On limestone and gypsum (calcium carbonate and calcium sulphate, respectively). Oh, and I know you meant "sinkholes"!
Limestone
Plants and animals that secret lime (CaCO3) flourish in tropical seas. Shells Of CaCO3 in many pile up in shallow off shore waters where they cemented themselves into limestone. Slightly acid grown water is a solvent of limestone, and creates tunnels, caves, and even caverns along cracks or joints in the rock. Some of the dissolved calcium carbonate is redeposit in caves and caverns stalactites and stalagmites.
Carbonic acid is what forms when carbon dioxide dissolves in water. It is a weak acid but will over time, dissolve many rocks, especially carbonates such as limestone. To see what a very weak solution can do over millions of years one only has to visit Carlsbad Caverns or other karst caves found throughout the world.
God
limestone dissolves from it thus creating caves and caverns.
Limestone
carbonic acid dissolves rock to form cavens, and dripstone is dissolved clcium corbonate in thr form of stalagmites/stalagtites
Various formations can occur in underground caverns, including stalactites, which hang from the ceiling, stalagmites, which rise from the ground, and columns, which are formed when stalactites and stalagmites meet. Other formations include flowstones, which are formed by water flowing down cave walls, and soda straws, which are thin, hollow stalactites.
Carbonic Acid .
calcium carbonate
Dreadful grammar! If this is someone's homework, direct plagiarism of this text will stand out like a sore thumb. To answer the question.... Of them, only limestone or perhaps sandstone but only if cemented by calcite, is soluble in acidic water. The rest are insoluble, although granite decays by extremely slow hydrolysis of one of its minerals (the feldspar if I remember correctly).
Carbonic Acid
Carbonic Acid
Limestone and places like limestone caverns.
i don't know that's why I asked you
The reaction of carbonic acid in rain and groundwater with the carbonate rock.
Caverns that form in limestone areas, due to rain water dissolving the limestone over millions of years, produce stalactites and stalagmites. Stalactites are icicle-like rock formations of deposited limestone hanging down from the cavern's roof. Stalagmites grow upwards from the cavern floor, due to the limestone solution dripping on the floor from the roof. In some cases, the stalactite and stalagmite joins in the middle to form a column.