Anastomosing river sedimentation in the Channel Country of central Australia

Article


Gibling, Martin R., Nanson, Gerald C. and Maroulis, Jerry C.. 1998. "Anastomosing river sedimentation in the Channel Country of central Australia." Sedimentology. 45 (3), pp. 595-619. https://doi.org/10.1046/j.1365-3091.1998.00163.x
Article Title

Anastomosing river sedimentation in the Channel Country of central Australia

ERA Journal ID1860
Article CategoryArticle
AuthorsGibling, Martin R. (Author), Nanson, Gerald C. (Author) and Maroulis, Jerry C. (Author)
Journal TitleSedimentology
Journal Citation45 (3), pp. 595-619
Number of Pages25
Year1998
Place of PublicationUnited Kingdom
ISSN0037-0746
1365-3091
Digital Object Identifier (DOI)https://doi.org/10.1046/j.1365-3091.1998.00163.x
Web Address (URL)https://onlinelibrary.wiley.com/doi/full/10.1046/j.1365-3091.1998.00163.x
Abstract

Anastomosing river plains of the Channel Country, central Australia, have aggraded slowly over the past 100 ka. Channel sediments accumulate mainly as accretionary benches of mud and sand, sandy channel-base sheets and vegetation-shadow deposits. The channels are laterally stable and the sediments have aggraded locally against erosional banks of tough floodplain muds. Channel sediments are profoundly affected by desiccation during dry periods and by bioturbation caused by within-channel trees and burrowing invertebrates, especially crayfish. Excavations show that mud-dominated channel bodies of low width:thickness ratio are generated by a combination of vertical and lateral accretion. Levees and braided surfaces, composed mainly of mud aggregates, border the channels and are activated during valley-wide floods which lay down distal mud sheets. Floodplain muds are converted to vertisols with gilgai, deep desiccation cracks, and impregnations of carbonate and gypsum. A fixed-channel facies model is applicable to the Channel Country river deposits. Anastomosis apparently results from the need for the system to move large volumes of water and moderate sediment loads across low-gradient interior basins. Channels distant from upland source areas receive an abundant supply of pedogenic, sand-sized mud aggregates generated on adjacent floodplains and reworked into braid bars during valley-wide floods. Some quartz sand is provided from excavation of subsurface Pleistocene sands in deep channels and waterholes and from aeolian dunes on the floodplains. Adjacent gibber plains supply some gravel to the system.

Keywordsrivers; channel sediments; river plains
Contains Sensitive ContentDoes not contain sensitive content
ANZSRC Field of Research 2020370901. Geomorphology and earth surface processes
370509. Sedimentology
410404. Environmental management
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Institution of OriginUniversity of Southern Queensland
Byline AffiliationsDalhousie University, Canada
University of Wollongong
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