98 



granite conies as sheer clilT, jumbled boulder, or sloping pavement to the sea on 

 all sides except for a small sandy beach, the landing place, on the east side of 

 Middle Island. The south and west faces of the islands are most rugged, and in 

 places precipitous clififs rise 200 feet or more. The ocean swell of the Great 



East Hiil. 



Mo-'i-n C_Tt6:W 



PLAN OF TEAKSON ISLAND 



■&a.sed on o. vi&ual SrcetcK map 

 l^repared hu T. D. Cam [oL>c.ll . 



Y/^y////^ "Trave-rrme plateaux. 

 |.-,v.;.::| At-ripky. •bfiTutLrxU 



I ~ ^ -"| ]?)lou3n su r\c< 



TVie-fo-U c^ tlie land, is \nJ.lcjitccl 

 ■Enj. joTin lines , lOh-icU approx^ mj-le, 



to looft co-ntbo-fs,lrut txTe on.lij 



dl Q.^jTCa rn m atTi C. 



jtKHiil 



Australian I'.ight. driven by moderate winds, dashes with great force against 

 these w.-ills. sending spray high in the air. In rough weather and in winter the 

 seas must be very heavy, and the spray be carried by the gales for some distance 

 inland. This is seen by the occurrence of such halophytes as Arihrocncmmn 

 and Siicda 200 to .500 feet above sea level. 



