The rock cycle is the process by which rocks of one kind change into rocks of another kind.
There are three main kinds of rocks: igneous rock, metamorphic rock, and sedimentary rock. Each of these rocks can change into the other kinds by one of these processes: cooling, melting, heat/pressure, weathering/erosion, and compacting (squeezing tightly together)and cementing.
Two other substances also can become rocks and enter the rock cycle. When heated deep under ground, rocks become magma (liquid rock). Above ground, it is called lava. Sediment, the particles from rock erosion and weathering, is the basis for sedimentary rock of the future.
Igneous rock is hardened magma, which can happen above or below ground. It can melt into magma, erode into sediment, or be pressed tightly together to become metamorphic.
Sedimentary rock is compacted sediment which can come from any of the other rocks. It can erode back into sediment, or be pressurized into metamorphic rock.
These processes can occur in different orders, and the cycle goes on forever. Earth has several processes for changing rocks. Wind and water can create sediment from rocks, and movement of one tectonic plate against another creates enormous heat and pressure which affects rocks greatly. Subduction converts all kinds into magma, which eventually rejoins the cycle as igneous rock.
References[change | change source]
- "Rock Cycle (2010)". The Hutchinson Unabridged Encyclopedia with Atlas and Weather guide. 2011 [last update]. http://www.credoreference.com/topic/rock_cycle. Retrieved 25 May 2011.
- Blatt, Harvey and Robert J. Tracy 1996. Petrology; igneous, sedimentary, and metamorphic. 2nd ed, Freeman. ISBN 0-7167-2438-3
- Fichter, Lynn S. 2000. The Wilson cycle and a plate tectonic rock cycle. James Madison University, Department of Geology and Environmental Science. 
- Earth floor: Cycles: exploring the environment. Retrieved 2011-05-09.