The Strange Adventures of a PebbleHawksworth, Hallam
Science
The Strange Adventures of a Pebble
Hawksworth, Hallam
Geology -- Juvenile literature; Physical geography -- Juvenile literature
Think of the hottest day in August you ever saw, and then multiply
by two. That will give you an idea of how hot a desert gets in the
day-time--something like 200 degrees; and 212 degrees boils eggs, you
know! But how cold do you suppose it gets at night? Fifteen minutes
after sunset the temperature drops to freezing. The reason of this is
that there are no clouds over the desert to keep the heat of the sand
wastes and the burning rocks from passing off rapidly into space. The
days are so hot and the nights are so cold that the rocks get a kind of
fever and ague, which makes them pull themselves to pieces.
THE "GOOSE-FLESH" ON THE ROCKS
It is the same process we have just read about in the story of the
stones of our fields, only it goes on much faster in the desert on
account of the more rapid changes of temperature. You know how your
skin will pucker up into goose-flesh when you are cold. The desert
rocks do something similar. Because rock is a poor conductor, the heat
of the day and the cold of the night penetrate only a little way--only
through the skin of the rock, as it were; so this skin, stretching in
the day-time and puckering up at night, becomes loosened and shells off
bit by bit. Then it is blown about and in time ground into sand by the
desert winds.
Some rocks have an additional way of getting picked to pieces. Granite
is one of these. It has several different kinds of mineral in it, and
some of these minerals contract and expand faster than others; some
more than others. As a consequence, the particles of the rock keep
pulling and hauling at each other. This helps to break it up into
little pieces, which soon become sand. The darker the rock, other
things being equal, the greater the changes, because anything dark--a
suit of clothes, for instance--absorbs heat faster than a light object.
[Illustration:
_From Norton's "Elements of Geology."
By permission of Ginn and Company_
HOW RAIN-DROPS HELP SPLIT BOULDERS
A big boulder in western Texas split, just as you see it here, by
rain-drops, with the help of the sun, and under the conditions
described in the text, sat for this photograph. A friend of mine
who has been all over that country says that on blistering-hot
days you can see little pieces pop out of the granite boulders,
like chips from an invisible chisel struck by an invisible hammer.
This is why: We Granites are made up of particles--little bits--of
several different minerals, and some of these minerals expanding
much faster than others pop themselves out.
]
The great mountain rocks of the desert, bare of all protecting soil and
verdure, are always crumbling as a result of all these causes, and so
the winds are constantly blowing them away, piece by piece.
HOW LITTLE RAIN-DROPS SPLIT BIG BOULDERS
Public-domain text, read in full here on John Shaqi.
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