File:Uvala Veliki-Lubenovac NVelebit Croatia.jpg
Summary
Veliki Lubenovac, length ca. 950 m, altitude ca. 1250 m, <a href="https://en.wikipedia.org/wiki/Croatia" class="extiw" title="en:Croatia">Croatian</a> <a href="https://en.wikipedia.org/wiki/Dinaric_Alps" class="extiw" title="en:Dinaric Alps">Dinaric Alps</a> of the <a href="https://en.wikipedia.org/wiki/National_Park_Sjeverni_Velebit" class="extiw" title="en:National Park Sjeverni Velebit">Northern Velebit National Park</a>. This beautiful, frequently visited area is one of several neighbouring closed karst depressions (<a href="https://en.wikipedia.org/wiki/Uvala_(landform)" class="extiw" title="en:Uvala (landform)">uvala</a>, if >1000 m and developed by both <a href="https://en.wikipedia.org/wiki/Fault_(geology)" class="extiw" title="en:Fault (geology)">tectonics</a> and <a href="https://en.wikipedia.org/wiki/Karst" class="extiw" title="en:Karst">karstification</a>).
Geology: Due to sizes, uvalas probably developed since <a href="https://en.wikipedia.org/wiki/Pliocene" class="extiw" title="en:Pliocene">Pliocene</a>, maybe even earlier by <a href="https://en.wikipedia.org/wiki/Fault_(geology)" class="extiw" title="en:Fault (geology)">faulting</a> and karstification. Due to its altitude the depression was overprinted in <a href="https://en.wikipedia.org/wiki/Glaciation" class="extiw" title="en:Glaciation">glacial</a> and periglacial times (<a href="https://en.wikipedia.org/wiki/Pleistocene" class="extiw" title="en:Pleistocene">Pleistocene</a>). Massive tectonics and karstification karstified the Velebit mountain chain way down, deeply under the Adriatic Sea level (!).
Licensing
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File history
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| Date/Time | Thumbnail | Dimensions | User | Comment | |
|---|---|---|---|---|---|
| current | 06:52, 22 December 2016 | | 1,200 × 895 (999 KB) | 127.0.0.1 (talk) | Veliki Lubenovac, length ca. 950 m, altitude ca. 1250 m, <a href="https://en.wikipedia.org/wiki/Croatia" class="extiw" title="en:Croatia">Croatian</a> <a href="https://en.wikipedia.org/wiki/Dinaric_Alps" class="extiw" title="en:Dinaric Alps">Dinaric Alps</a> of the <a href="https://en.wikipedia.org/wiki/National_Park_Sjeverni_Velebit" class="extiw" title="en:National Park Sjeverni Velebit">Northern Velebit National Park</a>. This beautiful, frequently visited area is one of several neighbouring closed karst depressions (<a href="https://en.wikipedia.org/wiki/Uvala_(landform)" class="extiw" title="en:Uvala (landform)">uvala</a>, if >1000 m and developed by both <a href="https://en.wikipedia.org/wiki/Fault_(geology)" class="extiw" title="en:Fault (geology)">tectonics</a> and <a href="https://en.wikipedia.org/wiki/Karst" class="extiw" title="en:Karst">karstification</a>).<br> Geology: Due to sizes, uvalas probably developed since <a href="https://en.wikipedia.org/wiki/Pliocene" class="extiw" title="en:Pliocene">Pliocene</a>, maybe even earlier by <a href="https://en.wikipedia.org/wiki/Fault_(geology)" class="extiw" title="en:Fault (geology)">faulting</a> and karstification. Due to its altitude the depression was overprinted in <a href="https://en.wikipedia.org/wiki/Glaciation" class="extiw" title="en:Glaciation">glacial</a> and periglacial times (<a href="https://en.wikipedia.org/wiki/Pleistocene" class="extiw" title="en:Pleistocene">Pleistocene</a>). Massive tectonics and karstification karstified the Velebit mountain chain way down, deeply under the Adriatic Sea level (!). |
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