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Igneous rocks form from the cooling and solidification of molten rock. Magma that cools slowly underground creates coarse grained, intrusive rocks like granite.

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Volcanic eruptions contribute to the formation of igneous rocks through the cooling and solidification of magma and lava, which can occur both on the surface and beneath the Earth.

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Sediments are transported by natural forces and eventually deposited in layers. These layers can accumulate in various environments, such as riverbeds, lakebeds, or ocean floors.

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If sedimentary rocks are buried deeper in the Earth's crust due to tectonic forces, they can undergo metamorphism, where heat and pressure transform them into metamorphic rocks like marble.

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If these metamorphic rocks are subjected to even higher temperatures and pressures, they can melt and become magma again, completing the cycle.

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Sediments are transported and deposited in various environments. They accumulate in layers and become compacted and cemented over time, forming sedimentary rocks.