mafic lava is the KIND of lava produced in mount (mt) Fuji.
The 1980 eruption of Mount St. Helens produced dacite, which has an intermediate-felsic composition.
Paricutin erupted mafic lava.
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.
As a shield volcano, Mauna Kea erupts mafic lava.
The 1980 eruption of Mount St. Helens produced dacite, which has an intermediate-felsic composition.
Mafic lava is hotter than felsic lava and therefore flows faster.
Paricutin erupted mafic lava.
Composite volcanoes can erupt both mafic and felsic material, but intermediate material is the most common.
Mauna loa erupts mafic lava.
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.
As a shield volcano, Mauna Kea erupts mafic lava.
it has mafic and felsic duhhhhh
== == Felsic lava has a higher silica content than mafic lava. Felsic lava is slower moving (high viscosity) than the less viscous mafic lava. Mafic lava is higher in dark minerals and higher in the elements iron and magnesium.
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
Mafic magma and Felsic magma.
mafic because it is-dark colored. Ultramafic - no light colored mineral which means it it attracts most heat from a volcano taking it longer to cool down from the lighter, in between substance known as felsic :D