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Soil/Landform Unit - Kowree undulating sand plains and ridges

Landform Unit Description

WLRA Landform Kowree undulating sand plains and ridges
Looking south-west ver Lowan Sand dunes with remnant vegetation, south of Morea
      Area: 105 925 ha
      4.52% of CMA region

      Rises (ridges), dunes and plains north-east of Edenhope and around Apsley comprise large extents of sands on ridges and plains. This low ridge/dune complex is part of the North West Dunefields and Plains. The low ridge, dune and gently undulating sand plain complex of Quaternary and Cainozoic aeolian sediments is part of a NNW/SSE orientated former stranded beach ridge sequence that is associated with neighbouring Ullswater, Nurcoung and Edenhope units and other ridge/depression units to the north (Goroke, Diapur). Ridge slopes (cleared and uncleared), dunes (cleared and uncleared) and gently undulating sheet/sand plains are common. Drainage is strongly aligned to the terrain with little surface expression apart from local depressions. Soils comprise brown and yellow, grey sodic texture contrast soils (Sodosols). Sandy soils or soils with a deep sandy surface occur on the crests and some dunes. Sheet and rill erosion, along with wind erosion are potential land degradation hazards. This unit is used for grazing (sheep, beef cattle), dryland cropping, nature conservation and plantation forestry. The main vegetation communities recorded include Shallow Sands Woodland, Plains Woodland and Heathy Woodland.
WLRA Landform Kowree undulating sand plains and ridges

WLRA Landform Kowree undulating sand plains and ridges
East-west trending Lowand Sand dunes
WLRA Landform Kowree undulating sand plains and ridges

WLRA Landform Kowree undulating sand plains and ridges

WLRA Landform Kowree undulating sand plains and ridges

Remnant vegetation east of Edenhope

Component
1
2
3
4
5
6
Proportion of soil-landform unit
15%
15%
15%
15%
25%
15%
CLIMATE
Rainfall (mm)

Annual: 545
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology

Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: sheep grazing; dryland cropping; plantation forestry
TOPOGRAPHY
Landscape

Undulating sand plains and ridges
Elevation range (m)
92–215
Local relief (m)
5–20
Drainage pattern
Deranged
Drainage density (km/km2)
0.2
Landform
Dunefields/ridgecrests/ridgeslopes
Gently undulating plains
Landform element
Dune crest (uncleared)
Dune crest (cleared)
Upper slope (uncleared)
Upper slope (cleared)
Mid slope
Lower slope/plain
Slope and range (%)
4 (1-7)
4 (1-7)
3 (2-7)
3 (2-7)
3 (2-6)
2 (0-5)
Slope shape
Convex
Convex
Linear
Linear
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class

Shallow Sands Woodland (22.6%), Heathy Woodland (16.7%), Plains Woodland (14.2%), Other (46.4%)
SOIL
Parent material

Aeolian sand

Aeolian sand

Aeolian sand

Aeolian sand

Aeolian sand

Paludal silt and clay
Description
(Corangamite Soil Group)
Sandy soils with and without pans (31)
Sodic brown, yellow and grey texture contrast soils (38)
Sandy soils with and without pans (31)
Sodic brown, yellow and grey texture contrast soils (38)
Sodic brown, yellow and grey texture contrast soils (38)
Sodic brown, yellow and grey texture contrast soils (38)
Soil type sites
LSWW11, LSWW17, LSWW13
LSWW11, LSWW17, LSWW13
LSWW11, LSWW17, LSWW13
LSWW11, LSWW17, LSWW13
Surface texture
Sand
Loamy sand
Sand
Loamy sand
Loamy sand
Loamy sand
Permeability
High
High
High
High
Moderate
Moderate
Depth (m)
> 1.5
> 1.5
> 1.5
> 1.5
1.3
1.3
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Soils can be susceptible to wind and sheet erosion where exposed, higher organic matter content and ground cover makes these less vulnerable than cleared dune crests. Low inherent soil fertility.Susceptible to wind and sheet erosion where exposed and surfaces with little organic matter. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Soils can be susceptible to wind and sheet erosion where exposed, higher organic matter content and ground cover makes these less vulnerable than cleared upper slopes. Low inherent soil fertility.Susceptible to wind and sheet erosion where surfaces with little organic matter are exposed. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Susceptible to wind and sheet erosion where surfaces with little organic matter are exposed. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Low susceptibility to wind and sheet erosion. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.
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