Lake District
Tarn Crag
506M
1659FT
About Tarn Crag
Overlooking the dark waters of Easedale Tarn, this rugged fell offers a quieter, more textured alternative to the busier paths of nearby Helm Crag. The ascent from Grasmere reveals a summit plateau defined by rocky outcrops and boggy hollows, providing an intimate perspective on the surrounding Central Fells.
Key Statistics
Rank
410th Highest in Region
Parent Range
Central Fells
Prominence
?
22m
Nearest Town
Elterwater
Geology
You are walking on layers of hardened volcanic ash and rocky debris. These stones were formed by explosive eruptions and the settling of volcanic sands.
Classifications
Find It
OS Grid Reference
NY289075
Latitude
54.4586°N
Longitude
3.0969°W
Did You Know?
- •The name is purely descriptive of its geography; 'Tarn' originates from the Old Norse 'tjörn', meaning a small mountain lake, while 'Crag' refers to the steep, broken cliffs of Borrowdale Volcanic rock that form the hill's eastern face.
- •The summit offers a specific, earned view across the Vale of Grasmere toward the Fairfield Horseshoe, with the distinctive serrated ridge of Helvellyn visible to the north-east beyond the bulk of Seat Sandal.
- •The summit plateau is a complex labyrinth of peat hags and small rock towers, making navigation surprisingly demanding during the thick mists that frequently roll into the Easedale valley from the west.
- •A popular high-level circuit links this summit with nearby Blea Rigg, following the undulating ridge line that separates the Easedale and Far Easedale valleys, keeping the Langdale Pikes in constant view to the south.
- •The ground on the approach from Codale Head has a remarkable ability to remain liquid long after the rest of the Lake District has dried out, often requiring a level of hopscotch usually reserved for school playgrounds.
