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GLACIAL GEOLOGY OF THE SARATOGA QUADRANGLE 9 



its geological origin is a fault scarp. Farther to the north the 

 country exhibits more distinctively the characteristics of the 

 Adirondack mountain region. The highest elevation is attained in 

 the summit of Mount McGregor, 1120 feet, crossed by the edge of 

 the sheet about 3 miles south of the northeastern corner. The 



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Fig. 1 Showing the surface contours in east-west section across the 

 Saratoga quadrangle — Horizontal scale, 1 inch = 4 miles ; vertical scale, 

 1 inch =1600 feet. _ The location of the sections on the map may be deter- 

 mined by the notations. 



