A stratovolcano, also known as a composite volcano, is a tall, cone-shaped volcano composed of alternating layers of solidified lava flows, volcanic ash, and other volcanic debris. These volcanoes are known for their steep slopes and are typically found at subduction zones, where tectonic plates converge.
Stratovolcanoes are formed through the eruption of viscous magma, which is rich in silica and traps gas, leading to explosive eruptions. The alternating layers of lava and volcanic debris build up over time, creating the characteristic cone shape of a stratovolcano.
One of the defining features of a stratovolcano is its steep, conical shape, which is a result of the build-up of alternating layers of lava and volcanic debris over many eruptions.
Stratovolcanoes are known for their explosive eruptions, which are caused by the buildup of pressure from the viscous magma and trapped gases. These eruptions can be highly destructive and can produce pyroclastic flows, ash clouds, and lahars.
Due to their explosive nature, stratovolcanoes pose significant hazards to nearby communities, including the potential for pyroclastic flows, ashfall, lahars, and volcanic gases. Understanding these hazards is crucial for effective disaster preparedness and risk mitigation.