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

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1gr.m.gr.m.LandgravePolar altit.5118Altit. of the Star7930Gemma50507945gr.m.gr.m.Buſchius.Polar Altitude5110Altit. of the Star7920Gemma.50507945Reinholdus.Polar Altitude5118Altit. of the Star7930Gemma.50507945
SALV. Rather they muſt needs be leſſe valid, if we will take
thoſe
that lead the way for a proof of the reſt: For (as it is clear)
the
uncertainty and inconcluſiveneſſe of thoſe, is manifeſtly
ſerved
to derive it ſelf from the errours committed in the
mental
obſervations, upon which the Polar Altitude, and height
of
the Star was thought to have been juſtly taken, all in effect
having
eaſily erred; And yet to find the Altitude of the Pole,
ſtronomers
have had Ages of time to apply themſelves to it, at their
leaſure
: and the Meridian Altitudes of the Star are eaſier to be
obſerved
, as being moſt terminate, and yielding the Obſervator
ſome
time to continue the ſame, in regard they change not ſenſibly,
in
a ſhort time, as thoſe do that are remote from the Meridian.
And
if
this be ſo, as it is moſt certain, what credit ſhall we give to
lations
founded upon Obſervations more numerous, more difficult
to
be wrought, more momentary in variation, and we may add,
with
Inſtruments more incommodious and erroneous?
Upon a
ſlight
peruſal of the enſuing demonſtrations, I ſee that the
putations
are made upon Altitudes of the Star taken in different
Vertical
Circles, which are called by the Arabick name, Azimuths; in
which
obſervations moveable inſtruments are made uſe of, not
ly
in the Vertical Circles, but in the Horizon alſo, at the ſame time;
inſomuch
that it is requiſite in the ſame moment that the altitude
is
taken, to have obſerved, in the Horizon, the diſtance of the

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