There are currently around 200 primary kimberlitic rock occurrences known in South Australia, located within seven discrete kimberlite provinces. These provinces span a distance of 400 km across the state, from the western side of Eyre Peninsula in the Gawler Craton, to beneath the Murray Basin east of Adelaide. By the early 1980s, almost all of the known outcropping kimberlitic intrusions had been located, while most subsequent discoveries have been confined to shallowly buried intrusive bodies that were located by interpretation of aeromagnetic surveys. Many of the intrusions discussed cannot be confirmed as definitely kimberlitic at this stage due to their pervasive alteration and weathering, which makes examination of the rock matrix material difficult. Diamondiferous kimberlites are now known to exist both in the Eurelia and Terowie Kimberlite Provinces. A detailed review of all available dating information indicates that the confirmed emplacement ages of the kimberlites range from 191 to 170 Ma, but there is other, regolith-derived evidence, based on the presence of detrital kimberlite indicators and diamonds scattered within older secondary units, which suggests that Lower Permian or older diamondiferous kimberlites may also exist in South Australia. Systematic characterisation of the kimberlitic rocks in South Australia is very incomplete. As part of a project intended to systematically map and describe all of the kimberlites and related rocks known in South Australia, heavy mineral samples have been collected from a number of kimberlites in every kimberlitic field within each province. Not all are true kimberlites (see Cooper et al. 2007), and emplacement ages are not continuous across the State. The appendix to the subject report provides the first accurate location details for all of this State’s known kimberlites, including for some that were previously rarely mentioned in publications, and also for many that have never had any particulars published.