Tertiary education of earth scientists in Australia, as in many other countries, is very conservative. Undergraduate courses are little different from those offered 30–50 years ago. Postgraduate courses, while more focused than undergraduate courses, are also conservative, but are changing more rapidly in response to industry and professional demands. In Australia the majority of earth science graduates are employed in the exploration and mining industry, yet there are few undergraduate courses that recognize this and endeavour to educate students for that market. This is probably because few academics have industrial experience at senior levels; many academics, and indeed many exploration geologists, believe the industrial aspects of the profession can be “learnt on-the-job”; and many academics are not aware of the needs of the industry in which their graduates gain employment. In Australia this conservatism results in a reluctance to develop courses in new areas of earth science such as regolith studies. As a result most new graduates have rarely studied regolith stratigraphy, materials, or process, yet it is this thin veneer covering fresh rock that is the prime exploration medium. The recognition of the importance of the regolith in exploration has been increasing in industry over the decade, but there are few earth science departments teaching regolith studies in any meaningful way at undergraduate levels, and only a few courses tackle the area at postgraduate level. Ideally all graduates in Australia, and elsewhere (where thick regolith dominate landscapes), should be familiar with the regolith and its formation because, above all else, it is the most visible part of the Earth. Regolith study is, of necessity, interdisciplinary. It is the zone of the Earth's crust in which the hydrosphere, atmosphere and biosphere interact with the lithosphere. Undergraduate courses involving regolith studies must incorporate a sound grounding in all the natural and physical sciences as well as in particular aspects of their application to regolith studies.