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Updated: June 20, 2025


Crevasses, with their blue depths of ice, were closed; the many-voiced streams were still; the moraines and boulders were only here and there visible through the universal shroud. The sky was without a cloud, the air transparent, but the glitter of the uniform white surface was exquisitely painful to the eyes and skin, and the travelers were obliged to wrap their heads in double veils.

A broad belt of wood, growing, as Agassiz afterward found, on an accumulation of old terminal moraines, spanned the lower valley from side to side. Through this wood there poured a glacial river, emptying itself into the bay. Strange to say, this glacier-washed forest, touching the ice on one side and the sea on the other, was full of flowers.

Here is found what is called the heavy timber, but the tallest and most fully developed sections of the forests, growing down in sheltered hollows on moist moraines, would be regarded in California only as groves of saplings, and so, relatively, they are, for by careful calculation we find that more than a thousand of these trees would be required to furnish as much timber as may be obtained from a single specimen of our Sierra giants.

Pine-trees marched up the sun-warmed moraines in long, hopeful files, taking the ground and establishing themselves as soon as it was ready for them; brown-spiked sedges fringed the shores of the newborn lakes; young rivers roared in the abandoned channels of the glaciers; flowers bloomed around the feet of the great burnished domes, while with quick fertility mellow beds of soil, settling and warming, offered food to multitudes of Nature's waiting children, great and small, animals as well as plants; mice, squirrels, marmots, deer, bears, elephants, etc.

A large proportion of the smaller lakes are dammed up by barriers of unstratified drift, having the exact character of the moraines of glaciers, and are termed by geologists "morainic," but some of them are true rock-basins, and would hold water even if all the loose drift now resting on their margins were removed.

It is younger than the earlier drift sheets, for it overlies their weathered and eroded surfaces. It thickens to the Iowan drift border, but is not found upon that drift. It is older than the Wisconsin, for in many places it passes underneath the Wisconsin terminal moraines.

Maurice and the cascade of Pissevache, close to the hamlet of Chaux-Fleurie, that they are most accessible, for at this place the sides of the valley at different levels ascend in little terraces, upon which the moraines have been preserved.

Its greatest thickness, as an independent glacier, is no doubt marked, not by the boulders lying higher up, but by the large moraine which shuts in the lake. The direct connection of this moraine with the glacier in its former extension is still further shown by two other moraines, on lower levels and less perfect, but having the same relation to the present terminus of the ice.

The relief to all is inexpressible; needless to say, we camped and had a meal. Marching in the afternoon, I kept more to the left, and closed the mountain till we fell on the stone moraines. Here Wilson detached himself and made a collection, whilst we pulled the sledge on. We camped late, abreast the lower end of the mountain, and had nearly our usual satisfying supper.

Such transverse or crescent-shaped moraines are everywhere the work of glaciers. All these moraines are the land-marks, so to speak, by which we trace the height and extent, as well as the progress and retreat, of glaciers in former times. Suppose, for instance, that a glacier were to disappear entirely.

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