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Soil/Landform Unit - Merryvale lakes and ridges

Landform Unit Description

WLRA Landform Merryvale lakes and ridges
Looking west towards lakes within the swales between former beach ridges
      Area: 1409 ha
      0.06% of CMA region

      This unit of low-lying terrain consists of a single depression (lake and lunette) complex about 25 km north-east of Edenhope. This plain, depression and associated rise (lunette) are part of North West Dunefields and Plains; more specifically they are part of the low ridge tops with remnant sands and orientated depressions (5.5.2). This low-lying plain occurs between NNW/SSE low sandy ridges. Plains, flats, drainage depression and a lunette occur as landscape components. Receiving drainage from the surrounding rises (low ridges), soils include yellow, brown and grey sodic texture contrast soils, with grey and brown cracking clay soils (Vertosols) in the depression. These clays occur on the dune as well as occasional red sodic texture contrast soils (Sodosols) associated with the crests. Sheet and wind erosion susceptibility is associated with the lighter topsoils of exposed crests. Compaction is also a potential land degradation susceptibility, as is waterlogging in the depression and to some extent the plain, where topsoil is shallow. Remnant vegetation is composed of vegetation communities such as Damp Sands Herb-rich Woodland, Red Gum Wetland, Brackish Lake Mosaic, Lunette Woodland and Plains Woodland.
WLRA Landform Merryvale lakes and ridges

WLRA Landform Merryvale lakes and ridges
Overgrown dried lake bed amid plains near Karnak
WLRA Landform Merryvale lakes and ridges

WLRA Landform Merryvale lakes and ridges

WLRA Landform Merryvale lakes and ridges
Gently undualting sandy rises near Karnak

Component
1
2
3
Proportion of soil-landform unit
70%
10%
20%
CLIMATE
Rainfall (mm)
Annual: 540
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology
Neogene marine sand and silt (Parilla Sand); Quaternary paludal silt and clay; Quaternary aeolian dune sand (Lowan Sand)
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep grazing
TOPOGRAPHY
Landscape
Lakes and lunette complex
Elevation range (m)
151–165
Local relief (m)
1
Drainage pattern
Dendritic
Drainage density (km/km2)
0.7
Landform
Playa plains
Landform element
Plain
Lunette
Closed depression
Slope and range (%)
1 (1-3)
5 (1-10)
0 (0-1)
Slope shape
Straight
Convex
Concave
NATIVE VEGETATION
Ecological Vegetation Class
Plains Woodland (50.0%), Brackish Lake Mosaic (25.4%), Red Gum Wetland (16.4%), Other (8.2%)
SOIL
Parent material

Marine sand and silt

Aeolian sand

Paludal silt and clay
Description
(Corangamite Soil Group)
Sodic brown, yellow and grey texture contrast soils (38)
Grey and brown cracking clay soils (37) and sodic red texture contrast soils (39)
Grey and brown cracking clay soils (37)
Soil type sites
LSWW11, LSWW17, LSWW13
NA174, LS3, LSWW9
LS3, LSWW9, LSWW5
Surface texture
Loamy sand
Light clay
Medium clay
Permeability
Moderate
Moderate - slow
Slow
Depth (m)
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 sheet and rill erosion along with wind erosion when exposed. Dispersive and deep subsoils susceptible to gully erosion on steeper slopes. Compaction of upper soil variable depending on soil depth and moisture content.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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