Plate Boundaries And Continental Drift Flashcards
Who proposed the theory of continental drift and when?
Alfred Wegener in 1912, worked on his idea until 1930 when he died
What is Pangaea and when did Wegener proposed it to exist?
Pangaea is the super continent of all the continents being together. He proposed it to exist in the Carboniferous period 250 million years ago
What is palaeomagnetism?
Changes in the polarity. The magnetism of the Earth experiences magnetic reversals every 400,000 to 500,000 years. These are recorded in the solid solidified rocks at constructive margins
How is the earths magnetic field shown in the rocks?
The lava holds iron particles and depending on the polarity at the time of formation, it can get locked in the rocks and examined to show the striped pattern.
How does sea floor spreading prove continental drift?
Fresh molten rock reaches ocean bed and older rock gets pushed away from the ridge in a ‘conveyor belt’ way. Sea floor spreading moves material across ocean floors, widening it. Plates moved by sea floor spreading from mid-ocean ridges to ocean trench where material gets subducted into the asthenosphere.
What did the 1960s ocean drilling programme prove?
Thickest and oldest sediment was found nearest to continents, and no rocks were older than 200 million years, confirming the constant recycling of the crust. Also found a spatial pattern of sediments, supporting sea floor spreading
What is the lithosphere?
Rigid outer layer of the earths rocks consisting of the crust and upper mantle. It is the coolest and most rigid part.
What is Mohorovičić discontinuity?
The boundary between mantle and crust where there are sudden changes in seismic wave velocities. Indicates transition between rock compositions.
Asthenopshere
Located below the crust, portion of the earths mantle that flows like molten plastic. It is involved in plate tectonic movement as convection currents happen here. Semi-molten, hot plastic.
What are convection currents?
Occurring within the molten rock, they act as a push force for the tectonic plates. The direction of movement and type of plate margin is determined by which way they flow. Heat rising and falling inside the mantle creates these currents generated by radioactive decay in the core.
Explain ridge-push and slab-pull.
Slab pull - subduction zone, force of the dense oceanic plate subducting under the continental plate and pulled by gravity into the mantle. Ridge push - pushing force plates experience when plates move apart.
How does palaeomagnetism prove evidence for continental drift?
There is a striped pattern on the ocean floor that begins with lava erupting. This lava contains iron particles and once erupted, they lock into the igneous rocks so the magnetic orientation is locked in depending on the polarity at that time. this shows continental drift because symmetrical patterns are created which pushes older rock away by sea floor spreading
How do the ages of sea floor rocks prove continental drift?
The oldest rocks in the ocean are only 200 million years old. The magma that erupts at a divergent plate boundary creates new rock that is destroyed after continuous formations as it reaches subduction at ocean trenches/convergent plate boundary. These rock movements on the ocean floor can explain continental drift.
What are the processes on a divergent plate boundary?
The two lithospheric plates move apart by convection currents which form in the asthenosphere, driven by heat from radioactive decay in the core. Two plates move apart forming new land.
What are transform faults?
Where the mid-ocean ridges are displaced, fault lines are created which transmit earthquakes as seismic waves travel along it as the blocks split.