iets is Ap teea se 
eres. 
Conglomerates with Gneiss, Talcose Schists, é-c. 381 
farther at Wallingford, are completed in the most satisfactory 
manner. 
It is at Plymouth, along the west shore of Plymouth Ponds, most 
fully developed, perhaps, just where the ponds are separated by a mass of 
detritus, which was most probably the moraine of an ancient glacier, as 
will be described in our Report on the geology of Vermont. 
8. 
The schist, which here is decidedly talcose schist for the most part, and 
not far from some of the gold diggings 
i : 8 
rock, or if it be broken across, in the direction of the strike, the pebbles 
will for the most part, appear so flattened that they become almost len- 
9. 
