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Paraparap Land System

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Between the lateritic plateaux of the Gherang Gherang land system and the basaltic plains of the Freshwater Creek land system, a long narrow plain extends from the Barwon River near Winchelsea to the middle reaches of Thompson Creek.

Deeply weathered duplex soils are found on most of this land system, with occasional areas of aeolian sand. Remnants of woodlands and open forests are found along many reserves with the unusual occurrence of Eucalyptus pauciflora on many of the better-drained and less fertile sites.

Most areas have been cleared for agriculture and, despite the fairly low rainfall, dairy farming is common. Other uses include sheep and beef cattle grazing and cereal cropping. Soil salting is a problem in many areas and some minor gully erosion has also occurred.
A Study of land in the catchments of the Otway Range and adjacent plains - paraparap

A Study of land in the catchments of the Otway Range and adjacent plains - paraparap

Clearing has been widespread, but an abundance of vegetation
in the road reserve adds an appealing dimension to the landscape.

A Study of land in the catchments of the Otway Range and adjacent plains - paraparap


Area: 138 km
2
Component and its proportion of land system
1
35%
2
30%
3
10
4
15%
5
10%
CLIMATE
Rainfall, mm
Annual: 600 – 650, lowest January (30), highest August (65)
Temperature, 0oC
Annual: 13, lowest July (9), highest February (19)
Temperature: less than 10oC (av.) June – July
Precipitation: less than potential evapotranspiration October – mid April
GEOLOGY
Age, lithology

Plio-Pleistocene sediments consisting of clayey sand, sandy clay and lateritic detritus
Recent aeolian sand
TOPOGRAPHY
Landscape

Gently undulating plain lying between basalt to the north and lateritic plateaux to the south
Elevation, m
40 – 130
Local relief, m
20
Drainage pattern
Dendritic
Drainage density, km/km2
2.5
Land form
Gentle rise
Valley floor
Land form element
Crest, upper slope
Middle slope
Crest, slope
Lower slope
-
Slope (and range), %
3 (0-11)
4 (1-7)
5 (2-10)
4 (0-7)
1 (0-2)
Slope shape
Convex
Linear
Irregular
Convex
Concave
NATIVE VEGETATION
Structure

Open forest

Woodland

Low woodland

Woodland

Woodland
Dominant species
E. viminalis, E. ovata,
E. pauciflora, Acacia melanoxylon
E. viminalis, E. ovata, Casuarina stricta,
C. littoralis
E. viminalis, E. obliqua
E. ovata, E. viminalis, Casuarina stricta
E. camaldulensis,
E. viminalis, Acacia melanoxylon
SOIL
Parent material

Sandy clay

Sandy clay

Siliceous sand

Sandy clay

Sand, silt and clay
Description
Mottled yellow and red duplex soils
Yellow-brown sodic duplex soils, coarse structure
Grey sand soils, uniform texture
Yellow sodic duplex soils
Brown gradational soils
Surface texture
Sandy loam
Fine sandy loam
Loamy sand
Sandy loam
Fine sandy loam
Permeability
Moderate
Low
Very high
Moderate
High
Depth, m
>2
>2
>2
>2
>2
LAND USE
Cleared areas: Dairy and beef cattle grazing on mainly improved pastures; cereal cropping; some sand extraction.
SOIL DETERIORATION HAZARD
Critical land features, processes, forms
Low inherent fertility, phosphorus fixation and leaching of permeable A horizons leads to nutrient decline.
Dispersible subsoils are prone to gully erosion and slumping of road batters.
Low inherent fertility and high permeability lead to nutrient decline. Weakly structured surfaces with low water-holding capacity are prone to wind erosion.
Sodic subsoils with high seasonal water tables are prone to soil salting. Dispersible subsoils are prone to gully erosion.
Seasonal saline water table development leads to soil salting. Rapid surface run-off from adjacent areas leads to scouring and gully erosion. Weakly structured surface soils in poorly drained areas are prone to compaction.
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