Magma is a complex high-temperature fluid substance. Temperatures of most magmas are in the range 700 °C to 1300 °C (or 1300 °F to 2400 °F), but very rare carbonatite melts may be as cool as 600 °C, and komatiite melts may have been as hot as 1600 °C. Most are silicate mixturess.
Mount Fuji is fed by basaltic magma, which generally ranges in temperature between 1,000 and 1,200 degrees Celsius or 1,830 to 2,200 degrees Fahrenheit.
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
High temperature=low viscosityLow temperature=high viscosity
temperature. Magma with higher silica content tends to have higher viscosity, while temperature can also affect viscosity by influencing the mobility of the magma's mineral components.
The temperature of magma typically ranges between 700°C to 1300°C, while the surface temperature of the sun is around 5500°C. Therefore, the sun's temperature is significantly higher than that of magma.
Mount Fuji is fed by basaltic magma, which generally ranges in temperature between 1,000 and 1,200 degrees Celsius or 1,830 to 2,200 degrees Fahrenheit.
The composition of the magma effects the temperature it will cool and solidify at. In general most magma solidify at about 1,200 degrees Fahrenheit.
Temperature, among other factors, effects the viscosity(thickness) of magma. However, for the most part, the temperature of magma is relatively consistent because magma is the type of molten rock that has not yet exited the volcano, so there are fewer factors to effect the temperature.
Magma is usually 1300 to 2400 degrees F (600 to 1300 degrees C)
The air affects magma. Once magma is released above ground, called lava, the air hardens it. While it is underground, the higher the temperature and pressure, the runnier the magma.
High temperature=low viscosityLow temperature=high viscosity
High temperature=low viscosityLow temperature=high viscosity
High temperature=low viscosityLow temperature=high viscosity
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.
temperature. Magma with higher silica content tends to have higher viscosity, while temperature can also affect viscosity by influencing the mobility of the magma's mineral components.
The temperature of magma typically ranges between 700°C to 1300°C, while the surface temperature of the sun is around 5500°C. Therefore, the sun's temperature is significantly higher than that of magma.
The composition of the magma plays a significant role in determining its melting temperature. Magma with higher silica content tends to have a higher melting temperature. Pressure also affects the melting temperature; higher pressure usually results in a higher melting temperature. Water content can lower the melting temperature of magma by acting as a flux, allowing minerals to melt at lower temperatures.