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Skiddaw
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Skiddaw
The eastern side of Skiddaw drains into Skiddaw Forest, much of the water reaching Candleseaves Bog. Geology
The bedrock of Skiddaw, commonly known as Skiddaw Slate, is the Kirkstile Formation.
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Skiddaw
Skiddaw Geol. (ˈskɪdɔː) The name of a mountain in the English Lake District, used attrib.: (a) in Skiddaw slate(s) (or Slate(s)), a thick group of slates, flags, and mudstones that outcrops in the northern part of the Lake District and out of which Skiddaw and neighbouring mountains have been eroded...
Oxford English Dictionary
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Skiddaw Group
For the Skiddaw group of hills, see Skiddaw Group
The Skiddaw Group is a group of sedimentary rock formations named after the mountain Skiddaw in the This rock sequence has previously been known as the Skiddaw Slates, the Skiddaw Slates Group and the Skiddavian Series.
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Skiddaw Little Man
To the north and east Little Man is connected to the Skiddaw massif, Lonscale Fell being the nearest separate fell to the east, away. Ascents
Many people climb Little Man via the tourist path from Keswick on the way to the summit of Skiddaw.
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Skiddaw Slate
Skiddaw slate is an early Ordovician metamorphosed sedimentary rock, as first identified on the slopes of Skiddaw in the English Lake District. In some places, there is evidence of intrusion of Skiddaw Granite into the Skiddaw Slates, close to the anticlinal axis of the Lake District.
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Musical Stones of Skiddaw
The Musical Stones of Skiddaw are a number of lithophones built across two centuries around the town of Keswick, northern England, using hornfels, a stone [5] “The Origin of the Musical Stones of Skiddaw”, by Dr. Alan Smith and Professor Bruce Yardley.
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Dodd (Lake District)
Computer-generated summit panorama
Skiddaw Hermit
In the 1860s, Dodd was home to a Scottish hermit called George Smith, who became known as the Skiddaw A short book was written about him in 1996 called the "Skiddaw Hermit" by Mary E. Burkett.
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斯基道峰
参考文献
外部连结
Skiddaw is at coordinates
Computer-generated virtual panoramas North South Index
Skiddaw photos, information and walks
湖区山峰
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Ullock Pike
Skiddaw, with Alfred Wainwright commenting:
‘There is no doubt in my mind that by far the best approach to the top of Skiddaw is by way of its north-west Geology
In common with much of the Northern Fells the Kirk Stile Formation of the Skiddaw Group predominates.
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Lonscale Fell
To the north of the fell is Skiddaw Forest. The single building in Skiddaw Forest is Skiddaw House, which has variously seen service as a shepherds' bothy and a Youth Hostel.
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石板琴
录像
The Musical Stones of Skiddaw being played
Video of the Great Stalacpipe Organ
The Parkbench Lithophone
The Ringing Rocks of Montana
键盘打击乐器组
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River Caldew
Source of river
The River Caldew's source is high up on Skiddaw, between the summit and Sale How. Course of river
From its source in the Skiddaw Forest the river runs east through a valley between Bowscale Fell and Carrock Fell.
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Mungrisdale Common
the area colloquially known as 'Back o'Skiddaw' to the north. The watershed continues across Skiddaw Forest between the headwaters of the Caldew and Glenderaterra, linking onward to Lonscale Fell in the Skiddaw range
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Great Calva
The three groups of fells can conveniently be thought of as the Skiddaw massif, the Blencathra group and Back O'Skiddaw. The single building in Skiddaw Forest is Skiddaw House which has variously seen service as a shepherds' bothy and a Youth Hostel.
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Bakestall
Dead Crags are composed of Skiddaw Slate and drop down into the corrie on the northern side of the fell. Ascents
Bakestall can be climbed as part of the less crowded northern approach to Skiddaw using the rough track to Skiddaw House (part of the Cumbria Way
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