62 
Another place to study the conglomerate Is along the road 
turning southwestwardly in block V/Y.9M, just east of the branch road run 
nlng north at 1^00 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 was has almost all been washed away .leav- 
ing the road full of boulders. The conglomerate here is very peculiar in 
that it consists almost entirely of dmall white pebbles with usually no 
imbedding matrix whatever. Fossils of course, are not easily found.On the 
other hand in the higher series of boulders there was observed a slab 4 
thick &lft. square with only a few larged" pebbles. In the lower series 
ther are a couple of slabs 2ft. square and over 6" thick and with '■ardly 
ary imbedding matrix.Some of the pebbles are as much as 1 thick. At lo40 
in the road .lust west of the house shown in V/Y.9M at 1360 are found a 
few very little worn specimens of the conglomerate, while an occasional 
more or less worn specimen is fou d all the way down int* the valley of 
tha Chemung. 
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