Travels in Alaska by John Muir
page 40 of 270 (14%)
page 40 of 270 (14%)
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A few, however, of these foaming, roaring streams--the Alsek,
Chilcat, Chilcoot, Taku, Stickeen, and perhaps others--head beyond the range with some of the southwest branches of the Mackenzie and Yukon. 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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