Laboratorio de Oceanografia Geologica, Fundacao Universidade Federal do Rio Grande (Av. Italia, km 8, Campus Carreiros, 96201-900 Rio Grande, RS, Brasil) lcalliari@log.furg.br The sediment distribution along modern beaches is the result of the complex interaction between the sediment source, the wave energy level and the general offshore slope upon which the beach is constructed (KOMAR, 1998). Sediments tend to be sorted according to the energy levels that the beach is exposed, so that beaches exposed to higher wave energy levels are expected to be composed by coarser sediments. In the composition of beach sediments, quantities of heavy minerals might be present. Since they are denser than quartz grains, they present a different hydraulic behaviour when compared to lighter grains. The behaviour of heavy minerals has been studied mainly related to erosional and/or accretional beach processes (e.g. SLINGERLAND, 1977; KOMAR et al., 1989; KOMAR, 1998). The straight wave-dominated southernmost coastline of Brazil is characterised by an extensive sandy coastal plain. The study area comprehends 220 km of sandy beaches located between the Patos Lagoon inlet and the Uruguayan border (Fig. 1). Beaches in this region are classified as dissipative and intermediate, associated to one or two longshore sandbars (CALLIARI; KLEIN, 1993). Seasonal variations are present, with accretion profiles during spring and summer and erosion profiles during autumn and winter. The climate of this coastal region is under the control of the high-pressure centre of the Atlantic anticyclone, whose latitudinal migration and the passage of polar front systems in 6-10 days intervals have a seasonally modifying influence on the climate. During cold fronts events, more common during winter months, SW winds become stronger (8 m.s
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