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Tidal bore

From Biocrawler, the free encyclopedia.

The tidal bore in. Upper , Alaska
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The tidal bore in. Upper Cook Inlet, Alaska

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 (not to be confused with a tsunami).

Bores occur 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. Bores take on various forms, ranging from a single breaking wavefront - effectively a shock wave - to 'undular bores' comprising a smooth wavefront followed by a train of solitary waves (solitons). 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 have been known to exhibit bores include:

Asia

South America

  • Amazon River, up to 4m (12 feet) high, running at up to 25 km per hour (15 miles per hour). It is known locally as the pororoca.

North America

Tidal bore on the Petitcodiac River
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Tidal bore on the Petitcodiac River

Europe

Oceania

Wikipedia (http://en.wikipedia.org/wiki/Main_Page) Tidal_bore (http://en.wikipedia.org/wiki/Tidal_bore) version history (http://en.wikipedia.org/w/index.php?title=Tidal_bore&action=history) GNU Free Documentation Lizenz (http://en.wikipedia.org/wiki/Wikipedia:Text_of_the_GNU_Free_Documentation_License) CC-by-sa (http://creativecommons.org/licenses/by-sa/2.5/)

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