Naddle Beck - Izeria

Naddle Beck is a minor river of Cumbria, England.

Rising beneath Dodd Crag, Naddle Beck flows northward to meet the River Greta. The major tributary of Naddle Beck is Shoulthwaite Gill, which drains the eastern side of High Seat and Bleaberry Fell. Mere Gill joins Shoulthwaite Gill beneath an old fort on Castle Crag. Other tributaries of Naddle Beck are Brown Beck and William's Beck.

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Glenderaterra Beck

Glenderaterra Beck is a watercourse in the county of Cumbria, England. The length of the Glenderaterra, and its major tributary Whit Beck is 4.8 miles (7.8 km), which have a total catchment area of 11.8 square kilometres (4.6 sq mi). The beck runs from its source on Burnt Horse through the valley between Lonscale Fell and Blencathra to its confluence with the River Greta at Brundholme near Threlkeld. Although the top of the stream from Burnt Horse is widely cited as the source of the Glenderaterra, the Royal Geographical Society and other authorities state that the source of a river is the furthest point from its mouth or confluence with the river it meets downstream, regardless of names attached to the contributing flows. So, the source must be Roughten Gill which starts on Blencathra, under Halls Fell top and turns the corner at a delightful and well-hidden sheepfold. It is longer than the stream in Sinen Gill which in turn is longer than the Burnt Horse contributor. On its southerly course, Glenderaterra Beck is joined by Sinen Gill and Roughten Gill, draining Blease Fell on Blencathra, and, lower down, Whit Beck, emanating from Jenkin Hill on Skiddaw. This river is used by Geography students for A Level and GCSE field studies.

St. John's Beck

St. John's Beck is a river in the Lake District of Cumbria, England. The beck has its beginning as an outflow of Thirlmere, whence it flows northwards through St. John's in the Vale, towards Threlkeld, where it meets the River Glenderamackin to form the River Greta.

River Glenderamackin

The River Glenderamackin, the Glendermackin or Glendermackin Beck is a watercourse in Cumbria, England. It is a headstream of the Greta. The river rises on Mungrisdale Common north of Blencathra and drains much of the eastern and southern sides of the mountain. The river runs east, then north before sharply turning south at the village of Mungrisdale, skirting almost all around the bottom of Souther Fell. Latterly, the river turns west to the north of Hutton Moor End and the Trout Beck joins it at Wolt Bridge to the south of Lowside. Not too far away it is soon swelled again by the waters of Mosedale Beck next to Dobson's Bridge. The Glenderamackin continues past Threlkeld, at which point it conjoins with St. John's Beck to form the River Greta.

Castlerigg stone circle

Castlerigg Stone Circle (alternatively Keswick Carles, or Carles) is situated on a prominent hill to the east of Keswick, in the Lake District National Park, North West England. It is one of around 1,300 stone circles in the British Isles and Brittany, constructed as a part of a megalithic tradition that lasted from approximately 3200 BC to 2500 BC, during the Late Neolithic and Early Bronze Ages. Various archaeologists have mentioned the beauty and romance of Castlerigg and its surrounding landscape. In his study of the stone circles of Cumbria, archaeologist John Waterhouse commented that the site was "one of the most visually impressive prehistoric monuments in Britain." Every year, thousands of tourists travel to the site, making it the most visited stone circle in Cumbria. This plateau forms the raised centre of a natural amphitheatre created by the surrounding fells and from within the circle it is possible to see some of the highest peaks in Cumbria: Helvellyn, Skiddaw, Grasmoor and Blencathra.