1985 Mexico city: Severe EQ due to these conditions (high MG, saturated, alluvium geology and close to epicentre)
Dilatancy might act as a response to lower the severity
Ground shaking: impact
Stability of buildings is affected more by swaying (horizontal) than vertical movements
Mitigations: protection through reinforced structures (Pendulum power), flexible foundations and shock absorbers at base
But ground displacement destroys infrastructure (roads, railways and pipelines) as well as streams/rivers causing problems in water supply and services (transport)
Liquefaction: The process by which soil becomes loose and flows like a liquid.
Liquefaction: Saturated, alluvium and fine-grained sand behave like liquids seismic vibrations. This causes the surface to lose strength: buildings and roads collapse and sink (Sulawesi Indonesia, 2018 EQ)
Depends on geology
Landslides/avalanches:
Steep slopes. deforested areas, monsoon rain increases vulnerability and risk
They bock transport routes, rivers and cause temporary dams which burst and flood downstream (2005, Kashmir)
They can overwhelm reservoirs upland as displaced water overtops/breaks through (1963 Vajont/Vaiont reservoir, Italy produced a 100m wave that inundated Piave river valley drowning 3000)
Tsunami: Waves of up to 200km wavelength, speeds of up to800km/hr caused by sudden displacement of water
Tsunamis are caused by submarine earthquakes but can also be caused by landslides, explosions and meteorites. As plates rebound after friction a column of water spits into ripple of waves; they gain height in shallow water and break after a drawdown of water occurs.
Impacts of tsunamis
Damage to property, possession and infrastructure, death and tragedy, disease, demand for necessities and psychological loss. e.g. case study of 2011 Tohoku, japan