95 



This description of the clay applies to the layer I have 

 marked as T. i. in PL ii. fig. 4, and also in the accom- 

 panying cuts. In the left hand figure the T. ii (the T. i of 

 the Plate) ovedies gravel, the squeezing up of which is 

 usually less marked than this. In the right hand figure 







i>.i>^ 



from Slade s Green, is shewn a remnant of a crumpled 

 ayer, the U.P. of a trail I have marked T. iil., and wLh 

 I have taken to be the same layer as that shewn in PI ii 

 fig. 7. coming down the cliiF. The layers of glaciated land- 

 scrape or boulder like clay, for the trail does not look like 



