TI1K M CCESSION OF STKAT1FIKD lt< >< 



Further, the Neozoic division is much thicker on the Kurupean 

 continent than it is in England, for in tin- Alps thick deposit* 

 come in l>et\ve<>n the Triassic and Jurassic Systems, and tin- 

 Neogene Series is of much greater thickne&s in Southern Kurope 



than it is in tin- north. 



