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Soil/Landform Unit - Powers Creek sand plains

Landform Unit Description

WLRA Landform Powers Creek gently undulating sand plain
Gently undulating sand plains near Langkoop that have been selectively cleared as a part of past pastoral runs
      Area: 7853 ha
      0.34% of CMA region

      Occurring south-west of Edenhope and adjoining the Glenelg Hopkins CMA boundary, this low gently undulating sand plain complex is part of the low ridge tops with remnant aeolian sands and orientated depressions division (5.5.2) within the North West Dunefields and Plains. This sand plain abuts the dissection of Mosquito Creek and is bound to the north by a less undulating plain (Apsley). The plain includes lower and upper slopes of very gentle rises, drainage depressions and swamps. Site drainage is slow to very slow but moderately well drained on the slopes. Sodic brown, yellow and grey texture contrast soils (Sodosols) with grey cracking clay soils (Vertosols) are major soils. Some of these soils are seasonally wet. Topsoils are often hardsetting and shallow. Sesaonal inundation and waterlogging can also be issues on the heavier soils. Grazing (sheep) is generally the common land use enterprise in conjunction with occasional broadacre cereal cropping. A number of vegetation communities have been recorded including Plains Woodland, Shallow Sands Woodland, Damp Heathland, and Seasonally Inundated Shrubby Woodland.
WLRA Landform Powers Creek gently undulating sand plain

WLRA Landform Powers Creek gently undulating sand plain
Lower slope of gently undulating sand plains near Langkoop
WLRA Landform Powers Creek gently undulating sand plain

WLRA Landform Powers Creek gently undulating sand plain

WLRA Landform Powers Creek gently undulating sand plain
Remnant vegetation on gently undulating sand plains

Component
1
2
3
4
5
Proportion of soil-landform unit
10%
20%
60%
5%
5%
CLIMATE
Rainfall (mm)
Annual: 640
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Quaternary aeolian dune sands, paludal silt and clay; Neogene marine sand and silt (Parilla Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep and beef cattle grazing
TOPOGRAPHY
Landscape
Gently undulating sand plains
Elevation range (m)
112–178
Local relief (m)
3
Drainage pattern
Dendritic
Drainage density (km/km2)
0.2
Landform
Undulating plains
Drainage complex
Landform element
Upper slope
Lower slope
Plain
Swamp
Drainage depression
Slope and range (%)
3 (1-10)
2 (1-7)
0 (0-1)
0 (0-1)
1 (0-5)
Slope shape
Convex
Convex
Straight
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (21.5%), Shallow Sands Woodland/Plains Sedgy Woodland/Seasonally Inundated Shrubby Woodland/Damp Sands Herb-rich Woodland Mosaic (19.3%), Damp Sands Herb-rich Woodland (15.8%), Heathy Herb-rich Woodland (6.2%), Other (36.4%)
SOIL
Parent material

Aeolian sand and silt

Marine sand and silt

Marine sand and silt

Paludal silt and clay

Marine sand and silt
Description
(Corangamite Soil Group)
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)
Grey and brown cracking clay soils (37)
Grey and brown cracking clay soils (37)
Soil type sites
LSWW11, LSWW17, LSWW13
LSWW11, LSWW17, LSWW13
LSWW11, LSWW17, LSWW13
LS3, LSWW9, LSWW5
LS3, LSWW9, LSWW5
Surface texture
Loamy sand
Loamy sand
Loamy sand
Medium clay
Medium clay
Permeability
Moderate
Moderate
Slow to moderate
Very slow
Very slow
Depth (m)
1.3
2
> 2
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Slopes susceptible to wind and sheet erosion where exposed. Susceptible to compaction where hardsetting. Upper soil is susceptible to acidification.Susceptible to wind and sheet erosion where exposed. Susceptible to compaction where hardsetting. Susceptible to wind and sheet erosion. Susceptible to compaction where hardsetting and restricted drainage. Upper soil is susceptible to acidification.Susceptible to seasonal inundation and waterlogging in swamps. Surface soils friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.Susceptible to seasonal inundation and waterlogging. Surface soils friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.
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