250 



KAEROO 1{(XKS IX TIIK MAIUXGABUSI. 



The name is, however, more <^'enerally applied to the 

 remnant of a dissected tahlehuid of sedimentary and volcanic- 

 rocks that in the sonth overlap on to the uplands of crystalline 

 vschists, the northern marp-in being defined by an escarpment 



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that faces the lower lyino> o-roimd on tlie nortli-west and east. 

 On tlie map attached hereto (Fig. 1) this tableland appears 

 as a wedge pushing bef-ueen the valleys and forming the 

 watershed of the Bume and Vniniati Eivers, the point being 



