Tidal bore



         


A tidal bore (or just bore) is a tidal phenomenon in which the leading edge of the incoming tide forms a wave (or waves) of water that travel up a river against the direction of the current. As such, it is a true tidal wave.

A bore occurs in a relatively few locations worldwide, in areas with a large tidal range, only on certain tides, and when an incoming tide is funnelled into a shallow, narrowing river via a broad bay. A bore is a natural example of a self-reinforcing solitary wave or soliton. Larger bores can be particularly dangerous for shipping, but also present a challenge to surfers.

The word bore derives through Old English from the Old Norse word bara, meaning a wave or swell.

Rivers that exhibit a bore include:

[Top]

Asia

[Top]

South America

[Top]

North America

[Top]

Europe







  View Live Article   This article is from Wikipedia. All text is available under the terms of the GNU Free Documentation License