Bowfell - Topography

Topography

The Southern Fells include the highest ground in England, a horseshoe which begins with Scafell and Scafell Pike in the west and then curves around the north of Upper Eskdale to take in Great End, Esk Pike, Bowfell and Crinkle Crags.

In addition to Eskdale, Bowfell has a footing in two other well known valleys. It stands at the head of Great Langdale — its east ridge dividing the two branches of Mickleden and Oxendale — while to the north is the Langstrath branch of Borrowdale. From all of these valleys Bowfell presents a striking profile with a conical top resting upon a wider summit plateau.

To the north west of Bowfell the main ridge drops to the depression of Ore Gap, named after its reddish soil, rich in haematite. Below the col on the northern side is Angle Tarn. This round waterbody occupies a corrie beneath Hanging Knotts, small trout lurking in its 50 ft depths. Its outflow is a tributary of the Langstrath Beck, making for Stonethwaite. To the south of Ore Gap runs Yeastyrigg Gill, the main headwater of Lingcove Beck, flowing into the fastness of upper Eskdale. Beyond the Gap the ridge makes the stoney three tiered climb to the white rocked summit of Esk Pike.

Southward of Bowfell the ridge falls steeply to Three Tarns, the col separating it from Crinkle Crags. The depression takes its name from a number of small pools, often two, but sometimes more after rain. Busco Sike flowing to the east is the longest feeder of Oxendale Beck in Great Langdale.

Bowfell sends out two subsidiary ridges to the east. The Band is a descending rigg starting from the southern end of the summit plateau. It is this ridge which divides Oxendale from Mickleden, making straight for Stool End Farm on the valley floor. The Band has a minor top about halfway down named White Stones, although most guidebooks do not consider it notable. The second ridge begins at the northern end of the summit plateau and crosses a sharp depression at the head of Rossett Gill to make for Rossett Pike. The continuation of this ridge provides the connection to the Central Fells, forming the northern wall of Great Langdale as it crosses Martcrag Moor, bound for the Langdale Pikes.