-Cinder cones are a common type of volcano, formed by explosive eruptions of fragmented magma (cinders).
-They are typically small, steep-sided cones with a central crater, often composed of loose, porous volcanic debris.
-Cinder cones are characterized by their rapid formation and tendency to be monogenetic, meaning they erupt only once in their lifetime.
How do cinder cones form?
-Cinder cones form through explosive volcanic eruptions where gas-rich magma is ejected, fragmenting into small, rock-like pieces called cinders. These cinders accumulate around the volcanic vent, building a cone-shaped structure over time. The angle of repose of the loose cinders creates the steep slopes characteristic of cinder cones.
