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Yeodene Creek Land System

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West of Yeodene, a rolling and irregular landscape forms part of a broad ridge extending from the foothills of the Ranges towards Colac. Tertiary sand outcrops on most parts of the landscape, often forming a veneer over exposures of Tertiary silt and clay.

The soils have loamy sand or sandy loam surface textures and are prone to nutrient and moisture deficiencies. Hardpans between the sand veneers and clay horizons may result in perched water tables, although only small areas have such poor site drainage that frequent waterlogging occurs.

Sand and gravel have been extensively mined in some areas, and pine plantations have been established near Yeodene. However, most of the area remains in a fairly natural state and constitutes a significant area of natural vegetation close to Colac. Its potential for recreation is at present not fully utilized. Only minor areas have been cleared for agriculture, but the establishment of improved pastures is difficult.
A Study of land in the catchments of the Otway Range and adjacent plains - yeodene

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

Acid sands in this comparatively dry area will not support vigorous
pastures and the control of weeds such as Pteridium esculentum
and
Rubus spp. is difficult.

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


Area: 58 km
2
Component and its proportion of land system
1
35%
2
25%
3
5%
4
30%
5
5%
CLIMATE
Rainfall, mm

Annual
: 750 – 850, lowest January (40), highest August (100)
Temperature, 0oC
Annual: 13, lowest July (8), highest February (9)
Temperature: less than 10oC (av.) June – August
Precipitation: less than potential evapotranspiration late October – early April
GEOLOGY
Age, lithology

Paleocene unconsolidated sand, silt and clay

Recent sand veneer
TOPOGRAPHY
Landscape

Rolling plain in the western parts of the Barwon catchment and northern parts of the Gellibrand catchment
Elevation, m
120 – 260
Local relief, m
40
Drainage pattern
Dendritic
Drainage density, km/km2
1.5
Land form
Plain
Land form element
Crest, slope
Slope
Broad slightly depressed area
Crest, slope
Drainage line
Slope (and range), %
9 (1-15)
15 (5-20)
2 (0-5_
8 (1-15)
3 (1-5)
Slope shape
Convex
Irregular
Concave
Linear
Concave
NATIVE VEGETATION
Structure

Woodland

Woodland

Low woodland

Open forest

Low woodland
Dominant species
E. viminalis, E. obliqua,
E. radiata
E. radiata, E. ovata,
E. viminalis
, occasionally E. obliqua
E. nitida, E. radiata, occasionally E. viminalis
E. obliqua, E. radiata
E. ovata, Acacia melanoxylon, Leptospermum juniperinum, Melaleuca squarrosa
SOIL
Parent material

Quartz sand

Silt and clay with sand veneer

Silt and clay with sand veneer

Clay, silt and sand

Colluvial and alluvial sand, silt and clay, plant remains
Description
Grey sand soils, uniform texture
Grey sand soils, weakly structured clay underlay
Grey sand soils, weakly structured clay underlay
Yellow gradational soils, weak structure
Black sand soils, uniform texture
Surface texture
Loamy sand
Loamy sand
Loamy sand
Sandy loam
Silty loam
Permeability
Very high
Low
Low
High
Moderate
Depth, m
>2
>2
0.6
>2
>2
LAND USE
Uncleared areas: Hardwood forestry for posts, poles and fuel; sand and gravel extraction; forest grazing; water supply; passive and active recreation; softwood forestry.
Minor cleared areas: Sheep and beef cattle grazing; dairy farming
SOIL DETERIORATION HAZARD
Critical land features, processes, forms
Very low inherent fertility and high permeability lead to nutrient decline.
Low inherent fertility and leaching of permeable surfaces lead to nutrient decline. Weakly structured surfaces and low permeabilities lead to sheet erosion on steeper slopes.
Low permeability and poor site drainage lead to seasonal waterlogging and soil compaction.
Weakly structured surfaces on steeper slopes are prone to sheet erosion.
High water tables lead to waterlogging and soil compaction. Run-off from adjacent hills leads to siltation and flooding.
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