What is the Parasitic cone?

The Parasitic Cone is a geological formation typically found in volcanic regions. It is created when a secondary volcanic vent, or fissure, erupts alongside a primary volcano, leading to the buildup of material around the new vent. This results in a smaller cone-shaped structure that is "parasitic" to the main volcano, often composed of lava, ash, and other volcanic debris. These formations can contribute to the complexity of volcanic landscapes and influence eruption dynamics.