390 



E. W. Berry — Pleistocene Flora of Alabama. 



The following species were identified from this outcrop : 

 Osmunda spectabilis, Pinus taeda, Arundinaria macro- 

 sperma, Betula nigra, Pag us americana, Quercus nigra, 

 Quercus prinus, Quercus phellos, Carpinus caroliniana, 

 Ostrya virginiana, Vlmus alata, Hicoria villosa, Juglans 

 nigra, Populus deltoides, Liquidambar styraciflua, Nyssa 

 bijlora, Yaccinium corymbosum, Xolisma ligustrina. 



IjOcality No. 5. — This locality is on the left bank of the 

 Chattahoochee River and therefore in the state of Georgia. 

 It is about one mile above the Abercrombe Landing exposure 

 and is represented by three unimportant species found in pieces 

 of Pleistocene clay along the river cove and not in place. The 

 species are Arundinaria macrosperma, Betula nigra, and 

 Carpinus caroliniana, all of which occur in the Alabama 

 Pleistocene. 



Locality No. 6. — This outcrop is on the right bank of the 

 Chattahoochee River near Abercrombe Landing, about one 

 mile below locality No. 5 and was described in the article pre- 

 viously mentioned.* The following species new to this local- 

 ity were collected : Pinus taeda, Populus deltoides, Phora- 

 dendron flavescens, Acer sacchaninum. 



Locality No. 7. — This outcrop shows the Pleistocene in a 

 pocket of the Lower Cretaceous on the left bank of the Ala- 

 bama River abont one-half mile below Grun Island and about 

 12 miles above Montgomery. It is shown in the following 

 diagrammatical section (fig. 3): 



Fig. 3. 



Diagrammatical Section of the Cretaceous and Pleistocene at Locality No. 7. 



Section. 

 Pleistocene. 



1. Light yellowish, somewhat argillaceous sand, with 



gravel base about 20 feet 



2. Buff sandy clay with leaf impressions " 6 " 



* Berry, loc. cit., 1907. 



