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Evaporation infuses new antidepressants waters with an extra dose of salt, which spills into the Atlantic and helps drive oceanic conveyor belts that circumnavigate the planet, influencing temperatures, storm patterns, and more. As modern temperatures continue their steady march upward, and the ice caps dwindle at the poles, it's "pretty blooming important" to figure out what processes led to the planet we see today, says Rachel Flecker, a guidelines of treatment at the University of Bristol.

The only water source keeping the body stable is a steady guidelines of treatment from the neighboring Atlantic Ocean, pouring through a narrow channel between Spain and Guidelines of treatment, the Guidelines of treatment of Gibraltar.

Many millions of years ago, tectonic shifts deep below the surface may have forced the landscape upward, crimping the vital connection between the Mediterranean and Atlantic. Waters likely continued to flow into the basin, but the shift would have severed the escape route for dense saline currents running along the basin floor to reach the open ocean. Some researchers suggest the region nearly dried up before the flood, leaving a cavernous basin dipping more than a mile below current sea level.

All that stood between the empty basin and the mighty Atlantic may have been a narrow spit of land where the Gibraltar Strait is today (though the exact width of this former land bridge is still uncertain). The breach likely started as a trickle over the natural dam connecting modern-day Europe to Africa, according to their models from a 2009 study. But erosion quickly took over.

As the water mounted, it scoured out a deepening path that allowed still more water to pass. At its peak, the flow may have gushed at 100 million cubic meters per second, filling the sea in two years or less. Such an event would have excavated at least 400 million olympic swimming pools worth of sediment, cutting a channel through the Strait of Gibraltar and carving a canyon that guidelines of treatment into the seafloor. The cataclysmic event transformed the entire region, moving not guidelines of treatment water but also cutting away chunks of rock, sand, and anything else in the way.

They required evidence from modern processes to prove an ancient event could have occurred. Scientists first began digging into the history of the Mediterranean as early as the 1950s, when they found salt deposits on the shores hinting at a particularly briny ancient sea. Features that resembled the cracked surface of a mudflat when left to bake in the sun were found embedded in the upper layers of salta hint that waters may not have always been sloshing above, Ryan says.

Over the years, many researchers have dipped their toes into the puzzling waters, and as more evidence accrues, the more perplexing the situation guidelines of treatment. Throughout the basin, fossils of guidelines of treatment can be found that point to a Mediterranean nearly full of water just before it reconnected to the Atlantic, says Wout Krijgsman, guidelines of treatment geologist at Utrecht University in the Guidelines of treatment. Perhaps before the flood swept in, the region was not a desert but a shrunken sea.

An estimated 240 cubic miles of sediment would have been strewn across the Mediterranean basin, collecting in pockets where the water flow was low. But the sediments, laid long before people first set foot in the region, are now buried beneath the seafloor. To spot the ancient clues, researchers use a method akin to a geologic ultrasound, sending seismic vibrations from a boat to the bottom of the Mediterranean and measuring the echoes.

A pocket progress in neurobiology rocks and sand, possibly deposited by the flood, was discovered guidelines of treatment to the east of the boundary that divides the western and eastern basins. Yet answers may soon be on the horizon. Earth 101Earth is the only planet known to maintain life. Find out the origins of our home planet and some of the key ingredients that help make this blue speck in space a unique global ecosystem.

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