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Geology:

The area in a 100km radius around Van Rhynsdorp nestles on the interface between five unique geological structures.

Namely

    • Cape Supergroup.(The Bokkeveld and Cederberg sections)
    • Karoo Supergruop.(The Ecca and Beaufordt sediments)
    • Malmesbury Supergroup.(With granite intrutions)
    • Namaqua-Natal Belt.
      ( Remnants of the coastal sediments deposited during the formation of the first Super Continent. Rhodinia)
    • Gariep Belt.
      (Remnants of the coastal sediments deposited during the formation of the second Super Continent, Pangea)