Salusbury, Thomas, Mathematical collections and translations (Tome I), 1667

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1
Let the Horizontal Lines be A F the upper, and C D the low­
er; between which let the Perpendicular A C, and inclined
Plane D F, be cut in B; and let A R be a Mean-Proportional
between the whole Perpendicular C A, and the upper part A B; and
let F S be a Mean-proportional between the whole Inclined Plane D F,
and the upper part B F.
I ſay, that the Time of the Fall along the
whole Perpendicular A C hath the ſame proportion to the Time along
its upper part A B, with the lower of the Plane, that is, with B D,
as A C hath to the Mean-proporti­
onal of the Perpendicular, that is
104[Figure 104]
A R, with S D, which is the ex­
ceſſe of the whole Plane D F above
its Mean-proportional F S.
Let a
Line be drawn from R to S, which
ſhall be parallel to the two Horizon­
tal Lines.
And becauſe the Time of
the Fall along all A C, is to the
Time along the part A B, as C A is
to the Mean proportional A R, if we ſuppoſe A C to be the Time of
the Fall along A C, A R ſhall be the Time of the Fall along A B,
and R C that along the remainder B C.
For if the Time along A C
be ſuppoſed, as was done, to be A C it ſelf the Time along F D ſhall
be F D; and in like manner D S may be concluded to be the Time a­
long B D, after F B, or after A B.
The Time therefore along the
whole A C, is A R, with R C; And the Time along the inflected
Plane A B D, ſhall be A R, with S D: Which was to be proved.
The ſame happeneth, if inſtead of the Perpendicular, another
Plane were taken, as ſuppoſe N O; and the Demonstration is the
ſame.
PROBL I. PROP. XIII.
A Perpendicular being given, to Inflect a Plane
unto it, along which, when it hath the ſame
Elevation with the ſaid Perpendicular, it may
make a Motion after its Fall along the Per­
pendicular in the ſame Time, as along the
ſame Perpendicular ex quiete.
Let the Perpendicular given be A B, to which extended to C,
let the part B C be equal; and draw the Horizontal Lines
C E and A G.
It is required from B to inflect a Plane reach­
ing to the Horizon C E, along which a Motion, after the Fall out

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