In the outer core of the earth's interior, the melting point of the rock is inferred to be lower than the actual temperature of the rock.
In geology, the physical composition of the planet earth shows that is composed of three distinct layers: crust, mantle, and core.
The earth's interior is called the core and the core is further divided into two segments: the outer core and the inner core.
The outer core lies adjacent to the mantle while the inner core is the center point.
Generally, the melting point of a solid substance decreases as pressure increases. So if we go deeper into the earth we will see that the pressure is quite high in the core due to which the melting point of rocks decreases than their actual temperature.
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