Stratovolcano
tall, conical volcano built up by many layers (strata) of hardened lava
A stratovolcano is a tall, conical volcano built up by many layers (strata) of hardened lava, tephra, pumice, and volcanic ash.[1] Unlike shield volcanoes, stratovolcanoes have a steep slope and explosive eruptions every now and then.
References
change- ↑ This article incorporates public domain material from the United States Geological Survey document "Principal types of volcanoes" (retrieved on 2009-01-19).