plate tectonics Flashcards
crust
- outer layer
- thick
- 5-50 km thick
mantle
- 2900km thick
- upper sections solid and part of lithosphere
- asthenosphere > movement in the asthenosphere causes plates to move
- lower mantle = solid due to density
outer core
- provided heat
- solid, iron, nickel
- 2400km thick
inner core
- solid, iron, nickel
- very hot, 2400km thick
features of continental crust
- 35 to 70 km thick
- very old, 1500 million yrs
- light, less dense
- light in colour, granite
features of oceanic crust
- 6 to 10km thick
- young, less than 200 million yrs
- heavier, more dense
- dark, crystals are very small, basalt
types of boundaries
- convergent = can be two oceans or two continental plates as well as one oceanic and one continental
- divergent
- transform
divergent plate boundary - names
North American and eurasian plates
features of divergent boundary
- mid ocean ridge
- shield volcanoes (lave, basic runny)
- transform faults
- rift valleys
- earthquakes
convergent boundary - names
Nazca and South American plates
features of convergent boundary
- earthquakes
- fold mountains
- acid lava cones
- deep ocean trenches
transform boundary - names
pacific and North American plates
- san Andreas fault
features of transform boundary
- earthquakes
- transform faults
epicentre
the point on the ground surface directly above the focus.
This is where most of the damage happens
focus
- the point in the crust where the movement actually takes place
- the most damaging quakes are those where the focus is shallow i.e. near the surface
p - waves
- Arrive first, spread outwards on all sides from the focus of the quake
- they compress and stretch the material they move through
- travel quickly, hear them as a boom
s - waves
- Come later and shift the materials up and down causing major damage
- only travel through solids but can cause liquefaction of the soil
- liquefaction can cause major landslides
surface waves
- Travel along the Earth’s surface, arrived last
- can be most destructive
- travels slow
fault strike
- Fracture in the rocks of earth’s crust in which rock masses slip past one another parallel to the strike
- due to the movement of two plates against one another and the release of built up strain
fault plane
- the line of opening that takes place from the focal point, along which the crustal rock may slide
Richter scale
- quantifies the strength of the earthquake (the amount of energy released). it uses a logarithmic scale
moment magnitude scale
- more accurate
- gives an estimate of the total energy released by an earthquake
mercalli scale
- measures the intensity of an earthquake
- bases its measurements on the observed effects of the earthquake and describes its intensity
faulting
- where part of the crustal rock layers crack and break, opening and moving in different directions
- Direction of movement depends on the type of pressure under which the rocks are placed