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Origin and age of the Mantung High Plain, a karst surface in the western Murray Basin of South Australia
  • Origin and age of the Mantung High Plain, a karst surface in the western Murray Basin of South Australia
  • The Mantung High Plain of the western Murray Basin is a karstic surface of low relief developed on the Early Miocene Mannum Limestone and plausibly interpreted as an example of a perched karstic plain. The Plain is attributed to corrosion planation
  • , i.e. dissolution and collapse down to the Pliocene water table associated first with the ancestral allogenic and exoreic River Murray that then flowed in shallow valley graded to a relatively high regional baselevel, and in later Pliocene times
  • to the estuary that inundated the valley. During the Quaternary the Plain was left high and dry (and converted to the High Plain) by the incision of the Murray and becoming graded to lower baselevels and water tables. Conservation was enhanced by the widespread
  • 2012
Late Pleistocene aeolian reactivation downwind of the Naracoorte East range, southeastern South Australia
  • Southeastern South Australia, straddling the coastal zone and semi-arid desert margins of the lower Murray-Darling Basin, provides an important record of landscape response to past environmental change during the Pleistocene. This study provides
  • 2012
‘How dare you say that about my friend’: negotiating disability and identity within Australian high schools
  • GORMAN-MURRAY, A.[b2]
  • 2012
Colluvial filling of a glacial bypass channel near the Chiemsee (Stöttham) and its function as geoarchive
  • MURRAY, A.[b2]
  • 2012