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Rain dissolves limestone into its component molecules.
These wash into streams and rivers which carry the molecules to the ocean.
In the ocean the molecules combine with calcium to form calcium carbonate, some of which settles on the sea floor and forms sediments.
Marine organisms use calcium carbonate to form shells and other body parts. When these organisms die their bodies settle on the ocean floor.
Immense heat and pressure turns the lowermost calcium carbonate layers into limestone rock.
Geologic forces push limestone to the surface where it is exposed to weathering and erosion.
Deep underground, extreme heat melts limestone, turning it into carbon dioxide. Volcanic eruptions release this carbon dioxide into the atmosphere, where it reacts with water to form a weak acid.