Cinder Cone

A cinder cone is a type of volcanic landform that forms when magma erupts explosively, throwing out volcanic ash and small lava fragments called cinders. These cinders pile up around the eruption vent, gradually building a steep, cone-shaped hill. Cinder cones are usually small, with a crater at the summit, and their composition is mostly volcanic ash and cinders. They often form quickly during eruptions and are common in volcanic areas. Despite their simplicity, they provide insight into volcanic activity and help scientists understand eruption processes.