Lava is spewed out of a vent like a cannonball, forming a cone-shaped volcano.
cinder cone volcanoes usually form around lithospheric plate boundaries.
cinder cone volcanoes usually form around lithospheric plate boundaries.
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Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.
Cinder cone volcanoes are much shorter and a little bit wider.
Cinder cone volcanoes form from the accumulation of cinders and tephra during an explosive volcanic eruption. This material is ejected from the volcano and falls around the vent, building up a cone-shaped structure. Examples of cinder cone volcanoes include Paricutin in Mexico and Sunset Crater in Arizona.
Three types of volcanoes are shield volcanoes, stratovolcanoes (composite volcanoes), and cinder cone volcanoes. Shield volcanoes have gentle slopes and are formed by low-viscosity lava, while stratovolcanoes are characterized by alternating layers of lava and ash. Cinder cone volcanoes are small, steep-sided volcanoes formed by pyroclastic material ejected during eruptions.
Cinder cone volcanoes erupt explosively, but not as violently as composite volcanoes.
Cinder cone volcanoes are made of pyroclastic material and most often form from moderately explosive eruptions.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Transform boundaries cannot form volcanoes.
Most Cinder Volacnoes are found in North America.