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Tsunami hazard assessment in the coastal area of Rabat and Sal´e, Morocco

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Figure

Fig. 1. Present-day tectonic sketch of the Nubia-Eurasia boundary. Deformation rates are in mm year−1 (from Serpelloni et al., 2007).
Table 2. Source parameters (from Fukao, 1973), L: the fault length in kilometers; W: the fault width in kilometers; D: the depth from the seabottom to the top of the fault in kilometers; µ: the shear modulus and Mw: the moment magnitude.
Fig. 4. Initial displacement (localisation and initial wave height) of (a): the 1755 Lisbon Earthquake (from Baptista et al., 2003) and (b): the1969 earthquake (from Fukao, 1973).
Fig. 6. Maximum water elevation – Lisbon augmented scenario ((a) large scale; (b) regional scale).
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