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Soil/Landform Unit - Grampians plains

Landform Unit Description

WLRA Landform Grampians plains
View of the eastern extent of the Grampians Range with prominent outwash slopes and long gentle plains grading away from the range
      Area: 31 150 ha
      1.33% of CMA region

      The Grampians plains soil-landform unit surrounds the Grampians Range as narrow zones of siliceous sand derived from outwash of the weathering and erosion from the range. Footslopes are characterised by gently undulating plains that graduate into plains with scattered drainage lines. Plains scattered amongst plains and lower and in topographic sequence away from the ranges. Soils are mostly deep and are dominated by brown and yellow texture contrast soils with sandy surfaces (Sodosols) that are quite variable in depth. Long gentle slopes are subject to periodic inundation and waterlogging during wet seasons. While the light sandy surfaces are generally well drained, they have extremely dense heavy subsoils that inhibit deeper water infiltration. Soils are typically acidic with low inherent fertility surface soils. There are a number of vegetation communities present including woodlands, forests and a number of complex and mosaic vegetation formations. Some of the more common vegetation communities include sandy heathlands, forests, shrubland and woodlands.
WLRA Landform Grampians plains

WLRA Landform Grampians plains
Looking across Mount William Creek towards the plains
WLRA Landform Grampians plains

WLRA Landform Grampians plains

WLRA Landform Grampians plains
Sandy plains at Moyston West

Component
1
2
3
Proportion of soil-landform unit
1%
49%
50%
CLIMATE
Rainfall (mm)

Annual: 860
Temperature (oC)
Minimum 7, Maximum 19
Precipitation less than potential evapotranspiration
October–March
GEOLOGY
Age and lithology

Quaternary alluvium, gravel, sand and silt; Neogene marine sand, sandstone, silt, laterite (Dorodong Sand); Quaternary colluvium, alluvium, gravel, sand and silt
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: sheep grazing; viticulture; olive plantations; residential development; native flowers; stone fruit; dryland cropping
TOPOGRAPHY
Landscape

Colluvial outwash slopes
Elevation range (m)
149–748
Local relief (m)
2
Drainage pattern
Parallel–dendritic
Drainage density (km/km2)
1.1
Landform
Gently undulating plains
Landform element
Drainage line
Undulating footslope
Gently undulating plain
Slope and range (%)
3 (1-7)
5 (3-10)
2 (1-6)
Slope shape
Concave
Concave
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Heathy Woodland (13.9%), Rocky Outcrop Herbland (7.6%), Shrubby Woodland (7.5%), Riparian Shrub (5.8%), Other (63.5%)
SOIL
Parent material

Alluvial gravel, sand and silt

Colluvial sand, silt and minor gravel

Marine laterite sand and silt, colluvial sand and silt, aeolian dune sand
Description
(Corangamite Soil Group)
Brown and yellow texture contrast soils (sandy surfaces) (17)
Brown and yellow texture contrast soils (sandy surfaces) (17)
Brown and yellow texture contrast soils (sandy surfaces) (17)
Soil type sites
Surface texture
Sandy loam
Sandy loam
Sandy loam
Permeability
Moderate
Moderate
Moderate
Depth (m)
> 2
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Flat areas subject to inundation and waterlogging, susceptible to gully erosion where sodic subsoil is exposed. Light sandy surface soils generally well drained to subsoil or hardpan. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Acidic, low inherent fertility surface soils.Susceptible to gully erosion where sodic subsoil is exposed. Light sandy surface soils generally well drained to subsoil or hardpan. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Acidic, low inherent fertility surface soils.Long gentle slopes are subject to periodic inundation and waterlogging. Light sandy surface soils generally well drained to heavy subsoil. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Soil may be susceptible to compaction. Acidic, low inherent fertility surface soils.
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