Description

According to an older theory of continental drift, the Eurasian and North American continental plates shift and grind together in an endless clash of subterranean forces under a gaping rift at the tip of the Reykjanes peninsula in southwest Iceland. Bjarnagjá is an 18m deep lava ravine on this very peninsula where the tectonic activity has caused Iceland to rise out of the ocean. The water in Bjarnagjá is mostly fresh groundwater but it is influenced by the salinity of the sea as the rift is o…

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