Annals of the South African Museum, Volume 84The Museum, 1981 - Natural history |
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Page 11
... elevation ( ? c . 20 m ) , since features associated with shorelines may extend over appreci- able vertical and horizontal distances . Ideally only the maximum elevation of a high sea - level should be recorded ( i.e. the shoreline ...
... elevation ( ? c . 20 m ) , since features associated with shorelines may extend over appreci- able vertical and horizontal distances . Ideally only the maximum elevation of a high sea - level should be recorded ( i.e. the shoreline ...
Page 20
... elevation from about -40 m to 30 m ( Rogers 1980 ) , although until recently only the upper 15-20 m had been placed on record ( Tankard 1975b ) . The sequence is apparently comprised largely of deposits laid down under terrestrial ...
... elevation from about -40 m to 30 m ( Rogers 1980 ) , although until recently only the upper 15-20 m had been placed on record ( Tankard 1975b ) . The sequence is apparently comprised largely of deposits laid down under terrestrial ...
Page 21
... elevation of only 20-25 m in the southern Namib Desert , and drops to even lower elevations northwards from the Orange River ( Table 2 ; Hallam 1964 ) . The implication is that the 33 m terrace is now also much lower than its as yet ...
... elevation of only 20-25 m in the southern Namib Desert , and drops to even lower elevations northwards from the Orange River ( Table 2 ; Hallam 1964 ) . The implication is that the 33 m terrace is now also much lower than its as yet ...
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3aS and 3aN acrae Aeolidiella Ampelisca Amphipoda Anyskop assemblage Baard's Quarry Baba Barnard bed 3aS Bergh bicuspidata bone Brink buccal cusp Cape Province Cape Town capensis Catriona Cenozoic cerata coast columbiana correlated Coryphella Cragievarus kitchingi crown height deciduous demissum dentary denticles deposits Diademodon dicynodonts digestive branch distal dorsal early Pliocene evidence Family fauna femur Flabellina fossa fossils genus Giraffa sp giraffids gland groove Hendey Hipparion holotype indicate Langebaanweg Langebaanweg area late Miocene late Tertiary lateral lingual mammals Marcus & Marcus marginal ridge maxilla Mesembriportax mesial mesiodistal middle Miocene Miocene muscle Namaqualand Nyanzachoerus occlusal pereopod phosphatic Pleistocene Pliocene posterior present QSM and PPM radular recorded region represented rhinophores river Robertia rows sea-level sediments separated shorelines Sivatherium slightly South Africa South African Museum south-western Cape species specimens SUID-AFRIKAANSE MUSEUM surface Tankard taxa teeth terrestrial tooth UNIVERSITY OF CALIFORNIA Varswater Formation ventral vertebrates