers, or even stretching
all the way across the main canyons, compelling the rivers to find a
channel beneath them.
The Stickeen was, perhaps, the best known of the rivers that cross
the Coast Range, because it was the best way to the Mackenzie River
Cassiar gold-mines. It is about three hundred and fifty miles long,
and is navigable for small steamers a hundred and fifty miles to
Glenora, and sometimes to Telegraph Creek, fifteen miles farther. It
first pursues a westerly course through grassy plains darkened here
and there with groves of spruce and pine; then, curving southward and
receiving numerous tributaries from the north, it enters the Coast
Range, and sweeps across it through a magnificent canyon three
thousand to five thousand feet deep, and more than a hundred miles
long. The majestic cliffs and mountains forming the canyon walls
display endless variety of form and sculpture, and are wonderfully
adorned and enlivened with glaciers and waterfalls, while throughout
almost its whole extent the floor is a flowery landscape garden, like
Yosemite. The most striking features are the glaciers, hanging over
the cliffs, descending the side canyons and pushing forward to the
river, greatly enhancing the wild beauty of all the others.
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