CORRELATION OFk CLIMATIC. RAC/AL, CULTURE & LIFE STAGES 1914 



:- POST GLACIAL DAVH- 

 ^ "Newer Loess ^gschnit 



::; E'. GLACIAL j^ 



;; WORM, WISCONSIN 'LAt^. 



; , 'Upper Drift ' „ , ''■^^. 

 ' Lowest Terraces -' o-'V 



3. INTER - ^ 

 GLACIAL ^ 



RISS - WURM ^ 

 SANGAMON ^ 



"Middle Loess" 



m. GLACIAL 



RISS, POLAND/ AN 

 ^'Middle Drifr ^^J 



Yllinoian 



GLACIAL 



M IN DEL- RISS 

 HELVETIAN 

 YARMOUTH 



H. GLACIAL 



MINDEL . SAXONIAN 

 KAN SAN 



"Old Drift" 



GLACIAL 



NORFOLK I AN 

 ; GUNZ-MINDEL 



I. GLACIAL 



GUNZ.SCANIAN 

 NEBRASKAN y^. 



GLACIAL 



AND 



INTERGLACIAL 



a 200.000 YEARS 



'','3 



LOWER 



)PALAEO 



LITHIC 



4 MOUSTERIAN 

 SOpOO YCARS 



3ACHEULEAN 



7SpO0 YEARS 



ZCHELLEAN 



lOOpOO YEARS 



I PRE-CHELLEAN 



IZSpOO YEARS 



COLD TUNDRA FAUNA 

 WOOLLY MAMMOTH d 

 RHINOCEROS. FIRST 

 STEPPE & REINDEER 



,8 II Z75pOO 



IB 300,000 , 



FIRST COLD 

 FAUNA 



'00 poo YEARS 



4.7Sp00 



COLD FOREST BED 

 FAUNA //V J BRITAIN 

 OOpOO YEARS 



STONE CULTURES 

 AND COLD FAUNAS 



NEANDERTHAL 



■■ (KRAPINA) 



PITHECAN- 

 THROPUS 

 (TRINILj 



HUMAN 

 RACES 



RECENT FOREST, MEADOW. ALPINE 



REINDEER PERIOD, ARCTIC 

 TUNDRA, STEPPE . ALPINE 

 FOREST, MEADOW 

 COLD FAUNA 



ARRIVAL-STEPPE, TUNDRA, FAUNA 



LAST WARM AFRICAN-ASIATIC 



FAUNA 



E.ANTIQUUS. HIPPOPOTAMUS 



D. MERCKII , E TROGON THERIi 



ALSO FOREST, MEADOW 



EUR ASIATIC FAUNA 



WARM AFRICAN ASIATIC 



FAUNA 

 E.ANTIQUUS, E. TROCONTH- 

 ERII , D. MERCKII, HIPPO- 

 POTAMUS 



WARM 

 AFRICAN ASIATIC FAUNA 

 E MERIDIONALIS-TROCON- 

 THERII , D ETRUSCUS, 



HIPPOPOTAMUS 



MACH/ERODUS 



PLIOCENE 

 WARM FOREST 



STAGES OF MAMMALIAN 

 AND PLANT LIFE 



Reproduced through the courtesy of 

 Charles Scribner's Sons 



GREAT EVENTS OF THE GLACIAL EPOCH 



To the left the relation of glacial and interglacial stages in Europe and North America, with 

 the author's theory regarding the divisions of time, the beginning of the Old Stone Age, and the 

 successive appearance in Kiirojie of difTcn^nt branches of the human race. 



To the right the prolonged warm temperate period in Europe in the non-glaciated regions, 

 followed by the relatively brief cold period during the past 70,000 years [From p. 41, Men of the Old 

 Stone Age] 



Chart prepared by Dr. C. A . Reeds of the American Museum, in cooperation with the author 



18 



