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Fig. 3 | Geoenvironmental Disasters

Fig. 3

From: New sedimentary and geomorphic evidence of tsunami flooding related to an older events along the Tangier-Asilah coastal plain, Morocco

Fig. 3

From the top of distal dune, facing N 333 we see in a general view to the Atlantic, notice the lack of vegetation on the proximal and intermediate dune; b Eroded landscape and unaffected soil; c opposite view to the maximum run-up limit; d Section in the proximal dune: on the lower part, the sand with the roots of a truncated paleosoil, on the upper part a pavement of residual carbonates concretions, notice the strong unconformity; e sand accumulation on basement of proximal dune, the brown organic matter removed from the upper dune; f Surface accumulation of highly marine unsorted materials on interdune gaps, including pottery, microliths, and marine fauna; g Section in a basal accumulation with brown sand, marine shell, microlithic industry, beach rocks

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