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Soil/Landform Unit - Morton drainage plains

Landform Unit Description

WLRA Landform Morton drainage plains
Morton plains, north-east of Watchem
      Area: 1805 ha
      0.08% of CMA region

      The plains and depressions are part of the hummocky dunes subdominant landscape within the calcareous dunefield of the North West Dunefields and Plains. These plains are also associated with the older alluvial plains of the Northern Riverine Plains (4.2) to the east. These low-lying plains/depressions lie between other plains (Kalkee and Charlton) and low hummocky dunefields (Beulah), and are generally orientated NNW/SSE. The plains are dominant with a drainage depression as a minor component that receives drainage from the surrounding units, though the terrain is essentially flat. Soil types are predominantly red sodic texture contrast soils (Sodosols), with yellow, brown and grey sodictexture contrast soils (Sodosols) and occasional grey and brown cracking clay soils (Vertosols) in the depressions. There is little resistance to wind movement due to the cleared flat terrain. Compaction is also a potential land degradation susceptibility, as is waterlogging in the depression and to some extent the plain, where topsoil is shallow. Dryland cropping is the major enterprise with some grazing (sheep). The four main vegetation communities found are Low Rises Woodland, Ridged Plains Mallee, Plains Woodland and Plains Savannah.
WLRA Landform Morton drainage plains

WLRA Landform Morton drainage plains
Plains with clayey roads
WLRA Landform Morton drainage plains

WLRA Landform Morton drainage plains

WLRA Landform Morton drainage plains

Channel weir

Component
1
2
Proportion of soil-landform unit
70%
30%
CLIMATE
Rainfall (mm)

Annual: 370
Temperature (oC)
Minimum 9, Maximum 22
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology
Neogene marine sand and silt (Parilla Sand); Quaternary silt, sand and minor gravel (Shepparton Formation); Quaternary fluvial gravel, sand and silt;
Quaternary aeolian lunettes, sand, silt and clay
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: sheep grazing; dryland grazing
TOPOGRAPHY
Landscape
Gently undulating plains
Elevation range (m)
101–114
Local relief (m)
1–2
Drainage pattern
Dendritic
Drainage density (km/km2)
0.1
Landform
Alluvial plains
Landform element
Plain
Drainage depression/closed depression
Slope and range (%)
1 (0-2)
0 (0-2)
Slope shape
Straight
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Plains Savannah (45.0%), Plains Woodland (45.4%), Ridged Plains Mallee (5.4%), Low Rises Woodland (1.5%)
SOIL
Parent material
Fluvial gravel, sand and silt
Paludal silt and clay, fluvial sand and silt
Description
(Corangamite Soil Group)
Sodic red texture contrast soils (27) and sodic yellow and grey texture contrast soils (28)
Sodic yellow and grey texture contrast soils (28) and cracking clay soils (29)
Soil type sites
LS17, WAR33, WLRA126
Surface texture
Sandy loam
Loamy sand to clay loam
Permeability
Moderate
Slow
Depth (m)
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Hardsetting surface susceptible to sheet and rill erosion along with wind erosion. Dispersive and deep subsoils susceptible to gully erosion where exposed. Soils are prone to compaction at critical moisture contents.Wind erosion along with sheet and rill erosion occur on hardsetting surfaces with little organic matter. Soils can be subject to inundation and waterlogging especially in low-lying areas. Subsoils are dispersive and susceptible to gully erosion on steeper slopes. Soils compact at critical moisture contents.
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