Volcanoes: What They are and What They TeachJudd, John W. (John Wesley)
Science
Volcanoes: What They are and What They Teach
Judd, John W. (John Wesley)
Volcanoes
It is a fact, which is capable of mathematical demonstration, that by
the action of these denuding forces the surface of all the lands of the
globe is being gradually but surely lowered; and this takes place at
such a rate that in a few millions of years the whole of the existing
continents must be washed away and their materials distributed over the
beds of the oceans.
[Sidenote: NECESSITY FOR COMPENSATING AGENCIES.]
It is evident that there exists some agency by which this levelling
action of the denuding forces of the globe is compensated; and a little
consideration will show that such compensating agency is found in the
subterranean forces ever at work within the earth's crust. The effects
of these subterranean forces which most powerfully arrest our attention
are volcanic outbursts and earthquake shocks, but a careful study of
the subject proves that these are by no means the most important of the
results of the action of such forces. Exact observation has proved that
almost every part of the earth's surface is either rising or falling,
and the striking and destructive phenomena of volcanoes and earthquakes
probably bear only the same relation to those grand and useful
actions of the subterranean forces, which floods do to the system of
circulating waters, and hurricanes to the system of moving air-currents.
If we ride in a well-appointed carriage with good springs, upon
a railway which is in excellent order, the movement is almost
imperceptible to us; and the rate of speed may be increased
indefinitely, without making itself apparent to our senses. The
smallest impediment to the evenness of the movement--such as that
produced by a small object placed upon the rails--at once makes itself
felt by a violent jar and vibration. How perfectly insensible we may
be of the grandest and most rapid movements is taught us by the facts
demonstrated by the astronomer. By the earth's daily rotation, we are
borne along at a rate which in some places amounts to over 1,000 miles
an hour; and by its annual revolution we are every hour transported
through a distance of 70,000 miles; yet concerning the fact and
direction of these movements we are wholly unconscious.
In the case both of the railway train and of our planet, we can only
establish the reality of the movement, and its direction and rate, by
means of observations upon external objects, which appear to us to
have a movement in the opposite direction. In the same way we can only
establish the fact of the movement of portions of the earth's crust
by noticing the changing positions of parts of the earth's surface in
relation to the constant level of the ocean. When this is done we find
abundant proof that while some parts of the earth's crust are rising,
others are as undoubtedly undergoing depression.
[Sidenote: POTENCY OF THE SUBTERRANEAN FORCES.]
Public-domain text, read in full here on John Shaqi.
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