178 W. J. MILLER PREGLACIAL COURSE OF UPPER HUDSON RIVER 



direction, and the Hudson behaves in an almost identical way, although it 

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STREAwj} —-- — —-.— 



Figure 1. — Sketch Map of the southeastern Adirondack Region 



Showing the relation of pre-Glacial drainage to that of the present. Pre-Glacial courses 

 shown only where essentially different from present streams 



