Paricutin is a cinder cone volcano.
Mount Paricutin is a Cinder Cone Volcano.
Paricutin is an example of a cinder cone volcano. It formed in 1943 in Mexico from a series of eruptions that built up a cone-shaped mountain.
Paricutin is a cinder cone, which spews a lot of ash.
Paricutin Mexico
Paricutin volcano in Mexico predominantly erupted mafic lava, which is rich in magnesium and iron and has a low silica content. This type of lava tends to flow more easily compared to felsic lava.
The Paricutin volcano qualifies as such.
Paricutin is located on a convergent boundary. The volcano formed as a result of the subduction of the Cocos Plate beneath the North American Plate in Mexico.
Paricutin is a cinder cone volcano.
It is called Paricutin volcano.
This most likely refers to Paricutin, which is a cinder cone.
The volcano Paricutin is located in Mexico.
Like most cinder cones Paricutin was fed by mafic magma.