Apr. 5, 2013 — In February 2010, a violent earthquake struck Chile, causing a tsunami 10 m in height. Affecting millions of people, the earthquake and giant wave also transformed the appearance of the coastline: the dunes and sandbars were flattened, and the coast subsided in places by up to 1 m. But although the inhabitants are still affected for the long term, the shore system quickly rebuilt itself. A team from IRD and its Chilean partners(1) showed that in less than a year, the sedimentary structures had reformed. The Chilean coast therefore represented a unique ”natural laboratory” for studying coastal formation processes. The subsidence of the coast also revealed the effects of rising sea levels on shores.