Page:Atlantis - The Antediluvian World (1882).djvu/52

From Wikisource
Jump to navigation Jump to search
This page has been validated.
34
ATLANTIS: THE ANTEDILUVIAN WORLD.

rope were formed; and there seems to have been from remote times a continuous rising, still going on, of the new lands, and a sinking of the old ones. Within five thousand years, or since the age of the "polished stone," the shores of Sweden, Denmark, and Norway have risen from 200 to 600 feet.

Professor Winchell says ("The Preadamites," p. 437):

"We are in the midst of great changes, and are scarcely conscious of it. We have seen worlds in flames, and have felt a comet strike the earth. We have seen the whole coast of South America lifted up bodily ten or fifteen feet and let down again in an hour. We have seen the Andes sink 220 feet in seventy years.… Vast transpositions have taken place in the coast-line of China. The ancient capital, located, in all probability, in an accessible position near the centre of the empire, has now become nearly surrounded by water, and its site is on the peninsula of Corea.… There was a time when the rocky barriers of the Thracian Bosphorus gave way and the Black Sea subsided. It had covered a vast area in the north and east. Now this area became drained, and was known as the ancient Lectonia: it is now the prairie region of Russia, and the granary of Europe."

There is ample geological evidence that at one time the entire area of Great Britain was submerged to the depth of at least seventeen hundred feet. Over the face of the submerged land was strewn thick beds of sand, gravel, and clay, termed by geologists "the Northern Drift." The British Islands rose again from the sea, bearing these water-deposits on their bosom. What is now Sicily once lay deep beneath the sea: it subsequently rose 3000 feet above the sea-level. The Desert of Sahara was once under water, and its now burning sands are a deposit of the sea.

Geologically speaking, the submergence of Atlantis, within the historical period, was simply the last of a number of vast changes, by which the continent which once occupied the greater part of the Atlantic had gradually sunk under the ocean, while the new lands were rising on both sides of it.