Highgate Platform railway station

Trout Beck is a 7.6 miles (12.3 km) long stream or beck in the English Lake District, Cumbria. It rises on the northwestern slopes of Great Dodd, with tributaries including Groove Beck and Thornsgill Beck, and flows east then north to the hamlet of Troutbeck. It then flows west, parallel to and south of the A66 road, going just south of Hutton Moor End then under the old Hutton Moor Road at Wolt Bridge where it joins the River Glenderamackin. To the west of Troutbeck hamlet the beck is bridged by the former Cockermouth, Keswick and Penrith Railway.

The Mosedale Viaduct carried the Cockermouth, Keswick and Penrith Railway over Mosedale Beck until its closure in 1972. Building work on the viaduct began in 1862, and the first test train crossed it in 1864. It is made of stone and has 12 arches, and is just over 140 yards (420 feet (130 m)) long. It was built single-track but was extended to the north in 1900 to accommodate two tracks. In 1997 British Rail Property Board agreed to defer plans to demolish the viaduct, in the light of proposals for the line to be reopened. It is featured in S1 Ep 4 of Walking Britain's Lost Railways.

Mosedale Beck is a river in Cumbria, England, which rises on the northern slopes of Great Dodd and flows north east, to the south of Clough Head before joining the River Glenderamackin to the east of Threlkeld village. This then flows west, alongside the A66 road south of Blencathra, to form the River Greta which flows into the River Derwent. Shortly before joining the Glendaramackin, Mosedale Beck is crossed by the Mosedale Viaduct of the former Cockermouth, Keswick and Penrith Railway, now a footpath.

Hutton Moor End is a hamlet on the Hutton Moor Road in the north east of the Lake District in Cumbria, England. It lies within the civil parish of Mungrisdale and is known locally as 'Moor End' as it is at the end of the Hutton Moor on an old route-way between Penrith to Keswick.

Souther Fell is a fell in the English Lake District. It stands to the south of Mungrisdale village in the Northern Fells. It is most famous for the appearance of a "spectral army", said to have been seen marching along its crest on Midsummer's Day, 1745. No such force was in the District at the time.

Mungrisdale is a small village and civil parish in the north east of the English Lake District in the historic county of Cumberland but now in the ceremonial county of Cumbria. It is also the name of the valley in which the village sits. Mungrisdale is a popular starting point for ascents of the nearby hills, such as Bowscale Fell, Bannerdale Crags and Souther Fell. It lies on the River Glenderamackin, a tributary of the Greta. Mungrisdale has no local amenities except for the Grade II* listed St Kentigern's Church built in 1756, a village hall and a pub, the Mill Inn. The civil parish of Mungrisdale is made up of the hamlets of Berrier, Bowscale, Haltcliff Bridge, Heggle Lane, Hutton Roof, Mosedale, Mungrisdale and Murrah. The parish had a population of 284 in 2001, increasing to 297 at the 2011 Census. Part of the parish lies within the Skiddaw Group SSSI (Site of Special Scientific Interest).

Troutbeck is a hamlet within Cumbria, England, a few miles to the west of Penrith. It was previously in the county of Cumberland. It lies within the Lake District, the civil parish of Hutton, and the unitary authority of Westmorland and Furness. Great Mell Fell is situated immediately to the east of Troutbeck. It is open-access land which belongs to the National Trust. There are five Roman temporary or marching camps just to the north of Troutbeck, adjoining the A66 Roman road. The place-name 'Troutbeck' is first attested in the Subsidy Rolls of 1332, where it appears as Troutbek. The name means 'trout stream'. The stream the Trout Beck heads towards it and then veers west where it joins the River Glenderamackin less than half a mile to the west of Hutton Moor End.

Troutbeck railway station was situated on the Cockermouth, Keswick and Penrith Railway between Penrith and Cockermouth in Cumberland (now in Cumbria), England. The station served the hamlet of Troutbeck. It opened to passenger traffic on 2 January 1865, and closed on 6 March 1972.

Bannerdale Crags is a fell in the English Lake District. It stands between Blencathra and Bowscale Fell in the Northern Fells.

Bowscale is a hamlet and former civil parish, now in the parish of Mungrisdale, in the Westmorland and Furness district, in the county of Cumbria, England. In 1931 the parish had a population of 27. The sable tarn in Sir Walter Scott's poem The Bridal of Triermain was reportedly based on Bowscale Tarn.

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.

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.