Your gateway to a wide range of natural resources information and associated maps

Victorian Resources Online

Soil/Landform Unit - Ullswater plains and rises

Landform Unit Description

WLRA Landform Ullswater plains and rises
Landscapes with swamps, sand plains, gentle rises and clay plains near Karnak
      Area: 60 933 ha
      2.60% of CMA region

      Rises (ridges), plains and depressions (lakes and lunettes) that occur north-east of Edenhope and also south of Natimuk form part of the ridge/depression complex of the North West Dunefields and Plains. This low ridge and depression (with lakes and lunettes) complex of Cainozoic aeolian and lacustrine sediments is part of a NNW/SSE orientated terrain surrounded by sand plains and associated rises/ridges (Kowree) and other ridge /depression units to the north (Goroke). Plains and ridges are found along with swamps/playas/lakes and lunettes, and sandsheet/plain. Drainage is strongly aligned to the terrain with little surface expression apart from local depressions. Soil types include brown and yellow grey sodic texture contrast soils (Sodosols) with grey and brown cracking clay soils (Vertosols) on plains and in local depressions. Sandy soils or soils with a deep sandy surface occur on the crests and lunettes. Sheet and rill erosion is possible for slopes in this unit. Soil compaction may be an issue on heavier soils. This unit is used for dryland cropping and grazing (sheep, beef cattle). Vegetation communities such as Red Gum Wetland, Plains Woodland, Shallow Sands Woodland and Damp Sands Herb-rich Woodland are some of the more expansive remnant vegetation types.
WLRA Landform Ullswater plains and rises

WLRA Landform Ullswater plains and rises
String of West Wimmera lakes and swamp surrounded by plains and stranded beach ridges rises
WLRA Landform Ullswater plains and rises

WLRA Landform Ullswater plains and rises

WLRA Landform Ullswater plains and rises
Lakes within the Ullswater plains

Component
1
2
3
4
5
Proportion of soil-landform unit
15%
30%
35%
7%
13%
CLIMATE
Rainfall (mm)
Annual: 555
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep and beef cattle grazing
TOPOGRAPHY
Landscape
Plains and rises
Elevation range (m)
128–202
Local relief (m)
2–3
Drainage pattern
Dendritic
Drainage density (km/km2)
0.6
Landform
Gently undulating plains
Landform element
Playa/water holding body (common alignment NNW-SSE with multiple in row - often 3)
Level plain
Ridge
Lunette
Sandsheet
Slope and range (%)
0 (0-1)
1 (0-3)
3 (1-6)
4 (1-6)
2 (1-4)
Slope shape
Concave
Straight
Convex
Convex
Linear
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (44.8%), Red Gum Wetland (14.6%), Shallow Sands Woodland (7.0%), Water Body – Fresh (7.0%), Other (25.8%)
SOIL
Parent material

Paludal silt and clay

Maine sand and silt, paludal silt and clay

Maine sand and silt

Aeolian sand

Aeolian sand
Description
(Corangamite Soil Group)
Seasonally wet soils: sodic yellow and grey texture contrast soils (33)
Grey and brown cracking clay soils (37) and sodic brown, yellow and grey texture contrast soils (38)
Sodic red texture contrast soils (39)
Sodic brown, yellow and grey texture contrast soils (38) and sandy soils with and without pans (31)
Sodic brown, yellow and grey texture contrast soils (38)
Soil type sites
NA171, NA141, NA178
LS3, LSWW9, LSWW5
NA174
LSWW11, LSWW17, WLRA74
LSWW11, LSWW17, LSWW13
Surface texture
Sandy clay
Loamy sand to medium clay
Sandy loam
Loamy sand
Loamy sand
Permeability
Very slow
Slow
Moderate
Moderate to high
Moderate
Depth (m)
> 2
> 2
< 2
> 1.5
> 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Susceptible to seasonal inundation, waterlogging and ultimately soil salinity. 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.Hardsetting upper soil susceptible to sheet and rill erosion along with wind erosion when exposed. Dispersive and deep subsoils susceptible to gully erosion on steeper slopes. Susceptible to compaction depending on soil depth and moisture content. 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.
Page top