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Soil/Landform Unit - Goroke plains and rises

Landform Unit Description

WLRA Landform Goroke plains and rises
Looking south-west from Minimay over the plains and sand rises with scattered swamps orientated generally along swales between sand ridges
      Area: 65 547 ha
      2.8% of CMA region

      Scattered along the southern boundary of the Little Desert is the Goroke plains and rises soil-landform unit. As part of the low ridges and orientated swales of the North Western Dunefields and Plains, the landscape includes broad ridges (up to 15 metres local relief) that alternate with swales containing chains of lakes or swamps. The ridges run NNW/SSE in direction and often have concentrations of sand on their eastern sides. Major land components include ridge (rise) crests and slopes with sodic red texture contrast soils (Sodosols), and swales with depressions/swamps of grey and brown cracking clay soils (Vertosols) and gently undulating plains of sodic brown, yellow and grey texture contrast soils. Land use is mainly dryland cereal cropping with hardsetting surfaces a limitation on ridges, and seasonal inundation and waterlogging a factor in swales. A variety of vegetation communities have been recorded including Lowan Sand Mallee, Heathy Woodland, Low Rises Woodland, Sandstone Ridge Shrubland, Plains Sedgy Woodland, Red Gum Wetland, Plains Woodland, Shallow Sands Woodland and Plains Savannah.
WLRA Landform Goroke plains and rises

WLRA Landform Goroke plains and rises
Swamp surrounded by plains and sandy rises
WLRA Landform Goroke plains and rises

WLRA Landform Goroke plains and rises

WLRA Landform Goroke plains and rises
Centre pivot irrigation near Morea

Component
1
2
3
4
Proportion of soil-landform unit
35%
10%
5%
50%
CLIMATE
Rainfall (mm)
Annual: 505
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: Nature conservation
Cleared areas: Dryland cropping; sheep grazing
TOPOGRAPHY
Landscape

Plain with prominent ridges
Elevation range (m)
111–223
Local relief (m)
10
Drainage pattern
Dendritic–parallel
Drainage density (km/km2)
0.2
Landform
Low rises (ridges)
Plains (swale)
Landform element
Upper slope
Rise crest
Drainage depression/swamp
Gentle undulating plain (mid to lower slopes)
Slope and range (%)
3 (2-8)
2 (1-5)
1 (0-3)
3 (0-5)
Slope shape
Convex
Convex
Straight
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Plain Woodland (48.8%), Shallow Sands Woodland (20.1%), Red Gum Woodland (7.5%), Other (23.1%)
SOIL
Parent material

Marine sand and silt, aeolian dune sand

Marine sand and silt, aeolian dune sand

Paludal silt and clay

Fluvial sand, silt and clay
Description
(Corangamite Soil Group)
Sodic red texture contrast soils (39)
Sodic brown, yellow and grey texture contrast soils (38) and sodic red texture contrast soils (39)
Grey and brown cracking clay soils (37)
Sodic brown, yellow and grey texture contrast soils (38)
Soil type sites
LSWW11, LSWW17, NA174
LS3, LSWW9, LSWW5
LSWW11, LSWW17, LSWW13
Surface texture
Sandy loam
Loamy sand
Medium clay
Loamy sand
Permeability
Moderate
Moderate
Slow
Moderate
Depth (m)
> 1.2
< 2
> 2
1.3
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Hardsetting upper soil susceptible to sheet and rill erosion along with wind erosion when exposed. Dispersive and deep subsoils susceptible to gully erosion on steeper slopes. Compaction of upper soil variable depending on soil depth and moisture content. Hardsetting upper soil susceptible to sheet and rill erosion along with wind erosion when exposed. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Susceptible to seasonal inundation and waterlogging in lower areas. Slightly susceptible to surface sheet erosion where soils are exposed. Surface soils are friable and only slightly susceptible to wind erosion. Soils susceptible to compaction.Susceptible to wind and sheet erosion where surfaces with little organic matter are exposed. Susceptible to compaction where hardsetting and restricted drainage.
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