Plate Tectonics: Why are areas more prone to tectonic hazards? Flashcards
What is the internal structure of the earth?
Core, Mantle, Crust
What are the features of the earth’s core?
- 3300 km thick
- Mostly iron and nickel
- Mix of solid inner and liquid outer
- 4400-6600 degrees celsius
What are the features of the earth’s mantle?
- 2900 km thick
- Mostly rock
- Liquid inner and solid outer
- 1000-3700 degrees celsius
What are features of the earth’s crust?
- 6-70 km thick
- Mostly basalt and granite
- Solid that melts under high heat
- Similar temperature to environment it is found in
What are the differences between oceanic crust and continental crust?
Oceanic
Location: Beneath deep oceans
Thickness: 5-8 km
Type and age of rock: Basalt, <200 million y/o
Continental:
Location: Beneath continents and shallow seas
Thickness: 35-70 km
Type and age of rock: Granite >4 billion y/o
What are the processes that cause plate movement?
- Convection currents
- Slab pull force
Describe the process of convection currents in causing plate movement
- Core heats the mantle
- Mantle expands and rises, spreading outwards beneath the plates
- This drags plates along, causing plates to move
- The mantle cools and sinks, pulling plates along
- Mantle nears core and is heated again, causing the process to repeat itself
Describe the process of slab pull force in causing plate movement
- The dense, sinking oceanic plate at a subduction zone pulls the entire plate along due to its weight
- This sinking plate drives the downwards moving portion of the convection current
- Mantle that is away from the subduction zone drives the upwards moving portion of the convection current
What are the types of plate boundaries? Briefly state.
- Divergent
- Convergent
- Transform
What are the types of divergent plate boundaries?
- Oceanic-oceanic divergent
- Continental-continental divergent
What are the types of convergent plate boundaries?
- Continental-continental convergent
- Oceanic-oceanic convergent
- Oceanic-continental divergence
Describe the events that occur at an oceanic-oceanic divergent boundary and the associated landforms
- Diverge
- Fractures form
- Magma rises to fill the cracks
- Cools and solidifies
- Forms new seafloow-> extends seafloor (seafloor spreading where newly formed rocks are closest to the ridge)
- Forms a mid-oceanic ridge
- Some forms undersea volcanoes
- When the volcano builds up and becomes exposed above sea level, it forms volcanic islands
Describe the events that occur at an continental-continental divergent boundary and the associated landforms
- Diverge
- Fractures form
- Plates are stretched
- Land between the faults sink
- Rift valley is formed (linear depression with steep sides)
- Block mountains are formed (Blocks of land standing higher than surrounding land
- Active volcanoes and earthquake fractures may form along the rift valley as well.
Describe the events that occur at an oceanic-oceanic convergence boundary and the associated landforms
- Converge towards each other
- Denser oceanic plate sinks under the less dense plate
- Oceanic trench forms at the zone of subduction (may set off earthquakes due to friction)
- Sinking oceanic plate melts in the mantle to form magma
- Magma rises through the cracks and forms a volcano
Describe the events that occur at an oceanic-continental convergence boundary and the associated landforms
- Denser oceanic plate and less dense continental plate converge
- Denser oceanic plate subducts beneath continental plate
- Oceanic trench forms at zone of subduction
- Fold mountains form on less dense continental plate as it buckles and folds
- Melted mantle rises from the crust
- Forms volcanoes on the continental plate
- May set of earthquakes due to friction