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The 1916 Charleston hurricane was a tropical cyclone that impacted parts of the Southeastern United States in July 1916. Torrential rainfall associated with the storm as it moved inland led to the Great Flood of 1916: a prolific and destructive flood event affecting portions of the southern Blue Ridge Mountains. This flood accounted for most of the damage and fatalities associated with the hurricane; most of these occurred in North Carolina. The hurricane was first detected as a tropical storm 560 mi (900 km) east of Miami, Florida on July 11. It took an unusually straightforward path towards the Carolinas and strengthened into a hurricane on July 12. The storm's peak sustained winds of 115 mph (185 km/h)—equivalent to a modern-day Category 3 hurricane on the Saffir–Simpson scale—were attained on July 13. It made landfall near Charleston, South Carolina, the next morning, and weakened as it continued inland before losing its tropical cyclone status on July 15 over western North Carolina.
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