728 FRANK CARNEY 
Directly west of Moravia at approximately the goo-foot contour 
is another area showing numerous striations which have an average 
direction of S. 37° E. The surface at this place is slightly steeper 
than that just noted. It also stands higher above the flood plain 
below. 
East of Moravia near the forks in the highway leading up the hill 
is another area of very active ice-polishing. Its altitude is 830 to 
Fic. 4.—Glaciated surface southwest of Moravia, N. Y. 
860 feet. We note here, however, two sets of striae; the stronger 
measures S. 56°-63° E. This set probably represents the general 
movement of the ice-sheet, modified perhaps slightly by local topog- 
raphy. ‘The direction of the weaker set is S. 19°-25° E. It should 
be noted that this surface stands at an angle in the Owasco Inlet 
valley. The north leg of this angle has approximately the direction 
of N. 32° W., and the south leg, S.8° W. Leading into the major 
valley from the east a tributary valley enters at this point. The 
striated surface, however, is some 100 feet below the rock bottom of 
this tributary valley which in accordance with the recent literature 
would be called a “hanging valley.” It is possible, therefore, that 
