Australia’s iconic towering limestone stacks hold a detailed archive of millions of years of climate history.
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How did Australia end up with so much iron ore? What we discovered in Western Australia redefines how we think about iron deposits – and provides clues on how we might find more.
Cratons are pieces of ancient continents that formed billions of years ago.
Top contributors
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Biodiversity Coordinator, Wilderness, University of the Witwatersrand
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Post-doctoral researcher, University of the Witwatersrand
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Postdoctoral Research Associate in Geological Sciences, University of Colorado Boulder
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Associate Professor, School of Geography, Earth and Atmospheric Sciences, The University of Melbourne