6i2 CLARENCE N. FENNER 



position either on the strike of the Kmestone or closely adjacent. 

 The strike of the limestone bed is parallel to that of the associated 

 gneisses — an indication that part at least of the foliation is to be 

 attributed to an original bedding. The manner in which minerals 

 from the magma may have been introduced into the limestone and 

 other sedimentary beds will be considered in the discussion which 

 follows. 



[To be continued] 



