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This topic has appeared in the English Wikipedia rankings 1 time. It first appeared on 2026-06-11 and was most recently seen on 2026-06-11.
The Chuniespoort Group in South Africa contains abundant, thick strata of dolomite deposits that range in depth from 40 m at Carolina, Mpumalanga to 2340 m at Penge and 2130 m at Rustenburg. The Transvaal Supergroup is home to the majority of South Africa's dolomite rocks. The Penge Formation and other dolomite series are analogous to the Chuniespoort Group.... This carbonate rock was created when fluids high in magnesium chemically change limestone to dolostone. With a mean annual rainfall of 700 mm over the past century, these dolomite rocks are ≈ 2500 Ma, which supports the carbonate rock's chemical weathering.
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