Table 6. — Range of Cretaceous fossils, region of Alabama River, Ala. 

 [Area on sketch map, flg. 2, p. 24.] 





S el mil chalk. 



Ripley 



forma- 

 tion. 



? 



So In i a chalk. 



Transition beds of Eutaw (ormalioii to Sol ma chalk. 



Eutaw formation (Tombigbeo. sand member). 





Ezogyja costata tana. 



Eatgyra pondcrosa zone. 





3 



1 



u 

 1 



I 



i 

 s 



□ 



I 



B 



I 



1 



a 



! 



•a 



5 



n 



i 



n 



! 



1 



5 



1 



1 



i 



s 



1 



i 



1 



1 



I 



1 



1 





Mortoniceros subaone. 



Species. 



1 



m 



I 



i 

 pi 



i 



a 



I 



1 



§ 



■a 



1 



if 



»■ 



-66 



? e | 

 ill 



I 



I 



i 



M 



U 



1 



s 



s 



1" 



S i 

 I 3 



9 



1 



1 



on 



s 



I 



t 

 1 



N 



SI 

 1 



I 



1 



B 

 ■a 



o 



1 



I 



3 



3 



! 



is 



3- = 

 'fit 



■a 

 | 



1 



1 



c 



i 



n 



= 

 i 



i 



1 

 s 



81 

 5 



M 



a 



| 

 E 



f' 



3 



3 



J, 



1 



m 

 1 



1 



M 



1 



1 



I 



g 



1 



i 



- 



s. 

 1 



I 



t 



! 



n 



o 



1 



i 



t 



I 



o 



1 



1 



Echinodcrmata: 































X 







X 















X 

























X 



X 



X 

























































Vermes: 









X 

























































jloliuscoidea: 





X 



X 



X 



X 

 X 





























































Molluscs: 







































































X 



































































X 



































































X 

 X 





































































































































X 











X 



X 





X 











































X 

 X 

 X 

















X 



X 



































































X 























































X 

 X 

 X 























































X 



X 



X 























































... 

























































































































































X 

























































































X 



X 



X 





X 



X 



X 

















X 



X 

 X 



X 







X 



X 

 X 























































































































X 

















X 



X 



X 



X 





X 



X 



X 



X 





X 







X 



X 



X 



X 







X 

 X 



X 



























































































:::::::: I"" 













X 







X 



















X 







X 











X 



X 

 X 



X 





































X 

























X 







X 



X 



X 



X 



X 



X 



X 



X 



























































X 























X 



















































X 













































X 



X 



X 



X 





















































































X 





X 





































X 



X 

 X 

 X 

































































































































X 



X 



X 

 X 









X 













































X 







































































































































X 

 X 



X 

 X 



X 



X 

























X 



X 





X 











































































































X 



''"v" 



X 



X 







X 



















X 















X 



X 

 X 



X 



































































































































X 





























































X 

 X 

 X 

 X 

 X 

 X 

 X 





































































X 

 X 

 X 

 X 

 X 



































































































































X 



X 



X 

 X 

 X 

 X 



























































































X 

























X 





X 



























































X 































































X 



X 

 X 



































































































































X 



X 



X 



X 













































































X 



















X 































X 



X 

 X 



X 

 X 

















































































































































X 







X 



X 



X 



X 











X 













X 







X 









X 











































































X 







X 





X 













X 













X 







X 













X 



X 



















































X 



X 



X 





X 









































































X 

 X 























X 



































































































































X 



























































X 





X 









































X 































































X 































































































.... 





























1 









172.— Bee. 24, T. 13, R. 10, east of CartowviUe, southwest of Minter, Ala. L. C. Johnson, collector. (Although the description of this locality is indefinite, the fossils 

 are probably from a horizon corn ^ponding to that at old Canton Landing anil in the upper pari of Prairie Bluff.) 



310.— The "Larry Dawson" blufl on Alabama River, just above the mouth of Tearup Creek. L. C. Johnson, collector. [Apparently a mixture of sevoral 

 near-by tor.ihli.r , In it .ill from practically tin? sauir liorizon.— L, W.S.] 



6439, 8789*— Alabama River, Old Canton Landing. Wflliox County, Ala., about U miles below the. mouth of Pino Darren Creek. L. W.Stephenson, collector 



270,0793.— Prairio Bluff, Alabama River, Wilcox County, Ala. L. C. Johnson and L. W. Stephenson, collectors. 



6791— Rocky Bluff, Alabama River, about a mile above Prairio Bluff, Wilcox County, Ala. (From chalk rock at top of section.) L. W. Stephenson, collector 



G794.— Shell Blulf on Shell Creek (or Prairie Creek), 5 miles southeast of Catherine, Wilcox County, Ala., a few hundred raids below bridgeo! Catherine- 

 Prairio Bluff road. L. W. Stephenson, collector. 



