Swirl How

Great Carrs is a fell in the English Lake District. It stands above Wrynose Pass in the southern part of the District.

Levers Water is a small lake in the English Lake District. It is located at the head of the Coppermines Valley, above Coniston village. To its south-west is Raven Tor, a spur of Brim Fell, and to its north-west are Little How Crags and Great How Crags, on the eastern side of the north–south ridge leading to Swirl How. A dam built in 1717 enlarged the existing tarn to provide water for the mines and for the village below.A public footpath on its north-east side connects the Coppermines Valley to Swirl Hawse, while to its south-west, a path leads up Gill Cove to Levers Hawse on the main ridge of the Coniston Fells.

The Wrynose Pass is a mountain pass in the Lake District National Park in Cumbria, England between the Duddon Valley and Little Langdale.

Brim Fell is a fell in the English Lake District. It stands to the west of Coniston village in the southern part of the District.

The Three Shire Stone is a boundary stone that marks the location where the historic English counties of Lancashire, Cumberland and Westmorland meet. The point is in the English Lake District at the summit of Wrynose Pass; latitude 54°25' North, longitude 3°7' West, elevation 1289 feet (393 m) above sea level (grid reference NY276027). The limestone monolith was cut in the Lancashire village of Cartmel in 1816 for the Furness roadmaster William Field; however, it was not erected until 1860, after his death. The front of the stone is inscribed with the word Lancashire. On the reverse side is the inscription W.F. 1816. It is grade II listed.In 1997, the stone was smashed into four pieces, probably as the result of a motor accident. It was restored in 1998 by stonemason Gordon Greaves of Troutbeck Bridge. The unveiling ceremony of the restored monument took place on 27 April 1998. The possible loss of the stone prompted organisations, including Friends of Real Lancashire, to raise money for its restoration. The National Trust moved the car park away from the restored stone, and placed some cobbles in the turf to mark the county boundaries radiating from it. The stone was found fallen and damaged in summer 2017, but was once again repaired and restored to its original location. It was still standing in August 2023.

The Brathay is a river of north-west England. Its name comes from Old Norse and means broad river. It rises at a point 1289 feet (393 m) above sea level near the Three Shire Stone at the highest point of Wrynose Pass (grid reference NY277028) in the Lake District. Its catchment area includes the northern flanks of Wetherlam, Great Carrs and others of the Furness Fells, as well as a substantial area of the Langdale Fells. The small stream at the top of Wrynose quickly gathers pace as it descends some 930 feet (283 m) in a distance of about two miles (3.2 km), running roughly parallel to, and south of, the Wrynose Pass road. Before flowing into Little Langdale Tarn it subsumes Bleamoss Beck, the outflow from Blea Tarn. Little Langdale Tarn is also replenished by the Greenburn Beck. The Brathay drains Little Langdale Tarn at its eastern side. It continues in an easterly direction, over Colwith Force where it falls 40 feet (12 m), before turning north and flowing into the tarn of Elter Water at an elevation of 187 feet (57 m) above sea level. Elter Water is also replenished by the Great Langdale Beck.The Brathay drains Elter Water and flows for about half a mile (0.8 km) in a south-easterly direction to Skelwith Force where it descends 15 feet (4.6 m). Passing under the A593 road at Skelwith Bridge, and continues in an easterly direction, to the hamlet of Clappersgate. After another quarter of a mile (400 m) it joins the River Rothay close to Croft Lodge south-west of Ambleside before flowing into the northern end of Windermere. The stretches of the Brathay around Clappersgate and Skelwith Force are popular with canoeists.For its entire length the River Brathay forms part of the boundary between the historic counties of Lancashire and Westmorland. Since local government re-organisation in 1974 the Brathay has been within the administrative county of Cumbria. The river also gives its name to the Brathay estate where the Brathay Exploration Group is based, just south of its confluence with the River Rothay on the edge of Windermere.

Grey Friar is a fell in the English Lake District, it is one of the Coniston Fells and is situated 13 kilometres (8 miles) west-south-west of Ambleside. It reaches a height of 770 metres (2,526 feet) and stands to the north west of the other Coniston Fells, a little off the beaten track and tends to be the least visited of the group. It is quite a large fell and forms the eastern wall of the Duddon Valley for several kilometres, in fact all drainage from Grey Friar goes to the Duddon Valley and not to Coniston Water.

Wetherlam (763 m) is a mountain in the English Lake District. It is the most northerly of the Coniston Fells, the range of fells to the north-west of Coniston village; its north-east slopes descend to Little Langdale.

The Old Man of Coniston is a fell in the Furness Fells of the Lake District in Cumbria, England, and is the highest point (county top) of the historic county of Lancashire. It is at least 2,632.62 feet (802.42 m) high, and lies to the west of the village of Coniston and the lake, Coniston Water. The fell is sometimes known by the alternative name of Coniston Old Man, or simply The Old Man. The mountain is popular with tourists and fell-walkers with a number of well-marked paths to the summit. The mountain has also seen extensive copper and slate mining activity for eight hundred years, and the remains of abandoned mines and spoil tips are a significant feature of the north-east slopes.

Goat's Water is a small accessible tarn in the English Lake District, located between Dow Crag and The Old Man of Coniston to the Duddon Valley, near the town of Coniston.

Cold Pike is a fell in the English Lake District. It is a satellite of Crinkle Crags and stands above the Upper Duddon Valley.

Dow Crag is a fell in the English Lake District near Coniston, Cumbria. The eastern face is one of the many rock faces in the Lake District used for rock climbing. The name Dow Crag originally applied specifically to the eastern face which looks down upon the tarn of Goat's Water, the fell itself having no need for a name before the inception of hill walking in the 19th century. As with many fells the name of a prominent feature was then applied to the whole mass. Dow was originally named Doe and still locally pronounced as "Doe".