Mount St. Helens has a magma chamber that can hold approximately 2 to 5 cubic kilometers of magma. However, the exact capacity can vary due to geological processes and the dynamics of volcanic activity. Since its major eruption in 1980, the volcano has continued to evolve, affecting the size and characteristics of its magma reservoir.
It happened because of an overflow of magma.
Mount St. Helens could possibly hold up to 0.3 cubic kilometers of magma in its magma chamber. However, the exact volume can fluctuate based on various factors such as temperature, pressure, and composition of the magma.
The magma beneath Mount St. Helens is typically of low viscosity due to its composition, which is rich in silica and gas. This low viscosity magma allows for gases to escape easily, resulting in explosive eruptions.
Mt. St. Helen's is in Washington, the state.
Mt. Hekla in Iceland has a composition of intermediate to felsic magma, which is rich in silica, giving it a higher viscosity compared to basaltic magma. This type of magma can lead to explosive eruptions.
450thousend littlers of magma the magma is a salty base and runny as it can get donot get in the path of this valcano
It happened because of an overflow of magma.
it was 2000 digrees faren height
it is basaltic, granitic i dont know which one but one of them i think
where did mt Helen's occur
Mount St. Helens could possibly hold up to 0.3 cubic kilometers of magma in its magma chamber. However, the exact volume can fluctuate based on various factors such as temperature, pressure, and composition of the magma.
The magma of the Hawaiian volcanoes has a basaltic composition, which means it has a low viscosity (it flows easily) and so can erupt easily without needing too much force behind it. This low viscosity magma cannot hold very much gas and so erupts effusively By contrast, the magma involved in the 1980 eruption of Mount St Helens had a dacitic composition, which has an extremely high viscosity. The high viscosity allows large mounts of gas to be stored in the magma under pressure. When the magma was exposed to lower pressure near the surface, the gas was released and expanded explosively, blasting the magma into ash and pumice.
On Mt Chimney to find it you need a magma emblem which you will get on Mt Pyre.
you can get a magma stone with buck at stark mt
The magma beneath Mount St. Helens is typically of low viscosity due to its composition, which is rich in silica and gas. This low viscosity magma allows for gases to escape easily, resulting in explosive eruptions.
The composition of Mt. Etna is basaltic.
on top of graveyard mt(mt pyre)