The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal lifeGrew, Edwin Sharpe
Science
The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life
Grew, Edwin Sharpe
Geology; Paleontology
The whole of the great globe which we call the earth is in this
state of strain; and it is always liable to rifts within itself and
to readjustments of the weights of its own parts. It is not so easy
to understand how a great globe spinning through space can be in a
state of strain, or can attempt to readjust the weight of its parts,
as in the instances we have just given of the quivering jelly or the
solid cathedral tower. Perhaps another illustration may help us. We
will presume that nearly everybody is acquainted with the modern
rubber-cored golf ball. The modern golf ball, as those who are
aware who either intentionally or unintentionally have cut through
its outer cover, consists first of a small hard core. Round this is
wound very tightly some two hundred yards of elastic. The tighter
this is wound the better, or at any rate the more "bouncing" will
be the resulting ball of india-rubber elastic. But consider what is
the usual condition of this rubber-wound ball. Like our jelly it is
always in a state of stretch or strain. Even when covered with the
outer shell which completes the golf ball, the whole ball is still,
we might say, in a state of strain or tension. That is one of the
reasons why it bounces, and why it flies better than the old solid
ball off the face of a golf club. But if you were to keep a golf ball
for a hundred years these strains in its interior would alter and
adjust themselves. One result would certainly be that the golf ball
might lose its elasticity. Another result would be that its shape
would slightly alter.
Now a golf ball, however carefully it is made, is not always evenly
made. It weighs a little more on one side than another; and the best
golf balls, those which fly truest and farthest, are those which are
most evenly made: so that we might say of them that the centre of
their weight was exactly the same as the centre of the ball. If it
is not, then the strains in the ball are always pulling it a little
more out of shape; and the ball, as golfers say, flies badly. Now
the earth is like a badly made golf ball. The centre of its weight,
or, as we call it, the centre of gravity, is not quite at the centre
of the earth. Moreover, owing to the enormous pressures which exist
right through the earth, and which are by no means the same at every
place inside the earth, but are, in fact, continually changing,
owing to hundreds of causes, the whole of the earth's interior is in
a state of unequal strain. What is the consequence that you would
expect? Is it not that the earth should always be making efforts to
adjust its weight, and, as it were, to distribute it evenly? It has
been doing this for millions of years. It has not yet finished.
Public-domain text, read in full here on John Shaqi.
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