KAKUOO K()< KS IX 'J'lIK M AFrXGABUSI. 



255 



notes state that the above beds are uudeilaiu by coug-lomerates 

 that disintegrate and form wide deposits of shingde, with red 

 ferrug-iuous grit and luird red ferruginous sandstone, indicating- 

 Escarpment grit. Under them are the fdays of the Malabo] a 

 beds. 



lY. — Table of Foematioxs. 



Assuming' the correctness of these notes, the rocks of the 

 portion of tlie Mafungabusi region under notice fall into the 

 followina' table : — 



Y. Sl'MMAKV OF 'illE XoTES. 



?^ HaiiKnuJhloru (iiniip. — That a sandstone is interbe(hled 

 in the basalts of the Mafungabusi was first noticed by 

 Mr. C. E. Parsons (2), wlio gave it as rougldy five to ten feet 

 in thickness. Measurements obtained in tlie Pasipas area, 

 near Pulawayo, sliow lliat the corresponding sedimentary beds 

 are not much thickei' and that the outcro]) may be masked by 



