On the magnet, magnetick bodies also, and on the great magnet the earth: a new physiology, demonstrated by many arguments & experiments
History
On the magnet, magnetick bodies also, and on the great magnet the earth: a new physiology, demonstrated by many arguments & experiments
Magnetism -- Early works to 1800
Although these stones now are in agreement with one another, so that F
would not seek H, yet if A was previously the boreal pole[163], F is now
boreal, and H also boreal; for the verticity is not changed (as Baptista
Porta incorrectly affirms in the fourth chapter of his seventh book);
since, though F and H do not agree, so that the one would incline to the
other, yet both turn to the same point of the horizon. If the hemisphere H
I be divided into two quadrants, the one pole takes up its position in H,
the other in I. The whole mass of the stone, as I have said, retains the
site of its vertex constant; and any part of the stone, before it was cut
out from the block[164], might have been the pole or vertex. But concerning
this more under _Direction_. It is important now to comprehend and to keep
firmly in mind that the vertices are strong on account of the force of the
whole, so that (the command being, as it were, divided by the æquinoctial)
all the forces on one side tend towards the north; but those of an opposite
way towards the south, so long as the parts are united, as in the following
demonstration.
[Illustration]
For so, by an infinite number of curves from every point of the equator
dividing the sphere into two equal parts, and from every point of the
surface from the æquator towards the North, and from the æquator towards
the Southern pole, the whole force tends asunder toward the poles. So the
verticity is from the æquinoctial {74} circle towards the pole in each
direction. Such is the power reposed in the undivided stone. From A vigour
is sent to B, from A, B, to C, from A, B, C, to D, and from them likewise
to E. In like manner from G to H, and so forth, as long as the whole is
united. But if a piece A B be cut out (although it is near the æquator),
yet it will be as strong in its magnetical actions as C D or D E, if torn
away from the whole in equal quantity. For no part excels in special worth
in the whole mass except by what is owing to the other adjoining parts by
which an absolute and perfect whole is attained.
_Diagram of Magnetic Vigour
transmitted from the plane of the Æquator
to the peripherery of the terella
or of the earth_
[Illustration]
Public-domain text, read in full here on John Shaqi.
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