Why this matters
Macfarquhar's Bed is a sea cliff composed of sedimentary rock, likely of Carboniferous or Devonian age. It formed through the deposition and lithification of marine sediments, later exposed by coastal erosion; it is notable for its geological continuity with other formations in the Scottish Highlands.
What is recorded here
Macfarquhar's Bed is shown as a cliff on the public map of Highland. The saved point is the map point or the centre of its mapped shape.
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