The Lighthouse Keeper Who Wished For The Greatest Storm

A Man and His Rock

The Eddystone Rocks lie fourteen miles south of Plymouth, just far enough offshore to be invisible from the coast on all but the clearest days. For centuries, they were simply a hazard: a cluster of gneiss outcrops rising barely above the waterline, exactly in the path of ships running up the English Channel toward Plymouth Sound. Nobody kept count of how many vessels they claimed, but estimates of hundreds of wrecks across the medieval and early modern periods are credible. The rocks had no lighthouse because conventional wisdom held that no structure could stand on them. They were too exposed. The sea broke over the tops of them in heavy weather.

Henry Winstanley was not a conventional man. He was an Essex merchant, a property developer, an eccentric builder of mechanical curiosities and water features. He had lost ships on the Eddystone. Sometime in the early 1690s he decided, apparently on his own initiative, to build a lighthouse on the rock. He began construction in 1696. The first design was a wooden hexagonal structure, more elaborate than sturdy, and the storms of 1698 and 1699 damaged it badly enough that he rebuilt it as a heavier, taller, more reinforced structure. The final version was completed by 1700 and featured a lantern room, a weather vane, a series of ornamental gilded details, and what contemporaries described as an air of confident theatricality that matched its builder's temperament.

Winstanley was proud of the lighthouse in the way a man is proud of something everyone told him was impossible. He reportedly said that he wished to be inside it during the greatest storm there ever was. Whether this was bravado, a genuine engineering boast, or simply the kind of remark that gets remembered because of what happened next is now impossible to know. He was, by November 1703, around 59 years old. He had gone out to the rock for maintenance work, accompanied by a small crew. He was inside the lighthouse when the storm arrived.

The Storm Builds

The weather had been deteriorating across England for nearly two weeks before the main event. A series of storms in mid-November 1703 had already brought high winds and heavy rain. Barometric pressure readings collected by observers across England and the Continent show the main system approaching from the Atlantic on the afternoon of November 26 (Old Style calendar; New Style November 7). The pressure dropped sharply across southwest England through the evening. It was one of the steepest falls in pressure ever documented in English meteorological records.

The storm reached the south coast around midnight. Modern meteorologists, working from the barometric records collected by contemporaries and later compiled by Hubert Lamb and Knud Frydendahl, have reconstructed the system as a powerful extratropical cyclone tracking northeast across England. Estimated maximum wind gusts reached 120 miles per hour. The track ran roughly from the Bristol Channel northeast toward the Humber, placing the most severe conditions directly over the English Midlands, the Thames Valley, and the English Channel.

It was, by any reconstruction, the most violent windstorm to strike England in the period of written record. The question of whether any storm before or since has exceeded it is difficult to answer definitively, because the instrumental record only extends so far. What is certain is that nothing before or since in England's documented history has caused destruction on this scale in a single night.

What It Did to the Land

The damage across England was total in a way that is difficult to comprehend now. In London, an estimated 2,000 chimney stacks collapsed in a single night. Queen Anne was sheltering in the cellar of St. James's Palace while the building shook and masonry fell around her. The lead roofing of Westminster Abbey, which had survived the weather of centuries, was torn off and found scattered in the streets. The Bishop of Bath and Wells was killed in his bed when a chimney stack collapsed through the ceiling of his chamber.

The Thames rose six feet higher than any previously recorded level, flooding roughly 5,000 homes along its banks. On the rivers and across the low-lying land of southern England, entire flocks of sheep were blown into flooded ditches and drowned. In the New Forest, approximately 4,000 mature oak trees were felled in a single night. Across England, an estimated 400 windmills were destroyed. Some of them spun so fast in the gusts that the friction of their shafts set them alight.

The death toll on land is estimated between 8,000 and 15,000 across England, though precise figures were never compiled. The range reflects the difficulty of counting deaths from chimney collapses, flooding, exposure, and the falling of trees and buildings across the width of the country. Contemporary accounts speak of entire villages left without roofs. The journalist and writer Daniel Defoe, who was 43 years old and living in London when the storm struck, spent the following months collecting eyewitness letters from across England and estimated the loss of life in his subsequent book at well over eight thousand.

The Goodwin Sands Disaster

The storm's worst single catastrophe happened not on land but at sea, on and around the Goodwin Sands, a large sandbar off the Kent coast near Deal. The Royal Navy's Channel Squadron had been at anchor in The Downs, the sheltered roadstead between the Goodwin Sands and the shore, when the storm struck. The anchorage, normally well-protected, offered no shelter from winds of this intensity.

Rear Admiral Basil Beaumont's squadron was destroyed at anchor. The ships Stirling Castle, Mary, Northumberland, and Restoration were all driven onto the Goodwin Sands and wrecked. Beaumont himself died when his flagship struck the sands. In all, the Royal Navy lost thirteen ships of the line in the storm, and more than 1,500 sailors drowned in the waters around Kent in a single night. The Goodwin Sands, already notorious for the number of vessels they had claimed over the centuries, became in a single event the site of the worst loss the Royal Navy had sustained in any peacetime disaster.

Survivors clinging to the wreck of the Stirling Castle were visible from shore the following morning. The local townspeople at Deal launched boats to reach them. Whether the rescuers reached the wreck before it broke up entirely is contested in the contemporary accounts. What is agreed is that the Goodwin Sands, already known as "the ship-swallower," consumed four of the King's largest warships so completely that virtually nothing remained on the surface by the next tide. The sea floor of the Goodwin Sands has since been surveyed and contains the remains of more vessels than any comparable area of British coastal waters.

