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1893 Great Charleston hurricane

Category 3 Atlantic hurricane

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Through Canada

In the Bahamas, abnormally high tides inundated some streets on New Providence and nearby Hog Island (modern-day Paradise Island), sweeping away the home of the assistant lighthouse keeper. The storm severely damaged pineapple cultivation facilities on Eleuthera and plantations on the Abaco Islands, where many other buildings were destroyed. In Florida, storm surge reached several feet above ground between Palm Beach and Jacksonville, while heavy rains fell, leading to flooding in a number of coastal communities. Coastal flooding impacted South Carolina from Georgetown southward, though the worst occurred between Winyah Bay and Murrells Inlet. The National Hurricane Center lists the combined death toll for Florida and South Carolina at 28. North Carolina reported extensive damage to crops, trees, homes, and shipping, as well as 22 fatalities. Many towns across Virginia, the Mid-Atlantic, New England, and Ontario experienced wind damage and some coastal and freshwater flooding. In Maryland, the storm caused two indirect deaths and about $1 million in damage in Baltimore alone. Inside the Great Lakes, the storm capsized nearly 40 vessels, leading to a loss of 54 lives. Four other people died in Buffalo, New York. Overall, 110 deaths are attributed to the storm.

Meteorological history

Meteorologist Charles J. Mitchell of the Weather Bureau noted in 1924 that this storm was first observed over the far eastern Atlantic at 11°0′N 26°0′W / 11.000°N 26.000°W on September 25. Consequently, the Atlantic hurricane database begins the track of this cyclone at 06:00 UTC on that day at 11°6′N 25°0′W / 11.100°N 25.000°W, approximately 275 mi (445 km) south-southwest of the westernmost islands of Cabo Verde. Initially a tropical storm, the system moved westward and intensified into a hurricane on September 28 and a Category 2 hurricane on the modern-day Saffir–Simpson scale on October 1. By the following day, the cyclone began a northwestward motion. The hurricane is also estimated to have strengthened into a Category 3 hurricane on October 2 and reached maximum sustained winds of 120 mph (195 km/h) shortly thereafter. The hurricane then moved west-northwestward for several days, beginning on October 6. After passing just north of the Abaco Islands on October 12, the storm curved northwestward and then north-northwestward. Remaining closely offshore Florida and Georgia, the cyclone passed only about 25 mi (40 km) east of Ormond Beach in the former at 00:00 UTC on October 13.

The hurricane then turned northeastward later on October 13 and at around 13:00 UTC, it made landfall near McClellanville, South Carolina, winds of 120 mph (195 km/h) and an atmospheric pressure of 955 mbar (28.2 inHg). Meteorologist Francis P. Ho estimated both figures in 1989, the latter based on a recorded atmospheric pressure of 959 mbar (28.3 inHg) and a maximum wind radius of 17 mi (27 km) and the sustained winds based on these calculations and the storm's latitude. Moved rapidly northward through North Carolina and the Appalachian Mountains, the cyclone was still a Category 1 hurricane as it passed 60 mi (95 km) west of Washington, D.C. The storm transitioned into an extratropical cyclone over far southern Quebec on October 14 after crossing Lake Ontario and continued northeastward until dissipating over the northeastern portions of the province on the following day. Overall, the hurricane achieved an accumulated cyclone energy rating of 63.5, one of the highest values ever recorded.

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