460 Serentifie Intelligence. 
Such a conclusion is at variance with the fact of the exist- 
ence of Lower Silurian fossils at some Vermont localities in the 
of the Nashua Valley, by L. 8. 
of Vigo and Huntington counties, by Mr. Cox; of Riply and Jen- 
nings counties, by W. W. Borden; of Orange, by M. N. Elrod 
and E. § i 
a depth of 3,000 feet; the first 88 feet were of drift; and then it 
entered a Niagara limestone, and continued through limestone 
and calcareous shale to 2,500 feet ; thence, through soft caleare- 
L 
upper stratum.” In another well 1,923} feet deep at Terre ape 
lieved, in the N iagara, the temperature obtained throug nie 
was 81° F.; and this is referred to waters from the lower part of 
the well filling it. 
