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Description The genesis of an ocean: In plate tectonics, the formation of an ocean starts with a rifting process in the crust as a result of mantle convection. An example of this is the African Rift Valley. In the next stage, the valley has opened up until sea water enters; a good example is the Red Sea. The spreading process continues, the ocean becomes wider and forms a mature ocean like the Atlantic.
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Author Hannes Grobe, Alfred Wegener Institute for Polar and Marine Research
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inception

20 June 2007

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Date/TimeThumbnailDimensionsUserComment
current21:29, 29 October 2007Thumbnail for version as of 21:29, 29 October 20071,614 × 2,312 (301 KB)Hgrobe{{Information |Description=to be done |Source=own work |Date=2007-08-31 |Author=~~~~ |Permission=Own work, share alike, attribution required (Creative Commons CC-BY-SA-2.5) |other_versions= }} {{self|cc-by-sa-2.5}}
08:59, 23 June 2007Thumbnail for version as of 08:59, 23 June 2007806 × 1,155 (131 KB)Hgrobe{{Information |Description=to be defined |Source=own work |Date=2007-06-20 |Author=~~~~, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany |Permission=Own work, share alike, attribution required (Creative Commons CC-BY-SA-2.5) |
19:13, 20 June 2007Thumbnail for version as of 19:13, 20 June 2007806 × 1,155 (131 KB)Hgrobe{{Information |Description=to be defined |Source=own work |Date=2007-06-20 |Author=~~~~, Alfred Wegener Institute for Polar and Marine Research, Bremerhaven, Germany |Permission=Own work, share alike, attribution required (Creative Commons CC-BY-SA-2.5) |

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