Whinlatter

Whinlatter is a small fell in the Lake District’s north-western sector, just north of Whinlatter Pass. The hill rises between the pass and the Vale of Embleton, forming part of a horseshoe around Aiken Beck’s valley. Its name comes from Old Norse and Gaelic, meaning ‘the gorse-covered slope’. The fell sits in the most northerly group of fells between the rivers Derwent and Cocker. Lord’s Seat, the highest point north of the pass, sends out a ridge that curves westward to become Whinlatter. The fell’s slopes are largely covered by Forestry England plantations, with conifer stands changing as trees are harvested and replanted. Thornthwaite Forest occupies the ridge line and flanks from Ullister Hill to Tarbarrel Moss, while Brown How’s lower slopes also lie within the forest. Aiken Beck’s quiet valley lies to the north, hidden between Brown How and Graystones, while Whinlatter Beck flows westward beneath the fell’s steepest face. The fell’s geology includes rocks of the Loweswater Formation, made up of greywacke sandstone turbidites. Visitors find a windshelter on Brown How and a modest cairn at Whinlatter Top. Views from the summit are limited close-up, showing Hopegill Head and Grisedale Pike across the pass. To the north, the Solway Firth and Scottish mountains appear, best seen from Brown How. Marked trails wind through the woodland, offering routes from the pass or Aiken Beck’s circuit. The fell’s quieter paths contrast with the busier routes around Lord’s Seat and Graystones.