The interior of Oates Land is characterised by a highland icefield where mountains in excess of 4000 m protrude above the thick ice cover as nunataks. These mountains show folded rocks that are a manifestation of the Early Palaeozoic Ross Orogeny. |
The interior of Oates Land is characterised by a highland icefield where mountains in excess of 4000 m protrude above the thick ice cover as nunataks. These mountains show folded rocks that are a manifestation of the Early Palaeozoic Ross Orogeny. |