Embed presentation
Download to read offline











The rock cycle describes how rocks continuously change from one type to another through geological processes such as weathering, erosion, deposition, burial, and melting. Igneous rocks form from cooling magma and are later exposed at the surface, where weathering breaks them into sediments that are transported and deposited to form sedimentary rocks. Increased heat and pressure can metamorphose sedimentary and igneous rocks into new metamorphic rocks. Metamorphic rocks may then melt to form new magma, restarting the cycle. The rock cycle does not always follow the same linear path, as shortcuts allow rocks to transition directly between types.









