asthenosphere
asthenosphere
In which region of the Earth's interior does the heat increase to the point that rocks can begin to melt?
The heat increases to the point that rocks can begin to melt in the region known as the mantle. This layer lies beneath the Earth's crust and is composed of solid rock, but under high temperatures and pressure, some rocks can melt and form magma.
Catalysts decrease activation energy.
The outer core is liquid and convects. The mantle also convects, although it is almost entirely solid and it is a matter of debate whether the entire mantle convects, or whether there are seperate layers each individually convecting.
asthenosphere
asthenosphere
asthenosphere
The heat increases to the point that rocks can begin to melt in the region known as the mantle. This layer lies beneath the Earth's crust and is composed of solid rock, but under high temperatures and pressure, some rocks can melt and form magma.
The heat increases to the point that rocks can begin to melt in the lower part of the Earth's mantle, known as the asthenosphere. This is where the temperature and pressure conditions allow for rocks to melt and form magma.
In which region of the Earth's interior does the heat increase to the point that rocks can begin to melt?
In which region of the Earth's interior does the heat increase to the point that rocks can begin to melt?
asthenosphere
In which region of the Earth's interior does the heat increase to the point that rocks can begin to melt?
Interior Designer
The Crust,The Mantle and The Core
What needs a heat source to begin evaporating. Normally the sun is the heat source that evaporates water on the earths surface.