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Table Mountain Sandstone (TMS), formally known by its geological name the Peninsula Formation Sandstone, is a group of rock formations within the Cape Supergroup sequence. While the term "Table Mountain Sandstone" remains widely used, it is no longer formally recognized; the correct geological name is "Peninsula Formation Sandstone," which is ...
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.
The Atlantic side of the Back Table is known as the Twelve Apostles, which extends from Kloof Nek (the saddle between Table Mountain and Lion's Head) to Hout Bay. The eastern side of this portion of the Peninsula's mountain chain, extending from Devil's Peak , the eastern side of Table Mountain (Erica and Fernwood Buttresses), and the Back ...
Isolated thick competent layers in a less competent matrix control the folding and typically generate classic rounded buckle folds accommodated by deformation in the matrix. In the case of regular alternations of layers of contrasting properties, such as sandstone-shale sequences, kink-bands, box-folds and chevron folds are normally produced. [10]
A piece of Table Mountain Sandstone. Ermelo Sandstone, Mpumalanga province, near der Farm de Roodepoort; Matatiele Sandstone, KwaZulu-Natal province, near Matatiele; Naboomspruit (also Golden Dawn or Golden Stone) Limpopo province, around Warmbaths; Nieuwoudtville Sandstone, Northern Cape province, near Nieuwoudtville
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