FOSSIL PLANTS FROM VERO. 
33 
there are it seems to me but two alternatives, and these apply equally 
and are in large part derived from a study of the physiography and 
the faunas and floras of the corresponding topographic forms in the 
other states of the Coastal plain. These alternatives are that they 
are about the same age as the Peorian interglacial deposits of the 
Mississippi Valley or are. immediately post Wisconsin and corre¬ 
spond with what the Scandinavian geologists have named Litorina 
time. 
