Why this matters
Eaves Crag is a sandstone sea cliff or coastal rock feature, likely formed during the Permian period, around 250 to 300 million years ago, through the deposition and lithification of aeolian (wind-blown) sands in a desert environment. It is notable as part of the Pennine Dialects of the Pennines and as a local landmark in the Bradford area.
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Eaves Crag is shown as a cliff on the public map of Bradford. The saved point is the map point or the centre of its mapped shape.
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