A solid layer made of iron and a nicel
The mantle extends 1800 miles into the earth and is divided into two parts. The upper mantle is part of the lithosphere an is strong and rigid. The lower mantle is part of the asthenosphere and is hotter and flows under pressure. This part of the mantle is soft and weak. The mantle makes up the largest percentage of the earth's interior.
It is the thickest layer of the Earth. The crust ( where we live ) is right on top of it. If something digs into the ground, it is still in the crust. It might seem really thin, but not that thin to us little people of the world! ;)
In the matle there are two layers, the asthenosphere and the lithosphere.
the lithoshpere is the outermost layer and is hard, thin, and brittle. this layer connects to the crust (earths outermost layer) and has cracks in it creating tectonic plates.
The asthenosphere (the lower layer) is made of soft almost liquid molten rock rock the lithosphere "floats" on this layer. The asthenosphere has convection currents which cause the movements of tectonic plates causing continental drift.
-----this was a brief run through of the mantle from yours truly the bored kid doing homework and answering questions.......I am always accurate but I may not always have a ton of detail- and will be adding a mark on my answers.
>E<
a mix of layers of hot rocks and magma/lava :)
extremely hot to the point of burning up
If we're talking layers of the earth, that would be the upper mantle, below the crust.
Partially molten, plastic like, flowing layer located below the solid part of Earth's mantle is the Asthenosphere. The asthenosphere is mechanically weak and ductiley deforming region of the upper mantle.
Mantle Is The Below Layer Of The Crust In Earth.
Convection currents in the mantle drive plate movements.
at the end of the earth.
The Process Is called solution
If we're talking layers of the earth, that would be the upper mantle, below the crust.
You might have been confused gum for taffy. The mantle is like taffy/gum because it is supposedly runny. (well, I guess I would be HOT taffy)
The asthenosphere is made of soft rock and bends like plastic in the mantle.
If the convection currents in the earth's mantle slowed down then the mantle would slow down. Eventually, the mantle would stop all movement.
The earth would look like it did when it formed
form_title=Install a Fireplace Mantle form_header=Upgrade the look of a room with a mantle. What type of mantle do you want installed?=_ What type of fireplace is in place?=_ What material would you like used?= () Wood () Marble () Tile () Brick () Laminate () Other
it would harden just like silly putty
the upper-mantle rocks are heavier while the lower mantle rocks are semisolid like melted plastic
The answer to this question would be the mantle.
It is the ability of the mantle (solid) to flow like liquid.
No, the main heat source for the mantle (as well as the core) is radioactive decay of elements like uranium within the mantle itself (or core, respectively). Heat rising from the core into the already hot mantle does set up the differential heat profile that drives much of the mantle convection, but even without the additional core heat the mantle would convect (but slower) so that its heat would rise to the crust.