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The amplitude of seismic waves is dependant on the medium through which they travel. Seismic waves in hard rock masses (e.g. granite) have lower amplitudes than those that travel through soft ground such as sediments and so a building constructed on granite is less likely to be damaged.

Soils can undergo a process known as liquefaction during earthquakes which can greatly reduce their ability to support imposed loads by building foundations. This can ultimately lead to structural damage or collapse.

This typically occurs in cohesionless soils (typically those with a higher content of larger grains such as sand sized clasts) which have water in the pore spaces, and are poorly drained.

For more information on liquefaction, please see the related question.

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