Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 2 of 2]Weld, Isaac
History
Travels through the states of North America, and the provinces of Upper and Lower Canada, during the years 1795, 1796, and 1797 [Vol. 2 of 2]
Weld, Isaac
Canada -- Description and travel -- Early works to 1800; United States -- Description and travel -- Early works to 1800
It is believed by many persons that the waters of Lake Ontario not only
rise and fall periodically every seventh year, but that they are
likewise influenced by a tide, which ebbs and flows frequently in the
course of twenty-four hours. On board the vessel in which I crossed the
lake there were several gentlemen of the country, who confidently
assured me, that a regular tide was observable at the Bay of Canti; that
in order to satisfy themselves on the subject, they had stood for
several hours together, on more than one occasion, at a mill at the head
of the bay, and that they had observed the waters to ebb and flow
regularly every four hours, rising to the height of fourteen inches.
There can be no doubt, however, but that the frequent ebbing and flowing
of the water at this place must be caused by the wind; for no such
regular fluctuation is observable at Niagara, at Kingston, or on the
open shores of the lake; and owing to the formation of the Bay of Canti,
the height of the water must necessarily vary there with, every slight
change of the wind. The Bay of Canti is a long crooked inlet, that grows
narrower at the upper end, like a funnel; not only, therefore, a change
of wind up or down the bay would make a difference in the height of the
water at the uppermost extremity of it; but owing to the waters being
concentrated there at one point, they would be seen to rise or fall, if
impelled even in the same direction, whether up or down the bay, more or
less forcibly at one time of the day than at another. Now it is very
seldom that the wind, at any part of the day or night, would be found to
blow precisely with the same force, for a given space of two hours, that
it had blown for the preceding space of two hours; an appearance like a
tide must therefore be seen almost constantly at the head of this bay
whenever there was a breeze. I could not learn that the fluctuation had
ever been observed during a perfect calm: were the waters, however,
influenced by a regular tide, during a calm the tide would be most
readily seen.
To return to the voyage. A few hours after we quitted Kingston, on the
7th of September, the wind died away, and during the whole night the
vessel made but little way; early on the morning of the 8th, however, a
fresh breeze sprang up, and before noon we lost sight of the land. Our
voyage now differed in no wise from one across the ocean; the vessel was
steered by the compass, the log regularly heaved, the way marked down in
the log book, and an exact account kept of the procedures on board. We
continued sailing, out of sight of land, until the evening of the 9th,
when we had a view of the blue hills in the neighbourhood of Toronto, on
the northern side of the lake, but they soon disappeared. Except at this
place, the shores of the lake are flat and sandy, owing to which
circumstance it is, that in traversing the lake you are generally
carried out of sight of land in a very few hours.
[Sidenote: NIAGARA.]
Public-domain text, read in full here on John Shaqi.
Reviews
Reviews
No reviews yet
Be the first to share your thoughts on this work.
Elsewhere in the archive
Join the Discussion
Join the discussion
Sign in to leave a comment or review.
Sign InorCreate an account