Int J Climatol 18:329–345, Tyson PD (1999) Late-quaternary and Holocene palaeoclimates of southern Africa: a synthesis. Mountain Rescue Teams, Drakensberg. We stay on the Luvuvhu 4×4 Trail until we exit the Park. We will design a safari or tour that will blow your socks off ! J Geophys Res 115:B02406. Holocene 9:295–309, King LC (1953) Canons of landscape evolution. Associated with Quaternary and Holocene climate changes, and triggered in part by the near-vertical cliffs along the escarpment edge, are a range of mass movement features to the east of the Great Escarpment. 2002). Proc Geol Assoc 122:179–185, Grab S, van Zyl C, Mulder N (2005) Controls on basalt terrace formation in the eastern Lesotho highlands. Koedoe 53(1) Art. Terra Nova 21:310–315, Partridge TC, Maud RR (2000) Macro-scale geomorphic evolution of southern Africa. Plant Ecol Divers 4:313–328, Duncan AR, Marsh JS (2006) The Karoo igneous province. We use 4×4 tracks to the top of the escarpment and camp at Mafefe camp – camping with ablutions, (Upgrade to rustic rondavel for additional R 550.00 per rondavel – only 5 x available). The geologic history of the Great Escarpment, which includes within it the Drakensberg escarpment, closely follows cycles of tectonic evolution and land surface denudation from the Jurassic to Miocene that affected the entire southern African region. Updates? Bell FG, Haskins DR (1997) A geotechnical overview of Katse dam and transfer tunnel, Lesotho, with a note on basalt durability. Higher altitudes (>3,200 m a.s.l) of the Drakensberg escarpment are today only marginally periglacial in character. The Drakensberg is the name given to the eastern portion of the Great Escarpment, which encloses the central Southern African plateau. So, you and your friends would like to go somewhere special, add a day or two to our normal offerings, father and son bonding time, or whatever! Evidence for the degree to which erosion has affected the land surface comes from exhumed igneous rocks, accordant summits that correspond to preserved palaeo-surfaces and apatite fission track thermochonometric dating that suggests erosion rates of 95 ± 43 m/Myr between 91 and 69 Myr (Brown et al. pp 47-55 | The “Drakensberg” – derived from the Afrikaans name, “Drakensberg” meaning “Dragon Mountains” is the name given to the Eastern Portion of the Great Escarpment. There is uncertainty in the magnitude of temperature and precipitation changes at this time, largely because these values were likely affected by distance from moisture source and orographic effects, as they are today. Meet up with participants who could not make Thursday departure. The lavas produced a ~1,500-m-thick basaltic capping along the Drakensberg escarpment (Duncan and Marsh 2006) and formed almost horizontally layered basalt flows (represented as scarp faces) individually 3–8 m thick (Grab et al.
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