File:Affouillement d'un lit marin par de la glace dérivante.png
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editDescriptionAffouillement d'un lit marin par de la glace dérivante.png |
Français : Lorsque la glace flottante atteint des zones peu profondes, sa partie immergée racle le fond marin, provoquant la formation d’un sillon – c’est le phénomène de l’affouillement. English: As an ice feature drifts into shallow waters, it comes into contact with the seabed, and produces a linear gouge while it keeps drifting. |
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Author | Lusilier |
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current | 13:14, 2 November 2012 | ![]() | 754 × 426 (82 KB) | Lusilier (talk | contribs) | User created page with UploadWizard |
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