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
=Future consequences of the continued uptilt within the lake
region.=—One of the most distinguished of American geologists, Dr.
G. K. Gilbert, in order to determine whether the uptilt revealed by
canted beach lines is still in progress, carried out an elaborate
study upon the gauge records preserved at the various gauging stations
about the Great Lakes. Upon the basis of these studies, he concluded
that the uplift continues, that the axes of equal uplift (isobases)
take their course about fifteen degrees north of west, so that the
lines of greatest uptilt should be perpendicular to this direction,
or fifteen degrees east of north. He further believed that the basin
was undergoing an up-cant in the simple manner of a trap door, the
hinge of which lay to the southward of Chicago, and the study of the
gauge records led him to believe that “the rate of change is such
that the two ends of a line one hundred miles long and lying in a
south-southwest direction are relatively displaced four tenths of a
foot in one hundred years.”
=Gilbert’s prophecy of a future outlet of the Great Lakes to the
Mississippi.=—The _natural_ rock sill, over which the waters of Lake
Chicago once flowed to the Mississippi, is to-day but eight feet above
the common mean level of Lakes Michigan and Huron, and if the tilting
of the lake region were to continue upon Gilbert’s assumption of a
canting plane with the hinge of the movement to the south of Chicago, a
time must come when the “Chicago outlet” will again come into use and
the lakes once more drain to the Mississippi and the Gulf. Upon the
basis of his measurements, Gilbert ventured the prophecy that the first
high-water discharge into the Mississippi should occur in from five
hundred to six hundred years, and for continuous discharge in fifteen
hundred years. In twenty-five hundred years Niagara Falls should at low
water stages be dry from this cause, and in thirty-five hundred years
it should have become extinct.
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