|Sub-round dunes occur on plains to the south and east of Lake Tyrrell. There are also smaller areas in the valley to the north and south of Lake Hindmarsh. Weakly developed north east - south west ridges also occur, mostly to the east of Lake Tyrrell.|
Geological maps show that, in these areas, the Woorinen Formation is underlain not by Blanchetown Clay, but by weathered Parilla Sand. This more porous substrate may have favoured the development of sub-round rather than linear dunes.
Stranded ridges are absent or weakly developed. Boundaries are clear except to the east of the area near Lake Tyrrell where, unit 5.1.5 has similar landforms but in different proportions. Alluvial plains of the Tyrrell and Lalbert Creeks cross the area from south to north.
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|The unit is relatively productive under agriculture, having a high proportion of medium-textured soils with favourable structure, water retention and fertility. The erosion hazard is moderate, the most susceptible sites being the upper western slopes most exposed to the prevailing strong winds. |
Seepage salting has not been observed. Two factors limiting this hazard are apparent, firstly the relatively high water-holding capacity of the upper layers on the hummocky dunes, and secondly the relatively porous substrate, namely Parilla Sand.
5.1.4 an example of hummocky dunes dominant (south east of Lake Tyrrell, north and south of Lake Hindmarsh