The famous Table Mountain forms part of the Cape Fold Belt, being made up of the local lowest ( oldest ) strata of the Cape Supergroup, composed predominantly of quartzitic sandstone which forms the impressive, almost vertical cliffs which characterize the mountain and the rest of the range which constitutes the backbone of the Cape Peninsula.
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The municipal area s northwesternmost corner in the Rhaunen State Forest ( Sangwald and Jungenwald ) is part of a Taunus quartzite block, whose continuation can also be seen in the higher elevations to the west, namely the Sandkopf, the Wildenburger Kopf and the M�rschieder Burr ( stratigraphy : Taunus quartzite; petrography : quartz sandstone and quartzitic sandstone with traces of claystone and siltstone ).
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