The geological history of New South Wales is very complex and spans almost two billion years of Earth history.
During this time there have been multiple phases of active continental growth , involving periods of widespread volcanic activity, sedimentation (in near-shore basins and in deep-sea areas), granite intrusion and intense folding and faulting as a consequence of the processes of plate tectonics.
These geological processes have resulted in the formation of new or additional areas of crust in the form of mountain chains or orogens. Over time, these mountain chains have been eroded to produce the overall subdued topography we see now.
NSW is a major producer of a variety of commodities, including gold, copper, zinc, silver and lead.
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Over 60% of NSW is covered by sedimentary basins.
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The geology of NSW has shaped the settlement as well as the economic and social development of the state and provided the basis for our agricultural industries.
Go to Statewide tectonics