Wild Boar Fell - Geography

Geography

Wild Boar Fell is a dramatic sight and a landmark for many miles around. Approached from the north it gives the misleading impression that it is a peak (see photo, above left). But from the south of the dale at Aisgill its true profile is seen, not dissimilar to Ingleborough, with steep sides and a flat top (consisting of a cap of millstone grit).

The classic route for walking up Wild Boar is via the bridle way from Hazelgill Farm, ascending west to High Dophinsty before following Scriddles ridge top to Blackbed Scar. Once there you are on Wild Boar Fell's table top plateau, a rather boggy expanse. The summit is marked by a trig point and Sand Tarn is about 300 m (1,000 ft) to the west, just below the summit.

The views from the top make a spectacular panorama. The Howgills, Pennines, the Lake district fells, the Yorkshire Three Peaks can all be seen and, on a clear day, there is even a glimpse of the sea at Morecambe Bay.

A common feature of many Pennine dales and Lake District fells are the groups of cairns on the high ground. There is a fine cluster of "stone men" on The Nab of Wild Boar Fell - and a smaller group on subsidiary peak, Little Fell (559 m, 1834 ft) at grid reference NY766008, 2 km to the north. There seems little agreement on when, why, or by which people such cairns were built. (One common suggestion, that they were built by shepherds as markers for paths, may explain some of the cruder "piles of stones"; but groups like those on The Nab surely need a more convincing explanation).