The Coastal Cliff of northern Chile (Spanish: Acantilado Costero) stretches over a length of more than 1000 km along the Atacama Desert. It makes up a large part the western boundary to the Chilean Coast Range in the regions of Tarapacá and Antofagasta, and Atacama. According to Roland Paskoff the modern cliff origined from a scarp retreat of a fault scarp, thus at present the cliff does not follow any fault.