666 EDWARD W. BERRY 



aspect which survived in Florida to the late Pleistocene. With 

 regard to the exact age of the Vero deposits 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 correspond with 

 what the Scandinavian geologists have named Litorina time. 



