88 J. G. GOODCHILD ON THE GLACIAL PHENOMENA OF THE 



thin sheets of laminated clays (fig. 10). Throughout the section the 

 stones comprise a larger proportion of waterworn materials than 



Fig. 10. — Section in Throstle-Hall Cutting, Settle and Carlisle Railway. 





O/v- 



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T ^SJZ>^> O^ 





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Intercalations of sand and gravel in till. T. Till. S. Sand and gravel. 

 Length 6 ft. 



may be found in the clay of the same kind at Longwathby. The 

 lamination of the gutta-percha clays is very well marked, and seems 

 to run in no well-defined general direction ; it is frequently inclined 

 at several degrees from the horizontal, and occurs in such a way 

 that it cannot possibly be the result of any thing but original 



Fig. 11. — Section in Settle and Carlisle Railway-cutting at Throstle 



Hall. 



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'p'oO <=>' o 



>-0 



Gutta-percha clays in lower till. Length 4 ft. 



deposition. Kg. 11 will, perhaps, make this clear ; it represents a 

 length of about 4 feet of the stony clays of the cutting, over the 



