The mantle is a hot crystalline material - not hot enough to be molten but hot enough to undergo ductile deformation. It behaves like a solid, but in longer times can behave as a viscous liquid.
The Earth's mantle convects due to the high temperatures of the Earth's core. However this flow (unlike that in liquids) is technically known as "creep". Creep is essentially a very, very slow deformation (mm / yr) that occurs in solid materials that are under stress for long periods of time. High temperatures can also increase the rate of creep. Both high stress (due to the weight of overlying material) and high temperatures occur in the mantle.
no part
No. It behaves like a solid.
The outer core of the mantle can be liquid.
It is the ability of the mantle (solid) to flow like liquid.
the rock that can flow like a liquid is a mantle because the mantle has two parts. The upper part is the solid rock. The solid rock of the mantle is part is the lithosphere. Below the solid rock, the mantle rock has the ability to flow like a liquid. Most of the mantle is made up of rock that can flow. Sanjida Ahmed 752/753
If we're talking layers of the earth, that would be the upper mantle, below the crust.
The mantle
no part
No. It behaves like a solid.
No. It behaves as a solid.
The mantle of Earth contains magma or so you can call it lava which is a liquid from 700-1200 degrees centigrade.
The continents "float" on the liquid mantle of the Earth because the metals that make up the mantle are very dense. The continents move when magma is pushed through the crust of the Earth in places like the Mid-Atlantic Ridge. The continents "float" on the liquid mantle of the Earth because the metals that make up the mantle are very dense. The continents move when magma is pushed through the crust of the Earth in places like the Mid-Atlantic Ridge.
The crust and the upper part of the mantle are the solid part of the Earth called the lithosphere.
The outer core of the mantle can be liquid.
The upper part is thick and fudge like, and the lower part is more like liquid. It's all hot, molten rock.
The core is solid metal surrounded by liquid metal, the mantle is liquid rock.
It is the ability of the mantle (solid) to flow like liquid.