Volcanic cone

Volcanic cones are among the simplest volcanic landforms. They are built by ejecta from a volcanic vent, piling up around the vent in the shape of a cone with a central crater. Volcanic cones are of different types, depending upon the nature and size of the fragments ejected during the eruption. Types of volcanic cones include stratocones, spatter cones, tuff cones, and cinder cones.^[1]^[2]

^ Poldervaart, A (1971). "Volcanicity and forms of extrusive bodies". In Green, J; Short, NM (eds.). Volcanic Landforms and Surface Features: A Photographic Atlas and Glossary. New York: Springer-Verlag. pp. 1–18. ISBN 978364265152-6.
^ Schmincke, H.-U. (2004). Volcanism. Berlin, Germany: Springer-Verlag. ISBN 978-3540436508.

[Poldervaart1971a-1] Poldervaart, A (1971). "Volcanicity and forms of extrusive bodies". In Green, J; Short, NM (eds.). Volcanic Landforms and Surface Features: A Photographic Atlas and Glossary. New York: Springer-Verlag. pp. 1–18. ISBN 978364265152-6.

[Schmincke2004a-2] Schmincke, H.-U. (2004). Volcanism. Berlin, Germany: Springer-Verlag. ISBN 978-3540436508.

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