[1] Weather maps and ship data indicate the development of a tropical depression in the southwestern Caribbean Sea around 06:00 UTC on June 21.

After briefly crossing the Yucatan Peninsula, the cyclone emerged into the Gulf of Mexico and eventually began moving more to the west-northwest.

The hurricane then curved northwestward and made landfall in Padre Island, Texas, at the same intensity around 01:00 UTC on June 28.

After moving inland, the storm quickly weakened and dissipated over Val Verde County just under 24 hours later.

Additionally, communication by telegraph and telephone were cut-off for several days and traffic was interrupted due to inundated streets.

[3] A low pressure area detached from a stationary front and developed into a tropical depression on August 14 while located about 185 mi (298 km) west-southwest of Bermuda.

[4] By August 16, the storm transitioned into an extratropical cyclone while situated about 290 mi (470 km) southeast of Sable Island, Nova Scotia.

[3] Weather maps and ship data indicated a tropical depression formed near the west coast of Africa on August 26.

Around 12:00 UTC on September 12, the storm became extratropical while located about 290 mi (470 km) southeast of Cape Race, Newfoundland and Labrador.

[4] In North Carolina, winds as high as 74 mph (119 km/h) at Hatteras caused severe crop losses, especially in areas adjacent to Pamlico Sound.

At the latter, northeast to southeast gales caused waterways to rise 10 ft (3.0 m) above previous high-water marks.

Eventually, the system curved southwestward and transitioned into a tropical storm on October 6 while situated about 325 mi (523 km) northwest of Bermuda.

Peaking with maximum sustained winds of 75 mph (121 km/h) and a minimum barometric pressure of 989 mbar (29.2 inHg), the hurricane made landfall near McClellanville, South Carolina, about eight hours later.

[3] The final tropical storm developed in the northwestern Caribbean Sea about 60 mi (97 km) southeast of Banco Chinchorro, Mexico, at 00:00 UTC on October 28.

[4] It transitioned into an extratropical cyclone in present-day Mayabeque Province before being absorbed by a frontal boundary shortly thereafter.

The first formed northeast of Bermuda on May 5, marking the third consecutive year in which a tropical cyclone originated before June.

Drifting slowly northward and westward, the system made landfall in southern Texas on June 16 and dissipated the following day.

The final cyclone that failed to tropical storm status developed in the northeastern Gulf of Mexico to the south of Tallahassee, Florida, on August 4.