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Soil/Landform Unit 136

Landform Unit Description

Unit 136 image a
The gently undulating plains have a geater density and depth of dissection further south near Lismore. Above is an example of the broad drainage depressions undulating across the plains
      Area: 58 432 ha
      4.38% of CMA region

      The gently undulating plains that exist between Lismore and Skipton have well developed regolith profiles on Quaternary basalt within the Western Plains. These gently undulating plains may have some stone on the surface on the gentle crests and upper slopes. The soils are texture contrast with variable depth surface horizons that are often shallow with sporadically bleached subsurfaces over strongly sodic medium or heavy clay subsoils. Local relief is low with a sparse drainage network and depressions generally having similar soils to the slopes. This drainage network does become more pronounced further south towards Lismore. The only significant vegetation class of these plains is the Plains Grassland/Plains Grassy Woodland Mosaic (0.9%). This is a large unit with few outliers, surrounded by other basaltic areas (including stony rises) and granite to the north. This unit surrounds a granitic unit (Unit 143) centred to the north of Lismore. The land use is extensively cropping and grazing (mainly sheep). Land degradation issues include waterlogging and overland due to the low relief and sometimes hardsetting sufaces.
Unit 136 geomorphology

Unit 136 image b
Crops are extremely productive on these gentle plains
with deeply developed regolith
Unit 136 cross section

Unit 136 graph

Unit 136 image c
uch of these plains are cropped and grazed in rotations

Component
1
2
3
4
Proportion of soil-landform unit
5%
50%
38%
7%
CLIMATE
Rainfall (mm)

Annual: 620
Temperature (oC)
Minimum 8, Maximum 19
Precipitation less than potential evapotranspiration
October-April
GEOLOGY
Age and lithology

Quaternary basalt, Neogene fluvio-marine sand, silt and clay
Geomorphology
LANDUSE
Uncleared areas: Nature conservation
Cleared areas: Sheep and cattle grazing; cropping (cereal); softwood plantations; water supply
TOPOGRAPHY
Landscape

Gently undulating basalt plains
Elevation range (m)
114-329
Local relief (m)
20
Drainage pattern
Dendritic
Drainage density (km/km2)
0.5
Landform
Low rises
Plains
Drainage depressions
Landform element
Broad low crests and stony rises
Long gentle slopes
Broad plains
Drainage lines and depressions
Slope and range (%)
4 (2-8)
2 (1-5)
1 (0-3)
3 (0-5)
Slope shape
Convex
Linear
Straight
Concave
NATIVE VEGETATION
Ecological Vegetation Class

Plains Gassland / Plains Grassy Woodland Mosaic (0.9%)
SOIL
Parent material

Basalt

Basalt and colluvium

Basalt

Basalt colluvium and
alluvium
Description
(Corangamite Soil Group)
Alkaline, mottled brown, grey or yellow texture contrast soils, shallow surface horizons (35)
Alkaline, mottled brown, grey or yellow texture contrast soils, shallow surface horizons (35)
Alkaline, mottled brown, grey or yellow texture contrast soils, shallow surface horizons (35)
Alkaline, mottled brown, grey or yellow texture contrast soils, shallow surface horizons (35)
Soil type sites
Surface texture
Clay loam
Clay loam
Clay loam
Clay loam
Permeability
Low
Low
Low
Very low
Depth (m)
<1.5
<2
<2
>2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS
Texture contrast soil, moderate water holding capacity and nutrient holding capacity in shallow surface and subsurface soils, higher in deep subsoil. Some stones, but mottled; low permeability. Strongly sodic subsoil, possible surface soil associated with poor drainage. Moderate site drainage.
Texture contrast soil, moderate water holding capacity and nutrient holding in shallow surface and subsurface soils, higher in deep subsoil. Some stones, but mottled; low permeability. Strongly sodic subsoil, possibly surface soil associated with poor drainage. Slow to moderate site drainage.
Texture contrast soil, moderate water holding capacity and nutrient holding capacity in shallow and deeper surface and subsurface soils, higher in deep subsoil. Some stones, mottled, low permeability. Strongly sodic subsoil, possible surface soil associated with poor drainage. Slow site drainage.
Texture contrast soil, moderate water holding capacity and nutrient holding capacity in shallow and deeper surface and subsurface soils, higher in deep subsoil. Very low to low permeabiity. Strongly sodic subsoil, possible surface soil associated with poor drainage. Very slow site drainage.
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