Cuspate forelands, also known as cuspate barriers or nesses in Britain, are geographical features found on coastlines and lakeshores that are created primarily by longshore drift. Formed by accretion and progradation of sand and shingle, they extend outwards from the shoreline in a triangular shape.
Las tierras bajas de Cuspate, también conocidas como barreras o nesses de cuspates en Gran Bretaña, son características geográficas que se encuentran en las costas y orillas de los lagos que se crean principalmente por la deriva de la costa.
