English: Ravni Dabar, length ca. 6500 m (650 m the fertile uvala floor only) (3 uvalas forming one large depression), altitude ca. 750 m, CroatianDinaric Alps. This beautiful area, frequently visited by sportive rock climbers, together with the neighbouring Crni Dabar and Dosen Dabar, forms the large closed karst depression (in this case 3 uvalas).
Geology: Due to sizes, uvalas probably developed since Pliocene, maybe even earlier by both, faulting and karstification. Massive tectonics and karstification karstified the Velebit mountain chain way down, deeply under the Adriatic Sea level (!).
Deutsch: Ravni Dabar, ca. 6500 m lang (650 m nur der sichtbare, fruchtbare Beckenboden) (3 Uvalas bilden eine Depression), in ca. 750 m über NN, KroatischeDinariden. Diese vielbesuchte Gegend des Velebit ist eine der drei benachbarten Uvalas (die anderen sind Crni Dol und Dosen Dabar), die zusammen eine recht große abflusslose Karstdepression bilden ).
Geologisch: Wegen seiner geologischen Beschaffenheit und Größe wahrscheinlich schon im Pliozän oder noch früher an der Bruchzone starker Verwerfungen und durch Verkarstung allmählich entstanden. Tektonik und Wasserlöslichkeit des Karbonatgesteins der Dinariden haben im Velebit eine Verkarstungstiefe bis weit unter Meereshöhe (!) bewirkt.
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Image title
Uvala, Ravni Dabar, Velebit, Croatia.
The floor and the mountains form a huge closed karst depression, the perimeter of which extends beyond the horizon and the back, including 2 other uvalas: Dosen Dabar and Crni Dabar.