Melting points of rocks igneous rocks form through the crystallization of magma there is a considerable range of melting temperatures for different compositions of magma.
Temperature to melt granite.
Often the silicates are grouped as high medium and low melting point solids.
The presence of water in the rock is important to lower the melting temperature.
This video is aheating melting and vitrification of granite by the halogen point heater.
Granite has poor primary permeability overall but strong secondary permeability through cracks and fractures if they are present.
Because of the mineralizers in the magma the temperature interval over which it crystallizes will be lower than that over which the rock can be melted in an open crucible in the laboratory.
Please note the fact that melting point of granite is 2210o to 2300o f 1210o to 1260o celsius whereas you cook your steak at around 350o to 450of 177o to 232o celsius.
It is strongly reduced in the presence of water down to 650 c at a few kbar pressure.
All the silicates are molten at about 1200 c when a part of rock and all are solid when cooled to about 600 c.
The melting temperature of dry granite at ambient pressure is 1215 1260 c 2219 2300 f.
Geothermal gradient is the rate of increasing temperature with respect to increasing depth in earth s interior.
Please check the following site for more information.
If you were trying to melt hawaiian basalt lava it would not melt but it would glow bright orange.
Paul woskov a senior research engineer at mit s plasma science and fusion center psfc is using a gyrotron a specialized radio frequency rf wave genera.
The melting point of granite is 550 degrees c.
Strictly speaking geo thermal necessarily refers to earth but the concept may be applied to other planets.
Away from tectonic plate boundaries it is about 25 30 c km 72 87 f mi of depth near the surface in most of the world.