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- W2564649412 abstract "FIorisbad, situated near the north-western rim of the main Karoo basin, is surrounded by rocks of the Ecca and Beaufort Groups of Permian Age. Black shales of the Ecca Group were deposited under reducing conditions by suspension settling in an inland sea. Shallower conditions set in due to an encroaching prograding delta which was followed by the fluvial sandstones and mudstones of the Beaufort Group deposited in a more continental environment. During the Jurassic Period dolerite magma intruded into the Karoo beds and crystallised in the form of sills and dykes. Post-Jurassic denudation marked by several erosional cycles under dominantly arid conditions, formed the Quaternary landscape characterised by small inselbergs surrounded by extensive plains. Calcrete developed in broad shallow valleys, pans were formed and wind-blown clay and silt from these deflation hollows accumulated as crescentic dunes on the leeward edges. The large lunette ofthe Soutpan extends over the Florisbad thermal spring. Younger red aeolian sand occurs as drapes over older rocks and unconsolidated deposits. Early man had an abundant supply of lydianite for the shaping of stone artefacts." @default.
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- W2564649412 date "1988-09-01" @default.
- W2564649412 modified "2023-09-23" @default.
- W2564649412 title "The regional geology of Florisbad : Quaternary deposits" @default.
- W2564649412 hasPublicationYear "1988" @default.
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