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Mount Pinatubo primarily erupts dacitic magma.
Mount Shasta typically has andesitic magma, which is a type of intermediate magma that is common in subduction zone environments. This type of magma is rich in silica and forms from the partial melting of both oceanic and continental crust.
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.
Ash and poised magma that will turn into Metal!
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.
The magma that erupts at Mount Pinatubo is mainly dacitic in composition, which is a type of intermediate magma that is rich in silica. This type of magma typically leads to explosive eruptions due to its high viscosity and gas content.
Mt. Cleveland has felsic lava, high in silica.
Mount Bird is in Antarctica. It has basalt magma.
Yes, Mount Adams is a volcano
Mount Shasta is a stratovolcano, which is a type of volcano characterized by a steep-sided cone shape and explosive eruptions due to volatile-rich magma.
The area of Mount Adams Wilderness is 191.335 square kilometers.
It is that it has high silica content