Unit 4 Flashcards
Crust
solid rocks on earth surface (oxygen, silicon, aluminum, iron, igneous and metamorphic rocks)
Mantle
Flowing rocks (mostly silicates)
Outer core
liquid iron and nickel
Inner core
solid iron and nickel
Asthenosphere
the soft, flexible upper layer of the mantle, on which the tectonic plates move
Continental drift
the theory that all of Earth’s continents were once joined together into a single large landmass (Pangea), and then moved apart, forming the continents we see today
Convection
transfer of heat by movement of a fluid
Convection currents
movement within hot fluids, when the heat source is on the bottom, such as in a boiling pot of soup on the stove. Convection currents happen because the hotter material is less dense and rises; when it reaches the surface, it cools and becomes less dense, so it sinks. This rising and sinking creates a circular motion within the fluid.
Convergent plate boundaries
where two tectonic plates move towards each other
Divergent plate boundaries
where two tectonic plates move away from each other
Gondwana
the southern continent formed when Pangea split into two pieces
Laurasia
the northern continent formed when Pangea split into two pieces
Lithosphere
the rigid, brittle layer made up of the crust and the uppermost part of the mantle. It is broken up into pieces called tectonic plates.
Mantle convection
convection currents in the mantle that occur because hot rock in the lower part of the mantle is less dense and rises, and cooler rock in the upper part of the mantle cools, becomes more dense, and sinks. Mantle convection is thought to be the mechanism driving the movement of tectonic plates.
Mid-ocean ridge
a system of connected underwater mountain ranges that run throughout the world’s oceans. There is a rift valley in the center of the mid-ocean ridge, where magma rises up from the mantle, and pushes out to either side, producing seafloor spreading.