Ragnarok : the Age of Fire and GravelDonnelly, Ignatius
Science
Ragnarok : the Age of Fire and Gravel
Donnelly, Ignatius
Atlantis (Legendary place); Comets; Drift
"Buried tree-trunks are often exhumed from the glacial drift at a
depth of from twenty to _sixty feet from the surface_. Dr. Locke has
published an account of a mass of buried drift-wood at Salem, Ohio,
_forty-three feet below the surface_, imbedded in ancient mud. The
museum of the University of Michigan contains several fragments of
well-preserved tree-trunks exhumed from wells in the vicinity of Ann
Arbor. Such occurrences are by no means uncommon. The encroachments
of the waves upon the shores of the Great Lakes reveal whole forests
of the buried trunks of the white cedar."[3]
These citations place it beyond question that the Drift came suddenly
upon the world, slaughtering the animals,
[1. The Great Ice Age," p. 149.
2. Ibid., p. 150.
3. Winchell, "Sketches of Creation," p. 259.]
{p. 51}
breaking up the forests, and overwhelming the trunks and branches of
the trees in its masses of _débris_.
Let us turn to the next question: Was it an extraordinary event, a
world-shaking cataclysm?
The answer to this question is plain: The Drift marks probably the
most awful convulsion and catastrophe that has ever fallen upon the
globe. The deposit of these continental masses of clay, sand, and
gravel was but one of the features of the apalling event. In addition
to this the earth at the same time was cleft with great cracks or
fissures, which reached down through many miles of the planet's crust
to the central fires and released the boiling rocks imprisoned in its
bosom, and these poured to the surface, as igneous, intrusive, or
trap-rocks. Where the great breaks were not deep enough to reach the
central fires, they left mighty fissures in the surface, which, in
the Scandinavian regions, are known as _fiords_, and which constitute
a striking feature of the scenery of these northern lands; they are
great canals--hewn, as it were, in the rock--with high walls
penetrating from the sea far into the interior of the land. They are
found in Great Britain, Maine, Nova Scotia, Labrador, Greenland, and
on the Western coast of North America.
David Dale Owen tells us that the outburst of trap-rock at the Dalles
of the St. Croix came up _through open fissures_, breaking the
continuity of strata, without tilting them into inclined planes."[1]
It would appear as if the earth, in the first place, cracked into
deep clefts, and the igneous matter within took advantage of these
breaks to rise to the surface. It caught masses of the sandstone in
its midst and hardened around them.
These great clefts seem to be, as Owen says, "lines
[1. "Geological Survey of Wisconsin, Iowa, and Minnesota," p. 142.]
{p. 52}
radiating southwestwardly from Lake Superior, as if that was the seat
of the disturbance which caused them."[1]
Public-domain text, read in full here on John Shaqi.
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