The mineral that significantly affects the thickness (viscosity) of magma is silica. Higher silica content in magma leads to increased viscosity, making it thicker and more resistant to flow. Conversely, magma with lower silica content is less viscous and flows more easily. This variation in viscosity plays a crucial role in determining the type of volcanic eruptions and the shape of volcanic landforms.
The composition of the minerals is not a factor that affects the size of mineral crystals formed in magma. The factors that do affect crystal size include cooling rate, amount of water present, and amount of pressure.
All of these factors affect the viscosity of magma. The amount of gases can influence the fluidity, while the silica content directly impacts thickness, and temperature affects the overall mobility of the magma. Therefore, none of these factors can be excluded as they all play a role in determining viscosity.
their are many types of magma because when a volcano has soft magma that means it either exploded small or the magma was going really slow and fast magma and big exploding volcano's are hard magma.:)
The mineral that crystallizes first from magma is olivine. Olivine has a relatively high melting temperature compared to other minerals, so it is among the first to solidify as magma cools and begins to solidify.
The mineral that affects magma thickness is silica. Magma with high silica content tends to be more viscous, resulting in thicker magma. Conversely, magma with low silica content is less viscous and flows more easily.
The mineral quartz affects the thickness of magma by increasing its viscosity. When quartz-rich magma cools and solidifies, it forms a dense and viscous rock, like granite. This high viscosity can result in explosive volcanic eruptions.
The mineral that significantly affects the thickness (viscosity) of magma is silica. Higher silica content in magma leads to increased viscosity, making it thicker and more resistant to flow. Conversely, magma with lower silica content is less viscous and flows more easily. This variation in viscosity plays a crucial role in determining the type of volcanic eruptions and the shape of volcanic landforms.
Mineral composition of the magma, Rate of cooling of the magma, Temperature of the magma, Presence of volatiles and Amount of water present in the magma.
Magma is not a mineral becauseIt is liquid.It does not have a definite chemical composition.
The composition of the magma affects how explosive a volcanic eruption will be.
evaporation
The rate of cooling of the magma determines the type of mineral formed by the magma or lava..
The melted mineral material in the mantle is called magma.
No, Magmatic is and adjective meaning of or realting to magma. Magma is not a mineral but molten rock underground.
Thickness affects sound.
The main factor is time spent in cooling and solidifying. More time means larger crystals.