Dale Head - Topography

Topography

The North Western Fells occupy the area between the rivers Derwent and Cocker, a broadly oval swathe of hilly country, elongated on a north-south axis. Two roads cross from east to west, dividing the fells into three convenient groups. Dale Head is the highest fell in the southern sector.

Dale Head is the apex of two hill ridges. The principal ridge descends from Dale Head to the north-east and forms several other fells, each given a chapter by Alfred Wainwright in his Pictorial Guides to the Lakeland Fells. These are High Spy, Maiden Moor and Catbells (alternative spelling, Cat Bells). This ridge forms the western side of Borrowdale and overlooks Derwent Water. The other ridge descends to the north-west and includes the fells of Hindscarth and Robinson; it overlooks Gatescarthdale and Buttermere.

Dale Head is named for its position at the head of the Newlands Valley. This stretches away due north for three and a half miles before debouching into the floodplain of the Derwent between Derwentwater and Bassenthwaite Lake. The eastern wall of the valley is formed by the High Spy to Catbells ridge, separating it from Borrowdale. Entering on the western side are a series of side valleys which drain the main mass of the North Western Fells. The source of Newlands Beck does not however flow from the apex of Dale Head as might be supposed from the name. Instead it has its birth at the col between the main summit and the eastern top, High Scawdel (1,815 ft). The northern face of the fell forming the dalehead is ringed with crags. The main faces are Dalehead Crags and Great Gable, not to be confused with the fell of that name.

The southern flank of the fell running down to the summit of the Honister Pass road (1,180 ft) has much gentler slopes, although there is outcropping rock on either side. Buckstone Hows and Yew Crag overshadow the road.From the top of the pass Gatesgarthdale Beck runs north west to Buttermere while Hause Gill flows east to Seatoller and Borrowdale. Across the road is Grey Knotts in the Western Fells.

The ridge to Hindscarth departs north west from the summit of Dale Head, soon narrowing into the fine and airy Hindscarth Edge. Both slopes are rocky, that to the south being known as Molds. Far Tongue Gill descends from the north of the ridge, a tributary of Newlands Beck.

Although High Scawdel stands east of the main summit, the high ground takes a great loop to the south around the head of Newlands Beck. It then drives north to the depression at Wilson's Bield (1,655 ft) before climbing to the summit of High Spy. The rest of the North Western Fells bear no tarns worthy of the name, but Dale Head has two. On the northern slope near the source of Newlands Beck is Dalehead Tarn, while the smaller Launchy Tarn lies near the top of High Scawdel. Dalehead Tarn is a shallow pool providing a popular stopping place for walkers. Its varied flora include water horsetail, sedge and bogbean. Launchy Tarn is smaller and may have been formed by overgrazing and erosion of the underlying peat.