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Updated: May 29, 2025
To go this distance the bodies followed the Conemaugh from Johnstown to the Kiskiminetas, at Blairsville, joining the Allegheny at Freeport, and the Ohio here, the entire distance from this point being about one hundred and fifty miles.
It begins to dawn on us that the catastrophe was brought about not merely by the bursting of the dam of the old canal reservoir, but by a rainfall exceeding in depth and area all previously recorded phenomena of the kind. The whole drainage basin of the Kiskiminetas, and more particularly that of the Conemaugh, was affected.
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