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Soil/Landform Unit - Mosquito Creek swamp sand plains

Landform Unit Description

WLRA Landform Mosquito Creek swampy sand plains
Centre pivot irrigator on swampy sand plain near Langkoop used for dairy production
      Area: 10 433 ha
      0.45% of CMA region

      As a valley complex associated with a northern tributary of the Glenelg River near the South Australian border, the Mosquito Creek unit is surrounded by plains (Apsley) and undulating sand plains (Powers Creek) that lead into the Glenelg River. There are four landscape components dominated by a level sand plain. The other minor components are gentle drainage slopes, drainage lines and swamp beds. Drainage will vary according to distance from drainage lines as well as slope and source area (hydraulic head). Soil types are predominantly yellow, brown and grey sodic texture contrast soils (Sodosols), with grey cracking clay soils in the depressions. Sheet and rill erosion are associated with the lighter topsoils and exposed surfaces. Waterlogging and salinity in the depressions and broader flats are also an issue. Grazing (sheep and cattle) is the dominant enterprise along with dryland cropping. Most vegetation communities (Creekline Sedgy Woodland, Riparian Woodland, Damp Heathland, Plains Sedgy Woodland and Red Gum Wetland) are associated with wetter areas including swamps and creeklines. Other vegetation communities include woodlands.
WLRA Landform Mosquito Creek swampy sand plains

WLRA Landform Mosquito Creek swampy sand plains
Swamp sand plain and centre pivot irrigator
WLRA Landform Mosquito Creek swampy sand plains

WLRA Landform Mosquito Creek swampy sand plains

WLRA Landform Mosquito Creek swampy sand plains

Sheep grazing on sand plain

Component
1
2
3
4
Proportion of soil-landform unit
65%
15%
10%
10%
CLIMATE
Rainfall (mm)
Annual: 635
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Quaternary aeolian dune sand, paludal silt and clay; Neogene marine sand and silt (Parilla Sand); Neogene marine sand, sandstone, silt and laterite (Dorodong Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep and cattle grazing
TOPOGRAPHY
Landscape
Swampy sand plains
Elevation range (m)
95–161
Local relief (m)
3
Drainage pattern
Dendritic
Drainage density (km/km2)
0.5
Landform
Sand plains
Swamps and drainage systems
Landform element
Level plain
Gentle drainage slope
Drainage line
Swamp bed
Slope and range (%)
0 (0-1)
2 (1-5)
0 (0-2)
0 (0-1)
Slope shape
Straight
Linear
Concave
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (38.2%), Shallow Sands Woodland/Plains Sedgy Woodland/ Seasonally Inundated Shrubby Woodland/Damp Sands Herb-rich Woodland Mosaic (19.7%), Creekline Sedgy Woodland (17.4%), Other (24.7%)
SOIL
Parent material

Marine sand and silt, aeolian dune sand

Marine sand and silt, aeolian dune sand

Marine sand and silt

Paludal silt and clay
Description
(Corangamite Soil Group)
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
LS3, LSWW9, LSWW5
LS3, LSWW9, LSWW5
Surface texture
Loamy sand
Loamy sand
Medium clay
Medium clay
Permeability
Slow
Moderate to slow
Very slow
Very slow
Depth (m)
1.3
1.3
> 2
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
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.Susceptible to seasonal inundation and waterlogging especially depressions. Surface soils friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.Susceptible to 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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