develop into the previous system split and spawned a tropical depression over the northern Bahamas on October 17. The depression moved rapidly northward ahead of an approaching frontal boundary. Historical weather maps indicated that the highest sustained winds were at 30 mph (50 km/h) and the minimum barometric pressure was . The depression was absorbed by the front on the same day. Tropical Storm Seven A weak low pressure area developed into the seventh storm of the season formed near the Cayman Islands on October 30. Initially a tropical depression, it tracked slowly north-northeastward and reached tropical storm status about six hours after forming. Early on October 31, the storm peaked with maximum sustained winds of 45 mph (75 km/h), several hours before making landfall in Sancti Spíritus Province several hours later. After emerging over the Bahamas, the storm slowly weakened. Late on November 1, the system struck Andros Island with winds of 40 mph (65 km/h). Thereafter, the cyclone accelerated and continued weakening, falling to tropical depression intensity late on November 3. Shortly thereafter, it transitioned into an extratropical cyclone while located about 215 mi (345 km) south of Cape Hatteras, North Carolina. The remnants contributed to the development of the system which brought devastating floods to the Northeastern United States. Following well above average precipitation in October, this system brought as much as to Vermont, contributing to the Great Vermont Flood of 1927. The flooding left at least $50 million (1927 USD) in damage and 85 deaths, with all but one death occurring in Vermont. Tropical Storm Eight The final tropical cyclone of the season developed from a low pressure area early on November 19, while situated about east-northeast of Barbuda. Initially a tropical depression, the cyclone deepened into a tropical storm about 12 hours later while moving north-northwestward. At 12:00 UTC on November 20, a ship observed a barometric pressure of , the lowest known pressure in association with the storm. Using the pressure-wind relationship, it is estimated that the storm reached maximum sustained winds of 60 mph (95 km/h) at that time. On November 21, the storm weakened and lost tropical characteristics, merging with a cold front about 585 mi (940 km) east-northeast of Bermuda at 12:00 UTC. The extratropical cyclone persisted for only about six more hours. This storm may have been subtropical, but in the absence of satellite imagery, it is considered a tropical