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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 ...
Table Mountain is the northernmost end of a 50-kilometre-long (30 mi) and roughly six-to-ten-kilometre-wide (4 to 6 mi) Cape Fold Mountain range that forms the backbone of the Cape Peninsula, stretching from the Cape of Good Hope in the south to Table Mountain and its flanking Devil's Peak (to the east) and Lion's Head and Signal Hill (to the ...
Possible tectonic setting during deposition of the Malmesbury group. (after Compton 2004) The late-Precambrian age Malmesbury Group is the oldest rock formation in the area, consisting of alternating layers of dark grey fine-grained greywacke, sandstone and slate, seen along the rocky Sea Point and Bloubergstrand shorelines, and from the Strand to Gordon's Bay.
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
2006 Table Mountain fire; ... 2021 Table Mountain fire; Table Mountain Sandstone This page was last edited on 5 February 2021, at 17:08 (UTC). ...
Table Mountain Group: Lithology; Primary: Sandstone, mudstone, siltstone, shale, and conglomerates: Other: Calcite: Location; Region: Western & Eastern Cape: Country South Africa: Type section; Named for: Bokkeveld mountains: Schematic diagram of a west-east (left - right) geological cross section through the Cedarberg portion of the Cape Fold ...
Both places feature coarser-grained sandstones that lack fining-upward sequences, thus pointing to an alluvial fan and braided river environment. The depositional environment changes towards the centre of the Stormberg as mudstones become more common, pointing to a change to fluvial - lacustrine deposits where sediments were deposited in low ...
The Transvaal Supergroup is a stratigraphic unit in northern South Africa and southern Botswana, situated on the Kaapvaal Craton, roughly between 23 and 29 degrees southern latitude and 22 to 30 degrees eastern longitude.