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| Great End | |
|---|---|
| Name | Great End |
| Elevation m | 910 |
| Prominence m | 30 |
| Range | Lake District fells, Western Fells |
| Location | Cumbria, England |
| Grid ref uk | NY217079 |
| Topo | OS Landranger 89, Explorer OL4 |
Great End Great End is a prominent fell in the Lake District of Cumbria, England, forming a dramatic north-facing cliff that overlooks Borrowdale and the eastern end of Seathwaite Tarn. It occupies a key position on the ridge linking Scafell and Pikes in the Western Fells, and is noted for its distinctive granite crags, historical climbing routes, and panoramic views toward Buttermere and Scafell Pike. The fell is a popular objective for walkers and climbers accessing routes from Seathwaite (Borrowdale), Grange, and the Styhead Tarn approach.
Great End stands at about 2,985 feet and marks the northeastern extremity of the high ridge running between Scafell Pike, Scafell, and Windermere-adjacent tops. The mountain presents a steep northern face with a series of broken crags and buttresses above the valley of Borrowdale and the hamlet of Seathwaite (Borrowdale). To the south and southwest, the fell descends via a broad, grassed saddle toward Esk Hause and the upper Borrowdale corries. The eastern slopes fall more gently toward Langdale-side valleys and feature several small tarns, while the western aspects link to the Wasdale drainage system through steep gills and scree.
Great End's crags are formed largely from Ordovician and Borrowdale Volcanic Group rocks, with coarse-grained granophyre and andesite giving rise to the rugged cliff faces favored by climbers. The area displays classic glacial geomorphology, including corrie hollows, morainic ridges, and striated bedrock associated with the last Ice Age glaciation that sculpted much of the Lake District topography. Mineralization in the wider region includes vein-hosted quartz and sporadic lead and copper occurrences historically exploited in nearby Coniston and Keswick mining districts. The natural history of the fell includes montane vegetation assemblages characteristic of upland Cumbria, with dwarf willow and bilberry on thin soils and acid grassland on gentler slopes.
Great End is renowned for both hillwalking and traditional rock climbing. Classic scrambling and walking lines approach via the Corridor Route from Seathwaite (Borrowdale) and the Styhead Tarn-linked ascent from Wasdale Head. The northern crags host numerous winter and summer climbs; notable classic rock routes on the buttresses were pioneered in the early 20th century and contributed to the development of British climbing ethics alongside ascents on Scafell Pike and Castle Rock of Triermain. Climbers also use Great End as part of long ridge traverses connecting Lingmell, Piers Gill, and neighboring peaks. Access for technical routes is frequently affected by seasonal weather patterns influenced by Atlantic frontal systems crossing Cumbria.
The name of the fell derives from early English and Norse influences that shaped much of Lake District toponymy, echoing place-name elements shared with nearby summits and valleys recorded in medieval charters and post-medieval maps. Great End appears on 18th- and 19th-century cartography produced by Ordnance Survey surveyors and is referenced in the writing of celebrated regional authors such as Alfred Wainwright and earlier topographers who cataloged the fells for recreational audiences. The mountain has featured in the history of British mountaineering and local Borrowdale community life, serving as a backdrop to shepherding, seasonal pasture rights, and small-scale resource use that paralleled developments in neighboring districts like Keswick and Coniston.
The upland habitats on and around the fell form part of broader conservation designations covering the Lake District National Park and associated Sites of Special Scientific Interest that aim to protect montane flora, upland breeding birds, and peatland function in the region. Bird species observed include upland specialists recorded across Cumbria and the Northern Pennines, while the plant communities reflect acid, nutrient-poor substrates vulnerable to overgrazing and recreational erosion. Conservation efforts by organizations such as National Trust and local landowners focus on path repair, re-vegetation of eroded areas, and grazing management schemes that align with regional initiatives and agri-environment measures administered in tandem with county-level stakeholders.
Great End is accessible year-round from several well-established trailheads, with popular approaches from Seathwaite (Borrowdale), Seathwaite Tarn car parks, and via the Borrowdale valley network served by local roads connecting Keswick and the west Cumbrian coast. The fell features in many walking itineraries promoted by regional guides and is often included in multi-day tours encompassing Scafell Pike and other high fells. Visitor amenities and safety information are provided through Lake District National Park Authority materials and local outdoor clubs associated with The Fell and Rock Climbing Club and regional mountain rescue services that coordinate emergency response in severe weather. Category:Mountains and hills of the Lake District