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Soil/Landform Unit 141

Landform Unit Description

Unit 141 image a
Depression and plains on the eastern margin of the lunette near Lake Durdeduke
      Area: 618 ha
      0.05% of CMA region

      A small depositional area developed from a swamp can be found to the west of Lake Murdeduke and north of Winchelsea. Basaltic plains (Unit 117) to the north and east, a lunette complex to the west (Unit 146) and alluvium to the south (Unit 156) surround this unit. The soils are grey and black cracking clays (Vertosols) that may be self-mulching. Remnant vegetation on these level plains has been cleared previously. Rainfall is moderate to low favouring cropping, particularly where friable organic rich surface soils exist. Site drainage is slow to very slow making the unit susceptible to waterlogging. The expansive clays generally require specific moisture conditions for maximum agricultural utility.
Unit 141 geomorphology

Unit 141 image b
Basalt floaters
Unit 141 cross section

Unit 141 graph

Unit 141 image c
Slopes of unit
43 that boraders this unit and a swamp
associated with Lake Murdeduke

Component
1
2
Proportion of soil-landform unit
95
5%
CLIMATE
Rainfall (mm)

Annual: 610
Temperature (oC)
Minimum 9, Maximum 19
Precipitation less than potential evapotranspiration
October-March
GEOLOGY
Age and lithology

Quaternary basalt and alluvium
Geomorphology
LANDUSE
Cleared: Sheep and beef cattle grazing; cropping (cereal)
TOPOGRAPHY
Landscape

Level plains
Elevation range (m)
77-88
Local relief (m)
1-2
Drainage pattern
Dendritic
Drainage density (km/km2)
1.7
Landform
Plains
Open depressions
Landform element
Slope and range (%)
0 (0-1)
1 (0-2)
Slope shape
Straight
Concave
NATIVE VEGETATION
Ecological Vegetation Class

Absent
SOIL
Parent material

Basaltic colluvium and alluvium

Basaltic colluvium and alluvium
Description
(Corangamite Soil Group)
Grey cracking clays (31)
Grey cracking clays (31)
Soil type sites
SW97, MM75, CLRA15
SW37, MM75, CLRA15
Surface texture
Light clay
Medium clay
Permeability
Low
Very low
>2Depth (m)
>2
>2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS
Expansive clay soils with a high nutrient holding capacity. Poor site drainage may lead to waterlogging and compaction.
Expansive clay soils with a high nutrient holding capacity. Very poor site drainage of these soil types may lead to innundation, waterlogging and compaction.
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