High Stile, Buttermere, Coast to Coast
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Nearing the summit of High Stile
High Stile above Ennerdale - Coast to Coast
High Stile, at 806 m, is the highest point on the High Stile Ridge, which stretches from Great Borne to Haystacks. Its summit qualifies as a Marilyn, offering commanding views over Ennerdale Valley to the south and Buttermere to the north-west. Below its southern face flows the River Liza, with the Coast to Coast path tracing the forested valley floor.
High Stile can be reached via the ridge from either end, or more directly — from High Gillerthwaite in Ennerdale (via Red Pike), or through Burtness Wood on the south shore of Buttermere.
Coast to Coast walkers taking the ridge as an alternative to the forest route typically ascend to Red Pike, then continue east over High Stile, High Crag, and Seat, descending to Scarth Gap beneath Haystacks to rejoin the main route.
High Stile and Dodd
From Gatesgarth, the broad sweep of High Stile is on full display, its towering northern face descending steeply to the valley floor. To its left rises the rounded shoulder of Dodd, an outlier that adds bulk to the mountain’s presence above Buttermere. The white glint of Comb Beck can just be seen tumbling from the hidden heights, vanishing behind a long boundary wall that cuts a stark diagonal across the lower slopes. Together, these features form one of the finest Lakeland prospects — especially in morning light, when shadow and contrast reveal every fold of the fellside.
High Stile Route via Bleaberry Tarn
High Stile is usually reached via Red Pike, following the ridge from Ennerdale Valley. A popular alternative starts from Buttermere, where a stepped path ascends through Old Burtness Wood, beside Sourmilk Gill, to reach Bleaberry Tarn. From there, the route climbs to The Saddle and joins the ridge at Red Pike, before continuing east to High Stile. Viewed from the Bleaberry Tarn path, the steepness of the northern face is striking — a reminder of the fell’s imposing presence above Buttermere.
High Stile & Dodd From Buttermere
From Buttermere’s southern shore, Dodd stands prominently in the foreground, backed to the south-east by the imposing bulk of High Stile. The north flanks of High Stile descend steeply into the dense sweep of Burtness Wood, which carpets the lower slopes and spills out onto the meadow-fringed edge of the lake. The route to Bleaberry Tarn climbs through this woodland, tracing a path toward the heights above.
Comb Beck, High Stile, High Crag
Comb Beck descends steeply from the rugged corrie between High Stile and High Crag, its shallow waters twisting over stone as they begin their fall toward Buttermere. To the west, the beck is flanked by the eastern slopes of High Stile; to the east, by the craggy face of High Crag Buttress. Against a deep blue sky, the beck gleams as it flows from the heights of Burtness Comb.
High Stile Path From Red Pike
The path from Red Pike to High Stile traces the ridge above the steep north-facing Chapel Crags corrie, which plunges toward Bleaberry Tarn. In contrast, the remnants of an old fence follow the more sheltered southern flank. At 807 m, High Stile is the tallest peak on the ridge and a Wainwright. An alternative descent drops north-west from the summit via a rugged spur between Eagle Crag and Grey Crag, leading steeply down to Buttermere. In mist, the summit dome — strewn with stones — emerges quietly from the haze.
Chapel Crags over Bleaberry Tarn
Chapel Crags, seen from Bleaberry Tarn, form a textbook example of a corrie backwall — a steep, jagged cliff face carved and plucked by glacial ice over millennia. From the tarn below, their height is easily underestimated; the scale is masked by the enclosed nature of the bowl and the quiet surface of the water, which belies the rugged drama overhead.
Corrie Divide at Chapel Crags
This steep buttress forms the eastern wall of the Bleaberry Tarn corrie, separating it from the neighbouring Comb Beck corrie. Rising sheer from the mist below, the crags here are part of Chapel Crags, their vertical face revealing the sculpting force of glacial ice. In the stillness, the boundary between the two bowls is defined not by ridgelines but by walls of shattered rock and shadow.
Twin Corries of High Stile
A corrie (or cirque) is a deep, rounded hollow formed by glacial erosion, typically on the north-facing slopes of mountains in the northern hemisphere. Over time, snow accumulates in these hollows. As it compacts under its own weight, the snow turns into dense glacial ice.
With each freeze-thaw cycle, the back wall of the hollow steepens and retreats, while plucking and abrasion by the moving ice deepens the basin below. If the process could be filmed over centuries, the ice would appear as a slow-flowing river of solid mass, descending the mountain and eventually carving out a U-shaped valley below.
As the glacier melts, it often leaves behind a rim of rocky debris (terminal moraine) at the corrie’s lip. Meltwater collects behind this barrier, forming a small lake known as a tarn. Eventually, the overflow cuts a notch through the moraine, forming a beck.
High Stile is flanked by two such glacial corries:
• To the west, the back wall of the corrie is Chapel Crags, framed by The Saddle and Dodd to the west and High Stile itself to the east. Nestled in its bowl is Bleaberry Tarn, a classic corrie lake, reaching a depth of around 4.5 m.
• To the east, the glacial basin is called Burtness Comb. Its back wall is Comb Crags, with Eagle Crag and Grey Crag forming the western flank, and White Cove and Sheepbone Buttress the eastern. Here, a moraine did not develop, so no tarn formed. Instead, spring-fed runnels emerge in the hollow to become Comb Beck, which tumbles steeply down to Buttermere.
Eagle Crag with Buttermere Below
From the summit of High Stile, a fleeting break in the mist reveals the north-east end of Buttermere, far below. The upper slopes remain shrouded, with drifting cloud curling around the summit ridge and obscuring the wider view. In this rare moment of clarity, the steep drop to Burtness Comb and the shoreline of Buttermere could just be made out — framed by the lingering mist above.
Cairned Crest of High Stile Ridge
High Stile stands at 806 m, its summit formed from a clustered cairn of large, weathered rocks. A narrow north-facing spur rises slightly higher, reaching 807 m, and marks the point where the descent to Buttermere begins. From there, the path drops steeply, skirting east around the steepest section before curving westward into Burtness Wood, en route to the lake. For Coast to Coast walkers taking the alternative Ennerdale ridge route, the onward path continues south-east along the summit ridge towards High Crag.
Misty Route to High Crag
High Crag (744 m) rises sharply as the eastern buttress of Burtness Comb, forming a towering wall opposite Grey Crag on High Stile. From the summit dome of High Stile, the ridge path dips before climbing over the stony rise of Eagle Crag, a prominent spur guarding the approach. The onward route to High Crag is clear, though narrowing and more exposed. As this photo reveals, the mist is once again descending — a reminder of the ever-changing mood on this high-level traverse. Though dramatic in profile, High Crag is readily attained from High Stile, making it a natural continuation for Coast to Coast walkers following the Ennerdale ridge.
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