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Faulting
Slow due to friction, stressed rocks along the fault, rocks rupture and are displaced when stress exceeds the strength of the rocks
Stress
Force that results from plate tectonic movements : tensional, compressional and shearing forces
Strain
Change in shape or location of the rocks due to stress
Normal dip slip fault
Hanging wall moves relative to the footwall
Reverse dip slip
Hangning wall moves up relative to footwall
Low angle thrust fault
hanging wall moves up relative to footwall
Same movement as a reverse fault just at a shallower angle
Strike slip
Crust either side of fault moves horizontally (laterally) in opposing directions
Body waves
Primary and secondary waves.
Travel through the interior of the earth
Arrive before surface waves
Have a higher frequency (shorter wavelength) than surface waves
Surface waves
Travel only through the crust of the earth
Lower frequency than body waves
Easily distinguishable on seismographs
Almost entirely responsible for damage caused in earthquake
Damage reduced in earthquakes with a deeper focus
Richter scale
Recorded with a seismograph
First estimates of magnitude
Moment magnitude scale
Absolute size of earthquake
Measurement of actual energy released
Focus
Place within the earth where the earthquake starts (point of fault rupture)
Deeper earthquakes mean less dangerous earthquake.
Loss of energy is reffered to as attenuation.
Epicentre
Place on the earths surface directily above the focus, where shaking is most violent.
Liquefaction
Occurs on the surface when water saturated sand rapidly changes from a solid to a,liquid
Can cause buildings to float
Common in mag 5.5 earthquakes occurring in younger sediments
Landslides
Most common secondary effects during an earthquake
Can cause significant loss of human life
Fires
Earthquakes can cause pipe rupture and sparks leading to large scale fires
Retrofitting
Adapting current structures with new materials that can make them resistant to the shaking during an earthquake