The so-called “storm of the century” hits the eastern part of the United States, killing hundreds and causing millions of dollars in damages, on November 25, 1950.
Also known as the “Appalachian Storm,” it dumped record amounts of snow in parts of the Appalachian Mountains. Forming over North Carolina just before Thanksgiving, the storm quickly moved north, striking western Pennsylvania, eastern Ohio, and West Virginia.
These areas were blanketed with several feet of snow for several days and travel was impossible for nearly a week in some places. An accompanying windstorm covered a far greater area.
New York City recorded a 94 mile-per-hour wind gust. At Bear Mountain, just north of the city, a 140 mph gust was recorded. The winds throughout New England were of hurricane-like force. In addition, high tides and wind-driven surf battered the coastline.
On the south edge of the storm, record low temperatures were recorded in Tennessee and North Carolina even without the wind chill. In Mount Mitchell, North Carolina, a temperature of 26 degrees below zero was recorded. The storm was unique, however, because it featured not only extremely strong winds and heavy snow but both record high and low temperatures.
In Pittsburgh, 30 inches of snow fell in a blinding snowstorm. Further north, Buffalo saw no snow, but experienced 50 mile-per-hour winds and 50-degree temperatures. Paul Kocin, a Weather Channel expert, has said that this storm “had the greatest contrast of weather elements in probably any storm, including the 1993 March Superstorm.” The extreme weather was deemed responsible for the loss of 160 lives over several days.