Caves :-
Caves commonly form in areas of limestone , although on
coastlines they are also occur other rocks . limestone is made of calcite .
which dissolve in the carbonic acid naturally present in rain water , and in
humin acids from the decay of vegetation . the acidic water trickle down
through cracks and joints in the limestone and between rock layers breaking up
the surfaces terrain into clints (blocks of rock), separated by grikes (deep
crack) , and punctuated by sink holes (also called swallow holes or potholes)
into which surfaces streams may disappear . underground , the acidic water
dissolve the rock around cervices opening up a network of passages and caves ,
which can became large caverns if the roofs collapse . various features are
formed when the dissolved calcite is redeposited : for example , it may be
rediposited along an underground stream to form gour (series of calcilite
ridges) , or in caves and passages to form stalactites , stalactites develop
where calcite is left behind as water drips from the roof; where the drops
land, stalagmites build up
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