Fornside

Legburthwaite is a village in the Allerdale district, in the county of Cumbria. It is located on the A591 road and the B5322 road. Legburthwaite has a disused place of worship and formerly, a youth hostel. It is just north of Thirlmere.

St John’s in the Vale is a glacial valley in the Lake District National Park, Cumbria, England. Within the vale are a number of farms and small settlements, in addition to several disused quarry and mining works. St John’s Beck meanders northward along the floor of the vale, and is the main outflow from Thirlmere reservoir, which is located to the south. Alongside the beck runs the B5322, St John’s in the Vale Road. The vale is in the heart of the northern Lake District and is surrounded by many of the most striking of the Lakeland fells. It runs from south to north, set between the rocky flanks of Clough Head to the east and the neighbours High Rigg and Low Rigg to the west. The southern end of the vale is a narrow pass between High Rigg and Great Dodd, just to the north of the small settlement of Legburthwaite. At its northern end the vale widens to meet the broad east-to-west valley of the River Greta near Threlkeld. The view north from the vale is dominated by the mountains Blencathra and Skiddaw. High on the western side of the vale lies St John’s in the Vale Church, located in a low pass between High Rigg on the southern side and Low Rigg to the north. This pass provides access for suitably capable vehicles between the vale and Dale Bottom in the Naddle Valley to the west of High Rigg. The present building dates from 1845, with the earliest reference to a church at the site being 1554. On the opposite side of the vale, cut into the northern flank of Clough Head, lies the Threlkeld Quarry and Mining Museum. This former commercial quarry, first opened in the late nineteenth century, was established as a museum in 1992. The picturesque writer William Gilpin describes a landslide that happened here on 22 August 1749 as being caused by ‘one of those terrible inundations, which wasted lately the vale of Brackenwait’.

The Thirlmere Aqueduct is a 95.9-mile-long (154.3-kilometre-long) pioneering section of water supply system in England, built by the Manchester Corporation Water Works between 1890 and 1925. Often incorrectly thought of as one of the longest tunnels in the world, the aqueduct's tunnel section is not continuous. The aqueduct was built to carry approximately 55,000,000 imperial gallons (250,000 m3) per day of water from Thirlmere Reservoir to Manchester. The construction of the reservoir and aqueduct was authorised by the Manchester Waterworks Act of Parliament. The first phase was completed in 1897 and, for the pipeline sections, subsequent phases were completed in 1925. The first water to arrive in Manchester from the Lake District was marked with an official ceremony on 13 October 1894. The route of the reservoir passes through Lancashire and then enters Manchester through Salford. It has been mapped on OpenStreetMap here: https://www.openstreetmap.org/relation/7937446

High Rigg is a small fell located in the English Lake District, approximately three miles southeast of the town of Keswick. It occupies an unusual position, surrounded on all sides by higher fells but not connected by any obvious ridge. This separation from its fellows ensures that it is a Marilyn (a hill with topographic prominence of at least 150m).

Watson's Dodd is a fell in the English Lake District, a minor rise on the main ridge of the Helvellyn range in the Eastern Fells, but a prominent shoulder on the west side of that range. At its foot is the imposing crag of Castle Rock, on which rock climbers have developed some 60 named routes.

Clough Head ( ) (meaning: hill-top above the ravine) is a fell, or hill, in the English Lake District. It marks the northern end of the main ridge of the Helvellyn range and is often walked as part of the ridge walk. The fell stands south of the village of Threlkeld and the A66 road, and it forms the steep eastern side of the tranquil valley of St John's in the Vale. On its western side the fell displays a dark mass of rocky crags and a deep-set rocky ravine. On the other side it has smooth grassy slopes. Beneath the north face is the steep valley or clough from which Clough Head gets its name. Also beneath the steep northern face lies the lower hill of Threlkeld Knotts, a granite hill which has been much quarried round its margin. A number of different types of rock are found on and around Clough Head, which were formed in very different circumstances. These include deep-sea sedimentation, effusive volcanic lava flows, explosive volcanism, an intrusion of granite, mineralisation and finally glacial sculpting. To understand the geology of Clough Head is to understand much of the geology of the Lake District. An old route known as the Old Coach Road passes beneath Clough Head. Most of the fell is Open Access land, which walkers can enter from either end of the Old Coach Road, or from a lane south of the village of Threlkeld. Four main routes lead to the summit.

St John's Church is in the valley of St John's in the Vale, Cumbria, England. It is an active Anglican parish church in the deanery of Derwent, the archdeaconry of West Cumberland, and the diocese of Carlisle. Its benefice is united with those of St Mary, Threlkeld, and Wythburn Church. The church is recorded in the National Heritage List for England as a designated Grade II listed building.

Raven Crag is a fell in the English Lake District that overlooks Thirlmere reservoir. It has subsidiary summits The Benn and Castle Crag.

Great Dodd (meaning: big round hill) is a mountain or fell in the English Lake District. It stands on the main ridge of the Helvellyn range, a line of mountains which runs in a north–south direction between the lakes of Thirlmere and Ullswater in the east of the Lake District. Great Dodd, with a height of 857 metres (2,812 ft) is the highest of the fells in this range to the north of Sticks Pass. Walkers may approach Great Dodd from either High Row near Dockray to the east, or from Legburthwaite to the west – or along the main ridge track from either north or south. Scramblers with climbing skills may be attracted to three gill climbs on the western side of the mountain. The summit of Great Dodd is a smooth, grassy, rounded dome, like its two southern neighbours, Watson's Dodd and Stybarrow Dodd. Together, these three are sometimes called ‘The Three Dodds’. These three are made of volcanic rocks of the Borrowdale Volcanic Group, and the tops of all three are covered by the same sheet of rock, which was formed in a series of huge volcanic explosions accompanying the formation of a volcanic caldera about 450 million years ago. Two attempts were made to mine mineral veins in the rocks of Great Dodd, but neither attempt was successful.

Threlkeld railway station was situated on the Cockermouth, Keswick and Penrith Railway between Penrith and Cockermouth in Cumbria, England. The station served the village of Threlkeld. The station opened to passenger traffic on 2 January 1865, and closed on 6 March 1972.

Stybarrow Dodd (the hill of the steep path) is a mountain or fell in the English Lake District. It stands immediately north of Sticks Pass on the main ridge of the Helvellyn range in the Eastern Fells, which is situated between the lakes of Thirlmere and the Ullswater. The summit of Stybarrow Dodd is a smooth, rounded, grassy dome, like those of its two northern neighbours, Watson's Dodd and Great Dodd. Together, these three rather similar fells are sometimes called ‘The Three Dodds’. All three are covered by the same sheet of volcanic rock.

The Threlkeld Quarry and Mining Museum is a museum located in Threlkeld three miles (4.8 km) east of Keswick, in the Lake District in Cumbria. It includes a quarry with a collection of antique machinery, such as locomotives and cranes, an underground tour of a simulated mine, a geological and mining museum, and mineral panning.