Lower Balonne alluvial floodplain
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Lower Balonne alluvia
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: 18 December 2015
This page should be cited as:
Lower Balonne alluvial floodplain, WetlandInfo 2015, Queensland Government, Queensland, viewed 11 February 2019, .