Travels In Alaska By John Muir













































































































































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Thirty-five miles above the Big Stickeen Glacier is the Dirt
Glacier, the second in size. Its outlet is a - Page 25
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Thirty-Five Miles Above The Big Stickeen Glacier Is The "Dirt Glacier," The Second In Size.

Its outlet is a fine stream, abounding in trout.

On the opposite side of the river there is a group of five glaciers, one of them descending to within a hundred feet of the river.

Near Glenora, on the northeastern flank of the main Coast Range, just below a narrow gorge called "The Canyon," terraces first make their appearance, where great quantities of moraine material have been swept through the flood-choked gorge and of course outspread and deposited on the first open levels below. Here, too, occurs a marked change in climate and consequently in forests and general appearance of the face of the country. On account of destructive fires the woods are younger and are composed of smaller trees about a foot to eighteen inches in diameter and seventy-five feet high, mostly two-leaved pines which hold their seeds for several years after they are ripe. The woods here are without a trace of those deep accumulations of mosses, leaves, and decaying trunks which make so damp and unclearable mass in the coast forests. Whole mountain-sides are covered with gray moss and lichens where the forest has been utterly destroyed. The river-bank cottonwoods are also smaller, and the birch and contorta pines mingle freely with the coast hemlock and spruce. The birch is common on the lower slopes and is very effective, its round, leafy, pale-green head contrasting with the dark, narrow spires of the conifers and giving a striking character to the forest. The "tamarac pine" or black pine, as the variety of P. contorta is called here, is yellowish-green, in marked contrast with the dark lichen-draped spruce which grows above the pine at a height of about two thousand feet, in groves and belts where it has escaped fire and snow avalanches. There is another handsome spruce hereabouts, Picea alba, very slender and graceful in habit, drooping at the top like a mountain hemlock. I saw fine specimens a hundred and twenty-five feet high on deep bottom land a few miles below Glenora. The tops of some of them were almost covered with dense clusters of yellow and brown cones.

We reached the old Hudson's Bay trading-post at Glenora about one o'clock, and the captain informed me that he would stop here until the next morning, when he would make an early start for Wrangell.

At a distance of about seven or eight miles to the northeastward of the landing, there is an outstanding group of mountains crowning a spur from the main chain of the Coast Range, whose highest point rises about eight thousand feet above the level of the sea; and as Glenora is only a thousand feet above the sea, the height to be overcome in climbing this peak is about seven thousand feet. Though the time was short I determined to climb it, because of the advantageous position it occupied for general views of the peaks and glaciers of the east side of the great range.

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