“…Nunataks of the escarpment consist largely of crystalline basement metamorphic rocks of Precambrian age (Spaeth & Fielitz, 1987), predominately gneiss, dated at ~1.1 Ga in the Heimefrontfjella (Jacobs, Bauer, Spaeth, Thomas, & Weber, 1996). At some localities within the Kirwan Escarpment, less resistant shales and sandstones of Permian age (the Amelang Plateau Formation) have been deposited onto the basement Precambrian metamorphic rocks (Aucamp, Wolmarans, & Neethling, 1972;Faure & Mensing, 2011). Jurassic tholeiitic basalts are also present within the sequence, and correspond in age with the main phase of Karoo volcanism in southern Africa (Duncan, Hooper, Rehacek, Marsh, & Duncan, 1997;Ferraccioli et al, 2005).…”