Most volcanoes of any type, including cinder cones, are found at plate boundaries, but some are associated with hot spots.
a cinder cone volcano is on a Divergent tectonic plate boundary
Cinder cone volcanoes are usually found on dry land and in corn fields
Cinder volcanoes, composite volcanoes, frision volcanoes, and cinder cone volcanoes.
Cinder cone volcanoes are much shorter and a little bit wider.
Cinder cones are the mountainous structure built up by some volcanoes. Most of the material that makes up the cone is ash and cinders expelled from the top of the cone.
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 usually form around lithospheric plate boundaries.
There are three. From smallest to largest, they are: Cinder Cones, Composite Volcanoes (also called Strata Volcanoes), and then Shield Volcanoes.
Most Cinder Volacnoes are found in North America.
volcanoes in guatemala
shield volcanoes have cinders that come out then land on it. that's what makes them bigger than cinder cone volcanoes.