Galilei, Galileo, The systems of the world, 1661

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1the Moon and Sun; neer, in a word, at the time of its conjun
ction
and change; remote, in its Full and Oppoſition; and the
greateſt
vicinity differ the quantity of the Diameter of the
nar
Orb.
Now if it be true that the virtue which moveth the
Earth
and Moon, about the Sun, be alwayes maintained in
the
ſame vigour; and if it be true that the ſame moveable
moved
by the ſame virtue, but in circles unequal, do in ſhorter
times
paſſe like arches of leſſer circles, it muſt needs be granted,
that
the Moon when it is at a leſſe diſtance from the Sun, that is
in
the time of conjunction, paſſeth greater arches of the Grand
Orb
, than when it is at a greater diſtance, that is in its Opppſition
and
Full.
And this Lunar inequality muſt of neceſſity be imparted
to
the Earth alſo; for if we ſhall ſuppoſe a right line produced from
the
centre of the Sun by the centre of the Terreſtrial Globe, and
prolonged
as far as the Orb of the Moon, this ſhall be the
diameter
of the Grand Orb, in which the Earth, in caſe it were
alone
, would move uniformly, but if in the ſame ſemidiameter we
ſhould
place another body to be carried about, placing it one
while
between the Earth and Sun, and another while beyond
the
Earth, at a greater diſtance from the Sun, it is neceſſary,
that
in this ſecond caſe the motion common to both, according
to
the circumference of the great Orb by means of the diſtance
of
the Moon, do prove a little ſlower than in the other caſe,
when
the Moon is between the Earth and Sun, that is at a leſſer
diſtance
.
So that in this buſineſſe the very ſame happeneth that
befals
in the time of the clock; that lead which is placed one
while
farther ſrom the centre, to make the vibrations of the
ſtaffe
or ballance leſſe frequent, and another while nearer, to
make
them thicker, repreſenting the Moon.
Hence it may be
manifeſt
, that the annual motion of the Earth in the Grand
Orb
, and under the Ecliptick, is not uniform, and that its
regularity
proceedeth from the Moon, and hath its Monethly
Periods
and Returns.
And becauſe it hath been concluded, that
the
Monethly and Annual Periodick alterations of the ebbings
and
flowings, cannot be deduced from any other cauſe than
from
the altered proportion between the annual motion and the
additions
and ſubſtractions of the diurnal converſion; and that
thoſe
alterations might be made two wayes, that is by altering
the
annual motion, keeping the quantity of the additions
altered
, or by changing of the bigneſſe of theſe, reteining the
uniformity
of annual motion.
We have already found the firſt
of
theſe, depending on the irregularity of the annual motion
occaſioned
by the Moon, and which hath its Monethly Periods.
It is therefore neceſſary, that upon that account the ebbings
and
flowings have a Monethly Period in which they do grow

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