No. It is a layer of rock. The very uppermost layer of the mantle is attached to the crust. The layer directly below it is very plastic-like, yet still considered rock. With increasing depth, the rock of the mantle becomes more and more rigid from increasing lithostatic pressure. The next layer after the mantle is the outer core, which is composed of iron and nickel in a liquid state. Finally, the inner core, solid, an alloy of iron and nickel.
"Plastic" perfectly describes the molten rock in the mantle. The word means that the rock is soft and flexible. When a person talks about "plastic" in common usage, they are referring to polymers such as polyethylene and polystyrene. No ordinary polymer can survive the temperatures in the mantle.
No, and we can be grateful that it is not. That's one of the most fanciful and mind-bending thoughts I've seen in a long while.
The bottom layer of the outer mantle is tough liquid iron and magnesium silicate rock, and the top layer is iron and magnesium silicate rock that is stiffer because the temperature is cooler.
The mantle experiences extremes in heat and pressure and may be partially melted.
The asthenosphere
yes it does
The asthenosphere
Asthenosphere
It is the theory of plate tectonics.
The Earth's plates are lighter than the mantle. The top layer of the mantle is almost plastic in it's ability to bend and move without breaking. Heat from the interior of Earth appears to rise in currents through the mantle. The crustal plates ride on these currents as new crust is created at the mid-ocean ridges, and destroyed at oceanic trenches.
They move because of the heat from the outer core and the mantle.
mantle.
Asthenosphere
It is the theory of plate tectonics.
crust
The layer of the Earth known as the asthenosphere, composed of highly viscous, plastic-like rock located in the upper mantle.
The Earth's plates are lighter than the mantle. The top layer of the mantle is almost plastic in it's ability to bend and move without breaking. Heat from the interior of Earth appears to rise in currents through the mantle. The crustal plates ride on these currents as new crust is created at the mid-ocean ridges, and destroyed at oceanic trenches.
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.
They move because of the heat from the outer core and the mantle.
The zone below the lithosphere is the mantle. Convection currents occur here because of the magnetism in the Earth. It is somewhat plastic like.
Convection in the earth's mantle.
The outer mantle
The rock of the upper mantle known as the asthenosphere is plastic-like but not molten. It acts like a conveyor belt, moving heat from Earth's interior upward, and cooled material downward in a big loop. New crust is created where mantle material reaches the surface at places called mid-ocean ridges. Older, colder oceanic crust is subducted and drawn into the mantle, completing the loop.
mantle.