Marine scientists have discovered an exceptionally well-preserved terrestrial landscape submerged in the coastal waters of the Maltese Islands, which reveals how the archipelago would have looked like 20,000 years ago.
At this time, Europe was experiencing the last ice age and sea level in the Mediterranean Sea was 130 metres lower than at present.
Malta, Gozo and Comino were connected and the archipelago was two and a half times larger than it is today.
Dingli Cliffs towered 380m above sea level whilst Valletta was located 10km inshore.
The coastline from Marsalforn to Pembroke consisted of steep coastal cliffs that were incised by more than 20 valleys.
Numerous limestone plateaus hosted collapsed caves and featured landslides along their margins.
A 40 km wide land bridge connected southeast Malta all the way to the south of Sicily.
Sea level rise during the last 20,000 years has sunk 450 km2 of this landscape, meaning that the largest part of the Maltese Islands is today under water.
By surveying the seafloor around the Maltese Islands with state-of-the-art mapping technology, an international team of geologists has reconstructed the majority of this submerged landscape in great...
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