Shield
Mount Fuji is a stratovolcano, which is a composite volcano formed by both lava flows and explosive eruptions. It is not a cinder cone or shield volcano.
Mount Shasta is considered a composite or stratovolcano due to its characteristic steep profile and alternating layers of lava flows and volcanic ash deposits. Shield volcanoes are wider and lower in profile, while cinder cone volcanoes are small, conical mounds built from ejected volcanic material.
Mount Parícutin is a cinder cone volcano, not a composite shield volcano. It formed through a single eruption in 1943 and is made up mainly of pyroclastic material such as ash, cinders, and lava flows, typical of cinder cone volcanoes.
strato volcano
Mount Pelee is a stratovolcano, which is a composite volcano that consists of both lava flows and layers of volcanic ash and tephra. It is not a cinder cone volcano, which is typically smaller in size and formed by eruptions of mostly cinder and ash.
It is a composite volcano.
it is a composite volcano
Mount Fuji is a composite volcano.
composite
Krakatoa is a composite volcano.
caldera/shield volcano
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Mount Fuji is a stratovolcano, which is a composite volcano formed by both lava flows and explosive eruptions. It is not a cinder cone or shield volcano.
Mount Fuji is a composite volcano.
Composite
Mount kenya is a stratovolcano ( composie volcano )
Mount Shasta is considered a composite or stratovolcano due to its characteristic steep profile and alternating layers of lava flows and volcanic ash deposits. Shield volcanoes are wider and lower in profile, while cinder cone volcanoes are small, conical mounds built from ejected volcanic material.