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

Victorian Resources Online

Soil/Landform Unit - Yarriambiack/Dunmunkle Creek

Landform Unit Description

WLRA Landform Yarriambiack - Dunmunkle Creek
View south towards the Western Uplands along Yarriambiack Creek
      Area: 20 445 ha
      0.87% of CMA region

      This unit of very low relative relief terrain of floodplains and terrace plains consists of the two major tributaries Dunnmunckle Creek and Yarriambiack Creek. This alluvial complex is part of the Northern Riverine Plains modern floodplains and sits within the clay plains to the east and west, older alluvial plain, and ridge and depression terrain. The floodplain, terrace plain, prior stream channels and terrace flats all occur on these creeks. Drainage consists of concentrating flow from the plains and loses topographical expression as the streams go north. Sodic grey texture contrast soils (Sodosols) with grey cracking clay soil (Vertosols) occur on the floodplains and depressions. Inundation and waterlogging are the main land degradation issues. Land use includes dryland cropping, grazing (sheep and cattle), water supply, recreation, nature conservation, residential development and hardwood forestry. Remnant vegetation communities include Plains Savannah, Lignum Swampy Woodland, Plains Woodland, Riverine Chenopod Woodland, Ridged Plains Mallee and Low Rises Woodland.
WLRA Landform Yarriambiack - Dunmunkle Creek

WLRA Landform Yarriambiack - Dunmunkle Creek
Plains on the western extent of Yarriambiack Creek
WLRA Landform Yarriambiack - Dunmunkle Creek

WLRA Landform Yarriambiack - Dunmunkle Creek

WLRA Landform Yarriambiack - Dunmunkle Creek
Black box near Murtoa

Component
1
2
3
4
Proportion of soil-landform unit
55%
30%
5%
10%
CLIMATE
Rainfall (mm)
Annual: 385
Temperature (oC)
Minimum 9, Maximum 22
Precipitation less than potential evapotranspiration
September–April
GEOLOGY
Age and lithology
Quaternary fluvial silt sand and minor gravel (Shepparton Formation); Neogene marine sand and silt (Parilla Sand)
Geomorphology
LANDUSE
Uncleared areas: water supply; nature conservation
Cleared areas: water supply; dryland cropping; sheep and beef cattle grazing
TOPOGRAPHY
Landscape
Alluvial plains
Elevation range (m)
91–161
Local relief (m)
3
Drainage pattern
Dendritic
Drainage density (km/km2)
1.0
Landform
Alluvial plains
Landform element
Floodplain
Terrace plain
Terrace flat
Prior stream
Slope and range (%)
3 (2-6)
2 (1-5)
1 (0-3)
2 (0-5)
Slope shape
Concave
Straight
Straight
Straight
NATIVE VEGETATION
Ecological Vegetation Class
Riverine Chenopod Woodland (42.7%), Plains Woodland (14.9%), Plains Savannah (14.2%), Lignum Swampy Woodland (13.5%), Other (13.0%)
SOIL
Parent material
Fluvial gravel, sand and silt, marine sand and silt
Alluvial gravel, and and silt
Alluvial gravel, and and silt
Alluvial gravel, sand and silt
Description
(Corangamite Soil Group)
Sodic grey texture contrast soils (21) and cracking clay soils (22)
Sodic grey texture contrast soils (21)
Sodic grey texture contrast soils (21)
Sodic grey texture contrast soils (21) and cracking clay soils (22)
Soil type sites
Surface texture
Sandy clay loam to medium clay
Sandy clay loam
Sandy clay loam
Sandy clay loam to medium clay
Permeability
Very slow
Slow
Slow
Very slow
Depth (m)
> 3
> 3
> 3
> 3
LAND CHARACTERISTICS, POTENTIAL AND LIMITATIONS

Critical land features, processes, forms
Floodplains are susceptible to inundation and waterlogging. Surface soils can be susceptible to sheet and rill erosion along with compaction at critical moisture contents. Slight susceptibility of surface soil to acidification.Terrace plains are susceptible to seasonal inundation and waterlogging. Surface soils can be susceptible to sheet and rill erosion along with compaction at critical moisture contents. Slight susceptibility of surface soil to acidification.Flat areas susceptible to inundation and waterlogging, but can be variable due to micro relief (gilgai). Soil compaction can occur at critical moisture contents. Slight susceptibility of surface soil to acidification.Prior stream plains are generally hardsetting (weakly structured) and experience periodic waterlogging. Surface soils can be susceptible to rill erosion during storm events. Slight susceptibility of surface soil to acidification and compaction.
Page top