Final answer:
Mt. Fuji, Japan, is not a classic cinder cone volcano but a stratovolcano. Paricutin in Mexico is an example of a classic cinder cone volcano.
Step-by-step explanation:
False.
Mt. Fuji, Japan, is actually considered a stratovolcano, also known as a composite volcano, not a classic cinder cone volcano. A stratovolcano is characterized by a steep-sided cone shape and a composite of alternating layers of lava and ash.
An example of a classic cinder cone volcano is Paricutin in Mexico, which is a simple, symmetrical cone formed by the eruption of cinders and other loose volcanic material.
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