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A cinder cone volcano is characterized by its steep, conical shape and is primarily built from volcanic ash, cinders, and small lava fragments ejected during explosive eruptions. These materials accumulate around the vent, creating the distinctive cone structure. Cinder cone volcanoes typically have a single vent and can erupt relatively quickly, often producing short-lived eruptions that result in a pile of loose debris. Examples include Paricutin in Mexico and Sunset Crater in Arizona.

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