Scotland
Geal Charn
766M
2513FT
About Geal Charn
Rising above the Spey Valley near Newtonmore, this rounded heathery peak offers a quiet, expansive experience. Its broad slopes are typical of the Monadh Liath, providing a genuine sense of isolation and clear, commanding views across the strath toward the high northern corries and granite plateaus of the Cairngorms.
Key Statistics
Rank
124th Highest in Region
Parent Range
Data coming soon
Prominence
?
55m
Nearest Town
Newtonmore
Geology
Beneath your boots lies the Glen Banchor Subgroup, made of ancient sands and muds transformed by heat and pressure into tough, layered rocks.
Classifications
Find It
OS Grid Reference
NH702049
Latitude
57.1167°N
Longitude
4.1446°W
Did You Know?
- •Derived from the Scottish Gaelic 'Geal Chàrn', the name translates as 'White Cairn'. This usually refers to the presence of quartzite rocks or the hill's tendency to retain a cap of white snow long after the surrounding glens have thawed.
- •Sitting on the southern fringe of the Monadh Liath—the 'Grey Moors'—this summit acts as a natural grandstand. The view across the Spey Valley is exceptional, directly facing the massive granite giants of the Cairngorms, including the deep cleft of the Lairig Ghru.
- •The approach from Glen Banchor follows the River Calder, a route that avoids the more industrial-scale wind farm developments found elsewhere in this range, preserving a sense of old-fashioned Highland wilderness.
- •On the descent towards Newtonmore, walkers often pass through lower slopes rich in ground-nesting birds such as golden plover and meadow pipits, whose calls are often the only sound on these quiet, wind-swept ridges.
- •Navigating the featureless, rolling plateaus of the Monadh Liath in poor visibility is a notorious test of compass skills; here, a peat hag can easily be mistaken for a mountain, and vice versa.
