We propose to apply in this note a simple mathematical model for the sedime
ntation of gravity deposits in deep water. An inverse method has been devel
oped in order to characterize the parameters associated with the submarine
flow. This method also provides the initial conditions, which constitute a
major uncertainty in geoscience modelling. Application of the inverse metho
d to the 1979 Nice air-port collapse (southern France), constrained by cabl
e breaks and/or deposit thicknesses, leads, for example, to the estimation
of the initial volume and/or the physical parameters of the flow (friction
coefficient, modified turbulent Schmidt number, etc.). The application of t
he model to this real case shows that only the simultaneous inversion of dy
namic (cable break times) and sedimentological (deposit) data allows a sati
sfactory reconstruction of the flow. (C) 2001 Academie des sciences/Edition
s scientifiques et medicales Elsevier SAS.