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| Seabed |
| The appearance of the underwater relief is the consequence of tectonic movements, abrasion or erosion which were active several million years ago, in times when certain parts of the seabed were land or the coastal area. Uneven areas on the bottom are constantly reduced by sedimentation of detritus from the land. That process is slow, but constant. |
| Vodice / Dalmatina / Kornati / Adriatica / Tribunj / Pirovac / Primosten / Jezera / Murter / Betina |
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