Earthquakes 3 Flashcards
Elastic Rebound Theory
«_space;refer to slides for diagram»_space;
- pate tectonic forces stress rocks -> deform
- Elastic deformation of lithosphere
- Brittle failure / deformation so litho eventually breaks
- stored elastic energy is released and deformed rocks go back to original state
(energy stored on either side of failure)
What theory describes how earthquakes occur?
elastic rebound theory
-> we feel the waves/vibration produced by elastic rebound
Describe the processes of plates at the boundary
- Plates lock = stress & deformation
- Plates release = earthquake & tsunami
does a rupture propagate far?
only along a portion of the fault
-> some areas are still locked
Describe how earthquakes occur in terms of the brittle and elastically deformed crust
- brittle crust ruptures at hypocentre
- elastically deformed crust rebounds and vibrates
- waves + energy propagate away in all directions
where is the epicentre in relation to the hypocentre?
directly above it
Which type of seismic wave hurt us?
surface waves
what are the two types of body waves?
- Pressure or primary
- Shear or secondary
P - waves
- fastest
- particle motion parallel to propagation (like slingy)
- can move through solids or fluids
S - waves
- slower than p waves
- particle motion is perpendicular to propagation (like waves)
- can ONLY move through solids
Can S waves move through fluids?
no
Can P waves move through fluids?
yes
Surface waves
- the damaging waves
- require a surface, cannot travel thru water (?)
- slower than body waves
What are the types of surface waves?
- Rayleigh wave
- Love wave
Rayleigh wave
- vertical and horizontal motion parallel to wave direction
- like an ocean wave