“…Occurrences of these characteristically low-gradient landforms have been widely mapped in the central Pyrenees, e.g., in the Noguera Pallaresa, Ariège, and Salat watersheds, and even more conspicuously in the Agly and Tech watersheds and around the edges of the eastern Neogene basins such as the Roussillon, Cerdagne, and Empordà. These pediments are particularly extensive among granitic outcrops but also in schist (Goron, 1931(Goron, , 1937(Goron, , 1941aZandvliet, 1960;Hartevelt, 1970;Lagasquie, 1969Lagasquie, , 1984aLagasquie, , b, 1987Calvet, 1996;Delmas et al, 2018). Around the edges of the Cerdagne Basin, a good example of P2 is the Plateau de la Perche (Fig.…”