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Soil/Landform Unit - Telangatuk plains

Landform Unit Description

WLRA Landform Telangatuk plains
Plains east of Lake Toolondo and est of the Black Range
      Area: 13 223
      0.56% of CMA region

      This unit of very low relative relief terrain has major occurrences near Lake Toolondo and west of the Black Range on the southern boundary of the Wimmera CMA region. This low plateau complex is part of the Western Uplands: low elevation plateaux division (2.3). This low plateaux complex of Cainozoic sediments is part of a continuous landform extending from the south (Dundas tableland). It is flanked by subdued ridges and dunefields (Darragan, Quantong) as well as residual fans and aprons (Ullswater) to the north. The level plain is the major landform feature with gently undulating sand plains, swamps/playas and lunettes also occurring. Soils include brown and yellow grey sodic texture contrast soils (Sodosols) with grey and brown cracking clay soil (Vertosols) in local depressions. Sandy soils or soils with a deep sandy surface (Tenosols) occur on the crests and lunettes. Wind erosion is a local issue where topsoils are light textured and exposed. This unit is used for dryland cropping and grazing (sheep, beef cattle). Remnant vegetation communities include Plains Woodland, Creekline Sedgy Woodland, Shallow Sands Woodland, Red Gum Wetland, Plains Grassy Woodland, Heathy Woodland and Cane Grass Wetland.
WLRA Landform Telangatuk plains

WLRA Landform Telangatuk plains
Cropped plains at Telangatuk East
WLRA Landform Telangatuk plains

WLRA Landform Telangatuk plains

WLRA Landform Telangatuk plains
Majestic red gum near Telangatuk East

Component
1
2
3
4
Proportion of soil-landform unit
10%
5%
60%
25%
CLIMATE
Rainfall (mm)
Annual: 515
Temperature (oC)
Minimum 8, Maximum 20
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Neogene marine sand and silt (Parilla Sand); Quaternary paludal silt and clay; Neogene marine sand, sandstone, silt laterite (Dorodong Sand);
Quaternary alluvial gravel, sand and silt
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: dryland cropping; sheep and beef cattle grazing
TOPOGRAPHY
Landscape
Flat plain
Elevation range (m)
149–202
Local relief (m)
1–2
Drainage pattern
Dendritic
Drainage density (km/km2)
0.5
Landform
Gently undulating plains
Landform element
Swamp/playa
Lunette
Level plain
Sandsheet/plain
Slope and range (%)
0 (0-1)
5 (3-10)
1 (0-3)
3 (1-6)
Slope shape
Concave
Convex
Straight
Linear
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (34.0%), Creekline Sedgy Woodland (18.0%), Plains Grassy Woodland (8.0%), Other 38.0%)
SOIL
Parent material

Paludal silt and clay

Aeolian sand

Marine sand and silt, paludal silt and clay

Aeolian sand
Description
(Corangamite Soil Group)
Seasonally wet soils: sodic yellow and grey texture contrast soils (33)
Sodic brown, yellow and grey texture contrast soils (38) and sandy soils with and without pans (31)
Grey and brown cracking clay soils (37) and sodic brown, yellow and grey texture contrast soils (38)
Sodic brown, yellow and grey texture contrast soils (38) and sandy soils with and without pans (31)
Soil type sites
NA171, NA141, NA178
LSWW11, LSWW17, WLRA74
LS3, LSWW9, LSWW5
LSWW11, LSWW17, WLRA74
Surface texture
Sand
Loamy sand
Loamy sand to medium clay
Loamy sand
Permeability
Very slow
Moderate to high
Slow
Moderate to high
Depth (m)
> 1.5
> 1.5
> 2
> 1.5
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Susceptible to seasonal inundation, waterlogging and ultimately soil salinity. Upper soils susceptible to sheet erosion and wind erosion when exposed. 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.Susceptible to inundation and waterlogging in lower areas. Slightly susceptible to surface sheet erosion where soils are exposed and sandy. Clayey surface soils are friable and only slightly susceptible to wind erosion. Soils susceptible to compaction at critical moisture contents.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.
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