Boyle, Robert, New experiments physico-mechanicall, touching the spring of the air and its effects, 1660

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1Riviolo makes it probable, that the At­
moſphere may, at leaſt in divers places, be
at leaſt 50 miles high.
So that according to
a moderate eſtimate of the thickneſs of
the Atmoſphere, we may well ſuppoſe,
that a Column of Air, of many miles in
height, leaning upon ſome ſpringy Cor­
puſcles of Air here below, may have
weight enough to bend their little ſprings,
and keep them bent: As, to reſume our
former compariſon, if there were fleeces of
Wooll pil'd up to a mountainous height
upon one another, the Hairs that com­
poſe the lowermoſt locks which ſupport
the reſt, would, by the weight of all the
Wool above them, be as well ſtrongly
compreſſed, as if a man ſhould ſqueeze
them together in his hands, or imploy any
ſuch other moderate force to compreſs
them.
So that we need not wonder, that
upon the taking off the incumbent Air
from any parcel of the Atmoſphere here
below, the Corpuſcles, whereof that un­
dermoſt Air conſiſts, ſhould diſplay them­
ſelves, and take up more room then be­
fore.
And if it be objected, That in Water,
the weight of the upper and of the lower
part is the ſame: I anſwer, That beſides

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