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 great prominence which we have given in the preceding pages
to earthquakes is owing to the growing belief in the influence of
earthquakes on the appearance and structure of those portions of the
world's crust which are known to us. There are two views which we
can take of earthquakes. One is to regard the larger number of them
as being caused by slipping movements of the earth's crust. Looking
at things in this way we should say that whenever there was a sudden
break in the earth's strata, such as might occur (in accordance with
an illustration given in a previous chapter) if all the level strata
were broken up like a crumpled page of type--then that an earthquake
would result. So that whenever we saw what geologists call a "fault"
in strata we should know that an earthquake had occurred there. And
why did it occur? Well, if we had a massive column of steel or of
granite five miles high, the steel or granite at the bottom of the
column would have to sustain such an enormous weight of material
above it that it would begin to spread. If we had a pyramid of the
same materials five miles high, the tendency to spread would not be
so great, but still it would be there. Consequently, wherever there
are high mountains there is a tendency of the earth strata beneath
them to spread, perhaps slowly, but inevitably; and if there is any
weakness in the structure of the rocks near the base of the mountain,
then these will give way with a crash. A great "fault" will be
produced, and with it an earthquake.
People living on the earth will only see the results of the
earthquake on the ground just immediately below their feet; and there
these results are often very destructive to life and property; yet if
they were all that happened, we should expect them to be covered up
in time, and the "geological record" of an earthquake would not be a
very important or even discernible thing a million years after it had
happened. But are these things, which the eye of man can perceive,
the only things that are happening during an earthquake? Is nothing
happening underneath the earth which will leave its mark thousands of
years after man has left the spot where the earthquake took place?
May it not be that the earthquake is the outcome of some mighty
force deep down in the earth; and may not this force cause both the
earthquake and the geological "fault" which remains as the witness
of its occurrence? If this be the case then the earthquake may be of
enormous importance in geology.
Public-domain text, read in full here on John Shaqi.
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