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

令人發(fā)膩

Tarn Hows and the Coniston Limestone (1:25 000 maps NY30 and SD39),ooded, supplied with concealed car parks and well provided with footpaths, some of which cater for wheel-chairs. It is a place for a delightful family stroll, one which includes toddlers and grandparents. It is also a place of great geological interest. The junction between the Borrowdale Volcanics

endure

The Brathay Flags of Banishead, Coniston (1:25 000 map SD29),he dip is usually to the south-east at 30° to 40°, although there are a few minor folds in some areas, Tarn Hows for example. The lithology is unique 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

貪婪地吃

DUCE

The Coniston Grits and Bannisdale Slates of Shap (1:25 000 maps NY50 and NY60),hap Wells. The area south of Shap Summit described here is perhaps not so well known but it is interesting. The exposed rocks are Coniston Grits and Bannisdale Slates of Silurian age, outcropping in the major Bannis-dale Syncline which crosses the greater part of the Lake District. It will be notice

Limousine

heirloom

Conclusion,ion. However, the topography and geology are diverse and there are areas and subjects I have not dealt with. The geological literature on the Lake District is enormous, and even before 1973, when the Cumberland Geological Society published R. A. Smith’s bibliography, there were more than 1000 books

Foreknowledge

,Einführung: Beispiele und Grundbegriffe,with at least some of the fundamentals. This is not necessarily so, however, and many who are expert in their own field can easily think that other disciplines are too specialised for their attention, that the subject matter may not interest them, or that there is little time in a busy life to maste

配偶

gimmick

,Erforschung der Differenzf?higkeit,geology and the solid rocks. It is not an arduous climb from Newlands Pass at 340 metres to High Snockrigg at 530 metres (NY 187 169), and it is an advantage to go on a clear day armed with binoculars when all the details of the topography can be picked out (figures 10, 11 and 12).

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