The Chautauquan, Vol. 04, December 1883Chautauqua Literary and Scientific Circle
History
The Chautauquan, Vol. 04, December 1883
Chautauqua Literary and Scientific Circle
Chautauqua Institution -- Periodicals; Chautauqua Literary and Scientific Circle -- Periodicals
The lifetime of a world like our earth may be truly said to be a lifetime
of cooling. Beginning in the glowing vaporous condition which we see in
the sun and stars, an orb in space passes gradually to the condition of a
cool, non-luminous mass, and thence, with progress depending chiefly on
its size (slower for the large masses and quicker for the small ones), it
passes steadily onward toward inertness and death. Regarding the state in
which we find the earth to be as the stage of a planet’s mid-life—viz.,
that in which the conditions are such that multitudinous forms of life
can exist upon its surface, we may call that stage death in which these
conditions have entirely disappeared.
Now, among the conditions necessary for the support of life in general
are some which are unfavorable to individual life. Among these may
be specially noted the action of those subterranean forces by which
the earth’s surface is continually modeled and remodeled. It has been
remarked with great justice, by Sir John Herschel, that since the
continents of the earth were formed, forces have been at work which
would long since have sufficed to have destroyed every trace of land,
and to have left the surface of our globe one vast limitless ocean. But
against these forces counteracting forces have been at work, constantly
disturbing the earth’s crust, and, by keeping it irregular, leaving room
for ocean in the depressions, and leaving the higher parts as continents
and islands above the ocean’s surface. If these disturbing forces ceased
to work, the work of disintegrating, wearing away, and washing off the
land would go on unresisted. In periods of time such as to us seem long,
no very great effect would be produced; but such periods as belong to
the past of our earth, even to that comparatively short part of the past
during which she has been the abode of life, would suffice to produce
effects utterly inconsistent with the existence of life on land. Only by
the action of her vulcanian energies can the earth maintain her position
as an abode of life. She is, then, manifesting her fitness to support
life in those very throes by which, too often, many lives are lost. The
upheavals and downsinkings, the rushing of ocean in great waves over
islands and seaports, by which tens of thousands of human beings, and
still greater numbers of animals, lose their lives, are part of the
evidence which the earth gives that within her frame there still remains
enough of vitality for the support of life during hundreds of thousands
of years to come.
Public-domain text, read in full here on John Shaqi.
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