File:Caverne.JPG
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Français : Le calcaire de Rodrigues s'est formé il y a environs 3 millions d'années. C'est probablement le retrait de la mer il y a 1 millions d'année qui a permis au vent de constituer sur le basalte des dunes de sable. A la fin de l'ere glaciaire l'apport de sable s'est arreté. La degradation du carbonate de calcium avec la pluie a constitué le calcaire. Les grottes se sont creusées sous l'action de l'erosion et de l'acidification des pluies |
| Date | sept08 |
| Source | Own work |
| Author | Dunog |
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I, the copyright holder of this work, release this work into the public domain. This applies worldwide. In some countries this may not be legally possible; if so: I grant anyone the right to use this work for any purpose, without any conditions, unless such conditions are required by law. |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 16:50, 10 September 2008 | | 2,048 × 1,055 (217 KB) | Dunog (talk | contribs) | {{Information |Description={{fr|1=caverne de Rodrigues}} |Source=Own work by uploader |Author=Dunog |Date=sept08 |Permission= |other_versions= }} <!--{{ImageUpload|full}}--> Category:Rodrigues |
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