In the mantle, there is a fluid-like layer called the asthenosphere which has convection currents, due to the heat of the inner core. Earth's plates are hypothetically "floating" on the asthenosphere. The currents in this layer push whatever is on top of it, thus the continents move.
The crustal plates move on the semi-fluid asthenosphere due to convection currents in the mantle. These convection currents cause the plates to either separate, collide, or slide past each other, leading to various geological phenomena like earthquakes, volcanic activity, and mountain formation.
The lithosphere is the continental crust, oceanic crust and upper part of the mantle. The convection currents move in the mantle mostly in the Asthenosphere layer under the lithosphere. As the convention currents move it makes the lithosphere spread and shake.
Convection currents are circular movements of fluid driven by temperature differences. In Earth's mantle, convection currents occur in the asthenosphere, which is the semi-solid layer beneath the lithosphere. These currents play a significant role in plate tectonics and the movement of Earth's crustal plates.
The soft part of the mantle where convection currents occur is known as the asthenosphere. This region lies beneath the lithosphere and is characterized by partially molten rock that allows for the flow of material. The convection currents in the asthenosphere are driven by heat from the Earth's core, facilitating the movement of tectonic plates above. These currents play a crucial role in geological processes such as plate tectonics and volcanic activity.
Convection Currents carry the plates
The convection currents running through the asthenosphere are widely believed to be the source of movement of the tectonic plates.
The lithosphere is generally thought of as the crust and outer mantle of the earth. They're solid, and there are no convection currents in solids as we normally think of them. As we move inward toward the core of the earth, we begin to encounter molten rock (magma), and convection currents exist in this superheated fluid.
b. asthenosphere Convection currents in the asthenosphere are believed to be responsible for driving plate movement through the process of mantle convection. This movement of the semi-fluid asthenosphere layer beneath the rigid lithosphere is thought to cause the plates to move over the Earth's surface.
The mantle is inferred to have convection currents that cause tectonic plates to move. Heat from within the Earth creates these currents, leading to the movement of the rigid plates on the Earth's surface.
from the bottom of the earth
There way more than that.
Convection currents move in the Mantle.
The asthenosphere, which is a partially molten layer in the upper mantle, has convection currents that cause tectonic plates to move due to the heat-driven circulation of rock material. These convection currents are responsible for the continuous motion of tectonic plates on the Earth's surface.
It is the movement of ductile rock in the asthenosphere caused by convection currents that creates movement of the lithospheric plates. It is the conveyor belt on which the plates move.
Convection currents move in upward direction
The heat driving convection currents in the asthenosphere primarily comes from the Earth's internal heat. This heat is generated through the radioactive decay of elements in the Earth's mantle and core. The flow of this heat causes the asthenosphere to partially melt and create convection currents that drive the movement of tectonic plates.