Concluding 'one of the
least-known correspondences of the history of science', in January
1955, only months before his death, Einstein remarked that:
"A great many empirical data indicate that at each point of the
earth's surface that has been carefully studied, many climatic
changes have taken place, apparently quite suddenly. This is
explicable if the virtually rigid outer crust of the earth
undergoes, from time to time, extensive displacement ..." Albert
Einstein
ALBERT EINSTEIN
1879-1955
"I came -- though the child of entirely irreligious (Jewish) parents
-- to a deep religiousness, which, however, reached an abrupt end at
the age of twelve. Through the reading of popular scientific books I
soon reached the conviction that much in the stories of the Bible
could not be true. The consequence was a positively fanatic orgy
of freethinking coupled with the impression that youth is
intentionally being deceived by the state through lies; it was a
crushing impression. Mistrust of every kind of authority grew out of
this experience, a skeptical attitude toward the convictions that
were alive in any specific social environment -- an attitude that
has never again left me."
Einstein appears unafraid to admit what he felt and thought,
even if it flew in the face of established intellectual tradition.
Concluding 'one of the least-known correspondences of the history of
science', in January 1955, only months before his death, Einstein
remarked that the:
"... gradualistic notions common in geology were ... merely a habit
of mind, and were not necessarily justified by the empirical data."
"A great many empirical data indicate that at each point of the
earth's surface that has been carefully studied, many climatic
changes have taken place, apparently quite suddenly. This, according
to Mr. Hapgood, is explicable if the virtually rigid outer
crust of the earth undergoes, from time to time, extensive
displacement ..."
Gradualistic theory - as opposed to catastrophism - has served to
this day as the dominant paradigm to explain not only the origin and
life of plants and animals, but that of the geology and paleontology
of the planet.
To Einstein, the 'gradualistic notions' of geology were 'a
habit of mind' and 'not necessarily justified by the empirical
data'. Defying contemporaries and predecessors alike, Einstein
went right to the heart again. The theory of earth crust
displacement formulated by Charles H. Hapgood - which
'electrified' Einstein - has since gained critical acclaim
and support from specialists in superficially unrelated fields.
"I find your arguments very impressive and have the impression that
your hypothesis is correct. One can hardly doubt that significant
shifts of the crust of the earth have taken place repeatedly and
within a short time."
In contrast to Einstein's enthusiasm for Hapgood's
inherently catastrophic theory of crustal displacement, Charles
Darwin went so far as to suggest that "he who can read Sir
Charles Lyell's grand work on the Principles of Geology
and yet does not admit how vast have been the past periods of time,
may at once close this volume (Origin of Species)."
Darwin's suggestion was right. Empirical evidence suggesting
sudden shifts of the earth's crust and significant climatic changes
do not mix easily with the theory of evolution. Without the vast,
uninterrupted ages of relative geological tranquility Darwin's
theory requires for the evolution of species, the doors to his
theory yawn wide open. Better close that book then, for now.
As for the mechanism that might dislocate the earth's crust from
it's core, Einstein wrote:
"In a polar region there is a continual disposition of ice, which is
not symmetrically distributed about the pole. The earth's rotation
acts on these unsymetrically deposited masses, and produces
centrifugal momentum that is transmitted to the rigid crust of the
earth. The constantly increasing centrifugal momentum produced this
way will, when it reaches a certain point, produce a movement of the
earth's crust over the rest of the earth's body, and this will
displace the polar regions toward the equator."