A localised phase of folding and faulting took place in West Spitsbergen in Palaeogene time (around 50-60 million years ago). Here is an overturned fold affecting Carboniferous rocks in the cliffs of Zeppelinfjellet. |
A localised phase of folding and faulting took place in West Spitsbergen in Palaeogene time (around 50-60 million years ago). Here is an overturned fold affecting Carboniferous rocks in the cliffs of Zeppelinfjellet. |