Mount Fuji primarily consists of basaltic and andesitic rocks, formed from volcanic activity. The mountain's structure is a stratovolcano, characterized by alternating layers of lava flows, volcanic ash, and other pyroclastic materials. The composition reflects its explosive eruptions and the presence of both fluid lava and more viscous magma. Additionally, the summit features a layer of volcanic rock known as "Fujiite," which is unique to this volcano.
Mount Fuji is a composite volcano.
it has metomorphic as rock and touchy lava
Mount Fuji is in Japan
The lava that formed Mount Fuji is primarily composed of dacite and andesite, which are intermediate in composition between basaltic and rhyolitic lava. This type of lava is viscous and flows relatively slowly, contributing to the steep slopes of Mount Fuji.
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mount fuji
The height of Mount Fuji is 11,388 feet. Mount Fuji is in Japan and it is the highest mountain there.
In Tokyo, Japan. Mount Fuji's height is 3,776meters.
Mount Fuji is a Volcanic mountain formed from volcanic vents in the Earth's crust that builds up over time when magma comes out as lava on the Earth and dries up into rock.
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Mount Fuji's elevation is 12,388 feet.
Mount Fuji is classified as a dormant volcano.