Frank Carney 
some three-quarters of a mile is very kamy both in surface appear- 
ance and in texture. 
From Benson Corners the drift for one and one-half miles 
south and east is made up of a maze of water-laid hills, (fig. i6), 
most irregularly distributed. Locally this belt of moraine is over 
one-half mile wide. Also, the kame aspect is very marked along 
the ice-front southwestward toward Asbury. 
In the vicinity of West Dryden the kame type likewise charac- 
terizes the drift. Indeed, the isolated areas in which water-laid 
moraine prevails are found irregularly scattered about the whole 
sheet. 
In this rather detailed inventory but two more particular locali- 
ties need be mentioned. Immediately westward from Fitts 
Corners the kame aspect of the drift is accentuated. This locality 
is on the divide between the Moravia-Freeville valley on the one 
hand and Fall Creek valley on the other; apparently ice-front 
waters had free drainage. These kame hills, therefore, have a 
topographical location that suggests quite a different genesis from 
the kame areas already described in, or adjacent to, valleys. 
Again, about one-half mile northeast of Morse Mill there is an 
extensive deposit of kame drift; and the water-laid moraine con- 
tinues northward, but not so well developed, into the next sheet. 
(6) Eskers. On this sheet two general types of eskers exist: 
(i) Those due to local topographic control; these are short, 
usually transverse to the direction of the valley axes, starting on 
one wall and terminating not far from the foot of the slope; (2) 
The other type appears to be less influenced by the minor details 
of relief. A full description of eskers appears in a later section. 
(7) Flood Plain Deposits. These deposits are of two types: (i) 
Valley trains, the form developed in narrow valleys between morainal 
loops. In the valley of Fall Creek, and in a portion of the 
Moravia-Freeville valley, the valley trains attain typical develop- 
ment; they are discussed in detail later (p. 392). (2) Outwash 
plains noted especially at the wide triangular junction of twoor more 
valleys where the several distributaries from the ice-front built up 
individual fans which coalesced into outwash plains. A few areas 
in the uplands have also been noted, bearing this same type of 
drift. 
(8) Lake Bottom Deposits. The high-level lakes, held by the 
ice in the topographical basins of the sheet, are marked by a 
I 
