IN NOVA SCOTIA. — WOODMAN. 235 



escarpment of the plateau, the northern edge of tlie great west- 

 ern granite massif, which runs from near Windsor to a point a 

 short distance east of Yarmouth. 



(8) The line of disturbance on the south shore of the pro- 

 vince remains unaccounted for. Additional data may show the 

 back country to have been affected, or they may not. 



(9) No information whatever has been given by observers 

 underground or on the water. It is particularly desirable that 

 data should be collected from these two sources, with a view to 

 establishing direction and relative intensity of shock, and 

 character of sensation, as compared with observations in 

 houses. 



