File:Affouillement d'un lit marin par de la glace dérivante.png
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Affouillement_d'un_lit_marin_par_de_la_glace_dérivante.png (754 × 426 pixels, file size: 82 KB, MIME type: image/png)
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Summary[edit]
DescriptionAffouillement 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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Source | Own work |
Author | Lusilier |
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Date/Time | Thumbnail | Dimensions | User | Comment | |
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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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