Kidsty Pike, High Street - Coast to Coast
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Head of Riggindale Beck, Kidsty Howes
Kidsty Pike, High Street, Mardale - Coast to Coast
The Coast to Coast Path leaves the broad whaleback of High Street on a narrowing ridge that breaks away eastwards towards Kidsty Pike and Kidsty Howes. At 780 metres, Kidsty Pike is the highest point reached on the entire Coast to Coast walk, a modest summit by Lakeland standards but one that feels emphatically mountainous due to its steep-sided setting above Riggindale. The fell forms the northern wall of that long, glacial valley, its rocky flanks dropping sharply towards Haweswater below.
From the High Street junction, the ridge runs for just over a mile, rising gently at first before tightening into a more dramatic spine. Near the summit, the crest steepens and twists through a turret of rock and broken ground, giving Kidsty Pike a craggier character than many of its grassy neighbours. Beyond the top, the ridge eases again as it descends towards Kidsty Howes, the terrain softening into sloping grass that carries walkers down towards the Haweswater shoreline and the next stage of the route.
Kidsty Pike
Kidsty Pike is a striking and easily recognisable summit, standing out clearly when viewed from a distance and offering expansive views down over Haweswater. Its sharp, narrow form is the result of strong glacial erosion on either side, with Riggindale cutting steeply away to the south and Randale falling to the north, while the upper reaches of Rampsgill influence the eastern shoulder of the ridge. Rather than a true pyramidal peak, Kidsty Pike is a sharply defined ridge-end summit, marking the highest point of the Coast to Coast walk.
Kidsty Pike Summit
The summit cairn of Kidsty Pike is surprisingly modest for such a striking mountain top. Although this is a Wainwright summit rising to 780 metres, the cairn stands only around 100 yards west of the higher neighbouring top of Rampsgill Head (792m), its close sibling on the ridge, the two summits separated by little more than a gentle dip along the High Street spur.
Twopenny Crag Kidsty Pike
Immediately east of the Straits of Riggindale, Twopenny Crag drops steeply and dramatically into the depths of Riggindale, its slopes falling away with little warning from the High Street ridge. The crag forms part of High Street’s eastern wall, emphasising the sudden transition here from broad upland plateau to sharply incised glacial valley.
High Raise Rampsgill Head
From The Knott, the view carries across the backwall of Rampsgill Head to the broad, grassy summit of High Raise (802m). Part of the steep enclosing wall of Rampsgill Head is visible from this angle, revealing how closely the fell presses against the High Street ridge. Rampsgill Head itself lies very close to the Coast to Coast Path as it approaches Kidsty Pike, its rounded summit passed almost in stride as the route threads between High Street and the Haweswater side of the fells.
High Raise Summit
From the path near Long Stile on High Street, the rounded 780-metre summit of Rampsgill Head comes clearly into view. Two paths trace the ridge around Twopenny Crag and the head of Riggindale Beck: the Coast to Coast Path keeping close to the rim of the escarpment, while a second line continues more directly to the summit cairns of Rampsgill Head. Beyond these foreground ridges, the broader, higher mass of High Raise rises in the background, its grassy summit reaching 802 metres.
Kidsty Pike
Zooming in on Kidsty Pike from Long Stile emphasises the vertiginous drop away from its 780-metre summit, where the ridge falls sharply into Riggindale. From this angle, the Pike stands prominently in the foreground, with High Raise rising beyond to the north-west at 802 metres, and the lower, broader dome of Low Raise visible to the north-east at 754 metres, together framing Kidsty Pike within the wider upland plateau of the High Street range.
Glacial Geography at Kidsty Pike
Arête Ridge
Kidsty Pike stands on a sharp arête formed where glaciers eroded back-to-back from the valleys of Riggindale and Haweswater.
Headward Erosion
Ice carved steep corries on either side of the ridge, progressively narrowing it into the knife-edge form seen today.
Steep Eastern Face
The dramatic drop into Riggindale marks the side of the ridge most aggressively eroded by glacial flow.
Hanging Valley Context
Riggindale itself forms part of the wider Haweswater glacial trough system, its depth reflecting the power of the trunk glacier.
Frost-Shattered Crest
Post-glacial freeze-thaw weathering contributed to the loose, angular rock along the summit crest.
Glacial Threshold
The descent from Kidsty Pike towards Haweswater follows a glacially steepened slope left after ice retreat.
Kidsty Howes
Kidsty Howes marks the abrupt, stumpy termination of the Kidsty Pike ridge, where the ground drops suddenly towards Haweswater. The descent is steep, but the path spirals down between rocky buttresses, easing the gradient and lending a surprising sense of structure to the fall of the ridge. As height is lost, the views open and shift repeatedly, revealing Haweswater from multiple angles, with Mardale Common, Branstree, and Harter Fell laid out across the reservoir, and long views extending down its length towards Bampton.
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