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A volcanic cone is a conical mountain or hill formed by volcanic eruptions, composed of cinders, tuff, breccia, and lava. Cinder cones, a common type, are built from pyroclastic rock fragments (cinders) that accumulate around a volcanic vent, creating a conical hill with a bowl-shaped crater. These cones typically form at an angle of about 30 degrees, the natural slope for loose material. While some cinder cones are small, others can reach heights of several hundred meters, such as Parícutin in Mexico. These formations are often found on the sides of shield volcanoes and are remarkably enduring due to their porous nature, which allows rainwater to be absorbed rather than causing erosion.12

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