the mantle is made up of solid hot rock.
Continental rock is less dense than mantle rock.
The mantle isn't 100% liquid because magma solidifies near the crust and becomes plastic in texture and not fluid but eventually cools down to form the lithosphere. Lower parts of the mantle are not liquid because the high pressure keeps rock from melting.
the plasic like rock of the lower mantle is the asthenosphere
The mantle rock would be densest where it is closest to the Earth's core, which is at the boundary between the mantle and the outer core. This is due to the high pressure and temperature conditions at this depth.
Rich in magnesium and iron due to their origin from ultramafic mantle rock. They are usually less viscous compared to melts formed from other types of rock. The composition of these magmas can vary depending on the degree of partial melting and the specific mantle source.
The Asthenospheric mantle and the Inner mantle are made up of solid rock and liquid rock.
Mantle rock is classified as ultramafic igneous rock.
No, solid rock located deep in the mantle is not called magma. Magma is molten rock that is found beneath the Earth's surface in the mantle and crust. Solid rock in the mantle is known as the lithosphere.
the two layers of rock that made up of mantle is the solid rock and liquid rock
Not exactly--the mantle is comprised of semisolid rock, or magma.
Melted rock in the Earth's mantle is called magma.
Yes, the mantle is largely composed of igneous rock. It is made up of solid rock that is partially molten, allowing for the movement of tectonic plates. Magma from the mantle can solidify to form igneous rock when it reaches the Earth's surface.
Continental rock is less dense than mantle rock.
The mantle is the hot rock.
Yes. It's true that slow movements of mantle rock called convection transfer heat in the mantle
When rock in the mantle cools, it becomes denser and can sink due to its increased weight compared to surrounding material. This process can lead to convection currents in the mantle, with cooler, denser material sinking and warmer material rising.
Igneous rock