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Orkney geology
Orkney
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Orkney Landscapes
The Orkney islands lie just to the north of
Scottish Mainland, exposed to the full force of the Atlantic weather. This
site looks at the physical landscape of the islands, the backdrop for
enthralling natural, historical and cultural landscapes celebrated widely in
song and verse. The geology is dominated by the Old Red Sandstone and the
archipelago gives its name to Lake Orcadie, a vast former lake basin dating
from around 380 million years ago. The hundreds of metres of sediment laid
down on its floor point to rhythmic climate shifts, with dunes and mud cracks
forming during arid phases. Mass mortality of shoals of primitive fish left
superb fossil remains. The record of desert and flood, volcanoes and
continental tectonics is inscribed in the stacked layers of sandstone forming the coastal cliffs.
The scenic framework certainly deserves attention. Controversy rumbles over the timing, pattern and
effects of glaciation on the islands. The hill tops of Hoy display both fossil
and active frost-generated features, landforms and sediments reminiscent of
much more elevated Scottish mountain tops and of the Arctic lowlands. Orkney also one of the
most active coastlines in the British Isles where a combination of sea level
change, rapid erosion and localised deposition has created shorelines of
immense variety, character and interest. The islands have been inhabited for
at least 7000 years, an occupation that has brought
profound changes in soils, vegetation and, increasingly, the landforms
themselves.
New paper on the last glaciers on Hoy |