The Outline of Science, Vol. 1 (of 4): A Plain Story Simply ToldThomson, J. Arthur (John Arthur)
Science
The Outline of Science, Vol. 1 (of 4): A Plain Story Simply Told
Thomson, J. Arthur (John Arthur)
Science
A sort of slow boiling of the internally hot earth often forced molten
matter through the cold outer crust, and there came about a gradual
assortment of lighter materials nearer the surface and heavier materials
deeper down. The continents are built of the lighter materials, such as
granites, while the beds of the great oceans are made of the heavier
materials such as basalts. In limited areas land has often become sea,
and sea has often given place to land, but the probability is that the
distinction of the areas corresponding to the great continents and
oceans goes back to a very early stage.
The lithosphere is the more or less stable crust of the earth, which may
have been, to begin with, about fifty miles in thickness. It seems that
the young earth had no atmosphere, and that ages passed before water
began to accumulate on its surface--before, in other words, there was
any hydrosphere. The water came from the earth itself, to begin with,
and it was long before there was any rain dissolving out saline matter
from the exposed rocks and making the sea salt. The weathering of the
high grounds of the ancient crust by air and water furnished the
material which formed the sandstones and mudstones and other sedimentary
rocks, which are said to amount to a thickness of over fifty miles in
all.
Sec. 3
Making a Home for Life
It is interesting to inquire how the callous, rough-and-tumble
conditions of the outer world in early days were replaced by others that
allowed of the germination and growth of that tender plant we call
LIFE. There are very tough living creatures, but the average organism is
ill suited for violence. Most living creatures are adapted to mild
temperatures and gentle reactions. Hence the fundamental importance of
the early atmosphere, heavy with planetesimal dust, in blanketing the
earth against intensities of radiance from without, as Chamberlin says,
and inequalities of radiance from within. This was the first preparation
for life, but it was an atmosphere without free oxygen. Not less
important was the appearance of pools and lakelets, of lakes and seas.
Perhaps the early waters covered the earth. And water was the second
preparation for life--water, that can dissolve a larger variety of
substances in greater concentration than any other liquid; water, that
in summer does not readily evaporate altogether from a pond, nor in
winter freeze throughout its whole extent; water, that is such a mobile
vehicle and such a subtle cleaver of substances; water, that forms over
80 per cent. of living matter itself.
Public-domain text, read in full here on John Shaqi.
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