Tectonic Plates Flashcards
what is the core of the earth
a ball of solid (inner layer) and liquid (outer layer) iron and nickel
what surrounds or is around the core of the earth and what is it
- the mantle is the next layer from the core
- it is semi-molten rock that moves very slowly
what is the most outer layer of the earth
the crust
what is the crust divided into
- several slabs of tectonic plates
- which float on the mantle
what are the two types of crust that plates are made up of
oceanic and continental
what are the differences between oceanic and continental crust in terms of thickness
- continental crust if 30 to 50 km thick
- oceanic crust is 5 to 10 km thick
- so continental crust is thicker
what are the differences between oceanic and continental crust in terms of density
- oceanic crust is denser than continental crust
- due to being more compressed and compact
why do tectonic plates move
because of the convection currents in the mantle beneath the crust
what are plate margins and what is the other name for them
- plate margins are where tow or more tectonic plates meet
- they are also called plate boundaries
what are the three types of plate margins
- destructive margins
- constructive margins
- conservative margins
what are destructive margins and what is a real world example of them
- they are margins where two plates are moving towards each other
- an example is the margin along the west coast of south america
how are destructive margins formed
- when an oceanic plate meets a continental plate
- the denser oceanic plate is forced down into the mantle and destroyed
what do destructive margins form
- volcanoes and ocean trenches
- ocean trenches are very deep sections of the ocean floor where the oceanic plate goes down
- mountain ranges are also formed when the plates collide and the ground is folded and forced upwards
what are constructive margins and what is an example of them
- they are margins where two plates are moving away from each other
- an example is the margin at the mid-altantic ridge
what do constructive margins form and how
- the magma rises from the mantle to fill the gap and cools
- creating new crust