“…In reality, however, seismic site response is influenced not only by the local (i.e., 1-D) site conditions but also by the three-dimensional (3-D) environment, such as bedrock slope, geometry of the soft soil layers, and topographical irregularities. One of the main pieces of empirical evidence of 3-D amplification effects comes both from the concentration of structural damage near topographic irregularities (such as a hill, a ridge, a canyon, a cliff, or a slope) as observed during past and recent earthquakes (e.g., Wyllie andBolt 1986, Çelebi 1987) and instrumental data (e.g., Davis and West 1973), clearly indicating that surficial morphology and topography can affect the propagation of seismic motion, which, in turn, can lead to significantly modified levels of ground shaking because of scattering, diffraction, or trapping of waves.…”