5ULI . (,l-i )| , sue. AM. 



VOL. 10, 1898, PL. 33 



Fku'IvK 1. — Sr.c'TiiiN (IN Pi,i:.vsANi' .S'i'UKKT, NKAi; \Vasmin(;i'o.\ Avknue 

 Hhovviiig (liiiiy sniul oC (.•on.siileriibk' thickness overlying stratitiL-il sunil and pelphly till 



Fuii'KK -. — Skctihn at Foot of 1'i.kasaxt SiitKiri' 



^linwini; ancient river tsraxel covered liy .stratitied sand and peat and underlain by Trenton limestone. 

 Taken at point '\f" in generalized section, figure 2, page ;;(j(i 



FlIiUKE ;!. — !;^ECTIOS TO EASTWARD OK THAI i<V FoilRK 1 



Lag gravel covered liy dune sand. Eolian deposits overlie till whi( h extends from eroded surface 

 ilownward to top of limestone. Taken at point "y"' of figure -2, page 3110 



EOLIAN DEPOSITS IN MINNEAPOLIS, MINNESOTA 



