the shaking of the ground caused by sudden motions along faults or fractures in the earths crust
define a hypocentre / focus
point of origin of an earthquake inside an earths crust
the focus point within the ground where the strain energy of the earthquake stored in the rock is released
define focal length
the distance between the hypocentre and the epicentre on the surface
define epicentre
the point on the Earth's surface directly above the focus/hypocenter of an earthquake
what is the 1st in the sequence of the generation of an earthquake
1. a gradual build up of tectonic strain
what is the 2nd in the sequence of the generation of an earthquake
2. the rock fractures when pressure exceeds the strength of the fault
what is the 3rd in the sequence of the generation of an earthquake
this results in a sudden release of energy creating seismic waves that radiate away from the point of the fracture
what is the 4th in the sequence of the generation of an earthquake
rebounding of the brittle crust on either side of the fracture causes the ground to shake which is felt on the surface
characteristics of a shallow focus earthquake
most damaging (often)
less than 40km deep
why are shallow focus earthquakes the most damaging (often)
seismic waves have less distance to travel to the surface and therefore loose less energy whilst travelling to the surface
why are shallow focus earthquakes not always most damaging
depends on other factors eg, how built up is the area
what are the 3 types of seismic waves
P waves and S waves and L waves
what are P waves
Primary waves, the seismic waves which are the first to arrive at the crust
have a short wave length
moves through rock and fluids
caused by compression - the 'shunting' effect
not the most damaging
faster than s waves, 8km/s
what are S waves
secondary waves, the seismic waves which are last to arrive at the crust
only moves through solid rock
longer wave length
vibrate at right angles to the direction of travel
causes more destruction
slower than p waves, 4km/s
what are L waves
love waves
only travel through the surface and move side to side
most destructive
slowest of the seismic waves
what two characteristics are used to measure earthquakes
magnitude
intensity
what is prediction of earthquakes
what is forecasting of earthquakes
what is magnitude
a measure of the amount of energy at the epicentre
- qualitative
how is magnitude used to measure earthquakes
moment magnitude scale is the most commonly used to measure the ammount of energy released at the epicentre, it is accurate especially for larger earthquakes
it measures the total energy released by the earthquake at the moment it occurs: called the siesmic moment
what does the moment magnitude scale use to measure magnitude
for example
-size of seismic waves
-ammount of rock movement/slippage
what is the range/scale of the MMS
1-10 but it is infinite, aka it can be extended if an earthquake needs
it uses a logarithmic scale
what is a logarithmic scale
each increase on a scale is an increased magnitude of x10
what is intensity
the ammount of ground shaking and damage caused by an earthquake
- more subjective
what is the relation ship between magnitude and frequency
inversely proportional
what is a seismometer
a device which measures the amount of ground shaking
it records both the vertical and horizontal movements of the ground
what does a seismometer produce
a seismogram
(essentially a peice of paper that shows the data)
what is an earthquake swam
a sequence of seismic events occurring in a local area within a relatively short period
aka:
foreshock, earthquake, aftershock
what does the modified mercalli scale measure
intensity
subjective (what you can feel and see eg how scared people are, how much destruction there is)
what is the modified mercalli scale marked in
by roman numerals I - XII
the higher numbers are usually based on observed damage and lower numbers are based on what people feel