J. D. Dana— Geology of Vermont and Berkshire. 45 
fig. 14 and the limestone are conformable. But there is also 
demonstrative evidence of this relation in sections. Fig. 1 
Stone and overlying gneiss) are in contact, and so also are 9 
and 10 (quartzyte and overlying gneiss). No, 1 is the east- 
ern border of the limestone of the Konkaput valley. The 
Sas aE GEESE ~ SS 9 
Three-mile Ridge, west side [UE ae HERE 5 1 8 
of Konkaput Valley. Devany’s Quarry, east side of Konkaput Valley. 
°F schist. This schist is mostly a whitish and gray gneiss, Hak 
tough and hard ; but with it there is granulyte, gray and blac 
mica schist, and blackish bornblendic schist. 
* This Journal, III, v, 84. 
