Conival

About Conival

Often overshadowed by its neighbour Ben More Assynt, this Munro offers a rugged, quartzite-strewn ascent from Inchnadamph. The climb follows the River Traligill before steepening onto a high, shattered ridge. Reaching the summit reveals a landscape of stark white rock and the vast, ancient moorland characteristic of the far north.

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Did You Know?

• •The name Conival is an anglicisation of the Gaelic Cona Mheall. While Mheall refers to a rounded hill, Cona likely stems from choinneamh, meaning 'meeting,' marking the peak's role as the junction for three significant ridges.
• •The mountain is largely composed of Cambrian quartzite. This bright white rock gives the upper slopes an icy appearance even in summer, but it creates a notoriously abrasive and unstable surface that is hard on both boots and knees.
• •The standard approach from the west follows the River Traligill, passing a series of impressive limestone swallow-holes where the water vanishes underground into Scotland’s largest cave system.
• •From the summit, the view west provides an exceptional profile of Suilven’s distinctive 'sugar loaf' shape and the long spine of Quinag, both of which appear to float above the maze of small lochans in the Assynt wilderness.
• •Despite its status as a distinct Munro, Conival is often regarded by walkers as a mandatory hurdle on the route to Ben More Assynt—a reputation the mountain defends by way of a particularly punishing final scree slope.