The Australian Continental Plate is generally considered to be one tectonic plate, and is classified as a Stable Continental Region [REF].
The uplifted Cadell fault forms a bifurcated scarp, the northern part of which extends for 55 kilometres from Deniliquin to Echuca with a height of 12-15 metres, and the southern part which extends for 13 kilometres south of Echuca with a height of about 3-4 metres.