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Frank Carney 
stream and the many short waterways coursing down the steep slope 
south of the delta. The surface of the delta likewise shows many 
distributaries. The permanent post-glacial drainage from the 
west lies at the foot of the northern wall of the valley, skirting the 
delta; a slight brook also has sectioned its southern portion. 
‘‘F.’’ The local gravel pit at Moravia is in this delta, the sur- 
face of which averages 885 feet in altitude. Fig. 23 gives a general 
view of the crest of this delta. Stream erosion near its north side 
Fig. 23. Deltas “F” and “G” from west slope of valley. Camera stands about 
200 feet above floor of valley. Inlet stream shows in foreground. 
reveals till deposits beneath the gravel. This same relation of 
unmodified drift has been disclosed also by the creek flowing 
westward from Montville. The village cemetery between Mor- 
avia and Montville is located on this delta. No development of 
it was mapped with certainty south of the highway from Moravia 
to Montville which follows, for the most of the distance, the bed 
of an inter-, or abandoned post-glacial stream. 
iiQyy This is the largest delta of the sheet; views of it are 
shown in figs. 23 and 24. In altitude it ranges from 1010 to 1060 
