Another place to study the conglomerate is along the road 
turning southwestwardly in block WY.9M, just east of the branch road run 
nine north at t^oo A.T.The specimens were not found in situ, but occur 
in two courses in the road from 1350 - 1365 and from 138:- 1392. No spec- 
imens were found higher up. The road here and further west also is very 
hilly and whatever soil there vras has almost all been washed away , lea 
ing the road full of boulders. The conglomerate here is very peculiar in 
that it consists almost entirely of dmall white g "° e 
imbedding matrix whatever. Fossils of course, are not easily -ound On the 
hand ln Ul e higher series of boulders there was observed a slab 4 
S5S “nlSi iu, only . f« W# pebbles. In U,e .«i~ <■ 
ther are a couple of slabs 2ft. square and over 6 thick and with h a d y 
ary imbedding matrix. Some of the pebbles are as much as J ^lre'fonn a 
in the road .lust west of the house shown in V/Y.9M at 1360 are found a 
pew very little worn specimens of the conglomerate, while an occasional 
more or less worn specimen is fou d all the way down into the valley of 
tha Chemung. 
- r • ~ 
3S? 
PPEVALEN 
SO* 1 ? LTN 
