Wetherlam

Wetherlam is a rugged, bulky mass dominating the northern end of the Coniston Fells. It’s a complex fell to explore, featuring dramatic crags and industrial mining scars. The ascent via Wetherlam Edge provides a satisfyingly airy scramble that avoids the crowds of the nearby Old Man of Coniston.

• •The mountain's eastern slopes were a major center for copper mining from the 17th to the 19th centuries, leaving a legacy of deep levels, open stopes, and the impressive Tilberthwaite Gill.
• •The summit plateau is composed of volcanic rock from the Borrowdale Volcanic Group, specifically the Seathwaite Fell Formation, which creates its characteristically craggy and broken appearance.
• •Its name originates from the Old Norse 'vedr' and 'lamb', which translates to 'wether-lamb mountain', indicating its historical importance for grazing castrated rams.
• •While the main summit is clear, the subsidiary top of Birk Fell is notorious for its confusing, undulating terrain that can easily lead tired hikers into a long, unintentional descent toward the wrong valley.
• •The descent toward Tilberthwaite is a notorious knee-shredder, offering a gradient so unrelenting that your joints will likely still be vibrating in protest three days after you have finished the hike.