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Soil/Landform Unit - Wartook granite hills

Landform Unit Description

WLRA Landform Wartook granite hills
Slopes on the western margin of the Wartook syncline
      Area: 2253 ha
      0.10% of CMA region

      Hills and footslopes at Wartook on the north-western edge of the Grampian Ranges are part of the Dissected Western Uplands. This granite hill landscape with rocky crests abuts the western extent of the Grampians Range and extensive plains associated with the MacKenzie River to the west. Footslopes, steep hillslopes and crests (with rock outcrop), and drainage lines occur in these hills. Drainage is concentrated from the steeper slopes, dissecting a number of colluvial slopes/fans then extending west to the MacKenzie River. Soil type is predominantly yellow texture contrast soils (Chromosols), sometimes sodic (Sodosols) on the lower slopes. There are also thin sandy and minor deeper sandy soils (Rudosols and Tenosols). Sheet, rill and gully erosion are the major land degradation threats, with wind erosion of light topsoils possible where exposed. This unit is used for grazing (sheep, beef cattle), water supply function in some areas, as well as nature conservation and recreation. Vegetation is largely either woodland or forest. Some vegetation communities present include Shrubby Woodland, Herb-rich Heathy Forest, Hills Herb-rich Woodland, Plains Grassy Woodland, Heathy Woodland, Heathy Dry Forest, Grassy Dry Forest and Damp Sands Herb-rich Woodland.
WLRA Landform Wartook granite hills

WLRA Landform Wartook granite hills
Hillslopes near Wartook with granite outcrop and native vegetation
WLRA Landform Wartook granite hills

WLRA Landform Wartook granite hills

WLRA Landform Wartook granite hills
Granitic hillslopes near Wartook

Component
1
2
3
Proportion of soil-landform unit
15%
10%
75%
CLIMATE
Rainfall (mm)
Annual: 765
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–March
GEOLOGY
Age and lithology
Quaternary alluvium, gravel, sand, silt; Devonian granite (Mackenzie River Granodiorite);
Quaternary colluvium, gravel, sand and silt; Silurian marine sandstone, minor conglomerate and siltstone (Grampians Group)
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation; recreational activities
Cleared areas: sheep and beef cattle grazing; water supply
TOPOGRAPHY
Landscape
Moderate–steep hills
Elevation range (m)
207–649
Local relief (m)
100–250
Drainage pattern
Dendritic
Drainage density (km/km2)
1.5
Landform
Hillslopes
Landform element
Steep hillslope
Drainage line
Footslope
Slope and range (%)
25 (10-32)
2 (0-4)
5 (1-10)
Slope shape
Convex
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Hills Herb-rich Woodland (21.0%), Damp Sands Herb-rich Woodland (18.9%), Plains Grassy Woodland (17.1%), Heathy Woodland (10.6%), Other (30.4%)
SOIL
Parent material

In situ
intrusive granite

Fluvial gravel, sand and silt

Fluvial gravel, sand and silt, intrusive granite
Description
(Corangamite Soil Group)
Yellow texture contrast soils (3)
Yellow texture contrast soils (3) and sodic yellow texture contrast soils (4)
Yellow texture contrast soils (3)
Soil type sites
Surface texture
Silty loam (sandy)
Silty loam (sandy)
Silty loam (sandy)
Permeability
Moderate
Very slow
Slow
Depth (m)
< 1
> 2
1.4
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Light loose surface soils that may be susceptible to wind, sheet and rill erosion in drier areas (including drier aspects). Susceptible to acidification in wetter areas.Light loose surface soils that are susceptible to gully erosion. Poor subsurface drainage, particularly on flats and depressions. Surface soils susceptible to acidification.Light loose surface soils that may be susceptible to wind, sheet and rill erosion in drier areas (including drier aspects). Poor subsurface drainage, particularly on flats and gentle slopes. Susceptible to acidification in wetter areas.
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