Xll 
THE GEOLOGIST. 
formations wliicii he examined agree well in zoological types with 
the eocene and miocene beds of England and France ; that he 
found no secondary fossils in those rocks which have been called 
upper secondary^ but that all the organic remains of the inter- 
mediate beds are characteristic of lower tertiary beds. 
With this brief remark we will take our leave of the subject, 
leaving such of our readers as are interested in any of the more 
minute details to be deduced from the subjects under considera- 
tion, to refer to the essays themselves of which we have pub- 
lished copious reports in these and preceding pages. 
The Editor. 
