The Romance of Modern Geology: Describing in simple but exact language the making of the earth with some account of prehistoric animal life — John Shaqi
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
If now, says he, we assume that all over the world this is the amount
carried down, we can see how seriously the level of the land is
lowered by rivers. The Mississippi carries from the land it drains
every year the 1/6000th part of a foot of rock. If we take the
general height of the land of the whole globe to be 2100 feet, and
suppose it to be continuously wasted at this rate, then the whole
dry land would be carried into the sea in 12,600,000 years. Or if
we assume the average height of the continent of Europe to be 940
feet, and to be lowered by its rivers at the same rate, then the last
vestige of Europe would have disappeared in 8,640,000 years. Such
figures are of course not exact; and it must always be remembered
that the rivers are merely robbing Peter to pay Paul, and whatever
they take away are always putting somewhere else, but we may learn
from the foregoing considerations that the lowering of the land is
much more rapid than is sometimes supposed. Another thing about the
excavating work of rivers has to be remembered. The torrents carry
sand, shingle, and rock with them, and these very materials act as
agents of destruction on the beds of the water-courses. If we want
to polish brass or steel we mix emery powder (or something finer or
coarser) with the polishing liquid. The torrent or river uses sand
or shingle as its polishing powder. It then wears out the rock over
which it travels, and sometimes carves it into holes or caverns,
gorges or ravines. Sometimes the process is varied, as when a stream
finds its way over a hard rock which overlies a softer rock. If the
arrangement is like that of a series of steps (there may be only one
or two steps) it is possible for the river as it foams in a waterfall
over the hard step at the top to eat its way into the lower softer
step. The lower softer step will gradually disappear, and then the
waterfall, still eating its way in, will begin to undermine the hard
top step, and when that has gone on long enough the hard top step
will fall down and the waterfall will have to begin a little farther
up the stream. In this way a waterfall, gorge, or ravine can be
constructed by a river.
[Illustration:
_Stereo Copyright, Underwood & U._ _London and New York_
The Grand Cañon of Arizona
The Colorado River at this point is nearly 200 feet wide. The man
is seated about 1200 feet above the river's level. This whole cañon
up to the top of the mountains in the distance has been worn away
by prehistoric current; and the river has gradually cut its bed
deeper.]
Public-domain text, read in full here on John Shaqi.
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