North Pennines
Hooksey
586M
1923FT
About Hooksey
Overlooking the deep troughs of Weasdale and Bowderdale, this quintessential Howgill fell offers smooth, steep gradients and reliable underfoot turf. While often overshadowed by higher neighbours, it serves as a panoramic gateway to the northern fells, providing a clear perspective on the long, velvet ridges leading toward The Calf.
Key Statistics
Rank
109th Highest in Region
Parent Range
Yorkshire Dales
Prominence
?
69m
Nearest Town
Westmorland and Furness
Geology
The ground here is formed from layers of sandstone, siltstone, and mudstone. These rocks belong to the Coniston Group and create Hooksey’s rugged landscape.
Find It
OS Grid Reference
NY685008
Latitude
54.4017°N
Longitude
2.4867°W
Did You Know?
- •The name likely stems from the Old Norse 'hōc', meaning a hook or bend, referring to the distinct curve of the ridge that separates the valleys of Weasdale and Bowderdale.
- •The ascent from the north follows a narrow spine between two perfectly glacial U-shaped valleys, offering an approach that remains remarkably quiet even during peak walking season.
- •Looking south-west, the view is dominated by the steep, fluted eastern face of Randygill Top, providing one of the best angles to appreciate the 'sleeping elephant' terrain characteristic of the Howgill Fells.
- •Hooksey sits just 14 metres shy of the 600-metre mark, a height deficit that ensures it remains a peaceful outlier compared to the more frequented 'Hewitt' summits nearby.
