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(a)
(b)
Fig. 4 a) Isoseismals of 1755 in the current district of Lisbon over the geological map, according
to Pereira de Sousa (1929); b) Chart of intensity (Mercally Modified), done from a possible similar
scenery to 1755 (scenery of Gorringe) (Mendes-Victor et al. 1994)
in the work of 1994, are still away from reproducing satisfactorily the damages
observed. For example, the population of Belem and Pedrou¸os, western areas of
Lisbon, reported just a small shaking, being later amazed when confronted with
what had happened in Lisbon.
Zone destroyed by fire
Hills
MMI = X
Fig. 5 Detail of the damages in the downtown Lisbon due to the vibration and fire (according to
Fran¸a, 1978)
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