Here's why:
* Small: Cinder cones are relatively small, usually less than 1,000 feet (300 meters) tall.
* Narrow base: They have a narrow base compared to their height, giving them a cone-shaped appearance.
* Steep sides: The sides are very steep, often sloping at angles of 30-40 degrees.
Cinder cones are formed by the accumulation of tephra, which is a mixture of volcanic rock fragments, ash, and cinders, ejected from a vent during an eruption. They are common features in volcanic areas around the world.