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Soil/Landform Unit - Mount Cole Creek

Landform Unit Description

WLRA Landform Mount Cole Creek
Mount Cole Creek and the Wimmera River converging west of Eversley
      Area: 20 368 ha
      0.87% of CMA region

      This unit is an alluvial valley complex associated with the upper Wimmera River and forms part of the alluvial terraces and floodplains subdivision (2.1.7) landscape of the Dissected Western Uplands. This alluvial unit is surrounded by many hilly to mountainous units including the Pyrenees Ranges, Mount Langi Ghiran and the Concongella hills from north to south. The alluvial plains/flats occur as elongated valleys that are confined by higher relief. Terrace plains and flats, gentle lower slopes, drainage depressions, valley flats and moderate upper slopes all occur within these valleys. Soil types are predominantly red sodic texture contrast soils (Sodosols) with yellow, brown and grey sodic gradational (Dermosols) and texture contrast soils (Chromosols), the latter in the depressions. Soil compaction is a potential land degradation susceptibility as is waterlogging on the depressions, broader flats and plains where topsoils are shallow. Fodder production and cereal cropping are common enterprises but grazing (sheep and cattle) is the dominant enterprise. Heathy Dry Forest and Grassy Forest vegetation communities are associated with exposed areas of the landscape, while Herb-rich Foothill Forest and Valley Grassy Forest are more associated with sheltered areas of the landscape. Other remnant vegetation include various woodlands.
WLRA Landform Mount Cole Creek

WLRA Landform Mount Cole Creek
Alluvial terraces of the Wimmera River near Crowlands
WLRA Landform Mount Cole Creek

WLRA Landform Mount Cole Creek

WLRA Landform Mount Cole Creek
Terrace plain railway cutting and Mount Cole Creek

Component
1
2
3
4
5
6
7
Proportion of soil-landform unit
12%
20%
23%
10%
5%
23%
7%
CLIMATE
Rainfall (mm)
Annual: 640
Temperature (oC)
Minimum 7, Maximum 19
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Cambrian marine sandstone, siltstone and biotite schist (St Arnaud Group); Quaternary fluvial gravel, sand and silt; Devonian granite
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: sheep and beef cattle grazing; dryland cropping; pasture production; water supply
TOPOGRAPHY
Landscape
Alluvial plain and valleys
Elevation range (m)
201–840
Local relief (m)
5
Drainage pattern
Dendritic
Drainage density (km/km2)
1.6
Landform
Alluvial terraces, plains and floodplains
Alluvial valleys
Landform element
Gentle slope
Terrace plain
Terrace flat
Drainage depression
Moderate upper slope
Gentle lower slope
Valley flat
Slope and range (%)
3 (1-6)
2 (0-10)
1 (0-2)
2 (0-5)
12 (10-30)
5 (3-20)
2 (1-10)
Slope shape
Straight
Straight
Convex
Straight
Concave
Convex
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (18.4%), Creekline Grassy Woodline (13.6%), Alluvial Terraces Herb-rich Woodland (12.0%)
SOIL
Parent material

In situ
intrusive granite, marine sandstone, siltstone and biotite schist

Fluvial gravel, sand and silt

Fluvial gravel, sand and silt

Fluvial gravel, sand and silt

In situ
marine sandstone, siltstone and biotite schist, intrusive granite

Alluvial gravel, sand and silt

Alluvial gravel, sand and silt
Description
(Corangamite Soil Group)
Red texture contrast soils (10)
Red texture contrast soils (10) and yellow and brown gradational and texture contrast soils (11)
Red texture contrast soils (10)
Sodic brown, yellow and grey texture contrast soils (12)
Yellow and brown gradational and texture contrast soils (11)
Yellow and brown gradational and texture contrast soils (11)
Sodic brown, yellow and grey texture contrast soils (12)
Soil type sites
Surface texture
Sandy loam
Sandy loam
Sandy loam
Loam, fine sandy (heavy)
Loamy sand
Loamy sand
Loam, fine sandy (heavy)
Permeability
High
High
High
Slow
High
High
Moderate to slow
Depth (m)
> 2
> 2
> 2
> 2
> 2
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Light soil surface susceptible to sheet and rill erosion and compaction. Subsoil susceptible to rill and gully erosion where sodic. Lighter soil variants are well drainage. Upper soil susceptible to acidification.Lighter surface susceptible to compaction and hardsetting with low organic matter levels. Soils are susceptible to sheet and rill erosion where slopes are steeper. Subsoil susceptible to rill and gully erosion. Lighter variants are well drained.Light soil surface susceptible to sheet and rill erosion and compaction. Subsoil susceptible to rill and gully erosion where sodic. Lighter soil variants are well drainage. Upper soil susceptible to acidification.Lighter surface susceptible to sheet and rill erosion and compaction. Subject to periodic inundation and waterlogging, especially during flood events. Lighter soil variants are well drained within the depressions. Upper soil susceptible to acidification.Lighter surface susceptible to sheet and rill erosion and compaction. Subsoil susceptible to rill and gully erosion where sodic and deeper. Lighter variants are well drained.Lighter surface susceptible to sheet and rill erosion and compaction, especially with low organic matter. Susceptible to rill and gully erosion where sodic subsoils are exposed. Lighter variants are well drained.Lighter surface susceptible to sheet and rill erosion and compaction. Subject to periodic inundation and waterlogging, especially during flood events. Lighter soil variants are well drained within the depressions. Upper soil susceptible to acidification.
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