PRE-CAPE ROCKS OF SOUTH AND WEST OF COLONY 51 



Klomp Boomen, and also through the Dwyka 

 glomerate resting upon the Table ^j 

 Mountain sandstone of the Bokke- ^ 

 veld Mountain on the south-west, 

 and upon the granite to the north- 

 east of the Doorn Kiver Valley; 

 but if the section had been drawn 

 along a line a few miles to the 

 south of that chosen, the conglo- & 

 inerate would lie upon the Ibiquas 

 beds. 



Some reddish shales and sand- 

 stones in the Verloren Valley in CM|^| j| 

 Piquetberg have been classed with 

 the Ibiquas series on account of 

 the great contrast in lithological 

 character between them and the 

 sericitic slates of the Malmesbury 

 beds with which they are in con- 

 tact on the farm Wit Drift. They 

 pass unconformably below the 

 Table Mountain sandstone, but 

 the nature of the junction with 

 the Malmesbury beds is not clear, 

 though there is little doubt that 

 it is also an unconformity. 



Another group of outcrops that 

 have been referred to the Ibiquas 

 series occurs near Honig Berg in 

 the Piquetberg Division ; they ^ 

 consist of red conglomerates with 



con- 



^ o co 



