64 Notice of Mr. Schoolerafi’s View of 
(p- 170) as being 
imbedded in it or ly 
gnei 
a 
granite in mountain masses, with some veins of green stone 
green stone porphyry, and gneiss ;”. it is said to terminate in 
very roug 1 and broken high lands. At page 213, itis men- 
tioned, still again, as giving ongin to the river St. Francis, 
and green stone porphyry, are among the larger masses of 
eu k “9 Th ~ : it see - ag . 2 
, ying promiscuously among the fragments 
| have tumbled down from the lofty cliffs 
is — porphyritic by crystals of greew and 
dspar.”” ale ca Ree ‘leer Baten: 
ght to doubt that the rock deseribed is 
incipal features delineated, correspond with 
As it is described as being» solitary, the 
