Earth Features and Their Meaning: An Introduction to Geology for the Student and the General ReaderHobbs, William Herbert
Science
Earth Features and Their Meaning: An Introduction to Geology for the Student and the General Reader
Hobbs, William Herbert
Geology; Physical geography
=The present rate of recession.=—There are various sketches, more or
less accurate, made in the early part of the nineteenth century, and
from the later period there are daguerreotypes, photographs, and maps,
which refer especially to the Canadian Fall; and which, taken together,
render possible a comparison of the earlier with the later brinks. By
comparing the earliest with the recent, views it is seen at a glance
that the Falls are receding, and at a quite appreciable rate (Fig.
382). A careful comparison of the maps made in 1842, 1875, 1886, 1890,
and 1905 of the brink of the Canadian Fall (Fig. 383) indicates that
for the period covered the rate of recession has been about five feet
per year, and similar studies made of the American Fall show that it
has been receding at the rate of only three inches per year, or one
twentieth the rate of the recession of the Canadian Fall.
[Illustration:
FIG. 383.—Map to show the recession of the brink of the Canadian Fall,
based upon maps of different dates (after Gilbert).]
=Future extinction of the American Fall.=—It is because of this many
times more rapid recession of the Canadian Fall that the Niagara
cataract, instead of lying athwart the gorge, enters it from its side.
The Canadian Fall is thus in reality swinging about the American, and
the time can already be roughly estimated when this more effective
drilling tool will have brought about a capture, so to speak, of the
American Fall through the cutting off of its water supply. It will then
be drained and left literally “high and dry”, an enduring witness to
the geological effect of an island in making an unequal division of the
waters for the work of two cataracts.
As already pointed out, the inefficiency of the American Fall as an
eroding agent is amply attested by the wall of blocks already appearing
above the water below it. The tourist who a thousand years hence pays
a visit to the Niagara cataract, provided the water flow is allowed to
remain as it has been, will find above this rampart of blocks a bare
cliff in part undermined, and surmounted by a nearly flat table surface
which is cut off from the existing cataract by a higher section of the
gorge (Fig. 384). It is quite likely that this table will furnish the
most satisfactory viewpoint of the future cataract of that date.
[Illustration:
FIG. 384.—Comparison of the present with the future falls.]
Public-domain text, read in full here on John Shaqi.
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