File:Veliki-Lubenovac Uvala NatPark-NVelebit Dinarides Croatia 3.jpg

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English: Veliki Lubenovac, length ca. 0,95km, altitude ca. 1,25km, croatian Dinaric Alps of the Northern Velebit National Park. This beautifull, frequently visited area is one of several neighbouring closed karst depressions (uvala, if >1km and developed by both tectonics and karstification).
Geology: Due to sizes, uvalas probably developed since Pliocene, maybe even earlier by faulting and karstification. Due to its altitude the depression was overprinted in glacial and periglacial times (Pleistocene). Massive tectonics and karstification karstified the Velebit mountain chain way down, deeply under the adriatic see level (!).
Deutsch: Veliki Lubenovac, ca. 0,95km lang, in ca. 1,25km über NN, kroatische Dinariden im Nationalpark Nationalpark Nördlicher Velebit. Diese vielbesuchte, weil schöne Gegend des Velebit ist eine von mehreren, benachbarten, allseits geschlossenen Karstdepressionen (Uvala, wenn größer als ca.1km und durch Verkarstung und auch durch Tektonik entstanden).
Geologisch: Wegen seiner geologischen Beschaffenheit und Größe wahrscheinlich schon im Pliozän oder noch früher an der Bruchzone starker Verwerfungen und durch Verkarstung allmählich entstanden. Wegen der Höhenlage in den Eiszeiten des Pleistozäns glazial und periglazial überprägt. Tektonik und Wasserlöslichkeit des Karbonatgesteins der Dinariden haben im Velebit eine Verkarstungstiefe bis weit unter Meereshöhe (!) bewirkt.
Date Unknown date
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?; May, 19th, 2014 (upload)
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Author LeonardoDj
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