Rocks are categorized into three main types based on how they form: igneous, sedimentary, and metamorphic.
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Igneous rocks have a crystalline texture and are identified by their mineral content and grain size. Examples include granite, which is coarse-grained and forms from slowly cooled magma, and basalt, which is fine-grained and forms from rapidly cooled lava.
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Sedimentary rocks usually have layered structures and may contain fossils. They form from the accumulation of materials in different environments. Common examples are limestone, made from marine organisms, and sandstone, which consists of compacted sand grains.
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Metamorphic rocks show foliation or banding due to changes in pressure and temperature. Schist and gneiss are typical examples that illustrate the intense conditions under which they form.
Understanding these rock types helps us learn about Earth’s geological history and the processes that shaped the planet, linking the rock and water cycles.