The Strait has an average depth of 365 metres (1200 ft) with its shallowest point being 50 metres (164 ft.) There is a general flow of water from west to east because the Mediterranean loses more water from evaporation than its rivers can replace and needs replenishment from the Atlantic. (An interesting fact when one considers that mighty rivers like the Nile, the Danube, the Don, the Volga and others all add to it.) The surface current runs from over two knots to as much as six knots and this was a problem during the days of sail and oared propulsion. Well below the surface there is an opposite current, colder and quite saline, running into the Atlantic. | The Strait has an average depth of 365 metres (1200 ft) with its shallowest point being 50 metres (164 ft.) There is a general flow of water from west to east because the Mediterranean loses more water from evaporation than its rivers can replace and needs replenishment from the Atlantic. (An interesting fact when one considers that mighty rivers like the Nile, the Danube, the Don, the Volga and others all add to it.) The surface current runs from over two knots to as much as six knots and this was a problem during the days of sail and oared propulsion. Well below the surface there is an opposite current, colder and quite saline, running into the Atlantic. |