3. CENTRE TOWNSHIP. F a . 211 



The only conspicuous evidence of the fault east of this 

 point is the repetition of the Hamilton upper shale without 

 inversion and the presence of the Genessee between the two 

 outcrops. The lower outcrop is at the fork of the road near 

 Mr. Sanderson's, and the higher at Mr. Wm. Brunner's. 

 In both cases the lower beds lie to the north. A plan of 

 the fault may be found in the account of Spring township. 



