File:Uvala-Mirovo NVelebit Dinarides Croatia.jpg

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English: Dundović Mirovo, length ca. 2km, altitude ca. 1,35km, 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).
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) as published research results of this and two neighbouring depressions 2011 confirmed. Massive tectonics and karstification karstified the Velebit mountain chain way down, deeply under the adriatic see level (!).
Deutsch: Dundović Mirovo, ca. 2km lang, in ca. 1,35km 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 >1km groß). Die Viehhaltung in den Steinumgrenzungen wurde aufgegeben.

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. Relikte der Gletscherarbeit wurden hier und in den beachbarten Depressionen Bilensko Mirovo und Tudorevo nachgewiesen (Publikation von 2011).

Tektonik und Wasserlöslichkeit des Karbonatgesteins der Dinariden haben im Velebit eine Verkarstungstiefe bis weit unter Meereshöhe (!) bewirkt.
Date October 2006; June 20th, 2014 (upload)
Source see author
Author Mountainman-69
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(Reusing this file)		 Explicit permission by author's email of May, 22nd, 22013

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