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Plate tectonics
describes the movement of the lithosphere in response to mantle convection.
Alfred Wegener
Proposed the theory of “continental drift”
Continental drift explained
Shape of continents
Contiguous geological features
Evidence of past glaciers near the equator
Fossils of similar animals on unconnected continents
Magnetism in ocean crust
Magnetometer record showing symmetrical magnetic field across ridge.
Earth’s Magnetic field
Earth’s rotation causes spiral flow in the liquid outer core that aligns with spin axis.
Electrically charged spiral flow generates Earth’s magnetic field
Where is new crust created?
Mid-ocean ridges
Convection flow of mantle pushes plate outwards.
Old plates are recycled into the mantle (subduction).
Supercontinent Cycle (Wilson Cycle)
Supercontinent
Continental rifting
Seafloor spreading
Subduction Initiation
Convergence
Orogenesis