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Soil/Landform Unit - Grampians outwash slope

Landform Unit Description

WLRA Landform Grampians outwash slopes
Outwash slopes of the Grampians Ranges, looking eastwards over the MacKenzie River towards Wartook
      Area: 12 797
      0.55% of CMA region

      Surrounding the Grampians Ranges are hillslopes that represent significant colluvial and alluvial deposits of Grampians sand and silt. Outwash slopes are far more extensive in the north of the Grampians Ranges than the south where local relief is varied between 15 and 45 metres. A significant source of high quality groundwater, these sands comprise acidic, grey texture contrast soils with deep sandy surfaces (Kurosols) and sandy soils with pans (Podosols). The light sandy surface soils are subject to mass movement (creep and sheet flow) on steep slopes where exposed, yet remain well to rapidly drained. Wind erosion may also be extensive where soil surfaces are exposed. There are many different vegetation types including woodlands, forest and shrubland. Some of the more prevalent vegetation communities include Valley Grassy Forest and Shrubby Foothill Forest in sheltered areas of the landscape, Heathy Dry Forest and Grassy Dry Forest in more exposed areas, and other communities such as Shallow Sands Woodland, Lateritic Woodland, Damp Sands Herb-rich Woodland, and Rocky Outcrop Shrubland.
WLRA Landform Grampians outwash slopes

WLRA Landform Grampians outwash slopes
Cleared alluvial outwsh slopes used in an olive plantation
WLRA Landform Grampians outwash slopes

WLRA Landform Grampians outwash slopes

WLRA Landform Grampians outwash slopes
Mount Difficult sandstone range with outwash slopes on the western margin

Component
1
2
3
Proportion of soil-landform unit
65%
15%
20%
CLIMATE
Rainfall (mm)

Annual: 815
Temperature (oC)
Minimum 7, Maximum 19
Precipitation less than potential evapotranspiration
October–March
GEOLOGY
Age and lithology
Quaternary colluvium, gravel, sand and silt; Silurian marine and non-marine sandstone, siltstone and minor conglomerate (Grampians Group);
Quaternary alluvium, gravel, sand and silt
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: sheep grazing; viticulture; olive plantations; lavender; stone fruit; residential development; water supply
TOPOGRAPHY
Landscape

Outwash hillslopes
Elevation range (m)
165–634
Local relief (m)
15–45
Drainage pattern
Parallel
Drainage density (km/km2)
1.1
Landform
Undulating outwash plains and rises
Landform element
Undulating rise
Drainage line
Hillslope (scree)
Slope and range (%)
5 (1-15)
5 (3-10)
12 (5-30)
Slope shape
Convex
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Heathy Woodland (13.2%), Sand Heathland (10.3%), Damp Sands Herb-rich Woodland (9.5%), Rocky Outcrop Herbland (8.0%),
Shallow Sands Woodland (6.8%), Other (47.1%)
SOIL
Parent material
Sandstone, siltstone and minor conglomerates
Alluvial gravel, sand and silt
Colluvial gravel, sand, silt and sandstone
Description
(Corangamite Soil Group)
Acidic, grey texture contrast soils (sandy surfaces) (16)
Sandy soils with pans (15)
Sandy soils with pans (15)
Soil type sites
Surface texture
Loamy sand
Loamy sand
Loamy sand
Permeability
High
High
High
Depth (m)
> 2
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Light sandy surface soils subject to mass movement (creep and sheet flow) on steep slopes, generally well to rapidly drained. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Acidic sandy soils with a low inherent soil fertility.Light sandy soils generally well drained to hardpan or rock. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Acidic soils with a low inherent soil fertility. Groundwater springs from Grampians colluvium are often associated with depressions.Light sandy soils subject to mass movement (creep and sheet flow) on steep slopes, generally rapidly drained to hardpan or rock. Weakly coherent surfaces with little organic matter are susceptible to sheet and wind erosion where exposed. Acidic soils with a low inherent soil fertility.
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