1.2 theory of plate tectonics Flashcards

1
Q

structure of the Earth - crust

A
  • continental is thicker and less dense (45-50km)
  • oceanic is thinner and more dense (6-10km)
  • seven major plates and some minor ones
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2
Q

what is the Mohorovičić discontinuity (Moho)

A

the boundary between the crust and the mantle

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3
Q

structure of the Earth - mantle

A
  • widest layer
  • lithosphere is upper mantle and crust
  • asthenosphere is a semi-molten layer which moves under high pressure
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4
Q

structure of the Earth - outer core

A
  • semi-molten
  • mostly liquid iron and nickel
  • 4500-6000 degrees C
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5
Q

structure of the Earth - inner core

A
  • solid centre
  • mostly iron
  • 6000 degrees C
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6
Q

what are convection currents

A
  • magma at the bottom of the mantle is heated by the core, giving it energy and causing it to rise
  • cooler rock sinks due to lower energy levels
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7
Q

what is the theory of convection currents to explain plate movements

A
  • heat from radioactive decay in the core moves up towards the crust
  • magma under the crust moves sideways at the Moho
  • this pulls the plates apart due to friction (divergent boundary)
  • magma cools and sinks pulling the crust downwards (convergent boundary)
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8
Q

what is the theory of sea floor spreading and slab pull to explain plate movements

A
  • the ocean floor is getting progressivley older and newer crust must be produced by molten rock rising from the core
  • as molten rock comes to the surface the crust is pushed outwards (ridge push)
  • oceanic crust is destroyed by subduction
  • in the subduction zone the oceanic crust is heaviest and pulled down by gravity under the continental crust
  • pushing at ridges (divergent boundaries) and pulling at convergent boundaries results in ocean floor spreading
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9
Q

how does paleomagnetism evidence the movement of tectonic plates

A
  • the earths magnetic field switches north and south every few million years
  • this means rock strata has alternating magnetization
  • the magnetic minerals in lava line up with the magnetic field and set when cooled
  • parallel strips of crust in opposite directions prove the floor has spread
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10
Q

what are volcanoes like at divergent boundaries and hotspots

A
  • shield volcanoes
  • mild and effusive
  • basaltic lava (low gas content, low viscosity, higher temperature)
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11
Q

what are volcanoes like at convergent boundaries

A
  • composite / strato
  • high magnitude eruptions due to friction and pressure build up in Benioff zone
  • explosive as magma is forcing its way to the surface
  • andesitic or rhyolitic lava (high gas content, high viscosity, lower temperature)
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