located south of the Mississippi River Delta. Beginning on September 14, the storm began to accelerate as it turned towards the northeast. Around 04:00 UTC on September 15, the cyclone made landfall in St. Marks, Florida, at peak intensity. The storm crossed the state quickly and briefly entered Georgia before emerging into the Atlantic less than eight hours after landfall. However, the system soon transitioned into an extratropical cyclone a short distance east of Sapelo Island around 12:00 UTC on September 15. The extratropical cyclone quickly accelerated parallel to the United States East Coast, before being absorbed by another extratropical system over Quebec. The storm's quick passage over the Florida peninsula left relatively minor damage. A train crossed over a washout on its railroad, causing it to derail. In Apalachicola, there was considerable damage to crops, and torrential rains caused $2,000 in damages. Electric power in the city was also disabled, and some buildings suffered structural damage, totaling to $8,000 in damages. Tallahassee observed of precipitation. In Georgia, Thomasville and Valdosta experienced "high winds and considerable rainfall," according to the Tallahassee Democrat. A few weather stations along the East Coast of the United States recorded sustained tropical storm force winds, including Hatteras, North Carolina; Atlantic City, New Jersey; and New York City, New York. There were scattered reports of wind damage across Atlantic Canada, including the toppling of telephone and electrical wires, and the deroofing of buildings and homes. In Nova Scotia, Annapolis Valley lost approximately 75% of its apple crops. The storm also left maritime impacts, damaging or destroying docks, wharves, and boats. At least one death occurred in Canada, while eight other people went missing along with their vessel. Tropical Storm Seven On September 16, a tropical storm with winds of developed out of a frontal boundary about southwest of the northwesternmost islands of the Azores. Moving slowly towards the northwest, gales were reported by ships in the region as the cyclone slowly intensified. On September 20, the storm began to move towards the southwest. The system reached peak intensity on September 21, with winds of , before transitioning into an extratropical cyclone about halfway between Bermuda and Nova Scotia as it recurved northwards on September 23. The extratropical cyclone later made landfall on Nova Scotia the following day, before dissipating over southern Greenland on September 26. Sustained winds in Atlantic Canada peaked at on Resolution Island in