From the rising path between Hartsop and Hayeswater, The Knott appears ahead as a rounded, domed shoulder above the tarn. It marks the point where the High Street ridge begins to swing east toward Rampsgill Head and Kidsty Pike, forming part of the enclosing corrie wall of Hayeswater. What first looks like a distant summit gradually reveals itself as the eastern rampart of this glacial basin.

Here the path rises above Hayeswater Gill before the tarn itself comes into view, hidden just beyond the lip of the track. A faint side path leads up toward The Knott, seen as a rounded dome beyond the broad shoulder of High Street. From this vantage, the ridge lines are read in layers, with The Knott emerging as a distinct summit above the enclosing fells.

As the Hayeswater path climbs higher, it meets the Coast to Coast route descending from Angle Tarn. The track skirts the northern flank of The Knott, passing close to its summit dome, and many walkers make the short detour to stand on this 739m Wainwright. From here, the ridge opens toward High Street and the wider Far Eastern fells.

The Knott’s summit is broad and understated rather than dramatic, but at 739m it commands an expansive view. Paths converge on the rounded crest, often marked by a steady line of walkers making the short climb from the Coast to Coast route. From the top, the surrounding fells unfold clearly — High Street, Gray Crag, Kidsty Pike and High Raise forming a wide mountain panorama.

From the Coast to Coast path on the northern flank, a short detour leads up to The Knott’s summit cairn — a great mound of loose stones crowning the rounded top. The cairn stands beside the old boundary wall that crosses Rest Dodd and continues along the High Street ridge, linking these high summits in a single sweeping line.

The Knott’s rounded dome rises to 739m, but for Coast to Coast walkers it is not a major climb, as much of the elevation has already been gained on the approach from Hayeswater. To the north-east, Well Gill rises and flows west to join Sulphury Gill, which spills over the cliffs in cascades and a final fall into Hayeswater Gill below. The Coast to Coast path skirts the western side of The Knott, curves around its northern flank close to the summit, and then leaves toward the Straits of Riggindale.

From The Knott, Hayeswater lies clearly below, its dark surface enclosed by the western corrie wall of Gray Crag. The line of Hayeswater Gill can be traced as it gathers beneath Thornthwaite Crag before slipping past the tarn’s southern shore. From this height, the structure of the glacial basin is read easily in the enclosing sweep of ridge and water.