Seismicity Flashcards
What is sesimicity
Movements within the earths crust cause stress to build up at points of weakness and rocks to deform. When the stress finally exceeds the strength of the rock, it fractures. The stored energy is suddenly released as an earthquake. Seismic waves spread out.
What is the hypocentre
The focus. The more shallow the more damaging
What is the focal length
The distance between the epicentre and the focus
Primary waves
Arrive at the detector first. They are longitudinal waves which means vibrations are along the same direction as the direction of travel (forward movement)
Secondary waves
Arrive at the detector second. They are transverse waves which mean the vibrations are at right angles to the direction of travel (vertical movement)
Love/Long waves
Surface waves - do not travel through liquid
Faster than secondary waves
Travels horizontally (side to side)
What can influence the impact of seismic activity
- geological conditions
- distance from epicentre
- time of day
- depth of earthquake
- preparation and education
- population density
Liquefaction
Process by which water saturated sediment temporarily loses strength and acts like a liquid
Earthquake shaking increases water pressure in the soil, the spaces between soil particles become filled with water which causes soil to lose strength and flow like a liquid
Mercalli Scale
This measures how much damage is caused by the earthquake based on observations
It is measured on a scale bwtween I and XII
This is a measure of intensity and changes according to which area you are measuring - damage nearer the epicentre would usually be greater than further away
Moment magnitude scale
Based on the total moment release of the earthquake. It can be used for any kind of earthquake, near or far.
Magnitudes are based on a logarithmic scale (base 10). What this means is that for each whole number you go up on the magnitude scale, the amplitude of the ground motion recorded by a seismograph goes up ten times
Can describe earthquakes so small it has negative numbers and the scale has no upper limit
Richter Scale
A logarithmic scale used to measure the magnitude of an earthquake
Goes from 1-10
How does a tsunami work
1 - a plate shifts abruptly causing an earthquake and displaces water
2 - waves are generated and move out in all directions across the ocean, some travelling as fast as 600mph
3 - as waves enter shallower water they compress, their speed slows and they build in height
4 - the wave height increases and associated currents intensify, becoming a threat to life and property
Indications that an earthquake will occur
- micro quakes
- bulging of the ground
- raised groundwater levels
- curious animal behaviour
- electrical and magnetic changes within local rocks
Prediction, Planning and Prevention
Prediction - impossible, understanding of plate tectonics help, micro quakes before main tremor, only vague predictions can be made
Preparedness - earthquake warning systems, evacuation, adaptation
Prevention - not possible, mitigation and adaptation methods
Contingency Planning
Individuals, organisations, local authorities, governments and internation aid agencies prepare for hazards in advance which aids management. eg special building designs, evacuation plans, practice drills, stock food and water, medical supplies