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Plate Tectonics
Brief Structure of the EarthDivided into layers:
– Core, mantle, crust
Brief Structure of the EarthLithosphere
– Crust and upper part of the mantle• About 100 km thick
• Rigid
Asthenosphere– Plastic (gooey) layer beneath the lithosphere
• More dense than the lithosphere
Brief Structure of the Earth
Continental Crust– Made up of continents and “edges” of the
oceans– Light
Oceanic Crust– Made up of ocean floor– More dense than continental crust
• Older oceanic crust is more dense than younger oceanic crust
Theory of Plate Tectonics
Developed in 1960’sCombined continental drift and seafloor
spreading.
Theory of Plate Tectonics
Stated that:– The crust and upper mantle (lithosphere) of the
earth are broken into sections called plates.– These plates sit on top of the plastic (gooey)
part of the mantle (asthenosphere).– These plates can move apart, converge, or slide
past one another through time.
Divergent Boundaries
Where plates are moving apart and new crust is forming.– Example: Mid-ocean ridges
Convergent Boundaries
Where two plates collide and crust is destroyed.– Subduction zone
• Area where a dense oceanic plate sinks under a light continental plate or another less dense oceanic plate
– Forms volcanoes.
– When two continental plates collide high mountains are formed.
Transform Boundary
Where one plate is sliding past another plate.– The plates may be going in opposite directions
or the same direction at different rates.• Earthquakes are common
Modern Theories for Cause of Plate Tectonics
All include convection currents in the mantle.
Convection Current
Cycle of heating, rising, cooling, sinkingCaused by differences in density due to
differences in temperature– Example – boiling pan of water
ForcesMovement of plates result in three
types of forces:– Tension – pulls rocks apart– Compression – pushes rocks together– Shearing – pushes rocks past each other
FaultSurface where rock has broken
apart and moved.3 types
– Normal fault– Reverse fault– Transform (or strike-slip) fault
Faults
Normal fault– Rock above the fault moves down.– Formed by tension.
Reverse fault– Rock above the fault plane moves up.– Formed by compression.
Transform fault– Bodies of rock slide past each other.– Formed by shearing.
Features of Tension Forces
Mid-ocean ridge– Where oceanic crust is being pulled apart.
Rift Valley– Where continental crust is being pulled apart.
Features of Compression Forces
Mountains– Continental-continental collisions
• Very high mountains (folded mountains) are formed.
– Oceanic-continental collisions• Volcanic mountains are formed.
– Oceanic-oceanic collisions• Island arcs (volcanoes that reach above the surface
of the ocean) are formed.
Features of ShearingEarthquakes
– Rocks on each side of a strike-slip fault become stuck in one place for a time and then move, releasing energy in the form of an earthquake.
Tracking Plate Movement
Plate movement is tracked using satellites and lasers.– Current rates of movement range from about 1
cm to about 12 cm per year.