Esk Pike

To the north-west of Esk Pike is the depression of Esk Hause, a broad saddle carrying a number of important paths. The ‘true’ Esk Hause—so named by Alfred Wainwright in his influential Pictorial Guide to the Lakeland Fells—is the north–south route from Borrowdale to Eskdale. A lower path—the ‘false’ Hause—runs east–west from Langdale to Wasdale, passing a stone windshelter. There are also paths climbing to the summits of Esk Pike and Allen Crags, together with the popular Calf Cove route to Scafell Pike, all contributing to make Esk Hause a confusing place in mist. The source of the main branch of the Esk flows south from the Hause, while to the north the topography is more complex. Allen Crags stands adrift from the main ridge, with the valleys of Langstrath and Grains Gill falling on either side. These combine some miles downstream to form the River Derwent, flowing through Borrowdale to Derwentwater and Keswick.

South-east of the summit of Esk Pike is Ore Gap, the col separating it from Bow Fell. The soil here is red due to haematite, and climbing lore suggests that magnetic compasses cannot be trusted in this locality.[1] North of the gap is Angle Tarn, a feeder of the Langstrath. This round tarn occupies a corrie beneath Hanging Knotts, small trout lurking in its 50-foot depths.[2]

Southward from the summit, Esk Pike throws out a long descending ridge into the uninhabited fastness of Upper Eskdale. This divides the Esk from its major upper tributary, Lingcove Beck, which has its beginnings at Ore Gap. Two miles in length, this ridge falls over a series of craggy steps to the confluence of the two streams at Lingcove Bridge. An old Packhorse Bridge, this is a focal point for those approaching from the south, particularly when the Esk is in spate. The south ridge has a number of subsidiary tops which are recognised by some guidebooks,[3] the principal summits being Pike de Bield (2,657 ft / 810 m.), Scar Lathing (1,440 ft / 439 m.) and Throstlehow Crag (1,325 ft / 404 m.). Scar Lathing is particularly impressive, presenting sheer cliffs above a bend in the Esk. Although of minor significance Pianet Knott on the eastern side of the ridge also has a very striking appearance from lower down the valley.