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'''Limestone''' is a common type of carbonate sedimentary rock. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of [[calcium]] carbonate. Limestone forms when these minerals precipitate out of [[water]] containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years.
'''Limestone''' is a common type of carbonate sedimentary rock. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of [[calcium]] carbonate. Limestone forms when these minerals precipitate out of [[water]] containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years.
 
==Dependencies==
*[[Calcium]]
*[[Lime]]
*[[Water]]
**'''Limestone'''
== See also ==
== See also ==
* [[Brick]]
* [[Brick]]

Revision as of 15:34, 19 December 2022

Limestone deposit in the karst of Dinaric Alps near Sinj, Croatia.

Limestone is a common type of carbonate sedimentary rock. It is composed mostly of the minerals calcite and aragonite, which are different crystal forms of calcium carbonate. Limestone forms when these minerals precipitate out of water containing dissolved calcium. This can take place through both biological and nonbiological processes, though biological processes, such as the accumulation of corals and shells in the sea, have likely been more important for the last 540 million years.

Dependencies

See also

References

This article uses material from the Wikipedia article Limestone, which is released under the Creative Commons Attribution-ShareAlike 3.0 Unported License (view authors). Wikipedia logo