Controls on channel deposits of highly variable rivers: Comparing hydrology and event deposits in the Burdekin River, Australia

Authors

Jan Alexander, University of East Anglia, Norwich Research ParkFollow
Christopher M. Herbert, University of East Anglia, Norwich Research Park
Christopher R. Fielding, University of Nebraska-LincolnFollow
Kathryn J. Amos, University of Adelaide

ORCID IDs

https://orcid.org/0000-0002-2830-2727

https://orcid.org/0000-0002-2397-6116

Document Type

Article

Date of this Version

2020

Citation

Sedimentology (2020) 67, 2721–2746 doi: 10.1111/sed.12717

Comments

2020 The Authors.

Abstract

Discharge event frequency, magnitude and duration all control river chan- nel morphology and sedimentary architecture. Uncertainty persists as to whether alluvial deposits in the rock record are a time-averaged amalgam from all discharge events, or a biased record of larger events. This paper investigates the controls on channel deposit character and subsurface strati- graphic architecture in a river with seasonal discharge and very high inter- annual variability, the Burdekin River of north-east Australia. In such rivers, most sediment movement is restricted to a few days each year and at other times little sediment moves. However, the maximum discharge magnitude does not directly correlate with the amount of morphological change and some big events do not produce large deposits. The Burdekin channel deposits consist of five main depositional elements: (i) unit bars; (ii) vegetation-generated bars; (iii) gravel sheets and lags; (iv) antidune trains; and (v) sand sheets. The proportions of each depositional element preserved in the deposits depend on the history of successive large dis- charge events, their duration and the rate at which they wane. Events with similar peak magnitude but different rate of decline preserve different event deposits. The high intra-annual and inter-annual discharge variability and rapid rate of stage change make it likely that small to moderate-scale bed morphology will be in disequilibrium with flow conditions most of the time. Consequently, dune and unit bar size and cross-bed set thickness are not good indicators of event or channel size. Antidunes may be more use- ful as indicators of flow conditions at the time they formed. Rivers with very high coefficient of variance of maximum discharge, such as the Bur- dekin, form distinctive channel sediment bodies. However, the component parts are such that, if they are examined in isolation, they could lead to misleading interpretation of the nature of the depositional environment if conventional interpretations are used.