478 THE CLIMATE OF THE PLEISTOCENE EPOCH. [Aug. IQOr,, 



not think it necessary to invoke epeirogenic changes to shift the- 

 centres of anticyclones. Such a system as that supposed to exist 

 in the Western Hemisphere in Glacial times might move eastward 

 by accretion on the east side, and an eating- away of the western 

 side by the Northern Pacific cyclone. 



The Peesident and Sir John Evans also spoke. 



The AtTTHOR, in consequence of the lateness of the hour, replied 

 very briefly to the various objections raised in the course of the 

 discussion, expressing the hope that if the paper were published a 

 number of these would prove to have been anticipated. 



