science π Ancient Mediterranean flood flowed at massive rate
Models suggest the Zanclean flood, which refilled the Mediterranean, reached a peak flow of roughly 100 million cubic metres per second through the Strait of Gibraltar. This event occurred around 5.33 million years ago, ending the Messinian Salinity Crisis when the Atlantic reconnected. The flow was estimated to be about 1,000 times the volume of the modern Amazon river. The water transfer happened quickly, possibly within a few months to two years. Scientists are using erosion data to model this immense geological event. π