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Speleologists divide cave systems into two main
categories, vertical and horizontal. Inalti
is a horizontal system that runs alone a system
of cracks and faults in the limestone. It is
thought to have formed in two stages. In the
first, water seeping down from the surface reacted
with carbondioxide in the soil to form an acidic
solution that eroded the limestone, widening
the existing cracks and creating an underground
water course. In the second stage, as the land
here was pushed upwards, the flow of water diminished
and the evolution of the cave stopped. The underwater
stream that had probably been linked to dolines
at a higher level found a new course for itself,
leaving the cavern dry. Once this had happened
stalactites, stalagmites and travertines began
to form.
Inalti Cave was opened to the public a few months
ago as a result of a joint project between Sinop
local authority and Black Sea Technical University
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