Geology
Recent to Pleistocene sediments.
Landform
Stream channel.
Original Vegetation
Insufficient data is available. |
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Soils
The soils in these drainage lines are quite variable. The flanks of the valleys are often stony since the incising stream reveals the deeper materials underlying the surrounding landscape. The valley floors are often comprised of sandy alluvium which may be quite deep due to wind action.
Chemical and Physical Analysis
No physical or chemical analyses have been carried out.
Land Use
The land use is generally similar to the adjoining land. The soils are generally prone to gully and side-wall erosion.