Lake District
Whitegill Crag
472M
1549FT
About Whitegill Crag
Rising steeply above the floor of Great Langdale, this rugged outcrop offers a quieter alternative to the busy paths of the Langdale Pikes. While modest in height, its position provides a front-row seat to the dramatic rock architecture of Pavey Ark and the winding path of the Mickleden valley below.
Key Statistics
Rank
474th Highest in Region
Parent Range
Central Fells
Prominence
?
5m
Nearest Town
Chapel Stile
Geology
The ground beneath you is made of hardened volcanic ash and stony debris. These layers formed from explosive eruptions that deposited thick blankets of volcanic dust and sandstone.
Classifications
Find It
OS Grid Reference
NY297072
Latitude
54.4558°N
Longitude
3.0846°W
Did You Know?
- •The name is derived from the Old Norse 'gil', referring to the narrow, steep-sided ravine of White Gill that cuts deep into the fellside immediately to the west of the summit.
- •Classified as a Synge, the summit is often gained via a stiff climb from the valley floor near Millbeck, serving as a dramatic gateway to the undulating plateau of the Central Fells.
- •The crag provides an exceptional vantage point for studying the Langdale Pikes; the massive face of Pavey Ark and the distinct 'thimbles' of Harrison Stickle appear remarkably close across the gap of the gill.
- •Geologically, the fell is composed of hard volcanic rhyolite, which forms the clean, steep tiers that have made the crag a respected destination for Lakeland rock climbers for decades.
- •It offers the rare satisfaction of feeling like you are hanging directly over the valley floor, though the proximity to the pubs below means the smell of chips occasionally drifts up to the summit on a southerly breeze.