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.
anywhere from 1,300 to 2,200 degrees Fahrenheit.
1300 degrees is the highest temperature, 600 degrees is the lowest temperature, and 1000 degrees Celsius is the typical temperature for magma.
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.
· It is determined by the primary factors of the magma's Temperature, its Composition, and the amount of Dissolved Gases it contains.
High temperature=low viscosityLow temperature=high viscosity
pressure and temperature
Magma is molten meaning liquid-like so it is able to move inside earth. The tectonic plates separate the earth and magma. This explains when the plates move earthquakes and volcanoes occur. Lava is not magma by the way! lava is hardened magma and magma is molten!
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.
felsic magma
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.
· It is determined by the primary factors of the magma's Temperature, its Composition, and the amount of Dissolved Gases it contains.
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.
Most often between 700 and 1300 degrees C..
yes but at conciderably high temperature! have you seen magma (larva?) Most lava or magma types will fall in a temperature range of 1300-2400oF (700 to 1300oC) so that is essentially burning rock... and other stuff that mixed into it.so if you can invent something thAT COULD throw a liquid out at that temperature or a gas at a slighly higher temperature i guess you can burn stone buildings ! COOL MAN!
pressure and temperature