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boulders “of those rocks on the side of Dent, two hundred feet 
above the level of the watershed of the valley that runs through 
between Dent and Kinniside to join Uldale. The reason of this 
curious disposition of the boulders we cannot now undertake to 
consider, nor can we enter upon the many trains of thought 
suggested by the facts that have been brought forward. The 
subject of which the distribution of boulders forms a part, has now 
become so much elaborated by the combined efforts of its numerous . 
investigators, that I should have to trespass too much on your 
time were I to attempt an explanation of the many facts that have 
just been reviewed. I prefer therefore to leave them at present 
for each to interpret and correlate for himself. On some future 
occasion I hope to return to the subject. 
