MORPHODYNAMICS AND SEDIMENTARY EVOLUTION OF ROCKY PLATFORMS IN FRONT OF THE CLIFFS OF ESTREMADURA (PORTUGAL) - (OBSERVATIONS OF MOBILE SUBMARINE SANDS)
H. Regnauld et al., MORPHODYNAMICS AND SEDIMENTARY EVOLUTION OF ROCKY PLATFORMS IN FRONT OF THE CLIFFS OF ESTREMADURA (PORTUGAL) - (OBSERVATIONS OF MOBILE SUBMARINE SANDS), Zeitschrift fur Geomorphologie, 39(3), 1995, pp. 313-330
Morphodynamics and sedimentary evolution of rocky platforms in front o
f the cliffs of Estremadura (Portugal) (observations of mobile sumbari
ne sands). - The rocky platform at the base of cliffs in Estremadura (
Portugal) is an area of active sediment transport. Sands are moved sho
reward along structural depressions (submarine channels) in the platfo
rm. Terrigenous products also arrive there from cliffs and slopes, esp
ecially where they are exposed to waves. These transits have links wit
h plant and algual covers. A cross section from the top of the slope,
to the rocka platform (through beach, submarine beach and submarine ch
annel in the platform) is presented. Grain size analysis and morphosco
py give a clue for the understanting of dynamics. A theoretical approa
ch is then conducted, using mainly sand deposition models developed by
Electricite De France. The sedimentary dynamics are mainly dependent
on the tidal sea level fluctuation.