Why this matters
Arnison Crag rises to approximately 250 metres and is composed primarily of Carboniferous limestone. It is a minor but distinctive craggy outcrop in a landscape shaped by glacial activity, and while lacking prominent folklore, it contributes to the regional character of the Lake District foothills.
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Arnison Crag is shown as a mountain / peak on the public map of Westmorland and Furness. The saved point is the map point or the centre of its mapped shape.
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