Abstract
Near Sydney, Australia, unconsolidated aeolian and alluvial sediments of Quaternary age form the Botany Sands aquifer and lie unconformably on Triassic-age sandstone (Narrabeen Group). Botany Bay is an inlet of the Pacific Ocean about 10 km south of the city centre. Reclamation of the northern foreshore of Botany Bay commenced in 1979. One impact of this reclamation was to move the saline interface in the aquifer southward.
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