PL S !J S \\r 1903 



probably PAUEOZOIC. I 



istes 3nd Qusrtntes CE3 Andesttic Series 



^ufrsofvery ancient 3p/ie3r,3nce. \u\W\i^ Basa/tic Series 



"jranite. u'^'c'*'-' Soapstone *rith 



■ ' '' * peMes or ancient n 



Imrtz-diorde. |:';^;:'-| 



\ncient nxks lol specirical/y determined 



I I 



Highly Generalized Geological Section 



A(g(^@©@ V D T D [L d ^ y o Fi 



along the line A B.C D E on plan ( Plate XXXIil.) 



£■3 I *s 



Plate KdV 



SECTION 

 oF Raised Coral Reef 



interstratlFied with "Soapstone" 



WALU BAY, near SUVA 



Soapstone simi/ar to Chat below the raised coraf reef .-^ii^^ 



Ye/lowish grey Coral- ReeP Aock /brmed c/i'efTy oT Corals. f 



a>3rna.Cai^ium. lic/^^nrncj . 'lai~ge Tr-dacna and , -J" 



, teeth oF C^rxharodon - (v. Fig 3 PfaOnnni) I ~ " 



Greenish grey "Soapstane". a fine /■ • ■ 



grained marine CuFraceous rock wit/' 

 Foraminifpra and in places remamp oF 

 plants partly converted -nto H-fv i^- .^ 



Thin bands oF tuFt ' cli'eHy tmi «■■■ / t 



oFaugite and Felspar a ys:oi i .' 



'onal thin growthi 

 Coral 



