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Soil/Landform Unit 106

Landform Unit Description

Unit 106 image a
The gentle slopes have shallow but well drained and fertile soils that support a variety of land uses
      Area: 317 ha
      0.02% of CMA region

      This unit consists of gently inclined very low cones as part of the volcanic Western Plains. This unit consists of two very low cones called Mount Rebecca and Gow Hill between Cressy and Shelford. The higher relative relief aids drainage compared with the surrounding poorer drained, gently undulating basaltic plains. The soils are shallow alkaline red texture contrast soils (Sodosols and Chromosols) with strongly structured subsoils. Little native vegetation occurs as remnants (<1%) of the vegetation class Plains Grassy Woodland. This area has lower rainfall, which in conjunction with the soil favours broadacre cropping. However, the surface soil is susceptible to surface sealing (and structure decline) where organic matter levels are depleted, which may also increase sheet and rill erosion susceptibility.
Unit 106 geomorphology

Unit 106 image b
The main land use of these gentle slopes is cereal cropping
Unit 106 cross section
Unit 106 graph



Component
1
2
3
Proportion of soil-landform unit
20%
35%
45%
CLIMATE
Rainfall (mm)

Annual: 600
Temperature (oC)
Minimum 8, Maximum 19
Precipitation less than potential evapotranspiration
October-March
GEOLOGY
Age and lithology

Quaternary basalt, minor Ordovician marine sandstone and shale
Geomorphology
LANDUSE
Uncleared areas: Nature conservation
Cleared areas: Cropping (cereal); sheep and beef cattle grazing
TOPOGRAPHY
Landscape

Low hills and volcanic cones
Elevation range (m)
14-452
Local relief (m)
20
Drainage pattern
Annular
Drainage density (km/km2)
<0.1
Landform
Rises
Landform element
Crest
Upper slope
Lower slope
Slope and range (%)
4 (1-10)
10 (5-20)
5 (2-10)
Slope shape
Convex
Convex
Convex
NATIVE VEGETATION
Ecological Vegetation Class

Plains Grassy Woodland (0.7%)
SOIL
Parent material

Scoria and basalt

Scoria and basalt

Scoria and basalt
Description
(Corangamite Soil Group)
Shallow alkaline red texture contrast soils (38)
Shallow alkaline red texture contrast soils (38)
Shallow alkaline red texture contrast soils (38)
Soil type sites
MM5075, MM5143
MM5075, MM5143
MM5075, MM5143
Surface texture
Loam, clay loam
Loam, clay loam
Loam, clay loam
Permeability
High
High
Moderate to high
Depth (m)
<1
<1.5
<2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS
Shallow soil. Texture contrast soils are prone to surface sealing. Strongly structured subsoils with low erodibility. Moderate to high nutrient holding capacity. Generally highly permeable.
Shallow to deep subsoil. Texture contrast soils are prone to surface sealing. Strongly structured subsoils with low erodibility. Moderate to high nutrient holding capacity. Generally highly permeable.
Moderate deep to deep soil. Texture contrast soils are prone to surface sealing. Strongly structured subsoil with low erodibility. Moderate to high nutrient holding capacity. Generally highly permeable.
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