*e same band may be used to demarcate the lower dlmits of the 
Chemung. 
B. Some distance west/o# 7E7&8, or 
south 1 side of the 
of arenaceous 
also 
road* t'herd crop out between 1215somd '30 __ _ 
beds with little if any biocky/ shales; but with a small amouht of 
1 ami hated shales and flags. No fossils were found except in one of 
the harder layers at 1 S3 5ft . A . T . The fossils here are Schizophoria 
impressa,Productella Tachryrnosa, and a bulbous or pyriform crinoid, 
some calyces and joints of which have been found(7B5). 100yds. s.w. 
in the bat* of the stream, at 1228ft. A. T. , the same bed is found wit 
" ““ disjurctus velmarcyi. This shows a declination of ah 
lie, a few degrees w.of S. Taking into consideration 
aip of 7B3 & 7B4 f there is seen to be an anticline, with an axis 
directed E.10S by WHO N,, approximately, ana having the greater 
pitch southerly. 
■ v/' ; ** m , 9fi 'i Wy * r • ■ • : ’ 4 y d* 1 • >. - '4f'* •*» •, y;* 1 ' 1 .. ■ • ■'>*• - ,v-' . *• •• ♦ * * . **-1%** ' 
9. At 1229f t . A.T . , in the creek is a brown flaggy layer 
( 7B6) with Ambocoel ias , Or this impressa, Spirifer nesacostalis, and 
many Leptodesmas;but apparently no$ in place ^he label is orobabl 
7B5 .5 . 
•• . • - , \ ■ * , % | /*'*% , v '• : *- f -r - ■: • • V . 4 ***, / -f * •' <Hjf , V . 
10. Above 7B5, therea are several more small outcrops of 
arenaceous beds, but Schizophoria impressa seems to be the only 
fossil met with. 
* .... .. - • 
■'fc 'A M .*#$>■&' v •• • #< f; , -V^W t ' A<‘ >'■ V ■, V:*' -f -*X ^ .. «. 
1610ft .A. T. , the Tropidoleptus zone crops out on 
the south side of the road. This zone consists , of 3or4 2 , 'to4 tt hard 
comDo-p^nf^^F 16 middle 1 or 2 inches of which is in each band 
