EDEN VALLEY AND YORKSHIRE-DALE DISTRICT. 



83 



water All the beds incline more or less towards the lowor end of 

 the valley ; but some small sections at right angles to the axis of the 

 drumlm show that the false-bedding planes slope outwards towards 

 the sides of the drumlm as well. Fig, 3 shows a small section 



Fig. S.— Section in the Settle ami Carlisle Railway -cutting at 

 Culgaith. 



Section at right angles to the axis of a drumlin. T. Upper till. S G Sand 

 and gravel. C. Laminated clay. T'. Lower till. r. Kock. Length 10 ft. ; 



exposed by a slip of the beds nearly at right angles to the axis'of 

 the drumlin. The lowest beds seen were of till full of glaciated 

 stones from the lower part of the basin of the Eden and from 

 Galloway. Lines of sand, and lenticular patches of laminated gutta- 

 percha clays, inclined at angles of about 30° towards the side of the 

 drumlin, serve to mark the stratification in this bed. Lying upon 

 the till, with an uneven line of junction, is a series of finely laminated 

 striped clays, having a thickness of from 3 to 9 feet (fig. 4). The 



Fig. 4. — Section in the Settle and Carlisle Railway -cutting at 

 Culgaith. 



Part of No. 3 on a larger scale, to show the irregular lamination of the clays 

 the drift. C. Laminated clays. T'. Lower till. Length 12 ft. 



02 



