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From a geomorphological perspective, the shelf in ideal cases is the part of the seabed adjacent to the continent, which forms a large submerged terrace that dips gently seaward.
6.2.2 Desde el punto de vista geomorfológico, la plataforma es típicamente la parte del lecho marino adyacente al continente que forma una gran terraza sumergida que desciende suavemente mar adentro.
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