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
2
Q
what is the Mohorovičić discontinuity (Moho)
A
the boundary between the crust and the mantle
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
4
Q
structure of the Earth - outer core
A
- semi-molten
- mostly liquid iron and nickel
- 4500-6000 degrees C
5
Q
structure of the Earth - inner core
A
- solid centre
- mostly iron
- 6000 degrees C
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
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)
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
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
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)
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)