Saint Thomas, while Saint Barthélemy experienced sustained winds between . On Saint Thomas, winds downed wires and trees and damaged homes. The storm also capsized ships in Saint Thomas harbor and at Tortola. Property damage on Saint Thomas alone exceeded $200,000, while 15 fatalities were reported. Most of the damage caused by the San Ciprián hurricane occurred in Puerto Rico, particularly along the island's northern half, with the cyclone drawing comparisons to the 1928 Okeechobee hurricane. The powerful winds destroyed numerous buildings. More than 40,000 homes were demolished, rendering 25,000 families homeless. Winds also knocked out communications systems, hampering relief efforts. Heavy losses were incurred to crops, particularly to citrus and coffee. The hurricane caused 257 deaths and injured 4,820 other people, while inflicting about $35.6 million in damage. Economic losses related to the hurricane amounted to about 20 percent of Puerto Rico's gross income. Significant damage to agriculture occurred in the Dominican Republic. Impacts in Jamaica and British Honduras were minimal. Tropical Storm Ten A tropical storm was first identified in the eastern Atlantic on September 28 as a small, compact system, with winds of and a minimum pressure of . Initially situated roughly south-southeast of Cape Race, Newfoundland, the storm moved southeastward and intensified slightly to peak with maximum sustained winds of . Thereafter, the storm interacted with an extratropical cyclone which pulled it to the northwest. The extratropical cyclone later absorbed the system at 06:00 UTC on September 30 near its location of development. Tropical Storm Eleven A tropical depression formed on October 7 from a broad low-pressure area in the central Caribbean offshore Honduras. Moving slowly to the west-northwest, the depression steadily intensified, reaching tropical storm strength at 12:00 UTC the same day. The storm continued to intensify as it moved towards the Yucatán Peninsula, reaching peak intensity late on October 9, with maximum sustained wind speeds of . The storm made landfall near Playa del Carmen at 04:00 UTC the next day, while still at peak intensity. Over land, the storm weakened to a tropical depression on October 11 as it curved northwestward. On the next day, the depression later emerged into the Gulf of Mexico, where it began to restrengthen. By 12:00 UTC on October 13, the elongated system regained tropical storm strength, before reaching a secondary peak intensity of . However, baroclinic forces caused the storm to become extratropical prior to striking Louisiana