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                <term xml:lang="en">mud banks</term>
                <term xml:lang="en">beach plan shape</term>
                <term xml:lang="en">cell circulation</term>
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              <p>Montjoly is a headland-bound embayed sandy beach in Cayenne, French Guiana, that shows long-term plan shapeequilibrium in spite of periodic changes in accretion and erosion that alternately affect either end of the beach. Thesechanges are caused by mud banks that move alongshore from the Amazon. The mechanisms involved in changes in theplan shape of the beach in response to the passage of one of these mud banks were monitored between 1997 and 2000from airborne video imagery and field work. The beach longshore drift to the northwest, driven by the incident easterlyto northeasterly swell usually affecting this coast, became temporarily reversed as the mud bank, migrating from east towest, initially sheltered the southeastern end of the beach. The difference in exposure to waves engendered a negativewave height gradient alongshore towards the southeast, resulting in the setting up of a cell circulation and counter-activelongshore drift from the exposed northwestern sector to the southeast. Sand eroded from the exposed sector accumulatedfirst in the southeastern, and then the central sectors of the beach. The effect of increasing beach sheltering by themudbank moving west is highlighted on the videographs by an ‘arrested’ pattern of beach shoreline development. Thevideographs show hardly any changes in beach plan shape since January 1999, due to sheltering of the beach from waveattack by the mud bank. It is expected that the eroded sector will recover in the future as the mud bank passes, leadingto re-establishment of the northwesterly sand drift. This temporally phased bi-directional drift within the confines of thebounding headlands results in a rare example of mud-bank-induced beach rotation, and probably explains the long-termequilibrium plan shape of Montjoly beach. Copyright  2002 John Wiley &amp;amp; Sons, Ltd</p>
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