File:Latmischer Golf und Bafasee Entwicklung.jpg
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Deutsch: Vor etwa 6000 Jahren begann die jüngere sukzessive Aufsedimentierung des westlichen Menderes-Grabens mit Sedimenten aus dem 25000 km² großen Einzugsbereich des Mäanders mit Vorschub eines Mündungsdeltas. Für den Deltavorschub konnten - beginnend in chalkolitischer Zeit - verschiedene Verlandungsstadien - u. a. auch die Abschnürung des Bafa Gölü - nachgewiesen werden. |
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| Source | Own work |
| Author | Volker Höhfeld |
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 10:22, 10 August 2020 | | 2,834 × 3,282 (931 KB) | Volker Höhfeld (talk | contribs) | Uploaded own work with UploadWizard |
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