87 



In cases where anticlinoria emerged, not contiguous to existing land 

 areas, it seems wlioUy within the prol)ahiIities that many of the transverse 

 streams assumed and maintained their courses across the minor folds of 

 the limbs. It has occurred to the writer tliat possibly this has been the 

 history of some of the numerous transverse streams in the Ouachita area 

 of Arkansas. 



