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1804 Antigua–Charleston hurricane

Hurricane in 1804

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The hurricane produced a wide swath of damage along its path, especially in Georgia and South Carolina. Maritime losses along the coastlines of both states were significant, with numerous ships damaged or destroyed. Crop damage, especially to rice, cotton, and corn, was also considerable, with impending harvests ruined by the hurricane's arrival. Strong winds and heavy rainfall inundated streets, residences, and fields, and also toppled chimneys, fences, and cracked windows across the region. Wharves, struck by stranded boats, endured significant damage as well. Dozens of residences and other structures were destroyed or rendered uninhabitable due to inundation or collapse. Notably, Aaron Burr, then attempting to flee authorities, visited St. Simons Island in Georgia during the hurricane, later returning to Hampton and giving a detailed account of the hurricane's effects. Damage in Savannah, Georgia, totaled $500,000, compared to $1,000,000 at Charleston, South Carolina.

Meteorological history

The 1804 Antigua–Charleston hurricane was first sighted on 3 September as it swept past Saint Barthélemy, Saint Kitts, and Antigua, drifting toward the west-northwest and soon approaching Puerto Rico and the Turks and Caicos Islands. The storm reached the Bahamas while turning northward on 4 September, nearing the northern Floridan coast by 6 September. It remained offshore on 7 September, gradually approaching the coast throughout the day, and eventually made landfall that evening along the coasts of Georgia and South Carolina. Observations in Savannah, Georgia, indicated north-to-northeast winds throughout 8 September, though other reports recorded northeast-to-easterly gusts; at Charleston, South Carolina, however, winds, initially northeast-to-east, curved southeastward later in the storm. Little information exists on the hurricane's whereabouts between North Carolina and New England, with a single report at Norfolk, Virginia of east-northeasterly winds veering east-to-east-southeast from 7 to 9 September, suggesting the disturbance's passage west of there. A severe gale arrived in New England on 11 and 12 September, though the long pause between the departure of the hurricane from the Carolinas and its arrival in the northeastern United States evidences the possibility that the two systems may have been unrelated.

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