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When metamorphic rocks are exposed to the surface of the earth, they will be broken down into sediments, then compacted into sedimentary rocks.

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When sedimentary rocks are buried deep in the earth, pressure and heat change the rocks into new, metamorphic rocks without melting.

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Metamorphic rocks are melted underground and become magma. When a volcano erupts, lava flows out. As the lava cools, the rock hardens.

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When large amounts of heat and pressure are applied to an igneous rock, it will compact and become a metamorphic rock

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When Sedimentary rocks are heated with immense amounts of heat, it will melt down to magma. After some time, it will cool down and become igneous.

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When an igneous rock is crushed into little shards of sediment, the sediment is eventually packed together with other pieces of sediment to form a sedimentary rock.

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Metamorphic rocks form deep within the Earth when either igneous rocks, sedimentary rocks, or other metamorphic rocks are exposed to heat and pressure. Uplifting and erosion help bring metamorphic rocks to the surface of the Earth. Rocks that have a branded or layered appearance to them are considered foliated, as opposed to rocks that do not have that appearance, which are nonfoilated. Some metamorphic rock examples include sandstone, shale, and limestone.

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Sedimentary rocks are formed by sediment collected over time, carried by erosion and other natural methods, and they usually in the form of layers at the bottom of lakes and oceans. This sediment can contain minerals, small plant parts and other organic matter. Over a long period of time, the sediment is condensed before consolidating into solid rock layers.

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Igneous rocks come from lava or magma that has been cooled down. Magma that has been cooled down and became rocks are called intrusive rocks, as to how rocks that cooled down from lava are extrusive. Some examples of igneous rocks include obsidian, granite, and basalt.