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http://jove.geol.niu.edu/students/mdare/VirtualFieldTrip/Mt_Fuji/MountFujiGeology.html#top
Mount Fuji is fed by basaltic magma, which generally ranges in temperature between 1,000 and 1,200 degrees Celsius or 1,830 to 2,200 degrees Fahrenheit.
Mount Fuji is fed by basaltic magma, which generally ranges in temperature between 1,000 and 1,200 degrees Celsius or 1,830 to 2,200 degrees Fahrenheit.
Baslatic magma is hotter.
Scientists have identified distinct phases of volcanic activity in the formation of Mt. Fuji. The first phase is composed of an andesite which forms the deep core of the volcano and this is covered by later basalt lavas.
Basaltic magma is hotter than andesitic magma. Basaltic magma typically has temperatures ranging from 1000°C to 1200°C, while andesitic magma has temperatures around 800°C to 1000°C.
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.
basaltic
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basaltic,andesitic,rhyolitic
Mount Bromo typically produces andesitic magma, which is intermediate in composition between basaltic and rhyolitic magma. Andesitic magma is known for its moderate silica content, resulting in eruptions that can be relatively explosive.
Basaltic magma usually forms a black rock.
Mount Rainier primarily erupts andesitic magma, which is a type of intermediate magma that is thicker and more viscous than basaltic magma. Andesitic magma often leads to explosive eruptions due to its high gas content and tendency to trap pressure.