Geology of KwaZulu-Natal

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Introduction

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Geological Timescale

Cenozoic

Zululand Group

Kimberlite Pipes

Faulting and Uplift

Drakensberg &

Lebombo Groups

Stormberg Group

Beaufort Group

Ecca Group

Dwyka Group

Natal Group

Natal Metamorphic Province

Pongola Supergroup

Kaapvaal Craton

 

Glossary

 

 
Geology of KwaZulu-Natal
 
  Kimberlite - but no diamonds Cretaceous
     
 

Following Gondwana breakup, there was a period of unique igneous activity. This formed numerous volcanoes of kimberlite rock, commonly known to contain diamonds.

Unfortunately, the kimberlite pipes of KwaZulu-Natal have not yielded any significant diamonds. This is due to the kimberlites having originated from beneath the Natal Metamorphic Province. Carbon crystallises to form diamond under high pressure and low temperature - conditions only found beneath the Kaapvaal Craton, such as in northern Lesotho.

     
 

 

 

The schematic diagram shows the structure of a KZN kimberlite pipe.

 

The Big Hole in Kimberly represents a kimberlite volcano that has been mined to recover diamonds.

     
   

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last updated:

26 Sep 2006

 

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The website was designed and compiled by Dr. G. Whitmore, Ms D. Meth and Dr. R. Uken (modified by T. Reinhardt.)