Volcanoes

Volcanoes — page 5
Cinder cones are the simplest type of volcanoes Lava flows out of a central vent and down the sides forming a cone The lava in a cinder cone volcano cools quickly It builds up rock to form the typical steep-sided cone The cinder cone can be part of another volcano system such as one growing on a shield volcano Paricutin in Mexico is a cinder cone volcano Strato volcanoes produce two types of lavas These lavas are thicker and cooler than basalt The thick lavas often plug the opening Different gases build up below the plug They make a more explosive eruption when they blow The tall sides may trigger mud or landslides and earthquakes during an eruption 8