File:Vrulja kod Omiša.jpg

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Summary

Submarine <a href="https://en.wikipedia.org/wiki/Karst_spring" class="extiw" title="en:Karst spring">karst spring</a>, emerging <a href="https://en.wikipedia.org/wiki/Fresh_water" class="extiw" title="en:Fresh water">fresh water</a> in the <a href="https://en.wikipedia.org/wiki/Adriatic_Sea" class="extiw" title="en:Adriatic Sea">Adriatic Sea</a>. "Vrulja Bay", South <a href="https://en.wikipedia.org/wiki/Croatia" class="extiw" title="en:Croatia">Croatia</a>.
4,5km N of <a href="https://en.wikipedia.org/wiki/Brela" class="extiw" title="en:Brela">Brela</a>, half way between <a href="https://en.wikipedia.org/wiki/Omi%C5%A1" class="extiw" title="en:Omiš">Omiš</a> and <a href="https://en.wikipedia.org/wiki/Makarska" class="extiw" title="en:Makarska">Makarska</a>.
Submarine, because the sea's water level rose by ca. 120 m since late <a href="https://en.wikipedia.org/wiki/Pleistocene" class="extiw" title="en:Pleistocene">Pleistocene</a> (<a href="https://en.wikipedia.org/wiki/Last_glacial_period" class="extiw" title="en:Last glacial period">last glacial period</a>, 25ka) and karstification of the <a href="https://en.wikipedia.org/wiki/Biokovo" class="extiw" title="en:Biokovo">Biokovo</a> mountains continues to an even lower level.

Licensing

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File history

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Date/TimeThumbnailDimensionsUserComment
current02:53, 4 January 2017Thumbnail for version as of 02:53, 4 January 20171,200 × 900 (823 KB)127.0.0.1 (talk)<p>Submarine <a href="https://en.wikipedia.org/wiki/Karst_spring" class="extiw" title="en:Karst spring">karst spring</a>, emerging <a href="https://en.wikipedia.org/wiki/Fresh_water" class="extiw" title="en:Fresh water">fresh water</a> in the <a href="https://en.wikipedia.org/wiki/Adriatic_Sea" class="extiw" title="en:Adriatic Sea">Adriatic Sea</a>. "Vrulja Bay", South <a href="https://en.wikipedia.org/wiki/Croatia" class="extiw" title="en:Croatia">Croatia</a>.<br> 4,5km N of <a href="https://en.wikipedia.org/wiki/Brela" class="extiw" title="en:Brela">Brela</a>, half way between <a href="https://en.wikipedia.org/wiki/Omi%C5%A1" class="extiw" title="en:Omiš">Omiš</a> and <a href="https://en.wikipedia.org/wiki/Makarska" class="extiw" title="en:Makarska">Makarska</a>.<br> Submarine, because the sea's water level rose by ca. 120 m since late <a href="https://en.wikipedia.org/wiki/Pleistocene" class="extiw" title="en:Pleistocene">Pleistocene</a> (<a href="https://en.wikipedia.org/wiki/Last_glacial_period" class="extiw" title="en:Last glacial period">last glacial period</a>, 25ka) and karstification of the <a href="https://en.wikipedia.org/wiki/Biokovo" class="extiw" title="en:Biokovo">Biokovo</a> mountains continues to an even lower level. </p>
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