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Soil/Landform Unit 179

Landform Unit Description

Unit 179 image a
Soils are derived from Quaternary volcanics with influence from surrounding granite and sedimentary hills. The soils are likely to experience soil compaction without controlled traffic and organic matter inputs into the topsoil
      Area: 604 ha
      0.05% of CMA region

      The gently undulating plains on Quaternary basalt occur near Anakie. Much of the land has been cleared with Plains Grassy Woodland and Creekline Grassy Woodland the dominant vegetation classes. Land use is mainly cropping (cereal) and grazing. Soils are typically alkaline mottled brown texture contrast in nature. While waterlogging is a minor limitation (dependent upon season and rainfall), soil compaction is a limitation for production of soils with shallow topsoils.
Unit 179 geomorphology

Unit 179 image b
Cropping and grazing are the major land uses of these fertile plains near Anakie
Unit 179 cross section

Unit 179 graph

Unit 179 image c
Sheep grazing on the undulating plains near Anakie

Component
1
2
Proportion of soil-landform unit
85%
15%
CLIMATE
Rainfall (mm)

Annual: 640
Temperature (oC)
Minimum 8, Maximum 19
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

Quaternary basalt, minor
Devonian granite
Geomorphology
LANDUSE
Uncleared areas: Water supply; nature conservation
Cleared areas: Sheep and beef cattle grazing; cropping (cereal); water supply
TOPOGRAPHY
Landscape

Gently undulating plains
Elevation range (m)
108–195
Local relief (m)
3
Drainage pattern
Dendritic
Drainage density (km/km2)
2.0
Landform
Plain
Landform element
Gentle plain
Drainage depression/line
Slope and range (%)
2 (1–4)
1 (0–3)
Slope shape
Straight
Convex
NATIVE VEGETATION
Ecological Vegetation Class

Plains Grassy Woodland (5.2%), Creekline Grassy Woodland (0.2%)
SOIL
Parent material

Volcanic silt and gravel

Clay and silt
Description
(Corangamite Soil Group)
Mottled brown texture contrast soils (36)
Grey and brown gradational soils (31)
Soil type sites
SW37, MM5060, CLRA15
Surface texture
Fine sandy loam
Loam to light clay
Permeability
Low
Very low
Depth (m)
>2
>2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS
Slowly permeable soils and hardsetting surfaces result in overland flow and waterlogging. Soil compaction is also a limitation for soils with shallow topsoils.
Moderate to high nutrient holding capacity in upper soil, high in subsoil. Moderate to high water holding capacity, moderately deep to deep soil. Very low permeability. Strongly sodic in subsoil. Expansive clay soils, very slow site drainage.
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