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The main 7 tectonic plates around the world are: the Eurasian plate; African plate; Indo-Australian plate; Pacific plate; North American plate; South American plate; and the Antarctic plate.
Tectonic Plate movement
the force of gravity
There are 15 main plates altogether they are the:African PlateAntarctic PlateEurasian PlateIndo-Australian PlateNorth American PlatePacific PlateSouth American PlateArabian PlateCaribbean PlateCocos PlateIndian PlateJuan de Fuca PlateNazca PlatePhilippine Sea PlateScotia PlateOf these the African Plate, the Eurasian Plate, the Indo-Australian Plate, the North American Plate, the South American Plate, and the Antarctic Plate are major continental plates.
Three processes that contribute to the motion of tectonic plates are convection currents, ridge push, and slab pull. Convection currents is when the mantle rises, cools, sinks and heats, then rises and repeats the cycle. Ridge push is a gravitational force that causes a plate to move. Slab pull is the movement of tectonic plate lithosphere due to convection currents in the asthenosphere.
slab pull
slab pull
Water flow
Water flow
The main 7 tectonic plates around the world are: the Eurasian plate; African plate; Indo-Australian plate; Pacific plate; North American plate; South American plate; and the Antarctic plate.
There are three primary types of tectonic plate boundaries. They pertain of Divergent boundaries, Convergent boundaries and Transform-fault boundaries.
Tectonic Plate movement
The slab sinks faster and this pulls on the rest of the plate, continuing plate tectonics. Mantle convection creates the instability that allows plate tectonics to get going and helps a little, but it's not thought to be the main driving force.
Escape of thermal energy form the Earth's core.
the force of gravity
The main 7 tectonic plates around the world are: the Eurasian plate; African plate; Indo-Australian plate; Pacific plate; North American plate; South American plate; and the Antarctic plate.
Our Tectonic plates shifting and moving around.