For the Latitude I consider what paralell runnes through (_DEG_)
or (_F_) and I finde the 30 to passe by (_D_) 45 by (_E_) the 15
by (_F_) the 45 Southward by (_G_) and those numbers are the
latitude of the place that are distant from the AEquator, (_CAB_).
[Illustration]
Concerning the means whereby the longitude of places is found
out, there is scarce any thing that hath troubled Mathematicians
so much as the observation of it. For because no standing marke
can be taken (the Heavens alwaies running about) it must needs
bee difficult. To measure vpon the earth, going alwaies vnder the
same paralell, is a way certain in regard of some few places, but
so troublesome in it selfe, and vnprofitable in regard of other
places that ly out of that paralell, that it may be accounted a
fruitlesse labour. The voyages & accounts of Marriners at Sea,
are so full of casualty & vncertainty by reason of the doubtfull
variation of the compasse, the vnequall violence of windes and
tides, the false making of their sea cards, by which they saile,
and the ignorance of the Masters for the greatest part, as there
can hardly be any assured reckoning made by them. The best means
of observation is by Eclipses of the Sunne & Moone, which in
severall Countries are sooner or later seene, according as one
place lies farther East or farther West from another. But this
also falls out so seldome, and when it happens, is so seldome
obserued, and when it is observed, hath so many difficulties in
the precise and exact observation of it; that wee may Well
account this inquiry after the longitude of places, to be one of
those things whereof wee must be content to be ignorant, & rather
to gesse at it in Grosse, then in vaine to striue for exactnesse,
which is the cause why the tables of the longitude and latitude
of Citties, though they many times agree in the latitude, doe yet
for the most part very much differ in the Longitude.
6 The sixth Distinction is by the Length or shortnesse of the Day
in Summer time in seuerall Quarters of the earth. And this
diuision is by Climates ([Greek: chlimata]) which are seuerall
spaces of the earth contained betweene two Paralells, in the
which the longest day in Summer excedes that in another Paralell
by halfe an Houre. There is a greate deale of Confusion and
difference betweene the late and ancient Geographers about the
distinction and diuers reckonings of the Climats. It is not
worth the labour to recount thei
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