TERMINAL MORAINE OF PUGET SOUND GLACIER 163 



moraine is built far enough to the south to lie in general over rock 

 surfaces above sea-level; indeed, the moraine forms a fairly con- 



GLAC1AT10N OF PUGET SOUND 



ffo-r/zontat Rutmg Extent of fas/?on G/aci at/on 



l/erf /cat Rul/ng- _ . On East - Cascade /Ve^e and / ce 



On West —O/ym pic Afe/e and tee 

 Dotted Areas Extra-mo ra/ni c l/ashon. Outwash 



stant boundary between the depressed region to the north, now 

 drift filled, and the rugged, stream-carved rock hills southward. 



The field work on which this paper is based has been done under 

 some difficulty because of the undeveloped nature of the country, 



