Like many stratovolcanoes, Mount St Helens has produced material of mafic, felsic, and intermediate composition. Overall, much of the material is itermediate. The 1980 eruption and later activity have produced dacite, which has an intermediate-felsic composition
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
A mafic lava flow will move faster than a felsic lava flow due to its lower viscosity. However, felsic magma tends to erupt explosively, producing fast-moving pyroclastic flows instead of lava flows.
mafic lava is the KIND of lava produced in mount (mt) Fuji.
Higher viscosity (felsic) lava is typically less hot than the lower viscosity (mafic) lava. Felsic magmas can erupt at temperatures as low as 650 to 750 °C. Poorer in aluminum and silica than felsic lavas, and also commonly hotter, intermediate lava (in the range of 750 to 950 °C), tends to be less viscous. Mafic to ultramafic lavas are believed to erupt up to 1600°C in the past.
The 1980 eruption of Mount St. Helens produced dacite, which has an intermediate-felsic composition.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
A mafic lava flow will move faster than a felsic lava flow due to its lower viscosity. However, felsic magma tends to erupt explosively, producing fast-moving pyroclastic flows instead of lava flows.
Mt. Vesuvius produces felsic lava in a pyroclastic explosion.
mafic lava is the KIND of lava produced in mount (mt) Fuji.
lava came out lava came out lava came out sik answers
Higher viscosity (felsic) lava is typically less hot than the lower viscosity (mafic) lava. Felsic magmas can erupt at temperatures as low as 650 to 750 °C. Poorer in aluminum and silica than felsic lavas, and also commonly hotter, intermediate lava (in the range of 750 to 950 °C), tends to be less viscous. Mafic to ultramafic lavas are believed to erupt up to 1600°C in the past.
The 1980 eruption of Mount St. Helens produced dacite, which has an intermediate-felsic composition.
lava mud ash
Felsic lava is a slower moving lava, with high silica content. Most felsic lava deposits as granite, granite, muscovite, and orthoclase.
Mafic lava is hotter than felsic lava and therefore flows faster.
Much of Mount Rainier is composed of andesitelava flows. Lava flows may accompany explosive eruptive activity, but they occur more often after explosive activity declines. The term "andesite" refers to the chemical composition of the rock. Andesite lavas tend to be moderately viscous and rather slow moving: on gentle slopes, they may move much more slowly than a person can walk.
Mount Rainier is a stratovolcano. This means that it is comprised of several layers of hardened rock, lava nad volcanic ash. Mount Rainier is thought to be one of the most dangerous volcanoes in existence.