Volcanoes form when magma rises from below the Earth's surface and erupts through openings called vents. As magma accumulates at the vent it builds up a mountain-like structure called a volcano. There are three main types of volcanoes defined by their shape and eruption characteristics: shield volcanoes which have broad bases and gentle slopes formed by fluid basaltic lava flows; cinder cone volcanoes which are steep-sided with a small base formed from explosive eruptions of thick sticky lava; and composite or stratovolcanoes which are large mountains formed by alternating explosive and effusive eruptions that build tall layers of ash and lava.