Lower Balonne Alluvial Floodplain
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Alluvial aquifers are formed from particles such as gravel, sand, silt and/or clay deposited by physical processes in river channels or on floodplains. These deposits store and transmit water through intergranular voids. In floodplain environments these alluvial aquifers may have groundwater flow systems ranging from a local (e.g. a few kilometres) to regional (e.g. hundreds of kilometres) scale.
Last updated: 22 March 2013
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Lower Balonne Alluvial Floodplain, WetlandInfo, Queensland Government, Queensland, viewed 4 August 2020, .