Temperatures of most magmas are in the range 700 °C to 1300 °C (or 1292 °F to 2372 °F), but very rare carbonatite melts may be as cool as 600 °C, and komatiite melts may have been as hot at 1600 °C
It depends on the rock type- different rock types have different melting temperatures (magma is molten rock) ie the rock called peridotite melts to produce basaltic magma. Other types of magma include rhyolitic and andesitic, which each come from different types of rock. And also it depends on the pressure at which the rock/magma is held at ie the deeper you go down into the earth, the higher a temperature would need to be to induce melting. It is too complicated to just say all magma has the same melting temperature, sorry.
The highest temperature for magma is 1300 degrees Celsius the lowest is 600 degrees Celsius
Minerals do not technically freeze, they crystallize. Magma crystallizes at 850 degrees Fahrenheit, unless it is in a hydro-thermal vein or deposit..
50000000
When the temperature of a rock rises above its melting point it turns into magma, usually found in the mantle (found below the Earth's crust).
The incipient melting point refers to how metal is heated. It is the point just before the metal reaches its melting point.
That depends on the solid: ice has a very low melting point, lard and butter have low melting points, chocolate has a relatively low melting point, wax has an intermediate melting point, lead has a high melting point, iron has a very high melting point, tungsten has an extremely high melting point.
Melting point of Gold = 1064.18 °C Melting point of Silver = 961.78 °C Melting point of Copper = 1084.62 °C Of cause an alloy of all three would probably have a eutectic melting behavour
what is the melting point of ice on top of the Himalayan
No. Water lowers the melting point of magma, both mafic and felsic.
The melting point of diamond is sufficiently high that magma would not melt it.
Magma forms where rock is heated to a temperature above its eutectic melting point.
a diamond's melting point is so highmagma will not melt it
The rock melts to form magma.
The composition of the magma is very important for solidificatoin temperature. When it starts to cool, crystals of minerals begin to grow. If it has a low silica content - which means high melting point - the magma will solidify at high temeratures. If it has a high silica content - which means low melting point - it will solidify at lower temperatures.
A volcano; magma is merely rock that has been heated to the point of melting.
A volcano; magma is merely rock that has been heated to the point of melting.
Magma occurrs by rocks melting inside a volcano
Magma comes from the melting of material in the crust or upper mantle.
Magma
This is the melting point.