| 784 | 785 | 786 | 787 | 788 |
| 1 | 306 | 613 | 919 | 1225 |
|
end of the ebb movement.
9
59.
That the flow and ebb are not general; for on the shore at Genoa
there is none, at Venice two braccia, between England and Flanders
1
8 braccia. That in the straits of Sicily the current is very strong
because all the waters from the rivers that flow into the Adriatic
pass there.
[Footnote: A few more recent data may be given here to facilitate
comparison. In the Adriatic the tide rises 2 and 1/2 feet, at
Terracina 1 1/4. In the English channel between Calais and Kent it
rises from 18 to 20 feet. In the straits of Messina it rises no more
than 2 1/2 feet, and that only in stormy weather, but the current is
all the stronger. When Leonardo accounts for this by the southward
flow of all the Italian rivers along the coasts, the explanation is
at least based on a correct observation; namely that a steady
current flows southwards along the coast of Calabria and another
northwards, along the shores of Sicily; he seems to infer, from the
direction of the fust, that the tide in the Adriatic is caused by
it.]
9
60.
In the West, near to Flanders, the sea rises and decreases every 6
86
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