Perpetual snow

Definition and stakes

Portrait of Alfred Russel Wallace Alfred Russel Wallace,  Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras

“ Perpetual Snow Nowhere Exists on Lowland Areas.—It is a very remarkable and most suggestive fact, that nowhere in the world at the present time are there any extensive lowlands covered with perpetual snow. The Tundras of Siberia and the barren grounds of N. America are all clothed with some kind of summer vegetation; [47] and it is {136}only where there are lofty mountains or plateaus—as in Greenland, Spitzbergen, and Grinnell's Land—that glaciers, accompanied by perpetual snow, cover the country, and descend in places to the level of the sea. ”
Source: Gutenberg

Portrait of Mayne Reid Mayne Reid,  The Desert Home: The Adventures of a Lost Family in the Wilderness

“ Why—that mountains whose tops pierce up into this cold region will most certainly be covered with perpetual snow. It is not likely that anything but snow ever falls upon their summits,—for when it rains upon the plains around them, it is snowing upon the high peaks above. Indeed, it is probable that most of the rain which descends upon the earth has been crystals of snow when it commenced its descent; and, afterwards melting in the lower and warmer regions of the atmosphere, takes the shape of water globules, and thus falls to the ground. ”
Source: Gutenberg

Portrait of Alfred Russel Wallace Alfred Russel Wallace,  Island Life; Or, The Phenomena and Causes of Insular Faunas and Floras

“ If the quantity is great it may take days or weeks to melt; and if snow continues falling it goes on accumulating all over the surface of a country (which water cannot do) , and may thus form such a mass that the warmth of the whole succeeding summer may not be able to melt it. It then produces perpetual snow, such as we find above a certain altitude on all the great mountains of the globe; and when this takes place cold is rendered permanent, no amount of {134}sun-heat warming the air or the earth much above the freezing-point. ”
Source: Gutenberg

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