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BULLETIN OF THE NATURAL HISTORY SOCIETY. 



Further along the street, eastward, hut off" it to the south, 

 there is a space ahout two hundred and forty feet from 

 north to south, going up the hill where the slates are 

 well exposed. For ahout one hundred and fifty feet of 

 this space the glacial striae and faults are well shown ; 

 beyond this, higher u\) the hill, the rocks are too much 

 weathered to give trustworthy results. 



The striiTe at this locality have a course of south, five 

 degrees west, and the fault planes along which the prin- 

 cipal displacements have occurred, have, as at the City 

 Road locality, a course of north, sixty degrees east. 



The following faults were observed here, beginning 

 at the north side of the exjiosed ledges : 



* Down-throw on south side, all other down-throws on north. 



