The imposing north-eastern cliffs, riven by gullies, rise some 600 ft from the Esk Hause path. Their orientation ensures that the sun rarely reaches them, the gullies often retaining snow well into the spring. From the left when viewed from below the principal fissures are South East Gully, Central Gully and Cust's Gully (see below). To the west of the cliffs a ridge descends more gradually in the general direction of Sty Head. This is known as The Band, and it too sports a harsh gash across its features. On the western side of The Band is the deep ravine of Skew Gill, a tributary of Wasdale-bound Lingmell Beck. At the base of The Band the ridge continues as the complex top of Seathwaite Fell, replete with numerous tarns. The largest is Sprinkling Tarn with its beautifully indented shoreline providing perfect foreground for views of the cliff.