In this study, we have carried out an analysis of the liquefaction pot
ential in a zone where there exists a variety of (geologic, paleoseism
ologic and historical) data which confirm the occurrence of past lique
faction. The obtained data have been mapped according to susceptibilit
y and liquefaction potential. The susceptibility map is based on geote
chnical data and a moderate to high susceptibility has been determinat
ed for the flood plain of the river and surrounding areas. In order to
estimate potential variability, we have worked with various sets of s
eismic sources and with a variation of the average SPT value which cha
racterizes each zone. The results indicate that the analysis of potent
ial is very sensitive to any variation in the variables that are invol
ved in its calculation. (C) 1998 Elsevier Science B.V.