Ting Mound

Lingmoor Fell is a fell in the English Lake District, situated eight kilometres (five miles) west of Ambleside. The fell reaches a height of 469 m (1,540 ft) and divides the valleys of Great Langdale and Little Langdale. The fell's name originates from the Old Norse word lyng meaning “heather covered”. The actual summit of the fell is named as Brown How on Ordnance Survey maps.

Slater's Bridge is a traditional packhorse bridge in Little Langdale in the English Lake District, standing at National Grid Reference NY3120502996.

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.

Little Langdale is a valley in the Lake District, England, containing Little Langdale Tarn and a hamlet also called Little Langdale. A second tarn, Blea Tarn, is in a hanging valley between Little Langdale and the larger Great Langdale to the north. Little Langdale is flanked on the south and southwest by Wetherlam and Swirl How, and to the north and northwest by Lingmoor Fell and Pike of Blisco. The valley descends to join with Great Langdale above Elter Water.

Great Langdale is a valley in the Lake District National Park in North West England, the epithet, "Great" distinguishing it from the neighbouring valley of Little Langdale. Langdale is also the name of a valley in the Howgill Fells, elsewhere in Cumbria. It is a popular location for hikers, climbers, fell-runners, and other outdoor enthusiasts who are attracted by the many fells ringing the head of the valley. Among the best-known features of Great Langdale are the Langdale Pikes, a group of peaks on the northern side of the dale. England's highest mountain, Scafell Pike, can be climbed by a route from Langdale. Langdale has views of, in particular, Dungeon Ghyll Force waterfall, Harrison Stickle, and Pike of Stickle. Great Langdale was an important site during the Neolithic period for producing stone axes and later, was also one of the centres of the Lakeland slate industry.

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 Langdale axe industry (or factory) is the name given by archaeologists to a Neolithic centre of specialised stone tool production in the Great Langdale area of the English Lake District. The existence of the site, which dates from around 4,000–3,500 BC, was suggested by chance discoveries in the 1930s. More systematic investigations were undertaken by Clare Fell and others in the 1940s and 1950s, since when several field surveys of varying scope have been carried out.Typical finds include reject axes, rough-outs and blades created by knapping large lumps of the rock found in the scree or perhaps by simple quarrying or opencast mining. Hammerstones have also been found in the scree and other lithic debitage from the industry such as blades and flakes. The area has outcrops of fine-grained greenstone or hornstone suitable for making polished stone axes. Such axes have been found distributed across Great Britain. The rock is an epidotised greenstone quarried or perhaps just collected from the scree slopes in the Langdale Valley on Harrison Stickle and Pike of Stickle. The nature and extent of the axe-flaking sites making up the Langdale Axe Factory complex are still under investigation. Geological mapping has established that the volcanic tuff used for the axes outcrops along a narrow range of the highest peaks in the locality. Other outcrops in the area are known to have been worked, especially on Harrison Stickle, and Scafell Pike where rough-outs and flakes have been found on platforms below the peaks at and above the 2000- or 3000-foot level. Recent research has shown that Langdale tuff was used for tools before the Neolithic 'axe factories' were established. In Maryport (Cumbria) it was selected for tool manufacture in the Final Palaeolithic and Mesolithic

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.

Holme Fell or Holm Fell is a fell in the Lake District in Cumbria, England. It is located between Coniston Water and Little Langdale, almost isolated from the neighbouring Coniston Fells by Yewdale Beck.

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

Chapel Stile is a village in Cumbria, England, located approximately 5 miles northwest of Ambleside, within the Langdale valley. It contains a school, Holy Trinity church, the Co-op and the Wainwrights' Inn (formerly The Langdale Hotel), and a quarry is located in the vicinity. Couples who choose to get married at the church are traditionally 'tied in' during the service. The local children tie up the church gates and the newlyweds are only released when coins (of small denomination) are thrown to said children. The Co-op has been established for well over a hundred years. Chapel Stile also gives access to the Langdale Pikes, Pike o' Stickle and Harrison Stickle. Other notable fells nearby are Pavey Ark, Bowfell and Pike o' Blisco. Rock climbing in the area includes Raven Cragg. A worthy climbing venue and less populated than its famous counterpart further in the Langdale valley at the back of the Old Dungeon Ghyll. In popular culture, or at least 'underground popular culture', there is a nu jazz track called 'Chapel Stile' by Pretz (N.Cowley). Due to its location within a popular tourist destination, around 85% of the homes within the community are now either second homes or holiday lets.

Blea Rigg is a fell in the English Lake District, lying between the valleys of Easedale and Great Langdale. One of the Central Fells, it is a broad plateau with a succession of rocky tops. Many routes of ascent are possible, beginning either from Grasmere or Great Langdale, though the paths are often poorly marked and hard to follow.