The hydrogeology, hydrology and hydrochemistry of the Condamine River Valley alluvium

Huxley, William John (1982) The hydrogeology, hydrology and hydrochemistry of the Condamine River Valley alluvium. Masters by Research thesis, Queensland University of Technology.


The Cainozoic alluvium of the Condamine River valley is interpreted to consist of sediments deposited as floodplain and sheetwash deposits in bedrock valleys eroded into Mesozoic sedimentary rocks and tertiary volcanics. A maximum recorded sediment accumulation of 134 m is centred just south of Dalby. The lower section ofboth the flood plain and sheetwash alluvium is composed of variegated sandy and clayey sediments and the upper section of brown and grey sandy and clayey sediments.

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ID Code: 35951
Item Type: QUT Thesis (Masters by Research)
Additional Information: Spine title : Hydrogeology--Condamine River Valley.
Presented to the Dept. of Applied Geology, Queensland Institute of Technology.
Keywords: Hydrology Queensland Condamine River, Groundwater Queensland Condamine River, Alluvium Queensland Condamine River, thesis, masters
Institution: Queensland University of Technology
Copyright Owner: Copyright 1982 William John Huxley
Deposited On: 22 Sep 2010 13:03
Last Modified: 04 Dec 2012 03:03

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