6790, 6792.— Hooto Bluff, Alabama River, about a mile above Prairie Blufl Landing, Wilcox County, Ala. (From gray marine sand forming lower part or bluff- 

 Rip ley formation.) L. W. Stephenson, collector. ° 1 



180.— Butto on natural mound, Mount Jones, near Portland) Ala. Sec. 12, T. 13, R. 9. (Horizon doubtful.) L. C. Johnson collector 



6S2-J. — One-third of a mile below the landing at Cahaba, Alabama River, Dallas County, Ala. L. W. Stephenson collector 



6S23.— Alabama River, just below railroad bridge at Selma, Dallas County, Ala. L. W". Stephenson collector 



64423.— Alabama River, House Bluff, about 12 miles above Benton, Ala.', right bank. (From base of SHma chalk.) L. W. Stephenson, collector. 



6146.— The Henderson place, V. or 3 miles south of Wetumpka, Ala. From beds near base of Selma chate. (This is a block of Selmachalk faulted down below 

 its normal position and thus preserved from erosion.) L. W . Stephenson, collector. 



64-17.— Adam Enscn's place, about 2 milessoutlloastofWetnmpka,Ala. From beds near base of Selmachalk. (This is a blocko* Selma chalk faulted down below 

 its normal position and thus preserved from erosion.) f,. W. Si rplien -on. collector. 



6832.— Field Just east of cut of Louisville & Nashville It. R., 2 miles southwest of the Union Station at Montgomery, Ala. (Weathered from beds near tho 

 contact between the Torabigbee sand member of tho Eutaw formation and tho overlying Selmachalk.) L. W. Stephenson, "collector. 



105°— No. 81—14. (To face page 24.) No. 6. 



a The numbers arc the collection numbers of tho U. S. Geological Survey; the collections are in the U. S. National Museum. 



307.— Alabama River, Morgans Landing, Autauga County, Ala. L. C. Johnson, collector. , , „ 



6S29.— In field one-h ,lf mile- west of Kenan's mill and .1 or :c. mil, - northwest of Selma, I 'alias Couiilv, Ala. L. W. Slepiieiison, collector. (These fossils occur 

 weathered from bi-ds near Hie contact between [be Tombighee sand member of the Kutaw formation and the overlying Selma chalk, ami doubtless a pari of them 

 camo from tho few feet of transition beds between tho two formations. However, some specimens are shown by tho adhering matrix to com o from bods beneath tho 

 transition beds, and these are judical ed in the table- as coming from a lower horizon.) 



141.— From BluegUt Creek near Selma, Ala. L. C. Johnson, collector. Parenthetical remarks under iis - 29 apply here also. 



142.— Southeast part of see. is, T. 17, R. 12, near Selma, Ala. L. C. Johnson, collector. Parenthetical remarks under iWH apply here also. 



140— Dug from bank of ravino In the NW. i sec. 14 on Valley Creek, 2-1 miles northwest of Selma, Ala. L. C. Johnson, collector. Parenthetical remarks 

 under Ijs29 apply hero also. 



321.— Near Hamburg. Perry County, Ala. I,. C Johnson, collector. Parenthetical remarks under HS20 apply hero also. 



205.— Prairies uf Ma :illon, Dallas Count v, Ala. (Weathered from tin' i ■cmiaitutig slrala.l L. C. Johnson, collector. 



C833.— Cut of tho Louisi.'illo & Nashvillo R. R., 2 miles southwest or the I'nion Station at Montgomery, Ala. L. W. Stephenson, collector. 



64426.— Same locality as 0-!-12u, described above, but from a lower stratum. _ 



176, 302, esjn CiMi.— Balto Smith Bluff, Alabama River, about 14 miles above Selma, Ala., by tho river, and 10 miles east of Selma by tho wagon road. L. \\ . 

 Stephenson and L.C.Johnson, collectors. 



293.— Cunninghams Bluff, Alabama River. L. C. Johnson, collector. 



6828.— From oyster ledges, in nivino one-half mile west of Kenan's mill, I 'alias County, Ala. C3 or :>,', miles norlhwesl of Selma). L. W.Stephenson, collector. 



147.— Surface, sees. 12 and 13, south of Valley Creek, east of Kenan's mill, 3 miles northeast of Solma, Ala. L. C. Johnson, collector. 



312.— Vallev Creek mar Selma, Ala. !,,('. Johnson, collector. „ , „ rt , . „ , 



6441.— Public road one-half miio east of Old Hamburg, Perry County, Ala. Top of Tombigbeo sand momber of liutaw formation. L. \\ . Stephenson, collector. 



