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hyperpycnal inflow |
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hyperpycnal inflow [¦hī·pər¦pik·nəl ′in‚flō] (hydrology) A denser inflow that occurs when a sediment-laden fluid flows down the side of a basin and along the bottom as a turbidity current. How to thank TFD for its existence? Tell a friend about us, add a link to this page, add the site to iGoogle, or visit webmaster's page for free fun content. |
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