Some Notes on Mount Royal. 



521 



Incline Eailway, which includes the bold, almost perpen- 

 dicular bluff, is encumbered by large blocks of Theralite 

 to sncl) an extent that it is difftcult to determine the 

 limits of the different formations, but at least a fairly 

 approximate idea can be formed as to their position from 

 the exposures which can be seen at different points. 



Here the altered limestone is also found exposed at 

 different places, and towards the Cemetery it reaches well 

 up to the top of the mountain, from which point it 

 appears to extend across the Cemetery in the direction of 

 Westmount. 



Fig. 3. 



From the Cemetery gate, the division between the two 

 formations runs in almost a direct line past Outremont 

 Quarry, to a point near Cote des ISTeiges, where it crosses 

 the Electric Eailway, Fig. 3, and then re-crossing it in the 

 direction of Westmount, passes under a heavy deposit of 

 drift, by which it is concealed until it re-appears at the 

 foot of the West-mount, or the Little Mountain. 



From the Mount Royal Cemetery gate to Westmount 

 there is a continuous and extensive exposure of altered 

 pmestone, that found in the Outremont Quarry being 



