UNALASKA AND THE ALEUTS
Early in the forenoon the clouds had lifted and the sun had come out, revealing a host of noble mountains, grandly sculptured and composed, and robed in spotless white, some of the highest adorned with streamers of mealy snow wavering in the wind—a truly glorious spectacle. To me the features of greatest interest in this imposing show were the glacial advertisements everywhere displayed in clear, telling characters—the trends of the numerous inlets and canons pointing back into the ancient ice-fountains among the peaks, the sculpture of the peaks themselves and their general out lines, and the shorn faces of the cliffs fronting the sea. No clearer and more unmistakable glacial inscriptions are to be found upon any portion of the mountain ranges of the Pacific Coast.
It seems to be guessed in a general way by most observers who have made brief visits to this region that all the islands of the Aleutian chain are clearly volcanic upheavals, scarce at all changed since the period of their emergence from the sea. This is an impression made, no doubt, by the volcanic character of the rocks of which they are composed, and by the numerous extinct and active volcanoes occurring here and there along the summits of the highest masses. But it is plain that the amount of
