The cave itself of course, as a geological entity.
In limestone:
The rock's internal structures such as its bedding-planes, joints, folds, faults and any fossils (since most caves are in limestone).
Precipitated calcium-carbonate 'speleothems' (stalactites, stalagmites and related formations)
Sediment banks - laboratory analysis which can give a lot of information on the cave's own development, palaeoclimate, etc (ditto with speleothems).
In lava caves:
The rock itself, and stalactite-like formations from lava dripping before it solidified.
By the way, why has Answers logged this as being in "Geology, Labour and Birth, Speleology"? I never realised human reproductive Biology is a topic within karst geology!
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