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Soil/Landform Unit - Rocky Point low hills and rises

Landform Unit Description

WLRA Landform Rocky point low hills and rises
Undulating rises west of Rocky Point and Mount Ararat
      Area: 4182 ha
      0.18% of CMA region

      Rises and low hills west of Ararat fall on the southern boundary of the Wimmera CMA region. This rise and low hill complex is part of the Dissected Western Uplands with a landscape chiefly derived on granite and Cainozoic sediments. The terrain abuts associated ridges and valleys of Palaeozoic metasediments of the Ararat Hills. Rise slopes comprise pronounced upper and lower segments with hillslopes and crests, with prominent drainage depressions and associated drainage lines. Drainage dissects this landscape, concentrating flow from the Ararat Hills to the east. Yellow sodic texture contrast soils (Sodosols) occur mainly on the lower slopes and flats (less drainage). Sheet and rill erosion are potential land degradation threats given the texture contrast nature of soils. Gully erosion and salting is also prominent. Used mainly for grazing (sheep, beef cattle), with occasional dryland cropping on the flats and lower slopes. Native vegetation communities including Grassy Dry Forest, Alluvial Terraces Herb-rich Woodland, Granitic Hills Woodland and Grassy Woodland exist on these rises and low hills.
WLRA Landform Rocky point low hills and rises

WLRA Landform Rocky point low hills and rises
Lower slopes and drainage depressions
WLRA Landform Rocky point low hills and rises

WLRA Landform Rocky point low hills and rises

WLRA Landform Rocky point low hills and rises
Natural springs occur in valley floors

Component
1
2
3
4
Proportion of soil-landform unit
15%
10%
55%
20%
CLIMATE
Rainfall (mm)
Annual: 790
Temperature (oC)
Minimum 7, Maximum 18
Precipitation less than potential evapotranspiration
October–March
GEOLOGY
Age and lithology
Devonian granite (Ararat granodiorite); Neogene fluvial gravel, sand and silt; Cambrian basalt, andesite, boninite, rhyolite, gabbro and lithics
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: sheep and beef cattle grazing; dryland cropping
TOPOGRAPHY
Landscape
Undulating rises and low hills
Elevation range (m)
252–402
Local relief (m)
40
Drainage pattern
Dendritic
Drainage density (km/km2)
1.9
Landform
Drainage depressions
Low hills
Rises
Landform element
Drainage line
Hillslope and crest
Upper slope
Lower slope
Slope and range (%)
1 (0-3)
15 (10-32)
6 (3-15)
4 (2-8)
Slope shape
Concave
Convex
Convex
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Granitic Hills Woodland (60.3%), Alluvial Terraces Herb-rich Woodland (29.1%), Other (10.6%)
SOIL
Parent material
Fluvial gravel, sand and silt
In situ intrusive granite
In situ intrusive granite
In situ intrusive granite, fluvial sand, silt and clay
Description
(Corangamite Soil Group)
Sodic yellow texture contrast soils (4)
Yellow texture contrast soils (3)
Yellow texture contrast soils (3)
Yellow texture contrast soils (3) and sodic yellow texture contrast soils (4)
Soil type sites
Surface texture
Sandy clay loam
Silty loam (sandy)
Silty loam (sandy)
Sandy clay loam
Permeability
Very slow
Slow to moderate
Slow to moderate
Slow
Depth (m)
> 2
1.2
1.6
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Light loose surface soils susceptible to wind, sheet and rill erosion. Sodic subsoil extremely susceptible to gully erosion. Poor subsurface drainage, particularly on flats and drainage 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). Susceptible to acidification in wetter areas.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 susceptible to wind, sheet and rill erosion. Sodic subsoil susceptible to gully erosion. Poor subsurface drainage leads to waterlogging on flats and break of slope. Surface soils susceptible to acidification.
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