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Titlebook: Geology and Scenery in the Lake District; F. Moseley Textbook 1986Latest edition Macmillan Publishers Limited 1986 District.geology.lake

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楼主: melancholy
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The Brathay Flags of Banishead, Coniston (1:25 000 map SD29),in the Lake District, consisting of uniform, fine-scale alternations of paler silt and darker mud as shown on figure 58. It will be noticed that there are approximately 10 layers per centimetre. The indications are that these striped mudstones accumulated quietly and steadily in a clay-rich sea.
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The Bannisdale Slates of Blawith Common and Beacon Tarn (1:25 000 maps SD28 and SD29),he rocks fall within the Bannisdale Slate Formation of Silurian age. They are banded mudstones with occasional massive greywacke sandstone ribs, which are more resistant to erosion and form ridges as indicated on figure 60. The banding in the mudstones is caused by the numerous paler silty laminae.
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Whitbarrow and the Carboniferous Limestone (1:25 000 map SD48),opping to investigate. Indeed it compares in beauty with any part of the Lake District, but it is limestone scenery and therefore quite different in character from other areas. A delightful walk starts near Witherslack Hall, and follows the footpath through the woods and on to the limestone pavements of Whitbarrow summit (figures 69 and 70).
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,Einführung: Beispiele und Grundbegriffe, they are kept simple and not confused by unnecessary jargon. I aim therefore to interpret the geological landscape of the Lake District so that those physically active members of our community who derive pleasure from fell walking will gain the added interest of knowing something of the ways in which the mountains were formed.
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,Differenzialgleichungen – wozu?,ften a question of ‘not being able to see the wood for the trees’, and I can think of a number of areas where the geology is obvious on aerial photographs but difficult to comprehend on the ground. On figure 24 the layers of rock can be seen to be inclined from left to right, that is towards the NNE at about 15° to 20°.
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