Convection Currents Flashcards
Convection Currents
Magma near the outer core is heated. This causes it to expand, become less dense and rise towards the crust. As it rises, it slowly begins to cool. Once the magma reaches the crust, it spreads out and moves ten tectonic plates with it. The cooling magma becomes less dense and begins to sink towards the outer core where it is reheated again, triggering the same cycle. The rising and falling motion of the magma creates circular currents also known as convection currents
Tectonic Plate
A large piece of Earth’s crust floating on the mantle
Plate Boundary
Where 2 or more tectonic plates meet
Oceanic Plate
Tectonic plate with water on top of it. These are normally heavier/more dense
Continental Plate
Tectonic plate with land on top of it. These are normally lighter/less dense.