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Submarine Geomorphology and Sedimentary Features around the Egadi Islands (Western Mediterranean Sea)
1. Introduction During the last glacio-eustatic cycle, which lasted for about 125,000 years, continental shelves around the globe experienced a significant and quite sudden environmental change. This change was due to a global drop in sea level, which led to the exposure of large marine areas to sub-aerial conditions. At the Last Glacial Maximum (LGM), which occurred about 20,000 years ago [1,2], the palaeo-sea level reached about 120–130 m below the current level.
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