G. C. Crick—Cretaceous Rocks of Natal and Zululand. 347 
Creek and its tributaries, beds of the same age, passing down possibly 
into rocks of Upper Albian age, are probably also present. The 
occurrence here of Cretaceous beds of an age younger than Cenomanian 
is somewhat douhtful. 
i Ad (eae £eca series (with coals) 
Khivelane.* °° i : Basalé 
Lia oe 
Phyoltite 
- -Liksilesat ~*~ 
s 
(Ei aglish Siiles 
Geological Sketch-map of part of Zululand. (After W. Anderson.) 
