Page:Transactions of the Geological Society, 1st series, vol. 2.djvu/69

Rh other, a subsidence to the south of the whole chain “en masse” took place, which caused the three dislocations referred to in the course of this paper, and which are nearly at right angles with the direction of the chain itself.

2. That the same subsidence may be supposed to have produced the general dip of the stratified rocks to the southwards.

2