The Scottish Maelstrom

The Gulf of Corryvreckan – the channel (0.6 miles wide) between the northern end of Jura and the island of Scarba – is home to one of the most notorious tidal whirlpools in the world.

On Scotland's west coast, the rising tide – the flood tide – flows northwards. As it moves up the Sound of Jura, to the east of the island, it is forced into a narrowing bottleneck jammed with islands and builds up to a greater height than the open sea to the west of Jura. As a result, millions of tonnes of sea water pour westwards through the Gulf of Corryvreckan at speeds of up to 8 knots – an average sailing yacht is going fast at 6 knots.

The Corryvreckan Whirlpool forms where this mass of moving water hits an underwater pinnacle, which rises from the 200m-deep sea bed to within just 28m of the surface, and swirls over and around it. The turbulent waters create a magnificent spectacle, with white-capped breakers, standing waves, bulging boils and overfalls, and countless miniature maelstroms whirling around the main vortex.

Corryvreckan is at its most violent when a flooding spring tide, flowing west through the gulf, meets a westerly gale blowing in from the Atlantic. In these conditions, standing waves up to 5m high can form and dangerously rough seas extend more than 3 miles west of Corryvreckan, a phenomenon known as the Great Race.

You can see the whirlpool by making the long hike to the northern end of Jura, or by taking a boat trip from Islay, Ardfern or the Isle of Seil.

For tide times, see