Project Summary
The project is located adjacent to major halloysite-kaolin deposits, including the Great White Kaolin Project, but has never been systematically explored for kaolin-halloysite.
The Eucla Basin contains sequences up to 300m thick of Tertiary marine, coastal and paleochannel sediments. Kaolin-halloysite deposits within the area of the Poochera Project are typically formed where acidic saline groundwater was developed during oxidation of lignitic, pyritic sands of the Eocene Pidinga Formation within buried fluvial channels. Widespread weathering involving the acidic saline groundwater has formed several significant kaolin deposits and occurrences on the Eyre Peninsula.
Highlights
Exploration

