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Welcome to the dank realm of the Earth's layers, where the litosphere reigns supreme. Skibidi past the core and mantle, where goons of magma chill before they become igneous rock. Think of it as a sigma grind to get that hard, compact structure. Sedimentary rocks are the chill vibes, forming from all the sediments like breccia and conglomerates, lowkey waiting to be noticed. Then we have metamorphic rocks, flexing their high-pressure style. They are the true edge of rock evolution, showcasing textures like crystal and relic. This geological journey is a wild ship through Earth's interior.