All three routes of the Coast to Coast path converge at Ravenseat, i.e. the red, blue and green routes. The path leaves Ravenseat for Keld, which means walking along the path above the west riverbank of the south section of Whitsun Dale. Looking back from Close Hills a vista opens out to the head of this section, with Ravenseat Farm assuming the central position.

Below a sheepfold, barely out of Ravenseat, is the Whitsundale Waterfall. Modest though it is on the drier days this can change very quickly in wet weather. There are actually two small waterfalls within close proximity.

In late spring and early summer the hay meadows around Ravenseat burst into blossom with prodigious displays of yellow globe flowers, dandelions and other meadow flowers. One of the hay meadows, due to the dense plethora of globe flowers, has been designated as an SSSI.

After leaving Ravenseat, Whitsundale Beck is forever changed. It has grown broader, deeper and swifter, and is nearing the end of its 2nd order beck status, to submit itself to the River Swale at High Bridge and become a 3rd order river.

How Edge, on both riverbanks, is an area of steep limestone cliffs with a small gorge through which the Whitsundale Beck is channeled.

At Oven Mouth the Whitsundale Beck enters another small gorge. On one of the steep arcs of the Beck the Reynoldson Sike converges with the Beck. The gulley created by the Sike is quite deep and looks modestly dramatic.

Gazing across the valley from Barney Brow, Hill Top Farm is prominent. Above the farm, about 200 yards from it, is Birkdale Tarn, a substantial tarn in the area designated as Tarn Moss.

Near the end of Whitsun Dale is Smithy Holme Farm. This is near to where the path turns into Swaledale.

Although named as Brian Cave on the OS, this is in fact a disused lime kiln. There appears to be nothing special about it. It is located immediately above the bridge at Low Bridge.

Great Ash Gill descends from Ashgill Side to converge with the River Swale very close to the Whitsundale Beck's convergence. The deep gulley sides are a testament to the soft terrain of the moorland. The view of the Gill is outstandingly dramatic when descending Little Moor at the very south of Whitsun Dale.