The Oolloo Dolostone and Tindall Limestone aquifers are substantially fractured and cavernous. Large volumes of water can be stored within these formations and water flows relatively easily through ...
The Tindall aquifer also underlies the adjoining Roper catchment. The Tindall aquifer is confined by the Jinduckin and Oolloo dolostone formations as water does not infiltrate through them to the ...
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