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Geological map of the Lake District showing the main structures and areas of mineralisation Skiddaw seen from Derwentwater. The Lake District's geology is very complex but well-studied. [33] A granite batholith beneath the area is responsible for this upland massif, its relatively low density causing the area to be "buoyed up". The granite can ...
The map shows the locations of the lakes with a volume over 4 x 10 6 m³ and gives an indication of the volume of water in each lake. The markers suggest this by showing the size of a drop of water where the volume of the drop would be in proportion to the quantity of water in the lake (the diameter of the drop is proportional to the cube root ...
The valley has an annual rainfall of 2,408 millimetres (94.8 in), [8] higher than the Lake District average, which is itself considerably wetter than the UK average. The land in Little Langdale is now mainly used for sheep and cattle farming, although until 1940 at least some of the farmland was ploughed.
The hill passes listed are routes within the Lake District National Park between two different valleys where a pathway is marked on the Ordnance Survey 1:50000 or 1:25000 map. Passes to be considered may be listed as "pass" or "hause" in the Ordnance Survey 1:50000 gazetteer provided also that a route crossing the ridge is marked on the map. [74]
The geology of England's Lake District is dominated by sedimentary and volcanic rocks of mainly Ordovician age underpinned by large granitic intrusions.Younger sedimentary sequences outcrop on the edges of the Lake District area, with Silurian to the south, Carboniferous to the north, east, and west and Permo-Triassic to the west and east.
See List of Wainwrights for them sorted by book, and the other Lake District fells he listed in The Outlying Fells of Lakeland. Scafell Pike, 978 m (3209 ft) Scafell, 964 m (3163 ft) Helvellyn, 950 m (3117 ft) Skiddaw, 931 m (3054 ft) Great End, 910 m (2986 ft) Bowfell, 902 m (2959 ft) Great Gable, 899 m (2949 ft) Pillar, 892 m (2927 ft)
Tarn Hows is an area of the Lake District National Park in North West England, It contains a picturesque tarn, approximately 2 miles (3.2 km) northeast of Coniston and about 1.5 miles (2.4 km) northwest of Hawkshead.
Coniston Water is a lake in the Lake District in North West England.It is the third largest by volume, after Windermere and Ullswater, and the fifth-largest by area. [1] The lake has a length of 8.7 kilometres (5 + 3 ⁄ 8 mi), a maximum width of 730 metres (800 yd), and a maximum depth of 56.1 m (184 ft 1 in).
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