The Earth's Shifting Crust by Charles Hapgood - wire of information

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EARTH'S SHIFTING CRUST
occurred in Siberia as the result of dust produced by massive
outbreaks of volcanism, would cover a considerable area,
enclosing the animal remains. Later, if the ice sheet developed
enough to move by gravity, the upper layers would
move, leaving a stagnant layer, at least in some places, to pro-
tect the animals, and only at the remote fringe or at high
points of the area would the now moving icecap containing
its load of rocks and pebbles be continuously in contact with
the ground. In Siberia the icecap, if there was one, never
grew thick enough to move by gravity. In North America,
on the other hand (at an earlier time), the icecap did grow,
until it began to move.
So we may conclude that the animals contained in the
great North American icecap were mostly living, at the time
they were overwhelmed by the snow, in the places where
they are now found. It would not be wise, of course, to exclude
entirely the transportation of animal remains in the
ice sheet; very certainly it occurred, and perhaps quite often,
but in all probability the vast majority of the animals were
in the stagnant ground-contact ice. We have seen that the
animals represented in the collection in the glacier indicate
a temperate climate, like that prevailing in New York State
today. Now the final question is, How did these millions of
animals, living in a temperate zone, get caught
in the ice
sheet?
Note that here there is no dispute about the climate at
the time the animals were living. Here the situation is free
from the uncertainty surrounding the exact climate in which
the Beresovka mammoth lived. The animals listed above are
sufficient in themselves to establish the fact of a temperate
climate; however, there is an additional piece of evidence,
in the form of a quite fascinating botanical analysis of the
contents of a mastodon's stomach. Hartnagel and Bishop
quote from a report by Dr. J. C. Hunt:
The remains, both of cryptogams and flowering species, were in
abundance. Stems and leaves of mosses were wonderfully distinct in
structure, so much so that I could draw every cell. I even readily de-