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Underwater Channel Swell |
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Underwater Channel Swell
a narrow ridge extending along the channel of an underwater valley. The length can be from several kilometers to several dozens of kilometers; the height is 5-10 to 20-30 m. The swell is usually composed of silty-sandy material and forms as a result of sediments deposited by lee currents flowing along underwater valleys. Want to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit the webmaster's page for free fun content. |
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