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
FIG. 388.—Bird’s-eye view of the cuestas south of Lakes Ontario and
Erie (after Gilbert).]
=Episodes of Niagara’s history and their correlation with those of
the Glacial Lakes.=—Of the early episodes of Niagara’s history, our
knowledge is not as perfect as we could desire, but the later events
are fully and trustworthily recorded. The birth of the Falls is to
be dated at the time when the ice front had here first retired into
what is now Canadian territory, thus for the first time allowing the
waters from the Erie basin to discharge over the Lewiston Escarpment
into the basin of the newly formed Lake Iroquois (Fig. 364, p. 334).
Since the level of Lake Iroquois was far above that of the present Lake
Ontario, the new-born cataract was not the equivalent in height of
the escarpment to-day. The Iroquois waters then bathed all the lower
portion of the escarpment, so that the foot of the Fall was upon the
borders of the Lake.
In order to interpret the history of the Niagara gorge, we must
remember that the effective drilling of this gorge was in each stage
dependent mainly upon the volume of water discharged from Lake Erie,
a large discharge being recorded by a channel drilled both wide
and deep, while that produced by the discharge of a smaller volume
was correspondingly narrow and shallow. To-day the gorges of large
cross section have, moreover, a relatively placid surface, whereas
through the constricted sections the water of the river is unable to
pass without first raising its level at the upper end and under the
head thus produced rushing through under an increased velocity. The
best illustration of such a constricted section is the Gorge of the
Whirlpool Rapids.
[Illustration:
FIG. 389.—Sketch map of the greater portion of the Niagara Gorge to
show the changes in cross section in their relations to Niagara history
(based upon a map by Taylor).]
Our reading of the history should begin at the site of the present
cataract, since the records of later events are so much the more
complete and legible, and it should ever be our plan to proceed from
the clearly written pages to those half effaced and illegible.
Public-domain text, read in full here on John Shaqi.
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