in which earth layers does crusal plate movement occur because of convection cells
Convection in the mantle is thought to be one of the potential driving mechanisms of plate movement.
Asthenosphere
mantle or upper mantle
Constant. The tectonic plates of the earth are floating on the mantle, convection current cells cause them to slide around.
The convection cells radiate heat.
Convection in the mantle is thought to be one of the potential driving mechanisms of plate movement.
They are the solid crustal rock floating on the top of a mantle convection cell. They formed the same way slag forms on the tops of convection cells in the molten metal in a smelter furnace. Sections of the mantle also float on the tops of convection cells in the molten metal of the liquid core. If you want to watch the tops of some convection cells form and move, get a cup of some hot drink (e.g. coffee or tea) and let it sit undisturbed for a minute or so to let all currents but convection currents stop. When you look at the surface of the hot drink it will be covered in very tiny polygons. These polygons are the tops of convection cells in the drink, don't they look something like a miniature map of crustal plates? Watch as they expand, contract, and move about.
Convention cells in the molten outer core cause convection cells in the mantle.
Asthenosphere
mantle or upper mantle
Convection cells turn down because when the cells are away from the heat source the cells begin to cool. If cells are cooler they are more dense. Therefore, the change in density causes the cells to sink.
Both continental and oceanic plates float on the top surface of the mantle, which is divided into convection cells. The movement of these convection cells drag the plates along: where convection causes the mantle material to fall the plates are pushed together and where convection causes the mantle material to rise the plates are pulled apart.
The crustal plates (made mostly of low density granitic rock) float on the mantle (made mostly of high density basaltic rock). Convection cells in the mantle move the floating crustal plates around.
Both continental and oceanic plates float on the top surface of the mantle, which is divided into convection cells. The movement of these convection cells drag the plates along: where convection causes the mantle material to fall the plates are pushed together and where convection causes the mantle material to rise the plates are pulled apart.
The plates of crustal rock floating on the mantle rockand being moved by the flow of mantle rock in convection cells driven by the heating of radioactive decay deep in the core and lower mantle.
The cells fill with water because of the movement of water by osmosis. (APEX)
The convection cells radiate heat.