Fossil Corals sollactsd toy Dr* Krnast Hows in th« ffsat Indies * 
Description off localities whence corals were collected* 
Specimens Gda* 2, 3, 4, 5* 
&ain*d coral reef, L&umni Feint, west of Sauteurs, St. Pat- 
ricks Parish, Granada* 
At 2S0 fast above sea level, where th® road crosses the end of 
L&urant Point, there are ejtpesqres of a -raised coral reef. It rests tip- 
on a fine-grained, decomposed rock, probably tuff* With the exception 
of veins and scams &£ calcareous material, the first true limestone I© 
& hard, massive rock composed of corals in place and growing on a rock 
composed of tuff in large and small frapseats and minute shells* This 
bed variss from 1 to 18 inches in thickness. {Specimens numbered Gda.2 
from this horizon*) 
0«i«u2* StBphmoeoanim intersept® (Eeper) 
Por it a s 9 £»« 
Above this ho risen , and of unknown thickness (about % or 6 feet 
from base to present upper surface) la & marly limestone filled with 
stag-horn corals ( Gda* 3 ) much broken and wave-worn. This bed contain© 
much volcanic material scattered through it In the form of fine sand, 
hornblende being prominent* 
Gd&. 8* Acropfra muricata (I4mu) ? 
On a hundred feat below this locality the same beds outcrop and 
the same general sect ion of the limestone occur© ( Oda* . 4 and 3 ) with, more 
marly limestone above# Under the limestones are 4 feet of thin -bedded, 
fine-grained tuffs, and under these a massive , decomposed rock# At this 
