Cindercone
A combination volcano develops from repeated lava eruptions and the accompanying tephra deposits Tephra is the debris from the eruption..
Composite
Cinder cone volcano
because of volcano eruptions
Cinder cone volcano
a volcano
The cone of a volcano is the mountain of erupted material that makes up much of the visible part of the volcano.The cone of a mountain is a the pile of material around a volcanic event formed from precious eruptions. The cone may consist of tephra, cooled lava flows, or a combination of both.
Tephra is stuff that comes out of the volcano, it is mainly disposed as rocks.
The Bus Obo volcano was formed by tephra and contains a type of lava called felsic lava.
Explosive eruptions will produce pyroclastic rocks such as scoria, pumice, and tuff.
It was formed by a neighbouring volcano called Chato. The successive eruptions from Chato formed Arenal.
It was formed by a neighbouring volcano called Chato. The successive eruptions from Chato formed Arenal.