Volcanologists classify volcanoes based on different criteria
One way to classify volcanoes is by their cones
Three main types of volcanic cones are shield, cinder, and composite cones
Shield volcanoes are formed by the accumulation of lava that oozes out from the volcano
Shield volcanoes have a broad, slightly domed structure that resembles a warrior's shield
An example of a shield volcano is the Mauna Loa Volcano in Hawaii
Cinder cones are built from ejected lava fragments
Cinder cones have a steep slope, wide crater, and are the most abundant of the three major volcano types
An example of a cinder cone is the Paricutin Volcano in Mexico
Composite cones or stratovolcanoes are large, nearly perfect sloped structures formed from alternate solidification of both lava and pyroclastic deposits
One example of a composite cone is the MayonVolcano