Seismic events Flashcards
Outline how earthquakes are formed?
At all plate boundaries, plates move due to gravitational sliding, slab pull and convection currents. Plates get stuck due to friction and tension and pressure builds up. When plates suddenly jerk past each other or crack forming fault lines, this releases the pressure sending shockwaves through the earth’s crust as earthquakes.
How are seismic events distributed?
Found along plate boundaries
Particularly: destructive and conservative plate boundaries.
The Ring of Fire accounts for 90% of the world’s Earthquakes.
The Alpine-Himalayan belt accounts for 5-6% of the world’s earthquakes.
How does the depth of focus affect nature and magnitude of earthquakes?
Deep focus earthquakes tend to be higher magnitude than shallow focus earthquakes. Deep focus earthquakes generally do less damage than shallow focus earthquakes as shock waves have to travel further to reach the surface reducing their power.
Why are earthquakes higher magnitude at destructive plate boundaries?
High pressure builds up between plates as subduction.
Why are earthquakes lower magnitude at constructive plate boundaries?
Fracturing (as plates move apart), injection of magma and eruption is frequent. So, tensional stresses do not have time to accumulate.
What are the three factors affecting the magnitude of earthquakes?
Type of plate boundary
Depth of focus
Rate of movement
Give three reasons why earthquakes may occur away from plate boundaries?
Reactivation of old fault lines - potentially due to deferred stress release OR…Large dams and reservoirs - pressure on underlying rocks reactivates old faults
Hydraulic fracturing
Subsidence of old deep mines
What is a body wave?
Travel through the earth can be divided into primary (p) waves or secondary (s) waves.
What is a surface wave?
Travel along the Earth’s surface, these cause the most damage, as cause more ground movement and travel more slowly so take longer to pass
What is a primary wave?
alternately compress and expand, so particle motion is parallel to direction of wave movement. Can travel through ALL substances, fastest.
what is a secondary wave?
transverse, movement of particles is perpendicular (90 degrees) from movement of wave (up and down). Cannot travel through air or water, slower but cause more damage (greater amplitude).
What is a Rayleigh wave?
transverse, movement of particles is perpendicular (90 degrees) from movement of wave (up and down). Cannot travel through air or water, slower but cause more damage (greater amplitude).
What are loves waves?
horizontal shear waves, move the ground from side to side at right angles to the direction of the movement. This can damage infrastructure and buildings.
What does the Richter scale measure?
Logarithmic scale measures the magnitude of an earthquake based on the amplitude of secondary waves.
What does the Moment Magnitude Scale measure?
Logarithmic scale measures earthquake magnitude based on the total amount of energy released. Distance a fault has moved x force required to move it.
What does the Mercalli scale measure?
Intensity of an event and its impact - 12 point scale, subjective.
What is the epicentre of an earthquake?
Point on the earth’s surface directly above the focus - where the earthquake is first felt.
What is the focus of an earthquake?
Point in the earth’s crust where the earthquake starts.
What is the relationship between magnitude and frequency of seismic events?
Negative relationship - as magnitude increases frequency decreases.
What are the two primary impacts of seismic events?
Ground rupture (displacement of the earth’s surface along fault lines). Ground shaking
Give three factors affecting the severity of ground shaking from seismic events.
Dependent on magnitude
Depth of focus
Distance from the epicentre
How do earthquakes result in tsunamis?
Earthquakes vertically move the seabed up by several meters. Displacing (moving) the water above. The greater the movement of the sea floor the greater the volume of water displaced and the bigger the wave produced - hence greater intensity at destructive plate boundaries as higher magnitude earthquakes.Large waves radiate outwards across the ocean away from the epicentre of the earthquake. In deep water no energy is lost to frictional drag with the seabed.When it reaches shallow water near the coast, as it approaches the shore, the water becomes shallower and the base is slowed down by friction, forcing the circular wave motion into an elliptical form, which heightens until it can no longer be maintained and breaks. This is called shoaling.A large wave hits the coast, a tsunami.