"No pen could describe it, nor tongue express it, nor thought conceive it unless by one in the extremity of it."

Daniel Defoe, The Storm, 1704

The Eddystone Rock

Out on the Eddystone rock, fourteen miles southwest of Plymouth, the storm reached Henry Winstanley's lighthouse sometime during the night of November 26. Nobody was watching. There were no other ships in the area, no observers close enough to see what happened in the dark and the spray. The lighthouse had been illuminated when vessels last sighted it in the days before the storm. After the night of November 26, it was gone.

A vessel out of Plymouth attempting the passage in the days after the storm found the rock bare. The lighthouse, which had stood for three years and had survived multiple previous gales with Winstanley inside it, had been taken by the sea. Winstanley and five other men, including the keeper and members of the maintenance crew, had vanished with it. Their bodies were never recovered. The only things remaining on the rock were the iron fastenings that had anchored the structure to the stone.

The Eddystone rock was left unmarked for the following years. The wreck toll on the approaches to Plymouth immediately increased. Trinity House, the body responsible for English lighthouses, commissioned John Rudyerd to design a replacement. Rudyerd's second Eddystone Lighthouse was completed in 1709, also of wood, and stood until 1755, when a fire started by the lantern consumed it entirely. The head keeper, Henry Hall, swallowed molten lead from the burning lantern during the fire and died twelve days later. His lead-filled stomach was preserved as a medical specimen.

The third Eddystone Lighthouse, designed by John Smeaton and completed in 1759, became one of the most celebrated engineering achievements of the eighteenth century. Smeaton's innovation was to interlock the granite blocks of the tower like a three-dimensional jigsaw, so that the structure acted as a single mass. His design was so sound that when the rock beneath it began to crack in the 1870s, the lighthouse itself was undamaged. It was carefully dismantled and re-erected on Plymouth Hoe, where it still stands today. The fourth, current lighthouse replaced it on the rock in 1882.

Daniel Defoe and the Birth of Modern Journalism

The night of November 26, 1703, produced one of the most significant documents in English literary history. Daniel Defoe, then 43 years old and working as a political journalist in London, survived the storm and immediately recognized that something unprecedented had occurred. He placed advertisements in newspapers asking survivors across England to send him firsthand accounts of what they had witnessed. Hundreds of letters arrived.

Defoe published the resulting book, The Storm, in 1704. It is a remarkable piece of work. Defoe was meticulous about attribution and about separating what correspondents claimed to have seen from what they were reporting secondhand. He included letters describing the storm at sea, in rural counties, in London, and on the rivers. He appended meteorological observations and attempted a systematic account of the damage. He was clear about the limits of what anyone could know: the destruction had been too widespread, too simultaneous, and too total for any one account to be complete.

Literary historians regard The Storm as the first work of modern journalism in the English language. It preceded Defoe's novels by fifteen years. Before Robinson Crusoe, before Moll Flanders, before any of the fiction that made him famous, there was this: a writer gathering eyewitness letters in the aftermath of a disaster, fact-checking them as best he could, and publishing them with enough editorial structure to produce a coherent account of something no single person had witnessed in its entirety.

The Storm at Sea

The Royal Navy's losses at the Goodwin Sands represented only a fraction of the total maritime toll from the storm. Hundreds of merchant vessels were caught in the English Channel, the North Sea, and the approaches to English and Dutch ports. The Dutch coast suffered badly; estimates of total European maritime deaths from the storm run considerably higher than the English naval figure alone. The storm made no distinction between warship and fishing boat, and the approaches to the Thames, the Humber, and the Mersey were thick with wreckage in the days following.

The Royal Navy's losses prompted an immediate inquiry. Admiralty records show a systematic accounting of the ships lost, the men drowned, and the anchors and cables that failed in the night. The inquiry found no negligence. The storm, the records concluded, was simply beyond any preparation the Navy had made or could have made. Thirteen ships of the line were a catastrophic loss. The Navy spent the following decade replacing them.

What the Barometers Recorded

The Great Storm of 1703 is one of the earliest weather events that can be quantitatively reconstructed. The barometer had been in use in England for about fifty years by 1703, and a number of observers kept systematic records. The storm's pressure signature across England was captured in enough independent measurements to allow modern meteorologists to build a plausible reconstruction of its track, intensity, and timing.

Hubert Lamb, the British climatologist who spent much of his career reconstructing historical European weather events, identified the 1703 storm as the most intense extratropical cyclone to strike England in the historical record. Working with Knud Frydendahl, Lamb published a reconstruction in 1991 based on the barometric readings, storm surge data, and contemporary accounts. Their conclusion: the central pressure of the system was probably around 950 millibars or lower as it crossed southern England, placing it in the same category as the most powerful Atlantic storms of the modern instrumental era.

The 1987 Great Storm, which caused catastrophic damage across southern England and northern France and which a BBC forecaster infamously dismissed as not worth worrying about the night before, reached minimum pressures of around 953 millibars. The 1703 storm, on the reconstruction, was likely more intense and almost certainly tracked farther south, placing the maximum winds directly over the most densely populated parts of England. The 1987 storm killed 22 people in England and felled 15 million trees. The 1703 storm killed perhaps 15,000 and felled, by one estimate, 25 million.

The difference is not only meteorological. In 1703 there were no weather forecasts, no storm warnings, no shuttered windows prepared in advance. The ships in The Downs had no warning to seek port. Henry Winstanley had no way of knowing that the storm arriving on the night of November 26 was unlike anything the Eddystone had yet faced. The barometers recorded it. Nobody knew how to read what they were saying.