189
And further that in the thinne
st medium though the acceleration were
pretty neer what was suppo
sed by the affore
said authors yet that it
was in none mathematically true - but that there would be in all
all mediums a certaine Degree of velocity w
ch. the same De
scending
body would neuer exceed. though other de
scending bodys might &
some other would neuer arriue to, After w
ch. Degree was attained
the progre
sse of the body would always be made by aequall spaces
in aequall times though neuer soe farr continued prouided the
Grauitating powers remained the same.
notice al
so was taken that Galileo had supposed that the motion
of a common pendulum was Isocrone,
and but that It was after
wards Experimented by mersennus that this a
ssertion would not hold
Though the other problem of Galileo of the Isocrone De
scent
of a body vpon the Inclined plaines w
thin the circumference of
a circle were mathematically & mechanically true
That m
r. Hugens was the fir
st that found out that the motion
of the weight of a pendulum in a cycloeid would make /all/ its
excur
sions Isocrone, but that he was not the first that applyed
the pendulum to a clock for the Regulating thereof.
S
r. Iohn Lowther queryd who it was that first found out that
the motion of the Descent of Heauy bodys was not the same w
thw
t Galileo had a
scerted ?
D
r. Croon supposd it was mon
r. monconys. And that he had it
from a Ie
suite in france. But m
r. Hooke supposd it to be long
before him and that he did not Remember the mention of it in his
trauells. but that the Iesuite Ricciolus had mentioned it Long
before in his Almage
st. -
D
r Croon added that De chales in his Cursus had sayd much
concerning it both from his own & others experiments - -
After this Di
scour
se was ended m
r. Hooke shewd an Experiment
of the compre
ssion of the water in a gla
sse pipe in order to the
exhibiting the experiment of examining the Depth of the Sea. And
It was very vi
sible that the effect did answer to w
t. was a
sserted
concerning it to wit that the compre
ssion was proportionate to
the Depth of the gla
sse below the surface. /
Ref: CELL/RS/HF_191 © Centre for Editing Lives and Letters