England - The Lake District & Cumbria
In the Lake District, 500 million years of geological processes have produced a physical landscape of mountains and lakes of great scenic beauty.
Slate developed from sediments in oceans and seas, volcanoes erupted, limestone was formed by the deposition of dead crustaceans and sandstone was created in desert conditions. Various minerals were also formed in joints and faults in the bedrock.
The … (read more)
Slate developed from sediments in oceans and seas, volcanoes erupted, limestone was formed by the deposition of dead crustaceans and sandstone was created in desert conditions. Various minerals were also formed in joints and faults in the bedrock.
The … (read more)
Wastwater Screes rocky reflections
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Wasdale is a valley and civil parish in the western part of the Lake District National Park in Cumbria, England. The River Irt flows through the valley to its estuary at Ravenglass. A large part of the main valley floor is occupied by Wastwater, the deepest lake in England (258 feet).
Autumn reflections on Wastwater - Cumbria
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Wasdale is a valley and civil parish in the western part of the Lake District National Park in Cumbria, England. The River Irt flows through the valley to its estuary at Ravenglass. A large part of the main valley floor is occupied by Wastwater, the deepest lake in England (258 feet, 78 mtr).
The pictue shows part of the Wasdale Screes, an area of unstable, loose boulders on the east bank of Wast Water, underneath Illgill Head and Whin Rigg.
Stormy sky over still water, Wast Water, Cumbria
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Wasedale and Wastwater in Autumn colours
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Bassenthwaite Lake from Derwent Fells
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Bassenthwaite Lake is one of the largest water bodies in the English Lake District. It is long and narrow, approximately 4 miles (6.4 km) long and 3⁄4-mile (1.2 km) wide, but is also extremely shallow, with a maximum depth of about 70 ft (21 m).
It is the only body of water in the Lake District to use the word "lake" in its name, all the others being "waters" (for example, Derwentwater), "meres" (for example, Windermere) or "tarns" (for example, Dock Tarn). It is fed by, and drains into, the River Derwent. The lake lies at the foot of Skiddaw, near the town of Keswick.
The view is to the northwest with the Solway Firth and Scotland on the horizon.
Perhaps better enlarged
Please tell me we're not heading for Skiddaw
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Taken on the Derwent Fells - Skiddaw is the mountain on the horizon with the slight covering of snow.
Northern Fells above Keswick - Lake District
Contrails at dawn
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Windblown contrails reflecting the light of the rising sun over Cumbrian Fells
Perhaps better enlarged
Dawn on a Cumbrian lane
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Pointing the Way - (HFF Everyone)
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HFF 26/2/21
Access gate and signpost on Green Lonning (Lane) for Embleton High Common and Ling Fell - Allerdale District, Cumbria
Cumbrian Sunset (HFF Everyone)
Over the hills and far away.....
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Cumbrian Fells
The fell, centre picture, is called Cat Bells and overlooks the town of Keswick and Derwent Water.
Cat Bells is a fell with a modest height of 451 metres (1,480 ft) but despite this it is one of the most popular fells in the area. It is situated on the western shore of Derwent Water within 3 miles (5 km) of the busy tourist town of Keswick.
The fell's unusual name may well have come from a distortion of "Cat Bields" meaning shelter of the wild cat, although this is not certain. The fell's name is sometimes written as Catbells.
Old stone bridge (Scale Bridge), Buttermere
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Over the footbridge towards Fleetwith Pike
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By Crummock Water
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Crummock Water looking north
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Sunlit High Ling Crag, Crummock Water
Over the footbridge towards Mellbreck
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