Mount Fuji is shield
Mount Kenya is neither a composite cone, cinder cone, nor a shield cone. It is a complex stratovolcano made up of layers of lava and ash.
Tambora was a composite cone.
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.
Mount Aso is a composite cone volcano, also known as a stratovolcano. It is characterized by its steep-sided profile and alternating layers of lava and volcanic ash.
Paricutin is a cinder cone volcano.
Mount Kenya is neither a composite cone, cinder cone, nor a shield cone. It is a complex stratovolcano made up of layers of lava and ash.
It is a composite volcano.
Composite
Mount Fuji is a composite volcano.
Tambora was a composite cone.
it is a composite volcano
Krakatoa is a composite volcano.
caldera/shield volcano
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.
Mount Aso is a composite cone volcano, also known as a stratovolcano. It is characterized by its steep-sided profile and alternating layers of lava and volcanic ash.
Paricutin is a cinder cone 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.