Scandale Fell
Topography
When viewed from the south around High Sweden bridge near Ambleside, High Pike has the look of a remote peak standing alone with cliffs falling away from the summit on its eastern side. However, in reality it is just a slight rise on the long southern ridge of Dove Crag with only about five metres of prominence which prevents it even qualifying as a “Nuttall”; nevertheless both Alfred Wainwright and Bill Birkett mention the fell in their books on the Lakeland Fells.
Geology
The crest of the ridge consists of the volcaniclastic laminated claystone and siltstone of the Esk Pike Formation. Beneath is the dacitic welded lapilli-tuff of the Lincomb Tarns Formation.
Ascents
High Pike is often climbed as part of the Fairfield horseshoe walk. The ascent from Ambleside leaves the centre of the town northerly and goes by Low Sweden Bridge to reach the open fell where a sizeable dry stone wall is followed firstly over Low Pike and then down to a depression at 480 m (1,570 ft) before climbing to the flat grassy summit of High Pike with its cairn standing on the edge of crags overlooking Scandale.
Summit
Much of the view from the top is curtailed by higher fells but there is a view of the Far Eastern Fells over the Scandale Pass and an excellent view of Ambleside and the head of Windermere.
References
- ^ British Geological Survey: 1:50,000 series maps, England & Wales Sheet 38: BGS (1998)
- A Pictorial Guide to the Lakeland Fells, Eastern Fells, Alfred Wainwright, ISBN 0-7112-2454-4
- Complete Lakeland Fells, Bill Birkett, ISBN 0-00-713629-3