A Cinder Cone is a type of volcano characterized by its steep, conical shape formed from volcanic ash, cinders, and small rocks ejected during eruptions. These materials accumulate around the vent, creating a hill or mound. Cinder cones are typically smaller than other volcano types, such as shield volcanoes or stratovolcanoes, and can reach heights of up to 1,000 feet. Eruptions from cinder cones are usually explosive but short-lived, often producing lava fountains that cool quickly and fall back to the ground. Many cinder cones are found in volcanic regions, such as the San Francisco Volcanic Field in Arizona, where they contribute to the diverse landscape.