Lingmell

Although standing in the shadow of its taller parent, Lingmell is very much a separate entity. In the manner of many fells it displays two contrasting aspects. The southern and western slopes– although steep– are smooth and rounded, while the northern and eastern faces fall as crags directly from the summit. The northern crag drops for a thousand feet toward the valley floor, with a further thousand feet of scree below.

The connection to Scafell Pike is via Lingmell Col, a grassy depression at 2,410 ft. Flowing west from the col is Lingmell Gill, descending through Hollow Stones to Brackenclose at the head of Wast Water. To the east of Lingmell Col runs Piers Gill, a stream descending from high on the Scafells. This flows right around the northern perimeter of Lingmell, finally entering Wast Water as Lingmell Beck, only a short distance from the entry point of Lingmell Gill. These two streams which girdle the fell both run through wide boulder strewn courses, evidence of flash flooding and the endless fall of rocks from the upper slopes. Lingmell sends out a long shoulder westward between the two streams. The southern face of this, riven with scree on its slow tumbling journey into Lingmell Gill is named Lingmell Scars. At the top of the shoulder are the many outcrops of Goat Crags.