TOPOGEAPIIY OF THE SAGAJII SEA. 



15 



is to be explained by the comparatively steep incline of the 

 bottom and the proximity of much greater depths, — offers ex- 

 ceptional facility to those who wish to study them. And to this 

 circumstance must be ascribed in great measure whatever success 

 I have had in collectins mv Hexactinellidan material. 



Mei-a 3. :Nrera 2. Mora 1. C. Mera. 





View of Cape SmiosaUi witli tlie ilera hills in the background. Seen iVom a point 



on the line ' Mei'a .".' 



