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A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
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A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
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A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology

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A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology
Journal Article

A note on contrasting morphodynamics of two beach systems with different backshores, Tetouan coast, northwest Morocco: the role of grain size and human-altered dune morphology

2013
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Overview
The Mediterranean coast of Tetouan, in Morroco, comprises headland-bound beach-dune systems bordering small coastal plains that have been considerably altered by socio-economic activities and coastal infrastructure essentially related to tourism development. To analyze the response of the beach-dune systems to high-energy winds and storms, three successive surveys covering storm and fair-weather conditions were conducted in February and March 2008 in two sites with contrasting grain-size and morphological characteristics. Ksar Rimal beach is characterized by coarse to very coarse sand and the finer-grained dunes on the backshore have been largely flattened, while Cabo Negro beach exhibits fine sand but the aeolian dunes associated with this beach are still partly intact. The results show that morphological changes are larger and faster on Ksar Rima beach than on Cabo Negro beach. The former beach has a greater tendency to erosion during storms but also shows rapid recovery expressed essentially through berm cut and fill.