UEOLOGIC STRUCTURE OF THE RIUFvlU CURVE. (;7 



the East Indies, and with the Lesser Antilles in the W^est Indies. 

 Though our islands have been only slightly disturbed by volcnnie 

 action in the southern part, yet they show the type of folded moun- 

 tain with parallel structure, as already treated in the preliminary note 

 of Prof. Koto, and ascertained by my own observations in nearly 

 all the islands of the interesting Kiukiu Curve. 



March 1901. 



