Beach ridges are landforms commonly developed on prograded coasts with beach
shorelines. A sequence of beach ridges, coupled with their subsurface deposits, can be …

Extreme storm events in the coastal zone are one of the main forcing agents of short-term
coastal system behavior. As such, storms represent a major threat to human activities …

This paper presents the geological and morphological evolution of the prograded Cassino
barrier during the middle and late Holocene. A special focus is given on the presentation …

Relict beach ridges of aeolian origin and associated soils are often used for inferring relative
sea level and climate with contrasting results. Most studies link the aeolian coastal deposits …

Clastic, depositional strandplain systems have the potential to record changes in the primary
drivers of coastal evolution: climate, sea‐level, and the frequency of major meteorological …

The criteria for zoning the surface fault rupture hazard (SFRH) along thrust faults are defined
by analysing the characteristics of the areas of coseismic surface faulting in thrust …

Beach ridges originate from various depositional processes and occur in a variety of
settings. This paper assesses their nature and distribution on the islands of the Greater …

Storm surges generated by tropical cyclones have been considered a primary process for
building coarse‐sand beach ridges along the north‐eastern Queensland coast, Australia …

On 8 November 2013, category 5 Supertyphoon Haiyan made landfall on the Philippines.
During a post-typhoon survey in February 2014, Haiyan-related sand deposition and …

Prograded barriers are distinctive coastal landforms preserving the position of past
shorelines as low relief, shore-parallel ridges composed of beach sediments and commonly …