tiani" 



>fx\H-lTHr 



ind that of die ra-lcluux k u-sult from t 



tlH^ (k 







hawk 

 iSt 



n^ the K 



urnai/ xsnt<-. Mr a'.' W .' nmvitt/r' 

 rvprpuced. he IS n-anled a. the type 



^ioi lie f,-u.e. iuth 



.11^' the littk oul Weieuuottoo 





^^i^'/o; 



the OMifinil ooi/mmlli't^niroUsock 



mtf, C 



££' 



^^hlch may have impelh-d the Kurm 

 <^>aitp ,1 dilh^^enr opinion of the bigi 

 tot rned hy the present writci' 



AVh 





. coniumt Meu- of tho myths of the 







^\id(>pH"id tunencvand iiiiperi.slia>)h' 



of onP 



'm^iL'u 



theseu.UHsa.apph>dton-il,e.o,M 



''x^ri;!;;;<:;!S^hef!u^^;K" 



/Ktonan evidence, ota former xolcanic period, 

 nate name, for the soutli east of Australia at U 



The mjthsoi Looein .ind Wiuonderrer suir^^ei 





