Brim Fell

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.

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.

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".

Swirl How is a fell in the English Lake District. It stands between Coniston and the Duddon Valley in the southern part of the District. It rivals the Old Man of Coniston as the highest point within the traditional County Palatine of Lancashire (it has been administered since 1974 by Cumbria County Council for local government purposes). The Coniston (or Furness) Fells form the watershed between Coniston Water and the Duddon valley to the west. The range begins at Wrynose Pass and runs south for around 10 miles (16 km) before petering out at Broughton in Furness on the Duddon Estuary. Alfred Wainwright in his influential Pictorial Guide to the Lakeland Fells took only the northern half of the range as Lakeland proper, consigning the lower fells to the south to a supplementary work The Outlying Fells of Lakeland. Swirl How being a significant high point of the Coniston Fells therefore qualifies as one of the 214 Wainwrights. Later guidebook writers have chosen to include the whole range in their main volumes.

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

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.

The Coniston copper mines were a copper mining operation in Lancashire, England. It was functional for hundreds of years in Coppermines Valley above Coniston Water. Today there are industrial remains of the industry and the Coniston Coppermines Youth Hostel is based in the old manager's building. Mining for copper in the valley dates back to the 16th century and the area continued to be mined until the 1950s. In 1982 the buildings in the valley were purchased by The Coppermines Lakes Cottages founder Philip Johnston who set about a comprehensive scheme of rebuilding, restoration and conservation. The buildings were sympathetically restored from the original Victorian sawmill. In 1974, the area of Coniston and the Furness Fells was transferred for administrative purposes to the area of Cumbria County Council.

Seathwaite Tarn is a reservoir in the Furness Fells within the English Lake District. It is located to the south of Grey Friar and to the west of Brim Fell (on the ridge between The Old Man of Coniston and Swirl How) and north east of the village of Seathwaite on the east of the Duddon Valley. In order to create a source of drinking water the existing tarn was considerably enlarged with a dam in 1904. During the dam construction some of the navvies rioted damaging buildings in the village, several rioters were shot, one dying the next day. The dam is almost 400 yards (366 m) long and is concrete cored with slate buttresses, the resulting depth of the tarn being around 80 feet (24 m). Water is not abstracted directly from the tarn, but flows some distance downriver to an off-take weir. On the slopes of Brim Fell, above the head of the reservoir, are the remains of Seathwaite Tarn Mine. This was worked for copper in the mid 19th century, and also appears as a location in the novel The Plague Dogs by Richard Adams. Rocks in the area were the first confirmed occurrence of wittichenite in the British Isles.Bronze Age ring cairns were found close to Seathwaite Tarn in 2003, these were excavated in 2003 and 2007.Seathwaite Tarn has suffered from acidification. An experiment in 1992–1993 to reduce the acidification by using a phosphorus-based fertiliser increased the pH from 5.1 to 5.6 and changed the levels of the different species of the rotifer assemblage significantly.

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.