Plate Boundaries Flashcards
What is the oceanic crust?
- The plate that is made up of more dense rock.
- It sinks easily due to its density and is constantly created at boundaries
- It is ‘young/new rock’ and forms our ocean bed
What is the subduction zone?
Where one plate is forced downwards below another plate and grinds past it causing huge amounts of friction and heat
What is a convergent (destructive) plate boundary?
Where two plates are moving towards each other, one of which is continental crust and one is made of oceanic crust
What is the continental crust?
- A plate that is made up of less dense rock which means it doesn’t sink
- It is very old and makes up our land surfaces
What is a plate boundary?
Where two very large crustal plates meet on the earth’s surface
What are fold mountains?
Large mountain ranges formed by the collision and ‘folding’ of two plates as they continually push into each other
What is an ocean trench?
A particularly deep point of the ocean bed where the oceanic and continental crust have dragged each other downwards
What the differences between the continental and oceanic crust?
- Continental is 70km thick, oceanic is 7km
- Oceanic is 200 million years old, continental is 3.6 billion years
- Oceanic is made of denser basalt, continental is made of granite
What is an example of a convergent plate boundary?
Nazca and South American plates
- Convergent plate boundary
Denser Oceanic plate (Nazca) is forced below the continental plate
- Convergent plate boundary
Less dense Continental plate (South American plate) moves towards Oceanic plate
- Convergent plate boundary
Pressure builds up at the subduction zone - friction causes melting of oceanic plate and can cause earthquakes when friction is released
- Convergent plate boundary
Molten rock (magma) builds up in the chamber
- Convergent plate boundary
When the pressure builds up magma escapes through a composite volcano
- Convergent plate boundary
Lighter continental crust remains at the surface but crumples into fold mountains (Andes)