Bowfell

To the north-west of Bowfell the main ridge drops to the depression of Ore Gap, named after its reddish soil, rich in haematite.

[1] To the south of Ore Gap runs Yeastyrigg Gill, the main headwater of Lingcove Beck, flowing into the fastness of upper Eskdale.

The predominant rocks on Bowfell are the volcaniclastic sandstones of the Seathwaite Fell Formation, with interbeds of andesite outcropping near the summit.

"[4] Below these faces runs the Climber's Traverse, a narrow path providing a high-level walking route to the summit from the highest point of The Band.

This largely horizontal line contours around beneath many of Bowfell's steeper crags, finally reaching the summit via a rocky route known as the River of Boulders, running parallel to the Great Slab.

Finally on the north- east corner of the summit ridge is Hanging Knotts, a complex series of faces and outcrops looking down upon Angle Tarn.

Equally time-consuming although perhaps more picturesque is the long march up Eskdale from Brotherikeld, gaining the ridge at either Ore Gap or Three Tarns.

The summit can also be reached from the top of Wrynose Pass by following the Right of Way starting close to the Three Shire Stone and heading in a northwesterly direction.