Multiple research teams have compiled extensive evidence for the highly catastrophic nature of the Zanclean Megaflood. Observations of more than 300 asymmetric, streamlined erosional ridges on and around the Sicily Sill indicate that powerful flows of turbulent water sculpted the landscape. As one study notes, the morphology of these ridges is “compatible with erosion by large-scale, turbulent water flow with a predominantly north-easterly direction”^[6][14]. Geological sampling of these ridges revealed a layer of rocky debris on top that is interpreted as rapidly deposited material eroded from the ridge flanks and adjacent areas. This debris layer, which marks the boundary between the Messinian and Zanclean periods, is a key piece of evidence supporting the sudden onset of the megaflood^[1][5][14].

Furthermore, seismic reflection data have uncovered a distinctive “W-shaped channel” on the continental shelf east of the Sicily Sill. This channel appears to connect the erosional features onshore to deep submarine canyons, particularly the Noto Canyon, thereby acting as a funnel for the massive floodwaters^[6][11][27]. Such geophysical imaging has been crucial in confirming that these features are not the result of gradual processes but instead reflect the high-energy dynamics of a catastrophic flood event.

Hydrodynamic models have been used to simulate the behavior of the megaflood. These computer simulations helped estimate peak flow velocities, discharge rates, and the evolution of the flood as it transitioned from the western to the eastern Mediterranean basin. Model predictions suggest that discharge rates during the event ranged between 68 and 100 Sverdrups (with one Sverdrup equaling one million cubic meters per second)^{[2][8][14][27]}. The floodwater is estimated to have reached speeds of up to 32 meters per second (72 miles per hour), and computer models indicate that as the water spilled over the Sicily Sill, its flow direction altered gradually in a clockwise manner, deepening channels further downstream^[5][6][13].

These dynamic simulations are supported by geological evidence; for instance, the deposition of bedload debris and the formation of streamlined ridges are consistent with rapid, high-energy water flows that can modify both subaerial and submarine landscapes almost instantaneously on a geological timescale^[1][13][19].

The reintroduction of water during the Zanclean Megaflood not only refilled the Mediterranean basin dramatically but also had long-lasting effects on regional topography and sediment deposition. The flood is implicated in the formation of vast sedimentary deposits in the western Ionian Basin, with estimates suggesting that volumes up to 1,600 cubic kilometers of chaotic megaflood sediment were transported and deposited over a short time span^[8][16][25].

Beyond reshaping the local landscape, the event had broader implications. Various studies have noted that such a massive and rapid influx of water would have induced seismicity, contributed to the erosion of canyons along the Malta Escarpment, and influenced the later development of Mediterranean ecosystems and human settlement patterns. As research has shown, “These findings not only shed light on a critical moment in Earth’s geological history but also demonstrate the persistence of landforms over five million years”^[9][16][18].

Importantly, the evidence for this event challenges previous models that favored a slow, gradual reconnection of the Mediterranean with the Atlantic. New data suggest that the basin underwent a dramatic environmental transformation over a timescale of only a few years, rather than the previously assumed 10,000 years^[4][20][24]. This recognition alters long-standing perspectives on the interplay between tectonics, climate, and oceanography in the Mediterranean region, and it provides a compelling example of how catastrophic events can dominate Earth's geological record.

A synthesis of evidence from diverse sources, including geological field observations, seismic imagery, and numerical modeling, strongly supports the hypothesis of the Zanclean Megaflood as a rapid and massive event that refilled the Mediterranean Sea at the end of the Messinian Salinity Crisis. Multiple independent studies converge on key points: the identification of over 300 streamlined erosional ridges, the rapid deposition of debris marking the critical boundary between geological periods, the discovery of a W-shaped subaqueous channel acting as a funnel for catastrophic flows, and model estimates indicating unprecedented water discharge rates and velocities^{[1][2][3][4][6][8][11][14][16][19][24][27][29]}.

This comprehensive picture reinforces the idea that Earth’s history is punctuated by sudden, extreme events capable of reshaping entire regions. The Zanclean Megaflood serves as a dramatic example of such processes, reminding us that even vast ocean basins can be transformed in a matter of years due to the dynamic forces of water and tectonics. Continued research and exploration along the Mediterranean margins promise to further illuminate the details of this extraordinary event and its lasting legacy on our planet^{[7][10][12][15][17][20][21][22][23][25][26][28][30]}.