Coastal erosion in sandy beaches along a tectonically active coast: The Chile study case

Coastal erosion in 45 sandy beaches covering nearly 2000 km along the tectonically active Chilean coast is assessed during the last four decades. The historical analysis is based on the assessment of decadal changes of the shoreline position extracted from topographic surveys, aerial photographs, satellite images and survey maps using the DSAS software. Results show that 80% of the sites presented erosion rates (>-0.2 m/y), 7% beaches accreted (>0.2 m/y) while 13% remained stable. Eroded beaches include headland bay beaches, embayed and pocket beaches. A discussion on the possible causes explaining these results is conducted. While changes in offshore wave climate are spatially smooth within the region, relative mean sea level changes are highly variable and modulated by tectonic activity; the reduction of the sediment supply explains erosion rates in few cases.

Automated summary

The study assessed coastal erosion in 45 sandy beaches along the tectonically active Chilean coast, covering nearly 2000 km, over the last four decades. The results show that 80% of the sites experienced erosion, 7% saw accretion, and 13% remained stable. Eroded beaches include headland bay beaches, embayed, and pocket beaches, with sediment supply reduction being a possible cause.