Here's how it works:
1. Igneous to Sedimentary:
* Igneous rocks form from cooled magma or lava.
* Weathering and erosion break down the igneous rock into smaller pieces called sediment.
* These sediments are transported by wind, water, or ice and deposited in layers.
* Over time, the sediments are compacted and cemented together, forming sedimentary rocks.
2. Sedimentary to Metamorphic:
* Sedimentary rocks are buried deep beneath the Earth's surface.
* The intense heat and pressure from the surrounding rocks cause the sedimentary rocks to change their mineral composition and texture.
* This transformation results in a metamorphic rock.
3. Metamorphic to Igneous:
* Metamorphic rocks can be further buried, melted, and then solidify as magma.
* This magma can erupt to the surface as lava, cooling and solidifying to form new igneous rocks.
The cycle can then repeat.
Important Note: Not all rocks will complete the full cycle. Some may be weathered and eroded before they have a chance to become metamorphic or igneous. The rock cycle is a continuous process with many potential paths.
