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Scientific American Supplement, No. 384, May 12, 1883 by Various
page 14 of 136 (10%)
the lock masters for twenty years back, it was found that the flow of
the river was in extreme low water 26,000 cubic feet per second, and
in highest water 190,000 cubic feet per second, in average years about
30,000 and 150,000 cubic feet respectively. The average flow in each
year would be nearly a mean between those quantities, namely, about
90,000 cubic feet per second. It was decided to locate the dam where it
is now built, namely, about the center of Carillon Rapid, and a mile
above the village of that name and to make it of a height sufficient to
raise the reach between the head of Carillon and Chute a Blondeau about
six feet, and that above the latter two feet in ordinary water. At the
site chosen the river is 1,800 feet wide, the bed is solid limestone,
and more level or flat than is generally found in such places--the banks
high enough and also composed of limestone. It was also determined to
build a slide for the passage of timber near the south shore (see map),
and to locate the new canal on the north side.

Contracts for the whole works were given out in the spring of 1873, but
as the water remained high all the summer of that year very little could
be done in it at the dam. In 1874 a large portion of the foundation,
especially in the shallow water, was put in. 1875 and 1876 proved
unfavorable and not much could be done, when the works were stopped.
They were resumed in 1879, and the dam as also the slide successfully
completed, with the exception of graveling of the dam in the fall of
1881. The water was lower that summer than it had been for thirty five
years before. The canal was completed and opened for navigation the
following spring.


THE DAM

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