Magma cools into igneous rock. The igneous rock is uplifted to the surface and weathered by freeze/thaw cycles, acidic rainfall and plant root growth into smaller particles which are eroded and eventually settle as sand on the ocean floor. As more and more sand accumulates, the sand particles can lithify into sandstone, a sedimentary rock. With increasing depth, or from proximity to a heat source, the sandstone particles can recrystallize, forming the metamorphic rock quartzite.
An example that is not part of the rock cycle would be a volcanic eruption, where molten rock (magma) is expelled from Earth's interior onto its surface. This event is a singular occurrence and does not illustrate the continuous processes of rock formation, transformation, and recycling that make up the rock cycle.
Cooling in the rock cycle means when the rock for example: Igneous rock is transforming it needs to cool when its first magma
When rocks change form in the rock cycle, we see an example of the conservation of mass. This principle states that the total mass of the rock remains constant throughout the cycle, even as it undergoes various processes such as weathering, erosion, and sedimentation.
Matter
Matter
Matter
How is called the elevation changes in a mountain region
matter
matter
matter
The conservation of matter.
Marble is formed from the metamorphism of limestone, a sedimentary rock. This process involves the recrystallization of the calcium carbonate minerals present in limestone under high temperature and pressure conditions. Marble is an example of a metamorphic rock in the rock cycle.