It is a cinder cone volcano.
Paricutin erupted in 1943 due to the movement of magma rising from the Earth's mantle through a vent in the surface, creating a new volcano. This kind of eruption, known as a monogenetic eruption, occurs sporadically and is not associated with a tectonic plate boundary.
stratovolcanic
strato volcanoe
cinder cone volcano
An Igneous Rock
Active VOlcanoe
pumice
Shield volcanoes.
what kind of extrusive ivgnouse rocks formed from paicutin volcano
it is a cc cinder cone
Shield volcanoes.
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