Your gateway to a wide range of natural resources information and associated maps

Victorian Resources Online

Soil/Landform Unit - Darragan rolling rises

Landform Unit Description

WLRA Landform Darragon rolling rises
Rolling rises to the north-east across a corridor to a former stranded beach ridge
      Area: 9491 ha
      0.40% of CMA region

      Rolling rises south of Horsham represent a sequence of ferruginised Neogene sediments (Parilla Sand) as part of the prominent ridges with eroded ferruginised northern spurs of the North Western Dunefields and Plains (5.5.3). Comprising rolling rises and defined drainage lines, major soils include sodic red and brown texture contrast soils (Sodosols) with cracking clays (Vertosols) confined to lower drainage depressions and flats. Soils are prone to compaction due to hardsetting surfaces that benefit from organic matter contributions to improve soil structure. Land use is variable between dryland cereal cropping, sheep and cattle grazing and occasional intensive industries (e.g. viticulture). Dominant woodland remnant vegetation includes Heathy Woodland, Riverine Chenopod Woodland, Grassy Woodland, Creekline Sedgy Woodland, Plains Woodland and Shallow Sands Woodland. Sandstone Ridge Shrubland is also found along ridges and rises in the landscape.
WLRA Landform Darragon rolling rises

WLRA Landform Darragon rolling rises
Ferruginised Parilla Sand cutting
WLRA Landform Darragon rolling rises

WLRA Landform Darragon rolling rises

WLRA Landform Darragon rolling rises
Looking southwards across cropped plains towards a rolling rise

Component
1
2
Proportion of soil-landform unit
10%
90%
CLIMATE
Rainfall (mm)

Annual: 500
Temperature (oC)
Minimum 8, Maximum 21
Precipitation less than potential evapotranspiration
October–April
GEOLOGY
Age and lithology

Neogene marine sand and silt (Parilla Sand);
Quaternary alluvium, gravel, sand and silt
Geomorphology
LANDUSE
Uncleared areas: nature conservation
Cleared areas: dryland cropping; sheep and beef cattle grazing; gravel extraction
TOPOGRAPHY
Landscape

Rolling rises
Elevation range (m)
117–193
Local relief (m)
10–15
Drainage pattern
Parallel
Drainage density (km/km2)
0.5
Landform
Rises
Landform element
Creek/drainage line
Rolling to undulating rise
Slope and range (%)
4 (1-7)
6 (3-10)
Slope shape
Convex
Concave
NATIVE VEGETATION
Ecological Vegetation Class

Grassy Woodland (35.0%), Plains Woodland (32.5%), Creekline Sedgy Woodland (13.3%), Sandstone Ridge Shrubland (12.6%), Other (6.1%)
SOIL
Parent material

Alluvial gravel, sand and silt

Marine sand and silt
Description
(Corangamite Soil Group)
Grey and brown cracking clay soils (37)
Sodic red and brown texture contrast soils (40)
Soil type sites
LS3, LSWW9, LSWW5
Surface texture
Medium clay
Loamy sand
Permeability
Slow
Moderate
Depth (m)
> 2
< 2
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Susceptible to inundation and waterlogging in lower areas. Slightly susceptible to surface sheet erosion where soils are exposed. Surface soils are friable and only slightly susceptible to wind erosion. Soils are susceptible to compaction at critical moisture contents.Weakly structured or hardsetting upper soil susceptible to sheet and rill erosion especially where significant slopes occur. Sandy surfaces can be susceptible to wind erosion. Dispersive and deep subsoils susceptible to gully erosion on steeper slopes. Ferricrete occurs at depth.
Page top