Miscellanea Curiosa, Vol. 1: Containing a collection of some of the principal phaenomena in nature, accounted for by the greatest philosophers of this age
History
Miscellanea Curiosa, Vol. 1: Containing a collection of some of the principal phaenomena in nature, accounted for by the greatest philosophers of this age
Natural history; Science -- Early works to 1800; Voyages and travels -- Early works to 1800
Lastly, to demonstrate the Excellency of this Doctrine, the Example of
the Tides in the Port of _Tunking_ in _China_, which are so
extraordinary, and differing from all others we have yet heard of, may
suffice. In this Port there is but one Flood and Ebb in 24 Hours; and
twice in each Month, _viz._ when the Moon is near the Æquinoctial there
is no Tide at all, but the Water is stagnant; but with the Moons
Declination there begins a Tide, which is greatest when she is in the
Tropical Signs: Only with this difference, that when the Moon is to the
Northward of the Æquinoctial, it Flows when she is above the Earth, and
Ebbs when she is under, so as to make High-water at Moons-setting, and
Low-water at Moons-rising: But on the contrary, the Moon being to the
Southward, makes High-water at rising, and Low-water at setting; it
Ebbing all the time she is above the Horizon. As may be seen more at
large in the _Philosophical Transactions_, Numb. 162.
The Cause of this odd Appearance is propos'd by Mr. _Newton_, to be from
the concurrence of two Tides; the one propagated in six Hours out of the
great _South-Sea_ along the Coast of _China_; the other out of the
_Indian-Sea_, from between the Islands in twelve Hours, along the Coast
of _Malacca_ and _Cambodia_. The one of these Tides, being produc'd in
North Latitude, is, as has been said, greater, when the Moon being to
the North of the Equator is above the Earth, and less when she is under
the Earth. The other of them, which is propagated from the _Indian Sea_,
being raised in South-Latitude, is greater when the Moon declining to
the South, is above the Earth, and less when she is under the Earth: So
that of these Tides alternately greater and lesser, there comes always
successively two of the greater and two of the lesser together every
Day; and the High-water falls always between the times of the arrival of
the two greater Floods; and the Low-water between the arrival of the two
lesser Floods. And the Moon coming to the Æquinoctial, and the alternate
Floods becoming equal, the Tide ceases, and the Water stagnates: But
when she has pass'd to the other side of the Equator, those Floods which
in the former Order were the least, now becoming the greatest, that That
before was the time of High-water, now becomes the Low-water, and the
Converse. So that the whole appearance of these strange Tides, is
without any forcing naturally deduc'd from these Principles, and is a
great Argument of the Certainty of the whole _Theory_.
_A Theory of the _Variation_ of the _Magnetical Compass_. By Mr. _Ed.
Halley_, Fellow of the Royal Society._
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