246 J. D. Dana on a Mohawk-valley Glacier. 
exactly conforms to the present trend of the valley, as shown on 
the accompanying map. ‘I'he line CY corresponds to the trend 
of the valley, and MK to that of the Mohawk vallev; and the 
two sets of lines, NS and WE, correspond to the direction of 
MAP OF CHERRY-VALLEY REGION, 
~ 
gs, 
Bry 
Sy 
‘ 
A, Cherry tile da village ; B, Burned Hill; CY, Course of the po Valle 
led 
ae a 7 ; oy 
t systell 
the pied glacier courses. ” The direction of the rma ot 
of these scratches is about north-northeast and south- south net 
varying to north-by-east and south-by by: -west, and that of the da 
about east-by-north and west-by-sor 
“The Onondaga limestone of sh e region is, in ma 
{as one the village and Judd’s Fa i oe paca 
hed, the scratches being ch 
deeply se , 
system 0 prions The same ean is pet Y hibited on. 
side of the road leading to Fort Plain (at G), one and a a 
