produced by the storm off of Pensacola, Florida on October 4. Squalls in western and northern Florida produced heavy rain, with a maximum occurring in Wewahitchka, which received . The precipitation produced localized flooding in the Tallahassee area. The squalls also produced strong winds, at times gusting to near Pensacola. A station at Naval Air Station Pensacola clocked a gust. These winds caused minor damage limited to uprooted trees and broken limbs. East Coast Rainfall from the remnants of Hilda extended as far northeast as Delaware as a result of the remnants interacting with a frontal boundary that extended across the United States East Coast. Extremely torrential rains fell over Georgia, peaking at south of Waynesboro. The largest precipitation totals occurred in the state's northeastern extremities, where widespread totals of or higher were reported. The rains resulted in flash flooding, causing extensive damage to roads and other infrastructure across Georgia. The excess floodwater caused streams to overflow their banks. At least 30 bridges were washed away by these swollen streams, and several county roads were washed out. The most considerable damage was reported in northeastern Georgia, coincident with the high rainfall totals there. Damage in Rabun County alone exceeded US$100,000. In addition to infrastructure damage, thousands of acres of farmland were inundated. Torrential rainfall continued northeastwards into the Carolinas, with statewide rainfall peaking at and in North and South Carolina, respectively. The rains in North Carolina exacerbated preexisting flood conditions which had previously caused widespread agricultural and infrastructural damage as well as soil erosion. Though not directly a result of Hilda's remnants, they were likely influenced by the storm's interaction with a frontal boundary. Already overflowing rivers and streams rose even further, reaching near-record levels. Raleigh experienced severe flooding, and roughly 4,000 people were forced to evacuate their homes due to dangerous floodwaters. Two cars in mountainous regions were swept into inundated areas during the floods, resulting in one death. Several tornadoes in six counties were also reported, injuring two. Extensive wind damage was reported in Wayne County. Heavy rains in South Carolina from October 4–6 resulted in localized flash flooding, particularly near streams. In mountainous regions, runoff from precipitation caused the Keowee, Saluda, and tributaries of the Broad River to swell, inundated and causing substantial damage to adjacent agricultural land and roads, in addition to breaching several small dams. The flooding triggered landslides, killing one person. Counties in the