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Updated: June 24, 2025


Another rolling crash, a diminishing rumble, and then the rich, deep voice of the singer: "Child of the Wind and Sun, I glide Like a tongue of flame o'er the mountain's side. Wherever falleth my blighting tread Lie the whitening bones of the silent Dead. For trail of wrath Is my red-wet path From the Sea's low rim to the glaciers high, Ai y-u-u yu yu-u-u-u! I live the better that others die.

If ever I find a girl uglier than I am I'll make her my bosom friend." She jabbed her pencil viciously at her notebook. The track by this time had been extended considerably beyond the lower crossing a circumstance which rendered their boat journey to the glaciers considerably shorter than the one Dan had taken with his cargo of dynamite.

In its northern part a river called the Tarim flows from west to east. It is formed by the Yarkand-darya and the Khotan-darya on the south, and receives other affluents along its course, for water streams down from the snowfields and glaciers of the wreath of mountains enclosing Eastern Turkestan.

"We will now describe the remains of these various phenomena as they are found in the Alps outside the actual glacial limits, in order to prove that at a certain epoch glaciers were much larger than they are to-day.

This valley is more wonderful and sublime, but not so beautiful and picturesque as that of Servox, through which I had just passed. The high and snowy mountains were its immediate boundaries, but I saw no more ruined castles and fertile fields. Immense glaciers approached the road; I heard the rumbling thunder of the falling avalanche and marked the smoke of its passage.

We pushed on to the northward throughout the afternoon, keeping as near the coast as possible, winding around among the thickly scattered peaks and crossing no less than nine low ridges of the mountain range. I noticed throughout the day the peculiar phenomenon of which I had read in Tyndall's Glaciers of the Alps the blue light which seemed to fill every footprint and little crevice in the snow.

Do you see the high cliffs yonder away to the nor'-east? Weel, there are great masses o' ice that have been formed against them by the melting and freezing of the snows of many years. When these become too heavy to stick to the cliffs, they tumble into the sea and float away as icebergs. But the biggest bergs come from the foot of glaciers. You know what glaciers are, Mivins?" "No, sir, I don't."

Now if, after all, it should not amuse you, I shall be much mistaken, that's all. Skip over the tiresome parts, of which there are many, and you will find an account of the journey we are going to make, and of many of the feelings we have had in seeing glaciers, seas of ice and mountains.

It is probable that the greatest refrigeration of Norway, Sweden, Scotland, Wales, the Vosges, and the Alps coincided very nearly in time; but when the Scandinavian and Scotch mountains were encrusted with a general covering of ice, similar to that now enveloping Greenland, this last country may not have been in nearly so glacial a condition as now, just as we find that the old icy crust and great glaciers, which have left their mark on the mountains of Norway and Sweden, have now disappeared, precisely at a time when the accumulation of ice in Greenland is so excessive.

But were we to go back to a long antecedent epoch, or to that of the Belgian and British caves with their extinct animals, and the signs they afford of a state of physical geography departing widely from the present, or to the era of the implement-bearing alluvium of St. Acheul, we might expect to find Scandinavia overwhelmed with glaciers, and the country uninhabitable by Man.

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