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Soil/Landform Unit - Little Desert linear dunes

Landform Unit Description

WLRA Landform Little Desert east-west dunes
Little Desert linear dunes
      Area: 45 139 ha
      1.93% of CMA region

      Within central areas of the Little Desert, a sequence of east-west dunes (linear dunes) have formed. The dunes comprise Lowan Sand that is thought to originate from deflation of underlying Parilla Sand as remnant stranded beach ridges. Running east-west, the Little Desert is relatively uncleared owing to the high concentration of sands and low inherent fertility. Major soils across the dunes and plains include sodic yellow and grey texture contrast soils (Sodosols) with deep sandy topsoils, and deep sandy profile also prominent on dune crests. Given the high concentration of sands across the dunes and plains, wind erosion is the major land degradation threat owing to the relatively incoherent nature of these sands. Vegetation includes a range of woodland, heathland, shrubland and mallee vegetation. Communities recorded include Shallow Sands Woodland, Plains Woodland, Damp Heathland, Sandstone Ridge Shrubland, Dunefield Heathland, Lowan Sands Mallee and Low Rises Woodland. Red Gum Wetland and Seasonally Inundated Shrubby Woodland have also been found in wetter areas of the landscape.
WLRA Landform Little Desert east-west dunes

WLRA Landform Little Desert east-west dunes
Cultivated east-west dunes near the Kaniva-Edenhope Road
WLRA Landform Little Desert east-west dunes

WLRA Landform Little Desert east-west dunes

WLRA Landform Little Desert east-west dunes
Sand plains on the northern margin of the Little Desert

Component
1
2
3
Proportion of soil-landform unit
15%
50%
35%
CLIMATE
Rainfall (mm)

Annual: 500
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology

Neogene marine sand and silt (Parilla Sand);
Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
5.2.2 Linear dunes of the Siliceous North West Dunefields and Plains
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep grazing
TOPOGRAPHY
Landscape

Linear east west dunes
Elevation range (m)
127–193
Local relief (m)
5–10
Drainage pattern
-
Drainage density (km/km2)
-
Landform
Dunes
Landform element
Dune crest
Dune slope
Sand plain
Slope and range (%)
4 (1-20)
7 (3-25)
2 (0-8)
Slope shape
Convex
Convex
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Lowan Sands Mallee (39.5%), Shallow Sands Woodland (21.3%), Dunefield Heathland (16.1%), Sandstone Ridge Shrubland (9.3%), Other (13.7%)
SOIL
Parent material

Aeolian sand

Aeolian sand

Aeolian sand, marine sand and silt
Description
(Corangamite Soil Group)
Sandy soils with and without pans (31)
Sodic yellow and grey texture contrast soils (32)
Sodic yellow and grey texture contrast soils (32)
Soil type sites
LSWW8, LSWW7, WIA24, WIA31
LSWW8, LSWW7, WIA24, WIA31
Surface texture
Sand
Loamy sand
Loamy sand
Permeability
High
Slow
Slow
Depth (m)
> 1.5
> 1.5
> 1.5
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Soils with low organic matter levels can be susceptible to wind and sheet erosion where exposed. Low inherent soil fertility.Susceptible to wind and sheet erosion where exposed. Low inherent fertility but well drained to pans or subsoil. Susceptible to compaction where hardsetting and lower slopes occurs.Susceptible to wind and sheet erosion where exposed. Low inherent fertility. Susceptible to compaction where hardsetting and poor drainage occurs.
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