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Virginia Water Safety Coalition Water Safety Resource Kit |
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What is a Rip Current? No matter how a rip current is formed, the effect is the same. A large amount of water at the shoreline rushes in a narrow path back to the sea. This path of water can extend as far as 3000 feet offshore, reach 90 feet in width, and travel up to four feet per second. Rip currents, sometimes incorrectly called undertows, do not pull swimmers under the water, but can pull even experienced swimmer away from shore. A rip current is formed when water that usually moves along the shore rushes out to sea in a narrow path. This can happen where (1) there is a break in an offshore sandbar, (2) the longshore current is diverted by a groin, pier, or jetty, or (3) longshore currents moving in opposite directions meet (click to view pictures) Signs of a Rip Current Stand on a high area, such as a sand dune or deck, and scan the water. To spot a rip current, look for the following characteristics:
What to do? (click to view image)
*Published courtesy of North Carolina Sea Grant, North Carolina State University, P.O. Box 8605, Raleigh, North Carolina 27695-8605, (919) 515-2454 |
This site maintained
by Meg Becker
for the Water Safety Coalition.
Last updated on April 26, 2001