of the Maumee Valley. 



titi :u ?tiniatelv with the confiLmration of the vallev, and 

 tow H !i,'^'''"^^^^"«f tl^e ice markings; its concavity is turned 

 UiT. ^ ^}^ '^^^«e o^ motion ; its greatest convexity is along the 

 ^v-^f yeast resistance. The notch at Fort Wayne, through 

 wh n? ^ Maumee flows, was perhaps first cut by the river to 

 cleaned J T^^tiring glacier gave rise, but has certainly been 

 ^ 01 the subsequent deposit of clay by a later current,— 



