1. Nature and Distribution Flashcards
Focus depth
Friction along margins builds stresses in the lithosphere
Faults send a series of seismic shockwaves to the surface
Point where pressure is released is the focus and point immediately above that in earth’s surface is epicentre
Focuses
Shallow focus (0-70km deep)- tend to cause greatest damage and 75% of all earthquake energy released
Intermediate focus: (70-300km deep)
Deep focus (300-700km deep)- Tend to be higher magnitude but cause less damage as shockwaves have to travel further reducing power
Constructive margin
Tend to be close to the surface and narrowly concentrated
Lowest magnitude, potentially destructive due to shallow focus
Destructive
Subduction of plate causes massive pressure to build up
Creates deep and shallow focus earthquakes
Most powerful
Conservative
Narrow zone of shallow depth earthquakes which can be very destructive and high magnitude
Intra-plate
Occur away from plate boundaries and associated with reactivation of old fault lines
Human activities such as mining and fracking can cause minor earthquakes
Rate of plate movement
Tectonic plates move in relation to each other at different rates
1-15cm per year
No relationship between rate of movement and magnitude