|Elevation||1,496 m (4,908 ft)|
|Last eruption||5050 BC ± 1000 years|
Caburgua-Huelemolle consists of four groups of cinder cones, namely they are Volcanes de Caburgua, Volcán Huelemolle, Volcán Redondo and Pichares. Volcanes de Caburgua is a group formed by six pyroclastic cones located at the southern tip of the Caburgua Lake, which is a lava-dammed lake created by volcanic activity from the just mentioned cones. Volcán Huelemolle is a group of three cinder cones lying between the rivers Liucura and Trancura.
- "Caburgua-Huelemolle". Global Volcanism Program, Smithsonian Institution. http://www.volcano.si.edu/world/volcano.cfm?vnum=1507-112.
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