The Earth's interior layers, core, mantle, and crust, are defined by thickness and composition. Different rock types – igneous, sedimentary, and metamorphic – are intricately linked to their formation processes.
The thickest interior layer of Earth is the mantle, while the thinnest is the crust. The Earth's core is primarily composed of iron and nickel, while the mantle is mainly made of silicate rocks. Igneous rocks originate from the cooling and solidification of magma or lava, sedimentary rocks form from the accumulation of sediments, and metamorphic rocks result from the alteration of existing rocks due to heat and pressure.
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