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
Prior to bringing forward the causes of magnetical motions, & laying open
the proofs of things hidden for so many ages, & our experiments (the true
foundations of terrestrial philosophy), we have to establish & present to
the view of the learned our New & unheard of doctrine about the earth; and
this, when argued by us on the grounds of its probability, with subsequent
{40} experiments & proofs, will be as certainly assured as anything in
philosophy ever has been considered & confirmed by clever arguments or
mathematical proofs. The terrene mass, which together with the vasty ocean
produces the sphærick figure & constitutes our globe, being of a firm &
constant substance, is not easily changed, does not wander about, &
fluctuate with uncertain motions, like the seas, & flowing waves: but holds
all its volume of moisture in certain beds & bounds, & as it were in
oft-met veins, that it may be the less diffused & dissipated at random. Yet
the solid magnitude of the earth prevails & reigns supreme in the nature of
our globe. Water, however, is attached to it, & as an appendage only, & a
flux emanating from it; whose force from the beginning is conjoined with
the earth through its smallest parts, and is innate in its substance. This
moisture the earth as it grows hot throws off freely when it is of the
greatest possible service in the generation of things. But the thews and
dominant stuff of the globe is that terrene body which far exceeds in
quantity all the volume of flowing streams and open waters (whatever vulgar
philosophers may dream of the magnitudes and proportions of their
elements), and which takes up most of the whole globe and almost fills it
internally, and by itself almost suffices to endow it with sphærick shape.
For the seas only fill certain not very deep or profound hollows, since
they rarely go down to a depth of a mile and generally do not exceed a
hundred or 50 fathoms. For so it is ascertained by the observations of
seamen when by the plumb-line and sinker its abysms are explored with the
nautical sounder; which depths relatively to the dimensions of the globe,
do not much deform its globular shape. Small then appears to be that
portion of the real earth that ever emerges to be seen by man, or is turned
up; since we cannot penetrate deeper into its bowels, further than the
wreckage of its outer efflorescence, either by reason of the waters which
gush up in deep workings, as through veins, or for want of a wholesome air
to support life in the miners, or on account of the vast cost that would be
incurred in pumping out such huge workings[103], and many other
difficulties; so that to have gone down to a depth of four hundred, or
(which is of rarest occurrence) of five hundred fathoms[104] as in a few
mines, appears to all a stupendous undertaking. But it is easy to
understand how minute, how almost negligibly small a portion that 500
fathoms is of the earth's diameter, which is 6,872 miles. It is then parts
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