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
But, the reader will naturally inquire, if "faults" gave rise to
earthquakes, and faults are the result of pressure, what produces the
pressure? And what produces the mountains? Before we answer that we
must again have recourse to examples taken from common experience.
A sheet of glass or of marble we usually regard as a thing that may
break but does not bend. But all of us have seen glass strips, if
they are long enough, bend under their own weight; and there are
even marble mantelpieces which, if examined, show that the slab of
marble has _bent_. Thus we can readily imagine that sometimes the
strata of the earth will bend by reason of the weight put upon them.
If that weight is not put on them quite evenly the strata will be
still more likely to bend; it will go from bending to buckling,
and from buckling to breaking. As soon as it breaks there will be
a "fault" formed. Those who recollect what we have said about the
enormous weight of the rocks one above the other will not have to
search far for the cause of weight sufficient to bend or buckle the
rock strata of the earth. And those who have followed carefully all
that has been written about the shifting of materials from the land
to the sea by the processes of denudation and erosion set up by rain
and wind and carried out by streams and rivers, will easily discover
where and how the shifting of great weights of the earth's surface
goes on. Little by little great weights are taken from one place
on the earth's surface to another, as we might shift the weights
in balanced scale-pans grain by grain, till at last the heavier
scale-pan goes down quickly, or it may be with a crash, and the
"fault" occurs, while the earthquake follows.
Public-domain text, read in full here on John Shaqi.
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