ISO 



NEW YORK STATE MUSEUM 



The beds are gray and nodular with redder strata. The outcrop 

 is in the strike and the beds apparently rise uniformly into the 

 Murailles. A displacement is evident along the bed of the brook 

 but its amount was not estimated. Red peak, which is the highest 

 and easternmost of the Murailles, is said by Logan to 



Le Coule. Nodular limestones and limestone conglomerate 



be capped by horizontal beds of " the conglomerate " which 

 I take to mean the conglomerate of Mt Ste Anne (Bonaven- 

 ture) but I was not able to verify the observation, the beds here 

 being apparently conformable in dip to those below. The displace- 

 ment of the tinted Perce strata (the term Perce is here used as 

 indicative of the horizon of the Perce rock) against the Cap Barre 

 beds is evident on the south road leading up the mountain side to 



