Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of GeologyLyell, Charles, Sir
Science
Principles of Geology: or, The Modern Changes of the Earth and its Inhabitants Considered as Illustrative of Geology
Lyell, Charles, Sir
Geology
On referring to the map (p. 79), the reader will see how all the great
rivers of Siberia flow at present from south to north, from temperate to
arctic regions, and they are all liable, like the Mackenzie, in North
America, to remarkable floods, in consequence of flowing in this
direction. For they are filled with running water in their upper or
southern course when completely frozen over for several hundred miles
near their mouths, where they remain blocked up by ice for six months in
every year. The descending waters, therefore, finding no open channel,
rush over the ice, often changing their direction, and sweeping along
forests and prodigious quantities of soil and gravel mixed with ice. Now
the rivers of Siberia are among the largest in the world, the Yenesei
having a course of 2500, the Lena of 2000 miles; so that we may easily
conceive that the bodies of animals which fall into their waters may be
transported to vast distances towards the Arctic Sea, and, before
arriving there, may be stranded upon and often frozen into thick ice.
Afterwards, when the ice breaks up, they may be floated still farther
towards the ocean, until at length they become buried in fluviatile and
submarine deposits near the mouths of rivers.
Humboldt remarks that near the mouths of the Lena a considerable
thickness of frozen soil may be found at all seasons at the depth of a
few feet; so that if a carcass be once imbedded in mud and ice in such a
region and in such a climate, its putrefaction may be arrested for
indefinite ages.[150] According to Prof. Von Baer of St. Petersburg, the
ground is now frozen permanently to the depth of 400 feet, at the town
of Yakutzt, on the western bank of the Lena, in lat. 62° N., 600 miles
distant from the polar sea. Mr. Hedenstrom tells us that, throughout a
wide area in Siberia, the boundary cliffs of the lakes and rivers
consist of alternate layers of earthy materials and ice, in horizontal
stratification;[151] and Mr. Middendorf informed us, in 1846, that, in
his tour there three years before, he had bored in Siberia to the depth
of seventy feet, and, after passing through much frozen soil mixed with
ice, had come down upon a solid mass of pure transparent ice, the
thickness of which, after penetrating two or three yards, they did not
ascertain. We may conceive, therefore, that even at the period of the
mammoth, when the Lowland of Siberia was less extensive towards the
north, and consequently the climate more temperate than now, the cold
may still have been sufficiently intense to cause the rivers flowing in
their present direction to sweep down from south to north the bodies of
drowned animals, and there bury them in drift ice and frozen mud.
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