THE POSTGLACIAL CONNECTICUT AT TURNERS FALLS 469 
on the higher land between Lake Pleasant and the next kettle 
to north. The gentle hollow in the foreground represents the 
ground between the kettles. The tree tops in the middle dis- 
FIG. 5. 
tance indicate the location of the kettle." Fig. 7 was taken to 
show that even if the kettles were filled up, there would still 
remain a shallow valley in the plain. The deeper southern por- 
™ This kettle, like the 100-foot cliff at D and some other features, does not appear 
on the Greenfield topographic sheet. ‘The Lily Pond ridge also is quite misrepre- 
sented. 
