'a|l t^e Beds be .the famej *tis certaiq ’ 
ttet that Fliiid hath hot received fluids 
of h dififererit nature^ from' divers places 
at leVeral times-flowing thither. 
^ .7. If ,in the f^me place there be differ¬ 
ent matter of^eds, then either at feveral 
times from divers places there hath been 
a conflux of different forts of Fluids 
(whether caufed by varioui winds, or 
jrapetuops falls of rain in certain placesj) 
or there hath been in the fame fediment, 
matter of different gravity, whereby the 
heavier bodies have fallen to the ground 
fir ft, the lighter afterwards; Which va¬ 
riety a viciflitude of tempefts may have 
occafionedj efpecially in places where an 
equal inequality of grounds is feen. 
8 . If amongft the Beds of the Earth, 
there be found fome Stony Beds, *£is 
certain, that near that place there 
hath Been a fpring of petrifying Water, 
or that fometimes there have happen'd 
Eruptions of fubterraneous fleams, or 
that the Fluid, parting fromi the depos'd 
fediment where the upper cruft was hard- 
nedby the heat of the Sun, hath return¬ 
ed again® ' . 
■ Concern^' 
■ • -ft 
