TABLE IX 



Geologic, Abcheologic, and Paleontologic Correlation of the Pleistocene 



Deperet, 1918-1921; Mayet, 1920-1921 





c3 

 ad 



Recent. 



Flint industries. 





Fourth Postglacial moraines. 



Azilian, Tardenois- 

 ^| ian, Magdalenian. 









1 Solutrean. 





IV. Monastirian Stage, Deperet. — After Monastir, 



J Aurignacian. 







Tunis. 









Mediterranean shoreline of 18-20 meters. 









Lower river terraces of 18-20 meters. 









Glacial moraines of IV Glaciation := 



Mousterian. 







Alpine-Wurm of Penck (Wurmien- 









Mecklenburgien ) . 









Mousterian industry in formation. Cold 

 mammoth-reindeer fauna. 















Third Interglacial regressive period == Riss- 



(Cold.) 



■^ 



a 





Wtirm recession of Penck. 



Acheulean. 



o 



C5 



III. Tyrrhenian Stage. — Defined by Issel, horizon 

 of Strombus ~bul)onius. 

 Mediterranean shoreline of 28-32 meters. 



(Warm.) 









II 





Erosion of middle river terraces of 28-32 







meters. 





a 

 £ 





Glacial moraines of III Glaciation = Riss 





3 





of Penck (Rissien-Polonien). 





o 





Ghellean industry at base of 30-meter ter- 



Chellean. 



EH 

 32 





race. Primitive amygdaloid weapons and 





l-H 





warm hippopotamus fauna associated. 





J 



PM 





Second Interglacial regressive period = Min- 



(Pre-Chellean?) 



II 





del-Riss of Penck. 







II. Milazzian Stage Deperet. — After peninsula of 





H 





Milazzo, northern Sicily.^ 



Mediterranean shoreline of 55-60 meters 

 Middle-high river terraces of 55-60 

 meters. 

 Glacial moraines of II Glaciation = 



"No traces of the 

 existence of man 

 on continent o f 



P 





Europe." Mayet, 

 1921. 







Mindel of Penck (Mindelien-Saxonien). 







Maximum glacial extension in northern 









and southern Europe. 









First Interglacial regressive period = Giinz- 









Mindel of Penck. 







I. Sicilian Stage (=Cromerian, England). — Gull 









of Conque d'Or, Palermo, Sicily. 









Mediterranean shoreline of 90-100 meters. 









Erosion of highest river terraces of 100 









110 meters. 









Glacial moraines of I Glaciation = Giinz 









of Penck (Gunzien-Scanien). 





(465) 



