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Newfound Gap Road landslide January 16, 2013. The January 2013 Southeastern United States floods occurred from January 14 to 17 and resulted in mudslides and washouts throughout the southern Appalachian Mountains region. [1] [2] [3] At the height of the flooding, 50 roads were declared impassable in Greene County, Tennessee alone. [4]
Floods in the United States (2000–present) is a list of flood events which were of significant impact to the country during the 21st century, since 2000. Floods are generally caused by excessive rainfall, excessive snowmelt, storm surge from hurricanes , and dam failure.
On September 22, The United States Geological Survey measured the greatest flow ever recorded on Sweetwater Creek, at 28,000 cubic feet per second (790 m 3 /s). [2] The flooding from the creek was met with water from the swollen Chattahoochee River, which blocked Interstate 20 west of Atlanta for two days. Many homes and businesses in the area ...
Maps show the areas impacted by storm surge, rainfall levels and more as Helene, once a major hurricane and now a tropical storm, moves inland from Florida's Gulf Coast over Georgia.
While Helene has weakened to a tropical storm, it is still unleashing life-threatening storm surge, winds and flooding rain to portions of the southeastern United States Friday morning.
Despite the big differences between Rafael and Helene, enough rain could fall on central and southeastern Georgia and the South Carolina Low Country to cause urban-style flooding, small stream ...
The 2013 Southeastern United States floods were ongoing flooding across the southeastern U.S. Flash floods began on the morning of July 2 and continued through Independence Day and into the next day. The hardest-hit areas as of Friday afternoon are the Florida Panhandle , northwest Alabama and the area around Columbus, Mississippi .
•Helene is unleashing a flooding disaster in some areas of the southeastern United States, especially in northern Georgia, upstate South C. Key takeaways:•Life-threatening, damaging and ...
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