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Lower Balonne alluvial floodplainLower Balonne alluvial floodplainSelect from the tabs below Lower Balonne alluviaAlluvial 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. Pictorial conceptual model PDF Additional links
Last updated: 18 December 2015 This page should be cited as: Queensland Government, Queensland (2015) Lower Balonne alluvial floodplain, WetlandInfo website, accessed 30 August 2024. Available at: https://wetlandinfo.des.qld.gov.au/wetlands/ecology/aquatic-ecosystems-natural/groundwater-dependent/lower-balonne-alluvia/ |