The size of the magma chamber and the viscosity of the magma.
Silica is something in the magma, so it is a pretty important part of magma because it pretty much a part that makes magma!
Magma is mainly consisting of molten rock, which is a mixture of solid minerals, gases, and liquid rock. The composition of magma can vary depending on factors such as depth, temperature, and the geological setting.
viscosity of magma build up of gases
The formation and composition of the magma, and the local subterranean geology.
Viscosity is the measure of a liquids resistance to flow. In the case of magma, the hotter it is, the lower the viscosity.
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
The size of the magma chamber and the viscosity of the magma.
magma that is low in silica and flows easily
Silica is the mineral that determines magma viscosity. Magma with high silica content tends to be more viscous, leading to slower flow and potentially more explosive volcanic eruptions.
The rate at which magma cools determines the size of the mineral crystal.
flows easily
Silica is something in the magma, so it is a pretty important part of magma because it pretty much a part that makes magma!
Magma is mainly consisting of molten rock, which is a mixture of solid minerals, gases, and liquid rock. The composition of magma can vary depending on factors such as depth, temperature, and the geological setting.
The composition of the magma and the local magnetic flux as it crossed the Curie point.
viscosity of magma build up of gases
The cooling rate of the magma primarily determines the size of a mineral crystal. Faster cooling rates lead to smaller crystals, while slower cooling rates result in larger crystals. Other factors such as the mineral composition and level of nucleation can also influence crystal size.