This study was carried out in Odiel Saltmarshes (Huelva, SWSpain). Erosion and accretion in slopes and intertidal mud flats were measured. Our results point out a general retrogression of slopes. Its intensity would depend on anthropic actions as boats traffic and alteration of estuary circulation by dykes construction. In the Integral Reserve of Enmedio Island, horizontal losses by erosion in slopes reached 3000 m2/year, which would imply the mobilization of 1850 m3 of sediments. This strong erosion could cause important changes in this protected area and to selt-up of the navigable channels of the estuary. Vegetation, as prairie of eelgrass Zostera noltii, decreased erosion and increased acretion rates. Sediment vertical dynamic in intertidal mud flats showed a seasonal pattern with a direct relation between erosion and rainfall distribution. Erosion control and rehabilitation in eroded areas are discussed.
