Review of the New York Geological Reports. 61 
ner of basaltic columns. A magnificent coral of snowy white- 
ness, of similar structure, with the prisms more than a foot long, 
and in masses weighing nearly a ton, was discovered many years 
ago at Charleston Landing, about eight miles above the Falls of 
the Ohio, in the coralline beds already referred to. 
{— riodoSusulig ‘g ‘snyunp unjhydoywhg -% ¢—— wn hydoymhy “1 “Hy 
‘gtd Saodoy 8, (ep 
Until the internal structure of Fig. 1 is described, it would be 
premature to decide upon its identity with fossils of other locali- 
ties ; but in its general form and external appearance it resembles 
a species found in abundance at Utica, a few miles above the 
Falls of the Ohio, and elsewhere in that vicinity. 'The same lo- 
cality also fi I that are doubtless the same as Fig. 2. 
