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
the Portuguese Rodriguez de {178} Lagos measures half a rumbe. The Dutch in
their nautical log fix it at a whole rumbe. Kendall, the expert Englishman,
with a true meridional compass admits only a sixth part of a rumbe. A
little to the East of Cape Agullias Diego Alfonso makes no variation, and
shows by an Astrolabe that the compass remains in the true meridian.
Rodriguez shows that the compass at Cape Agulhas has no variation if it is
of Portuguese construction, in which the needles are inclined half a rumbe
to the East. And there is the same confusion, negligence, and vanity in
very many other instances.
* * * * *
CHAP. XIIII.
On the variation under the æquinoctial line,
_and near it_.
In the North the magnetick needle varies because of the Boreal eminences of
the continent; in the South because of the Austral; at the æquator, if the
regions on both sides were equal, there would be no variation. But because
this rarely happens some variation is often observed under the æquator; and
even at some distance from the æquator of three or 4 degrees toward the
North, there may be a variation arising from the south, if those very wide
and influential southern continents be somewhat near on one side.
* * * * *
CHAP. XV.
The variation of the magnetick needle in the great
Æthiopick and American sea, beyond
_the æquator_.
Discourse hath already been had of the mode and reason of the variation in
the great Atlantick Ocean: but when one has advanced beyond the æquator off
the east coast of Brazil the magnetick needle turns aside toward the
mainland, namely, with that end of it which points to the south; so that
with that end of the versorium it deviates from the true meridian toward
the west; which navigators observe at the other end and suppose a variation
to occur toward the east. But throughout the whole way from the first
promontory on the east of Brazil, by {179} Cape St. Augustine and thence to
Cape Frio, and further still to the mouth of the Strait of Magellan, the
variation is always from the south toward the west with that end of the
versorium which tends toward the antarctick pole. For it is always with the
accordant end that it turns toward a continent. The variation, however,
occurs not only on the coast itself, but at some distance from land, such
as a space of fifty or sixty German miles or even more. But when at length
one has progressed far from land, then the arc begins to diminish: for the
magnetick needle turns aside the less toward what is too far off, and is
turned aside the less from what is present and at hand, since it enjoys
what is present. In the Island of St. Helena (the longitude of which is
less than is commonly marked on charts and globes) the versorium varies by
one degree or nearly two. The Portuguese and others taught by them, who
navigate beyond the Cape of Good Hope to the Indies, set a course toward
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