Goodwin Sands

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Goodwin Sands is a 10-mile-long (16 km) sandbank at the southern end of the North Sea lying 6 miles (10 km) off the Deal coast in Kent, England. The area consists of a layer of approximately 25 m (82 ft) depth of fine sand resting on an Upper Chalk platform belonging to the same geological feature that incorporates the White Cliffs of Dover. The banks lie between 0.5 m (1 ft 8 in) above the low water mark to around 3 m (10 ft) below low water, except for one channel that drops to around 20 m (66 ft) below. Tides and currents are constantly shifting the shoals. More than 2,000 ships are believed to have been wrecked upon the Goodwin Sands because they lie close to the major shipping lanes through the Straits of Dover. The few miles between the sands and the coast is also a safe anchorage, known as The Downs, used as a refuge from foul weather. Due to the dangers, the area—which also includes Brake Bank—is marked by numerous lightvessels and buoys. Notable shipwrecks include HMS Stirling Castle in 1703, VOC ship Rooswijk in 1740, the SS Montrose in 1914, and the South Goodwin Lightship, which broke free from its anchor moorings during a storm in 1954. Several naval battles have been fought nearby, including the Battles of the Goodwin Sands (Battle of the Narrow Seas) in 1602 and the Battle of Dover in 1652, and the Battle of Dover Strait in 1917. When hovercraft ran from Pegwell Bay, Ramsgate, they made occasional voyages over the Sands, where boats could not go safely. Southeast from Goodwin Sands lies the Sandettie Bank.