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clusion as to the relative position of the two schists, 
by traversing the little glen which leads down to 
following these along the shore I could come to no 
PROF. T. G. BONNEY ON THE GEOLOGY 
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at one place on the southern side the beds dipped pretty clearly to 
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the cove, I found that I only lost sight of the mica-schist beneath 
the turf for a very short distance, and have no doubt that the rock 
exposed in the headlands on either side of this cove belongs to the 
same bed, and that the sea has cut across the crown of a sharp arch 
which brings up the underlying chloritic schist (fig. 3). 
