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.
54°36′43″N3°04′48″W / 54.6119°N 3.0800°W
The Rothay is a spate river of the Lake District in north-west England. Its name comes from Old Norse and translates literally as the red one. This has come to mean trout river. It rises close to Rough Crag above Dunmail Raise at a point about 1542 feet above sea level. Its catchment area covers Grasmere Common including Easedale Tarn, the southern flanks of Fairfield, and several of the fells to the east of Dunmail Raise, including Great Rigg, Rydal Fell, Scandale Fell and Heron Pike.
High Seat is a fell in the centre of the English Lake District. Despite being below 2,000 ft it is the highest point for about 5 miles (8 km) in any direction; a consequence of the curious fact that the centre of the district is lower than the surrounding parts.
The Trout Beck is a fast flowing stream of the Lake District in North West England. It is one of the main sources of replenishment for Windermere, and is part of the Leven catchment. Its name comes from Old Norse and appears in documents from 1292 as Trutebyk. The river rises between the peaks of Stony Cove Pike and Thornthwaite Crag in the High Street range, at a height of about 1,970 feet (600 m).
The River Lowther is a small river which flows through limestone rock in Cumbria, England. It is a tributary of the River Eamont which in turn is a tributary of the River Eden which flows into the Solway Firth near Carlisle. The Lowther begins with the confluence of the Keld Gill and the Keld Dub near the village of Keld. It flows north-west until it passes between Bampton and Bampton Grange, before turning north until it flows into the River Eamont close to Penrith.
The River Bleng is a tributary of the River Irt in the county of Cumbria in northern England.
The River Mint is a river in Cumbria, England. The Mint starts life at Whelpside at the confluence of Bannisdale Beck, running south-east from Bannisdale Head, and a smaller stream draining a group of small valleys from headwaters in The Forest, Combs Hollow and Mabbin Crag.
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 River Wampool is a river flowing through north western Cumbria in England. It is in the Waver and Wampool catchment which includes the towns of Silloth and Wigton.
Leck Beck is a watercourse in Lancashire with its source on Crag Hill in Cumbria between Leck Fell and Casterton Fell.
Sandwath Beck is a river running through Cumbria in England.
Artle Beck is a minor river of Lancashire, England.
The River Greta is a river in County Durham, England. It is a tributary of the River Tees and flows through the northern part of the old North Riding of Yorkshire. The name "Greta" derives from the Old Norse "Griótá", meaning "stony stream".
Chapel Beck is a minor river in the county of Cumbria in England.
Coledale Beck is a minor river running through Cumbria in England.
Keskadale Beck is a minor river of Cumbria, England.
Scope Beck is a minor river in the county of Cumbria in England.
Stonethwaite Beck is a minor river in Cumbria, England. It is a tributary of the River Derwent.
Arkle Beck is the stream running through the valley of Arkengarthdale in the Yorkshire Dales, England. It is a tributary of the River Swale, which it joins just past Reeth at Grinton Bridge. The beck itself has several tributaries which include:
The Bannisdale Horseshoe is an upland area in Cumbria, England, near the eastern boundary of the Lake District National Park, surrounding the valley of Bannisdale Beck, a tributary of the River Mint. It is described in the final chapter of Wainwright's book The Outlying Fells of Lakeland.