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
forward many cogent arguments to show that Mars might be inhabited,
and that great telescopes can discover signs on it, and may discover
further signs, which are a reason for supposing it to be so. It is
not, however, within the range of this book to examine these reasons
in detail; and we need only say that in the first decade of the
twentieth century most astronomers, despite the close examination
of Mars and its markings, which had been conducted for more than a
generation, were still not convinced that life as we know it could
exist there.
CHAPTER XII
THE HARDENING OF ROCKS
After the time when the great overflows of lava took place, spreading
over continents and sometimes seas, there was an era when the
explosions and outbursts began to diminish in violence, and the
world slowly settled down to conditions something like those which
we see in our own day. The seas were forming; there was rainfall and
summer and winter on the earth. The rains and the winds, the summer
heats and winter snows were more violent than now, and the volcanic
activity of which we have spoken was much more fierce than anything
of which mankind has any recollection. In the British Isles the
rainfall in a year averages something in the neighbourhood of thirty
inches. In some regions of the earth it is as much as four times
that amount, and deluges of fifteen inches have fallen in a day. But
in the era of which we have spoken deluging rains that were to be
measured in feet rather than inches fell incessantly. The air was
saturated with moisture, and it no sooner descended on the warm earth
than it steamed back to the clouds again. For reasons not unlike
these, nor unconnected with them, the great currents of air fed by
the constant transference of vapour from the earth to the skies, and
the condensation of the vapour to rain, falling again on the earth,
were greatly magnified. Thus the rocks of the earth, some of them
only cooling and not yet hardened, were subjected to "weathering"
of a kind of which it is hard to form any sufficient idea. The key
to all geology is that what is going on now on the earth is similar
to what always has been happening, (differing in degree rather than
in kind), and that consequently the rocks of millions of years ago
were washed by rivers down to the lower levels and were deposited
as sediment in streams, in lakes, and in the sea. Thus the age of
the "sedimentary rocks" began while the earth was still too warm to
preserve any vestiges of life.
Public-domain text, read in full here on John Shaqi.
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