Category:Rock formations in Magaliesberg

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English: Feldspar-rich quartzitic rocks, i.e. quartzite metamorphosed under extreme temperatures of magma flows, are distinguishable by their coarse white crystals. These leave the interesting mushroom shapes after weathering. Ripple marks on a former seabed are still visible on the northern slopes, usually inclined at 10-20 degrees.

Media in category "Rock formations in Magaliesberg"

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