The Western United States: A Geographical ReaderFairbanks, Harold W. (Harold Wellman)
Science
The Western United States: A Geographical Reader
Fairbanks, Harold W. (Harold Wellman)
Physical geography -- West (U.S.); West (U.S)
Years ago people disputed as to the way in which the earth was made.
Those who lived where all the rocks had, like lava, the appearance
of having once been melted, believed that fire had done all the
work. Those who lived where the rocks appeared to be formed of
hardened mud, sand, and lime, substances such as we find accumulating
under water, said that water alone had been the means. But in later
years the earth's surface has been more widely explored, and now
it is known that both opinions were partly right. Water and fire
have both been concerned in the making of the earth.
In the great valleys fire-formed rocks are rare, but they are more
or less abundant in all mountainous regions, for where mountains
are, there the crust of the earth is weakest. There are many reasons
for believing that the interior of the earth is very hot. We know
that the surface is settling in some places and rising in others,
and that where the strain of the upheaval is too great the rocks are
broken. These convulsions sometimes cause earthquakes and sometimes
volcanic eruptions, when enormous quantities of molten rock are
poured out over the surface. In all the long history of our earth
probably no greater flood of lava than that which made the Columbia
plateau was ever spread over the surface of any region. Travel where
you will over the plains of southern Idaho, central Washington,
or Oregon, and examine the rocks which here and there rise above
the soil or are exposed in the canons, and you will find that they
all appear to have been formed by fire.
[Illustration: FIG. 7.--SNAKE RIVER AT IDAHO FALLS
Just beginning to cut a canon in the volcanic plateau]
These rocks are dark in color and very hard. They are not arranged
in regular layers like sandstone and shale; many of them show numerous
little cavities which once contained steam. These cavities give
to the rock a slag-like appearance. In this kind of rock, which
we shall call lava, there are, of course, no remains of shells
or bones of animals such as are often found in rocks formed from
sand or clay.
Do not picture to yourself the Columbia plateau as one continuous
stretch of level land, for it is broken by many mountain ranges.
Some of these are old mountains which were too tall to be buried
by the lava, but most of them have been formed out of the plateau
itself. The eruptions which made the plateau extended through a
very long time, perhaps hundreds of thousands of years, and the
older lava is deeply decayed and covered with soil. Some of the
later flows show extremely rough and rugged surfaces and are probably
only a few hundred years old.
[Illustration: MAP OF THE COLUMBIA PLATEAU]
Public-domain text, read in full here on John Shaqi.
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