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Rocks break apart from erosion and are transported by rivers and streams to lakes and oceans.

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Metamorphic rocks melt due to high temperatures.

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Rocks are subjected to high heat and pressure.

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As sediments pile up, it is compressed and heated in the earth.

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Magma cools either by intrusive or extrusive cooling.

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Sediments are produced when rocks are uplifted, weathered and eroded.

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If the rock is heated enough, it fully melts ang turns into magma.

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Sandstone, Limestone, & Conglomerate are examples of Sedimentary rocks.

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The high pressures and temperatures lithify the loose sediment into a sedimentary rock.

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Marble, Gneiss, Schiss & Slate are examples of metamorphic rocks.

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When rocks are subjected to very high heat and pressure, it alters the chemical and structural makeup of materials within the rock and turns into a metamorphic rock.

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Granite, Basalt & Pumice are examples of Igneous rocks.

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Igneous rocks are formed when the magma cools, (either by intrusive or extrusive cooling), and turns into rock.