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a karst landscape is one where there are sinkholes and caves. the karst landscape changes slowly as the rock gives way to erosion and then to subsidence. despite this, the rocks do not exhibit a uniform appearance. there are many different kinds of rock in the area. some look like concrete. the sinkholes are almost always formed on limestone, which was laid down as coral reefs millions of years ago. the exposed rock is sometimes thick and sometimes thin, sometimes cracked, and sometimes even studded with organic material like oysters and mussels. sinkholes form under pressure. as the water pressure increases, it cracks the rock layers, causing a cave to form. the cave is the subsurface portion of the sinkhole. due to air pressure, the cave is a place where gases (carbon dioxide is the most common one) are always present. the gases dissolve the carbonates of the rocks. oxygen, which is always present in the air, combines with the carbonates to make carbonic acid.
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