The Geology of the Lake District: And the Scenery as Influenced by Geological Structure

Author:   J. E. Marr
Publisher:   Cambridge University Press
ISBN:  

9781107492820


Pages:   238
Publication Date:   12 March 2015
Format:   Paperback
Availability:   Manufactured on demand   Availability explained
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The Geology of the Lake District: And the Scenery as Influenced by Geological Structure


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Author:   J. E. Marr
Publisher:   Cambridge University Press
Imprint:   Cambridge University Press
Dimensions:   Width: 14.00cm , Height: 1.30cm , Length: 21.60cm
Weight:   0.280kg
ISBN:  

9781107492820


ISBN 10:   1107492823
Pages:   238
Publication Date:   12 March 2015
Audience:   Professional and scholarly ,  Professional & Vocational
Format:   Paperback
Publisher's Status:   Active
Availability:   Manufactured on demand   Availability explained
We will order this item for you from a manufactured on demand supplier.

Table of Contents

1. Introduction; 2. Lower Palaeozoic rocks: A. The Skiddaw slates; 3. Lower Palaeozoic rocks: B. The Borrowdale series; 4. Intrusive igneous rocks connected with the Borrowdale series; 5. Lower Palaeozoic rocks: C. The Coniston limestone; 6. Lower Palaeozoic rocks: D. The Stockdale shales; 7. Lower Palaeozoic rocks: E. The lower Coniston flags = Brathay flags; 8. Lower Palaeozoic rocks: F. The upper Coniston flags, Coniston grits and Bannisdale slates; 9. Lower Palaeozoic rocks: G. The Kirkby Moor flags; 10. Discussion of the conditions under which the rocks of lower Palaeozoic age were formed in Lakeland; 11. The changes at the end of lower Palaeozoic times; 12. The changes at the end of lower Palaeozoic times (continued); 13. The carboniferous rocks; 14. Post-carboniferous changes; 15. Events in the district between the time of formation of the dome and the glacial period; 16. The glacial period: the ice-sheet; 17. The glacial period: ice-erosion; 18. The glacial period: accumulation; 19. The glacial period: glacial overflow valleys. Oscillations of the ice; 20. Post-glacial changes; Index.

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