Plate XXX. 



General plan for the geological structure of Mino, Owari, and Ecliizen, in wLicli 

 are shown the regular course (blue lines) of valleys from N. W. to S. E., indicating 

 the positions of the pro-existing transverse fault, and the black lines being the 

 direction of the strike of Pahçozoic complex, with the dips as marked with the arrow- 

 heads. The heavy red line is the course of the ' great fault of Neo". 



