Granitic magma is highly viscous, meaning it has a high resistance to flow. Granitic magma does not reach the surface very often. It cools underground, thus we have granite. If granitic magma actually reaches the surface it would result in a highly explosive eruption.
An explosive one: granite forms viscous lava, and forms a hard plug inside the volcano, and when pressure below the plug is substantial enough, the volcano blows. Big time. This varies in interpretation, so it could be Plinian, if you want a specific term, but overall, the eruption is very violent, and the violence and scale varies from case to case.
cinder cone volcano and composite volcano.
normally found in a volcanic eruption zone where carbon is present
pikatela
Pahoehoe is one substance usually not present in explosive volcanic eruptions. Tephra, lava and other gasses are typically present during an eruption.
There are two factors that determine how explosive a volcano is. The two factors are the amount of gas that is present in the lava and how easy or difficult that gas can be released into the atmosphere.
The essential minerals are Quartz, Felspar and Mica. Accessory minerals may alsobe present but all the three above must be present for the rock to be a granite.
normally found in a volcanic eruption zone where carbon is present
pikatela
Pahoehoe is one substance usually not present in explosive volcanic eruptions. Tephra, lava and other gasses are typically present during an eruption.
There are two factors that determine how explosive a volcano is. The two factors are the amount of gas that is present in the lava and how easy or difficult that gas can be released into the atmosphere.
Basaltic magma usually produces a Hawaiian or Stombolian style of eruption.
At present there is no observed volcanic activity of Mars. The super volcano of Olympus Mon on Mars is thought to be inactive, dating its past eruption from several to 15+ million years ago.
They can be. Most mountain ranges form when the land is thrust upward by tectonic activity, so the type of rock present depends on what rock is present to begin with. The cores of mountain ranges, though, are often made of granite and gneiss. Volcanic mountains are not made of limestone.
The essential minerals are Quartz, Felspar and Mica. Accessory minerals may alsobe present but all the three above must be present for the rock to be a granite.
quiet
Never say never, but it's mica.
An example of a "quiet" eruption would be the 1983-present eruption of Kilauea in Hawaii. A violent eruption would be the 1980 eruption of Mount St Helens.
nothing