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Deuxième étape de la formation d'un upwelling : La couche superieure de la mer s'entasse au large, créant un déséquilibre.
Auteur : Nicolas Raymond
Date : 27 juillet 2005
Logiciel utilisé : Blender
Licence : Creative Commons avec obligation de mentionner l'auteur, les travaux dériver doivent utiliser une licence identique.
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 10:41, 13 December 2005 | | 640 × 480 (49 KB) | Muu-karhu (talk | contribs) |
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